Class
Book_
Copyright N°.
COPYRIGHT DEPOSIT.
DEDICATED
TO
MY DISTINGUISHED GUIDES THROUGH THE UPPER
PALEOLITHIC CAVERNS OF
THE PYRENEES, DORDOGNE, AND THE CANTABRIAN MOUNTAINS OF SPAIN
EMILE CARTAILHAC
HENRI BREUIL
HUGO OBERMAIER
1
w <
w u
§ Q
& <
glacial time.)
LOWER PALEOLITHIC
4. Mousterian. (Fourth Glacial
" 40,000.
time.) — j
3. Acheulean. (Transition to
River-
Drift and
Terrace
Period.
shelters.)
2. Chellean.
" 100,000.
1. Pre-Chellean (Mesvinian.)
EOLITHIC.
* This table is a modification of that of Obermaier in his Mensch der Vorzeit.zi To each period
of the chronologic reckoning should be added the 1900 years of our era.
Geologic History of Man
Man emerges from the vast geologic history of the earth in
the period known as the Pleistocene, or Glacial, and Postglacial,
the 'Diluvium' of the older geologists. The men of the Old
Stone Age in western Europe are now known through the latter
GEOLOGIC HISTORY OF MAN 19
half of Glacial times to the very end of Postglacial times, when
the Old Stone Age, with its wonderful environment of mammalian
and human life, comes to a gradual close, and the New Stone
Age begins with the climate and natural beauties of the forests,
meadows, and Alps of Europe as they were before the destroying
hand of economic civilization fell upon them.
It is our difficult but fascinating task to project in our imag-
ination the extraordinary series of prehistoric natural events
which were witnessed by the successive races of Palaeolithic men
in Europe ; such a combination and sequence never occurred be-
fore in the world's history and will never occur again. They
centred around three distinct and yet closely related groups of
causes. First, the formation of the two great ice-fields centring
over the Scandinavian peninsula and over the Alps ; second, the
arrival or assemblage in western Europe of mammals from five
entirely different life-zones or natural habitats; third, the ar-
rival in Europe of seven or eight successive races of men by
migration, chiefly from the great Eurasiatic continent of the
East.
Throughout this long epoch western Europe is to be viewed
as a peninsula, surrounded on all sides by the sea and stretching
westward from the great land mass of eastern Europe and of
Asia, which was the chief theatre of evolution both of animal
and human life. It was the 'far west' of all migrations of
animals and men. Nor may we disregard the vast African land
mass, the northern coasts of which afforded a great southern
migration route from Asia, and may have supplied Europe with
certain of its human races such as the 'Grimaldi.'
These three principal phenomena of the ice-fields, the mam-
mals, and the human life and industry, together establish the chro-
nology of the Age of Man. In other words, there are four ways
of keeping prehistoric time: that of geology, that of palaeontology,
that of anatomy, and that of human industry. Geologic events
mark the grander" divisions of time ; palaeontologic and anatomic
events mark the lesser divisions ; while the successive phases of
human industry mark the least divisions. The geologic chro-
20 MEN OF THE OLD STONE AGE
nology deals with such immense periods of time that its ratio to
the animal and to the human chronology is like that of years to
hours and to minutes of our own solar time.
The Glacial Epoch when first revealed by Charpentier39 and
Agassiz,40 between 1837 and 1840, was supposed to correspond to
a single great advance and retreat of the ice-fields from various
centres. The vague problem of the antiquity of Pliocene man
and Diluvial man soon merged into the far more definite chro-
nology of glacial and inter glacial man. As early as 1854, Morlot
discovered near Diirnten, on the borders of the lake of Zurich,
a bed of fossil plants indicating a period of south temperate cli-
mate intervening between two great deposits of glacial origin.
This led to the new conception of cold glacial stages and warm
interglacial stages, and Morlot41 himself advanced the theory
that there had been three glacial stages separated by two inter-
glacial stages. Other discoveries followed both of fossil plants
and mammals adapted to warmer periods intervening between
the colder periods. Moreover, successive glacial moraines and
' drifts/ and successive river 'terraces' were found to confirm
the theory of multiple glacial stages. The British geologist,
James Geikie (1871-94) marshalled all the evidence for the
extreme hypothesis of a succession of six glacial and five inter-
glacial stages, each with its corresponding cold and warm climates.
Strong confirmation of a theory of four great glaciations came
through the American geologists, Chamberlin,42 Salisbury,43 and
others, in the discovery of evidence of four chief glacial and three
interglacial stages in northern portions of our own continent.
Finally, a firm foundation of the quadruple glacial theory in
Europe was laid by the classic researches of Penck and Bruckner44
in the Alps, which were published in 1909. Thus the exhaustive
research of Geikie, of Chamberlin and Salisbury, of Penck and
Bruckner, and finally of Leverett45 has firmly established eight
subdivisions or stages of Pleistocene time, namely, four glacial,
three interglacial, and one postglacial. These not only mark the
great eras of European time but also make possible the synchrony
of America with Europe.
GEOLOGIC HISTORY OF MAN
21
Since most of the skeletal and cultural remains of man can
now be. definitely attributed to certain glacial, interglacial, or
Major Divisions
Periods and Epochs
Advances in Life
Dominant Life
Quaternary.
HOLOCENE.
PLEISTOCENE,
or
ICE AGE.
Recent alluvial.
Postglacial
stage.
Glacial stages.
Rise of world civiliza-
tion.
Industry in iron, cop-
per, and polished
stone.
Extinction of great
mammals.
Dawn of mind, art,
and industry.
Age of Man.
Iron, Bronze,
and New
Stone Ages.
Men
of the
Old Stone Age.
Tertiary.
PLIOCENE.
Late Tertiary.
Transformation of
man-ape into man.
Age of
Mammals
and
Modern
Plant Life.
MIOCENE.
Culmination of mam-
mals.
OLIGOCENE.
Early Tertiary.
Beginnings of anthro-
poid ape life.
EOCENE.
Appearance of higher
types of mammals,
and vanishing of
archaic forms.
PALJEOCENE.
Rise of archaic mam-
mals.
Late
Mesozoic.
Cretaceous.
Extinction of great
reptiles.
Age
OF
Reptiles.
Extreme specializa-
tion of reptiles.
Comanchian.
Rise of flowering
plants.
Early
Mesozoic.
Jurassic.
Rise of birds and fly-
ing reptiles.
Triassic.
Rise of dinosaurs.
PLACE OF THE OLD STONE AGE IN THE EARTH'S HISTORY
(Indicated in heavy -face letter.)
Compare Schuchert's Table, 19 14.
postglacial stages, vast interest attaches to the very difficult
problem of the duration of the whole Ice Age and the relative
duration of its various glacial and interglacial stages. The fol-
22 MEN OF THE OLD STONE AGE
lowing figures set forth the wide variations in opinion on this
subject and the two opposite tendencies of speculation which
lead to greatly expanded or greatly abbreviated estimates of
Pleistocene time :
DURATION OF THE ICE AGE
1863.
Charles Lyell,46 Principles of Geology
. 800,000
years.
1874.
James D. Dana,47 Manual of Geology
.720,000
1893.
Charles D. Walcott,48 Geologic Time as Indicated by
the Sedimentary Rocks of North America
.400,000
a
1893.
W. Upham,49 Estimates of Geologic Times, Amer.
Jour. Sci., vol. XLV
. 100,000
it
1894.
A. Heim,50 Ueber das absolute Alter der Eiszeit. . . .
. 100,000
a
1900.
W. J. Sollas,51 Evolutional Geology
. 400,000
cc
1909.
Albrecht Penck,52 Die Alpen im Eiszeitalter
.520,000-
-840,000
1914.
James Geikie,53 The Antiquity of Man in Europe. .
. 620,000
(min.)
We may adopt for the present work the more conservative
estimate of Penck, that since the first great ice-fields developed
in Scandinavia, in the Alps, and in North America west of Hud-
son Bay a period of time of not less than 520,000 years has
elapsed. The relative duration of the subdivisions of the
Glacial Epoch is also studied by Penck in his Chronologie des
Eiszeitalters in den Alpen}2 These stages are not in any degree
rhythmic, or of equal length either in western Europe or in
North America.
The unit of glacial measurement chosen by Penck is the time
which has elapsed since the close of the fourth and last great
glaciation ; this is known as the Wiirm in the Alpine region and
as the Wisconsin in America. While more limited than the ice-
caps of the second glaciation, those of the fourth glaciation were
still of vast extent in Europe and in this country, so that an esti-
mate of 20,000 to 34,000 years for the unit of the entire Postglacial
stage is not extreme. Estimating this unit at 25,000 years and
accepting Reeds's54 estimate of the relative length of time occu-
pied by each of the preceding glacial and interglacial stages, we
reach the following results (compare Fig. 14, p, 41) :
GEOLOGIC HISTORY OF MAN
Relative
Duration
Grand
Totals
Descent
of Alpine
Snow-Line
Postglacial Time.
(Period of Upper Palaeolithic culture, Cro-
Magnon and Briinn races)
IV. Glacial Stage (=Wurm, Wisconsin).
(Close of Lower Palaeolithic culture, Neanderthal
race)
3d. Interglacial Stage.
(Opening period of Lower Palaeolithic culture,
Piltdown and pre-Neanderthaloid races)
III. Glacial Stage (=Riss, Illinoian)
2d. Interglacial Stage ( = Mindel-Riss, Yarmouth) . .
(Period of Heidelberg race.)
II. Glacial Stage ( = Mindel, Kansan)
1 st. Interglacial Stage ( = Gunz-Mindel, Af tonian) .
(Period of Pithecanthropus or Trinil race.)
I. Glacial Stage ( = Giinz, Nebraskan)
Units
Years
25,000
25,000
25,000
200,000
25,000
75,000
25,000
Years
25,000
50,000
150,000
175,000
37S,ooo
400,000
475,000
500,000
Meters
1,200
1,250
1,300
The Postglacial time divisions are dated by three successive
advances of the ice-caps, which broadly correspond with Geikie's
fifth and sixth glaciations ; they are known in the Alpine region
as the Buhl, Gschnitz, and Daun. These three waves of cold and
humid climate, each accompanied by glacial advances, finally
terminated with the retreat of the snow and ice in the Alpine
region, the same conditions prevailing as with the present cli-
mate. The minimum time estimates of these Postglacial stages
and the corresponding periods of human culture, as calculated by
Heim,50 Nuesch,55 Penck,52 and many others, are summarized in
the Upper Palaeolithic (p. 281).
Geologic and Human Chronology
There are four ways in which the lesser divisions and sequence
of human chronology may be dated through geologic or earth-
forming events. First, through the age of the culture stations
or human remains, as indicated by the ' river-drifts ' and 'river
terraces ' in or upon which they occur ; second, through the age
of the open ' loess' stations which are found both on the ' older
terraces' and on the plateaus between the river valleys; third,
24 MEN OF THE OLD STONE AGE
through the age of the shelters and caverns in which skeletal and
cultural remains occur ; fourth, through the age of the ' loam '
deposits, which have drifted down on the 'terraces' from the
surrounding meadows and hills. The men of the Old Stone Age
were attracted to these natural camps and dwelling-places both
by the abundance of the raw flint materials from which the palae-
oliths were fashioned and by the presence of game.
In more than ninety years of exploration only three skeletal
relics of man have been found in the ancient ' river-drifts ' ; these
are the 'Trinil,' the 'Heidelberg/ and the 'Piltdown'; in each
instance the human remains were buried accidentally with those
of extinct animals, after drifting for some distance in the river
or stream beds. It is only in late Acheulean times that human
burial rites or interments begin and that skeletal remains are
found. Owing to the less perishable nature of flint, relics of the
quarries and stations are infinitely more common; they are found
both in the river sands and gravels, in the 'river terraces/ and
in the 'loess' stations of the plateaus and uplands. Thus pre-
historic chronology is based on observations of the geologist, who
in turn is greatly aided by the archaeologist, because the evolution
stages of each type of implement are practically the same all over
western Europe, with the exception of unimportant local inven-
tions and variations. In brief, the large divisions of time are
determined by the amount of work done by geologic agencies;
the comparative age of the various camp sites is determined by
their geologic succession, by the mammals and plants which oc-
cur in them, and finally by the cultural type of any industrial
remains that may be found.
Times of the 'High' and 'Low' River 'Terraces'
The so-called 'terrace' chronology is to be used by the pre-
historian with caution, for it is obvious that the 'terraces' in
the different river-valleys of western Europe were not all formed
at the same time ; thus the testimony of the ' terraces ' is always
to be checked off by other evidence.
GEOLOGIC HISTORY OF MAN
25
As to the origin of the sands and gravels which compose the
'terraces' we know that the glacial stages were periods of the
wearing away of vast materials from the summits and sides of
the mountains, which were transported by the rivers to the
valleys and plains. These vast deposits of glacial times spread
out over the very broad surfaces of the pristine river-bottoms,
which in many valleys it is important to note were from ioo to
1 50 feet above the present levels. The diminished and contracted
N.W.
a!
.500 m
-400
0 ! 2 4 a 6 5 ro"" f2km.
Fig. 6. Terraces on either side of the valley of the River Inn, Scharding, Austria,
formed by sand and gravel deposits partly covered with loess. After Bruckner.
lb. Very broad river deposits of First Glaciation, on the first erosion level, covered
with the 'Upper Loess' of the Second Interglacial Stage.
lib. Somewhat narrower river deposits of Second Glaciation on the second erosion
level.
II lb. Still, narrower river terraces of the Third Glaciation on the third erosion
level, covered with the 'Lower Loess' of the Third Interglacial Stage.
IVb. Fourth or lowest terrace of the Fourth Glaciation on the fourth erosion level.
Va. Erosion terraces, Achen.
Via. Post-Buhl erosion.
Loess', 'Upper Loess' of Second Interglacial. Loess", 'Lower Loess' of Third In-
terglacial.
streams of interglacial times cut into these ancient river beds,
forming narrower channels into which they transported their
own materials. Thus, as the successive ' river terraces' were
formed, a descending series of steps was created along the sides
of the valleys. In many valleys there are four of these ' terraces,'
which may correspond with several glacial stages ; in other val-
leys there are only three; in others, again, like the valley of
the River Inn which flows past Innsbruck in the Tyrol (Fig. 6),
there are five ' terraces,' while in the valley of the Rhine above
Basle there are six, corresponding, it is believed, with the mate-
rials brought down by the four great glaciations and with the
river levels of Postglacial times. In general, therefore, the 'high
terraces' are the oldest ones, that is, they are composed of
26
MEN OF THE OLD STONE AGE
materials brought down during the pluvial periods of the First,
Second, and Third Glacial Stages, while the 'lower terraces'
and the 'lowest terraces' in the alpine regions are composed
of materials borne by the great rivers of the Fourth Glacial and
Postglacial Stages. In the region around the Alps the 'higher
terraces' are products chiefly of the third glaciation; in the
Rheinfdder HUL
Upper Schworstadt
-400 m
-350
km
Fig. 7. Cross-section through the terraced Pleistocene formations of the Rhine valley
above Basle, Switzerland. After Penck.
lb. Outwash of the First Glaciation — Giinz — Deposits on the first erosion level.
lib. Outwash of the Second Glaciation — Mindel — Deposits on the second erosion level.
Illb. Outwash of the Third Glaciation — Riss — Deposits on the third erosion level.
IVb. Outwash of the Fourth Glaciation — Wiirm— Deposits on the fourth erosion level.
Va. Erosion terrace, Achen oscillation — fifth erosion level.
Trrr* > Post-Buhl erosion — sixth and seventh erosion levels.
Vila. J
IIIc. Moraine of the Third Glaciation — Riss.
The section of the Rheinfelder Hill lies 3 km. west from the Moliner Field.
valley of the Rhine they are visible near Basle. On the upper
Rhine the 'low terraces' are products of the fourth glaciation;
they cover vast surfaces and contain remains of the woolly mam-
moth (E. primi genius) , an animal distinctive of Fourth Glacial
and Postglacial times.
More remote from the glacial regions, but equally subject to
the inundations of glacial times are the ' high terraces ' along the
River Seine, which are ninety feet above the present level of
the river and contain the remains of mammals characteristic
of the First Interglacial Stage, such as the southern elephant (E.
meridionalis) , while the 'low terraces' along the Seine are only
fifteen feet above the present level of the river and contain
mammals belonging to the Third Interglacial Stage. Similarly,
GEOLOGIC HISTORY OF MAN 27
the 'high terraces' of the River Eure contain mammals of First
Interglacial times, such as the southern elephant (E. meridionalis)
and Steno's horse (E. stenonis) ; these fossils occur in coarse river
sands and gravels which were deposited by a broad stream that
flowed at least ninety feet above the present waters of the
Eure.
The human interest which attaches to these dry facts of
geology appears especially in the valleys of the Somme and the
Marne in northern France; here again we find 'high terraces/
'middle terraces/ and 'low terraces'; the latter are still sub-
ject to flooding. In the deep gravels upon each of these terraces
we find the first proofs of human residence, for here occur the
earliest Pre-Chellean and Chellean implements associated with
the remains of the hippopotamus, of Merck's rhinoceros, and of
the straight- tusked elephant (E. antiquus), together with mam-
mals which are characteristic both of Second and Third Inter-
glacial times.
This raises a very important distinction, which is often mis-
understood; namely, between the materials composing the orig-
inal terraces and those subsequently deposited upon the terraces.
It appears to be in the latter that human artifacts are chiefly, if
not exclusively, found.
Times of the Loam Stations
The 'loam' which washes down over the original sand and
gravel 'terraces' from the surrounding hills and meadows is of
much later date than the 'terraces' themselves, and the archae-
ologist in the valley of the Somme as well as in that of the Thames
may well be deceived unless he clearly distinguishes between the
newer deposits of gravels and of loams and the far older gravels
and river sands which compose the original 'terraces.' This is
well illustrated by the observations of Commont on the section
of St. Acheul.56 The loams and brick-earth are of much more
recent age than the original gravels and sands of the 'terraces'
which they overlap and conceal; the lowest and oldest 'loam'
28
MEN OF THE OLD STONE AGE
{limon fendille) contains Acheulean flints, while the overlying
'loam' contains Mousterian flints. Although occurring on the
'higher terraces,' these flints are of somewhat later date than
the primitive Chellean flints which occur in the coarse gravels
and sands that have collected upon the very lowest levels (Fig. 59).
A similar prehistoric inversion doubtless occurs in the 'ter-
races' of the Thames, for materials on the 'highest terrace'
(Fig. 8) contain Acheulean flints, while materials on the 'lowest
terrace' belong to a much more recent age.
1
!
South §
r Feet
North
Eocene
Beds
100
Sea Level
CretaceousX m
ChalM \ m
•f miles
Fig. 8. Section — Four terraces indicated in the valley of the Thames at Galley
Hill, near London. Site of the discovery of the 'Galley Hill Man' in deposits
overlying one of the high terraces. Site also of Gray's Thurrock, a deposit of
Third Interglacial times containing mammals and flints of Chellean age. A
typical camping station of 'river-drift man.' Drawn by Dr. C. A. Reeds.
We have no record of a single Palaeolithic station found in the
true original sands and gravels of the 'higher terraces' in any
part of Europe ; only eoliths are found on the ' high terrace '
levels, as at St. Prest.
The earliest palaeoliths occur in the gravels on both the ' mid-
dle ' and ' upper terraces ' of the Somme and the Marne, proving
that the gravels were deposited long subsequent to the cutting
of the original terraces. Geikie,57 moreover, is of the opinion
that the valley of the Somme has remained as it is since early
Pleistocene times, and that even the 'lowest terrace' here was
completed at that period ; this is contrary to the view of Commont,
who considers that this 'lowest terrace' belongs to Third Inter-
glacial times ; a restudy of the stations along the Thames may
throw light upon this very important difference of opinion.
GEOLOGIC HISTORY OF MAN
29
Times of the 'Loess' Stations
The glacial stages were generally times of relatively great
humidity, of heavy rain and snow fall, of full rivers charged with
gravels and sands, and with loam the finest product of the ero-
Fig. 9. Magdalenian loess station of Aggsbach, in Lower Austria. A quarry-
camping station of the open-plains type. This typical Postglacial loess de-
posit contains flints of early Magdalenian age. After Obermaier.
sive action of ice upon the rocks. This loam on the barren
wastes left bare by the glaciers or on the river borders and over-
flow basins was retransported by the winds and laid down afresh
in layers of varying thickness known as 'loess.' There was no
' loess ' formation either in Europe or America during the humid
climate of First Interglacial times, but during the latter part of
the Second Interglacial Stage, again toward the close of the
Third Interglacial Stage, and finally during Postglacial times
there were periods of arid climate when the 'loess' was lifted
and transported by the prevailing winds over the ' terraces ' and
30 MEN OF THE OLD STONE AGE
plateaus and even to great heights among the mountain valleys.
As observed by Huntington58 in his interesting book The Pulse
of Asia, even at the present time there are districts where we
find 'loess' dust filling the entire atmosphere either during the
heated months of summer or during the cold months of winter.
In Pleistocene Europe there were at least three warm or cold
arid periods, accompanied in some phases by prevailing westerly
winds,59 in which * loess' was widely distributed over northern
Germany, covering the 'river terraces,' plateaus, and uplands
bordering the Rhine and the Neckar. These 'loess' periods
can be dated by the fossil remains of mammals which they con-
tain, also by the stations of the flint quarries in different culture
stages. Thus we find late Acheulean implements in drifts of
'loess' at Villejuif, south of Paris. Among the most famous
stations of late Acheulean times is that of Achenheim, west of
Strasburg, and not far distant is the 'loess' station of Mom-
menheim, of Mousterian times ; both belong to the period of the
fourth glaciation. An Aurignacian 'loess' station is that of
Willendorf, Austria.
Times of the Limestone Shelters and Caverns
Beginning in the late or cold Acheulean period, the Palae-
olithic hunters commenced to seek the warm or sheltered side of
deepened river- valleys, also the shelter afforded by overhanging
cliffs and the entrances of caverns. It is quite probable that
during the warm season of the year they still repaired to their
open flint quarries along the rivers and on the uplands ; in fact,
the river Somme was a favorite resort through Acheulean into
Mousterian times.
In general, however, the open rivers and plateaus were aban-
doned, and all the regions of limestone rock favorable to the
formal ion of shelter cliffs, grottos, and caverns were sought out
by the early Palaeolithic men from Mousterian times on ; and thus
from the beginning of the Mousterian to the close of the Upper
Palaeolithic their lines of migration and of residence followed the
GEOLOGIC HISTORY OF MAN
31
exposures of the limestones which had been laid down by the
sea in bygone geologic ages from Carboniferous to Cretaceous
times. The upper valleys of the Rhine and Danube traversed
the white Jurassic limestones which are again exposed in a broad
band along the foot-hills of the Pyrenees, extending far west to
the Cantabrian Alps of modern Spain. In Dordogne the great
horizontal plateau of Cretaceous limestone had been dissected
by branching rivers, such as the Vezere, to a depth of two hun-
Fig. 10. Ideal section of the bluff overlying the Diissel River, near Diisseldorf , showing
the mode of formation of the famous Neanderthal Cave, where the original type of
the Neanderthal race was discovered in 1856. A typical resort of the 'cave man.'
After Lyell.
c. Entrance of percolating waters from above.
/. Exit from the grotto.
a-b. Interior of the cavern.
dred feet. Under overhanging cliffs long rock shelters were
formed, such as that of the Magdalenian station at La Madeleine.
Many caverns were formed, some of them in early Pleistocene
times, by water percolating from above and (Fig. 1 1) resulting in
subterranean streams which issued at the entrance ; this formed
the expanded grotto, sometimes a chamber of vast dimensions,
such as the Grotte de Gargas. Outside of this, again, may be an
abri or shelter of overhanging rock. In other cases the rock
shelter is found quite independent of any cave.
Where the glaciers or ice-caps passed over the summits of the
hills the subglacial streams penetrated the limestone of the
mountain and formed vast caverns, such as that of Niaux, near
the river Ariege. Here a nearly horizontal cavern was formed,
extending half a mile into the heart of the mountain. The ma-
32
MEN OF THE OLD STONE AGE
terial with which the floors of the caverns are covered is either a
fine cave loam or the insoluble remainder of the limestone form-
ing a brown or gray clayey substance. The Magdalenian artists
produced drawings on these soft clays and, in rare instances, used
them for modelling purposes, as in the Tuc d'Audoubert. The
sands and gravels were also swept in from the streams above and
carried by strong currents along the wall surfaces, smoothing and
polishing the limestone
in preparation for the
higher forms of Upper
Palaeolithic draughts-
manship and painting.
It would appear that
the majority of the cav-
erns were formed in plu-
vial periods of early
glacial times ; the for-
mation had been com-
pleted, the subterranean
streams had ceased to
flow, and the interiors
were relatively dry and
free from moisture in
Fourth Glacial and Post-
glacial times, when man first entered them. There is no
evidence, however, that the cavern depths were generally in-
habited, for the obvious reason that there was no exit for
the smoke ; the old hearths are invariably found close to or
outside of the entrance, the only exception being in the en-
trance to the great cavern of Gargas, where there is a natural
chimney for the exit of smoke. There was no cave life, strictly
speaking — it was grotto life; the deep caves and caverns were
probably penetrated only by artists and possibly also by magi-
cians or priests. It is in the abris or shelters in front of the grottos
and in the floors of the caverns that remarkable prehistoric
records arc found from late Acheulean times to the very close of
Fig
Formation of the typical limestone cav-
ern. After Gaudry.
V. Vertical section of limestone cliff showing
(S) waters percolating from above; (A-0) inte-
rior of the cavern; and (G) grotto entrance, orig-
inal exit of the cavern waters. H. Horizontal
section of the same cavern showing the (G)
grotto entrance and (A, G, 0, B) the ramifica-
tions of the cavern.
GEOLOGIC HISTORY OF MAN
33
the Palaeolithic, as in the wonderful grotto in front of the cave
at Castillo, near Santander. Thus, as Obermaier60 observes : " In
Chellean times primitive man was a care-free hunter wandering
as he chose in the mild and pleasant weather, and even the colder
climate of the arid 'loess' period of the late Acheulean was not
sufficient to overcome his love of the open; he still made his
camp on the plains at the edge of the forest, or in the shelter of
some overhanging cliff." Only in rare instances, as at Castillo,
were the Acheulean hearths brought within the entrance line of
the grotto.
Geologic Time
Penck, igio
Geikie, 1914
.Wiegers, 1913
Boule, Breuil,
Obermaier, 191 2
Schmidt, 1912
Postglacial.
Magdalenian.
Bronze.
Neolithic.
Azilian.
Magdalenian.
Solutrean.
Aurignacian.
IV. Glacial.
Solutrean.
Magdalenian.
Solutrean.
Aurignacian.
Mousterian.
Mousterian.
Third Inter glacial.
Mousterian.
Mousterian.
Early Mousterian.
Cold Acheulean.
Warm "
Chellean.
Pre-Chellean.
III. Glacial.
Mousterian.
Cold Acheu-
lean.
Second Inter glacial.
Acheulean.
Chellean.
Warm Acheu-
lean.
Chellean.
II. Glacial.
Pre-Chellean
First Interglacial.
DIFFERENCES OF OPINION AS TO THE GEOLOGIC AGE OF THE
PALEOLITHIC CULTURE STAGES
The right-hand column represents the theory adopted in this volume.
Interpretation of these four kinds of evidence as to the an-
tiquity of human culture in western Europe still leads to widely
diverse opinions. On the one hand, we have the high authority
of Penck61 and Geikie62 that the Chellean and Acheulean cul-
tures are as ancient as the second long warm interglacial period.
84 MEN OF THE OLD STONE AGE
An extreme exponent of the same theory is Wiegers,63 who would
carry the Pre-Chellean back even into First Interglacial times.
On the other side, Boule,64 Schuchardt,65 Obermaier,66 Schmidt,67
and the majority of the French archaeologists place the begin-
ning of the Pre-Chellean culture in Third Interglacial times.
In favor of the latter theory is the strikingly close succession
of the Lower Palaeolithic cultures in the valley of the Somme, fol-
lowed by an equally close succession from Acheulean to Mag-
dalenian times, as, for example, in the station of Castillo. It
does not appear possible that a vast interval of time, such as that
of the third glaciation, separated the Chellean from the Mous-
terian culture.
On the other hand, in favor of the greater antiquity of the
Pre-Chellean and Chellean cultures may be urged their alleged
association in several localities with very primitive mammals of
early Pleistocene type, namely, the Etruscan rhinoceros, Steno's
horse, and the saber-tooth tiger, as witnessed in Spain and in
the deposits of the Champs de Mars, at Abbeville.
It is true, moreover, that at points distant from the great
ice-fields, like the valley of the Somme and that of the Marne,
we have no other means of separating glacial from interglacial
times than that afforded by the deposition and erosion of the
' terraces ' ; in fact, the interpretation of the age of the cultures
may be similar to that applied to the age of the mammalian
fauna. There are no proofs of periods of severe cold in western
Europe in any country remote from the glaciers until the very
cold steppe-tundra climate immediately preceding the fourth
glaciation swept the entire land and drove out the last of the
African-Asiatic mammals.
Geographic Changes
The migrations of mammals and of races of men into western
Europe from the Eurasiatic continent on the east and from
Africa on the south were favored or interrupted by the periods
of elevation or of subsidence of the coastal borders of the ^Egean,
Mediterranean, and North Seas, and also of the Iberian and
GEOGRAPHIC CHANGES
35
British coast-lines. The maximum period of elevation of the
coastal borders, as represented in the accompanying map (Fig.
12), never occurred in all portions of the continent of Europe at
the same time, because there were oscillations both on the nOrth-
15 20 15 10 W. 0 E
20 30 »0 SO M
as 10 ~\ i .Tu ~ ~-^^Ip^£--^ -_^l" J^? "3
5M0'\ I jjf LliL" PROBABLE IsEA LEVEL AT THE }t!ME oAmAXIMUM EL EVATION, 1 __ \ SECOND CLACIATION. MINOEL ~$£~' -~^=T\XJ='
Strait of Gibraltar Garonne Phone North Skager
Valley Valley Sea Rak
SNOW LINES OF THE FOUR PRINCIPAL GLACIAL EPOCHS OF THE PLEISTOCENE PERIOD
A~B Profile across Europe along the line A-B of map
5 Presenr snow line
4 Snow line of the Fourth ONurm) Glacial Epoch
3 « « « ,. Third fffiss) » »
2 n n n » Second CMindel) »» >»
; « »» f » First (Gi/nz) « »
Fig. 13. An ideal earth section from the North Cape across the Scandinavian
plateau, through the North Sea, Swiss Alps, Pyrenees, and Straits of Gibraltar, to
the Atlas Mountains in northern Africa, along the line indicated on the map (Fig. 25,
p. 65) , illustrating the sea-level at' the time of the greatest elevation of the conti-
nent during the Second Glacial Stage, as compared with the present sea-level;
also the successive lines of descent of the region of perpetual snow during the four
great glacial advances, as compared with the present snow-line. From studies
by Dr. C. A. Reeds.
glaciation reached from 1,200 m. (3,937 ft.) to 1,500 m. (4, 921 ft.)
below the present snow-level, with the consequent formation of
vast ice-caps hung with glaciers which flowed great distances
down the valleys of the Rhone and of the Rhine and left their
moraines at very distant points. The moraines and drifts of the
lesser glaciations, such as the first and fourth, stand considerably
within the boundaries of these outer moraines and drift fields.
On the contrary, the warmer climates of interglacial times are
indicated by the sun-loving plants found at Hotting, along the
valley of the Inn, in the Tyrol, which are proofs of a tempera-
ture higher than the present and of the ascent of the snow-line
300 m. (984 ft.) above the existing snow-level of the Alps.
38 MEN OF THE OLD STONE AGE
The alternation of the cold climates of the glacial stages with
the warm temperate climates of the interglacial stages formed
great oscillations of temperature (Figs. 13, 14). The fossil
plant life indicates that during the periods of the First, Second,
and Third Interglacial Stages the climate of western Europe
was cooler than it had been during the preceding Pliocene
Epoch and somewhat warmer than it is at the present time in
the same localities. During the First, Second, and Third Glacial
Stages there was certainly a marked lowering of temperature in
the regions bordering the great glacial fields. This is indicated
by the arrival in the northern glacial border regions of animals
and plants adapted to arctic and subarctic climates.
It has been generally believed that the whole of western
Europe was extremely cold during these glacial stages, and that
the heat-loving animals, the southern elephants, rhinoceroses,
and hippopotami, were driven to the south, to return only with
the renewed warmth of the next interglacial stage.
There is, however, no proof of the departure of these suppos-
edly less hardy mammals nor of the spread over Europe of the
more hardy arctic and steppe types until the advent of the
Fourth Glacial Stage. Then, for the first time, all western Europe
north of the Pyrenees experienced a general fall of temperature,
and conditions of climate prevailed such as are now found in the
arctic tundra regions of the north and in the high steppes of
central Asia, which are swept by dry and cold winter winds.
Fluctuations of temperature, of moisture, and of aridity in Pleis-
tocene time, are evidenced not only by the rise and fall of the
snow-line and the advance and retreat of the ice-caps but also by
the appearance of plant and animal life in the periods of the 'loess'
deposition, indicating the following cycles of climatic change as
witnessed from beginning to end of the Third Interglacial Stage :
IV. Glacial maximum, cold and moist climate, arctic and cold
steppe fauna and flora.
Cool and dry steppe climate, wide-spread deposition of
' loess.'
CLIMATIC CHANGES 39
Interglacial maximum, a long period of warm temperate
forest and meadow conditions.
Glacial retreat, cool and moist climate bordering the gla-
cial regions.
III. Glacial maximum, cold and humid climate bordering the
glaciers, favorable to arctic and subarctic plant and
animal life.
That great fields of ice and advancing glaciers alone do not
constitute proof of very low temperatures is shown at the present
time in southeastern Alaska, where very heavy snowfall or pre-
cipitation causes the accumulation of vast glaciers, although the
mean annual temperature is only io° Fahr. (5.560 C.) lower than
that of southern Germany. Neumayr69 estimated that during
the Ice Age there was a general lowering of temperature in Eu-
rope of not more than 6° C. (10.80 Fahr.), and held that even
during the glacial advances a comparatively mild climate pre-
vailed in Great Britain. Martins70 estimated that a lowering of
the temperature to the extent of 40 C. (7.20 Fahr.) would bring
the glaciers of Chamonix down to the level of the plain of Geneva.
Penck estimates that, all the atmospheric conditions remaining
the same as at present, a fall of temperature to the extent of 40
to 50 C. would be sufficient to bring back the Glacial Epoch in
Europe. These moderate estimates entirely agree with our
theory that animals of African and Asiatic habit nourished in
western Europe to the very close of the Third Interglacial
Stage, and that then for the first time the warm fauna, or
faune chaude, gradually disappeared.
Similarly the hypothesis of extremely warm or subtropical
conditions prevailing in interglacial times as far north as Britain,
which originated with the discovery of the northerly distribution
of the hippopotami and rhinoceroses, animals which we now
associate with the torrid climate of Africa, is not supported by
the study either of the plant life of interglacial stages or by the
history of the animals themselves. It is quite probable that
both the hippopotami and the rhinoceroses of the 'warm fauna'
40 MEN OF THE OLD STONE AGE
were protected by hairy covering, although not by the thick
undercoating of wool which protected the woolly rhinoceros and
woolly mammoth, animals favoring the borders of glaciers and
flourishing during the last very cold glacial and Postglacial
periods.
The combined evidence from all these great events in western
Europe leads us to conclusions somewhat different from those
reached by Penck as to the chronology of human culture. In
the chart (Fig. 14) on the opposite page, prepared by Dr.
C. A. Reeds in collaboration with the author, a new correlation
of geologic, climatic, human, industrial, and faunal events is
presented. The great waves of glacial advance and retreat
(oblique shading) are based upon Penck' s estimates of the rise
and fall of the snow-line (vertical dotted lines) in the Swiss Alps.
(Compare Fig. 13.) The length of these waves corresponds
with the relative duration of the glacial and interglacial stages
as estimated by the varying amounts of erosion and deposition
of materials. The entire Palaeolithic or Old Stone Age is thus
seen to occupy not more than 125,000 years, or only the last
quarter of the Glacial Epoch, which is estimated as extending
over a period of 525,000 years. The present opinion of the
leading archaeologists of France and Germany, which is shared
by the author, is that the Pre-Chellean industry is not older
than the Third Interglacial Stage. As the Piltdown man was
found in deposits containing Pre-Chellean implements, he prob-
ably lived in the last quarter of the Glacial Epoch, and not in
early Pleistocene times as estimated by some British geologists.
This causes us to regard the Piltdown remains as more recent
than the jaw of Heidelberg, which all authorities agree is prob-
ably of Second Interglacial Age. According to our estimates the
Heidelberg man is nearly twice as ancient as the Piltdown man,
while Pithecanthropus (Trinil Race) is four times as ancient.
Yet the Piltdown man must still be regarded as of very great
antiquity, for he is four limes as ancient as the final type of Ne-
anderthal man belonging to the Mousterian industrial stage.
The various arcrueologic and pakeontologic evidences for this
Fig. 14. Great events of the Glacial Epoch. To the left the relation of glacial and in-
terglacial stages in Europe and North America, with the author's theory regarding the
divisions of time, the beginning of the Old Stone Age, and the successive appearance
in Europe of different branches of the human race. To the right the prolonged
warm temperate period in Europe in the non-glaciated regions, followed by the
relatively brief cold period during the past 70,000 years. Prepared by Dr. C. A.
« Reeds, in co-operation with the author.
41
42 MEN OF THE OLD STONE AGE
general correlation theory of the Glacial Epoch are fully dis-
cussed in the succeeding chapters of this volume.
Mammals of Five Distinct Geographic Regions
(Compare Color Map, PL II, and Fig. 15)
As we have already observed, during the whole history of
mammalian life in various parts of the world never did there
prevail conditions so unusual and so complex as those which
surrounded the men of the Old Stone Age in Europe. The suc-
cessive races of Palaeolithic men in Europe were all flesh eaters,
depending upon the chase. The mammals, first pursued only
for food, utensils, and clothing, finally became subjects of artis-
tic appreciation and endeavor which resulted in a remarkable
aesthetic development.
From the beginning to the end of Palaeolithic times the vari-
ous races of man witnessed the assemblage in Europe of animals
indigenous to every continent on the globe except South America
and Australia and adapted to every climatic life-zone, from the
warm and dry plains of southern Asia and northern Africa to
the temperate forests and meadows of Eurasia; from the heights
of the Alps, Himalayas, Pyrenees, and Altai Mountains to the
high, arid, dry steppes of central Asia with their alternating heat
of summer and cold of winter ; from the tundras or barren grounds
of Scandinavia, northern Europe, and Siberia to the mild forests
and plains of southern Europe.71 Members of all these highly
varied groups of animals had been evolving in various parts of
the northern hemisphere from the Eocene Epoch onward. In
Pliocene times they had become thoroughly adapted to their
various habitats. Throughout early Pleistocene times, with the
increasing cold extending southward from the arctic circle,
such mammals as the elephant, rhinoceros, musk-ox, and rein-
deer had become thoroughly adapted to the climate of the ex-
treme north. There is every reason to believe that when these
tundra quadrupeds first arrived in Europe, during early mid-
glacial stages, they had already acquired the heavy coat of hair
MIGRATIONS OF MAMMALS
43
Recent
Prehistoric.
Return of the Alpine Mammals to the Mountains.
Wide dispersal of Forest and Meadow Mammals
over the Northern Hemisphere.
Postglacial.
Severe climate.
IV. Glacial.
Cold Steppe cli-
mate.
3d Interglacial.
Warm climate.
III. Glacial.
Reindeer and
Woolly Mam-
moth in North
Germany and
the Alps.
2d Interglacial.
II. Glacial.
Reindeer and
Woolly Mam-
moth in North-
ern Germany.
est Interglacial.
I. Glacial.
Musk-ox in Sus-
sex, England.
Also the stag, giant deer, bison, wild
• cattle, forest horse, boar, wolf, fox,
lynx, wildcat, several species of bear.
Survival of many Pliocene African-
Asiatic Mammals, mingled with Pliocene
and recent Eurasiatic Forest and Mead-
ow Mammals.
Retreat of the Tundra and Steppe Mammals to the
North and East.
Mingling in the lowlands of France and Germany
of the Reindeer-Mammoth fauna, the Alpine
fauna, the Steppe Mammals, and the hardy Eur-
asiatic Forest and Meadow Mammals.
Arrival of tbe Tundra Mammals from the North.
Arrival of the Steppe Mammals from Western Asia.
Southward migration and extinction of all the
African-Asiatic Mammals except the lions and
hyaenas.
Mingled African-Asiatic and Eurasiatic Mammals
in different parts of the non-glaciated regions,
the hippopotamus, southern mammoth, straight-
tusked elephant, Merck's broad-nosed
rhinoceros, lion, hyaena, jackal, sabre-
tooth tiger.
Period of
Recent
Animals
Reindeer
Period
in
Western
Europe.
Period
OF THE
Hd?popotamus,
Rhinoceros,
AND
Elephant.
Also
of the
Stag
AND
Bison
in
Western
Europe.
Geologic
and
Climatic
Stages.
Early Migrations
of Scandinavian
and North Sibe-
rian Mammals
near the Ice-
fields.
'Warm' African- More hardy Eur-
Asiatic Mammals. asiatic Mammals.
Temperate and shel- Cool temperate for-
tered parts of ests and mead-
Western Europe. ows.
Regions near More Sheltered Non-Glaciated Re-
the ice-feelds gions remote from the glacial
and Glacial Borders and Ice-fields.
Borders.
Three
Chief
Life
Periods.
MIGRATIONS AND EXTINCTIONS OF MAMMALIAN LIFE DURING THE
FOUR GLACIAL, THREE INTERGLACIAL, AND POSTGLACIAL STAGES
44 MEN OF THE OLD STONE AGE
and undercoating of wool, such as now characterizes the musk
ox, one of the living representatives of this northern fauna.
The five great sources of mammalian migration into western
Europe in Pleistocene times were accordingly as follows:
i. Warm plains of northern Africa and of southern Asia. "African-
Asiatic" fauna — hippopotamus, rhinoceros, elephant.
2. Temperate meadows and forests of Europe and Asia. "Eura-
siatic" fauna — deer, bison, horse.
3. High, cool mountain ranges — Alps, Pyrenees, Caucasus, Urals.
Fauna — chamois, ibex, ptarmigan. (See Fig. 185.)
4. Steppes and deserts. Dry, elevated plateaus and steppes of east-
ern Europe and central Asia. Fauna — desert ass and horse, saiga ante-
lope, jerboa. (See Fig. 186.)
5. Tundras and barren grounds within or near the arctic circle.
Fauna — reindeer, musk-ox, arctic fox. (See Figs. 95 and 96.)
(Compare Figs. 14 and 15.)
In the warm plains, forests, and rivers of southern Asia and
northern Africa there developed the elephants, rhinoceroses,
hippopotami, lions, hyaenas, and jackals, which, taken together,
may be known as the African- A sialic fauna. It contains alto-
gether fourteen species of mammals. The great geographic area
from the far east to the far west over which ranged similar or
identical species of these pachyderms and carnivores is indicated
by the oblique lines in the geographic chart (Fig. 15).
The north temperate belt of Asia and Europe, with its hardy
forests and genial meadows, was the home of the even more
highly varied Eur astatic Forest and Meadow fauna. This includes
twenty-six or more species. Of these the red deer, or stag, was
most characteristic of the forests and the bison and wild cattle* of
the meadows. Even at the very beginning of Pleistocene times
there appear the stag, the wild boar, and the roe-deer with their
natural pursuers, the wolf and the brown bear. From the northern
woods came the moose and the wolverene. Most of these mam-
mals were so similar to existing forms that the older naturalists
* Bison and wild cattle arc grass eaters, and their natural habitats are the open plain
and meadow regions. They also range into open forest lands where grasses can be found.
The prehistorii 'urns' and 'wisent' of Europe were both found in forests, but this may
not have been their natural habitat in Palaeolithic times. See Appendix, Note IV.
MIGRATIONS OF MAMMALS
45
placed them in existing species, but the tendency now is to sepa-
rate them or place them in distinct subspecies. Mingled with
these forest and meadow mammals were a few others which have
Fig. 15. Zoogeographic map. Range of the large mammals of Africa and southern
Asia in Pliocens and Pleistocene times until nearly the close of the Lower Palaeo-
lithic (oblique lines). Range of the forest and meadow fauna of Europe and
Asia from early Pleistocene to prehistoric times; stag and bison fauna (horizontal
lines). Present range of the tundra or barren-ground mammals (dots) which wan-
dered south during the fourth glaciation, expelling the large Asiatic mammals.
Present range of mammals of the deserts and steppes of eastern Europe and
southern Asia, which also invaded western Europe during the glacial and Post-
glacial stages (vertical lines). The alpine mammals dwelt in the high mountain
regions and invaded the plains and lowlands during Fourth Glacial and Post-
glacial times.
since become extinct, such as the giant deer (Megaceros), the
giant beaver (Trogontherium), and the primitive forest and
meadow horses. From this region also there developed the cave-
bear (Ursus spelceus). Certainly it is astonishing to find the re-
mains of these mammals mingled with those from southern Asia
and Africa, as is frequently the case. In early glacial times the
46 MEN OF THE OLD STONE AGE
bison and wild cattle mingled freely with the hippopotami and
rhinoceroses, but in late glacial and Postglacial times they oc-
curred as companions of the mammoth and the woolly rhinoceros.
In prehistoric times they survived with the mammals brought
from the Orient by the Neolithic agriculturists.
During a great glaciation, but especially during the severe
climate of late Pleistocene times, the Alpine mammals were
driven down from the heights into the plains and among the
lower mountains and foot-hills. Thus the ibex, chamois, and
argali sheep from the Altai Mountains are represented both in
drawing and in sculpture by the men of the Reindeer Period.
Still more remarkable is the arrival in Europe of the Steppe
Fauna of Russia and of western Siberia, mammals which now
survive in the vast Kirghiz steppes, east of the Caspian Sea
and the Ural Mountains, where the climate is one of hot, dry
summers and prolonged cold winters, with sweeping dust and
snow storms. These animals are very hardy, alert, and swift of
foot, such as the jerboa, the saiga antelope, the wild asses, and-
the wild horses, including the Przewalski type, which still sur-
vives in the desert of Gobi. From this region also came the
Elasmo there (E. sibiricum) , with its single giant horn above the
eyes. Very distinctive of the fauna frequenting the caverns are
the small rodents, including the dwarf pikas, the steppe hamsters,
and the lemmings. These animals were attracted into Europe
during the 'steppe' and 'loess' periods of cold, dry climate.
The advance of the great Scandinavian glaciers from the
north crowded to the south the Tundra or Barren Ground fauna
of the arctic circle. The herald of this fauna during the First
Glacial Stage was the musk-ox, which appears in Sussex, and then
came the reindeer of the existing Scandinavian type. These
animals are followed by the woolly mammoth (£. primigenius)
and the woolly rhinoceros (D. antiquitatis) with their panoply of
hair and wool which had long been developing in the north.
Finally in the Fourth Glacial Stage arrived the lemming of the
river Obi, also the more northern banded lemming, the arctic
fox, the wolverene, and the ermine, as well as the arctic hare.
MIGRATIONS OF MAMMALS
47
These tundra mammals for a short period mingled in places with
survivors of the African-Asiatic fauna, such as Merck's rhinoc-
eros and the straight- tusked elephant (E. antiquus). In general,
they swept southward as far as the Pyrenees over country which
had long been enjoyed by the African-Asiatic mammals, while
the hippopotami and the southern elephants retreated still far-
ther south and became extinct.
The only survivors of the great African- Asiatic fauna in
Fourth Glacial and Postglacial times were the hyaenas (H.
crocuta spelcea) and the lions (Felis leo spelcea). The lion fre-
quently appears in the drawings of the cavemen.
The various species belonging to these five great faunae ap-
parently succeed each other, and wherever their remains are
mingled with the palaeoliths, as along the rivers Somme, Marne,
and Thames, or in the hearths of the shelters and caverns, they
become of extreme interest both in their bearing on the chronology
of man and on the development of human culture, art, and in-
dustry. They also tell the story of the sequence of climatic
conditions both in the regions bordering the glaciers and in the
more temperate regions remote from the ice-caps. Thus they
guide the anthropologist over the difficult gaps where the geologic
record is limited or undecipherable. The general succession of
these great faunae is illustrated in Fig. 14 and also in the above
table.
(1) Lamarck, 1815.1.
(2) Schaaffhausen, 1 858.1.
(3) Darwin, C, 1909.2.
(4) Lamarck, 1 809.1.
(5) Lyell, 1863. 1, pp. 84-89.
(6) Darwin, C, 1871.1, p. 146.
(7) Darwin, C, 1909. 1, p. 158.
(8) Retzius, A., 1864.1, p. 27.
(9) Op. cit., p. 166.
(10) Broca, 1875. 1.
(11) Schwalbe, G., 1914.1, p. 592.
(12) Cartailhac 1 903.1.
(13) Dechelette, 1908.1, vol.. I.
(14) Reinach, S„ 1889. 1.
(15) Schmidt, 1912.1.
(16) Avebury, 1913.1.
(17) Eccardus, 17 50.1.
(18) Mahudel, 1 740.1.
(19) Buckland, 1824. 1.
(20) Godwin- Austen, 1 840.1.
(21) Christol, 1829. 1.
(22) Schmerling, 1833. 1.
(23) Boucher de Perthes, 1846.1.
(24) Op. cit.
(25) Rigollot, 1854.1.
(26) Lubbock, 1862. 1.
(27) Avebury, 1913-1, PP- 2, 3.
(28) Lartet, 1861.1.
(29) Lartet, 1875. 1.
(30) Breuil, 1912.7, p. 165.
(31) de Mortillet, 1869. 1.
(32) Piette, E., 1907. 1.
48
MEN OF THE OLD STONE AGE
(33) Riviere 1897. 1.
(34) de Sautuola, 1 880.1.
(35) Schmidt, 1912.1.
(36) Bourgeois, 1867. 1.
(37) Schmidt, op. cit., p. 5.
(38) Obermaier, 1912.1, pp. 170-174;
316-320; 332, 545.
(39) Charpentier, 1841.1.
(40) Agassiz, 1837. 1 ; 1840. 1; 1840.2.
(41) Morlot, 1854. 1.
(42) Chamberlin, 1895. 1; 1905. 1, vol.
Ill, chap. XIX, pp. 327-516.
(43) Salisbury, 1905. 1.
(44) Penck, 1909. 1.
(45) Leverett, 1910.1.
(46) Lyell, 1867. 1, vol. I, pp. 293-
301; 1877. 1, vol. I, p. 287.
(47) Dana, 1875. 1, p. 591.
(48) Walcott, 1 893. 1.
(49) Upham, 1893. 1, p. 217.
(50) Heim, 1894. 1.
(51) Sollas, 1900.1.
(52) Penck, 1909.1, vol. Ill, pp. 1153-
1176.
(53) Geikie, 1914.1, P- 302.
(54) Reeds, 191 5.1.
(55) Niiesch, 1902. 1.
(56) Geikie, op. cit., pp. 111-114.
(57) Op. cit., p. 108.
(58) Huntington, 1907. 1.
(59) Leverett, 1910.1.
(60) Obermaier, 1912.1, p. 132.
(61) Penck, 1908. 1 ; 1909. 1.
(62) Geikie, 1914.1, p. 312.
(63) Wiegers, 191 3.1.
(64) Boule, 1888. 1.
(65) Schuchardt, 1913.1, p. 144.
(66) Obermaier, 1909.2; 191 2.1.
(67) Schmidt, 1912.1, p. 266.
(68} Penck, 1909. 1, vol. Ill, p. 1168,
Fig. 136.
(69) Neumayr, 1 890.1, vol. II, p. 621.
(70) Martins, 1847. 1, pp. 941, 942.
(71) Osborn, 1910.1, pp. 386-427.
CHAPTER I
ANCESTRY OF THE ANTHROPOID APES — PLIOCENE CLIMATE, FORESTS,
AND LIFE OF WESTERN EUROPE — TRANSITION TO THE PLEISTO-
CENE, OR AGE OF MAN — THE FIRST GLACIATION, ITS EFFECTS ON
CLIMATE, FORESTS, AND ANIMAL LIFE — THE PREHUMAN TRINIL
RACE OF JAVA — THE EOLITHS OR PRIMITIVE FLINTS — THE SEC-
OND GLACIATION — THE HEIDELBERG, EARLIEST KNOWN HUMAN
RACE — THE THIRD GLACIATION
The partly known ancestors of the anthropoid apes and the
unknown ancestors of man probably originated among the for-
ests and flood-plains of southern Asia and early began to migrate
westward into northern Africa and western Europe.
As early as Oligocene times a forerunner of the great apes
(Propliopithecus), most nearly resembling the gibbons, appears
in the desert bordering the Fayum in northern Egypt. Early in
Miocene times true tree-living gibbons found their way into
Europe and continued throughout the Pliocene in the forms
known as Pliopithecus and Pliohylobates, the latter being a true
gibbon in its proportions ; it ranged northward into the present
region of Germany. Another ape which early reached Europe
is the Dryopithecus; it is found in Miocene times in southern
France ; the grinding- teeth suggest those of the orang, the jaw
is deep and in some ways resembles that of the Piltdown man.
A third ape {Neopithecus) occurs in the Lower Pliocene near
Eppelsheim, in Germany, and is known only from a single lower
molar tooth, which recalls the dentition of Dryopithecus and more
remotely that of Homo. In the Pliocene of the Siwalik hills of
Asia is found Palceopithecus, a generalized form which is believed
to be related to the chimpanzee, the gorilla, and the gibbon ; the
upper premolars resemble those of man.
None of these fossil anthropoids either of Europe or of Asia
can be regarded as ancestral to man, although both Neopithecus
49
50
MEN OF THE OLD STOXE AGE
and Dryopithecus have been placed in or near the line of human
ancestry by such high authorities as Branco and Gaudry. When
Dryopithecus was first discovered by Lartet, Gaudry1 considered
it to be by far the most manlike of all the apes, even attributing
to it sufficient intelligence for the working of flints, but fuller
Fig. 16. The gibbon is primitive in its skull and dentition, but extremely special-
ized in the adaptation of its limbs to arboreal life. Photograph
from the New Vork Zoological Park.
knowledge of this animal has shown that some of the living
anthropoids are more manlike than Dryopithecus. This animal
is closely related to the ancestral stock of the chimpanzee,
gorilla, and orang. The jaw, it is true, resembles that of the
Piltdown man (Eoanthropus), but the grinding-teeth are much
more primitive and there is little «eason to think that it is an-
tral to any human type.*
* A recent article by A. Smith Woodward describes the fourth known specimen of
Dryopithecus, lately discovered in northern Spain (sec Woodward, 1914.2).
ANCESTRY OF THE ANTHROPOID APES 51
Among these fossil anthropoids, as well as among the four
living forms, we discover no evidence of direct relationship to
man but very strong evidence of descent from the same ances-
tral stock. These proofs of common ancestry, which have already
been observed in the existing races of man, become far more
conspicuous in the ancient Palaeolithic races ; in fact, we cannot
interpret the anatomy of the men of the Old Stone Age without
Fig. 17. The orang has a high rounded skull and long face. Photograph
from the New York Zoological Park.
a survey of the principal characters of the existing anthropoid
apes, the gibbon, the orang, the chimpanzee, and the gorilla.
The gibbon is the most primitive of living apes in its skull
and dentition, but the most specialized in the length of its arms
and its other extreme adaptations to arboreal life. As in the
other anthropoids, the face is abbreviated, the narial region is
narrow, i. e., catarrhine, and the brain-case is widened, but the
top of the skull is smooth, and the forehead lacks the promi-
nent ridges above the orbits; thus the profile of the skull of
52
MEN OF THE OLD STONE AGE
the gibbon (Fig. 16) is more human than that of the other an-
thropoid apes. When on the ground the gibbon walks erect and
is thus afforded the free use of its arms and independent move-
ments of its fingers. In the brain there is a striking develop-
ment of the centres of sight, touch, and hearing. It is these
characteristics of the modern gibbon which preserve with rela-
Fig. 18. The chimpanzee. This figure illustrates the walking powers of the
chimpanzee, the great length of the arms, and the abbreviation of the
legs. Photograph from the Xew York Zoological Park.
tively slight changes the type of the original ancestor of man,
as noted by Elliot Smith.2
The limbs of the orang are less elongated and less extremely
specialized for arboreal life than those of the gibbon but more
so than those of the chimpanzee and the gorilla. The skull is
rounded and of great vertical height, with broad, bony ridges
above the orbits and a great median crest on top of the skull in
old males. The lower jaw of the orang is stout and deep, and,
although used as a fighting weapon, the canine tusks are much
ANCESTRY OF THE ANTHROPOID APES
53
less prominent than in either the gibbon, chimpanzee, or
gorilla.
In the chimpanzee we observe the very prominent bony ridges
above the eyes, like those in the Trinil and Neanderthal races
of men. Of all the anthropoid apes the lower jaw of the chim-
Fig. 19. The chimpanzee. This figure shows certain facial characteristics
which are preserved in the Neanderthal race of men. Note also the
shortening of the thumb and the enlargement of the big toe. Photograph
from the New York Zoological Park.
panzee most nearly resembles that of- the Piltdown man. The
prognathous or protruding tooth rows and receding chin sug-
gest those in the Heidelberg, Piltdown, and Neanderthal races.
When the chimpanzee is walking (Fig. 18) the arms reach down
below the level of the knees, whereas in the higher races of man
they reach only half-way down the thighs.
54
MEN OF THE OLD STONE AGE
Thus, the fore limb, although much shorter than that of the gib-
bon, is relatively longer than that of any human race, recent or
ancient. We observe also in the walking chimpanzee (Fig. 18)
Existing
Apes and
Man.
Gibi
As
JON.
la.
Man
(Homo sapiens).
Asia, Europe.
Chimpanzee. Gorilla.
Africa. Africa.
/
f
Orang.
Asia.
Cro-Magnon and
other races.
i
i
i
/
/
/
/
/
/
/
/
/
Macaque
of Eu-
rope.
i
j
Glacial or
Pleistocene
Age.
More primitive spe-
cies, human and
prehuman.
Neanderthal race.
Piltdown race.
|
/
/
/
/ /
Heidelberg race.
1
i
! 1
!
Pliocene
Age.
Primitiv
bon c
rope
{Pliohyl
; Gib-
>f Eu-
obates) .
Trinil race
(Pithecanthropus) .
Unknown Pliocene
ancestors of man.
: / /
Ancestral a'nthro- /
poids of Asia /
!/ /
i / /
Macaques
of Asia
and
Europe.
j
i
Miocene
Age.
i
Earliest 'Gibbons
of Europe
(Pliopithecus).
!
i
|
Primitive anthropoids
of Asia and Europe. /
J J /
/
/
Oligocene.
Ancestral anthro-
poids of Egypt
(Propliopithecus) .
Small monkeys
of Egypt.
V
--~ ,,- —
-^
Unknown ancestral stock
of the Old World pri-
mates, including man.
ANCESTRAL TREE OF THE ANTHROPOID APES AND OF MAX
From the unknown and ancestral stock of the anthropoid apes and man the gibbon was the first
to bran< h off in Oligocene times; the oramc; then branched off in a widely different direction.
The Bt hi of the chimpanzee and of the gorilla branched off at a more recent date and is
more nearly allied to that of man. Five early human races have been found in Europe in
Gla< i.il or Pleistocene times, but no traces of other primates except the macaques, which are
related to the lower division of the baboons, have been found in Europe in Pleistocene times.
Modified after Gregory. (For latest discovery see Appendix, Note VII.)
ANCESTRY OF THE ANTHROPOID APES
55
that the upper part of the leg, the thigh-bone, or -femur, is rela-
tively long, while the lower part, the shin-bone, or tibia, is rela-
tively short. Indeed, both in the arm and in the leg the upper
bones are relatively long and the lower bones are relatively short.
These proportions, which are inheritances of arboreal life, are
in very marked contrast to those observed in the arms and
Fig. 20. The Gorilla. An immature female, about three years of age,
showing none of the adult male characteristics. Photo-
graph from the New York Zoological Park.
legs of the Neanderthal race of men, in which the limbs are of
the terrestrial or walking type.
We observe also in the chimpanzee a contrast between the
grasping power of the big toe, which is a kind of thumb, and the
lack of that power in the hand, in which the thumb is nearly
useless ; in all apes this function is characteristic of the foot, in
man of the hand alone. The opposable thumb, with its power of
bringing the thumb against each of the fingers, is the one char-
acter which is lacking in every one of the anthropoid apes and
which was early developed among the ancestors of man.
The skull of the chimpanzee is longer than that of the orang,
the most prominent feature in the top view being the extreme
protuberance of the orbits, which are surrounded by a supra-
oG
MEN OF THE OLD STONE AGE
orbital and circumorbital bony ridge, which is also strongly de-
veloped in the Neanderthal skull as well as in the Pithecanthropus
or Trinil skull but, so far as we know, is entirely lacking in that
of Piltdown. As in the orang and the gorilla, a crest develops
along the middle of the top of the skull for the insertion of the
powerful muscles of the jaws, a crest which is wholly wanting
in the gibbon and probably wanting in all the true ancestors
of man.
The gorilla illustrates in the extreme the specializations which
are begun in the chimpanzee, and which are attributable to a
Fig. 21. Contrast of the projecting face (prognathism), retreating forehead, and
small brain-case of a young gorilla, as compared with the vertical face, promi-
nent nose, high forehead, and large brain-case of a high race of man. After
Klaatsch.
life partly arboreal, partly terrestrial, with the skull and jaws used
as powerful fighting organs. The head is lengthened by the for-
ward growth of the muzzle into an extreme prognathism. The
limbs and body of the gorilla show a departure from the primitive,
slender-limbed, arboreal type of apes and are partly adapted to
a bipedal, ground-dwelling habit.
As regards psychic evolution,3 Elliot Smith observes that the
arboreal mode of life of the early ancestors of man developed
quick, alert, and agile movements which stimulated the progress-
ive- development of the posterior and lateral portions of the
brain. The sense of smell had been well developed in a previous
terrestrial life, but once these creatures left the earth and took
ANCESTRY OF THE ANTHROPOID APES
57
to the trees, guidance by the olfactory sense was less essential,
for life amidst the branches of the trees is most favorable to the
high development of the senses of vision, touch, and hearing.
Moreover, it demands an agility and quickness of movement
that necessitate efficient motor centres in the brain to co-ordinate
and control such actions as tree life calls for. The specialization
of sight awakens curiosity to examine objects with greater mi-
Mascufa^
SELF CONTROL/
ATTENTION
CONDUCT
'ditory
Fig. 22. Side view of a human brain of high type, showing the chief areas of
muscular control and of the sensory impressions of sight and hearing, also the
prefrontal area in which the higher mental faculties are centred. Modified after
M. Allen Starr.
nuteness and guides the hands to more precise and skilled move-
ments.
The anatomy of man is full of remote reminders of this orig-
inal arboreal existence, which also explains the very large and
early development of the posterior portions of the brain, in which
the various senses of sight, touch, and hearing are located.
The first advance from arboreal to terrestrial life is marked
by the power of walking more or less erect on the hind limbs and
thus releasing the arms ; this power is developed to a greater or
less degree in all the anthropoid apes ; with practice they become
58 MEN OF THE OLD STONE AGE
expert walkers. The additional freedom which the erect atti-
tude gives to the arms and to the movements of the hands and
the separate movements of the ringers is especially noticeable in
the gibbon. The cultivation of the powers of the hand reacts
upon the further growth and specialization of the brain; thus
the brain and the erect attitude react upon each other. In
Fig. 23. The evolution of the brain. Outlines (side view) of typical human
and prehuman brains, showing the early development of the posterior por-
tions of the brain and the relatively late development of the anterior portions,
the seat of the higher mental faculties.
the gibbon there is a marked increase in the size of those por-
tions of tbe brain which supply the centres of touch, vision, and
hearing.
Discussion as to how the ancestors of man were fashioned has
chiefly dealt with the rival claims of four lines of structural evo-
lution : first, the assumption of the erect altitude; second, the
development of the opposable thumb; third, the growth of the
brain; and fourth, the acquisition of the power of speech. The
argument for the erect attitude suggested by Lamarck, and ably
put by Munro4 in 1893, indicates that the cultivation of skill
ANCESTRY OF THE ANTHROPOID APES 59
with the hahds and fingers lies at the root of man's mental su-
premacy. Elliot Smith's argument that the steady growth and
specialization of the brain itself has been the chief factor in lead-
ing the ancestors of man step by step upward indicates that
Fig. 24. The evolution of the brain. Outlines (top view) of typical human
and prehuman brains, showing the narrow forebrain of the primitive type
and the successive expansion^ the seat of the higher mental faculties in
the successive races.
v
such an advance as the erect attitude was brought about be-
cause the brain had made possible the skilled movements of
the hands.
The true conception of prehuman evolution, which occurred
during Miocene and Pliocene times, is rather that of the coin-
cident development of these four distinctively human powers.
It appears from the limb proportions in the Neanderthal race
60 MEN OF THE OLD STONE AGE
that the partly erect attitude and walking gait were assumed
much earlier in geologic time than we formerly imagined. The
intimate relation between the use of the opposable thumb and
the development of the higher mental faculties of man is sus-
tained to-day by the discovery that one of the best methods of
developing the mind of the child is to insist upon the constant
use of the hands, for the action and reaction between hand and
brain is found to develop the mind. A similar action and reac-
tion between foot and brain developed the erect gait which re-
leased the hand from its locomotive and limb-grasping function,
and by the resultant perfecting of the motion of thumbs and fin-
gers turned the hand into an organ ready for the increasing
specialization demanded by the manufacture of flint imple-
ments.
This is the stage reached, we believe, in late Pliocene times
in which the human ancestor emerges from the age of mammals
and enters the age of man, the period when the prehistory of
man properly begins. The attitude is erect, the hand has a well-
developed opposable thumb, the centres of the brain relating to
the higher senses and to the control of all the motions of the
limbs, hands, and fingers are well developed. The power of
speech may still be rudimentary. The anterior centres of the
brain for the storing of experience and the development of ideas
are certainly very rudimentary.
Change of Environment in Europe
Considering that the origin and development of any creature
are best furthered by a struggle for existence sufficiently severe
to demand the full and frecjuenL exercise of its powers of mind
and body, it is interesting to trace the sequence of natural events
which prepared western Europe for the entrance of the earliest
branches of the human race. The forests and plants portray
even more vividly than the animals the changing conditions of
the environment and temperature which marked the approach
and various vicissitudes of the great Ice Age.
PLIOCENE CLIMATE, FORESTS, AND LIFE 61
The forests of central France in Pliocene times, as well as
those of the valley of the Arno in northern Italy, were very similar
to the forests of the middle United States at the present time,
comprising such trees as the sassafras, the locust, the honey-
locust, the sumach, the bald cypress, and the tulip. Thus the
regions which harbored the rich forest and meadow fauna of
northern Italy in Upper Pliocene times abounded in trees fa-
miliar to-day in North and South Carolina, including even such
distinctively American forms as the sweet gum (Liquidambar
styraciflua) , the sour gum (Nyssa sylvatica), and the bay, beside
those above mentioned. To the south, along the Mediterranean,
there also flourished trees incident to a more tropical climate, the
bamboo, the sabal palm, and the dwarf fan-palm ; most interest-
ing is the presence of the sabal, which now flourishes in the sub-
tropical rain forests of central Florida. The sequoia also was
abundant. Toward the close of the Pliocene the first indications
of the coming Glacial Epoch were a lowering of the temperature,
and, in the higher mountainous areas perhaps, a beginning of the
glacial stages.
The ancestors of the modern forests of Europe predominated
in central France : the oak, the beech, the poplar, the willow, and
the larch. It is these forests, which survived the vicissitudes of
glacial times, that gave descent to the forests of Postglacial
Europe, while all the purely American types disappeared from
Europe and are now found only in the temperate regions of the
United States.5
We have seen that few anthropoid apes have been discovered
either in the Middle or Upper Pliocene of Europe ; the gibbon-
ape line disappears with the Pliohylobates of the Upper Pliocene.
These animals are, however, rarely found in fossil form, owing
to their retreat to the trees in times of flood and danger, so that
we need not necessarily assume that the anthropoids had actually
become extinct in France. The primates which are found in the
Upper Pliocene belong to the lower types of the Old World
monkeys, related to the living langur of India and to the macaque
and baboon. The evidence, as far as it goes, indicates that the
62 MEN OF THE OLD STONE AGE
ancestors of man were at this time evolving in Asia and not in
Europe. This evidence, nevertheless, would be completely off-
set if it could be proven that the eoliths, or primitive flints, found
in various parts of Europe from Oligocene to Pleistocene times
are really artifacts of human or prehuman origin.
The mammals of Europe in Pliocene times were derived by
very remote migrations from North America and, more directly,
from southern Asia. The Oriental element is very strong, in-
cluding types of rhinoceroses now peculiar to Sumatra and south-
ern Asia, numerous mastodons very similar to the south Asiatic
types of the times, gazelles and antelopes, including types re-
lated to the existing elands, and primitive types of horses and of
tapirs. Among the carnivores in Europe similar to south Asiatic
species were the hyaenas, the dog bears (Hycenarctos) , the civets,
and the pandas (Ailurus) ; there were also the sabre- tooth tigers
and numerous other felines. In the trees were found the south
Asiatic and north African monkeys ; and in the forests the axis
deer, now restricted to Asia. But the most distinctive African-
Asiatic animal of this period was found in the rivers ; namely, the
hippopotamus, which arrived in Italy in the early Pliocene and
ranged south by way of the Sicilian land bridge into northern
Africa and east along the southern shores of the Black Sea to
the Siwalik hills of India. Thus, many of the ancestors of what
we have termed the African- Asiatic mammal group of Pleistocene
times had already found their way into Europe early in Pliocene
times. In middle and late Pliocene times there arrived three
very important types of mammals which played a great role in
the early Pleistocene. These are :
The true horses (Equus stenonis) of remote North American
origin.
The first true cattle (Leptobos elatus), originating in southern
Asia.
The true elephants, hrst Elcphas planifrons and later E. mcridi-
onalis, better known as the southern mammoth, both orig-
inating in Asia.
TRANSITION TO THE PLEISTOCENE 63
The forests and river borders of the valley of the Arno, near
Florence, contained all these African-Asiatic animals in Upper
Pliocene times. Here they received their names which remind
us of this region of Italy as it is to-day, such as the Etruscan
rhinoceros (Dicer orhinus etruscus), the Florentine macaque (Ma-
cacus florentinus) , Steno's horse (Equus stenonis), the Etruscan
cattle (Leptobos etruscus), which was the earliest ox to reach
Europe.
In Italy and France these African-Asiatic mammals were
mingled with ancestors of the more hardy Eurasiatic forest and
meadow group. Of these the most graceful were a variety of
deer with very elaborate or many-branched antlers, hence known
as the 'polycladine' deer. In the forests roamed the wild boars
of Auvergne (Sus arvemensis), also the bears of Auvergne (Ursus
arvernensis) , lynxes, foxes, and wildcats. In the rivers swam the
otter and the beaver, closely allied to existing forms. Among the
rocks of the high hills were the pikas or tailless hares (Lagomys),
also hamsters, moles, and shrews.
Many of the most characteristic animals of the dry modern
plateaus of Africa had disappeared from Europe before the close
of Pliocene times, namely, species of gazelles, antelopes, and the
hipparion horses, all of which were adapted to the dry uplands
or deserts of Africa. In the remaining faune Pliocene recente of
French authors we find evidence that the Pliocene in all of western
Europe closed with a moist, warm, temperate climate, with wide-
spread forests and rivers interspersed with meadows favorable
to the life of a great variety of browsing deer as well as of grazing
elephants, horses and cattle. The flora of the Middle Pliocene
as found at Meximieux indicates a mean annual temperature of
620 to 630 Fahr.
One of the proofs of the gradual lowering of temperature
toward the close of Pliocene times in Europe is the southward
retreat and disappearance of the apes and monkeys ; the Upper
Miocene gibbon is found as far north as Eppelsheim, near
Worms, Germany; in Lower Pliocene times the monkeys and apes
are found only in the forests of the south of France; in Upper
64 MEN OF THE OLD STONE AGE
Pliocene times they are recorded only in the forests of northern
Italy ; the evidence, so far as it goes, indicates a gradual retreat
toward the south.
Finally, at the end of the Pliocene there existed very close
geographic relations eastward with the mammalian life of India
by way of what was then the isthmus of the Dardanelles and
southward with the mammalian life of Africa by way of the
Sicilian land bridge. This would indicate that the long lines of
eastward and westward migration were open and favorable to the
arrival in western Europe of new migrants from the far east,
including perhaps the most primitive races of man. There is not
the least evidence that Pliocene man or ancestors of man existed in
Europe, excepting such as may be afforded by the problematic
eoliths, or most primitive flints.
The First Glaciation '
In Upper Pliocene times cold marine currents6 from the north
began to flow along the southeastern coast of England, with in-
dications of a gradually lowering temperature culminating at a
time when the sea abounded in the arctic mollusks, which have
been preserved in the 'Weybourn Crags,' a geologic formation
along the coast of Norfolk. This arctic current was the herald
of the First Glacial Stage.
It does not appear that a glacial cap of any considerable
extent was formed in Great Britain at this stage, but about this
time the first great ice-cap was formed in British North America
west of Hudson Bay, which sent its ice-sheets as far south as
Iowa and Nebraska. In the latter State forests of spruce and
other coniferous species indicate the appearance of a cool tem-
perate flora in advance of the glaciation. In the Swiss Alps the
snow descended 1,200 meters below the present snow-line, and
in Scandinavia and northern Germany the first great ice-sheets
were formed from which flowed the glaciers and rivers convey-
ing the 'Old Diluvium,' or the * oldest drift.' Accompanying the
cold .wave along the eastern coast of England we note, in the
famous fossil deposits known as the 'Forest Bed of Cromer,'
THE FIRST GLACIATION
65
which overlie the Weybourn Crags, the arrival from the north
of the fir-tree (Abies). This is most significant, because it had
hitherto been known only in the arctic region of Grinnell Land,
and this was its first appearance in central Europe. Another
Fig. 25. The First (Gtinz) Glacial Stage was far less extensive than that in the above map,
which shows Europe in the Second Glacial Stage, during the greatest extension of the
ice-fields and glaciers (dots), a period of continental depression in which the Mediter-
ranean, Black, and Caspian Seas were connected. The line from Scandinavia to the
Atlas Mountains corresponds with the section shown in Fig. 13, p. 37. Drawn by
C. A. Reeds, after James Geikie and Penck.
herald of northern conditions was the first occurrence of the
musk-ox in England, which is attributed7 to the 'Forest Bed'
deposits.
While Great Britain was less affected at this time than other
regions, there is no doubt as to the vast extent of the First Glacial
Stage in British America, in Scandinavia, and in the Alps ; in the
latter region it has been termed 'the Gunz stage' by Penck and
Bruckner. The 'drift' deposits have a general thickness of 98^
66 MEN OF THE OLD STONE AGE
feet (30 m.), but they are largely covered and buried by those
of the far more extensive Second Glacial Stage. The Scandi-
navian ice-sheet8 not only occupied the basin of the Baltic but
overflowed Scania — the southern part of Sweden — and extended
as far south as Hamburg and Berlin. In the Alps the glaciers
Fig. 26. The musk-ox, belonging to the tundra region of the arctic circle, which is
reported to have migrated as far south as the southern coast of
England during the First (Giinz) Glacial Stage.
passed down all the great mountain valleys to the low grounds of
the foreland, implying a depression of the snow-line to 4,000 feet
below its present level.
The First Interglacial Stage. Eoliths
Proofs that a prolonged cool wave passed over Britain dur-
ing the first glaciation are seen in its after effects, namely, in the
modernization of the forests and in the disappearance both in
Britain and France of a very considerable number of animals
which were abundant in Upper Pliocene times. Yet by far the
greater part of the Pliocene mammal life survived, a fact which
tends to show that, while very cold conditions of climate and
great precipitation of moisture may have characterized the regions
immediately surrounding the ice-fields, the remainder of western
Europe at most passed through a prolonged cool period during
THE FIRST INTERGLACIAL STAGE 67
the climax of the First Glacial Stage. This was followed during
the First Interglacial by the return of a period somewhat warmer
than the present.
This First Interglacial Stage is known as the Norfolkian, from
the fact that it was first recognized in Europe in the deposits
known as the 'Forest Bed of Cromer/ Norfolk, which contain
rich records not only of the forests of the period, but of the noble
forms of mammals which roamed over Great Britain and France
in Norfolkian times. The forests of Norfolk, in latitude 5 2° 40' N.
mainly abounded in trees still indigenous to this region, such as
the maple, elm, birch, willow, alder, oak, beech, pine, and spruce,
a forest flora closely corresponding to that of the Norfolk and
Suffolk coasts of England at the present time, although we find
in this fossil flora several exotic species which give it a slightly
different character.9 From this tree flora Reid concludes that
the climate of southeastern England was nearly the same as at
present but slightly warmer.
We note especially that a very great change had taken place
in the entire disappearance in these forests of the trees which in
Pliocene times were common to Europe and America, as described
above ; in other words, the flora of Europe was greatly impover-
ished during the first cold wave.
In southern France, as at the present time, the interglacial
climatic conditions were milder, for we find numerous species
of plants, which are now represented in the Caucasus, Persia,
southern Italy, Portugal, and Japan. Thus the First Intergla-
cial Stage, which was a relatively short one, enjoyed a tempera-
ture now belonging about 40 of latitude farther south.
This First Interglacial Stage is also known as the St.-Prestien,
because among the many localities in France and Italy which
preserve the plant and mammal life of the times that of St. Prest,
in the Paris basin, is the most famous. Here in 1863 Desnoyers10
first reported the discovery of a number of mammal bones with
incision lines upon them, which he considered to be the work of
man. These deposits were regarded at the time as of Pliocene
age, and this gave rise immediately to a wide-spread theory
OS MEN OF THE OLD STONE AGE
of the appearance of man as early as the Pliocene. The human
origin of the incisions discovered by Desnoyers has long been a
matter of dispute and is now regarded as very improbable. Sim-
ilar lines may be of animal origin, namely, marks left by claws
Fig. 27. The giant deer (Megaceros), which first appears in western Europe during the
First Interglacial Stage, probably as a migrant from the forested regions of Eurasia.
After a painting by Charles R. Knight, in the American Museum of Natural History,
or teeth, or due to accidental pressure of sharp cutting surfaces.
However, we do not pretend to express an opinion of any value
as to the cause of these incisions. Supposed confirmation of the
evidence of Desnoyers of the existence of Pliocene man was the
alleged finding by Abbott of several worked flints, two in situ, in
the 'Forest Bed of Cromer,' Norfolk. Many years later in sim-
ilar deposits at St. Prest were discovered the supposed 'eoliths'
which have been referred to the Etage Prestien by Rutot. The
age of the Si. Prest deposits is, therefore, a matter of the very
highest interest and importance.
EARLY PLEISTOCENE FAUNA 60
St. Prest is not Pliocene; it is rather the most ancient Pleis-
tocene deposit in the basin of Paris,11 and these incised mammal
bones probably date from the First Interglacial Stage. The bed
which has yielded the incised bones and the rich series of fossils
consists of coarse river sands and gravels, forming part of a ' high
terrace/ o8>< feet (30 m.) above the present level of the river
Eure. This, like other 'high terraces,' contains a characteristic
First Interglacial fauna, including the southern mammoth {E.
meridionalis) , and Steno's horse {E. stenonis). We also find here
other very characteristic early Pleistocene mammals, such as the
Etruscan rhinoceros {D. etruscus), the giant hippopotamus of
early Pleistocene times {H. major), the giant beaver of the early
Pleistocene {Trogontherium) , three forms of the common beaver
{Castor) , and one of the bison {Bison antiquus) . This mammalian
life of St. Prest is very similar to that of Norfolk, England ; to
that of Malbattu in central France, Puy-de-D6me ; of Peyrolles,
near the mouth of the Rhone, in southern France ; of Solilhac
near Puy ; of Durfort, Gard ; of Cajarc, Lot-et- Garonne ; and
finally to that of the valley of the Arno, in northern Italy.
One reason why certain authors, such as Boule and Deperet,
have placed this stage in the Upper Pliocene is that the mam-
mals include so many surviving Pliocene forms, such as the
sabre-tooth tigers {Machcerodus), the ' polycladine ' deer with the
elaborate antlers (C. sedgwicki), the Etruscan rhinoceros, and
the primitive Steno's horse. But we have recently discovered
that, with the exception of the 'polycladine' deer, these mam-
mals certainly survived in Europe as late as the Second Inter-
glacial Stage, and there is said to be evidence that some even
persisted into the Third Interglacial Stage.
It is, therefore, the extinction or disappearance from Europe
of many of the animals very abundant even in late Pliocene
times which marks this fauna as early Pleistocene. Anthropoid
apes are no longer found; indeed, there is no evidence of the
survival of any of the primates, except macaques, which survive
in the Pyrenees to late Pleistocene times; the tapir has entirely
disappeared from the forests of Europe ; but the most signifi-
70
MEN OF THE OLD STONE AGE
cant departure is that of the mastodon, which is believed to
have lingered in north Africa and which certainly survived in
America into very late Pleistocene times. The animal life of
western Europe, like the plant life, has lost one part of its
Pliocene aspect while retaining another part, both in its mamma-
lian fauna and in its forest flora.
The living environment as a whole, moreover, takes on a
novel aspect through the arrival, chiefly from the north, of the
7 v SmmI
Fig. 28. The sabre-tooth tiger (Machcsrodus), which survives from the Upper Pliocene
and is widely distributed over western Europe until the Middle Pleistocene. After
a painting by Charles R. Knight, in the American Museum of Natural History.
more hardy animals and plants which had been evolving for a
very long period of time in the temperate forests and meadows
of Eurasia to the northeast and northwest. From this Eurasiatic
region came the stag, or red deer (Cervus elaphus), also the giant
deer (Megaceros), and from the northerly swamps the broad-
headed moose (Alces latifrons). The presence of members of the
deer family (Cervidae) in great numbers and representing many
different lines of descent is one of the most distinctive features
of First Interglacial times. Beside the new northerly forms
mentioned above, there was the roe-deer (Capreolus), which still
survives in Europe, but there is no longer any record of the
EARLY PLEISTOCENE FAUNA 71
beautiful axis deer (Axis), which has now retreated to southern
Asia. The ■ polycladine ' deer, first observed in the valley of the
Arno, is represented in First Interglacial times by Sedgwick's
deer (C. sedgwicki), in Norfolk, and by the species C. dicranius
of northern Italy, where there also occurs the 'deer of the Car-
nutes' (C. carnutorum).
We observe that browsing, forest-living, and river-living types
predominate. Among the forest-frequenting carnivores were the
wolverene, the otter, two kinds of bear, the wolf, the fox, and
the marten; another forest dweller was a wild boar, related to
the existing Sus scrofa of Europe.
Thus in the very beginning of Pleistocene times the forests of
Europe were full of a wild life very similar to that of prehistoric
times, mingled with which was the Oriental element, the great
elephants, rhinoceroses, ancl hippopotami connecting Europe with
the far east. Among these eastern migrants in the early Pleis-
tocene were two new arrivals, the primitive wild cattle (Bos
primigenius) , and the first of the bison (Bison prisons) .
The theoretical map of western Europe during First Inter-
glacial times (Fig. 12, also Fig. 56) enables us to understand
these migrations from the northeast and from the Orient. As in-
dicated by the sunken river channels discovered on the old con-
tinental shelf, the coast-line extended far to the west to the bor-
ders of the continental plateau which is now sunk deep beneath
the ocean; the British Isles were separated from France not by
the sea but by a broad valley, while the Rhine, with the Thames
as a western tributary flowed northward over an extensive flood-
plain, which is the present floor of the North Sea basin.12 It is
not improbable that the rich mammalian life deposits in the
'Forest Bed of Cromer,' Norfolk, were washed down by tribu-
taries of this ancient Rhine River.
In all the great rivers of this enlarged western Europe occurred
the hippopotami, and along the river borders and in the forests
browsed the Etruscan rhinoceros. Among the grazing and
meadow-living forms of the Norfolk country of Britain were
species of wild cattle (Bos, Leptobos), together with two species
72 MEN OF THE OLD STONE AGE
of horses, including a lighter form resembling Steno's horse (E.
stenonis cocchi) of the Val d'Arno &nd a heavier type probably
belonging to the forests. The giant elephant of this period is the
southern mammoth (£. meridionalis trogontherii), a somewhat
specialized descendant of the Pliocene southern mammoth of the
valley of the Arno ; this animal is best known from a superb
specimen discovered at Durfort (Fig. 42) and preserved in the
Paris Museum. It is said to have attained a height of over 12
feet as compared with 11 feet 3 inches, the height of the largest
existing African elephants. It is probable that all these south
Asiastic migrants into Europe were partially or wholly covered
with hair, in adaptation to the warm, temperate climate of the
summers and the cool winters. To the south, in the still milder
climate of Italy, the arrival of another great species, known as
the 'ancient' or ' straight- tusked elephant' (E. antiquus), is re-
corded. This animal had not yet reached France or Britain.
Preying upon the defenseless members of this heterogeneous
fauna were the great machaerodonts, or sabre-tooth tigers, which
ranged over Europe and northern Africa and into Asia. It
does not appear that the true lions (Felis leo) had as yet entered
Europe.
An intercommunication of life over a vast area extending
6,000 miles from the Thames valley on the west to India on the
southeast is indicated by the presence of six or more similar or
related species of elephants and rhinoceroses. Twenty-five hun-
dred miles southeast of the foot-hills of the Himalayas similar
herds of mammals, but in an earlier stage of evolution, roamed
over the island of Java, which was then a part of the Asiatic
mainland.
The Trinil Race of Java
The human interest in this great life throng lies in the fact
that the migration routes opened by these great races of animals
may also have afforded a pathway for the earliest races of men.
Thus the discovery of the Trinil race in central Java, amidst a
THE TRINIL RACE 73
fauna closely related to that of the foot-hills of the Himalayas
and more remotely related to that of southern Europe, has
a more direct bearing upfm our subject than would at first
appear.
On the Bengawan River in central Java, a Dutch army sur-
geon, Eugen Dubois, had been excavating for fossils in the hope
of finding prehuman remains. In the year 1891 he found near
Trinil a deposit of numerous mammal bones, including a single
upper molar tooth which he regarded as that of a new species of
Fig. 29. Restoration of Pithecanthropus, the Java ape-man, modelled
by the Belgian artist Mascre. under the direction of
Professor A. Rutot, of Brussels, Belgium.
ape. On carefully clearing away the rock the top of a skull ap-
peared at about a meter's distance from the tooth. Further ex-
cavation at the close of the rainy season brought to light a second
molar tooth, and a left thigh-bone about 15 meters from the spot
where the skull was found, imbedded and fossilized in the same
manner. These scattered parts were described by Dubois13 in
1894 as the type of Pithecanthropus erectus* a term signifying the
* There is a vast Pithecanthropus literature. That chiefly utilized in the present de-
scription includes Dubois,13 Fischer,14 Schwalbc,15 Buchner.16
74 MEN OF THE OLD STONE AGE
upright-standing ape-man. The specific term erectus refers to
the thigh-bone, of which the author observes : " We must there-
fore conclude that the femur of Pithecanthropus was designed for
the same mechanical functions as that of man. The two articu-
lations and the mechanical axis correspond so exactly to the same
parts in man that the law of perfect harmony between the form
and function of a bone will necessitate the conclusion that this
Fig. 30. The Solo or Bengawan River in central Java. Scene of the discovery of the
type specimen of Pithecanthropus erectus in 1894. After Selenka and
Blanckenhorn. Compare map (Fig. 32, p. 75).
fossil creature had the same upright posture as man and likewise
walked on two legs. . . . From this it necessarily follows that
the creature had the free use of the upper extremities — now su-
perfluous for walking — and that these last were no doubt already
far advanced in that line of differentiation which developed them
in mankind into tools and organs of touch. . . . From a study
of the femur and skull it follows with certainty that this fossil
cannot be classified as simian. . . . And, as with the skull, so
also with the femur, the differences that separate Pithecanthropus
from man are less than those distinguishing it from the highest
anthropoid. . . . Although far advanced in the course of differ-
entiation, this Pleistocene form had not yet attained to the human
THE TRINIL RACE
75
Volcano
La woe 3Z5+ M
i
type. Pithecanthropus erectus is the transition form between
man and the anthropoids which the laws of evolution teach us
must have existed. He is the ancestor of man."
Thus the author placed Pithecanthropus in a new family, of
the order Primates, which he named the Pithecanthropidae.
The geologic age
of the bones referred
to is a matter of first
importance. The re-
mains of Pithecan-
thropus lay in a de-
posit about one meter
in thickness, consist-
ing of loose, coarse,
tufaceous sandstones,
gray clay, and under
SS\I
1000 M
500M
V /" * ujfz\ and Recent /^/^£
y^> ^ ~ -^ Yy - /\ Mluvium .,
/ > *> ^M-r, ? \ Neogene
''?> ''All35 t\ trinil 1
0 10 20 30 tf SO to 70 30 Kilometers
Fig. 31. Geological section of the volcano of Lawoe
in the Solo River basin. Drawn by C. A. Reeds.
below this a stratum of hard, blue-
that marine breccia. Above the Pith-
ecanthropus layer were the 'Kendeng' strata, a many-layered
tufaceous sandstone, about 15 meters in thickness. This geo-
logic series was considered by Dubois and others to be of late
Tertiary or Plio-
cene age ; Pithe-
canthropus ac-
cordingly became
known as the long-
awaited 'Pliocene
ape-man.' Subse-
quent researches
by expert geolo-
gists have tended
to refer the age to
the early Pleisto-
cene.17 According
to Elbert18 the
Kendeng strata
overlying the Pithecanthropus layer correspond to an early plu-
vial period of low temperature and, in point of time, to the
zsmile
Fig. 32. Map of the Solo River, showing the Pithecan-
thropus discovery site, also two excavations (Pit No. i,
Pit No. 2) in the ancient gravel of the river-bottom, made
by the Selenka-Blanckenhorn expedition of 1907. After
Selenka and Blanckenhorn.
76 MEN OF THE OLD STONE AGE
Ice Age of Europe. For even in Java one can distinguish
three divisions of the Pleistocene period, including the first
period of low temperature to which the Pithecanthropus layer is
referred.
The fossil mammals contained in the Pithecanthropus layer
have also been thoroughly studied,19 and they tend to confirm
the original reference to the uppermost Pliocene. They yield a
very rich fauna similar to that of the Siwalik hills of India, in-
cluding the porcupine, pangolin, several felines, the hyaena, and
River Solo
I Pithecanthropus r 6> Profile of the skull of Pithecanthropus, as restored by
J.-H. McGregor. 19 14. One-third life size.
known, it will be found to be very similar to that of the Heidel-
berg man, the final conclusion being that Pithecanthropus and
the nearly allied Heidelberg man may be regarded as the common
ancestors of the Neanderthal race, on the one hand, and of the
higher races on the other. There are, however, reasons for ex-
cluding Pithecanthropus from the direct ancestral line of the higher
races of man.
This prehuman stage has, none the less, a very great signifi-
cance in the developmental history of man. In our opinion it is
the very stage which, theoretically, we should anticipate finding
in the dawn of the Pleistocene. A similar view is taken by
Buchner,24 who presents in an admirable diagram (Fig. 117) the
80
MEN OF THE OLD STONE AGE
result of his comparison of twelve different characters in the
skulls of Pithecanthropus, the Neanderthals, the Australians, and
the Tasmanians. One of the main objects of Buchner's research
was a very detailed comparison of the Trinil skull with that
of the lowly and now extinct Tasmanian race, which, we observe
Fig. 37. Three views of the skull of Pithecanthropus, as restored by
J. H. McGregor, showing the original (shaded) and restored
(black lines) portions. About one-quarter life size.
in the diagram, occupies a position only a little higher than that
of the Spy-Neanderthal race.
If the femur belongs with the skull, the Trinils were a tall race,
reaching a height of 5 feet 7 inches as compared with 5 feet 3
inches in the Neanderthals. The thigh-bone (Fig. 122) has a very
slight curvature as compared with that of any of the apes or
lemurs, and in this respect is more human ; it is remarkably
elongate (455 mm.), surpassing that of the Neanderthals; the
THE TRINIL RACE
81
shin-bone (tibia) was probably correspondingly short. The two
upper grinding-teeth preserved are much more human than those
of the gibbon, but they do not resemble those of man closely
enough to positively confirm the prehuman theory. Dubois ob-
serves :25 "That the tooth belongs to some hominid form needs no
Fig. 38. Profile view of the head of Pithecanthropus, the Java ape-man,
after a model by J. H. McGregor. One-quarter life size.
further demonstration. Aside from its size and the greater
roughness of the grinding surface, it differs from the human
grinder in that the less developed cusp of Pithecanthropus is the
posterior cusp next the cheek, while in man it is generally the
posterior cusp next the tongue. The simplification of the crown
and the root of the Trinil grinder is quite as extensive as it usually
is in man."
Various efforts have been made to supplement the scattered
and scanty materials collected by Dubois. The Selenka expedi-
tion of 1907-8 brought back a human left lower molar as the
only result of an express search for more Pithecanthropus remains.
82
MEN OF THE OLD STONE AGE
Dubois is also said to possess the fragment of a primitive-looking
lower jaw from the range known as the Kendeng Hills, at the
southern base of which lies the village of Trinil.
It remains for us to consider the stage of psychic evolution
attained by the Trinil race, and this naturally turns upon the
i'*
I
Fig. 39. Front view of the head of Pithecanthropus, the Java ape-man,
after a model by J. H. McGregor. One-quarter life size.
erect attitude and what little is known of the size and proportions
of the brain.
The assumption of the erect attitude is not merely a question
of learning to balance the body on the hinder extremities.26 It
involves changes in the interior of the body, the loss of the tail,
the freeing of the arms, and the establishment of the diaphragm
as the chief muscle of respiration. The thigh-bone of Pithecan-
thropus is so much like that of man as to support the theory that
the erect position may have been assumed by the ancestors of
man as early as Oligocene times. It would appear that Pithe-
canthropus had free use of the arms and it is possible that the
THE TRINIL RACE
83
control of the thumb and fingers had been cultivated, perhaps
in the fashioning of primitive implements of wood and stone.
The discovery of the use of wood as an implement and weapon
probably preceded that of the use of stone.
Elliot Smith describes this stage of development as follows :'27
". . . The emancipation of the hands from progression threw
the whole responsibility upon the legs, which became more effi-
cient for their pur-
pose as supports once
they lost their pre-
hensile powers and
became elongated
and specialized for
rapid progression.
Thus the erect atti-
tude became stereo-
typed and fixed and
the limbs specialized,
and these upright
simians emerged from
their ancestral forests
in societies, armed
with sticks and stones and with the rudiments of all the powers
that eventually enabled them to conquer the world. The greater
exposure to danger which these more adventurous spirits en-
countered once they emerged in the open, and the constant
struggles these first semihuman creatures must have had in
encounters with definite enemies, no less than with the forces of
Nature, provided the factors which rapidly weeded out those
unfitted for the new conditions and by natural selection made
real men of the survivors."
The undeveloped forehead of Pithecanthropus and the dimin-
utive frontal area of the brain indicate that the Trinil race had a
limited faculty of profiting by experience and accumulated tra-
dition, for in this prefrontal area of the brain are located the
powers of attention and of control of the activities of all other
Fig. 40. Side view of brain of high type, illustrating
the contrast between the motor, sensory, and idea-
tional centres in a high type of modern brain; and
Elliot Smith's characterization of the probable cen-
tres in the Pithecanthropus type of brain. Modified
after M. Allen Starr.
84
MEN OF THE OLD STONE AGE
parts of the brain. In the brain of the ape the sensory areas of
touch, taste, and vision predominate, and these are well devel-
oped in Pithecanthro-
pus. The central area
of the brain, which is
the storehouse of the
memories of actions and
of the feelings associ-
ated with them, is also
well developed, but the
prefrontal area, which
is the seat of the faculty
of profiting by experi-
ence or of recalling the
consequences of previ-
ous responses to experi-
ence, is developed to a
very limited degree.28
Thus, while the brain
of Pithecanthropus is
estimated at 855-900
c.cm., as compared with
600 c.cm. of the largest
simian brain, and 930
c.cm. of the smallest
brain recorded in the
lower members of the
FlG. 41. Diagram showing the side (lower figure) , . . ,,
and top (upper figure) views of the outline of the nUman race, it indicates
Pithecanthropus brain as compared with that of ^ verv low Stage of in-
thc chimpanzee and the higher human types of «•
the Piltdown, Neanderthal, and modern races. telllgence.
Absence of Pal^eoliths and Presence or Eoliths in Western
Europe
Returning to First Interglacial conditions in Europe, we ob-
serve that the river courses flowed through the same valleys as
at present but that in early glacial times the channels were far
EOLITHS, OR PRIMITIVE FLINTS 85
broader and were elevated from ioo to 150 feet above the present
relatively narrow river levels. The vast floods of the succeeding
glaciation filled these valleys, but some of the 'high terraces'
were already formed. It is extremely important to note that
Pre-Chellean flints or true palaeoliths have never been found in
the sands or gravels of these 'high terraces.'
Eoliths found on this ' high- terrace ' level at St. Prest belong
to the Prestien culture of Rutot,29 who regards this station as of
Upper Pliocene age. These, like other supposed Eolithic flints,
are very rough, but, rude as they are, they generally exhibit one
part shaped as if to be grasped by the hand, while the other part
is edged or pointed as for cutting. It is generally admitted that
these flints are mostly of accidental shapes, and there has been
little or no proof of their being fashioned by human hands. On
this point Boule30 observes : "As to the eoliths, I have combated
the theory not only because it seems to me improbable but because
a long geological experience has shown me that it is often impos-
sible to distinguish stones split, cut, or retouched by purely physi-
cal agents from certain products of rudimentary workmanship."
On the other side, it is interesting at this point to quote the
words of MacCurdy :31 "My opinion, based on personal experi-
ence, ... is that the existence of a primitive industry, antedat-
ing what is commonly accepted as Palaeolithic, has been estab-
lished. This industry occurs as far back as the Upper Miocene
and continues on through the Upper Tertiary into and including
the Lower Quaternary. The distinguishing characters of the in-
dustry remain but little changed throughout the entire period,
the subdivision of the period into epochs being based on stratig-
raphy [geologic stages] and not on industrial characters. The
requirements in the way of tools being very simple and the
supply of material in the way of natural flakes and fragments of
flint being very plentiful, the inventive powers of the population
remained dormant for ages. Hammer and knife were the orig-
inal tools. Both were picked up ready-made. A sharp-edged,
natural flake served for one, and a nodule or fragment served for
the other. When the edge of the flake became dulled by use, the
86 MEN OF THE OLD STONE AGE
piece was either thrown away or the edge was retouched for
further use. If hammer or flake did not admit of being held com-
fortably in the hand, the troublesome points or edges were re-
moved or reduced by chipping. The stock of tools increased
slowly with the slowly growing needs. As these multiplied and
the natural supply of raw material diminished, the latter was
supplemented by the manufacture of artificial flakes. When the
lesson of associating definite forms of implements with definite
uses was learned, special types arose, notably the amygdaloid
implement and the poniard. Then came the transition from the
Eolithic to the Palaeolithic, a stage that has been so thoroughly
investigated by Rutot."
It is not improbable that the Trinil race was in a stage of
Eolithic culture ; it is highly probable that the prehuman races
of this very remote geologic age used more than one weapon of
wood and stone.
The Great Second Glaciation
(Fig. 25, p. 65)
In early Pleistocene times a general elevation of southern Eu-
rope united the islands of the Mediterranean with Europe on the
north and with Africa on the south, forming broad land connec-
tions between the two continents which afforded both northward
and southward migration routes. At this time certain character-
istically African mammals, such as the straight-tusked elephant
and the lion, were probably finding their way north; Sicily at
this time gained its large fauna of elephants and hippopotami,
and the island of Malta was connected with the mainland, as
well as the easterly islands of Cyprus and Crete. It appears
probable that the connection between the Italian mainland and
Malta was renewed more than once.
The approach of the second glaciation is indicated along the
southeast coast of Great Britain by the subsidence of the land and
the rise of the sea, accompanied by a fresh arctic current, bring-
ing with it an invasion of arctic mollusks which were deposited
in a layer of marine beds directly over those which contain the
Pl. III. Pithecanthropus erectus, the ape-man of Java. Antiquity estimated at
500,00c years. After the restoration modelled by J. H. McGregor. It is not im-
probable that the prehuman races of this remote geologic age used more than one
natural weapon of wood or stone, the latter of the accidental 'Eolithic' type.
THE SECOND GLACIATION 89
rich warm fauna and flora of the 'Forest Bed of Cromer/ Nor-
folk.32 It also appears probable that a cold northern current
swept along the western coasts of Europe, and Geikie estimates
that a lowering of temperature occurred of not less than 200
Fahr., a change as great as is now experienced in passing from
the south of England to the North Cape.
The second glaciation was by far the greatest both in Europe
and America. In the region of the Pyrenees, which at the very
much later period of the Third Interglacial Stage became a favor-
ite country with Palaeolithic man, there were glaciers of vast
extent. This is realized by comparison with present conditions.
The largest of the present glaciers of the Pyrenees is only 2 miles
in length and terminates at a height of 7,200 feet above the sea.
During the greatest glaciation the snow appears to have de-
scended 4,265 feet below its present level. From the Pyrenees
through the Gallego valley into Spain there flowed a glacier 38
miles in length, while to the north the glacier in the valley of the
Garonne flowed for a distance of 45 miles to a point near Montre-
jeau. Even in its lower reaches this glacier was over half a mile
in thickness. To the east was a glacier 38 miles in length, filling
the valley of the Ariege and covering the sites of such great Pa-
laeolithic caverns as that of Niaux ; it is probable that at this time
the formation of this cavern began. That these glaciers were all
prior to the period of the Lower Palaeolithic Acheulean culture is
proven by the fact that Acheulean implements are frequently
met with lying on the surface of the moraines laid down by these
ancient ice-floes.33
To the north was the vast Scandinavian ice-field, which swept
over Great Britain and beyond the valleys of the Rhine, Elbe,
and Vistula, reaching nearly to the Carpathians. Even the lesser
mountain chains were capped with glaciers, including the Atlas
Mountains in northern Africa.
In North America from the great centre west of Hudson Bay
the ice-cap extended its drift southward into Missouri, Iowa,
Kansas, and Nebraska, beyond the limits of earlier and sub-
sequent glaciations.
90 MEN OF THE OLD STONE AGE
The materials of the chief 'high terraces' of the great river-
valleys of western Europe were deposited at this time.
Life or the Warm Second Interglacial Stage
The long warm period which followed the great glaciation is
remarkable in presenting the first proofs of the presence of man
in western Europe. It is the period of the Heidelberg race of
man {Homo heidelbergensis), known only from a single jaw dis-
covered by Schoetensack in the Mauer sands near Heidelberg,
in 1907. No other proofs of the existence of man have been
found in any of the deposits which took place during this vast
interval of geologic time, unless we accept the theory of Penck
and of Geikie that the Pre-Chellean and Chellean quarries of
the River Somme belong in the Second Interglacial Stage.
The vast duration of this interglacial time is evidenced both
in Europe and America by the deep cutting and wearing away
of the 'drifts' brought down by the second glaciation. Penck
believes that this 'long warm stage' represents a greater period
of time than the entire interval between the third glaciation and
the present time. The climate immediately following the re-
treat of the glaciers was cool and moist in the glaciated regions,
but this was followed by such a prolonged period of heat and
dryness that the glaciers on the Alps withdrew to a point far
above their present limits.
In one of the old 'high terraces' of the River Inn, in the
north Tyrol, is a deposit containing the prevailing forest flora of
the period, from which Penck concludes that the climate of Inns-
bruck was 20 C. higher than it is at the present time. Correspond-
ing with this the snow-line stood 1,000 feet above its present level,
'and the Alps, save for the higher peaks, were almost completely
denuded of ice and snow. A characteristic plant is the Pontic
alpine rose {Rhododendron poniicum), which nourishes now in an
annual temperature of 57°-65° Fahr.,34 indicating that the cli-
mate of Innsbruck was as genial as that of the Italian slopes of
the Alps to-day. This rhododendron is now found in the Cau-
casus. Other southern species of the time were a buckthorn,
THE SECOND INTERGLACIAL STAGE 91
related to a species now living in the Canary Islands, and the
box. There were also more hardy plants, including the fir {Pinus
sylvestris), spruce, maple, willow, yew, elm, beech, and moun-
tain-ash. The forests of the same period in Provence were, for
the most part, similar to those now found in that region ; out
of thirty-seven species twenty-nine still occur in this part of
southern France. On the whole, the aspect of southern France
at this time was surprisingly modern. The forests included oaks,
elms, poplars, willows, lindens, maples, sumachs, dogwood, and
hawthorn. Among the climbing plants were the vine and the
clematis. Here also were some forms which have since retreated
to the south, such as species of the sweet bay and laurel which
are now confined to the Canary Islands. The great humidity
of the time is indicated by the presence of certain species of con-
ifers which require considerable moisture. As in First Intergla-
cial times, the presence of the fig indicates mild winters.
It is difficult to imagine forests of this modern character,
which farther northward included a number of still more tem-
perate and hardy species, as the setting of the great African and
Asiatic life that roamed all over western Europe at this time. It
was the presence of hippopotami, elephants, and rhinoceroses
which gave to Lyell, Evans, and other early observers the im-
pression that a tropical temperature and vegetation were char-
acteristic of this long life period. These animals were formerly
regarded as proofs of an almost tropical climate, but the more
trustworthy evidence of the forests, strengthened by that of the
presence of very numerous hardy types of forest and meadow
animals, has set aside all the early theories as to extremely warm
temperatures during. Second Interglacial times.
The remains of what is still conveniently known as the ' faune
chaude, ' or warm fauna, are chiefly found in the sands and gravels
of the ancient beds of the Neckar, Garonne, and Thames, and
other rivers of the north and south, also in Essex, England. The
most surprising fact is that the mammal life of western Europe
remained entirely unchanged by the vast second glaciation just
described ; the few extinctions which occurred as well as a num-
92
MEN OF THE OLD STONE AGE
ber of new arrivals may be attributed to new geographical con-
nections with Africa on the south and to the steady progress of
migration from the far east.
Fig. 42. The hippopotamus {H. major) and the southern mammoth (E. meridional is
trogontherii), a pair of mammals which enjoyed a similar range over western Europe
from the close of the Pliocene until the middle of Third Interglacial times, when their
remains are found associated with flints of Pre-Chellean, Chellean, and early Acheulean
age. One-sixtieth life size. Drawn by Erwin S. Christman.
There were four very important and distinctive new arrivals
from the African-Asiatic world, namely, the straight-tusked or
ancient elephant (E. antiquus), the broad-nosed rhinoceros (D.
rnerckii), the African lion (Felis leo), and the African hyaena (H.
striata), which bespeak close geographical connections with
THE SECOND INTERGLACIAL STAGE 93
northern Africa. Of these the ancient elephant and the broad-
nosed rhinoceros were close companions; they enjoyed the same
regions and the same temperatures, their remains are very fre-
quently found together, and they survived to the very end of the
great life stage of western Europe, which closed with the advent
of the fourth glaciation. They are in contrast to the other pair
Fig 43. The other and hardier pair of large African- Asiatic mammals, namely, the
broad-nosed or Merck's rhinoceros (R. merckii) and the straight-tusked or ancient
elephant (E. antiquus), which entered western Europe in Second Interglacial times and
survived until Third Interglacial times, when their remains are found intermingled
with flints of the Acheulean and early Mousterian cultures. These mammals were
doubtless hunted by men of the early Neanderthal races. One-sixtieth life size.
Drawn by Erwin S. Christman.
of great mammals which was already present in Europe in Plio-
cene and First Interglacial times, namely, the southern mam-
moth, at this stage known as Elephas trogontherii, which had a
preference for the companionship of the hippopotamus (77. major) ;
it would seem that these animals were less hardy because both
in
MEN OF THE OLD STONE AGE
disappeared from Europe a little earlier than the ancient elephant
and Merck's rhinoceros.
The African lion would appear to have been a competitor of
the sabre-tooth tiger, for the latter animal now becomes less
abundant, although there is reason to believe that it survived
until the Third Interglacial Stage. With the ancient Pliocene
Fig. 44. Map showing the wide geographic distribution (horizontal lines) of Merck's
rhinoceros and the straight- tusked elephant, which first entered western Europe dur-
ing the First Interglacial Stage and survived until nearly the close of the Third Inter-
glacial Stage. The hippopotamus, which entered Europe in Pliocene times, survived
until after the middle of the Third Interglacial Stage and had a more limited dis-
tribution. After Boule.
type of the sabre-tooth were also found the Etruscan rhinoceros,
the primitive bear of Auvergne (Ursus arvernensis), and the giant
beaver (Trogontherium cuvieri).
The northern forests of the time were frequented by the broad-
faced moose, the giant deer, and the roe-deer, as well as by noble
specimens of the stag (Cervus elaphus). In the open forests and
meadows the wild cattle (Bos primigenius) began to be more
THE HEIDELBERG RACE 95
numerous and the bison (Bison prisms) also occurred. Among
the meadow or forest frequenting forms were horses of larger size,
such as the horses of Mosbach and of Siissenborn. In this assem-
blage of northern and southern types it is noteworthy that the
Eurasiatic forest and meadow types of mammals greatly predomi-
nate in numbers and in variety over the African- Asiatic types;
this, together with the flora, is an indication that the climate was
of a temperate character ; it is probable, therefore, that all the
mammals were well protected with a hairy covering and adapted
to a temperate climate. The fact that the fauna as a whole re-
mained practically unchanged throughout the second glaciation
is a proof not that it migrated to the south and then returned
but that the non-glaciated regions of western Europe were tem-
perate rather than cold.
The Heidelberg Race
To us by far the most interesting mammalian life is that found
south of the mouth of the Neckar along the ancient stream Elsenz,
Heidelberg man. where were deposited the lower ' sands of
Ancient elephant. Mauer/ containing the lower jaw of the Hei-
Etruscan rhinoceros, delberg man and the remains of many ani-
Mosbach horse. , r , -. . ■, m, ,. r ,-,.
w-ld , mals of the period. The enumeration of this
Broad-faced moose. entire fauna is very important, as indicating
Red deer, or stag. the temperate climatic conditions which sur-
Roe-deer. rounded the first true species of man which
Primitive bison , , .. , , , . i • -r- ^u
fwisent) has thus far been discovered m Europe. I he
Primitive ox discoverer, Schoetensack,35 referred these
(Aurochs, urus). mammals and the Heidelberg man to the
Auvergne bear. -p-rgt Tnterglacial Stage, and a similar opinion
Denmger s bear. _ , . . . ~ ., . ' rm
Lion has recently been expressed by Geikie. Ine
Wildcat. presence of the Etruscan rhinoceros would ap-
w°lf- pear to point to such great antiquity, but the
Beaven evidence afforded by this primitive animal is
overborne by that of three mammals which are highly character-
istic of Second Interglacial times ; these are the straight-tusked or
96
MEN OF THE OLD STONE AGE
ancient elephant (E. antiquus), the lion, and the Mosbach horse.
Excepting only the Etruscan rhinoceros, all these species fre-
quenting the ancient stream Elsenz and deposited with the
1 sands of Mauer ' occurred also in the forests and meadows of the
region now known as Baden, where the fossil mammal deposits
of Mosbach near the Neckar are found. A similar mammalian
life of a somewhat more recent time occurs in the river gravels of
Sussenborn, near Weimar. The horses of Mauer, of Mosbach,
SO "
Sea Level
Z000
[Mo
Middle Triassic \Mm
\Mu
Loner Trias sic
(So
Upper MuschelkalH
Middle
Lower ••
Upper Buntsandsrem
Middle
'3000 4-000 meters
Recent, marl, ham, sand
Redeposited loess of the slopes
younger loess
•i loam
Older
} Reetni
J Pleis-
tocene
Fig. 45. Section of the valley of the stream Elsenz, near Heidelberg, showing the location
of the Mauer sand-pit in which the Heidelberg jaw was discovered. An
ancient layer of river-drift. Drawn by C. A. Reeds.
and of Sussenborn* were of much larger size and of more
specialized character than Steno's horse of First Interglacial
times.
Thus the Heidelbergs, the first human race recorded in west-
ern Europe, appear in southern Germany early in Second Inter-
glacial times, in the midst of a most imposing mammalian fauna
of northern aspect and containing many forest-living species,
such as bear, deer, and moose ; in the meadows and forests
browsed the giant, straight- tusked elephant {E. antiquus), which
from the simple structure of its grinding-teeth is regarded as
similar in habit to the African elephant now inhabiting the
forests of central Africa ; the presence of this animal indicates a
relatively moist climate and well-forested country. The Etrus-
* These horses ure now identified respectively as E. mauerensis, E. mosbachensis, ana
E. sussenbornemis.
THE HEIDELBERG RACE
97
can rhinoceros differed from the larger Merck's form in the pos-
session of relatively short-crowned grinding-teeth, adapted to
Fig. 46. Sand-pit at Mauer, near Heidelberg, discovery site of the jaw of Heidel-
berg man. After Schoetensack.
a-b. 'Newer loess,' either of Third Interglacial or of Postglacial times.
b-c. 'Older loess' (sandy loess) of the close of Second Interglacial times.
c-f. The 'sands of Mauer.'
d-e. An intermediate layer of clay.
The white cross (X) indicates the spot at the base of the 'sands of Mauer' at
which the jaw of Heidelberg was discovered.
browsing habits and a forested country ; on the head were borne
two horns ; it was a long-limbed, rapidly moving type ; the herds
98 MEN OF THE OLD STONE AGE
of bison and of wild cattle (urus) which roamed over the plains
were now subject to the attack of the lion.
The discovery in 1907 of a human lower jaw in the base of
the 'Mauer sands' is one of the most important in the whole
history of anthropology. The find was made at a depth of 79
feet (24.10 m.) from the upper surface of a high bluff (Fig. 46),
in ancient river sands which had long been known to yield the
very old mammalian fauna described above. For years the
Fig. 47. The Heidelberg jaw, type of Homo heidelbergensis. About
two- thirds life size. After Schoetensack.
workmen had been instructed to keep a sharp lookout for human
remains. The jaw had evidently drifted down with the river
sands and had become separated from the skull, but it remained
in perfect preservation. The author's description may first be
quoted.36 The mandible shows a combination of features never
before found in any fossil or recent man. The protrusion of the
lower jaw just below the front teeth which gives shape to the
human chin is entirely lacking. Had the teeth been absent it
would have been impossible to diagnose it as human. From a
fragment of the symphysis of the jaw it might well have been
classed as some gorilla-like anthropoid, while the ascending ramus
resembles that of some large variety of gibbon. The absolute
certainty that these remains are human is based on the form of
the teeth — molars, premolars, canines, and incisors are all essen-
i
THE HEIDELBERG RACE 99
tially human and, although somewhat primitive in form, show
no trace of being intermediate between man and the anthropoid
apes but rather of being derived from some older common an-
cestor. The teeth, however, are somewhat small for the jaw ;
the size of the border would allow for the development of much
larger teeth ; we can only conclude that no great strain was put
on the teeth, and therefore the powerful development of the bones
of the jaw was not designed for their benefit. The conclusion is
Fig. 48. Side view of Heidelberg jaw (centre) compared with that of a chimpanzee (right)
and of an Eskimo (left) ; the latter an individual of exceptionally large proportions.
that the jaw, regarded as unquestionably human from the nature
of the teeth, ranks not far from the point of separation between
man and the anthropoid apes. In comparison with the jaws of
Neanderthal races, as found at Spy, in Belgium, and at Krapina,
in Croatia, we may consider the Heidelberg jaw as pre-Neander-
thaloid; it is, in fact, a generalized type.
In a conservative spirit, Schoetensack named the type rep-
resented by this jaw Homo heidelbergensis. Other authors have
regarded it as of distinct generic rank ; thus it has been termed
Paleoanthropus heidelbergensis by Bonarelli.37 The jaw itself is
extremely massive; the canine teeth, unlike those of the an-
thropoid apes and of the Piltdown race, do not project beyond the
line of the other teeth and were therefore not used as weapons
of offense and defense as in the anthropoids, in which these teeth
100
MEN OF THE OLD STONE AGE
are prominently developed as tusks. As noted by Schoetensack,
the teeth are not very massive in proportion to the jaw itself,
which is the most powerful
human jaw known, even ex-
ceeding the largest Eskimo
jaw and indicating a skull of
very massive and primitive
character. It resembles that
of the ape in the recession of
the chin, hence it has been
termed amentalis. There is
a large development of the
coronoid process of the man-
dible for the attachment of
the temporal muscle. This
jaw may well have been used
as a tool in the last stages
of the preparation of hides, as
is the practice of the Eskimo
races. We observe that the
powerful bony branches of
the jaw, when regarded from
above, close in upon the
space left for the tongue ; in
fact, the bone closes in to
such an extent as to inter-
fere seriously with the free
use of the tongue in articu-
late speech.
It would seem that in the
jaw, and probably in all
Fig. 49. The jaws shown in Fig. 48 seen
from above. A massive Eskimo jaw (above),
the Heidelberg jaw (centre), the jaw of a
chimpanzee (below). other characters of the skullj
as they become known, the Heidelberg race will be found to be
a Neanderthal in the making, that is, a primitive, more powerful,
and more ape-like ancestral form. In the matter of the retreat-
ing chin, the true Neanderthals of Spy, Malarnaud, Krapina,
THE HEIDELBERG RACE
101
and La Chapelle rank exactly half-way between the most in-
ferior races of recent man and the anthropoid apes.
Not only among the Eskimos, but generally throughout the
savage races of Australia and of other countries, the jaws are used
as tools ; among the Australians the teeth are very much worn
Fig. 50. Restoration of the Man of Heidelberg by the Belgian artist Mascre,
under the direction of Professor A. Rutot, of Brussels. This restoration pre-
sents an advance upon the Pithecanthropus type. In our opinion the Heidel-
berg man was more human and less ape-like in appearance.
down but are in admirable preservation. When seen from above,
we observe that the ' Heidelberg' grinding- teeth form a perfect
arch, or horseshoe-shaped arrangement, whereas in all the apes
the two lines of grinding-teeth are almost parallel with each other.
Thus, while there may be wide differences of opinion as regards the
relationships of the Heidelberg man, all agree that Schoetensack's
discovery affords us one of the great missing links or types in the
chain of human development.
The typical mammalian life of Second Interglacial times as
found at Mosbach and Siissenborn belongs perhaps to a some-
what more recent stage of Second Interglacial times than that of
the 'Mauer sands,' for in these localities the Etruscan rhinoceros
102 MEN OF THE OLD STONE AGE
is wanting and the more specialized broad-nosed rhinoceros is
abundant ; this animal differs from the Etruscan form in the pos-
session of relatively long-crowned grinding-teeth, which were bet-
ter adapted to grazing habits. On the head were borne two horns.
A variety of the southern mammoth (E. trogontherii) is so highly
characteristic of Second Interglacial times that Pohlig refers to
this life period as the E. trogontherii stage. From the structure of
its grinding-teeth it is regarded as similar in habit to the Asiatic
elephant, which now inhabits the forests of India, but it has the
peculiar concave forehead distinctive of the mammoth and quite
unlike the convex forehead of the Indian elephant. The bears of
this period belong to the primitive species U. deningeri and U.
arvernensis, for so far there is no certain record of the presence of
the true brown bear of Europe (17. arctos). The sabre- tooth
tiger of this time is preserved in the caverns of the Pyrenees near
Montmaurin, associated with the remains of the striped hyaena
(H. striata), a species which was widely distributed over western
Europe in early Pleistocene times. This species was contempo-
rary with, and later replaced by, the spotted hyaena (H. crocuta),
from which the very hardy cave-hyaena (H. crocuta speloza) of the
1 Reindeer Period,' descended. We observe that the 'polycla-
dine' deer of Upper Pliocene and First Glacial times has disap-
peared from western Europe ; nor are there any traces of the
axis deer. The hippopotamus is still represented by the giant
species, H. major.
Early Northern Migrations of the Reindeer
The animals that we have described belong in the warmer
and more temperate regions of Europe. In the regions near the
glaciers the reindeer was already to be found; in fact, this char-
acteristically northern animal is recorded in the gravels of Stis-
senborn, near Weimar.
There is evidence of a succession of climatic changes in the
region of Heidelberg. The Heidelberg jaw with its temperate
mammalian fauna occurred at the very base of the Mauer bluff,
MIGRATIONS OF THE REINDEER 103
but higher up the bluff (Fig. 46) on a corresponding level are
found the remains of mammals which indicate a marked lowering
of temperature and which are referred by some authorities to the
period of chilling climate that characterized northern Europe
toward the close of Second Interglacial times. The reindeer also
occurs in the 'high terrace' gravels of the River Murr, near
Steinheim ; thus, at Mauer, at Siissenborn, and at Steinheim, we
find proof that the reindeer had begun to spread over the colder
regions of Europe, and there is some ground for belief that it
found its way even as far south as the Pyrenees.
The evidence of the first cold, arid period which for the time
greatly affected the climate of western Europe is also found in
the layer of so-called ' ancient loess .' which lies in the bluff above
the ' sands of Mauer.' This loess covers the warm mammalian
deposits of the 'sands of Mosbach' as well as the 'high terraces'
of many of the ancient river- valleys. Both in Europe and Amer-
ica the climatic sequence of the Second Interglacial Stage from
moist to dry appears to have been the same.
Thus, after the recession of the ice-fields of the second glacia-
tion, the climate was at first cold and moist ; then followed a long
warm stage, favorable to the spread of forests ; this was finally
succeeded by a period of aridity in which the most ancient
'loess' deposits occurred. In Russia, also, the third glaciation
was preceded by an arid and steppe-like climate with high winds
favorable to the transportation of 'loess.'
No palaeoliths or other proofs of human occupation have been
found in this cold, dry period, for there is no evidence in any
part of Europe of camping stations in this 'ancient loess' such
as we find in the 'loess' which was deposited during the similar
arid period toward the close of Third Interglacial and again dur-
ing Postglacial times. Nor have we any record of the mammalian
life in this 'ancient loess' of Europe.
104 MEN OF THE OLD STONE AGE
The Third Glaciation *
This arid period in northern Europe and in North America
was followed by the moist, cool climate of the third glaciation.
It is estimated by Penck that the advance of these new ice-fields
began 120,000 years ago and that the period of advance and re-
treat of the glaciers was not less than 20,000 years. In the Alps
the snow-line descended 1,250 metres below the present level;
consequently this glaciation was more severe than the first but
somewhat less severe than the second. In northern Europe the
Scandinavian ice-field did not cover so wide an area as during the
second glaciation, although Britain and Scandinavia were again
deeply buried by ice; the glacial cap and glaciers flowed in a
westerly and southwesterly direction across Denmark and the
southern portion of the basin of the Baltic into Holland and
northern Germany. In the Alps the third glaciation sent vast
ice-floes along the valley of the Rhine, into eastern France, and
into the valley of the Po, where this glaciation was even more
extensive than the second. But the greatest glacier of this time
was that of the Isar, a southern tributary of the Danube, which
rises in the Bavarian Alps.38
During the Third Glacial Stage certain of the 'middle terraces'
along the Rhine and other rivers flowing from the Alps were
formed. In Britain,39 whereas during the second glaciation the
ice-fields extended as far south as the Thames, during the third
glaciation they did not extend beyond the midlands ; yet an
arctic climate prevailed over southern England, with tundra con-
ditions and temperature, as indicated by the plant deposits at
Hoxne40 in Suffolk. Even before the third glaciation began in
Europe a great ice-cap had formed over Labrador, on the eastern
coast of North America, and the ice-sheets flowing to the south
and southwest extended as far as Illinois, depositing the great
Illinoian 'drifts.'
* This tfhu iation as it occurs in northern Europe has been termed Polandian by Geikie ;
in the Alps Penck has termed it the Riss ; in America it is known as the Illinoian from
the great drifts it deposited over the State of Illinois.
THE THIRD GLACIATION
105
Along the borders of these great ice-fields in both countries
a cold and moist climate prevailed, for a prime condition of glacia-
tion is the heavy precipitation of snow. In northern Europe, be-
tween the great Alpine and Scandinavian ice-fields of the third
glaciation a cold climate undoubtedly prevailed; in the region
EUROPE DURING THE THIRD GLACIAL EPOCH. (RISS)
A- 8 Line of Profile
(AFTER JAMES GEIK1E)
Fig. 51. The ice-fields and glaciers of the Third Glacial Stage are seen to be much less
extensive than those of the Second Glacial Stage, shown in Fig. 25, p. 65. The conti-
nental depression and invasion of the sea is also believed to have been less extensive.
At this stage there are broad areas free from ice between the Scandinavian, the Alpine,
and the Pyrenean ice-caps. Drawn by C. A. Reeds, after James Geikie. (Compare
Fig. 13.)
of the Neckar River, near Cannstatt, is found a deposit known as
1 mammoth loam,' which Koken believed to be contemporaneous
with the period of the third glaciation, although the evidence is
certainly not convincing.41 Here are found fossil remains of the
Scandinavian reindeer, also of two very important new arrivals
in Europe from the tundra regions of the far northeast, animals
106
MEN OF THE OLD STONE AGE
which had wandered along the southern borders of the Scandi-
navian ice-sheet from the tundras of northern Russia and Siberia.
This is the first appearance in western Europe of the woolly mam-
moth (E. primigenius) and the woolly rhinoceros (D. antiquitatis) .
In this /mammoth loam' there also occur two species of horse,
the giant deer (Megaceros), the stag, the wisent, and the Aurochs.
If the woolly mammoth and the woolly rhinoceros actually en-
tered eastern Germany at this time, they certainly retreated to
the north with the approach of the warm temperate climate of the
Third Interglacial Stage, because no trace of these animals has
been found again in Europe until the advent of the fourth gla-
ciation.
(i
(2
(3
(4
(5
(6
(7
(8
(9
(io
(ii
(12
(13
(14
(15
(16
(i7
(i*
(19
(20
Gaudry, 1890. 1.
Smith, G. E., 1912.1, p. 582.
Op. cit.
Munro, 1893. 1.
Osborn, 1910.1, pp. 306, 307.
Geikie, J., 1894. 1, pp. 329~336;
1914.1, p. 227.
Dawkins, 1 883.1, pp. 576-579.
Geikie, J., 1914.1, p. 248.
Reid, C, 1908. 1.
Desnoyers, 1 863.1.
Haug, 1911.1, p. 1807.
Geikie, J., 1894. 1, p. 682; 1914.1,
p. 250.
Dubois, 1894. 1.
Fischer, 1913.1.
Schwalbe, 1899. 1; 1914.1.
Buchner, 1914.1.
Yolz, 1 907. 1.
Elbert, 1908. 1.
Selenka, 191 1.1.
Pilgrim, 1913.1.
(21) Schwalbe, 1899. 1, pp. 227, 228.
(22) Op. cit., p. 223.
(23) Schwalbe, 1914.1, pp. 601-606.
(24) Buchner, 1914.1, p. 129.
(25) Dubois, 1894,1, p. 14.
(26) Keith, 1912.1.
(27) Smith, G. E., 1912.1, p. 595.
(28) Op. cit.
(29) Rutot, 1907. 1.
(30) Boule, 1913.1, pp. 266, 267.
(31) MacCurdy, 1905. 1, pp. 468, 469.
(32) Geikie, J., 1914.1, p. 251.
(33) Op. cit., p. 255.
(34) Op. cit., p. 238.
(35) Schoetensack, 1908. 1.
(36) Op. cit., pp. 25-43.
(37) Bonarelli, 1909. 1.
(38) Penck, 1909. 1.
(39) Geikie, J., 1914.1, p. 258.
(40) Op. cit., pp. 257-262.
(41) Schmidt, 1912.1, p. 181
CHAPTER II
ARRIVAL OF THE PRE-CHELLEAN FLINT WORKERS DURING THE THIRD
INTERGLACIAL — GEOGRAPHY, CLIMATE, AND THE RIVER DRIFTS
— PRE-CHELLEAN FLINT INDUSTRY — THE PILTDOWN RACE —
MAMMALIAN LIFE — CHELLEAN AND ACHEULEAN INDUSTRIES —
THE USE OF FIRE — THE SECOND PERIOD OF ARID CLIMATE — THE
NEANDERTHAL RACE OF KRAPINA, CROATIA
The geologic epoch of the arrival of the Pre-Chellean flint
workers in western Europe is by far the most important and in-
teresting one before the prehistorian. Upon it depends the ques-
tion of the duration of the Old Stone Age, the date of appearance
of the Piltdown and of the Neanderthal races, and the whole
sequence of climatic and geographic changes surrounding the
early history of man. After weighing all the evidence very care-
fully, the balance of opinion seems to sustain the view that this
epoch should be placed after the close of the third glaciation and
before the advent of the fourth, that is, during the Third Inter-
glacial Stage.
Penck estimated that the third warm interglacial stage*
opened about 100,000 years ago and lasted between 50,000 and
60,000 years. According to the theory that we have adopted in
this work, the Third Interglacial and Fourth Glacial embraced
the entire period of Lower Palaeolithic time, a period of from
70,000 to 100,000 years, much longer than that of Upper Palaeo-
lithic time, which is estimated at 16,000 to 25,000 years.
Geologic Antiquity of the Beginning of the Stone Age
Attention should first be called to the fact that, preceding the
epoch we have now entered, the glacial and interglacial forces
*This stage is known as the Helvetian or Diimtenian of Geikie; it is the Riss-Wiim:
of Penck's terminology and the Sangamon of the American glaciologists.
107
108
MEN OF THE OLD STONE AGE
operating over the great peninsula of western Europe had left
their impress chiefly on the glaciated areas and only to a minor
degree on the free, non-glaciated areas. Until toward the close
of Third Interglacial times no traces of northern much less of
arctic forests and animals are discovered anywhere, except along
the borders of the ice-fields. It would appear as if the animal
and plant life of Europe were, in the main, but slightly affected
^POSTGLACIAL ^A(/A^
^ "Newer Loess'
Glacial Epoch Culture Stages Human Types
Fig. 52. Human types and culture stages of the last third of the Glacial Epoch. Theo-
retic estimates of the geologic and time divisions and introduction of human races during
the Third Interglacial, Fourth Glacial, and Postglacial Stages (see Fig. 14, p. 41).
Prepared by the author with the aid of C. A. Reeds.
by the first three glaciations. We cannot entertain for a moment
the belief that in glacial times all the warm flora and fauna mi-
grated southward and then returned, because there is not a
shred of evidence for this theory. It is far more in accord with
the known facts to believe that all the southern and eastern forms
of life had become very hardy, for we know how readily animals
now living in the warm earth belts are acclimatized to northern
conditions.
If, on the other hand, we depend solely on the testimony of
the life conditions, we might conclude that the Pre-Chellean flint
workers reached western Europe either in Second Interglacial
DATE OF THE PRE-CHELLEAN INDUSTRY
109
times, or during the third glaciation, or again during Third In-
terglacial times. Let us consider this evidence of the fossil
mammals more closely.
In favor of the theory that the Pre-Chellean culture is as an-
cient as Second Interglacial times; we should consider the fact
Fig. 53. Distribution of the principal Pre-Chellean and Chellean industrial stations
in western Europe.
that in several localities palaeoliths of Pre-Chellean if not of
Chellean type have been recorded in association with the re-
mains of a number of the more primitive mammals which we have
described above as characteristic of Second Interglacial times.
For example, at Torralba, Province of Soria, Spain, there has
been discovered1 an old typical Chellean camp site, containing
abundant remains of the broad-nosed rhinoceros and of the south-
ern mammoth, mingled with the remains of other mammals of
very ancient type, identified as the Etruscan rhinoceros and as
Ill)
MEN OF THE OLD STONE AGE
Steno's horse. Again, along the River Somme. near Abbeville, in
the gisemerU du Champ dc Marsr it is said that Pre-Chellean and
Chellean implements have been found in association with the
Etruscan rhinoceros, Steno's horse, and very numerous specimens
of the sabre-tooth tiger and of the striped hyaena. Moreover, in
Fig. 54. Western Europe during the extension of the ice-fields and glaciers (dots) of the
Third Glacial Stage — a period of continental depression believed to have been less
extensive than that of the Second Glacial Stage (see Fig. 25, p. 65). The line from
Scandinavia to northern Africa corresponds to the section shown in Fig. 13, p.
Drawn by C. A. Reeds, after Geikie and Penck. (Compare Fig. 13.)
Piltdown, Sussex, Pre-Chellean flints and the Piltdown skull are
said to have occurred in a layer containing a rhinoceros which
may be identified with the Etruscan. If these very ancient
species of animals are rightly recognized and determined, and if
they are truly found as reported in close association in the same
layers with Pre-Chellean and Chellean flints, the evidence may
DATE OF THE PRE-CHELLEAN INDUSTRY 111
be considered as quite strong that the beginning of Chellean cul-
ture dates from Second Interglacial times; unless, indeed, it should
prove that these primitive species of mammals survived into
Third Interglacial times in certain favored districts. We should
also consider the possibility that these more ancient animals, the
sabre-tooth tiger, Steno's horse, the Etruscan rhinoceros, and the
giant beaver, did not really belong in the same layer with these
Fig. 55. Excavation at Chelles-sur-Marne, the Palaeolithic station where Chellean flint
implements were first discovered. We observe the very close, regular, and unbroken
succession of the geological layers containing the Chellean, Acheulean, and Mousterian
flints.
old palaeoliths but were accidentally washed into this layer from
other more ancient deposits. As a rule, it is the most recent
animals which establish a prehistoric date, because we know that
a palaeolith cannot be older than the most recent mammal with
which it occurs.
The record of the three early glaciations is not fully written
in the animal and plant life, but it appears to be found in the
river channels. Both in England and France these channels at-
test flooded conditions during the earlier glaciations, in which large
112 MEN OF THE OLD STONE AGE
quantities of gravels and sands were transported, and it is of these
materials that the 'high terraces' were built up. It is chiefly
the geologic evidence which establishes the Pre-Chellean date.
Geologic and climatic lines of evidence in France indicate
that the Pre-Chellean culture is first witnessed during the begin-
ning of Third Interglacial times. This is the opinion of Boule,
Haug, Obermaier, Breuil, Schmidt, and many other geologists
and archaeologists. That the first Palaeolithic flint workers found
their way into western Europe during the early part of Third
Interglacial times is consistent with our observations on the se-
quence of climate, on the formation of the 'low river terraces,'
where palaeoliths of the earliest type occur, as well as with the
general succession of mammalian life throughout the climatic
changes of this interglacial period. It would appear, in explana-
tion of the facts cited above regarding the fossil mammals, that
when the Pre-Chellean flint workers established their camps along
the valley of the River Somme in northern France a very genial
climate prevailed in this region, favorable even, as we shall see,
to the survival of some of the Pliocene types of mammals, such
as the sabre- tooth tiger and the Etruscan rhinoceros.
During the early part of the Third Interglacial Stage the cli-
mate, so far as we can judge by the unchanged aspect of the
animal life, remained of the same warm temperate character.
Two only of the surviving Pliocene forms, namely, the sabre-
tooth tigers and the Etruscan rhinoceroses, became rare or extinct.
From evidence afforded in Kent's Hole, Devonshire, Dawkins is
led to believe that the sabre- tooth tiger survived in Britain until
Postglacial times. All the rest of the animal world, both the
African- Asiatic and the Eurasiatic mammals, continued to nourish
throughout western Europe.
Not until the latter part of Acheulean times do we discover
proofs of a decided change of climate ; in the approach of arid
conditions similar to those of the steppes of western Asia there
was a renewal of the great dust-storms and depositions of 'loess,'
such as had previously occurred toward the close of Second Inter-
glacial times ; this was followed by the still colder climate of the
i
DATE OF THE PRE-CHELLEAN INDUSTRY 113
fourth glaciation, which corresponds with the closing period of
Lower Palaeolithic culture.
The evolution of the Pre-Chellean into the Chellean and
finally into the Lower Acheulean palaeoliths certainly occupied a
very long period of time if we assign it merely the 50,000 or 60,000
years allotted to the Third Interglacial; but even this allotment
seems far too long when we observe the relatively limited depth
of the river deposits in which these flint cultures succeed each
other. For we cannot fail to be impressed by the regular and
very close and unbroken succession of the geologic layers contain-
ing the Chellean and Acheulean artifacts. (See Fig. 55.)
None the less it follows that a long lapse of time must be
allowed for each culture period, and for the advance in technique.3
It is this wide distribution that has enabled the de Mortillets
(father and son), Capitan, Riviere, Reboux, Daleau, Peyrony,
Obermaier, Commont, Schmidt, and others to establish in vari-
ous parts of Europe the main stages of the industrial evolution
of the Old Stone Age, or Lower Palaeolithic.
Subdivisions of the Lower Palaeolithic Cultures4*
Mousterian. Late industry of the Neanderthal races. Extensive use of
the 'flake.'
Late Mousterian. La Quina scrapers, small ' coups de poing,' and bone
anvils, closing with the Abri Audit culture.
Middle Mousterian. Culmination of the Mousterian ' point ' finely flaked
and chipped on one side, the best examples approaching the Solutrean
perfection of technique.
Early Mousterian. Heart-shaped ' coups de poing ' and Mousterian flake
'points' and flake scrapers.
Acheulean. Early industry of the Neanderthal races. Extensive use of
the nodular core.
Late A cheulean. Miniature ' lance points ' of La Micoque type, triangular
'coups de poing,' and flint flakes of Levallois type.
Middle Acheulean. Pointed oval 'coups de poing,' much lighter than the
Chellean types, and small implements similar to the Chellean but
much improved in workmanship.
Early Acheulean. Broad oval 'coups de poing' much more symmetrical
than the Chellean but still rather heavy. Small types.
* Modified after Schmidt.
114 MEN OF THE OLD STONE AGE
Chellean.
Late Chellean. Long pointed 'coups de poing,' in most cases flaked on
both sides, with little of the crust of the nodule adhering and the edges
still unsymmetrical. First appearance of the oval 'coups de poing.'
Early Chellean. First appearance of 'coups de poing' of almond shape.
Small implements, including scrapers, planes, and borers. All imple-
ments unsymmetrical and with uneven edges.
Pre-Chellean. Probable industry of the Piltdown and of the (Pre-
Neanderthaloid) Heidelberg races. Use of chance and accidental
forms. Forms partly accidental; retouch limited to the few strokes
necessary to give a point or edge to the tool, or to allow a firm grasp
(protective retouch). Prototypes of 'coup de poing' formed of flint
nodules with crust only partially removed.
If we suppose that the Pre-Chellean flint workers arrived
in Europe not earlier than Third Interglacial times, we can ex-
plain all the gradations in the evolution of their implements in
connection with the changes of climate and of animal life which
the geologic and fossil deposits reveal, especially in the valleys of
the Somme and of the Thames.
If, on the other hand, the Pre-Chellean is dated in Second In-
terglacial times,* it carries this culture back another hundred
thousand years and involves our prehistory in great difficulties.
First, there is no proof whatever that the Pre-Chellean and Chel-
lean flint workers lived during the period of the formation of the
'high river terraces' of the third glaciation, for no Palaeolithic
flints have ever been found buried in the sands or gravels of the
'high terraces.' The occurrence of archaic flints on the 'high
terraces' of the Somme and of the Seine is in superficial gravel
beds which were deposited long after these 'terraces' had been
cut by river action ; this is best seen in the Somme, where archaic
flints occur alike in the gravels deposited upon the 'low,' 'mid-
dle,' and 'high terraces.' Second, there is no proof that the
Pre-Chellean and Chellean flint workers passed through the cold
climatic period of the third glaciation ; nowhere in Europe have
* The weakness of Penck's argument for placing the Chellean in the Second Inter-
glacial was exposed by precise observations of Boule5 and Obermaier6 in the Alps, the
Jura, and the Pyrenees.
DATE OF THE PRE-CHELLEAN INDUSTRY 115
any records been found of their camps or stations in association
with the cold fauna or flora of Third Glacial times. Third, the
geographical evidence is equally at variance with the theory that
the Pre-Chellean flint workers entered Europe during the Second
Interglacial Stage, for we know positively that in many of the
great river-valleys of Europe, especially those surrounding the
Alps, the rivers were at much higher levels than at present and
that they were transporting the materials out of which the 'high
terraces ' were being formed or cutting these * terraces ' down by
erosion.
In other words, the geography of Europe in First and Second
Interglacial times was very different from what it is at present;
most of the river- valleys were broader and less deep ; some of
them had been eroded to a point below their present levels and
had begun to silt up in alluvial deposits. In Third Interglacial
times the river geography of Europe was substantially as it is
to-day, although the coast-lines were still very different.
When Pre-Chellean man appeared, we shall see that the
river-valleys of the Somme and Marne, in northern France, as
well as of the Thames, in southeastern England, were closely
similar to what they are at present in respect to their water-
levels ; in other words, the inland geography of Europe in the
north in Chellean times and in central and southern France in
the immediately succeeding Acheulean times was very much like
it is at present. The superficial characters of the valleys were
different ; the streams in Chellean times flowed through gravels
and sands, partaking of a glacial aspect; one or more of the
' river terraces' composed of sands and gravels were still sharply
defined, for the soft covering of 'loam' and alluvial soil from
the surrounding uplands and hills had not yet washed down to
soften the outlines of the 'terraces.' Neither were the 'terraces'
covered with the newer deposits of 'loess.'
Fig. 56. Restoration of the geography of western Europe during the Third Interglacial
Stage, showing the ancient land areas (dots) and the ancient river channels now
submerged by the sea. Modified after Avebury's Prehistoric Times by permission of
Henry Holt & Co. The six white crosses (X) indicate the location of the principal Pre-
Chellean stations of Filtdown on the Onse, and Cray's Thurrock on the Thames,
in England; of Abbeville, on the north bank, and St. Achcul, on the south bank of the
Somme, and Chclles on the Marne, in France; and of Helin in Belgium. It will be
observed that the English stations are separated from the others only by the ancient
broad valley corresponding with the present English Channel.
GEOGRAPHY AND CLIMATE 117
Secular Changes or Climate in Lower Paleolithic Times
We find evidences of four climatic and life phases during the
long period of Lower Palaeolithic evolution, as follows :
4. Cold Moist Climate. — Advent of the fourth glaciation. Arrival of the
'full Mousterian' culture and of the Neanderthal race in Belgium and
France. Repair of men to the warmer shelters, grottos, and entrances to
the caverns. Final disappearance of the hardy Merck's rhinoceros and the
straight-tusked elephant. Arrival of the tundra fauna, the reindeer, the
woolly mammoth, and the woolly rhinoceros. Refrigeration of western
Europe as far south as northern Spain and Italy. Wide distribution of
cold alpine, tundra, and steppe mammals all over Germany and France, and
into northern Spain. Cold tundra flora in the Thames valley, and at Hoxne,
in Suffolk. Migration of the tundra mammals, the reindeer, mammoth,
and rhinoceros all over southern Britain, Belgium, France, Germany, and
Austria.
3. Arid Climate in Western Europe. — Period of the close of the Acheulean
culture ; some of the flint workers seeking the shelter of cliffs and approach-
ing the entrances to the grottos during the cold season of the year. A dry
steppe climate, prevailing westerly winds, and deposits of 'loess' all over
northern France and Germany. Appearance of the first Neanderthaloid
men in Krapina, Croatia. Cool forest flora in the region of La Celle-sous-
Moret near Paris, followed by depositions of 'loess' and increasingly cool
and arid climate. Early Mousterian industry. Disappearance first of the
more sensitive pair of Asiatic mammals, the hippopotamus and the southern
mammoth (E. trogontherii) ; persistence of the more hardy, straight-tusked
elephant (E. antiquus) and the broad-nosed rhinoceros (D. merckii).
2. Continued Warm Temperate Period. — Time of the Chellean culture
found at Chelles, St. Acheul, Gray's Thurrock, Ilford, Essex, and southward
in Torralba, Spain. Abundance of hippopotami, rhinoceroses, southern
mammoths, and straight-tusked elephants in northern Germany at Taubach,
Weimar, Ehringsdorf, and Achenheim. Rare appearance of sabre-tooth
tigers. Temperate forest and alpine flora of Durnten and Utznach, Switzer-
land. Early Acheulean culture widely distributed over all of western
Europe.
1. Early Warm Temperate Period. — The warm climate of the Pre-Chel-
lean culture period, as seen in the valleys of the Somme, of the Thames, and
of the Seine near Paris, favorable to the southern mammoth and the hip-
popotamus. Apparent survival of the sabre-tooth tiger and the Etruscan
rhinoceros in favored regions. A warm temperate forest flora in La Celle-
118 MEN OF THE OLD STONE AGE
sous-Moret near Paris and in Lorraine. Arrival of the Pre-Chellean flint
workers and of the Piltdown race in southern England.
It is believed that the climate of Third Interglacial times when
it reached its maximum warmth was again somewhat milder than
the present climate in the same region. In the Alps the glaciers
and the snow-line retreated once more to their present levels.
The period opened with humid continental conditions. The
areas left bare by the ice were gradually reforested. A picture
of the climate in this warm period is presented in the region near
Paris in the so-called tuf de La Celle-sous-Moret (Seine-et-Marne) .
This tufa, which is a hot-springs deposit, overlies river-gravels of
Pleistocene age.7 The lower levels of the tufa contain the syca-
more-maple {Acer pseudoplatanus) , willows, and the Austrian pine,
indicating a temperate climate. Higher up in the same deposits
we find evidences of increasingly mild temperatures in the pres-
ence of the box (Buxus) and not infrequently of the fig-tree ; the
Canary laurel (Laurus nobilis) is somewhat rarer and both it
and the fig indicate that the winters were mild, because these
plants have the peculiarity of flowering during the winter season ;
we infer, therefore, that the climate was somewhat milder and
more damp than it is in the same region at the present time.
The mollusks also indicate greater equability of climate. These
deposits are believed to correspond with the period of Chellean
and early Acheulean industry.
The plants in the highest levels of the same tufa, however,
indicate the advent of a colder climate and also connect this
with the Acheulean culture stage through the presence of Acheu-
lean flints. The deposit of tufa is covered by a sheet of 'loess'
corresponding with the return of an arid period in late Acheulean
times, in the very heart of northern France. Thus we have a
record in the region near the present city of Paris of three cli-
matic phases, which are also more or less completely indicated
in deposits to the north along the River Somme and in the valley
of the ancient Thames.
In western France we again interpret the fossil flora of Lor-
raine as belonging to the cooler closing period of Third Intergla-
GEOGRAPHY AND CLIMATE 119
cial times and to the advent of the fourth glaciation, for here
the most northern varieties of the larch (Larix) and of the moun-
tain-pine (Pinus lambertiana) predominate.
The clearest view of the contemporary alpine forests is found
near Zurich in the lignitic deposits of Diirnten and of Utznach,
which are so characteristic of the temperate period of the Third
Interglacial Stage that Geikie has proposed to call this stage the
Durntenian* It was, we recall, at Diirnten that Morlot9 found
the first proofs of a warm or temperate interglacial flora, between
the deposits of a retreating glacier and those of an advancing
glacier ; for Diirnten is well within the region which was covered
by the vast ice-fields both of the third and fourth glaciations.
The forests which nourished there in Third Interglacial times
were similar to those now found in the same region, consisting of
the spruce, fir, mountain-pine, larch, beech, yew, and sycamore,
with undergrowth of hazel. With this hardy flora are associated
the remains of the straight- tusked elephant, of Merck's rhi-
noceros, of wild cattle, and of the stag ; another evidence for our
opinion that all these Asiatic mammals had become habituated
to the cool temperate climate of the north.
Life on the River Somme from Pre-Chellean to
Neolithic Times
The borders of the River Somme at St. Acheul give us a vista
of the whole story of the succession of geologic events; the great
changes of climate, the procession of animal life, the sequence of
human races and cultures. Here Commont10 has found the key
to the history of this entire country and enabled us to parallel
events here with those occurring far away in Taubach, on the
borders of the Thuringian forest, and at Krems in Lower Austria,
as studied by Obermaier. This is because the ' older ' and ' newer '
loess periods, the succession of climates and of mammals, and
the development of human cultures were all not local but con-
tinental events. The purely local events are found in the kinds
of gravels and soils which washed down over the terraces.
120
MEN OF THE OLD STONE AGE
It is very important first to clearly picture in our minds and
understand the geography of the Somme at the time of the arrival
of the Pre-Chellean flint workers. It appears certain that all
three of the old river terraces composed of limestone had been
cut long before and that the river had already reached the bottom
level of the underlying chalk rock.11 The higher terrace, then as
now, was ioo feet above the Somme, the middle terrace about
70 feet, and the lowest terrace extended from a height of about
40 feet down underneath the present river level (see Fig. 59).
r
irn^M
P "^ s
T3
■3 s
S3 UJ
w 0) S3
*•» 42
^ 43
o •£
93
43 O
+-> «-i
§^
u o
4) 3 «
2 *C 42 «j
§*-|§
g o o ex
u
-- M Sit
, . rH ,93
ra q O
9i »: « fi «
oj T3 o n, j)
£ ° SJ
g g »-. •-
2 o. } ^ sabre_tooth ti were
and meadow fauna, in- °
eluding deer, bison, and very numerous as attested by the dis-
wild cattle. covery of the lower jaws of thirty or
more individuals. The short-faced
hysena (H. brevirostris) is also found, and there are several species
of deer and wild cattle.
This remarkably rich collection of mammals is associated
with flints of primitive Chellean or, possibly, of Pre- Chellean
type.12 In Torralba, Spain, the same very ancient animals occur,
and it appears possible that this was the prevailing mammalian
life of Pre-Chellean times.
We may conclude, therefore, that there is considerable evi-
dence, although not as yet quite convincing, that the early Chel-
lean flint workers arrived in western Europe before the disap-
pearance of the Etruscan rhinoceros and the sabre-tooth tiger.
126 MEN OF THE OLD STONE AGE
The Pre-Chellean Stations
(See Figs. 53 and 56.)
The dawn of the Palaeolithic Age is indicated in various river-
drift stations by the appearance of crude flint weapons as well
as tools or implements, in addition to the supposed tools of
Eolithic times. There is an unmistakable effort to fashion the
flint into a definite shape to serve a definite purpose : there can
no longer be any question of human handiwork. Thus there
gradually arise various types of flints, each of which undergoes
its own evolution into a more perfect form. Naturally, the
workers at some stations were more adept and inventive than at
others. Nevertheless, the primitive stages of invention and of
technique were carried from station to station; and thus for
the first time we are enabled to establish the archaeological age
of various stations in western Europe.
Only a few stations have been discovered where the Palaeo-
lithic men were first fashioning their flints into prototypes of the
Chellean and Acheulean forms. With relation to the theory
that these primitive flint workers may have entered Europe by
way of the northern coast of Africa, we observe that these stations
are confined to Spain, southern and northern France, Belgium,
and Great Britain. Neither Pre-Chellean nor Chellean stations
of unquestioned authenticity have been found in Germany or
central Europe, and, so far as present evidence goes, it would
appear that the Pre-Chellean culture did not enter Europe directly
from the east, or even along the northern coast of the Mediter-
ranean, but rather along the northern coast of Africa,* where
Chellean culture is recorded in association with mammalian re-
mains belonging to the middle Pleistocene Epoch.
The southernmost stations of Chellean culture at present
known in Europe are those of Torralba and San Isidro, in central
Spain. Tn the Department of the Gironde is the Chellean station
of Marignac, and it is not unlikely that other stations will be dis-
* Industry similar to the Chellean, but not necessarily of the same age, is distributed
all over eastern Africa from Egypt to the Cape.
PRE-CHELLEAN FLINT INDUSTRY
127
covered in the same region, because the Palaeolithic races strongly
favored the valleys of the Dordogne and Garonne, but thus far
this is the only station known in southern France which represents
this period of the dawn of human culture.
The chief Pre-Chellean and Chellean stations'' were clustered
along the valleys of the Somme and Seine. /Of those rare sites
Fig. 60. Very primitive palaeoliths from Piltdown, Sussex, consisting chiefly of tools and
points of triangular and oval form, fashioned out of flint nodules split in two and flaked
on one side only, with very coarse marginal retouch. After Dawson. Nos. i and 2 are
nearly one-half actual size; No. 3 nearly one-quarter actual size.
presenting a typical Pre-Chellean culture, we may note the neigh-
boring stations of St. Acheul and Montieres, both in the suburbs
of Amiens on the Somme, and the station of Helin, near Spiennes,
in Belgium, explored by Rutot. A very primitive and possibly
Pre-Chellean culture was found on the site of the Champ de Mars,
at Abbeville. This culture also extended westward across the
broad plain which is now the Strait of Dover to the valley of the
Thames, on whose northern bank is the important station of
128
MEN OF THE OLD STONE AGE
Gray's Thurrock, while farther to the south is the recently dis-
covered site of Piltdown, in the valley of the Ouse, Sussex.
The r!int tools (Fig. 60) found in the layer immediately over-
lying the Piltdown skull are excessively primitive and indicate
that the Piltdown flint workers had not attained the stage of
craftsmanship described by Commont as 'Pre-Chellean' at St.
Acheul. "Among the flints/' observes Dawson, "we found sev-
eral undoubted flint implements besides numerous 'eoliths.'
The workmanship of the former is
similar to that of the Chellean or
Pre-Chellean stage; but in the ma-
jority of the Piltdown specimens the
work appears chiefly on one face of
the implements."
In the Helin quarry near Spien-
nes13 occur rude prototypes of the
Palaeolithic coup de poing associated
with numerous flakes which do not
greatly differ from those in the lowest
river-gravels of St. Acheul; there is a
close correspondence in the workman-
ship of the two sites, so that we may regard the Mesvinian of
Rutot* as a culture stage equivalent to the Pre-Chellean. The
river-gravels and sands of Helin which contain the implements
also resemble those of St. Acheul in their order of stratification.
Of special interest is the fact that a primitive flint from this
Helin quarry, known as the ' borer,' is strikingly similar to the
'Eolithic' borer found in the same layer with the Piltdown skull
in Sussex. By such indications as this, when strengthened by
further evidence of the same kind, we may be able eventually to
establish the date both of this Pre-Chellean or Mesvinian culture
and of the Piltdown race.
In considering the Pre-Chellean implements found at St.
Acheul in 1906, we note14 that at this dawning stage of human
* Schmidt, regards the Strepyan implements, which are considered by Rutot and others
to be transitional, between the Mesvinian and the Chellean, as closely similar to the
Pre-Chellean of France and probably of the same age.
Fig. 61. Primitive coups de poing or
'hand-stones' of Pre-Chellean
type, found in the lower gravels
of the middle and high terraces
at St. Acheul. After Commont.
One-quarter actual size.
PRE-CHELLEAN FLINT INDUSTRY
129
invention the flint workers were not deliberately designing the
form of their implements but were dealing rather with the
chance shapes of shattered blocks of flint, seeking with a few well-
directed blows to produce a sharp point or a good cutting edge.
This was the beginning of the art of 'retouch,' which was done
by means of light blows with a second stone instead of the ham-
mer-stone with which the rough flakes were first knocked off.
The retouch served a double purpose: Its first and most im-
portant object was further to sharpen the point or edge of the
Fig. 62. Primitive gratloir, or planing tool (side and edge views), of Pre-
Chellean type, found in the lowest gravels of the terraces at
St. Acheul. After Commont. One-quarter actual size.
tool. This was done by chipping off small flakes from the upper
side, so as to give the flint a saw-like edge. Its second object
was to protect the hand of the user by blunting any sharp edges
or points which might prevent a firm grip of the implement.
Often the smooth, rounded end of the flint nodule, with crust
intact, is carefully preserved for this purpose (Fig. 61). It is
this grasping of the primitive tool by the hand to which the terms
'coup de poing,' 'Faustkeil,' and 'hand-axe' refer. 'Hand-
stone' is, perhaps, the most fitting designation in our language,
but it appears best to retain the original French designation,
coup de poing.
As the shape of the flint is purely due to chance, these Pre-
Chellean implements are interpreted by archaeologists chiefly
according to the manner of retouch they have received. Already
130 MEN OF THE OLD STONE AGE
they are adapted to quite a variety of purposes, both as weapons
of the chase and for trimming and shaping wooden implements
and dressing hides. Thus Obermaier observes that the concave,
serrated edges characteristic of some of these implements may
well have been used for scraping the bark from branches and
smoothing them down into poles; that the rough coups de poing
would be well adapted to dividing flesh and dressing hides; that
the sharp-pointed fragments could be used as borers, and others
that are clumsier and heavier as planes (see Fig. 62).
The inventory of these ancestral Pre-Chellean forms of im-
plements, used in industrial and domestic life, in the chase, and
in war, is as follows :
Grattoir, planing tool. R indudes fi possibly six
Racloir, scraper. _. ^ ,
Percoir, drill, borer. chief tyPeS- The true coup de
Couteau, knife. poing, a combination tool of
Percuteur, hammer-stone. Chellean times, is not yet devel-
Pierre de jet? throwing stone ? , . ,, -p, ~, ,, , , ,
p , . J r oped in the Pre-Chellean, and the
coup de poing, hand-stone. other implements, although sim-
ilar in form, are more primitive.
They are all in an experimental stage of development.
Indications that this primitive industry spread over south-
eastern England as well, and that a succession of Pre-Chellean
into Chellean culture may be demonstrated, occur in connection
with the recent discovery of the very ancient Piltdown race.
The Piltdown Race 15
The 'dawn man' is the most ancient human type in which
the form of the head and size of the brain are known. Its
anatomy, as well as its geologic antiquity, is therefore of pro-
found interest and worthy of very full consideration. We may
first review the authors' narrative of this remarkable discovery
and the history of opinion concerning it.
Piltdown, Sussex, lies between two branches of the Ouse,
about 35 miles south and slightly to the east of Gray's Thurrock,
the Chellean station of the Thames. To the east is the plateau
of Kent, in which many flints of Eolithic type have been found.
THE PILTDOWN RACE
131
The gravel layer in which the Piltdown skull occurred is situ-
ated on a well-defined plateau of large area and lies about 80
feet above the level of the main stream of the Ouse. Remnants
of the flint-bearing gravels and drifts occur upon the plateau and
Fig. 63. Discovery site of the famous Piltdown skull near Piltdown, Sussex. After
Dawson. A shallow pit of dark-brown gravel, at the bottom of which were found the
fragments of the skull and a single primitive implement of worked flint (see Fig. 65).
the slopes down which they trail toward the river and streams.
This region was undoubtedly favorable to the flint workers of
Pre-Chellean and Chellean times. Kennard16 believes that the
gravels are of the same age as those of the 'high terrace' of the
lower valley of the Thames ; the height above the stream level
is practically the same, namely, about 80 feet. Another geologist,
Clement Reid,17 holds that the plateau, composed of Wealden
chalk, through which flowed the stream bearing the Piltdown
gravels, belongs to a period later than that of the maximum de-
132 MEN OF THE OLD STONE AGE
pression of Great Britain ; that the deposits are of Pre- Glacial or
early Pleistocene age ; that they belong to the epoch after the
cold period of the first glaciation had passed but occur at the very
base of the succession of implement-bearing deposits in the south-
east of England.
On the other hand, Dawson,18 the discoverer of the Piltdown
skull, in his first description states : "From these facts it appears
probable that the skull and mandible cannot safely be described
as being of earlier date than the first half of the Pleistocene Epoch.
The individual probably lived during the warm cycle in that age."
The section of the gravel bed (Fig. 64) indicates that the re-
mains of the Piltdown man were washed down with other fossils
by a shallow stream charged with dark-brown gravel and un-
worked flints; some of these fossils were of Pliocene times from
strata of the upper parts of the stream. In this channel were
found the remains of a number of animals of the same age as the
Piltdown man, a few flints resembling eoliths, and one very primi-
tive worked flint of Pre-Chellean type, which may also have been
washed down from deposits of earlier age. These precious geo-
logic and archaeologic records furnish the only means we have of
determining the age of Eoanthropus, the 'dawn man,' one of
the most important and significant discoveries in the whole his-
tory of anthropology. We are indebted to the geologist Charles
Dawson and the palaeontologist Arthur Smith Woodward for
preserving these ancient records and describing them with great
fulness and accuracy as follows (pp. 132 to 139):
Several years ago Dawson discovered a small portion of an
unusually thick human parietal bone, taken from a gravel bed
which was being dug for road-making purposes on a farm close
to Piltdown Common. In the autumn of 191 1 he picked up
among the rain-washed spoil-heaps of the same gravel-pit another
and larger piece of bone belonging to the forehead region of the
same skull and including a portion of the ridge extending over
the left eyebrow. Immediately impressed with the importance
of this discovery, Dawson enlisted the co-operation of Smith
Woodward, and a systematic search was made in these spoil-
THE PILTDOWN RACE
133
heaps and gravels, beginning in the spring of 191 2 ; all the material
was looked over and carefully sifted. It appears that the whole
or greater part of the human skull had been scattered by the
workmen, who had thrown away the pieces unnoticed. Thor-
feJlysfe^
43*
<3>
<&>
d>
: £»•
<3 \
c&.
: : % ':<&j' . * \ ;
t£> ' .
<3Z7
<^>
^ shows a marked retrogression of technique in contrast to the
steady progression which we have observed up to this time. We
have, in fact, witnessed a number of successive stages of progres-
sion, which are to be followed in the Mousterian by a stage of
retrogression. Such a retrogression in industrial development
may for certain known or unknown reasons occur in the same
race. It is a noteworthy parallel that in the Upper Palaeolithic,
where the Solutrean culture represents the climax and perfection
of flint working, the succeeding Magdalenian shows marked
retrogression in the technique of flint retouch.
THE NEANDERTHAL RACE OF KRAPINA 181
The Krapina Neanderthaloids
In northern Croatia, near the small town of Krapina, in the
valley of the Krapinica River, is the now famous cavern of Kra-
pina, where in 1899 was made the fourth discovery of the remains
of men of the Neanderthaloid race in western Europe, twelve
Fig. 90. The grotto of Krapina, overlooking the valley of the Krapinica River, near
Krapina, Croatia, in Austria-Hungary. After Kraemer.
years after the discovery of the men of Spy, in Belgium, and
forty-three years after the discovery of the man of Neanderthal.
Even now opinion is divided as to the age of the human remains
found in this cavern. The discoverer, Professor Gorjanovic-
Kramberger of Agram considered that the stone implements and
chips were of Mousterian age, and Breuil still refers them to the
early, or so-called warm, Mousterian period; this opinion is
shared by Dechelette. Schmidt, however, regards Krapina as a
true Acheulean station, lacking in some of the typical implements,
and of the same age as the 'loess' station of Ehringsdorf.
182
MEN OF THE OLD STONE AGE
The mammals found in the cavern certainly belong to the
very late Acheulean period and include Merck's rhinoceros, the
cave-bear, the urus, a species of horse, the giant deer (Megaceros),
the beaver, and the marmot (Arctomys marmotta).
The cavern was originally washed out by the river, but now
it is 82 feet above the present water-level. When found it was
completely filled with sand and gravel deposits, weathered frag-
ments from the roof and walls, and loose stones and boulders.42
Enclosed in this mass, in separate strata which are perfectly
Fig. 91. Cross-section of the valley traversed by the Krapinica River showing the loca-
tion of the grotto known as the Krapina recess on the bank to
the left. Drawn by C. A. Reeds.
distinguishable, there lay, variously distributed through the
different layers, thousands of animal bones, mingled with hun-
dreds of human bones, and hundreds of stone implements and
chips.
During the years 1 899-1 905 Gorjanovic-Kramberger made a
thorough exploration of the contents of this cavern, and published
a complete account of his researches in 1906.43 There were about
three hundred pieces of human bones, among them many small
fragments, also many sizable pieces of skull and several entire
limb bones perfectly preserved. The bones are of a strongly
characterized type, and the lower jaws, face bones, bones of the
thigh and arm, the teeth, and the bones of many children establish
the Krapina race as belonging unquestionably in the same group
with that of Neanderthal and of Spy.
THE NEANDERTHAL RACE OF KRAPINA
183
The skull of the Krapina man (Fig. 93) is somewhat broader
or more brachycephalic than that of any other members of the
Neanderthal race. In general, the race is somewhat dwarfed, of
broader head form and with less prominent supraorbital processes.
The species is unquestionably Homo neanderthalensis., of which
\9 Uinsus spelaeus
forrjwlw&ofTiy^bed^
1
1
1
1
Fig. 92. Detail showing the interior contents of the Krapina grotto be-
fore its excavation in the years 1899 to 1905. After
Gorjanovic-Kramberger.
the Krapina men constitute a local race. Schwalbe and Boule
observe that the greater breadth of the Krapina skull is partly
due to the manner in which the bones have been put together,44
and they do not consider that the Krapina man represents a
different subrace {Homo neanderthalensis krapinensis) as held by
the discoverer. The cephalic index of one Krapina skull is re-
corded as 83.7 per cent (?) as compared with 73.9 per cent, the
cephalic index of the true H. neanderthalensis, a difference which,
as above noted, may be partly due to the restoration. The bones
are in such a fragmentary condition that it is impossible to form
a proper estimate of the brain capacity in either the males or
females of this race ; nor is it possible to estimate the stature.
The space between the eyes is the same as in the Neanderthal
184 MEN OF THE OLD STONE AGE
race ; the angle of the retreat of the forehead (520) is nearly the
same as in the Gibraltar female Neanderthal skull (500), this
high forehead being due to the lesser development of the supra-
orbital ridges. That the brain was of a low, flat-headed Nean-
derthal type is shown by the close similarity of the index of the
height of skull (42.2) to that of one of the men of Spy (44.3), as
compared with the lowest index among the existing races of men
(48.9); yet the Krapina man presents a considerable advance
Fig. 93. Profile view, right side, of one of the skulls from Krapina. This skull
is much broader than that of the typical Neanderthaloid. After
Gorjanovic-Kramberger. One-quarter life size.
over Pithecanthropus, in which the index of the height of skull is
only 34.2.
The jaw is more slender than that of the Heidelberg man
but is still thick and massive ; the chin is receding, a character-
istic of all the Neanderthal races.
The broken condition of all the human bones in this cavern,
and che abundant indications of fire, have led to the charge that
the Neanderthals of Krapina were cannibals, and that these
mingled remains are the bones of animals and men collected here
during cannibalistic feasts. Against this supposition Breuil ob-
serves that none of the human bones are split lengthwise, as is
the usual practice when extracting the marrow, but they are
broken crosswise. This is the only evidence of such practice that
has been found during all Palaeolithic times, and we should hesi-
tate to accept it unless corroborated by other localities.
The various layers indicate that the cavern was successively
occupied by man ; in or near the hearths are found stone imple-
THE NEANDERTHAL RACE OF KRAPINA
185
ments, broken and incinerated bones, and pieces of charcoal,
which may indicate that this grotto was visited only at intervals,
perhaps during the colder seasons of the year.
(i
(2
(3
(4
(5
(6
(7
(8
(9
(10
(ii
(12
(i3
(14
(IS
(16;
(i7
(i*
(19
(20
(21
(22
Harle, 1910.1.
d'Ault du Mesnil, 1 896.1, pp.
284-296.
Obermaier, 1912.1, p. 146.
Schmidt, 1912.1, pp. 118-126.
Boule, 1888. 1.
Obermaier, 191 2.1, pp. 327-329.
Haug, 1907. 1, vol. II, pp. 327-
329.
Geikie, 1914.1, p. 262.
Morlot, 1854.1.
Commont, 1906. 1.
Geikie, 1914.1, pp. 107-111.
d'Ault du Mesnil, op. tit.
Schmidt, 1912.1, pp. 124, 125.
Obermaier, 1912.1, p. 118.
Dawson, 1913.1; 1913.2; 1913.3.
Kennard, 1913.1.
Reid, 1913.1.
Dawson, 1913.1, p. 123; 1914.1,
pp. 82-86.
Keith, A., 1913.1; 1913-2; IQI3-3-
Smith, G. E., 1913.1; 1913.2;
1913.3; 1913-4-
Boule, 1913.1, pp. 245, 246.
Schwalbe, 1014.1, p. 603.
(23) Osborn, 1910.1, pp. 404-409.
(24) Ewart, 1904. 1 ; 1907. 1; 1909. 1.
(25) Obermaier, 191 2.1, p. 120.
(26) de Mortillet, 1869. 1.
(27) Obermaier, op. cit., p. 116.
(28) Lyell, 1 863. 1, p. 164.
(29) Geikie, 1914.1, pp. 119, 263, 264.
(30) Schmidt, 1912.1, pp. 125, 126.
(31) Geikie, op. tit., p. 228.
(32) Avebury, 1913.1, p. 342, Fig.
236.
(33) Schmidt, op. cit., pp. 17-105.
(34) Breuil, 1912.5, p. 14.
(35) Obermaier, 191 2.1, p. 164.
(36) Obermaier, op. cit., pp. 124, 125,
127, 130.
(37) Commont, 1908. 1.
(38) Dechelette, 1908. 1, vol. I, pp.
80-90.
(39) Geikie, 1914.1, p. 255.
(40) Hnzheimer, 1913.1, p. 145.
(41) Obermaier, 1912.1, p. 127.
(42) Fischer, 1913.1.
(43) Gorjanovic-Kramberger, 1901.1;
1903. 1 ; 1906. 1.
(44) Schwalbe, 1914.1, p. 597.
CHAPTER in
CLOSE OF THE THIRD INTERGLACIAL. TEMPERATE, AND ARID CLI-
MATE, ACHEULEAN INDUSTRY — ADVENT OF THE FOURTH GLA-
CIATION, PROFOUND CHANGES IN ANIMAL AND PLANT LIFE —
THE ARCTIC TUNDRA PERIOD OF MAMMALIAN AND PLANT LIFE
— CHARACTERS OF THE NEANDERTHAL RACE, OF THEIR MOUS-
TERIAN FLINT INDUSTRY — SUPPOSED CAUSES OF EXTINCTION OR
DISPERSAL
We now reach a prolonged and important stage in the pre-
history of Europe, namely, the period of the fourth glaciation,
of the final development of the Neanderthal race of man, of the
Mousterian industry, of the beginnings of cave life, of the chase
of the reindeer, and its use for food and clothing.
In all Europe the Acheulean industry appears to have come to
a close during a period of arid climate, warm in some parts of
western Europe and cool or even cold in others. The seasonal va-
riations may well have been extreme, as on the steppes of south-
ern Russia, where exceedingly hot summers may be followed by
intensely cold winters, with high winds and snow-storms destruc-
tive of life.
It is this seasonal alternation, as well as the recurrence, either
seasonal or secular, of milder climate, which explains the survival
or return of the Asiatic fauna even after the close of the Acheulean
industry and when the Mousterian industry was well advanced.
From deposits found at Grimaldi, in the Grotte des Enfants and
in the Grotte du Prince, it has long been said that men of early
Mousterian times lived contemporary with the hippopotamus,
the straight-tusked elephant, and Merck's rhinoceros in the genial
climate of the Mediterranean Riviera. More recently the same
animals have been found as far north as the Somme valley in the
'river-drifts' of Montieres-les-Amiens.1 Here, again, we find re-
186
CLOSE OF THE THIRD INTERGLACIAL 187
mains of the hippopotamus, the stright-tusked elephant, and its
companion, Merck's rhinoceros, in Mousterian deposits, a surpris-
ing discovery, because it had always been supposed that a cold
climatic period had set in all over western Europe even before
the close of the Acheulean culture. But there is also evidence of
a temperate climate still prevailing in the Thames valley in the
period of the Mousterian ' floors.' 2 Again, along the Vezere
valley, Dordogne, we find that at the station of La Micoque,
where the industry marks the transition between late Acheulean
and early Mousterian times, Merck's rhinoceros is found in the
lowest layers associated with remains of the moose (Alces).
There is evidence that Merck's rhinoceros and the straight-
tusked elephant lingered in western Europe during the whole
period of the early development of the Mousterian industry.
As observed above, these animals were hardier than the southern
mammoth, which was the first of the Asiatic mammals to disap-
pear, soon to be followed by its companion, the hippopotamus.
Even after the advent of the closely associated tundra pair, the
woolly mammoth and the woolly rhinoceros, Merck's rhinoceros
persists, as, for example, in the deposits of Rixdorf, near Berlin,
where this ancient type occurs in the same deposits with the
woolly mammoth, the woolly rhinoceros, the reindeer, and the
musk-ox, as well as with the forest forms, the moose, stag, wolf,
and forest horse. The extreme northern latitude of this deposit
explains the absence of the straight-tusked elephant, which may
at the time have been living farther to the south. The same
mingling of south and north Asiatic mammals is found at Stein-
heim, in the valley of the Murr, some degrees to the west and
south of Rixdorf, not far from Gottingen, where we find Merck's
rhinoceros3 and the straight-tusked elephant in association with
the woolly mammoth, the woolly rhinoceros, the giant deer, and
the reindeer.
Thus the Neanderthal races were entering the Mousterian
stage of culture during the close of the Third Interglacial Stage
and during the early period of the advance of the ice-fields from
the great centres in Scandinavia and the Alps. As these ice-
188 MEN OF THE OLD STONE AGE
fields slowly approached each other from the north and from the
south a very great period of time must have elapsed during which
all the south Asiatic mammals " abandoned western Europe or
became extinct, with the exception of the lions and hyaenas,
which became well fitted to the very severe climate that pre-
vailed over Europe during the fourth glaciation, and even during
the long Postglacial Stage which ensued. The large carnivora
readily become thoroughly adapted to cold climates, as they sub-
sist on animal life wherever it may be found; tigers of the same
stock as those of India have been found as far north as the river
Lena, in latitude 5 2° 25', where the climate is colder than that of
Petrograd or of Stockholm, while the lion throve in the cold
atmosphere of the upper Atlas range. Thus the cave-lion (Felis
leo spelcea) and the cave-hyaena (H. crocuta spelcea) doubtless
evolved an undercoating of fur as well as an overcoating of long
hair, like the tundra mammals. In size the lion of this period in
France often equalled and sometimes surpassed its existing rela-
tives, the African and west Asiatic lion ; it frequently figures in
the art of the Upper Palaeolithic artists and survived in western
Europe to the very close of Upper Palaeolithic times.
The Fourth Glaciation
Penck4 has estimated that the first maximum of the fourth
glaciation in the Alps was reached 40,000 years ago, and that
after the recession period the second maximum ended not less
than 20,000 years ago. This would extend the Mousterian in-
dustry over a very long period of time, for there can be no doubt
that the Mousterian culture was practically contemporaneous
with the fourth glaciation, even if a briefer period of time should
be allotted to this great natural event.
The fourth glaciation, like the first, is believed to have been
contemporaneous in Europe and North America,5 a fact which
is of especial importance to American anthropologists in connec-
tion with the question of the date of arrival of primitive man
in America. In both countries the glaciation reached an early
THE FOURTH GLACIAL STAGE
189
maximum, which was followed by a period of recession of the
ice-fields, a time during which a somewhat more temperate cli-
mate prevailed, but this in turn gave way to a second advance of
as great severity as the first.*
Fig. 94. Europe during the extension of the ice-fields and glaciers of the Fourth Glacial
Stage. This is also supposed to have been a period of land depression and of extension
of the inland seas of southern Europe. Britain was probably connected with France.
The ice-covered areas in western Europe and Britain were far more limited than during
the Third Glacial Stage, yet the climate appears to have been more severe than at any
previous period. For the snow-level compare Fig. 13. Drawn by C. A. Reeds after
Geikie and De Geer.
In the north, Scandinavia and Finland were again enshrouded
in ice, and a great mer de glace occupied the basin of the Baltic
Sea, sending its terminal moraines into Denmark and Schleswig-
*The entire fourth glaciation has been termed Mecklenburgian by Geikie;6 the recession
may correspond with his Fourth Interglacial Stage, the Lower Forestian. It is the
Wiirm of Penck in the Alpine region, with a first and second maximum separated by the re-
cession known as the Laufenschwankung. In America it is the early Wisconsin with the
Peorian recession interval, followed by the late Wisconsin, which is the final great glaci-
ation of America.
190
MEN OF THE OLD STONE AGE
Holstein and over the northern provinces of Germany, but this
great ice-field did not again become confluent with that of Great
Britain.7 At the commencement of the fourth glaciation large
Ftg. 95. The two large tundra mammals, the woolly rhinoceros (upper), drawn from the
work of Upper Palaeolithic artists and from the specimen discovered at Starunia, in
Galicia, Austria; and the woolly mammoth (lower). These hardy animals gradually
replaced the African- Asiatic pair, Merck's rhinoceros and the straight-tusked elephant.
Drawn by Erwin S. Christman. One-sixtieth life size.
glaciers descended over the Scottish mountain valleys and filled
many of them even to the sea; the coast subsided at least 13c
feet in this region. In southern Britain along the valley of the
Thames there spread an arctic flora, with the polar willow (Salix
polaris) and the dwarf birch (Betula glandulosa) ; an arctic plant
ARCTIC TUNDRA LIFE 191
bed has also been discovered in the valley of the Lea. Thus the
tundra climate extended from the Scottish lowlands to the south
of England, the land being bleak and almost treeless.8 This, we
believe, was also the period of the arctic flora at Hoxne, Suffolk,
and of the arctic plant bed in the valley of the Thames. At this
time the valley was frequented by the reindeer, the woolly rhi-
noceros, and the mammoth, whose remains are entombed in the
low-level alluvia swept down from the sides of the valley, so that
the remains of this arctic fauna may in places actually overlie
those of the more deeply buried and far more ancient warm
Asiatic fauna of Chellean times. Like the Somme, the Thames9
was then from 10 to 25 feet below its present level, the bottom
having since silted up with alluvial soil.
This was the period of the deposition of the ( upper drift'
over the north German lowlands, the Alps, and northern England,
also of the early and late Wisconsin, or ' upper drift,' which
spreads very widely over the Eastern States, from Wisconsin
southward and eastward to the latitude of New York. The
gravels and sands of some of the ' lowest terraces' were also
deposited.
Mammalian Life of Mousterian Times
The three successive phases of climate and environment sur-
rounding the Neanderthal men during the period of the develop-
ment of the Mousterian industry, were in descending order as
follows :
3. Extreme Cold Climate of the Last Great Glacial Advance. Period of the
late Mousterian industry of La Quina. Spread of all the arctic and tundra
mammals over western Europe, including the musk-ox; migrations of the
obi and banded lemming of the extreme north. Life and industry of
the Neanderthal races, chiefly in the shelters, grottos, and entrances to the
caverns.
2. Cold Moist Climate. Period of the middle or ' full Mousterian' industry
of the Neanderthal races. Appearance of the tundra life, including well-
protected mammals and birds from the arctic region, also descent of the
Alpine types to the foot-hills and river borders. First forerunners of the
steppe life; the full Eurasiatic forest and field life widely spread over
192 MEN OF THE OLD STONE AGE
Europe. Life and industry chiefly in the shelters, grottos, and entrances
to the caverns. Reindeer very abundant.
i. Warm or Cool Arid Climate. Transition from the Acheulean to the
early Mousterian culture, as observed in the stations of La Micoque and of
Combe-Capelle. The so-called 'warm Mousterian' fauna, including the
surviving hippopotamus, Merck's rhinoceros, and the straight-tusked ele-
phant in northern and southern France; herds of bison, cattle, and wild
horses in southwestern France. Tribal life, with the industry partly in
open stations, partly under sheltering cliffs.
This is the beginning of the ' Reindeer Period/ for this mi-
grant from Scandinavia, with its companions of the northeastern
tundras, the woolly mammoth and the rhinoceros, wandered
slowly southward before the advancing Scandinavian ice-fields,
which were greatly augmented by the increasingly cold and
moist climate. Thus these animals are found in the north with
flints of the Mousterian culture before they appear in the more
genial region of Dordogne. In the somewhat older Acheulean-
Mousterian station .of La Micoque, along the Vezere, the fire-
hearths contain almost exclusively the remains of horses and
relatively few remains of bison and wild cattle, but no reindeer.
A fireplace near the station of Combe-Capelle yields numerous
remains of the bison, only a few of the horse, and the first of the
reindeer. Before the appearance of the reindeer in the valley of
the Vezere we may picture the meadow-lands as covered with
bison and wild horses, the latter of the type which is now charac-
teristic of the high plateaus of central Asia, while the bison of
the period appears to be more similar to the American buffalo
than to the surviving European form.
Gradually the tundra animals spread toward the south with
the cold climate which for the first time swept all over western
Europe. The whole aspect of the country slowly changed with
the approach of the reindeer, and the northern flora of the spruce,
the fir, and the arctic willow clad the more sheltered river- valleys
and hillsides, while the plateaus and fields were partly or wholly
deforested.
Thus the country became adapted chiefly to the tundra types
of mammals; and in the middle Mousterian strata these herds,
Fig. 96. Typical tundra fauna. "Gradually the tundra animals pressed toward the
south with the cold climate which for the first time swept all over western Europe."
The wolverene, Gulo luscus borealis ; the barren-ground reindeer, Rangifer tarandus
(drawn from the living type); the arctic fox, Canis la go pus ; the musk-ox, Ovibos mos-
chatus ; and the banded lemming, Myodes torquatus. One-twenty-fifth life size. The
lemming (A) is also shown one-seventh life size. Drawn by Erwin S. Christman.
194 MEN OF THE OLD STONE AGE
newly migrated from the far north and from the northeastern
steppes bordering the Obi River, largely outnumber the steppe
forms, which are limited to two or three species. Of these the
principal types are the steppe horse, related to the Przewalski
horse now living in the desert of Gobi, the steppe suslik (Spermo-
philus rufescens), and the steppe grouse, or moor-hen. The more
characteristic forms of steppe life, such as the saiga antelope, the
jerboa, and the kiang, were all later arrivals and did not appear
until after the close of the Mousterian industry and the disap-
pearance of the Neanderthal race.
This was due to the fact that the climate surrounding the
Neanderthal race in Mousterian times was cold and moist, with
heavy rainfalls in summer and snow-storms in winter, a climate
thoroughly suited to the arctic tundra mammals with their heavy
covering of hair acting as a rain shed and the undercoating of
wool protecting them in the most severe weather.
The mammal lif e during the fourth glaciation, as it spread into
the middle Rhine and Westphalian region, is fully recorded in the
' loess' deposits of Achenheim and in the famous grotto of Sir-
genstein, on the upper Danube, lying northwest of Munich,
where, together with traces of the most primitive Mousterian in-
dustry, are found remains of the mammoth, the bison, the rein-
deer, a species of wild horse, and the cave-bear. Following these
mammals there is a record in the same deposit of the arrival of
the Obi lemming, from northern Russia.
The fact that only seven Mousterian stations are known in
all Germany, or eight if we include the site of the Neanderthal
burial, may be accounted for by the relatively close proximity of
the great Scandinavian glacier on the north, which was only 350
miles distant from the great Alpine glacier on the south. To
the east were the plains of Bohemia and the vast lowland region
stretching northeastward to the tundras and eastward to the
steppes, through which came the great migrations of tundra and
steppe life.
S3
SI
SO
48
ML
11
C1. \
l\
*2
«ik
HANOVER
O
V***,
r
DUSSELDORF
-_-BT____,
*k •Thiedi
¥
1 v "
Tartinshbnle*
..-4-
* Neanderthal *Valverhdhle.
Bdirmanns/iohlem
cologne/
I
\JfyrtsteiH%
\n, ?ndeTl
^5
7F
IT
IB
• PALAEOLITHIC STATIONS
O CITIES OF MODERN GERMANY
Fig. 97. The seven Mousterian stations of Germany lay between the Scandinavian glacier
(IV) on the north and the Alpine glacier (IV) on the south (dotted areas) . They include
the grottos of Sirgenslein, Irpfelhohle, and Rauberhohle, along the valley of the Danube ;
Kartstein and Buchenloch, near the middle Rhine, and Banmannshohle, south of Han-
over; also the open loess station of Mommenheim. The Mousterian grotto of Wild-
kirchli, in Switzerland, lay within the limits of the Alpine ice-fields; and the burial at
Neanderthal, near Dusseldorf, was probably of Mousterian age. After R. R. Schmidt,
modified and redrawn.
190 MEN OF THE OLD STONE AGE
Geographic and Climatic Environment of the Neander-
thal Race
Let us first glance at Dordogne. Among the stations of the
early Mousterian industry we have seen that the Neanderthals
in the valley of the Vezere, at La Micoque, were in the midst of
a fauna chiefly composed of the bison and of the wild horse, the
remains found in the hearths being almost exclusively of the latter
animal.* In the primitive Mousterian station of Combe-
Capelle near by the fire-hearths yield remains of the bison but
only a few of the horse.
Among the earliest caves inhabited by man10 was that of Le
Moustier, situated on the right bank of the Vezere, and about 90
feet above it. This shelter and cave were examined as early as
1860-3 by Lartet11 and Christy and subsequently by de Vibraye,12
Massenat,13 and others. Besides the deposits in the floor of the
grotto there, a deep Mousterian culture layer has been found
under the cliff in front, and this has been selected for our repre-
sentation of the life of the men of Mousterian times, and of the
flora of the Vezere in this early period (see frontispiece) . Peyrony
observes that, here as elsewhere, the older and lower industrial
camps were farther away from the shelters; indeed, in this very
region there are evidences that the Chellean and Acheulean flint
workers occasionally visited the plateaus above ; but as time
passed and the weather became more severe the Neanderthals
began to work nearer to the overhanging cliffs, and finally directly
beneath them. At this classic station of Le Moustier, one of the
most complete skeletons of Neanderthal man was unearthed by
Hauser, in 1908. There was a continuous residence here in mid-
dle and upper Mousterian times, extending into the lower Aurig-
nacian of the Upper Pakeolithic. The contemporary fauna in
these deposits included the mammoth, the reindeer, the giant deer
(Megaceros)j the horse, the bison, the woolly rhinoceros, and the
* Obermaier, Breuil, and Schmidt assign La Micoque to the transition between late
Acheulean and early Mousterian times.
ENVIRONMENT OF THE NEANDERTHAL RACE 197
cave-bear. During the habitation of this typical station by man
the climate was very cold and damp.
In this region is found the complete record of the course of
Mousterian evolution, both in the implements and in the advent
of new forms of life; the number of reindeer gradually increases
in the ascending layers with the development of the Mousterian
industry. There is a constant gradation from the Acheulean into
the Mousterian industrial types; according to Cartailhac, this
Fig. 98. The type station of Le Moustier, on the right bank of the Vezere, Dordogne.
The culture layer is on the middle terrace, overlooking the hamlet of Le Moustier.
(Compare frontispiece, PL i.) Photograph by Belves.
industry is all the work of the same people, with no sharp lines
of division.
Thus at Combe-Capelle, where the debut of the true Mous-
terian culture took place, we find a number of large coups de
poing, pointing back to the early Acheulean implements. The
gradations which are exhibited here in these successive layers are
quite in contrast to the advance of the industry at the close of
Mousterian times in the very same locality, where there is an
abrupt cultural transition toward the Aurignacian.
Southern Britain tells of a similar sequence, which we may
interpret as follows. Belonging either to the temperate climate
198
MEN OF THE OLD STONE AGE
of early Mousterian times, or to the period of the recession of the
fourth glaciation, known in the Alps as the Lanfenschwankung,
are the Mousterian stations along the Lea and near the mouth
of the Thames at Crayford (Worthington Smith/4 Geikie15).
These Palaeolithic ' floors' of Mousterian times are buried be-
FlG. 99. Excavations of the Mousterian culture layer under the cliff of Le Moustier.
Photograph by N. C. Nelson.
neath 4 to 5 feet of sand and loam and rest upon the surface of
older river-gravels. Among the later river deposits several old
land surfaces have been discovered ; they consist of a few inches
of angular gravel, crowded in places with unabraded implements
and flakes which obviously occur just where they were left by
Palaeolithic workmen. At one point there is evidence that the
flint maker squatted over his work, with his knees slightly apart,
for the chips are thrown to the right and left in small piles.
Here and there, mixed with these Mousterian implements, are
more archaic forms which may have been drifted down from the
older land surfaces above.
ENVIRONMENT OF THE NEANDERTHAL RACE 199
One such floor has been traced by Worthington Smith16
through Middlesex and on both sides of the Thames. Plant
remains occur plentifully on this old land surface, including im-
pressions of portions of leaves, stems of grass, rushes, and
sedges. The birch, alder, pine, yew, elm, and hazel have been
recognized. The common male fern is of frequent occurrence,
while the royal fern (Osmunda regalis) is found in profusion.
Upon the whole, this assemblage of plants indicates a temperate
climate. The flints described and figured by Worthington Smith
are either of the late Acheulean 'Levallois flake' type or else of
early Mousterian age. This writer17 notes the great number of
instruments known as trimmed flakes, which are found on the
Palaeolithic ' floor' ; these are flakes of large size, trimmed to an
implement-like form on one side, while the other side is left per-
fectly plain ; the examples are remarkably constant to one form.
The type of implement here described resembles the flakes of
Levallois or Combe- Capelle, or even the typical ' point' from
Le Moustier. Such flakes, shaped into the Mousterian forms of
racloir, or scraper, are very common in the gravels of the Lea
and of the Thames.
While the remains of the woolly mammoth are found here,
there are also indications of the presence of a well-marked tem-
perate flora. These high-level ' river-drifts ' along the Thames18
were certainly deposited when the climatic conditions were tem-
perate, but they are succeeded by deposits indicating a renewed
cold period, which may represent the cold 'full Mousterian'
times of the Lower Palaeolithic habitation of the Thames. Here
we find the remarkable sheets of contorted 'drift' attributable
to the movements of the frozen soil and subsoil when exposed to
the heat of the summer sun. At the same time there may have
been deposited along the Thames the alluvial loams and gravels,
occasionally containing stones and rocks, which were brought down
by ice-rafts ; these low-level gravels are not to be confused with
the underlying 'old river-gravels' which contain the warm tem-
perate hippopotamus fauna, for they were accumulated under very
cold conditions ; they yield remains of the woolly rhinoceros and
200
MEN OF THE OLD STONE AGE
of the mammoth. Thus, on the high levels of the Thames as
well as on the low levels we find evidences of the human culture
and of the extinct fauna of the period of the fourth great gla-
ciation.
The upper waters of the Rhine and Danube were also fre-
quented by late Acheulean and early Mousterian flint workers.
At a point far distant from southern England there is the cavern
of Wildkirchli on the Santis Mountains, near Appenzell, in Swit-
zerland ; in Mousterian times this was in the very heart of the
»***> ■■ ' —
Jf* •* ''^'fJ^Mu
j00*f*m
/ im^'^l
raK*^l
jtu y \a > **BWMi
^><
it^lfll
• ^' '">.«' . '
- -/
'*
*** " , \
■ :
ft'
?
+
tt
Ft
?
+
••
tt
->
+
?
p
+
+
tt
+
tt
p
+
P
tt
?
+
B.— INDUSTRIAL AND DOMESTIC
9. Lampe Lamp
io. llssotr poltsher
11. Mortier Mortar
12. Hachette
(Tranchette) Chopper
*i3. Coup de Poing Hand- Axe, etc. . .
14. Grattoir Planing Tool
15. Racloir Scraper
16. Percoir Drill, Borer....
*i7. Couteau Knife
18. Enclume Anvil Stone
19. Percuteur Hammer-Stone . . .
C— ART, SCULPTURE, ENGRAVING
*30. mlcrolithique drill, graver,
and Etcher
21. Ciseau Chisel
22. Gravette Etching Tool
23. Burin Graver
(also Mortar, Hammer-Stone, and
Polisher)
* = twice mentioned (in different classifications).
+ or \X denotes an unusual or culminating development.
Again, the burial customs of the Neanderthals were in many
respects followed by the Cro-Magnons ; they chose, in fact, the
same kind of burial sites, namely, at the entrances of grottos
ARRIVAL OF THE CRO-MAGNONS
271
or in proximity to trie shelters. Some degree of ceremony must
have marked these burials, for with the remains were interred
implements of industry and warfare together with offerings of
food. Most of the Neanderthal burials were with the body ex-
tended ; the two burials of the Grimaldi race were with the
THE BONE IMPLEMENTS APPEARING AT THE CLOSE OF THE LOWER
PALEOLITHIC AND HIGHLY CHARACTERISTIC OF
THE UPPER PALEOLITHIC
The Typical Bone Implements
A.— WAR, CHASE, FISHING
*i. Lames Blades
2. Poignard Dagger
3. Hamecon? Fish-Hook?
4. Propulsetir Spear Thrower
5. Harpon Harpoon
6. pointe de sagaie javelin point..
7. Pointe de Lance Spear Point. . .
B.— INDUSTRIAL AND DOMESTIC
8. Spatule
9. Navette
10. Epingle
11. Aiguille
*i2. Lames
13. COMPRESSEUR
14. LlSSOIR
15. Coin
16. Ciseau
17. POINCON
Spatula. .
Shuttle . .
Pin
Needle . . .
Blades...
Anvil
Smoother.
Wedge
Chisel
Awl
C— CEREMONIAL, SOCIAL
18. BAton de Com-
mandement ceremonial staee
19. Baguette Wand
Lower Paleolithic
Upper Paleolithic
+
tt
* = twice mentioned (in different classifications).
+ or If denotes an unusual or culminating development.
limbs in a flexed position and tightly bound to the body, prob-
ably with skin garments or thongs. The Cro-Magnon burials
are either with the body extended, as in the Grottes de Gri-
maldi, or with the limbs flexed, as in the Aurignacian burial of
Laugerie Haute.
272 MEN OF THE OLD STONE AGE
Whether the Neanderthals were exterminated entirely or
whether they were driven out of the country is not known ; the
encounter was certainly between a very superior people, both
physically and mentally, who possibly had the use of the bow
and arrow, and a very inferior and somewhat degenerate people
that had been already reduced physically and perhaps numer-
ically by the severe climatic conditions of the fourth glaciation.
The Neanderthals were dispossessed of all their dwelling-places
and industrial stations by this new and vigorous race, for at no
less than eighteen points the Aurignacian immediately succeeds
upon the Mousterian industry and in a few instances Cro-
Magnon burials occur very near the Neanderthal burial sites.
In the racial replacements of savage as well as of historic
peoples the men are often killed and the women spared and
taken into families of the warriors, but no evidence has thus
far been found that even the Neanderthal women were spared
or allowed to remain in the country, because in none of the
burials of Aurignacian times is there any evidence of the cross-
ing or admixture of the Cro-Magnons and the Neanderthals.
The chief source of the change which swept over western
Europe lay in the brain power of the Cro-Magnons, as seen not
only in the large size of the brain as a whole but principally in
the almost modern forehead and forebrain. It was a race which
had evolved in Asia and which was in no way connected by any
ancestral links with the Neanderthals ; a race with a brain
capable of ideas, of reasoning, of imagination, and more highly
endowed with artistic sense and ability than any uncivilized
race which has ever been discovered. No trace of artistic in-
stinct whatever has been found among the Neanderthals ; we
have seen developing among them only a sense of symmetry
and proportion in the fashioning of their implements. After
prolonged study of the works of the Cro-Magnons one cannot
avoid the conclusions that their capacity was nearly if not quite
as high as our own ; that they were capable of advanced educa-
tion ; that they had a strongly developed aesthetic as well as a
religious sense; that their society was quite highly differentiated
Pl. VI. The head of the Cro-Magnon type of Homo sapiens, a race inhabiting
southwestern Europe from Aurignacian to Magdalenian times. Antiquity in
western Europe estimated as at least 25,000 years. After the restoration modelled
by J. H. McGregor. For the bodily proportions of this finely developed race
compare PI. VII.
UPPER PALAEOLITHIC CULTURES 275
along the lines of talent for work of different kinds. One de-
rives this impression especially from the conditions surrounding
the development of their art, which are still mysterious and an
interpretation of which we shall attempt to give in the follow-
ing chapter.
Cultural, Racial, and Climatic Divisions
The Upper Palaeolithic covers the greater part of the ' Rein-
deer Epoch' as it was conceived by Lartet and Christy, who
began their systematic study and exploration of the caves of
Dordogne in 1863. They were soon joined by Massenat and the
Marquis de Vibraye, while Dupont took up the work in Belgium
and Piette made the artistic development, especially in the
Pyrenees, his chosen field.
Lartet was the first to perceive that the culture of the grotto
of Aurignac was quite distinct from that of the Lower Palaeo-
lithic in northern France; he also recognized in the shelter of
Laugerie Haute, in Dordogne, that there was still another cul-
ture, which is now known as the Solutrean; also that in the
shelter of Laugerie Basse, in Dordogne, there was yet another
industry, that which we now know as Magdalenian. M. de
Mortillet was the first to recognize the superiority of the Solu-
trean industry in stone, which in this period reached its height,
and its succession by the Magdalenian period, in which the in-
dustry in bone and horn reached a climax; but he failed to
recognize the very important preceding position of the Aurig-
nacian, and it was not until 1906 that the clear presentation by
Breuil of the entire distinctness of the Aurignacian industry led
to the adoption by the Archaeological Congress at Geneva of
three cultural divisions of the Upper Palaeolithic. In the mean-
time Piette had discovered that in the Mas d'Azil there was a
distinct cultural phase, the Azilian, following the Magdalenian,
and thus a fourfold division of the Upper Palaeolithic (Breuil,7
Obermaier8) was established, as follows :
AZILIAN. — Industry of the surviving Cro-Magnon and other resident
races, and of newly arrived brachycephalic and dolichocephalic races in
276 MEN OF THE OLD STONE AGE
western Europe; decadent forms of flint and bone workmanship; entire
absence of art. Daun stage of Postglacial retreat; Europe with a milder
climate and forest and meadow fauna like that of early historic times.
MAGDALEN I AN. —Closing stage of the industry and art of the Cro-
Magnon race; bone implements highly developed; marked decline in the
flint industry. Close of Postglacial Period; climate alternately cold and
moist (corresponding with the Biihl and Gschnitz Postglacial advances of
the ice in the Alpine region), or cold and arid; Europe covered with the
tundra and steppe fauna; life chiefly in the shelters and grottos.
SOLUTREAN. — Culminating stage of flint industry; apparent in-
vasion in eastern Europe of the Briinn (Briix, Predmost, and [?] Galley Hill)
race. The highly developed flint industry of the Solutrean types; art
development of the Cro-Magnon race partly suspended. Dry, cold climate;
life largely in the open.
AURIGNACIAN. — Appearance of the Cro-Magnon race in south-
western Europe, succeeding the Mousterian industry; art of engraving
and drawing and sculpture of human and animal forms developing. Animal
life the same as during the fourth glaciation; climate cold and increasingly
dry; life chiefly in the grottos and shelters.
The successive phases of development of Upper Palaeolithic
industry and art have been traced with extraordinary precision
in Dordogne, in the Pyrenees, in northern Spain, and along the
Danube and upper Rhine by a host of able workers — Cartailhac,
Capitan, Peyrony, Bouyssonnie, Lalanne, and others. Breuil
has made himself master especially of the Aurignacian and has
succeeded Piette as the great historian of Upper Palaeolithic art.
Obermaier's chief service has been the comparison of the Upper
Palaeolithic of the Danubian region with that of Dordogne and
northern Spain both in regard to the geologic age and the archae-
ologic and racial succession. The labors of Schmidt along the
upper Rhine and Danube have not only brought this region into
definite prehistoric relation with the Dordogne and the Pyrenees
but have given us by far the clearest evidence of the relation
between the human and the industrial development and the suc-
cession of climatic phases in northern Europe. Finally, the ex-
plorations of Commont along the River Somme have proved that
this region, too, was frequented throughout all Upper Palaeolithic
times, during which it exhibits an industrial development hardly
less important than that of the Lower Palaeolithic.
UPPER PALEOLITHIC CULTURES 277
There are two very distinct lines of thought among these
archaeologists : the first is shown in the tendency to regard the
industries as mainly autochthonous, or as following local lines of
development; the exponents of this theory dwell most strongly
on the transitions between the Mousterian, the Aurignacian,
and the Solutrean industries. For example, the chief object of
Schuchhardt's tour9 through the Palaeolithic stations of Dor-
dogne was to observe the transitions from one period to another
and the evidence afforded of successive changes of climate.
This writer is impressed with the transitions ; he notes that the
typical curved knives of the Abri Audit furnish a transition
from the Mousterian scrapers to the Aurignacian ' points' of
La Gravette and La Font Robert; that the Solutrean takes
up all the hne threads of the Aurignacian culture and spins
them further into Magdalenian times. Thus we get an Aurig-
nacian-Solutrean-Magdalenian industrial cycle which is compar-
able to the Chellean-Acheulean-Mousterian cycle.
Breuil, on the other hand, from the archaeologist's stand-
point— because he is not especially interested in the matter of
racial development — is a strong exponent of the idea of suc-
cessive invasions of cultures, either from the south or Mediter-
ranean region or from the central region of Europe, which he calls
the ' Atlantic ' ; and he distinguishes sharply between these
two great areas of Upper Palaeolithic evolution, namely, the
southern and the central European, pointing out that it was only
after the establishment of more genial climatic conditions, like
those of modern times, that there was an added element of
northern or Baltic invasion. Certainly the archaeologic testi-
mony strongly supports this culture-invasion hypothesis and it
appears to be strengthened in a measure by the study of the
human types, although this study has not progressed beyond
the stage of hypothesis. When the Upper Palaeolithic races
have been studied with as close attention as those of the Lower
Palaeolithic we may be able to establish positively the relation
between these human types and the advance of certain cultures
and industries.
278 MEN OF THE OLD STONE AGE
Distribution of Upper Palaeolithic Human Fossils
Our present view, as drawn from a consideration of the facts
before us, is that western Europe in Upper Palaeolithic times was
entered by four or five distinct races, all belonging to Homo
sapiens, only three of which became established :
5. The Furfooz (Of net, and [?] Grenelle) race, extremely broad-headed,
entering central Europe possibly from central Asia, bringing an Azilian
culture, without art or developed flint industry. (Alpine type.)
4. A dolichocephalic race with a narrow face, associated with the Fur-
fooz race, either connected with the Brunn and Briix, or an advance wave
of one of the dolichocephalic Neolithic races. (Mediterranean type.)
3. The Brunn (Briix, Pfedmost, and [?] Galley Hill) race, long-headed,
with a narrow, short face, probably entering central Europe directly from
Asia through Hungary and along the Danube; bringing a perfected Solu-
trean culture; inferior in brain development to the Cro-Magnons, in in-
dustrial contact with them but not displacing them.
2. The Cro-Magnon race, long-headed with a very broad face, entering
Europe in closing Mousterian or early Aurignacian times, probably from
the south along the Mediterranean coast, and bringing in an Aurignacian
flint industry and art spirit characteristic especially of Aurignacian and
Magdalenian times ; greatly reduced in number in closing Magdalenian
times, but leaving descendants in various colonies in western Europe.
1. The Grimaldi race, in the transition between the Mousterian and the
Aurignacian; negroid or African in character; apparently never established
as a race of any influence in western Europe.
The presence of these five races, and perhaps of a sixth if
the 'Aurignacian man' of Klaatsch proves to be distinct from
the Cro-Magnon, is firmly established by anatomy. It is most
important constantly to keep before our minds certain great prin-
ciples of racial evolution : (1) that the development of a racial
type, whether long-headed or broad-headed, narrow-faced or
broad-faced, of tall or of short stature, must necessarily be very
slow; (2) that this development of the races which invaded west-
ern Europe took place for the most part to the eastward in the
vast continent of Asia and eastern Europe ; (3) that, once estab-
lished through a long process of isolation and separate evolution,
these racial types are extremely stable and persistent ; their head
UPPER PALAEOLITHIC RACES
279
form, their bodily characters, and especially their psychic char-
acters and tendencies are not readily modified or altered ; nor are
they in any marked degree blended by crossing. Crosses do not
produce merely blends; they chiefly produce a mosaic of distinct
characters derived from one race or the other.
Fig. 135. Geographic distribution of Upper Palaeolithic human fossils in western Europe.
We must therefore imagine western Europe in Upper Palae-
olithic times again as a terminal region ; a great peninsula toward
which the human migrants from the east and from the south
came to mingle and superpose their cultures. These races took
the great migration routes which had been followed by other
waves of animal life before them ; they were pressed upon from
behind by the increasing populations of the east ; they were at-
tracted to western Europe as a fresh and wonderful game coun-
try, where food in the forests, in the meadows, and in the streams
abounded in unparalleled profusion. The Cro-Magnons espe-
280
MEN OF THE OLD STONE AGE
daily were a nomadic hunting people, perfectly fitted by their
physical structure for the chase and developing an extraordinary
appreciation of the beauty and majesty of the varied forms of
animal life which existed in no other part of the w^orld at the
time. Between the retreating Alpine and Scandinavian glaciers
Europe was freely open toward the eastern plains of the Danube,
1 POST GLACIAL W>fy&*
4 "Ne wer L oess " ^gschnitz
' JK GLACIAL
WORM, WISCONSIN 1&W>
17
PREHISTORIC
NEOLITHIC
8 AZIUAN-TMDENOISIAN\ UPPFR
6S0LUTREAN \ PALAEO'
i5_AURIGNACIAN_ LUTMJ_C_
25,000 YEARS
4M0USTERIAN
50p00 YEARS
3ACHEULEAN
75,000 YEARS
2CHELLEAN
100,000 YEARS
I PRE-CHELLEAN
I25P00 YEARS
6\/50X)00 „
LOWER
^PALAEO-
LITHIC
.JG_QEN_ELLE_
CRO-MAGNON
CRIMALDI
NEANDERTHAL
(KRAP/NA)
P/LTDOWN
Fig, 136. Epitome of human history in western Europe during the Third Interglacial,
Fourth Glacial, and Postglacial Stages; showing also the three Postglacial advances
and retreats which succeeded the close of the Fourth Glacial Stage in the Alpine
region, theoretically corresponding with the climatic vicissitudes of Postglacial time.
From the data of Penck and Schmidt. Drawn by C. A. Reeds. (Compare Fig. 14.)
extending to central and southern Asia ; on the north, however,
along the Baltic, the climate was still too inclement for a wave
of human migration, and there is no trace of man along these
northern shores until the close of the Upper Palaeolithic, nor of
any residence of man in the Scandinavian peninsula until the
great wave of Neolithic migration established itself in that
region.
The climatic and cultural relations of Upper Palaeolithic times
may be correlated* in descending order as follows :
* This correlation agrees in the main with that of Schmidt in his Diluviale Vorzclt
Deutschlands.10
GEOGRAPHY AND CLIMATE 281
6. The Daun or final Postglacial advance of the glaciers of the Alps,
estimated at 7,000 B. C. Europe with its modern or prehistoric forest
fauna, the lion lingering in the Pyrenees, the moose in Spain. Azilian-
Tardenoisian, closing stage of the Upper Palaeolithic culture; western
j^urope peopled by the broad-headed race of Furfooz and Ofnet, also by a
narrow-headed race. Baltic Migration, Maglemose culture.
5. The Gschnitz stage in the Alps or second Postglacial advance. Cli-
mate still cold and moist but gradually moderating. Decline of the Mag-
dalenian. Period of the retreat of the tundra and steppe animals; mam-
moth, reindeer, and arctic rodents becoming more rare; Eurasia tic forest
mammals becoming more abundant.
Close of steppe period. Cro-Magnon race still dominant in western
Europe in the Late Magdalenian stage of culture.
4. Interval between the Buhl and Gschnitz Postglacial advances in the
Alps. A renewed steppe and 'loess' period. Climate cold and dry.
Mammoth and woolly rhinoceros, reindeer, full tundra and steppe fauna
very abundant. Cro-Magnon race in the stage of Middle Magdalenian
culture.
3. The Buhl stage of Postglacial advance in the Alps ; renewal of severe
conditions of cold moist climate, and spread all over western Europe of
the arctic banded and Obi lemmings of the Upper Rodent Layer. Biihl
moraines in Lake Lucerne estimated as having' been deposited between
16,000 and 24,000 years B. C. Cro-Magnon race dominant in the Early
Magdalenian stage of culture. \ X , ^^° -\^> ,^rv
2. Period of the first Postglacial interval or Achen retreat of the glaciers
in the Alpine region. A dry cold climate. Cro-Magnon and Briinn races
in the stage of Solutrean culture.
1. Close of fourth glaciation, between 24,000 and 40,000 years B. C.
Cold and moist but increasingly dry climate succeeding the fourth glacia-
tion and deposition of Lower Rodent Layer, or first invasion of the arctic
tundra rodents. Cro-Magnon and possibly Aurignacian race in the stage
of Aurignacian culture.
BEGINNING OF THE UPPER PALEOLITHIC
The Aurignacian Industry
We now glance at western Europe as it was between 25,000
and 30,000 years ago, at the opening of the Upper Palaeolithic.
During Aurignacian times France was still broadly con-
nected with Great Britain.11 The British Islands were not
282 MEN OF THE OLD STONE AGE
only united with each other but with the continent, while the
elevation of the Scandinavian peninsula converted the Baltic
Sea into a great fresh-water lake, the old shores of which are
readily traced. Geikie also maintains that the rise of land in
Scotland after the fourth glaciation was accompanied by an
amelioration of climate and the advent of more genial conditions ;
a strong forest growth covered the lowlands, hence this is termed
the Lower Forestian stage of the physiographic history of north-
ern Britain; it corresponds to the temporary period of the
retreat of the glaciers in the Alpine region, which Penck has
named the Achenschwankung. The latter author is not inclined
to connect any marked rise of temperature in the Alpine region
with this interval of time ; to our knowledge no fossil plant
beds have been preserved which would give us such indications,
and the animal life, as we shall see, certainly affords only a
very slight indication of a rise in temperature in the retreat
of certain of the snow-loving tundra and northern steppe lem-
mings to the north; the greater number of tundra forms re-
mained. The continental elevation of the northern coast-line
of Europe would explain the advent of a dry continental cli-
mate and the renewal of high prevailing winds, at least during
the warmer and drier summer seasons, for it is certain that at-
mospheric conditions such as produced the great dust-storms
and deposition of ' loess' after the second and third glaciations
prevailed again in western Europe after the fourth glaciation.
This gave rise to deposits of what is known among geologists
as the 'newer loess,' and we find these sheets of 'newer loess'
spreading immediately above the Mousterian culture at a num-
ber of different points in western Europe.
When the Cro-Magnon race entered this part of Europe the
climate was becoming more dry and stimulating; the summers
were warm or temperate, the winters very severe. Great ice-
caps still spread over the Scandinavian peninsula and also over
the Alps, but the borders of the ice-fields no longer reached the
plains; in a sense, the Glacial Epoch had not yet closed, for
during the whole period of Postglacial time the glaciers of the
GEOGRAPHY AND CLIMATE
283
Alps, beginning in early Magdalenian times, developed three re-
newed advances, each somewhat less vigorous than the preced-
ing one, with intervening stages of a drier climate.
The greater number of the Aurignacian stations, like those
of Mousterian times, were under the shelters or within the
•w
Jr**i*^* Hi *****
in V
lit
^•"•*Z*ir.
Fig. 137. ' Tectif orms ' — schematic drawings in lines and dots believed to represent
huts and larger shelters built of logs and covered with hides. From the
walls of the cavern of Font-de-Gaume, Dordogne. After Breuil.
entrances of the grottos and caverns ; all the stations in south-
western France are of this character. There was, however, a
great open camp at Solutre, which was a most famous hunting
station for the wild horse in Aurignacian times. In northern
France there are several open stations, such as those of Mon-
tieres and St. Acheul, along the River Somme, and to the east,
284 MEN OF THE OLD STONE AGE
along the middle Rhine, there are several open * loess ' stations,
such as those of Achenheim, Volklinshofen, Rhens, and Metter-
nich. It may very well be that these open stations were visited
only during the mild summer season. The continued choice of
sites which naturally afforded the greatest protection from the
weather, in France, Britain, Belgium, and all along the Dan-
ube, as well as in the genial region of the Riviera, is a sure in-
dication of a prevailing severe climate. It is hardly possible,
however, that the closed or protected stations were the only
residences of these people; they merely indicate the points
where the flint industry was continuously carried on and also
the vast foyers and gathering places; but there is little doubt
from the evidence afforded by the signs on the walls of the cav-
erns, known as 'tectiforms,' that huts and large shelters built of
logs and covered with hides were grouped around most of these
stations and scattered through the country at points favorable
for hunting and fishing. These would be the only dwelling-
places possible in such vast open camps, for example, as Solutre.
Climate and Life of Aurignacian Times
3. First Postglacial Retreat, Achenschwankung in the Alpine region.
Period of Solutrean industry. A cold dry climate, with dust-storms and
wide-spread deposition of 'loess' in western Europe. Flint workers seeking
many open stations. Horses and wild asses numerous on the prairies; rein-
deer and wild cattle very abundant.
2. Recession of the Ice-Fields of the Fourth Glaciation. Period of Aurig-
nacian industry. Climate cold and increasingly dry ; renewal of the dust-
storms and deposits of the 'newer loess.' Flint industry in the caverns,
grottos, shelters, and a few open stations. Opening of the Upper Palae-
olithic period. Arrival of the Cro-Magnon race.
1. Final Stage of Fourth Glaciation. Close of the Lower Palaeolithic
Mousterian culture. Gradual extinction of the Neanderthal race.
The arrival of the Cro-Magnon race and the beginning of the
Aurignacian industry took place during the period of retreat of
the ice-fields of the fourth glaciation. As we pass from the
levels of the early Aurignacian industry into those of the middle
and upper Aurignacian, we find that the mammal life of Mous-
MAMMALIAN LIFE
285
terian times continued in its prime all over western Europe, with
the addition, one by one, of some new forms from the tundras,
such as the musk-ox, and the successive arrival from the moun-
tains and steppes of western Asia of such characteristic forms as
the argali sheep and the wild ass, or kiang.
Mam-moth'
Woolly rhinoce
Fourth
Glaciation,
Fig. 138. Geographic distribution (horizontal lines) of the reindeer, mammoth, and
woolly rhinoceros, the three chief mammals of the tundra fauna, with reference to
the retiring ice-fields (dots) of the Fourth Glacial Stage. After Boule and Geikie.
(Compare Figs. 95 and 96.)
The extremely cold and moist climate of the fourth glacia-
tion had passed, and a somewhat drier but still extremely cold
climatic condition prevailed throughout western Europe. Dur-
ing the early Aurignacian the two northern types of lemming,
the banded lemming {My odes torquatus) and the Obi lemming
(Myodes obensis), were still found along the upper Danube, as in
the grottos of Sirgenstein, Ofnet, and Bockstein. From middle
Aurignacian on through Solutrean times these denizens of the
extreme north disappear from this region of Europe. Further
286 MEN OF THE OLD STONE AGE
evidence of a dry, cold climate is found in the recurrence of
dust-storms and in the great deposits of 'newer loess' begin-
ning in certain parts of Europe at the very close of the Mous-
terian industry and extending through both middle and late
Aurignacian and Solutrean times in all the region of the upper
Rhine, along both shores of the Danube, and westward in the
valley of the Somme, in northern France. This period is there-
fore believed to correspond with the Achen retreat of the great
glaciers still covering the Alpine region.
Another striking proof of the amelioration of climate is the
return of the flint workers to many of the open stations, old
and new, in various parts of western Europe, the climate being
more endurable because less humid. In Mousterian times the
open stations were very rare and were perhaps visited during
the summer season only; in Aurignacian times they were
more abundant, there being twelve open stations out of a total
of about sixty stations thus far discovered ; in Aurignacian and
Solutrean times the type station of Solutre was much frequented,
and many other open camps are found in various parts of west-
ern Europe.
This is still the Reindeer Period; in fact, it is the typical
' Reindeer Epoch' of Lartet, and the predominant forms of life
are the woolly mammoth and the woolly rhinoceros; but for a
time the reindeer seems to have been less abundant, and Aurig-
nacian times are marked apparently by a very greatly increased
number of horses. The animal life throughout retains its
northern or arctic character ; the tundra species predominate,
the hardy forms of the forests and meadows of Eurasia are next
in number, and then are found a few of the steppe forms, with
here and there forms characteristic of the Alps. The entire
fauna of the Aurignacian may be summed up as follows :
The wild ass, or kiang, of the Asiatic deserts appears in late
Aurignacian times in the region of the upper Rhine and upper
Danube, as seen in the deposits of Wildscheuer, Thaingen, Kess-
lerloch, and Schweizersbild, and also there probably arrived
in Europe at this time the Elasmo there (E. sibericum). a gigan-
MAMMALIAN LIFE
287
Tundra Life.
Reindeer, woolly mammoth,
wholly rhinoceros, musk-
ox (rare), arctic fox, arctic
hare, arctic wolverene, arc-
tic ptarmigan.
Banded and Obi lemmings
in lower Aurignacian only.
ibex, alpine
Alpine Life.
Argali sheep,
ptarmigan.
Steppe Life.
Steppe horse, kiang,
tral Asiatic ass.
cen-
tic rhinoceros, distinguished from all others that we have been
considering by the entire absence of the anterior horn and
by the possession of an enormous
single horn situated on the forehead
above the eyes, also by the elabo-
rate foldings of the dental enamel,
to which the name ' Elasmo there '
refers; its teeth were especially
adapted to a grassy diet; it ap-
parently wandered into Europe from
the arid grassy plains of central and
western Asia, and its appearance is
connected with the extensive de-
forestation accompanying the tundra
and steppe periods of mammalian
life.
These periodic arrivals from cen-
tral Asia suggest the existence of
migration routes which may also
have been followed by tribes of Pa-
laeolithic hunters.
There is no evidence at this
time of the presence of the more
characteristic animals of the steppes,
such as the saiga antelope, the jer-
boa, and the steppe hamster, which
enter Europe during the later period
of Magdalenian culture. As an in-
dication, perhaps, of the dryness of
the climate we observe that the moose (Alces) is no longer
recorded, although it reappears in western Europe in later Mag-
dalenian times. The giant deer (Megaceros) appears in southern
Germany with the early Aurignacian culture, but this would
seem to be the time of its extinction, because it does not occur
in association with any of the later industries. For a time the
bison in Dordogne, in southern Germany, and in Austria appears
Forest Life.
Red deer, roe-deer, giant
deer, brown bear, cave-
bear, wildcat, wolf, fox,
otter, lynx, weasel.
Meadow Life.
Bison, wild cattle.
Asiatic Life.
Cave-hyaena, cave-lion,
? cave-leopard.
288 MEN OF THE OLD STONE AGE
to be far more abundant than the wild cattle ; the latter animals
are not recorded either by Schmidt or Dechelette in association
with the Aurignacian culture, but they reappear in the moister
period of Magdalenian times.
The remains of similar late Pleistocene mammals lie scat-
tered over a large area in Britain, and we must conclude' from
their presence, observes Dawkins,12 that Britain was still broadly
connected with the mainland of Europe. This is proved by
the occurrence of the mammoth fauna in various places now
covered by the sea, as in Holyhead Harbor, off the coasts of
Devonshire and of Sussex, and in the North Sea. On the Dog-
ger Bank the accumulation of bones, teeth, and antlers is so
great that the fishermen of Yarmouth have collected in their
nets and dredges more than three hundred specimens. They
belong to the bear, wolf, cave-hyaena, giant deer, Irish elk, rein-
deer, stag, bison, urus, horse, woolly rhinoceros, mammoth, and
beaver, and are to be viewed as the remains of animals deposited
by river currents, as in the case of similar accumulations on
land. Had they been deposited by the sea they would have
been sifted by the action of the waves, the smaller being heaped
together in one place and the larger in another. The carcasses
had evidently been collected in the eddies of a river that helped
to form the Dogger Bank, which now rises to within eight fath-
oms of the sea-level.
One of the animals of the Aurignacian period which is best
known is the 'horse of SolutreV Around the great Aurignacian
camp at Solutre there accumulated the remains of a vast number
of horses, which are estimated at not less than 100,000; the
bones are distributed in a wide circle around the ancient camp,
consisting of broken or entire skeletons compacted into a veri-
table magma, with which occur also remains of the reindeer, the
urus, and the mammoth interbedded with all the types of Aurig-
nacian implements. The majority of these horses belong to the
stout-headed, short-limbed forest or northern type, measuring
54 inches (13.2 hands) at the withers, and about the size of the
existing pony.13 The joints and hoofs were especially large, and
THE CRO-MAGNON RACE 289
the long teeth and powerful jaws were adapted to feeding on
coarse grasses ; the greater part of the remains are those of horses
from five to seven years of age. There is no evidence that the
men of Aurignacian times either bred or reared these animals;
they pursued them only for food. The discovery that the horse
might be used as an animal of transport appears to have been
made in the far East, and not in western Europe.
The animal and plant life of the Aurignacian station near
Krems, on the Danube, above Vienna,14 includes a strong ele-
ment of the tundra forms — the arctic fox, wolverene, mammoth,
rhinoceros, musk-ox, reindeer, hare, and ptarmigan. The steppe
fauna, on the other hand, is rare, including only the suslik, but
not the saiga antelope or any of the other characteristic steppe
types. The principal objects of the chase were not only the
mammoth, which was extraordinarily abundant, but also the
reindeer and wild horses ; the ibex is rare.
Obermaier observes that the chart of the geographic distri-
bution of the Aurignacian shows this culture to belong essentially
to the provinces surrounding the entire Mediterranean, from
Syria (the grottos of Lebanon) through north Africa (Algiers) to
Spain. It also has a strong development throughout France,
entering middle and southern Germany and passing along the
Danube to Austria, Poland, and southern Russia (Mezine) north
of Kiev. There is no doubt that the mammoth hunters of
Krems belonged in this wide-spread distribution ; the shells used
for ornaments, which unmistakably recall those of the Riviera,
are only in part local from the neighborhood of Vienna; the
larger part is from the Mediterranean. We may imagine that
these shells passed through several hands among this race of
nomadic hunters, and this is not surprising in view of the girdle
which the Aurignacian stretched around the entire Mediterranean
Sea.
Discovery of the Cro-Magnon Race
The earliest discovery of a member of this race was that by
Buckland, in the cave of Paviland, which opens on the face of
290
MEN OF THE OLD STONE AGE
a steep limestone cliff, about a mile east of Rhossilly, on the coast
of Gower, Wales.15 As described by Sollas, a painted skeleton,
long known as the 'Red Lady,' was found in the kitchen mid-
den which forms the floor of this cave ; recent investigation has
proved that this skeleton belongs to a man of the Cro-Magnon
race ; the associated implements are of Aurignacian type. Pavi-
FiG. 139. Section of the sepulchral grotto of Aurignac, the type station of Aurignacian
culture, as restored by Lartet from the description of the original condition of
the grotto as it was in 1852. After Lyell.
land cave is thus the first Aurignacian station discovered in
Britain and marks the most westerly outpost of the Cro-Mag-
non race.
In 1852 the sepulchral grotto of Aurignac, on the nearest spur
of the Pyrenees, in Haute- Garonne, was accidentally discovered
by a laborer. It was almost filled with bones, among which were
two entire skulls and many fragments, numbering altogether no
less than seventeen skeletons of both sexes and of all ages. The
mayor of Aurignac ordered all the bones to be taken out and re-
interred in the parish cemetery. Thus, in i860, when Lartet
visited this grotto and determined it as the type station of a
distinct industry, all the human remains had been lost beyond
THE CRO-MAGNON RACE
291
recovery, and with them all possibility of learning to what race,
culture, and geologic age they belonged. On a sloping terrace
in front of the grotto was the hearth containing one hundred flint
implements, mingled with the remains of a typical reindeer fauna.
In 1868 Lartet explored a grotto in the little hamlet of Cro-
Magnon, near Les Eyzies, on the Vezere, where he found five
N.E.
S.W.
Fig. 140. Section of the Grotto of Cro-Magnon, in which the fossilized skeleton
of the 'Old Man of Cro-Magnon/ type of the Cro-Magnon race, was discovered
in 1868, together with the remains of four other individuals. After Louis
Lartet. Scale = 1-125.
skeletons, which have become the type of the great Cro-Magnon
race of Upper Palaeolithic times. The grotto was accidentally
discovered by workmen building a road in the Vezere valley.
Here Lartet found the skeleton of an old man, now known as the
i old man of Cro-Magnon ' ; then that of a woman, whose fore-
head bore the mark of a wound from some heavy blow ; close
to her lay the fragments of a child's skeleton and near by those
of two young men. Flint implements and perforated shells were
found with these skeletons.
In May, 1868, the material was first described by Broca,16
his excellent account being later reprinted and amplified in the
Reliquice Aquitanicce of Lartet and Christy.17 Broca referred to
202
MEN OF THE OLD STONE AGE
these skeletons as incontestable proofs of the contemporaneous
existence of man and the mammoth. The associated mammalian
life was that of the reindeer and the industry is now known to be
of the Aurignacian stage. In his classic original description of
this type Broca remarks upon the high stature, the face very
Fig. 141. Head of the very tall skeleton of Cro-Magnon type discovered in the Groltc
des Enfants. After Verneau. One-quarter life size.
broad in relation to its height, with very long and very narrow
orbits; the large and markedly dolichocephalic skull, with an
unusually large brain capacity, noting that the brain capacity
of the Cro-Magnon woman surpasses that of the average male
of to-day; the forehead correspondingly broad, vertical, convex
on the median line ; the bones of the limbs robust, and the shin-
bones flattened transversely; altogether a very high racial type
of skeleton belonging to the species Homo sapiens.
THE CRO-MAGNON RACE
293
Verneau,18 in his description of the Cro-Magnon type, empha-
sizes the disharmonic form of the head, for the dolichocephalic
form of the skull is combined with a face very broad for its height,
and this, in fact, is the unique and most distinctive feature of
the Cro-Magnon race. The cheek-bones are both broad and
high. It is curious that in this face, so broad across the cheek-
Fig. 142. Head of the 'Old Man of Cro-Magnon,' rejuvenated by the restoration of
the teeth, showing the method of restoration of the features adopted in all the models
by J. H. McGregor. The diameter of the head across the cheek-bones is seen to be
greater than that across the cranium. (Compare Figs. 146 and 147, also PL VI.)
bones and cheek arches, the space between the eyes is small, the
nose is narrow and aquiline, and the upper jaw is noticeably
narrow; it is no less remarkable that this upper jaw projects
forward, while the upper part of the face is almost vertical, as in
the highest types of Homo sapiens. The eye sockets, which are
remarkably broad, are rather shallow, and their angles are but
slightly rounded off, so that the form suggests a very long rec-
tangle ; the mandible is thick and strong, and the chin massive,
294
MEN OF THE OLD STONE AGE
triangular, and very prominent ; the marks of muscular attach-
ment denote great muscular development around the thick,
strong jaws, in which the parts for the attachment of the vertical
DISCOVERIES CHIEFLY OF THE CRO-MAGNON AND GRIMALDI
RACES*
Referred to Aurignacian Times
Date of
Discovery
Locality
Number of Individuals
Culture Stage
Cro-Magnon and (?) Aurignacian Race
1823.
Paviland cave, western Wales.
One skeleton.
Burial.
Aurignacian.
1852.
Aurignac, Haute- Garonne, Pyrenees,
Seventeen skeletons.
?
France.
Burial.
1868.
Cro-Magnon, Dordogne, France.
Three incomplete
skeletons and
fragments of two
others.
? Burial.
n
1872-1884.
Grottes de Grimaldi, Baousse-Rousse,
Italy.
Burial.
1. Grotte des Enfants
Four skeletons.
11
(Grotte de Grimaldi).
2. Grotte de Cavillon.
One
"
3. Barma Grande.
Six
"
4. Baousso da Torre.
Three "
"
1909.
Combe-Capelle, Dordogne.
Type of Homo aurig-
nacensis, Klaatsch.
Burial.
1909.
Laugerie Haute, Dordogne.
One skeleton.
Burial.
?
Solutre.
Fragments.
?
Camargo (Santander), Spain.
Fragment of skull.
"
Willendorf, Austria.
Fragments.
Late Aurignacian.
Cave of Antelias (Syria).
Scattered bones.
Aurignacian.
Grimaldi Race
1906.
Grottes de Grimaldi, Baousse-Rousse,
Italy.
1. Grotte des Enfants
Two skeletons.
Aurignacian or 1
(Grotte de Grimaldi).
Late Mous- 1
terian.
* Obermaier,19 R. Martin.20
muscles are unusually large. I would add, says Verneau, to
these essential characteristics the surprising capacity of the
cranium, which Broca estimated as at least 1,590 c.cm. The
majority of these features are found in almost all of the skulls
of the Cro-Magnon race in the Grottes de Grimaldi. The top
THE CRO-MAGNON RACE 295
view of the skull is unusual on account of the extreme prominence
of the eminences of the parietals, which give the skull a pentag-
onal effect when seen from above. The eyebrow ridges show
decided prominences above the orbits but disappear completely
in the median line and at the sides and thus differ totally from
those in the Neanderthal head.
Of the numerous skeletons found in the Grottes de Grimaldi,
or Baousse-Rousse, near Men tone, the one first discovered is
most widely known as the 'man of Mentone,' which was found
in the Grotte de Cavillon, in 1872, by Riviere; hence this is
sometimes spoken of as the Mentone race ; but, as Verneau shows,
while the measurements of the skulls of Baousse-Rousse show
some variety, they do not exceed what might be expected in
individual variation, and we conclude that all the men of tall
stature found in the Grottes de Grimaldi belong to the Cro-
Magnon race, which is not to be confused with the very distinct
dwarf Grimaldi race discovered in the Grottes de Grimaldi by
Verneau, in 1906, in a lower level than any of the skeletons of
the Cro-Magnon type.
In Aurignacian times, lofty stature seems to have been a gen-
eral characteristic of this race, but there appears to have been a
gradual decrease in height, so that in later industrial times the
race in general is somewhat smaller in stature. The heights are
as follows :
Cro-Magnon type of Dordogne 1.80 m. 5 ft. 10 % in.
" woman slightly inferior in size.
Baousse-Rousse, Grottes de Grimaldi.
Adult males of
Cavillon 1.79 m. 5 ft. 10 yi in.
Barma Grande II 1.82 m. 5 ft. 11 y2 in.
Baousso da Torre II 1.85 m. 6 ft. % in.
Barma Grande 1 1.93 m. 6 ft. 4 in.
Grotte des Enfants 1.94 m. 6 ft. 4 y2 in.
Average 1.87 m. 6 ft. 1 ^ in.
Woman of Barma Grande estimated at 1.65 m. 5 ft. 5 in.
Youth of 15 years, Barma Grande, estimated at 1.65 m. 5 ft. 5 in.
The woman had not reached complete development. As
there is a variation of 6 inches in the height of the various male
296
MEN OF THE OLD STONE AGE
skeletons, it is evident that we cannot reach a trustworthy con-
clusion from a single subject ; but there would seem to be quite
a disparity in height between the sexes.
The very large skeleton from the Grotte des Enfants, measur-
ing 6 feet 4*4 inches, was found associated with the remains of
Fig. 143. The abri or shelter of Laugerie Haute, Dordogne, France, where the Aurig-
nacian burial of a skeleton referred to the Cro-Magnon race, was discovered
in 1909. Photograph by Belves.
the reindeer, 15 feet below the surface, from which it would ap-
pear probable that the skeleton antedates the Aurignacian skel-
eton of Laugerie Haute, and even of Cro-Magnon. Thus the
so-called man of Mentone may be an ancestor of the race which
was found in Cro-Magnon and other regions of Dordogne. It
is these men of great height, found in Barma Grande and the
Grotte des Enfants, which Verneau selects for his description of
the primitive members of the Cro-Magnon race, which at this
time lived along the Riviera and in the valley of the V6zere and
later spread over a vast area in western Europe. It is probable
THE CRO-MAGNON RACE
297
that in the genial climate of the Riviera these men obtained
their finest development ; the country was admirably protected
wummwM:!
HPi
i
Fig. 144. Comparative view of the Neanderthal skeleton (left) from La Chapelle-anx
Saints, and of the skeleton of a very tall member of the Cro-Magnon race (right) dis-
covered in the Grotte des Enfants. After Boule and Verneau. Both figures are ap-
proximately one-seventeenth life size.
from the cold winds of the north, refuges were abundant,
and game by no means scarce, to judge from the quantity of
animal bones found in the caves. Under such conditions of
298
MEN 01' THE OLD STONE AGE
life the race enjoyed a fine physical development and dispersed
widely.
With an average height of 6 feet ilA inches, these cave-dwellers
may be said to demonstrate one of the most striking traits of
the Cro-Magnon race. In the proportions of the limbs and in
the great size of the upper part of the chest these men are re-
moved from the modern European type and approach some of
the African negroid types, although there is not the least resem-
blance to the negro type in the skull or in the dentition. In
contrast with the Neanderthals are three characters of the limbs :
n.i
Fig. 145. Sections of the tibia or shin-bone, (i) the normal triangular type;
and (2) the extremely platycnaemic flattened type characteristic of the
Cro-Magnon race. After Broca.
the leg was very long in comparison with the arm ; they show a
remarkable lengthening of the forearm in proportion to the upper
arm and a still more remarkable lengthening of the lower leg or
shin-bone in proportion to the thigh-bone ; the tibia has an index
of 81-86 per cent as compared with the femur, which is relatively
greater than that of the average modern European, with a tibio-
femoral index of 79.7 per cent. This long shin-bone indicates
that these men were swift of foot, quite in keeping with their
undoubted nomadic habits and wide distribution. The flatness
of the tibia, which is strongly marked in 62 per cent of the
skeletons, may well be due to the habit of squatting while en-
gaged in fashioning flints and in other industrial occupations.
The leg, long in comparison with the arm, and the thigh-bone,
strongly developed, are both characters of a hunting race. The
foot has a very protruding heel, but the sole and the toes are
THE CRO-MAGNON RACE 299
of moderate length. The hip-girdle is of a type which has noth-
ing negroid about it, but is as fine as that of the most civilized
whites; it is marked by its strength, the augmentation of all
the vertical and transverse diameters, and the reduction of the
anteroposterior diameters. The shoulders are exceptionally
broad. The fact that the arms are relatively short as com-
pared with the legs is also a high racial character. The upper
arm is very robust, and in some cases the left arm is more largely
developed, in others the right.
In all the skulls from these grottos near Mentone, the face
shows the essential features of the Cro-Magnon race, its breadth
being due to the development of the cheek-bones and the zygo-
matic arches, for the upper jaws are narrow, and the nose is thin
or leptorhine. At the root the nose shows a marked depression,
but it rises immediately to a considerable prominence ; it thus
undoubtedly had an aquiline profile. The orbits always present
the form of a long rectangle, so characteristic of the race along
the Vezere. All these characters leave no doubt of the racial
affinity of the skeletons from the Grottes de Grimaldi with the
original Cro-Magnon type. It must be concluded, therefore,
that certain peculiar features noted in the type of the 'old man
of Cro-Magnon' are purely individual, and that we are not jus-
tified in assuming the admixture of a foreign element to ac-
count for the weakness of some characteristics which we notice
in the majority of the Cro-Magnon subjects from the caves of
Grimaldi. *
The highly evolved characters of the skeleton in this race
are in keeping with the extraordinarily great cranial capacity.
Broca estimated the 'old man of Cro-Magnon' as having a
cranial capacity of 1,590 c.cm., and in the female the brain is
estimated at 1550 c.cm. Verneau estimates the five large male
skulls of Cro-Magnon type at Grimaldi as having an average
capacity of 1,800 c.cm., the lowest being 1,715 c.cm., and the
highest 1,880 c.cm. This race, observes Keith,21 was one of
the finest the world has ever seen. The wide, short face, the
extremely prominent cheek-bones, the spread of the palate and
300
MEN OF THE OLD STONE AGE
a tendency of the upper cutting teeth and incisors to project
forward, and the narrow, pointed chin recall a facial type which
is best seen to-day in tribes living in Asia. to the north and to
the south of the Himalayas. As regards their stature the Cro-
:\.n\:/s-
Fig. 146. Restoration of the head of the 'Old Man of Cro-Magnon,' in pro-
file, modelled after the type skull of Cro-Magnon, Dordogne, with the
teeth restored and the head given a younger appearance. After the
model by J. H. McGregor. One-quarter life size.
Magnon race recalls the Sikhs living to the south of the Him-
alayas. In the disharmonic proportions of the face, that is,
the combination of broad cheek-bones and narrow skull, they
resemble the Eskimo. The sum of the Cro-Magnon characters
is certainly Asiatic rather than African, whereas in the Gri-
maldis the sum of the characters is decidedly negroid or African.
We shall trace this great race through the Solutrean and
THE CRO-MAGNON RACE
301
Magdalenian stages of the Upper Palaeolithic and consider its
disappearance and possible distribution at the close of Mag-
dalenian times. It will then be interesting to consider the evi-
dence of the survival of the descendants of this race in various
Fig. 147. Restoration of the head of the ' Old Man of Cro-Magnon,' front
view. After the model by J. H. McGregor. One-quarter life size.
parts of western Europe and possibly among the primitive in-
habitants of the Canary Islands, known as the Guanches.
Evidence of Other Races
It is a mooted question whether the Cro-Magnons were the
only people inhabiting Europe in early Aurignacian time or
whether there were also two other races, the Grimaldi and the
Aurignacian. As we have seen in the preceding pages, there
is no evidence that the negroid Grimaldi race ever became es-
302 MEN OF THE OLD STONE AGE
tablished in Europe ; the idea of the presence of a negroid race has
taken the fancy of archaeologists like Breuil and Rutot, when seek-
ing an African, Egyptian, or Bushman analogy in certain phases
of early Aurignacian art ; but it rests merely on the slender evi-
dence afforded by the isolated skeletons of a woman and of a boy.
The case of the Aurignacian race is different; this is held
by competent anatomists (Klaatsch,22 Keith23) to be distinct from
the Cro-Magnon race and to bear some resemblance to the
Briinn (Briix, Pfedmost, [?] Galley Hill) race which, we know,
became established in central Europe certainly as early as So-
lutrean times, if not before.
The so-called Aurignacian race (Homo sapiens aurignacensis) ,
described as a subspecies of existing man, is based upon a type
found in the shelter of Combe-Capelle near Montferrand, Peri-
gord, in the summer of 1909 by O. Hauser.24 It is commonly
known as the ' Combe-Capelle ' man from the scene of its dis-
covery, or as the Aurignacian man (Homo aurignacensis) ; if a sub-
species, it certainly belongs to Homo sapiens. The adult male
skeleton was discovered lying undisturbed in the lowest stratum of
an Aurignacian industry and was carefully disinterred by Klaatsch
and Hauser. It was apparently a case of ceremonial burial;
a great number of unusually fine flints of early Aurignacian type
was found with it, also a necklace of perforated shells (Littorina,
Nassa) ; the limbs were bent.25 Water saturated with lime had
dripped upon the burial-place, resulting in the remarkable preser-
vation of the skeleton. This skeleton is compared by Klaatsch
with that of Briinn, Moravia, and of Galley Hill, near London,
from which he concludes that it represents a distinct type, the
Aurignacian race ; the stature is 5 feet 3 inches, as compared with
6 feet il/i inches, the average in the five Cro-Magnon males of
Grimaldi; the brain case is well arched and falls within the
variation limits of Homo sapiens. The skull is very long and
narrow, the cephalic index being 65.7 per cent; in some points
it shows a striking similarity to that of Briinn, in others it varies
from it in the direction of the recent European form ; the face
is not narrow nor is it prognathous ; the lower jaw is small with a
BURIAL CUSTOMS 303
well-developed chin. Klaatsch finds many characteristics re-
sembling those of the Cro-Magnon race, including the Chancelade
type which is a late Cro-Magnon. He suggests that the Cro-
Magnon type may be considered a further development of the
Aurignacian. It seems probable that the Aurignacian man is a
member of the true Cro-Magnon race and that additional evidence
is required to establish it as distinct. Schliz26 considers that this,
Fig. 148. Brain outline of the man of the so-called Aurignacian race discovered at
Combe- Capelle in 1909 (after Klaatsch), as compared with the brain outlines
of a chimpanzee and of Homo sapiens.
skull is an intermediate form between that of the Cro-Magnon
and the Briinn race, an indication that these two races were
undergoing a parallel development.
Burial Customs
Similar customs of burial prevailed widely in Aurignacian
times, as we have observed from the use of color in the Paviland
interment of western Wales and in the Briinn interment of
Moravia. This is a feature seldom found in the Neanderthal
burials, although the latter are accompanied by signs of great
reverence and by an abundance of ornaments and finely finished
flints. Up to the present time the races of the Upper Palaeolithic
have been studied with far less anatomical precision than those
of the Lower, and the attribution of many of the burials to the
Cro-Magnon race awaits verification.
304 MEN OF THE OLD STONE AGE
We have little record of the Paviland burial except that the
skeleton was that of a man of the Cro-Magnon race and col-
ored red. Of the burial of Aurignac we have no record other
than that seventeen skeletons were placed close together; it
would appear that this compound burial may have been the
sequel of a battle or, less probably, that of an epidemic. The
type skeletons of the Cro-Magnon race were simply lying on
the surface of a deep shelter ; thus there has always been some
doubt as to their exact archaeological age ; a large number of
perforated shells was found among the bones, as well as pen-
dants of ivory.
The most remarkable Cro-Magnon burials of undoubted Au-
rignacian age are those of the Grottes de Grimaldi ; the infant
skeletons found here are neither colored nor decorated, but oc-
curred with a vast number of small perforated shells (Nassa),
evidently forming a sort of burial mantle. Similarly, the fe-
male skeleton was enveloped in a bed of shells not perforated;
the legs were extended, while the arms were stretched beside
the body; there were a few pierced shells and a few bits of
silex. One of the large male skeletons of the same grotto had
the lower limbs extended, the upper limbs folded, and was
decorated with a gorget and crown of perforated shells ; the
head rested on a block of red stone. In the 'man of Mentone/
found in 1872, the body rested on its left side, the limbs were
slightly flexed, and the forearm was folded ; heavy stones pro-
tected the body from disturbance ; the head was decorated with
a circle of perforated shells colored in red, and implements of
various types were carefully placed on the forehead and chest.
Similarly in the burial of Barma Grande three skeletons were
found placed side by side in a layer of red earth containing a
large quantity of peroxide of iron ; two of the skeletons rested
on the left side, the limbs extended or slightly flexed ; the fore-
head and chest and one of the limbs were encircled with shells.
In the burial of the so-called Aurignac man of Combe-Ca-
pelle, described above, the limbs were outstretched and the body
was decorated with a necklace of perforated shells and sur-
AURIGNACIAN INDUSTRY 305
rounded with a great number of fine Aurignacian flints. It
appears that in all the numerous burials of these grottos of Au-
rignacian age and industry of the Cro-Magnon race we have
the burial standards which prevailed in western Europe at this
time.
We must infer that the conception of survival after death
was among the primitive beliefs, attested by the placing with
the dead of ornaments and of weapons and in many instances
of objects of food. It is interesting to note that the grottos and
shelters were so frequently sought as places of burial, also that
the flexed limbs or extended position of the body prevailed
throughout western Europe into Neolithic times, as well as the
use of color through the Solutrean into Magdalenian times. It
is probable from their love of color in parietal decorations, and
from the appearance of coloring matter in so many of the burials,
that decoration of the living body with color was widely prac-
tised, and that color was freshly applied, either as pigment or
in the form of powder, to the bodies of the dead in order to pre-
pare them for a renewal of life.
Aurignacian Flint and Bone Industry
As pointed out in the introduction of this chapter, the geo-
graphical distribution of the early Aurignacian industry is espe-
cially interesting in its bearing upon the routes by which the Cro-
Magnon race entered Europe. "We can hardly contemplate an
origin directly from the east," says Breuil,27 "because these ear-
lier phases of the Aurignacian industry have not as yet been met
with in central or eastern Europe." A southerly origin seems
more probable, because the Aurignacian colonies appear to sur-
round the entire periphery of the Mediterranean, being found in
northern Africa, Sicily, and the Italian and Iberian peninsulas,
from which they extended over the larger part of southern
France. In Tunis we find a very primitive Aurignacian like that
of the Abri Audit of Dordogne, with implements undoubtedly
similar to those of Chatelperron, in France. Even far to the
306
MEN OF THE OLD STONE AGE
east, in the cave of Antelias, in Syria, as well as in certain stations
of Phoenicia,28 culture deposits are found which are character-
istically Aurignacian. Again, in southern Italy implements of
typical Aurignacian form, tending toward the superior stage, are
found in the grotto of Romanelli, Otranto.
On the other hand, in favor of the theory of local or autoch-
thonous evolution of this culture is the direct succession described
below of Aurignacian prototypes and early Aurignacian imple-
ments above the older Mousterian layers in the various stations
of Dordogne. In fact, the
Art.
Microlithique, microlith.
Burin, graver
(first appearance).
Industrial.
Coup de poing, hand-stone
(rare and degenerate).
Pointe, point.
* Chatelperron (curved).
double-pointed.
relation of the Aurignacian
industry to the preceding
Mousterian is one of the most
important in the history of
Palaeolithic archaeology, be-
cause of the change of race
which occurred at this time.
How far is it derivative and
autochthonous, how far is it
new and influenced by inva-
sion and the handicraft of a
new and superior race?
First, as for transition from
the older culture, it is impor-
tant to note throughout that
the ' Aurignacian retouch' is
identical with the Mousterian ;
this retouch is on one side of
the flake only and gives it a
short, abrupt, and blunt edge.
As we shall see, it is essenti-
ally different from that dis-
covered by the Solutrean flint
workers and employed in Solutrean times, a superior technique
which produced a sharp, thin edge, many of the implements
* Denotes very frequent occurrence of a typical form.
Racloir,
scraper.
convex.
concave.
straight.
double-edged.
triple-edged.
Grattoir,
planing tool.
Percoir,
drill, borer.
Couteau,
knife, blade.
Enclume,
anvil stone.
Percuteur,
hammer-stone.
rar and Chase.
Pointe,
point.
Pierre de jet,
throwing stone.
Couteau,
knife, blade.
Pointe de lance,
bone lance-heads.
AURIGNACIAN INDUSTRY
307
being dressed on both sides. On the other hand, Breuil con-
cludes that the early Aurignacian industry can only in part be
derived from the late Mousterian and that it is partly due to
the invasion of a race which ranks much higher in the scale of
intelligence than the Neanderthal.
The pure early Aurignacian industry is seen in the regions of
Dordogne and the Pyrenees in the layers of Chatelperron, Ger-
molles, Roche au Loup, Haurets, and Gargas. The cave of
Fig. 149. Implements designed for engraving and sculpture. Evolution of the angu-
late graving- tool or burin, from the early Aurignacian of Chatelperron (left), to the
late Solutrean of Placard (right). After Breuil. About one-third actual size. These
small implements, chiefly made from elongated flakes and distinguished by a sharp
angulate edge at one end suitable for graving on bone or stone, are especially charac-
teristic of the Aurignacian stage of culture, in which they first appear. 1, 2. Chatel-
perron points. 6. Prototype of the Magdalenian 'parrot-beak.' Some of these burins,
such as 7, are made into grattoirs or planing tools at the other end.
Gudenushohle, near Krems, in Lower Austria, exhibits a very
primitive phase of the early Aurignacian. Here numerous small
flints were found, resembling those found at Brive by the Abbes
Bardon and Bouyssonie; similar microliths are also found at
Pair-non-Pair, Gironde, at various stations in Dordogne, and at
the Grottes de Grimaldi, on the Riviera, in layers of corre-
sponding age.
The chief invention of this stage is the ' Chatelperron point'
(Fig. 149), a direct development from the curved point of the
Abri Audit (Fig. 151) and a dominant type of the early Aurig-
nacian culture. Small almond-shaped ' coups de poing' are
308
MEN OF THE OLD STONE AGE
still met with at Chatelperron and a few other localities, but
Breuil suggests that these may not be real examples of Aurig-
nacian industry but implements carried off from older sta-
tions.
The use of elongated flakes is another feature of this early
industry, but the retouch of the edges cannot compare with the
fine 'grooved retouch' of the middle Aurignacian; as yet the
flakes are thick and large. Many of the scrapers are 'keeled'
(grattoirs carenes) .
An entirely new implement appears in addition to the trian-
gular and elongate flakes of flint shaped into points and scrapers
of forms ; this is the primitive graving-tool, or burin, which at
first is quite rare, but which we know was designed by the
Cro-Magnon artists for their
Art Implements.
Microlithique,
* Burin,
Ciseau,
* Gravette,
microlith.
graver,
chisel,
etching tool
(first appearance).
New Industrial Implements.
Pointe, point
(leaf-shaped).
* Grattoir carene, keeled scraper.
Perqoir, drill, borer.
* curved (first appearance) .
Couteau, knife, blade.
* curved-in edges.
Poinqon, awl
(bone).
New Implements of War and Chase.
Pointe a cran, shouldered point
(stone).
Pointe de sagaie, javelin point
(bone).
early engravings on stone (Fig.
149).
A fourth highly distinctive
feature of the early Aurigna-
cian is the use of a variety of
implements of bone and horn
consisting chiefly of javelin
points and drills and of coarse,
spatula-like tools.
In the middle Aurignacian
the flake industry reaches its
perfection of form and tech-
nique; the edges of the flakes
are shaped all around with the
'grooved retouch' resulting in
symmetrical forms such as the
oval, double-ended 'points,'
the leaf-shaped 'points,' and
the double scrapers ; this, in
is the culmination of the 'Aurignacian retouch,' which
The retouch of the long flakes is
fact
afterward begins to decline.
* Denotes very frequent occurrence of a typical form.
AURIGNACIAN INDUSTRY
309
fine and parallel, but as yet the flakes themselves are generally
thick and heavy, so that their ends are, perforce, much broader
than those of the Solutrean and Magdalenian fashion. One of
the most distinctive forms of this middle Aurignacian industry
is the ' keeled scraper' {grattoir carene) with an abruptly grooved
retouch (Fig. 150).
Still more significant in connection with the rapid artistic
development of these people is the remarkable increase in the
Fig. 1 50. Implements suitable for the dressing of hides and for sculpture. The keeled
scraper or planing tool — grattoir carene — characteristic of the Aurignacian culture.
After Breuil. About two-fifth actual size, i, 2, 3. Short and broad types appearing
in the middle Aurignacian. 4, 5. More elongated types of the advanced middle Au-
rignacian from Cro-Magnon, Dordogne. 6. Elongated type (pic) of the close of the
middle Aurignacian. 7, 8. Small grattoir s with handles, suitable for sculpture.
number and variety of graving- tools, including numerous curved
gravers. Almost all the chief types of gravers (burins) have
now been invented, and tools of bone have become extremely
numerous and varied. To engraving and linear design have
been added the art of sculpture and the primitive use of color
(Breuil,29 Schmidt30).
In the Dordogne region this evolution of the middle Aurig-
nacian is exemplified at Le Ruth, Le Roc de Combe-Capelle, and
the principal layers of the Abri Audit as well as at the shelter of
Laussel. It is well developed also at Le Trilobite, on the head-
waters of the Seine.
310
MEN OF THE OLD STONE AGE
Art.
Microlithique,
microlith.
Burin,
graver.
Ciseau,
chisel
(of stone and bone).
Gravette,
etching tool.
Pic,
pick
(triangular or quadrangular,
for sculpture).
In the late Aurignacian (Breuil,31 Obermaier32) there is a no-
table departure from the Mousterian fashion of chipping the
flakes ; even the dis-
tinctive blunt ' Aurig-
nacian retouch' is
somewhat weakened;
but at the same time
the work on the elon-
gated flakes becomes
more facile and skilful.
For delicate, artistic
work there appear ex-
tremely small imple-
ments or 'microliths'
of various shapes.
The early and mid-
dle Aurignacian
1 point' and the 'grat-
toir,' sharpened all
around, as well as the
incurved flake become
less frequent. The
grattoirs, or planing
tools, are somewhat
higher and narrower
than those of the early
Aurignacian but not very different in form; two forms of
grattoir are recognized, one long and not very thick, the other
high and keel-shaped (grattoir carene).
Among the percoirs a curved form is very characteristic, and
we also note a variety of small knives, or couteaux.
The inventive genius of this people is displayed in the rapidly
increasing variety of flint implements designed for fishing or for
the chase. Toward the end of the Upper Aurignacian there
appears the shouldered spear head (pointe a cran), and also a
* Denotes very frequent occurrence of a typical form.
Ceremonial.
Baton de commandement, ceremonial staff
(first appearance).
New Industrial Implements.
Grattoir, planing tool
* long but not thick.
Aiguille, needle
(bone, first appearance).
New Implements of War and Chase.
Lance and spear head types, of stone :
(a) Pointe a cran, shouldered point.
(b) Pointe a soie, tongued point
(Font Robert type).
(c) Pointe de lau- laurel-leaf
rier(?), point(?).
Couteau, knife, blade
(bone, first appearance).
AURIGNACIAN INDUSTRY
311
lance form of which the most perfect types have been found at
Willendorf , in Austria, and at Grimaldi, on the Riviera. More or
less sporadically there appear specimens of the tongued spear
heads (pointes a sole), such as are found at Spy, Font Robert,
and Laussel. This type of flint is constantly found associated
with rudely formed prototypes of the Solutrean laurel-leaf point.
Decorative art has now become a passion, and graving-tools
of great variety of shape, curved, straight, convex, or concave,
Fig. 151. Implements of industrial use, of the chase, and of fishing; also suitable for
fine engraving and etching on stone or bone. Evolution of the Aurignacian pointe
with abrupt retouch along one edge, from the base to the summit of the Aurignacian.
After Breuil. About one-third actual size. 1-4. Primitive curved points from the
Abri Audit, Dordogne. 5. More evolved curved point from Gargas. 6, 7. Points
from Chatelperron, at the base of the middle Aurignacian. 11-28. Microlithic points
from La Gravette and Font Robert. The form of 28 suggests that of the pointe a cran
or ' shouldered point ' characteristic of the late Solutrean.
diversified both in size and in style of technique, are very numer-
ous. We may imagine that the long periods of cold and inclem-
ent weather were employed in these occupations. The use of
the reindeer horn is developing, and the decoration of the bone
with very fine lines drawn by the microlithic tools is at times
very remarkable. Here appear the earliest examples of the so-
called baton de commandement, which is supposed to have served
as a ceremonial staff or wand ; it is made of the reindeer antler
with a great hole bored at the point where the brow tine unites
312
MEN OF THE OLD STONE AGE
with the main beam ; some of these batons are ornamented with
rude engravings, but not as yet with sculpture.
Strong and very sharp graving- tools were also needed for the
sculpture out of ivory and soapstone of such human figures and
figurines as the statuettes found in the Grottes de Grimaldi and
at Willendorf and still more powerful tools for such work as the
large stone bas-reliefs of Laussel. At this time the Cro-Mag-
nons were also fashioning stronger tools for the engraving of
Fig. 152. Prototypes of the Solutrean laurel-leaf point, probably an imple-
ment of war or the chase. After Breuil. Large symmetrical flakes chipped
over the entire surface. 1, 2. Late Aurignacian types from Font Robert.
3, 4, 5. Points from the Proto-Solutrean layer of the Grotte du Trilobite.
animals in stone, for shallow forms of bas-relief on the walls of
the caves, and for other animal outlines. The most evolved
animal figures of this period arouse the thought of Magdalenian
art in its beginnings.
As this industrial evolution widens it is apparent that we
witness not the local evolution of a single people but rather the
influence and collaboration of numerous colonies reacting more
or less one upon the other and spreading their inventions and
discoveries. These people were essentially nomadic and no
doubt carried the latest types of implements from point to point
or bartered them in trade. Thus there is not only a definite
succession in such places as Dordogne, but in more remote re-
gions the form of the implements may take on some important
AURIGNACIAN INDUSTRY 313
differences.33 There are also other localities where the industry
seems for a while to be suspended; thus in the Cantabrian Moun-
tains of Spain we find only the early and the late Aurignacian.
Stations similar in culture to those of Dordogne extend
northward into Germany and Belgium and eastward into Aus-
tria and Poland. Thus the characteristic flint spear heads,
known as the pointe a sole and pointe a cran extend from
Laussel along the Vezere to Willendorf, in Austria; and the
female figures of Baousse-Rousse (Grimaldi) and of Willendorf
represent the same stage of evolution as the large stone bas-
relief of Laussel. Again, we observe some relations between
the Aurignacian cultures of Austria and of the Italian penin-
sula, such as the pointe a cran, derived from the gravette
and found both in various stations of northern Italy and at
Willendorf. In western Russia the Aurignacian station of Me-
zine, Chernigov, shows clearly the types of the superior Aurig-
nacian in the graving of bone and ivory, in the small batons
recalling those of Spy, in Belgium, and of Brassempouy, in
southwestern France, in the large bone piercers perforated at
the head, suggesting the primitive needles from the shelter of
Blanchard, and in the degenerate statuettes resembling the
type of Brassempouy.
Distribution or the Aurignacian Industry
When the general geographic distribution of the Aurignacian
(Fig. 153) is compared with that of the Mousterian (Fig. 125) it
is surprising to find how many of the stations are identical; it
would appear as if the Cro-Magnons had driven the Neander-
thals from their principal stations over all of western Europe for
the pursuit of their own industries and of the chase. We have
already spoken of the invasion of the Mousterian stations along
the Riviera, in the Pyrenees, in the Cantabrian Alps, and along
the Dordogne and the Somme ; this occupation also extends
along the Meuse, the Rhine, and the Danube ; but, whereas
there are only six stations in all Germany of unquestioned
Mousterian age, there are more than double that number in
314
MEN OF THE OLD STONE AGE
Aurignacian times. The Cro-Magnons entered the grottos of
Sirgenstein and Rauberhohle, near the headwaters of the Dan-
ube ; northwest of Sirgenstein they established the open ' loess '
station of Achenheim, west of Strasburg ; in the lower layers of
A
1- Miremont
9-Abn Audit
Z-La Ferrassie
10-La Moiithe
3-Gorged' Enfrr
n-La Roche St. ChrUtoplu
4_ Laugerie Haute
\Z-Fongal
5-Le Ruth
13" Lanssel
6"" La Rocliette
X4rFant-de- Gaume
7- Crd-Magnon
15-Sireuil
irPataud
16-La Grese
Fig. 153. Geographic distribution of the principal Aurignacian industrial stations in
western Europe.
the l newer loess ' was also the station of Volklinshof en, south of
Achenheim; along the middle Rhine were the 'loess' stations
of Rhens and Metternich, and to the far north, close to the
borders of the Scandinavian glacier, was the somewhat doubtful
Aurignacian station of Thiede. The Cro-Magnon men entered
the Sirgenstein grotto and scattered the implements of their
culture above the 'lower rodent layer/ composed of the Obi
lemming, and also left remains of the woolly rhinoceros, the
woolly mammoth, the stag, and the reindeer on the floor of
THE BIRTH OF ART
315
the cavern. The Upper Aurignacian also extends down the
Danube as far as Willendorf, and possibly to Brlinn, Moravia,
which last, however, may be of Solutrean age. Altogether be-
L
1
'"» « w-
1
^ -
1
4
t t
*
J ■
Fig,. 154. Outlook over the Bay of Biscay from the entrance of the cavern of Pindal,
in the province of Asturias, northern Spain. Photograph by N. C. Nelson.
tween seventeen and twenty Aurignacian stations have been
discovered in the region north of the Danube and along the
Rhine.
Aurignacian Art*
The strongest proof of the unity of heredity as displayed
in the dominant Cro-Magnon race in Europe from early Aurig-
nacian until the close of Magdalenian times is the unity of their
* Breuil.34 Schmidt.35
316 MEN OF THE OLD STONE AGE
art impulse. This indicates a unity of mind and of spirit. It is
something which could not pass to them from another race, like
an industrial invention, but was inborn and creative. These
people were the Palaeolithic Greeks; artistic observation and rep-
resentation and a true sense of proportion and of beauty were
instinct with them from the beginning. Their stone and bone
industry may show vicissitudes and the influence of invasion
and of trade and the bringing in of new inventions, but their
art shows a continuous evolution and development from first to
Fig. 155. Outline of a mammoth painted in red ochre in the cavern of Pindal,
and attributed by Breuil to the Aurignacian. Only two limbs are
represented. After Breuil.
last, animated by a single motive, namely, the appreciation of
the beauty of form and the realistic representation of it.
This art, as first discovered by Lartet and further made known
through the brilliant studies of Piette and Breuil, is industrial
{Vart mobilier), consisting of the decoration of small personal be-
longings, ornaments, and implements of stone, bone, and ivory.
According to the later researches of Sautuola, Riviere, Cartai-
lhac, Capitan, and Breuil it is also mural or parietal part parietal),
consisting of drawings, engravings, paintings, and bas-reliefs on
the walls of caverns and grottos. It remained for Breuil espe-
cially to demonstrate that the mobile and the parietal art are
identical, the work of the same artistic race, developing along
THE BIRTH OF ART 317
closely similar lines, step by step. Thus the art becomes a new
means not only of interpreting the psychology of the race but
of establishing the prehistoric chronology.
Dating of the Art
One of the first questions which rises in our mind is this —
how is this art dated ; how can these steps be positively deter-
mined ?
The age of these engraved or painted designs on the walls of
the caverns is determined in a number of ways described by
Breuil.36 The simplest method is where the wall designs of one
period are covered by the archaeological layers of succeeding
periods. This has been observed in four cases, as at Pair-non-
Pair, Gironde, where primitive engravings of horses, caprids, and
bovids are buried under flints characteristic of the late Aurig-
nacian mingled with bones of the mammoth, rhinoceros, lion,
hyaena, bison, and reindeer. Again, the deeply engraved bison
on the wall of the grotto of La Greze, Dordogne, is found beneath
a talus of Solutrean flints associated with remains of the bison,
reindeer, and rhinoceros. In the Grotte de la Maine, Dordogne,
are found several finely engraved middle Magdalenian figures of
animals buried beneath late Magdalenian implements associated
with the reindeer fauna.
Very important, indeed, is the age of the sculpture and bas-
reliefs found in Laussel. The human sculptures are determined
to be of late Aurignacian age, because they are buried in an
early Solutrean talus. The splendid wall sculptures of the series
of horses in the Cap-Blanc shelter, near the Laussel shelter, are
shown to be of middle Magdalenian age, because of the upper
Magdalenian strata which covered and partly concealed them.
In other instances we can date a drawing in a cavern by the
period at which the opening was closed ; for example, the cave of
La Mouthe, Dordogne, was closed in by a Magdalenian layer of
flints which touched the roof and firmly sealed up the entrance
until recent times. Again, at Gargas, Hautes-Pyrenees, we
318
MEN OF THE OLD STONE AGE
know that the last occupation by the Cro-Magnons was near
the end of Aurignacian times, as indicated by a hearth filled
Fig. 156. Primitive painted outlines of animals from the cavern walls of Font-dc-Gaumc,
Dordogne, attributed by Breuil to the early Aurignacian. The outlines represent the
horse, ibex, cave-bear, wild cattle, and reindeer. After Breuil.
with late Aurignacian flints and with the remains of the bear,
hyaena, horse, and reindeer ; the opening of the grotto was
buried beneath these foyers, which obstructed the entrance until
the cave was rediscovered at a comparatively recent date. Also
THE BIRTH OF ART
319
at Marsoulas, Haute- Garonne, there are two hearths, one late
Aurignacian, the other late Magdalenian ; the grotto was then
closed until recent times. The grotto of Niaux, on the Ariege,
which contains fine examples of drawings of middle Magdale-
nian times at a distance of 1,800 feet from the entrance, was
protected for a long period by a lake 6 feet deep and several
hundred feet long. At Altamira, near Santander, the superb
frescoed ceiling was buried, long before Neolithic times, by the
w
Fig. 157. The woolly rhinoceros, painted in red ochre with shading and partial rep-
resentation of the hair, in the cavern of Font-de-Gaume, Dordogne. Attributed by
Breuil to the late Aurignacian. Possibly Magdalenian. After Breuil.
closing up of the entrance, which was rediscovered only about
thirty years ago.
A third method of dating the art is still more significant ; it
is through a similarity in the engravings on bone, found in the
old hearths associated with flints, to the mural decorations which
are found upon the walls. Thus, at Altamira, engravings on
bone associated with Solutrean and Magdalenian flints enabled
Alcalde del Rio and Breuil to date the engravings on the lime-
stone walls. Hence, in grottos which have never been closed
up and which have been frequented at different times from the
Palaeolithic to the present epoch one observes that the mural
designs in the caverns are invariably accompanied by Upper
Palaeolithic implements with a similar style of decoration ; and
this is the case at Font-de-Gaume, Combarelles, Portel, Mas
d'Azil, Castillo, Pasiega, and Hornos de la Pena. The bone en-
320 MEN OF THE OLD STONE AGE
gravings of the female red deer found at Altamira are identical
in their artistic period with those found on the walls of the same
grotto. The excavations at Castillo, where numerous shoulder-
blades of the deer were found engraved in the same style as those
of Altamira, prove that all these engravings and drawings are
to be referred to ancient Magdalenian rather than to upper
Solutrean times. The engravings upon the walls in the grotto
of Hornos de la Pena, of Aurignacian times, are dated through
the discovery at the base of the layer of Aurignacian flints of an
engraved equine figure similar to the engravings at Altamira.
A fourth method applies to those not infrequent cases when
two or three designs are superposed one upon the other, from
which it necessarily follows that the underlying designs must
antedate those above.
Through the application of these four methods Breuil has
succeeded in dating all the steps in the advance of art from
Aurignacian into Magdalenian times.
Engraving, Painting, and Sculpture
In the archaic drawings of the caverns of Pair-non-Pair, La
Greze, and La Mouthe most of the animal figures are somewhat
heavily and deeply engraved ; the proportions are not true ; the
head is usually too small, with a large, short body which is often
lightly modelled, resting on thin extremities. Quadrupeds are
frequently represented with but two legs, as in the case of the
mammoth. That the powers of observation were only gradually
trained is shown by the fact that details which in later drawings
are well observed are here overlooked; the profile drawings of
animals, with one fore leg and one hind leg represented, are quite
like those of children.
Progress toward a true representation of animal form in
drawing begins very early ; even in middle Aurignacian times
primitive drawing and engraving commences to replace sculp-
ture. Both the flint 'burins' and the engravings on the walls
of the grottos show that the beginnings of drawing may be
THE BIRTH OF ART
321
traced back to early Aurignacian times. While the Palaeolithic
artists early in the Aurignacian had obtained a certain facility
in plastic work, their drawings, which are solely contours —
somewhat imperfect and deeply engraved lines — show a grad-
ual development. The degree of skill attained
in late Aurignacian times we know from the
engraving of a horse on a stone fragment from
Gargas, and from a sketch of the hinder quarter
of a horse found in the cave of Hornos de la
Peria, which is engraved on the frontal bone of
one of the wild horses ; the latter is strikingly
similar to one of the engravings found at the
entrance to the same grotto. The engravings
on a slab of slate of the heads of two woolly
rhinoceroses37 (Fig. 161) probably belong to the
late Aurignacian. Similar attempts are found
in the Abri Lacoste. Ornamentation develops
in the middle Aurignacian, but retains a simple
geometric character.
The parietal art on the walls of the caverns,
mostly deep engravings, consists of stiff profiles
in single lines and in red or black coloring. The
animals represented are the ibex, the horse, the
bison, and rarely the mammoth. The caves
where these are found are Pair-non-Pair, La
Greze, La Mouthe, Bernifal, Font-de-Gaume,
Altamira, and Marsoulas. Crucibles for grind-
ing the color are found in the grotto of Mar-
soulas, the color being made by grinding up the
red and yellow oxides of iron.
The development of art during the whole
Aurignacian is continuous and is undoubtedly the
work of one race ; Breuil considers it the work certainly either of
the tall Cro-Magnons or of the small Grimaldis ; there is, however,
no evidence of the survival of the Grimaldi race, and we may
safely attribute this entire art development to the Cro-Magnons.
Fig. 158. Female
figurine carved in
crystalline talc,
discovered at the
Grottes de Grimaldi,
near Mentone.
This figurine, pos-
sibly modelled
after one of the
Grimaldi negroids,
represents the en-
ceinte condition
common to many
of these figures.
It is peculiar in
showing that ab-
normal develop-
ment behind the
hips known as
steatopygy. After
Reinach.
MEN OF THE OLD STONE AGE
The creative spirit manifested itself along many different
lines. In the fashioning of bone in early Aurignacian times there
begins a new industry capable of great possibilities ; out of com-
binations of lines there develop geometric figures ; in animal fig-
ures there is an attempt at simple symmetric relations, but a
full, free composition is not attained. With further experience
in working with bone and ivory, we find
in the middle Aurignacian the first plastic
representations of the human figure in the
round.
The Cro-Magnon artist undertook this
plastic work, choosing chiefly for his sub-
ject the female figure. These small plastic
models were probably designed as idols;
the figures arp often misshapen; in the
face the eyes frequently are not indicated
I at all ; in some cases the ear is indicated ;
they recall the style of the modern cubists.
■ V More care is given to the sculpture of the
^P form of the body than of the face. The
ivory statue known as the Venus of Bras-
sempouy lies at the base of the middle
Aurignacian; of the same epoch are the
female statuettes of Sireuil, and the torso
from Pair-non-Pair, whereas the soapstone
figurine of Mentone and the ivory statu-
ettes of Trou Magrite, Belgium, belong to
the late Aurignacian. The spread of these
idols, which are altogether characteristic of the earlier period of
the Upper Palaeolithic, is traced eastward to Willendorf, Aus-
tria, and to Brunn, Moravia.
Breuil's great contention is a certain similarity to north
African art, which would seem to agree with his theory that the
Cro-Magnon people followed the southern shores of the Medi-
terranean, bringing with them the Aurignacian industry and the
glyptic art of the female statuettes similar to those of baked
Fig. 159. Statuette in
limestone from the grotto
of Willendorf, Lower Aus-
tria, attributed to the late
Aurignacian. This fe-
male figurine, possibly an
idol and generally known
as the 'Venus of Willen-
dorf,' is about four and
one-half inches in height.
After Szombathi.
THE BIRTH OF ART
323
clay which are found along the valley of the Nile. These figu-
rines have in common the great development of all the parts
connected with maternity, and in some cases a coiffure or head-
dress very much like that found in the most primitive Egyp-
tian work. The extreme corpulence of all the figurines has
been compared with the 'steatopygy,' or development of what
Fig. 160. Female figurine in soapstone, discovered at the Grottes de Grimaldi,
near Mentone, and attributed to the late Aurignacian. After Ober-
maier. This seems to be a prototype of modern cubist art.
are politely known as the 'posterior curves/ of the female in
many African races. But only one of these Aurignacian figu-
rines is truly l steatopygous ' ; the others are simply corpulent, a
condition due to eating large quantities of fat and marrow, and
probably to a very sedentary life. It is noteworthy that none
of the male figures in drawing and sculpture is corpulent. While
the art of the statuettes appears to come to a close in late Au-
rignacian times, it may extend into the Solutrean at Briinn,
Moravia, and at Trou Magrite, Belgium. With due regard for
analogies, it would rather appear probable that this archaic
sculpture was autochthonous.
324
MEN OF THE OLD STONE AGE
The art of engraving and drawing was almost certainly
autochthonous, because we trace it from its most rudimentary
beginnings. This northern art developed from the beginning of
Upper Palaeolithic times over the whole of southwestern France
and in the northwest of Spain, being contemporaneous with the
descent of the alpine fauna from the Pyrenees and the Alps and
Fig. 161. Superposed engravings of various mammals on a slab of slate found in the
Grotte du Trilobite, Yonne, France. In detail are seen the profiles of two woolly rhi-
noceroses superposed on the rump of a mammoth with tail upturned. After Breuil.
the presence all over western Europe of the tundra fauna. It
was, by preference, an animal art, begun by the Aurignacians
but largely suspended in Solutrean times.
Painting38 also had its birth in the Aurignacian, in the simple
contours of the hand pressed against a wall surface or outlined
with color, accompanied by primitive attempts at linear drawing
in color and painted groupings ; for example, the crude outlines of
the bison in the grotto of Castillo are of Aurignacian age, also the
THE BIRTH OF ART 325
black linear designs of the deer and of the ibex in the cavern of
Font-de-Gaume, Dordogne, the striking red linear design of the
mammoth in the grotto of Pindal, in northern Spain, represent-
ing the animal as with two limbs, and the red outlines of wild
Z00
i ft
' 0F«
fk
f%::; -:: \J
f / v
Fig. 162. Silhouettes of complete and of partly mutilated hands from the walls
of the grotto of Gargas in the Pyrenees. After Breuil.
cattle in Castillo. Breuil also attributes to Aurignacian times
the spirited figure of the woolly rhinoceros in red ochre in the
cave of Font-de-Gaume, as well as the outline of the stag in red
color.
We are impressed throughout with three qualities in this
Aurignacian design : first, the very close observation of the
animal form; second, the attempt at realistic effect produced
with very few lines ; third, the element of motion or movement
MEN OF THE OLD STONE AGE
in these animals. For example, the two heads of the woolly rhi-
noceros in the slab engravings of the Trilobite grotto (Fig. 161)
are remarkably correct in proportion ; there is an attempt with
fine lines to indicate the wool hanging along the lower surface of
the head ; behind these two figures is the rump of an elephant
Fig. 163. The* long, overhanging cliff of Laussel on the Beune is a typical rock shelter,
first sought in Acheulean times, and also visited during the Mousterian, Aurig-
nacian, and Solutrean stages. Photograph by N. C. Nelson.
with the tail upturned, an adaptation of the artist to the form
of the slate fragment ; the outlines of the feet both of the rhi-
noceros and the mammoth are remarkably accurate representa-
tions of these pachyderms.
In the more advanced development of draftsmanship in late
Aurignacian times the engravings of these animals not merely
approach the truth, but characteristic features are strikingly
represented ; and with a few sure lines the proportions of the
body as a whole are better preserved, while the complicated
curves of the hoofs and of the head show very close observation.
THE BIRTH OF ART
327
In the grotto of La Greze overhanging the Beune, a small
tributary of the Vezere, was found an archaic Aurignacian out-
line of the bison deeply incised on the limestone walls. The
grotto of Gargas,* Hautes-Pyrenees,39 is one of the most fa-
mous stations ; it was entered in closing Mousterian times and
was occupied at intervals during the Aurignacian stage. Beneath
the Mousterian layer is a deep deposit of entire skeletons of the
cave-bear without any traces of human industry. These layers
lie beyond the grotto in the vast foyer which opens above into
Fig. 164. Section of the rock shelter of Laussel, showing the superposed industrial
layers from Acheulean to Solutrean times. After Lalanne.
a great chimney, so that this is one of the true cavern habitations.
The drawings along the walls of the cave include a large number
of figures in a very unequal style, which belong chiefly to middle
and upper Aurignacian times. Among these are two figures of
birds, several mammals, a few primitive drawings of wild cattle,
the bison, the ibex, and numerous representations of the horse.
A long serpentine band of color meanders among some of these
drawings. Most interesting are the silhouettes of the hand in
black and red produced by pressing the hand against the lime-
stone wall and covering the surrounding surface with color. It
would appear that the fingers were mutilated or cut off at the
middle joint, because one, two, three, and four of the fingers are
wanting, but the thumb is never mutilated. This mutilation
* The writer had the privilege of visiting all these caverns in the company either of
Professor Emile Cartailhac, or of the Abbe Breuil.
328
MEN OF THE OLD STONE AGE
of the hand may be compared with similar practices prevailing
among some Australian tribes.
In the cavern of Marsoulas, on the headwaters of the Garonne,
the conditions are altogether different; the parietal art here
represents two cultural stages, the late Aurignacian and the late
Magdalenian. There is a small entrance grotto with two
hearths, corresponding to these
two industries. The entrance
to the cave is well up on the
side of the hill, and the drawings
which belong with the upper
Aurignacian culture are some-
what damaged. Again, we find
designs extending along the wall
below the drawings. There are
numerous outlines of the bison
in black, the entire side of the
body being covered with splashes
of red.
The great abri of Laussel, on
the Beune, was first visited by
the Neanderthals, for there are
two Mousterian layers and
above them two Aurignacian
layers, the lower belonging to
the middle Aurignacian industry
and the upper to the closing
Aurignacian period. This long, overhanging cliff of Laussel is a
typical shelter, first sought in Acheulean times, revisited in
Mousterian times, then again in middle or late Aurignacian, in
Solutrean, and finally in Magdalenian times. As these succes-
sive layers rise they approach the shelter of the cliff, so that
the Magdalenian flint workers were directly beneath the over-
hanging rock shelter, which opened outward toward the sun.
In the upper Aurignacian layer Lalanne discovered two bas-
reliefs representing the figures of a man and of a woman. The
Fig. 165. Bas-relief of a woman with a
drinking horn, sculptured on the face
of a boulder within the shelter of Laus-
sel, and attributed to the late Aurig-
nacian. After Lalanne. About one-
eighth actual size.
THE BIRTH OF ART
329
bas-relief of the woman represents a nude figure holding the
horn of a bison in the right hand ; this is cut from a block of
limestone with a relief of about two centimetres, and it measures
forty-six centimetres in height ; with the exception of the head,
the entire body is polished, and at certain points there remain
traces of red coloring. A little
farther on the artist had modelled
the figure of a man in three-
quarter view in the attitude of
casting a spear or of an archer
drawing the bow; the top of the
head and the extremities of the
limbs have been broken away ; the
figure measures forty centimetres
in height. These bas-reliefs of
Laussel are regarded as sincere rep-
resentations, for the artist has pre-
sented as accurately as possible the
contemporary human figure ; both
the man and the woman are rep-
resented in motion. On the tech-
nique employed in this primordial
sculpture, Doctor Lalanne observes
that we find at Laussel a series of
tools perfectly adapted to attain
this result, many of which would
have been inexplicable unless found
to occur in connection with the
sculpture itself. It is curious to note how many analogies there
are between the flint utensils of the primitive sculptor and those
of the sculptors of our own day. First, we find tools designed
to remove the rock, there are points, pickaxes, chopping tools
for shaping the rock, saws, and coarse stone planers ; all of
these are perfectly adapted to the hand, from which we may
conclude that our artist was right-handed. There is a great
number of graving-tools, or burins, all forms being represented
Fig. 166. Bas-relief of a spear
thrower or hunter, sculptured on
the face of a boulder within the
shelter of Laussel. After Lalanne.
About one-sixth actual size.
330 MEN OF THE OLD STONE AGE
— plain, double, fine, coarse, and combinations of the burin and
grattoir. Some of the burins show the sharp-angled point cen-
tred at the extremity of a blade ; these are the ordinary types ;
but in many the blade ends with a terminal retouch, which
may be transverse, oblique, concave, or convex with the point
to one side. The grattoirs, or planers, are equally numerous,
with examples of all the known forms. Many of these are
formed at the end of a blade ; a few are circular, and others are
at the opposite end of a pointed blade ; the latter are particu-
larly fine and are retouched around the entire edge. But the
artist did not merely carve his subjects; he also coated them
with a paint made of ochre and manganese ; he crushed his
coloring matter on a palette of schist, and we have found one
of these unbroken and still bearing the red and ochre colors.
This palette is io>^ inches long and 6 inches wide ; it is oblong
in form.
Distribution of the Solutrean Industry
The period of the Solutrean industry is one of the most diffi-
cult to interpret in the whole prehistory of western Europe.
The remains of this industry in several localities lie directly be-
tween those of the Aurignacian and the Magdalenian ; in others,
as at Solutre, they directly follow the Aurignacian. There is no
doubt that this represents a very long and a very important
epoch in Upper Palaeolithic development. From the cultural
standpoint it represents a climax in the flint industry, but a
period of suspension or of arrested development in art.
A glance at the maps of the Mousterian (Fig. 125), the Aurig-
nacian (Fig. 153), and the Solutrean (Fig. 167) culture stations
shows that the geographic distribution of the Solutrean is en-
tirely unique ; whereas the Aurignacian culture may be said to
girdle the Mediterranean, both on its southern and northern
coasts, the Solutrean culture is absent in this entire region. The
interpretation of this strange phenomenon offered by Breuil,
that the Solutrean culture entered Europe directly from the
east and not from the south, may be connected with the theory
ORIGIN OF THE SOLUTREAN CULTURE
331
that toward the end of Aurignacian times a new race from the
central east was working westward through Hungary and along
the Danube — a race of inferior mental type, but extremely ex-
pert in fashioning the flint spears and lances with what is known
as the Solutrean 'retouch.' This may be the race of Brtinn,
|® CEREMONIAL BURIALS \
1- Gorge d>Enfer
7- Les£y;ies
Z- Laugerie Basse
8- Liveyre
3- Laugerie Haute
9- Rey
4-Le Ruth
10- La Griie
5- Crd-Magnon
H- Moulin de Laussel
fi- Palaud
12- Laussel
| • X HUMAN FOSSILS]
Fig. 167. Geographic distribution of the principal Solutrean industrial stations in
western Europe.
Briix, and Pfedmost, the remains of which are found in two
localities associated with these highly perfected flint spear heads.
Either by the invasion of this race or, more probably, by the in-
vasion of the highly perfected spear-head industry itself, the type
station of Solutre, on the Saone, was established and the region
of Dordogne reached, where this industry progressed at twelve
different stations.
There is no doubt whatever that the new and entirely dis-
tinct Brunn race penetrated the Danubian region at this time,
332 MEN OF THE OLD STONE AGE
but there is no evidence from skeletal remains that it reached
France. It is quite possible that some of the flint workers adept
in the Solutrean 'retouch' migrated into the far western sta-
tions of Dordogne, bringing with them their beautiful technique,
but without leaving traces of their skeletal remains through
ceremonial burial. This unsettled problem affords one of the
many reasons why the anatomy of all the Upper Palaeolithic
men of western Europe should be most carefully studied and
compared.
Another mystery of Solutrean times is the arrest of the ar-
tistic impulse which had animated the Cro-Magnons through-
out the entire Aurignacian. Evidences of artistic work in Solu-
trean times are very rare, and some drawings which have been
attributed to the Solutrean, as at Altamira, have now been re-
ferred to the Magdalenian. Is it possible that the Cro-Magnon
race for a time suspended its artistic endeavor only to renew
it under the different conditions of environment of Magdale-
nian times? Unfortunately, the Solutrean burials afford very
little evidence on this point. One interpretation which may be
offered is that the Solutrean was evidently a period of open-air
life, and that the new implements of the chase of Solutrean
type absorbed the industrial energies of these people, for the
weapons were fashioned in enormous numbers. Consistent with
this theory of climatic influence is the fact that the return of
the severe climate of Magdalenian times, which crowded the
men again into the shelters and grottos, was accompanied by a
renewal of the artistic development continuing from the point
where it had been interrupted in closing Aurignacian times.
That Aurignacian and Magdalenian art is the work of one race
there can be no question whatever; that this race was the
Cro-Magnon is now absolutely demonstrated.
The climate of Solutrean times is generally believed to have
been cold and dry. In the region of Dordogne throughout this
period the reindeer was still far more numerous than any other
animal; so we may safely conclude that this was the principal
object of the chase and of food ; in fact, it would appear that the
HUMAN FOSSILS 333
reindeer were resident forms in the valley of the Vezere, hunted
and consumed throughout the year.40 Here we also occasionally
find the northern steppe or Obi lemming, an animal which at the
same time extends along the borders of the Volga River toward
southern Russia. It would appear that in Solutrean times in
southwestern France there prevailed a dry, cold continental
subarctic climate like that of the Caspian, Volga, and Ural steppes
of the present day. With the mammoth and the reindeer occur
a great variety of northern European forest forms — the true fox,
the hare, the stag, the brown bear, the wolf, the bison, and the
urus. Most interesting is the identification of the jackal belong-
ing to the ancient species C. neschersensis. In the type indus-
trial locality of Solutre the reindeer is very abundant in the
fire-hearths associated with the lower Solutrean industry, but
less abundant in the upper levels; an antelope, perhaps the
saiga antelope, is said to be found among the crude engravings
on bone.
Solutrean Races
There were certainly two distinct races of men in Europe
during Solutrean times, to the east the race of Brunn and to
the west the race of Cro-Magnon. Remains attributed to the
Cro-Magnons have been found in the Departments of Charente,
Gironde, Lot, Haute- Garonne, Tarn, and Dordogne. But most
of these remains are very fragmentary and cannot readily be
determined racially. The fragments of ten skulls and a few other
bones found, in the Grotte du Placard, Charente, are attributed
to late Solutrean and to early Magdalenian times and consti-
tute one of the most exceptional discoveries which have thus
far been made in France ; the interments probably date from
the early Magdalenian (p. 380), but are probably of a race
surviving from the Solutrean. The section of the cave deposit
is from 23 to 26 feet in thickness and is highly instructive ; it
shows eight cultural layers, separated by layers of debris and
succeeding each other in the following order:
334 MEN OF THE OLD STONE AGE
8. Neolithic layer.
7-4. Magdalenian layers; in the lowest layer is the ceremonial burial
of four skulls.
3. Solutrean layer with shouldered points {pointes a cran) and a few
laurel-leaf points {pointes de lanrier).
2. Solutrean layer with laurel-leaf points but no shouldered points;
knives, grattoirs, scrapers, borers, in great numbers, together with javelin
points and awls in bone and ornamented with notches, and fragments of
red chalk and black lead found embedded with the Solutrean points.
1. Mousterian layer.
Race of Brunn, Brux, Predmost, and (?) Galley Hill
In 187 1 a skullcap, now in the Royal Museum of Vienna, was
discovered in the course of coal mining at Brux, Bohemia. In
1 89 141 a skeleton, apparently of the same race, was discovered
at Brunn, Moravia, deeply embedded in loess along with bones
of the woolly mammoth and other great Pleistocene mammals.
In 1892 it was described by Makowsky,42 who a few years be-
fore had excavated from the loess sand in the neighborhood of
Briinn the fragmentary skull now known as Briinn II. Both
these skulls are of a somewhat low racial type, and for a long
time they were regarded as transition forms between the Nean-
derthals and Homo sapiens, but in 1906 Schwalbe43 showed the
affinity between the skulls of Brux and Briinn and at the same
time their entire distinctness from the Neanderthal skull and
their approach to lower forms of Homo sapiens. The chief dis-
tinction of these skulls is their extreme elongation or dolicho-
cephaly, the ratio of width to length being 69 per cent in the
Brux skull, and 68.2 per cent in the Briinn skull. The latter
ranks lower in racial type than the Australian negroids. The
chief distinction from the Neanderthal skull is in the index of
the height of skull (51.22 per cent) and in the absence of the
prominent ridges extending across the eyebrow region above
the nose ;* the forehead, in brief, is more modern, the frontal
* Despite Schwalbe's statement, the supraorbital ridges in this skull appear to form a
complete bridge. Doctor Hrdlicka regards the related Predmost skull as distinctly show-
ing Xeanderthaloid affinity.
THE BRtTNN RACE
335
angle being 74.7-75 per cent. The brain capacity in this race
is estimated, according to Makowsky,44 at 1,350 c.cm. Both
the Briix and Briinn skulls are harmonic ; they do not present
Fig. 168. The type skull known as Briinn I — supposed male — discovered at Briinn,
Moravia, in 189 1. It was found deeply imbedded in loess along with bones of the
woolly mammoth, woolly rhinoceros, giant deer, reindeer, and other Pleistocene
mammals, and is believed to be of Solutrean age. After Makowsky. One-third
life size.
the very broad, high cheek-bones characteristic of the Cro-
Magnon race, the face being of a narrow, modern type, but
not very long. There is evidence that the neck and shoulders
336
MEN OF THE OLD STONE AGE
were powerful and muscular; the prominence of the chin is
pronounced ; the dentition is macrodont, that is, the last lower
molar is of exceptionally large size ; there was no prognathism
or protrusion of the jaws. The second Brtinn skull (Briinn II)
may represent a female type of the Briinn race, the cephalic
index being estimated at 72 per cent.
DISCOVERIES CHIEFLY OF THE CRO-MAGNON AND BRUNN RACES*
Referred to Solutrean Times
Date of
Discovery
Locality
Number of Individuals
Culture Stage
Cro-Magnon Race ( ?)
Grotte du Placard,
Fragments of ten skulls
Late Solutrean and
Charente, France.
and a few other bones.
early Magdale-
nian.
Pair-non-Pair,
Skull fragments.
Solutrean.
Gironde, France.
Lacave,
(( (C
"
Lot, France.
Montconfort,
" "
«
Haute- Garonne, France.
Roset,
('( 11
Late Solutrean.
Tarn, France.
Badegoule,
Bones.
Solutrean.
Dordogne, France.
Brunn-Brux-I
Predmost Race
1880.
Predmost,
Portions of twenty skel-
Solutrean.
Moravia, Austria.
etons.
1891.
Briinn,
Male skeleton (Briinn I) .
"
Moravia, Austria.
(?) Female skeleton
• (Briinn II).
Ballahohle,
Skeleton of infant.
(?) «
Miskolcz, Hungary.
( ?) Galley Hill.
One skeleton.
Unknown.
* Obermaier,45 R. Martin.46
There is a possibility47 that the Briinn race was ancestral
to several later dolichocephalic groups which are found in the
region of the Danube and of middle and southern Germany.
Schliz characterizes the Briinn skull as distinguished by the
retreating forehead, by massive eminences above the orbits sep-
arated by a cleft in the median line, by broad, low orbits, and
prominent chin. These characters are met with again in one
of the dolichocephalic skulls found in the interment at Ofnet,
THE BRtFNN RACE 337
at the very close of Upper Palaeolithic times. It would thus
appear that the Brunn race is distinct from the Cro-Magnon
race, that it represents a long-headed type which became estab-
lished along the Danube as early as Solutrean times, and that
it may possibly be connected with the introduction of some of
the peculiar features of the Solutrean culture.
One of the skeletons of Brunn, found at a depth of 12 feet
below the surface of the 'loess/ was lavishly adorned with
tooth-shells, perforated stone discs, and bone ornaments made
from the ribs of the rhinoceros or mammoth and from the teeth
of the mammoth; associated with these was an ivory idol, ap-
parently of a male figure, of which only the head, the torso, and
the left arm remain. The skeleton and many of the objects
found with the sepulture were partly tinted in red. An ivory
figurine belongs to the Eburneen stage of Piette and appears
to indicate that the burial was of Aurignacian rather than of
Solutrean age.
The Pfedmost ' mammoth hunters' also probably belonged
to this race. They are represented by the remains of six indi-
viduals excavated since 1880 at Predmost, Moravia, by Wankel,
Kfiz, and Maska. The bones were found in a very much shat-
tered condition. Maska has since discovered a collective burial
of fourteen human skeletons, with remains of six others; the
bodies were covered with stones, but no flints or objects of art
were buried with them. The dimensions of the limbs indicate
a race of large stature. The skeletons were deeply buried in
' loess/ and above and below the rich archaeological layer were
abundant debris of the mammoth, representing between eight
and nine hundred specimens. Along with the numerous flints,
including laurel-leaf spear heads of middle Solutrean type, were
found other objects and even primitive works of art in bone and
ivory. There is no question that the human remains belong to
the middle Solutrean stage.48
With this race is also associated by many authors (Schwalbe,
Schliz, Klaatsch, Keith) the Galley Hill skull, which was found
in 1888, buried at a depth of 8 feet in the 'high terrace' gravels
338 MEN OF THE OLD STONE AGE
90 feet above the Thames.49 Sollas thinks it highly probable
that the remains were in a natural position and of the same age
as the high-level gravels and the Palaeolithic flints and remains
of extinct animals which they contained, but Evans and Dawkins
regard the Galley Hill man as belonging to a long-headed Neo-
lithic race interred in a Palaeolithic stratum. The gravels of the
'high terrace' in which the Galley Hill skull was buried are by
no means of the geologic antiquity of 200,000 years assigned
to them by Keith;50 they are probably of Fourth Glacial or of
Postglacial age, and lie within the estimates of Postglacial time,
namely, from 20,000 to 40,000 years.
The antiquity of the Galley Hill cranial type has been main-
tained with ability by Keith. The skull is extremely long or
hyper dolichocephalic, the cephalic index being estimated by
Keith at 69 per cent;51 the brain capacity is estimated at be-
tween 1,350 c.cm. and 1,400 c.cm. ; the cheek-bones are not
preserved, so that no judgment can be formed as to this most
distinctive character of the Cro-Magnon race. With this Gal-
ley Hill race Keith also compares the Combe- Capelle, or Aurig-
nacian man of Klaatsch,52 although he mistakenly considers the
Combe- Capelle man of much less geologic antiquity. He con-
tinues: "Thus, while the writer is inclined to agree in provi-
sionally assigning the Combe-Capelle man to the Galley Hill
race, he believes that further discoveries will show that the
Combe-Capelle man belongs to a branch marked with certain
negroid features."
SOLUTREAN FLINT INDUSTRY
The 'Solutrean retouch' marks one of the most notable ad-
vances in the technique of flint working ; it is altogether distinct
from the 'Aurignacian retouch,' which is an heritage from the
Mousterian.™ The flint is chipped off by pressure in fine, thin
flakes from the entire surface of the implement, to which in its
perfected form the craftsman can give a thin, sharp edge and
perfect symmetry. This is a great advance on the abrupt Aurig-
SOLUTREAN INDUSTRY
339
nacian retouch, in which the flint is chipped back at a rather
blunt angle to make a sharp edge. According to de Mortillet,
Fig. 169. Typical Solutrean implements of war and chase. After de Mortillet. Pointes
en feuille de laurier, or laurel-leaf points, artistically retouched on both surfaces, at
both ends, and on both borders; regarded by de Mortillet rather as blades of poniards
than as javelin heads. 120. Lozenge-shaped form from the type station of Solutre,
Saone-et-Loire. 121. Elongate form found at Solutre. 122. The largest pointe dis-
covered at Solutre. 123. One of the smallest points found at Solutre. 124. Solutrean
point from Laugerie Haute, Dordogne. 127. Point from Gargas, Vaucluse. 128.
Point of exceptionally fine workmanship. 130. One of eleven very large Solutrean
laurel-leaf points found in a cache at Volgu; probably a votive offering, as the flints
are too slender to be of any use and one at least shows traces of coloring. All the
flints are shown one-quarter actual size, except 129, which is one-half actual size.
the Solutrean method of pressure made possible the execution of
much more delicate work.
The question at once arises, did this industrial advance take
place in France or was it an invention brought from the east?
On this point Breuil observes54 that in the highest Aurignacian
340 MEN OF THE OLD STONE AGE
levels in Belgium, in Dordogne, and at Solutre the Solutrean
technique becomes faintly apparent either in the 'stem' points
{pointes a sole) of Font Robert, La Ferrassie, and Spy or in the
double-edged points tending toward the laurel-leaf type of the
Solutrean, but that all the other implements remain purely
Aurignacian.
Relations and Subdivisions of Solutrean Culture
Lower {Early) Magdalenian.
Prototypes of bone harpoons.
Beginnings of animal sculpture.
Absence of any trace of the laurel-leaf spear heads of Solutrean times.
Upper {Late) Solutrean.
Typical shouldered points {pointes a cran) — elongate flakes worked on
one or both sides and notched. Small laurel-leaf spear heads.
Bone javelin points, awls, and needles, very finely worked. Placard.
Lacave.
Middle {High) Solutrean.
Large 'laurel-leaf spear heads worked on both sides. Climax of Solu-
trean flint industry. Placard.
Lower {Proto-) Solutrean.
Primitive 'laurel-leaf and 'willow-leaf spear heads, most of them
worked on only one side. Grotte du Trilobite.
Transition from Aurignacian.
Pedunculate spear heads {pointes a soie) of primitive Font Robert type.
Climax of human sculpture.
As to the chief source of Solutrean influence, the same au-
thor remarks that, since this culture is entirely wanting in cen-
tral and southern Spain, in Italy, in Sicily, in Algeria, and in
Phoenicia, we should certainly not look to the Mediterranean
for its origin but rather to eastern Europe ; for in the grottos
of Hungary we find a great development of the true Solutrean,
while so far the Aurignacian has not been found here, although
we do find traces of the earlier transitional stages below the
levels of the true laurel-leaf points. We must admit, therefore,
that in all probability the Solutrean culture reached Europe
from the east and that its source is as mysterious as that of
the Aurignacian, which, as we have seen, was of southern and
probably of Mediterranean origin. It is not impossible that the
SOLUTREAN INDUSTRY 341
evolution of the laurel-leaf point took place in Hungary, for
it was certainly not evolved in central or western Europe.
At Pfedmost, in Moravia, we observe an advanced Aurig-
nacian industry which had adopted a Solutrean fashion in its
spear heads. Here the laurel-leaf implements are few, while
the implements of bone are abundant; but in the Solutrean
stations of Hungary there are no bone implements. As the Solu-
trean technique comes to perfection the laurel-leaf spear head,
so characteristic of the full Solutrean industry, is created and
is met with in Poland, in Hungary, in Bavaria, and then in
France, where the industry extends southward to the west and
east of the central plateau. In France it appears quite sud-
denly in the Grotte du Trilobite (Yonne), and also in Dordogne
and Ardeche, where the Proto-Solutrean types show marked
impoverishment, both in the variety and in the execution of
most of the flint implements, the only exception being the flat-
tened spear heads, pointes a face plane, which show a regular
Solutrean retouch, beautiful but monotonous. Laurel-leaf points
discovered at Crouzade, Gourdan, and Montfort denote the
presence of the true Solutrean culture, but this culture does not
approach the stations in the neighborhood of Brassempouy.
Toward the north the grotto of Spy, in Belgium, affords ex-
amples of Proto-Solutrean types, which have also been traced
in several British caverns, but it is not certain that true Solu-
trean implements are found in Britain.
In Picard a Proto-Solutrean layer has been found, but no
laurel-leaf points. In the type station of Solutre in south-
eastern France Breuil discovered two Solutrean layers, quite
different from each other : one rich in bone implements and
graving-tools, with small flint laurel leaves retouched on only
one face; the other poor in bone implements but with large
laurel-leaf spear heads.
The Solutrean culture never penetrated to the south of the
great barrier of the Pyrenees, but, passing through the Vezere
valley, in Dordogne, it spread along the western coast to the
northern slopes of the Cantabrian Mountains into the province
342
MEN OF THE OLD STONE AGE
of Santander, Spain. Here the laurel-leaf points of the middle
Solutrean are found at Castillo, while the shouldered points,
pointes a cran, typical of the later Solutrean, are found at Al-
tamira, together with bone implements. None the less, it should
be noticed that in the southwest of Europe the earlier phases
Fig. 170. The type station of Solutrean culture, near the present village of Solutre, in
south central France, sheltered on the north by a steep roCKy ridge and with a
fine sunny exposure toward the south.
of the Solutrean are characterized by a decrease in the use of
bone, which, however, increases again in the upper levels.
The type station of the Solutrean culture is the great open-
air camp of Solutre, near the Saone, sheltered on the north by a
steep ridge and with a fine, sunny exposure toward the south.
The traces of this great camp, which is the largest thus far dis-
covered in western Europe, cover an area 300 feet square and
are situated within a short distance of a good spring of water.
As explored, in 1866, by Arcelin,65 Ferry, and Ducrost, this sta-
tion had already been occupied in Aurignacian times; and two
SOLUTREAN INDUSTRY
343
sections, taken at two different points, showed the deposits of
the old camp to be from 22 to 26 feet in thickness, representing
superposed Aurignacian and Solutrean fire-hearths with thick
layers of intermediate debris. In the Aurignacian level is found
the vast accumulation of the bones of horses already described.
Fig. 1.71. Centre of the great open camp of Solutre, covering an area 300 feet square, with
the village of Solutre in the distance. First occupied in Aurignacian times, and a favorite
and densely inhabited camp throughout the Aurignacian and Solutrean stages. In Aurig-
nacian times the remains of thousands of horses were accumulated around this station.
In the middle Solutrean levels great fireplaces are found with
flint utensils and the remains of abundant feasts among the
charred debris. The fauna includes the wolf, the fox, the hy-
aena, both the cave and the brown bear, the badger, the rab-
bit, the stag, wild cattle, and two characteristic northern forms
— the woolly mammoth and the reindeer ; the remains of the
last are the most abundant in the ancient hearths.
In all the Solutrean stations, beside the bone implements,56
we find two distinct classes of flints. The first belongs to the
entire 'Reindeer Epoch' and consists of single and double
344 MEN OF THE OLD STONE AGE
scrapers, drills, burins, retouched flakes, and plain ones of
small dimensions.
The second is composed of the 'leaf types, which are solely
characteristic of the Solutrean and which degenerate and entirely
disappear at its close ; these latter are the arrow and lance head
forms, many of which are fashioned with a rare degree of per-
fection and exhibit the beautiful broad Solutrean retouch across
the entire surface of both sides of the flake, together with per-
fect symmetry, both lateral and bilateral; they are commonly
known as the willow-leaf (narrow) and the laurel-leaf (broad)
forms. The explorers of the type station of Solutre have dis-
covered five principal shapes, as follows : (i) irregular lozenge ;
(2) oval, pointed at both ends; (3) oval, pointed at one end;
(4) regular lozenge ; (5) arrow-head form with peduncle, doubt-
less for attachment to a shaft. The perfected Solutrean laurel-
leaf spear heads do not reappear in any other Upper Palaeolithic
period, but their resemblance to Neolithic flints is very marked.
The ' willow-leaf ' spear heads {pointes de saute) , chipped on
only one side, characteristic of the early Solutrean, may possibly
be contemporary with the closing Aurignacian culture of Font
Robert. At Solutre layers have also been discovered rich in
bone implements and in graving-tools, as well as small 'laurel-
leaf points worked on only one face. As regards the general
tendencies of the early Solutrean culture in Dordogne, at the
Grotte du Trilobite (Yonne), and in Ardeche, there is a marked
decline in the work in bone and in the variety and workmanship
of all the implements, excepting only that of the primitive
flattened spear heads, made of flakes, retouched in Solutrean
fashion, but on one side only. Typical deposits of early Solu-
trean culture are found at Trou Magrite, in Belgium, at Font
Robert, Correze, and in the third level of the Grotte du Trilo-
bite, Yonne ; in the second level we find flints with the nascent
Solutrean retouch.
The distinctive implement of the 'high' or middle Solutrean is
the large 'laurel-leaf point, flaked and chipped on both sides and
attaining a marvellous perfection in technique and symmetry.
SOLUTREAN INDUSTRY 345
The finest examples of these spear heads are the famous pointes
de laurier, fourteen in number, discovered at Volgu, Saone-et-
Loire, in 1873 : they were found together in a sort of cache and,
it would seem probable, were intended as a votive offering, for
one at least was colored red, and all were too fragile and delicate
to be of any use in the chase. They are of unusual size, the
smallest measuring 9 inches, and the largest over 13^. In
workmanship they are equalled only by the marvellous Neolithic
specimens of Egypt and Scandinavia.
At Solutre and other stations implements of bone are also
found, although by no means of such frequent occurrence as in
the later divisions of the Solutrean. While the most easterly
Solutrean stations of Hungary exhibit no bone implements,
these are abundant at Pfedmost, in Moravia, where the culture
altogether is of an advanced Aurignacian type, with the Solu-
trean retouch used in the shaping of its flint spear heads. The
bone industry includes a number of awls and smoothers, as well
as numerous ' batons de commandement.' On this level at
Pfedmost a few works of art are found consisting of the rep-
resentations of four animals sculptured on nodules of lime-
stone, the subjects apparently being reindeer, and also of one
single engraving on bone.
The chief invention of the late Solutrean is the ' shouldered
point' (pointe a cran), a single notched and very slender dart.
These notches are the first indication of the value of the barb
in holding a weapon in the flesh. Here also is a stem for the at-
tachment of the shaft of the dart. In earlier stages of the Solu-
trean one finds flints where the unsymmetrical base of the 'point'
shows a small obtuse tongue or stem. The elongate peduncle at
the base of such spear heads (pointes a sole) is developed into the
pointe a cran, or shouldered point, made of long, fine flakes,
with a short retouch on one or both sides, and found in the late
Solutrean at the grotto of Lacave, at Placard, and at many of
the stations in Dordogne. No example of the pointe a cran
has ever been found at the type station of Solutre, but it is of
frequent occurrence at the stations between the Loire and the
346
MEN OF THE OLD STONE AGE
Cantabrian Pyrenees, being found at Altamira, at Laugerie
Haute, at Monthaud (Indre), in Chalosse and Charente, while
the great cave of Placard has yielded no less than 5,000 speci-
mens, whole and broken.
Fig. 172. Typical Solutrean implements of the chase, of fishing, and of industry. After
de Mortillet. 131,132. A laurel-leaf point retouched on both sides. 133-138. Various
forms of the pointe a cran, or 'shouldered point,' a type distinctive of the late Solutrean.
It has an elongated peduncle or stem at one side adapted for the attachment of a wooden
shaft, and was probably an implement of the chase, being suitable for fishing or for
hunting small game. The examples figured show a great variety of finish and retouch.
137 is from Placard and 138 from the Grottes de Grimaldi. 139. Poincon, or awl, beau-
tifully shaped. 140. Per coir, drill or borer. 141. Flake retouched on one border, re-
calling the style of the Aurignacian points. 142, 143. Finely retouched points, suit-
able for engraving or etching. All the flints are shown one-half actual size.
At Monthaud there are also found bone implements in-
cluding a number of poinqons (awls) and a series of sagaies
(javelin points). Solutrean sagaies, however, are very rare and
very primitive as compared with the Magdalenian.
SOLUTREAN ART 347
The successive phases of Solutrean industry are all shown in
southern France. As to its stratigraphic relations, the type
station of Solutre exhibits lower and middle Solutrean above
Aurignacian hearths and deposits; that of Placard, Charente,
shows the middle and upper Solutrean overlaid by a Magdale-
nian layer. In the Grotte du Trilobite the Solutrean layer lies
between one of Aurignacian and one of primitive Magdalenian ;
it is here that we find the clearest transition from the Aurig-
nacian culture in the appearance of prototypes of the laurel and
willow-leaf points, made of flakes, retouched on only one side.
At Brassempouy the Solutrean lies immediately beneath a Mag-
dalenian layer, with engraved bones and Magdalenian flints.
Needles, which are particularly abundant in the Magdalenian
epoch, are also found in a number of the Solutrean stations.
In the grotto of Lacave, Lot, in an upper Solutrean layer, Vire
has found beautiful bone needles, pierced at one end and of fine
workmanship, and engraved utensils of reindeer horn ; here also
was found the head of an antelope engraved on a fragment of
reindeer horn. The local fauna of this period included the horse,
the ibex, and the reindeer.
Solutrean Engraving and Animal Sculpture
The artistic work of Solutrean times is not so rich as that of
the Aurignacian. This, as we have suggested, may be partly
attributable to the less wide-spread distribution of the Solu-
trean culture, as well as to the great importance which was at-
tached to the careful fashioning of the stone weapons. None
the less we can trace indications of the development of both
phases of art, the linear and the plastic, and especially the begin-
nings of animal sculpture. From the full, round sculpture of
Aurignacian times there follows in Solutrean times a develop-
ment of carving in bone of the Rundstabfiguren (baton, or cere-
monial staff), and of high relief. The Hon57 and the head of a
horse at Isturitz, in the Pyrenees, which Breuil attributes to a
late Solutrean period, are typical examples of this work.
348 MEN OF THE OLD STONE AGE
Relatively rare are the parietal and mobile engravings as well
as the schematic representations, such as are found at Placard
and Champs Blancs. According to Alcalde del Rio, there are
found at Altamira, in northern Spain, very simple, finely en-
graved figures of the doe on the bone of the shoulder-blade ; the
head and neck are covered with lines, and both the eye and the
nostril as well as the form of the ear are very characteristic of
the animal. Breuil, however, considers these as belonging rather
to earlier Magdalenian times.
Decorative art certainly makes some advances over the Au-
rignacian work, because the arrangement of the geometric figures
is quite clear, and the execution shows marked progress in the
technique of engraving.
At Pfedmost, near the site of the human burial described
above, there has been discovered a statuette of the mammoth
sculptured in the round, in ivory, which proves that animal
sculpture was well advanced in Solutrean times. The statuette
was found six to nine feet beneath the surface of the 'loess,' in
an undoubted Solutrean layer. The accompanying fauna is of
a truly arctic character: the mammoth being extraordinarily
abundant; the tundra forms including the mammoth, woolly
rhinoceros, musk-ox, reindeer, arctic fox, arctic hare, glutton,
and banded lemming ; the Asiatic forms including the lion and
leopard; the forest and meadow fauna embracing the wolf,
fox, beaver, brown bear, bison, and wild cattle, moose, and
horse, also the ibex. Among the remnants of 30,000 flints there
are a dozen points (feuilles de laurier) and other pieces with the
Solutrean 'retouch.' The industry in ivory, bone, and reindeer
horn is also varied, including numerous poniards, polishers,
piercers, dart-throwers, and batons de commandement.
This ivory sculpture of the mammoth indicates very accu-
rately the characteristic contours of the top of the head, and of
the back ; the striations on the side represent the falling masses
of hair. Other sculptured figures representing the mammoth are
believed to be of Magdalenian age, the best known being the
figures found in the grottos of Bruniquel and Laugerie Basse,
SOLUTREAN ART 349
a fragment from Raymonden, Dordogne, and a bas-relief in the
grotto of Figuier, Gard. All these sculptures of the mammoth
have in common the indication of a very small ear — similar to
that in the Pfedmost model — feet shaped like inverted mush-
rooms, bordered with short, coarse hairs, the tail terminating in
Fig. 173. Mammoth sculptured on a fragment of ivory tusk from the Solutrean station
of Predmost, Moravia. After Maska. This figure is covered with fine lines repre-
senting the long, hairy coating, and measures about four and one-half inches.
a long tuft of hairs. If the figure of Pfedmost is of Solutrean
age, it is by far the earliest of all the sculptured or engraved
animal representations in the mobile art, and is also the most
complete of the animal figurines of this group. It is certainly
of more recent date than the engraved designs of Aurignacian
age in the grottos of Gargas and of Chabot or than the red or
black tracings of the mammoth, also of Aurignacian age, at
Castillo, Pindal, and Font-de-Gaume. It is probable that the
mammoth figures of Combarelles are of later date than the
Pfedmost sculpture and belong to the beginning of Magdalenian
times, while those at Font-de-Gaume belong to the end of Mag-
350
MEN OF THE OLD STONE AGE
dalenian times and are the most recent of all the parietal designs.
Despite the differences in age and technique, all the designs of the
mammoth are undoubtedly the work of artists of a single race ;
they agree in faithfully portraying the external form of this great
proboscidian which wandered over the steppes and prairies of
western Europe from the beginning of the fourth glaciation until
near the close of Postglacial times.
(i) Breuil, 191 2.7.
(2) Verneau, 1906. 1, pp. 202-207.
(3) Op. cit., p. 204.
(4) Keith, 1911.1, p. 60.
(5) Obermaier, 1912.1, p. 178.
(6) Breuil, 191 2. 7, p. 174.
(7) Op. cit.f pp. 165-168.
(8) Obermaier, 191 2.1, pp. 177, 178.
(9) Wiegers, 1913.1.
(10) Schmidt, 1912.1, p. 266.
(11) Geikie, 1914.1, p. 278.
(12) Dawkins, 1880.1, pp. 148, 149.
(13) Ewart, 1904. 1.
(14) Obermaier, 1909.2, p. 145.
(15) Sollas, 1913.1, p. 325-
(16) Broca, 1868.1.
(17) Lartet, 1875. 1.
(18) Verneau, 1886. 1; 1906. 1, pp. 68,
69.
(19) Obermaier, 191 2.2.
(20) Martin, R., 1914.1, pp. 15, 16. (49)
(21) Keith, 1911.1, p. 71.
(22) Klaatsch, 1909. 1.
(23) Keith, op. cit., p. 56.
(24) Hauser, 1909. 1.
(25) Fischer, 1913.I;
(26) Schliz, 1912.1, p. 554.
(27) Breuil, 1912.7, p. 175.
(28) Op. cit., p. 183.
(29) Op. cit., pp. 177-180.
(30) Schmidt, 191 2.1, p. 266.
(31) Breuil, op. cit., p. 178.
(32) Obermaier, 1912.1, p. 181.
(33) Breuil, 191 2.7, p. 169.
(34) Breuil, 191 2.1, pp. 194-200.
(35) Schmidt, 1912.1.
(36) Breuil, op. cit.
(37) Schmidt, 1912.1, p. 142.
(38) Breuil, 1912.1, p. 202.
(39) Breuil, 1912.6.
(40) Hilzheimer, 1913.1, p. 151.
(41) Fischer, 1913.1.
(42) Makowsky, 1902. 1.
(43) Schwalbe, 1906. 1.
(44) Makowsky, op. cit.
(45) Obermaier, 1912.1, pp. 342-355-
(46) Martin, R., 1914.1, pp. 15, 16.
(47) Schliz, 1912.1.
(48) Dechelette, 1908. 1, vol. I, p.
28.
Keane, 1901.1, p. 147.
(50) Keith, 1911.1, p. 30.
(51) Op. cit., pp. 28-45.
(52) Op. cit., pp. 51-56.
(53) Obermaier, 191 2.1, p. 93.
(54) Breuil, 1912.7, p. 188.
(55) Arcelin, 1 869.1.
(56) Dechelette, 1 908.1, vol. I, pp.
i37-i4i-
(57) Schmidt, 191 2.1, p. 144, Tafel B.
CHAPTER V
MAGDALENIAN TIMES — CLIMATE AND^ MAMMALIAN LIFE OF EUROPE
— CUSTOMS AND LIFE OF THE CRO-MAGNONS ; THEIR INDUSTRY
IN FLINT AND BONE; THEIR DISTRIBUTION — DEVELOPMENT OF
THEIR ART, ENGRAVING, PAINTING, SCULPTURE — ART IN THE
CAVERNS — CLIMAX OF THE MAGDALENIAN ART AND INDUSTRY OF
THE CRO-MAGNONS — APPARENT DECLINE OF THE RACE.
The art and industrial epoch of Magdalenian times is by far
the best known and most fascinating of the Old Stone Age.
This period forms the culmination of Palaeolithic civilization;
it marks the highest development of the Cro-Magnon race pre-
ceding their sudden decline and disappearance as the dominant
type of western Europe. The men of this time are commonly
known as the Magdalenians, taking their name from the type
station of La Madeleine, as the Greeks in their highest stage
took their name from Athens and were known as the Athenians.
We would assign the minimum prehistoric date of 16,000
B. C. for the beginning of the Magdalenian culture, and since
we have assigned to the beginning of the Aurignacian culture
the date of 25,000 B. C, we should allow 9,000 years for the
development of the Aurignacian and Solutrean industries in
western Europe.
Introduction. Industrial and Artistic Development
Well as this culture is known, its origin is obscured by the
fact that it shows little or no connection with the preceding
Solutrean industry, which, as we have noted (p. 331), seems like
a technical invasion in the history of western Europe and not
an inherent part of the main line of cultural development. Thus
Breuil1 observes that it appears as if the fundamental elements
of the superior Aurignacian culture had contributed by some
351
352 MEN OF THE OLD STONE AGE
unknown route to constitute the kernel of the Magdalenian
civilization while the Solutrean episode was going on elsewhere.
Again, early Magdalenian art bears striking resemblances to the
superior Aurignacian art of the Pyrenees, especially the parietal
art, as shown by comparing the Aurignacian engravings of Gar-
gas with the early Magdalenian of Combarelles. Moreover, the
same author observes that, if there is one certain prehistoric
fact, it is that the first Magdalenian culture was not evolved
from the Solutrean — that these Magdalenians were newcomers
in western France, as unskilful in the art of shaping and retouch-
ing flints as their predecessors were skilled. Ancient Magda-
lenian hearths are found in many localities close to the levels of
the upper Solutrean industries with their shouldered spear
points (pointes a cran) and highly perfected flint work. Yet the
Magdalenians show a radical departure from the Solutrean type
of flint working ; both in Dordogne (Laugerie Haute and Laus-
sel) and in Charente (Placard) the splinters of flint are massive,
heavy, badly selected, often of poor quality, and poorly retouched,
sometimes almost in an Eolithic manner ; at the same time, the
chance flints, that is, the piercers and graving- tools made from
splinters of any accidental shape, are abundant. To these peo-
ple flint implements appear to be altogether of secondary im-
portance ; although the flints are very numerous, they are not
finished with any of the perfection of the Solutrean technique ;
the laurel-leaf spear head and shouldered dart head have disap-
peared entirely, but a great variety of smaller graving and chas-
ing forms are employed for fashioning the implements of bone
and horn. What a contrast to the beautiful flints so finely re-
touched and of such carefully selected materials, found in the
very same stations in middle and upper Solutrean layers!
Thus Breuil, always predisposed to believe in an invasion of
culture rather than in an autochthonous development, favors
the theory of eastern origin for the Magdalenian industry, be-
cause this is not wanting either in Austria or in Poland ; two
sites of ancient Magdalenian industry have been found by Ober-
maier in the ' loess' stations of Austria, while in Russian Poland
ORIGIN OF THE MAGDALENIAN CULTURE 353
the grotto of Maszycka, near Ojcow, exhibits workings in bone
resembling those found at the grotto of Placard, Charente, in the
layers directly succeeding the base of the Magdalenian. The
fact that near the Ural Mountains there has also been found a
peculiar Magdalenian culture, the origin of which is not western,
inclines us to believe that the Magdalenian culture extended from
the east toward the west, and then, later, toward the Baltic.
This theory of the eastern origin of the Magdalenian industry
has, however, to face, first, the very strong counter-evidence of
Fig. 174. One of the large bison drawings in the cavern of Niaux, on the
Ariege, showing the supposed spear or arrow heads with shafts on its side.
The artist's technique consists of an outline incised with flint followed by
a painted outline in black manganese giving high relief. After Cartailhac
and Breuil. Greatly reduced.
the close affinity between Aurignacian and Magdalenian art,
which Breuil himself has done the most to demonstrate ; second,
the physical, mental, and especially the artistic unity of the Cro-
Magnon race in Aurignacian and Magdalenian times. The
recent discovery of two Cro-Magnon skeletons together with two
carved bone implements of Magdalenian type, at Obercassel,
on the Rhine, links the art with this race and with no other, be-
cause, as we remarked above, an artistic "instinct and ability
cannot be passed from one race to another like the technique of
a handicraft. Breuil2 himself has positively stated that the
whole Upper Palaeolithic art development of Europe was the
work of one race : if so, this race can be no other than the Cro-
Magnon.
We must, therefore, revert to the explanation offered in a
preceding chapter, that the Solutrean technique was an intrusion
354
MEN OF THE OLD STONE AGE
or an invasion either brought in by another race or acquired
from the craftsmen of some easterly race, perhaps that of Briinn,
Briix, and Pfedmost. Why the art of fashioning these perfect
Solutrean spear, dart, and arrow heads was lost is very difficult
to explain, because they appear to be the most effective imple-
ments of war and of the
chase which were ever
developed by Palaeo-
lithic workmen.
It is possible, al-
though not probable,
that the bow was in-
troduced at this time
and that a less perfect
flint point, fastened to
a shaft like an arrow-
head and projected with
great velocity and ac-
curacy, proved to be far
more effective than the
spear. The bison in the
cavern of Niaux show
several barbed points
adhering to the sides,
and the symbol of the
fleche appears on the sides of many of the bison, cattle, and other
animals of the chase in Magdalenian drawings. From these
drawings and symbols it would appear that barbed weapons of
some kind were used in the chase, but no barbed flints occur at
any time in the Palaeolithic, nor has any trace been found of
bone barbed arrow-heads or any direct evidence of the existence
of the bow.
In compensation for the decline of flint is the rapid develop-
ment of bone implements, the most distinctive feature of Mag-
dalenian industry. In the late Solutrean we have noted the
occasional appearance of the bone javelin points (sagaies) with
Fig. 175. Decorated sagaies, or javelin points, of
bone; pointed at one end and bevelled at the
other for the attachment of a shaft. After Breuil.
MAGDALENIAN CULTURE
355
their decorative motifs; these become much more frequent in
Magdalenian times. They occur in the most ancient Magda-
lenian levels of the grotto of Placard, Charente, which are prior
even to the appearance of prototypes of the harpoon, the evolu-
tion of which clearly marks off the early, middle, and late divi-
sions of Magdalenian times. These primitive javelins, decorated
Fig. 176. Head of the forest or of the steppe horse engraved on a fragment
of bone, from the Grotte du Pape, Brassempouy. After Piette.
in a characteristic fashion, are found in Poland, at the grotto of
Kesslerloch and other places in Switzerland, at many stations in
Dordogne and the region of the Pyrenees in southern France,
and in the Cantabrian Mountains of northern Spain.
It is only above the levels where early types of these javelin
points occur that the rudimentary harpoons of the typical early
Magdalenian are found. The discovery of the bone harpoon as
a means of catching fish marks an important addition to the food
supply, which was apparently followed by a decline in the chase.
Later, to the javelin, lance, and harpoon is added the dart-
thrower (propulseur) , which gradually spreads all over western
356 MEN OF THE OLD STONE AGE
Europe, where also the evolution of these bone implements and
of the decoration with which they are richly adorned enables
the trained archaeologist to establish corresponding subdivisions
of Magdalenian time.
From the uniform character of Palaeolithic art in its highest
forms of engraving, painting, and animal sculpture we may infer
the probable unity of the Cro-Magnon race, especially throughout
western Europe. During Magdalenian times various branches
of art reached their highest point and were the culmination of
Fig. 177. Polychrome wall-painting of a wolf from the cavern of Font-de-Gaume.
After Breuil.
a movement begun in the early Aurignacian. The artist, whose
life brought him into close touch with nature and who evidently
followed the movements both of the individual animals and
of the herds for hours at a time, has rendered his observations in
the most realistic manner. Among the animals represented are
the bison, mammoth, wild horse, reindeer, wild cattle, deer, and
rhinoceros ; less frequent are representations of the ibex, wolf,
and wild boar, and there are comparatively few representations
of fishes or of any form of plant life ; the nobler beasts of prey,
such as the lion and the bear, are often represented, but there are
no figures of the skulking hyaena, which at that time was a rare
if not almost extinct animal. While many figures are of real
MAGDALENIAN CULTURE
357
artistic worth and reach a high level, others are more or less
crude attempts ; the composition of figures or of groups of animals
is rarely undertaken.
The artistic sense of these people is also manifest in the deco-
ration of their household utensils and weapons of the chase.
Here the smaller animals of the chase, the saiga, the ibex, and
Fig. 178. Crude sculpture of the ibex, from the Magdalenian deposit at
Mas d'Azil on the right bank of the Arize. After Piette.
A little less than actual size.
the chamois, are executed with a sure hand. Sculpture of animal
forms in the large, which begins in Solutrean times, is continued
and reaches its highest point in the early Magdalenian. At this
period the use of sculpture as a means of decoration arises and
extends into the middle and late Magdalenian. These latter
divisions are also distinguished by the reappearance of human
figurines, nude, like the Aurignacian, and occasionally somewhat
more slender. Thus it would appear that the artistic spirit,
more or less dormant in Solutrean times, was revived.
358 MEN OF THE OLD STONE AGE
In the variety of industries we find evidences of a race en-
dowed with closely observant and creative minds, in which the
two chief motives of life seem to have been the chase and the
pursuit of art. The Magdalenian flints are fashioned in a some-
what different manner from the Solutrean : long, slender flakes
or 'blades' with little or no retouch are frequent, and in other
implements the work is apparently carried only to a point where
the flint will serve its purpose. No attempt is made to attain
perfect symmetry. Thus the old technical impulse of the flint
industry seems to be far less than that among the makers of the
Solutrean flints, while a new technical impulse manifests itself
in several branches of art : arms and utensils are carved in ivory,
reindeer horn and bone, and sculpture and engraving on bone
and ivory are greatly developed. We find that these people are
beginning to utilize the walls of dark, mysterious caverns for
their drawings and paintings, which show deep appreciation for
the perfection of the animal form, depicted by them in most life-
like attitudes.
We may infer that there was a tribal organization, and it has
been suggested that certain unexplained implements of reindeer
horn, often beautifully carved and known as 'batons de com-
mandement,' were insignia of authority borne by the chieftains.
There can be little doubt that such diversities of tempera-
ment, of talent, and of predisposition as obtain to-day also pre-
vailed then, and that they tended to differentiate society into
chieftains, priests, and medicine-men, hunters of large game and
fishermen, fashioners of flints and dressers of hides, makers of
clothing and footwear, makers of ornaments, engravers, sculptors
in wood, bone, ivory, and stone, and artists with color and brush.
In their artistic work, at least, these people were animated with
a compelling sense of truth, and we cannot deny them a strong
appreciation of beauty.
It is probable that a sense of wonder in the face of the
powers of nature was connected with the development of a re-
ligious sentiment. How far their artistic work in the caverns
was an expression of such sentiment and how far it was the
Pl. VII. Cro-Magnon man in the cavern of Font-de-Gaume, Dordogne, restored in the
act cf drawing the outlines of one of the bisons on the wall of the Galerie des Fresques.
Drawn under the direction of the author by Charles R. Knight.
MAGDALENIAN CULTURE
359
outcome of a purely artistic impulse are matters for very care-
ful study. Undoubtedly the inquisitive sense which led them
into the deep and dangerous recesses of the caverns was accom-
panied by an increased sense of awe and possibly by a senti-
ment which we may regard as more or less religious. We may
dwell for a moment on this very interesting problem of the
Fig. 179. Decorated batons de commandement carved from reindeer horn with a large
perforation opposite the brow tine. After Lartet and Christy.
origin of religion during the Old Stone Age, so that the reader
may judge for himself in connection with the ensuing accounts
of * Magdalenian art.
"The religious phenomenon/ ■ observes James,3 "has shown
itself to consist everywhere, and in all its stages, in the conscious-
ness which individuals have of an intercourse between them-
selves and higher powers with which they feel themselves to be
related. This intercourse is realized at the time as being both
active and mutual. . . . The gods believed in — whether by
crude savages or by men disciplined intellectually — agree with
each other in recognizing personal calls. . . . To coerce the
spiritual powers, or to square them and get them on our side,
was, during enormous tracts of time, the one great object in our
dealings with the natural world."
360 MEN OF THE OLD STONE AGE
The study of this race, in our opinion, would suggest a still
earlier phase in the development of religious thought than that
considered by James, namely, a phase in which the wonders of
nature in their various manifestations begin to arouse in the
primitive mind a desire for an explanation of these phenomena,
and in which it is attempted to seek such cause in some vague
supernatural power underlying these otherwise unaccountable
occurrences, a cause to which the primitive human spirit com-
mences to make its appeal. According to certain anthropolo-
gists,* this wonder-working force may either be personal, like
the gods of Homer, or impersonal, like the Mana of the Mel-
anesian, or the Manitou of the North American Indian. It
may impress an individual when he is in a proper frame of
mind, and through magic or propitiation may be brought into
relation with his individual ends. Magic and religion jointly
belong to the supernatural as opposed to the every-day world
of the savage.
We have already seen evidence from the burials that these
people apparently believed in the preparation of the bodies of
the dead for a future existence. How far these beliefs and the
votive sense of propitiation for protection and success in the
chase are indicated by the art of the caverns is to be judged in
connection with their entire life and productive effort, with
their burials associated with offerings of implements and arti-
cles of food, and with their art.
The Three Climatic Cycles of Magdalenian Times
The culture of the Cro-Magnons was doubtless influenced
by the changing climatic conditions of Magdalenian times, which
were quite varied, so that we may trace three parallel lines of
development: that of environment, as indicated by the climate
and the forms of animal life, that of industry, and that of art.
The entire climatic, life, and industrial cycle of which the
* From notes by Doctor Robert H. Lowie (Nov. 16, 1914) of the American Museum
of Natural History on the opinions of Marett (Anthropology) and of James.
MAGDALENIAN CLIMATE 361
Magdalenian marks the conclusion has been presented in Chapter
IV (p. 281). After a very long period of cold and somewhat arid
climate following the fourth glaciation, it would appear that west-
ern Europe in early Magdalenian times again experienced a stage
of increasing cold and moisture accompanied by the renewed
advance of the glaciers in the Alpine region, in Scandinavia,
and in Great Britain. This is known as the Buhl stage in the
Alps, in which the snow-line descended 2,700 feet below its
present level and the great glaciers thrust down along the south-
erly borders of Lake Lucerne a series of new moraines distinctly
overlying those of the fourth glaciation. Another indication of
the lowered temperature and increased moisture in the same
geographic region is found in the return of the arctic lemmings
from the northern tundras ; these migrants have left their re-
mains in several of the large grottos north of the Alps, espe-
cially in Schweizersbild and Kesslerloch, composing what is
known as the Upper Rodent Layer, with* which are associated
the implements and art objects of the early Magdalenian cul-
ture stage.
We have adopted the minimum estimate of 25,000 years
since the fourth glaciation, but Heim4 has estimated that the
much more recent prehistoric event of the advance of this minor
Buhl glaciation began at least 24,000 years ago, that it extended
over a very long period of time, and that the Buhl moraines in
Lake Lucerne are at least 16,000 years of age.
The three climatic changes of Magdalenian times are there-
fore as follows :
First, the Buhl Postglacial Stage in the Alps, which corre-
sponds with what Geikie has named the Fifth Glacial Epoch,
or Lower Turbarian, in Scotland ; for he believes that a relapse
to cold conditions in northern Britain was accompanied by a
partial subsidence of the coast lands, that snow-fields again
appeared, that considerable glaciers descended the mountain
valleys, and even reached the sea. At this time the arctic
alpine flora of Scotland also descended to within 150 feet of the
sea-level. The result of this renewed or fifth glaciation in
362
MEN OF THE OLD STONE AGE
western Europe was the advent of the great wave of tundra
life and the descent to the plains of all the forms of Alpine life.
Second, it would appear that in middle Magdalenian times,
after the Buhl advance, there occurred a temporary retreat of
the ice-fields, and that during this period the full tide of life from
the steppes of western Asia and eastern Europe for the first time
^POSTGLACIAL )
*^s^%*&
"i\k
J
-i^-e-
4^
^ ' I
i
Ml
yj
%^^^^ul
|
\
Ny/i'
3-?
■d&ml rl
mm
•SKS^
fj i)ti//'
S^ /:.
< X,:,„y^ -
Ia
,1! ip"
; \.X~*~
— =
N^
Fig. 184. Heads of four chamois engraved on a fragment of reindeer horn, from the
grotto of Gourdan, Haute-Garonne. After Piette.
(Alces), indicated by the artists of Aurignacian times as present
in the Cantabrian Pyrenees.
It is the above entire Eurasiatic forest and meadow fauna
which survived all the climatic vicissitudes of Pleistocene time,
and which alone remained in western Europe to the very close
of the Upper Palaeolithic culture, and into the period of the
arrival of the Neolithic race.
The descent of the European and Asiatic alpine types of mam-
mals to the lower hills and valleys is one of the most striking
episodes of Magdalenian times. The argali sheep (Ovis arga-
loides) of western Asia had already appeared in the upper Danu-
bian region during the Aurignacian; it is replaced in Magda-
lenian times by the ibex (Ibex priscus), and by the chamois,
which descended along the northern slopes of the Alps and of
the Pyrenees, and became numbered among the most highly
favored subjects of the Magdalenian artists, especially in the
370 MEN OF THE OLD STONE AGE
mobile art of ivory and bone, and in the decoration of their
spear throwers and batons de commandement. From the moun-
tains also come the pikas or tailless hares (Lagomys pusillus),
the alpine marmot (Arctomys mar motto), the alpine vole (Arvi-
cola nivalis), and the alpine ptarmigan (Lagopus alpinus).
The Tundra Climate or Early Magdalenian Times
In the first cold moist period the full wave of arctic tundra
life appeared in the whole region between the Alpine and Scan-
dinavian glaciers during the renewed descent of the ice-fields;
this was the tundra stage of early Magdalenian times, accom-
panying the Buhl advance. At the stations of Thaingen, Schwei-
zersbild, Kastlhang, and Niedernau, appears the musk-ox, to-
gether with the woolly mammoth, the woolly rhinoceros, and the
reindeer. The discovery of the grotto of Kastlhang, a reindeer
hunting station in the Altmuhltale of Bavaria6 fills out what
has long been a gap in the geographic distribution of the early
Magdalenian. The principal objects of the chase here were
the reindeer, the wild horse, the arctic hare, and the ptarmi-
gan ; the royal stag is very rare, and the bison is wanting en-
tirely; a strong arctic character is given to the fauna by the
presence of the banded lemming, the arctic wolverene, and the
arctic fox. From this region the musk-ox migrated far to the
southwest, reaching the northern slopes of the Pyrenees. At
the same time the arctic grouse, the whistling swan, and other
northern birds entered the region of the Rhine and the Dan-
ube. But the surest indicators of a cold tundra climate pre-
vailing during the period of the Buhl advance are the banded
lemming (Myodes torqualus) and the Obi lemming (Myodes oben-
sis), which are found in the same deposits with the arctic hare,
the reindeer, and the woolly mammoth mixed with the imple-
ments of the early Magdalenian industry at the stations of
Sirgenstein, Wildscheuer, and Ofnet along the upper and mid-
dle Danube. There also appear the ermine and the arctic wol-
verene ; in fact, almost all the characteristic forms of tundra
■^ijki. -
©:
^.*n~
Fig. 185. Characteristic forms of alpine life, which descended from the mountains or
migrated from the highlands of western Asia in Aurignacian and Magdalenian times:
the ibex, the chamois, the alpine ptarmigan, the argali sheep, and the (A) alpine vole,
all shown one-twenty-fifth life size; and the (.4) alpine vole also one-fifth life size.
372 MEN OF THE OLD STONE AGE
life except the polar bear, which only enters the northern tun-
dras in the summer season.
The regions of the northern Alps bordering the great gla-
ciers of the Bilhl and Gschnitz advances, were barren stretches
of rock, and the valleys and plateaus now free from ice became
tundras, where the swamps alternated with patches of polar wil-
lows and stunted fir-trees, while other areas were covered with
low, scrubby birches, or reindeer moss and lichens. The return
of these hard conditions of life undoubtedly exerted a great in-
fluence both upon the physical and mental development of the
Cro-Magnon race ; it was at the very period when the life con-
ditions in western Europe were most severe that the artistic de-
velopment of these people began to revive. Forced to return to
the shelters and grottos, which certainly were less frequented
in Solutrean times, there was time for the development of the
imagination and for its expression both in the mobile and parietal
arts. There was a less vigorous development of the flint indus-
try, and apparently a degeneration in physique and stature.
In Germany and northern Switzerland, on the headwaters of
the Rhine and the Danube, the entrance and departure of the
northern waves of life are recorded, especially in the grottos of
Sirgenstein, Schussenquelle, Andernach, Schmiechenfels, and
Propstfels. It would appear that the woolly mammoth and the
woolly rhinoceros were not hunted in this region, for their remains
are not preserved in any of the grottos or stations mingled with
the middle or late Magdalenian cultures. On the other hand,
we find the steppe horse, the kiang, the stag, and the reindeer
very abundant indeed. The bison is absent, and wild cattle
are very rare ; so that this region is not typical of the mammalian
life of Magdalenian times as found in Dordogne and in the
Pyrenees.
The migration of the woolly mammoth and woolly rhinoceros
along the Pyrenees and westward into the Cantabrian Moun-
tains, and the crossing of the Pyrenees by the reindeer, have
already been described. In the mural frescos of Font-de-Gaume,
Dordogne, it is noteworthy that the very latest engravings are
MAMMALIAN LIFE 373
those of the mammoth superposed on the fine polychromes
which belong to the period of middle Magdalenian art.
The Dry Steppe Climate of Middle Magdalenian
Times
The cold, dry period, when the full tide of steppe life reached
western Europe, is of somewhat uncertain date; it probably
began during the stage of the middle Magdalenian industry and
continued into the late or high Magdalenian. There was cer-
tainly an environment attractive to these peculiar and very
highly specialized mammals, which at the present time are neu-
tral in color, swift of foot, inured to existence on very sparse vege-
tation, and adapted to extremes of heat and cold. Among the
smaller steppe forms were the suslik or pouched marmot of the
steppes (Spermophilus rufescens) and the steppe hamster (Cricetus
phceus)j also the Siberian vole (Arvicola gregalis) ; still more
characteristic was the great jerboa (Alactaga jaculus) , with long,
springy hind legs, and the saiga antelope (Antilope saiga). With
these mammals appeared the steppe grouse (Perdix cinerea),
which is found along the Danube in late Magdalenian strata;
another bird characteristic of the northern steppes and tundras
is the ' woodcock owl' (Brachyotus palustris). Accompanying
these mammals was undoubtedly the steppe horse (Equus przewal-
ski), now restricted to the desert of Gobi; it is said to occur in
the grottos of northern Switzerland.
It would appear that the saiga antelope may have reached
eastern Europe in late Solutrean times, for its outline is said to
be found in an engraving at Solutre. Widely spread over Europe
was the giant Elasmothere ; it would seem very unlikely that
this animal was present in Magdalenian times, for it certainly
would have attracted the attention of the artists. Neither have
we any positive artistic records of the wild ass, or kiang, although
certain of the drawings in the grottos of Niaux and Marsoulas,
of the middle Magdalenian, also of Albarracin, in Spain, may be
interpreted as representing this animal. Thus the Asiatic steppe
and desert fauna, which in the region of the upper Rhine and
Fig. 186. Steppe mammals from the steppes and deserts of Asia, which invaded western
Europe in Upper Palaeolithic times; the first arrivals appearing during the cold, dry
period of late Acheulean times, becoming more numerous in the dry period of Aurig-
nacian and Solutrean times, and completely represented in Magdalenian times. The
saiga antelope, the (A) steppe hamster, the (B) great jerboa, and the kiang, or Asiatic
wild ass, are all shown one-twenty-fifth life size. The (^4) steppe hamster is also shown
one-fifth life size and the (B) great jerboa one-twelfth life size. Drawn by Erwin S.
Christman.
MAMMALIAN LIFE
375
Danube was restricted to two species of mammals in Aurignacian
and Solutrean times, rises to nine or ten species in middle Mag-
dalenian times, so that for the first time during the entire 'Rein-
deer Epoch' the steppe and tundra faunae are equally balanced.
There are also six or seven species of birds from the moors and
uplands of central Asia. The bird life
depicted in middle Magdalenian art
includes the ptarmigan or grouse, the
wild swan, geese, and ducks.
The present flora of the subarctic
steppes in southeastern Russia and
southwestern Siberia includes forests
of pine, larch, birch, oak, alder, and
willow, extending along the banks of
the rivers and streams and inter-
spersed with broad, low, grassy plains.
There are many gradations between
the low and high steppes;7 the cli-
mate in summer is relatively warm,
the temperature rising to 700, while
the average temperature in mid-winter
hardly exceeds 300 ; in general there is FlG- l87- Ptarmigan, or grouse,
, , - carved in reindeer horn, from
a strong contrast between the summer Mas d'Azii After Piette. The
and Winter Seasons, the Steppe lands restored portions (head and feet)
are indicated by dotted lines.
in summer are practically rainless, so
that the sand and dust rise with every wind. Thus, both in
summer and winter sand and dust storms play an important
role. The great snow-storms of the subarctic steppes are as
destructive as those of the more northerly tundras and often
result in great loss of life. Numerous discoveries tend to prove
that similar conditions prevailed in western Europe during Mag-
dalenian times. Thus at Chateauneuf-sur-Charente, a mingled
tundra and steppe fauna is found containing the bones of many
young animals which must have perished during a blizzard. It
will be recalled that in this region is the station of Le Placard
of late Solutrean and Magdalenian age. Near Wiirzburg, Ba-
376 MEN OF THE OLD STONE AGE
varia, there is a fauna buried in the 'loess' containing twenty
species of mammals of the tundras and steppes, together with
the bison and the urus.8
Perhaps the strongest proof of the extension of cold, dry-
steppe conditions of climate is the migration of the saiga ante-
lope (Saiga tartarica) into the Dordogne region, where it is rep-
resented both in carvings and engravings, and into other parts
of southwestern France, where its fossil remains have been found
in thirteen localities in association with a cold steppe fauna.
In the same region have been found the remains of the musk-ox
(Ovibos), one of the most distinctive members of the arctic
fauna.
Human Races or Magdalenian Times
It appears that the Cro-Magnon race continued to prevail,
yet anthropologists have long been divided in opinion as to the
racial affinity of the men found in the Magdalenian industrial
stage. The most famous burials are those of Laugerie Basse
and Chancelade in Dordogne, each consisting of skeletons of in-
ferior stature, not improbably belonging to women. They cer-
tainly represent a race somewhat different from the typical
Cro-Magnons of Aurignacian times, as found at Cro-Magnon
and in Grimaldi. The archaeologist de Mortillet referred both
these skeletons to a new race, the race de Laugerie. Schliz, who
has most recently reviewed this subject, has, however, rightly
treated all these people as Cro-Magnons of a modified type.
The Magdalenian skeleton of Laugerie Basse, found by Mas-
senat in 1872, was resting on the back, with the limbs flexed,
and with it was a necklace of pierced shells from the Mediter-
ranean : the body apparently had been covered with a layer
of Magdalenian implements. According to the length of the
femur, the individual was 1.65 m., or 5 feet 1 inch in height;
the bones were strong and compact; the skull was well arched,
with a straight forehead and a cephalic index of 73.2 per cent.
The so-called Chancelade skeleton was found in the shelter
of Raymonden in 1888, at a depth of 5 feet, and was also in a
HUMAN FOSSILS
377
folded position, resting directly on the rock and covered with
several layers of artifacts of the later Magdalenian culture ; the
limbs were so tightly flexed as to prove that they had been en-
veloped in bandages. This skeleton shows a well-arched skull,
a high, wide forehead, and a dolichocephalic head form, but
the limbs are comparatively small, the height not exceeding
W&fflMWiMr :&
f
W$k '"■ t*B
Bill
■ ' ^ ''*
**3*-^--. ^W'"
"
Ljr
■§
' jH
1 , fSi
1 '■'"' x'
uc
Fig. i88. The a&n of Laugerie Basse, Dordogne, a famous Magdalenian station and
burial site of the skeleton of Laugerie Basse. This ancient rock shelter, like that of
Cro-Magnon and many others, shows at the present day a cluster of peasants' dwell-
ings around its base. Photograph by Belves.
1.50 m., or about 4 feet 7 inches; the upper arm and thigh
are short, compact, and clumsy, and the femur is crooked with
comparatively thick ends ; this skeleton is generally classed with
the Cro-Magnon race, but Klaatsch considers that it may be-
long to a distinct type. We cannot disregard, says Breuil,9 the
anatomical characters attributed by Testut to the man of Chance-
lade and its resemblances to the actual Eskimo type ; this indi-
cation is in favor of a new element, arriving perhaps from Asiatic
Siberia, but acquiring in western Europe the, artistic culture
378
MEN OF THE OLD STONE AGE
realized and conserved in certain districts by the Aurignacian
tribes and their derivatives. All of the Aurignacian, Solutrean,
and Magdalenian races, however, recall very forcibly the race
of Cro-Magnon, which tends to prove that these transformations
in culture were not made without a notable element of human
continuity.
DISCOVERIES OF MAGDALENIAN AGE CHIEFLY ATTRIBUTED TO
THE CRO-MAGNON RACE*
Date of
Discovery
Locality
Nature of Remains
1863.
Bruniquel (Tarn-et-Garonne, France).
Skeletal fragments. Burial.
1864.
La Madeleine (Dordogne, France).
Skeletal fragments.
1869.
Laugerie Basse I (Dordogne, France).
Skeletal fragments.
1871.
Gourdan (Haute-Garonne, France).
Skeletal fragments.
1872.
Laugerie Basse II (Dordogne, France).
1 skeleton. Burial.
1872-1873.
Sorde (Duruthy) (Landes, France).
1 skeleton. Burial.
1874.
Freudenthal (near S chaff hausen, Swit-
zerland).
Fragments of skulls and of pelvis.
1874.
Kesslerloch (near Thaingen, Switzer-
land).
Collar-bone.
1883.
Le Placard (Charente, France).
8 skulls, chiefly fragmentary.
1888.
Chancelade (Raymonden) (Dordogne,
France).
1 skeleton, almost complete. Burial.
1894.
Les Hoteaux (Ain, France).
1 skeleton, almost complete. Burial.
1914.
Obercassel (near Bonn, Germany).
2 skeletons, male and female, almost
complete. Burial. Early Magda-
lenian.
Les Eyzies (Dordogne, France).
Skeletal fragments.
La Mouthe (Dordogne, France).
1 tooth, 1 vertebra.
Limeuil (Dordogne, France).
Skull fragments.
Grotte des Hommes (Yonne, France).
3 skulls and other skeletal fragments.
Brassempouy (Landes, France).
2 teeth.
Grotte des Fees (Gironde, France).
Fragments of upper and lower jaw.
Lussac (Vienne, France).
Fragment of lower jaw.
Mas d'Azil (Ariege, France).
1 skull top. Early Magdalenian.
Lourdes (Hautes-Pyrenees, France).
Skull fragments.
Castillo (Santander, Spain).
Skull fragment. Early Magdalenian.
Gudenushohle (Austria).
1 infant's tooth.
Andernach (north of Koblenz, Ger-
2 child's incisors and 7 rib fragments.
many).
After Obermaier,10 R. Martin,11 and others.
Another Magdalenian burial is that at Sorde, Landes, in the
grotto of Duruthy; this skeleton was discovered in 1872, buried
at a depth of 7 feet, the body being ornamented with a neck-
lace and a girdle of the teeth of the lion and of the bear, pierced
and engraved. Seven skulls found in 1883 in the grotto of
Placard, Charente, also belong to the Magdalenian. The
HUMAN FOSSILS 379
skeleton discovered in 1894 in the grotto of Les Hoteaux, Ain,
was buried at a depth of 6 feet beneath Magdalenian imple-
ments ; the body, resting on the back, was covered with red
ochre ; the thigh-bones were inverted, indicating that the limbs
had been dismembered before burial — a custom observed among
certain savages.
These are the best preserved Magdalenian remains which
have been discovered in France up to the present time. The
Fig. 189. Human skull-tops cut into ceremonial or drinking bowls, from the
Magdalenian layer of Placard, Charente. After Breuil and Obermaier.
matter of chief significance is the survival of modes of burial
characteristic of the Cro-Magnons in Aurignacian times, with the
use of color and of ornaments and with the body in some instances
folded and bandaged.
In the great grotto of Placard, near Rochebertier, Charente,
a new feature in the mode of interment has been discovered — the
separation of the head from the body.* The previous ceremonial
burials, which began certainly among the Neanderthals in Mous-
terian times, always show the custom of burying the entire body ;
in the Upper Palaeolithic there commences the new custom of
imbedding the body in ochre or red coloring matter, and this
* This custom is observed again in Azilian times in the burials at Ofnet on the
Danube (see page 475).
380 MEN OF THE OLD STONE AGE
obtains from the Aurignacian burials of Grimaldi to the Azilian
burial of Mas d'Azil. The flexing of the limbs occurs fre-
quently in Upper Palaeolithic times. It would appear as if the
new ceremonial of Placard had been introduced in the earliest
Magdalenian times, for in the lowest Magdalenian layers four
skulls were found closely crowded together, with the top of the
cranium turned downward; of other portions of the skeleton only
a humerus and a femur were found. In an upper layer of the same
industrial stage a woman's skull and jaw were found, surrounded
by snail shells, many of them perforated. Still more singular is
the occurrence in Magdalenian strata of this grotto of two sep-
arate skull-tops, fashioned by some sharp flint implement into
bowls (Fig. 189).
Again, at Arcy-sur-Cure three skulls have been discovered
placed closely together, and with them a flint knife in a layer
superposed upon an Aurignacian industry. The Placard type of
burial of the head only is shown again in the Azilian stage at
Ofnet, Bavaria.
The uncertainty regarding the racial afhnity of the men of
Magdalenian culture has now been entirely removed by the dis-
covery, in February, 19 14, of two skeletons at Obercassel, near
Bonn, the first instance of complete human skeletons of Quater-
nary age being found in Germany.12 As reported by Verworn,13
the skeletons lay little more than a yard apart ; they were cov-
ered by great slabs of basalt, and lay in a deposit of loam deeply
tinged with red. This red coloring matter, which extended com-
pletely over the skeletons and surrounding stones, indicates
that it was a ceremonial burial similar to that practised by the
Aurignacian Cro-Magnons. Along with the skeletons were found
bones of animals and several specimens of finely carved bone,
but no flint implements of any kind. The bone implements
include a finely polished 'lissoir' of beautiful workmanship,
placed beneath the head of one of the skeletons; the handle
is carved into a small head of some animal resembling a marten ;
the sides show the notched decoration so typical of the French
Magdalenian. The second specimen of carved bone is one of
HUMAN FOSSILS
381
the small, flat, narrow horse-heads, engraved on both sides,
such as are found at Laugerie Basse and in the Pyrenees. One
of the skeletons is of a woman about twenty years of age, and,
as is usual in young female skeletons, it exhibits the racial char-
acters in a much less marked degree than the male skeleton,
which belongs to a man of between forty and fifty years; the
cephalic index is 70 per cent; the supraorbital ridges are well
developed, and the orbits are distinctly rectangular; the limb
bones indicate a body about 155 cm., or 5 feet 1 inch, in height.
Fig.
190. The skulls of two skeletons of the Cro-Magnon race, one male (right) the
other female (left) , recently discovered at Obercassel near Bonn, associated
with Magdalenian implements. After Bonnet.
In contrast to this more refined skull, the extremely broad
and low face of the man is entirely disproportionate to the mod-
erately broad forehead and well rounded skullcap ; the breadth
of the face is 153 mm. and exceeds the greatest width of the
skull, which is only 144 mm. This is a markedly disharmonic
type, the width of the face being due not only to the broad upper
jaw but to the exceptional size and breadth of the cheek-bones.
The skull is decidedly dolichocephalic, the cephalic index being
74 per cent ; the brain capacity is about 1,500 c.cm. ; the orbits
are rectangular, and above them extends an unbroken supraor-
bital ridge, with a slight median frontal eminence ; the nasal
opening is relatively small ; the lower jaw has a strongly marked
chin ; the crowns of the teeth have been worn down until the
382 MEN OF THE OLD STONE AGE
enamel has almost disappeared. While the muscular attachments
indicate great bodily strength, the height does not exceed 5 feet
3 inches. As pronounced Cro-Magnon features, both of the
Obercassel skulls show an unusually wide face ; in both the pro-
files are straight and the root of the nose depressed, the nose is
narrow, and the orbits are rectangular. But, observes Bonnet,
the greatest width of these skulls is not found across the parietals,
as in the typical Cro-Magnons, but just above the ear region, a
much lower position; in this respect the Obercassel skulls re-
semble the skull of the Chancelade skeleton.
This very important discovery of two undoubted descendants
of the Cro-Magnon race associated with bone implements of
lower Magdalenian workmanship appears to prove conclusively
that the Cro-Magnons were the art-loving race. The Obercassel
skeletons confirm the evidence afforded by the burials in France
that these people were of low stature ; perhaps because of the
severe climatic conditions of Magdalenian times they had lost
the splendid physical proportions of the Cro-Magnons living
along the Riviera in Aurignacian times. The skull also, while
retaining all the pronounced Cro-Magnon characters, had under-
gone a modification in the point of greatest width.
In the reduction of the stature of the woman to 5 feet 1 inch
and of the man to 5 feet 3 inches, and in the reduction of the
brain capacity to 1,500 c.cm., we may be witnessing the result
of exposure to very severe climatic conditions in a race which
retained its fine physical and mental characteristics only under
the more genial climatic conditions of the south.
The Four Industrial Phases of Magdalenian Culture
The industrial development belongs throughout to central
and western Europe rather than to the Mediterranean. It is
remarkable that it does not extend along the African coast, or
even into Italy or southern Spain. It has been found to present
four great steps or phases as follows :
The earliest types 14 of the incipient Magdalenian culture or
MAGDALENIAN INDUSTRY
383
Proto-Magdalenian, are nowhere better represented than under
the great shelter of Placard, in Char en te, where the deep succes-
sive deposits compel a realization of the long period of time re-
quired for the evolution of the Magdalenian with its wonderful
artistic culmination. Even prior to any discovery of the harpoon
or of any example of the art of engraving comparable to the
Fig. 191. The great abri, or rock shelter, of La Madeleine, type station of the Magda-
lenian industry. Ruins of the abbey beyond. Photograph by Belves.
classic series of higher levels we find three levels of incipient
Magdalenian industry at Placard. Similar local horizons, recog-
nizable from the type of their javelin points (sagaies) and from
their decorative motifs, are also found at Kesslerloch, Switzer-
land, and as far east as Poland. From Dordogne they extend
into the Pyrenees and into the Cantabrian Mountains of northern
Spain, but not farther south. There is thus a very primitive
Magdalenian industry wide-spread over central and western
Europe, either autochthonous or influenced from the east, but
certainly not from the Mediterranean. It is only above these
384 MEN OF THE OLD STONE AGE
primitive horizons that layers are discovered with the rudimentary
harpoons, and then with the perfected harpoons with single and
double rows of barbs. It would appear as if the basins drained
by the Dordogne and the Garonne were at once the most densely
populated and also the centres from which industry, culture, and
art spread to the east and to the west.
In the heart of the Dordogne region is the great rock shelter
of La Madeleine, the type station of Magdalenian culture, and
around it are no less than fifteen stations. This station, in which
the lowest industrial layer {niveau inferieur) is subsequent to the
Proto-Magdalenian phase and belongs to the early Magdalen-
ian, was extensively excavated by Lartet and Christy15 dur-
ing the decade following its discovery, in 1865, and more recently
by Peyrony and others. The industrial deposit is situated at
the base of an overhanging limestone escarpment on the right
bank of the Vezere River; it extends for a distance of 50 feet
with an average thickness of 9 feet, the lowest or early Mag-
dalenian levels reaching down below the present level of the
Vezere. It is a significant fact that the river floods which from
time to time occur here also occasionally drove out the flint
workers in Magdalenian times. It indicates an unchanged topog-
raphy and similar conditions of rainfall. We must picture this
cliff fringed with a northern flora, these river banks as the haunt
of bison and reindeer, and the site of a long, narrow camp of
skin-covered shelters.
Among the numerous specimens of typical Magdalenian in-
dustry and art which have been found here may be mentioned
a geode of quartzite, apparently used to contain water, and stone
crucibles, usually of rounded form, adapted to the grinding up
of mineral colors for tattooing or artistic purposes; one of
these crucibles, showing traces of color, still remains. The finest
among the art objects is the spirited engraving, on a section of
ivory tusk, of the woolly mammoth charging ; this is one of the
most realistic pieces of Palaeolithic engraving which has ever been
found ; there are indications that the artist used this relatively
small piece of ivory for the representation of three mammoths;
MAGDALENIAN INDUSTRY 385
but in the reproduction (Fig. 199) all the lines are eliminated
except those belonging to the single charging mammoth ; we
observe especially the elevation of the head and the tail, also the
remarkably lifelike action of the limbs and body.
Very numerous industrial levels are discovered in eight or ten
overlying hearths, which are, however, divided into three main
levels, as follows :
Niveau superieur (late Magdalenian culture).
Harpoons with a double row of barbs. Indications that the climate was
colder and drier, resembling that of the steppes. Bison, horses, and
reindeer abundant.
Niveau moyen (middle Magdalenian culture).
Harpoons with barbs on one side only; also batons de commandement.
Indications that the climate was more moist, with frequent inunda-
tions from the river. Bison, reindeer, and horses less abundant.
Niveau inferieur (early Magdalenian culture).
Harpoons with a single row of barbs. Indications of animal sculpture.
Remains of bison and of reindeer, but those of horses especially nu-
merous.
In the Early Magdalenian we note the invention of the
harpoon ; its first crude form is that of a short, straight point of
bone, deeply grooved on one face, the ridges and notches along
one edge being the only indications of what later develop into
the recurved barbed points of the typical harpoon. As noted
above, this invention was destined to exert a very strong influ-
ence on the habits of these people. Large fish undoubtedly were
very abundant in all the rivers at that time, and this new means
of obtaining an abundant food supply probably diverted the
Cro-Magnons in part from the more ardent and dangerous pur-
suit of the larger kinds of game. The discovery soon spread, and
among a number of localities where prototypes of the harpoon
are found may be mentioned Placard, in Charente ; Laugerie
Basse, in Dordogne ; Mas d'Azil, on the Arize ; and Altamira,
in northern Spain. In the early Magdalenian also a great va-
riety of flint drills or borers are developed in connection with
the fashioning of bone, including the * parrot-beak ' type, or
386
MEN OF THE OLD STONE AGE
recurved flint. The microlithic flints, exclusively designed for
fine and delicate artistic work, are more abundant than in any
Fig. 192. Industrial and art implements of Magdalenian times, chiefly elongate flakes
retouched at one or at both ends for various uses. After de Mortillet. 160. Long,
narrow flint blade from the type station of La Madeleine. 161. A similar implement
from the grotto of Mursens, Lot. 162. A 'knife' flake from Laugerie Basse, Dordogne.
163. A flint blade, very characteristic of the period, from La Madeleine. 164. A minute
flake with cutting border and short, curved point. 165. An elongate flake shaped into
a graltoir, or planing tool, at one end, from La Madeleine. 166. An elongate, pointed
graving-tool, retouched at the end and at one side. 167. A pointed tool of chalcedony.
168. A minute pointed flake. 169. A 'parrot-beak' graving-tool of flint. 170. A
straight flint graver, from Les Eyzies, Dordogne. 171. A similar graver, from Lau-
gerie Basse. 172. A similar graver, from La Madeleine. 173. Flint graver with base
retouched, from the Gorge d'Enfer. 174. A double-ended implement, burin and gral-
toir, from Laugerie Basse. 175. Flint burin, or graver, approaching the 'parrot-beak'
type of 169, from Les Eyzies. 176. Double burin, or graver, of flint, from the Grotte
du Chaffaud, Vienne. All figures arc one-third actual size.
previous stage, and were used to shape and finish the bone im-
plements which chiefly distinguish the Magdalenian culture.
Other implements which enable us to recognize the early Mag-
MAGDALENIAN INDUSTRY
387
dalenian culture layers are javelin points of bone or reindeer-
horn with oblique bases, small staves of reindeer-horn or ivory,
oval plates of bone frequently decorated with engraved designs,
and slender, finely finished needles.
The Middle Magdalenian implements were more widely
distributed than the early types, the most characteristic weapon
being the harpoon with a well-defined single row of barbs (Breuil,16
Schmidt17). According to Breuil, this single-rowed harpoon is
Fig. 193. Typical forms of Magdalenian bone harpoons. After Breuil. (^4) 1 to 9,
single-rowed harpoons, characteristic of the early and middle Magdalenian; 1, 4, 8,
from Bruniquel; 2, 5, from Laugerie Basse; 6, from Mas d'Azil; 7, from La Mairie;
3 and 9, from Valle and Castillo. About one-quarter actual size. (B) 10 to 15, double-
rowed harpoons, characteristic of the late Magdalenian; 10, 12, from Bruniquel; 11,
from Massat; 13, from Mouthier; 14, from La Madeleine; 15, from Kesslerloch,
Switzerland. About one- third actual size.
rare in the lower layers but abundant in the upper layers of
middle Magdalenian times ; with it occur examples of the single-
rowed harpoon with swallow-tail base. Other implements of
this stage are the bone javelin points with cleft base, small
bone staves richly decorated, also numerous needles, finer and
more slender than those of the early Magdalenian. It is very
interesting to note that there are no distinctive inventions in
the flint industry, which shows no important advances, although
microlithic flints are still more abundant than before. For in-
dustrial purposes scrapers continue to be very abundant, as
well as borers for the perforation of bone implements. The
388 MEN OF THE OLD STONE AGE
middle Magdalenian industry is best represented in the deposits
of central and southern France, at Raymonden, Bruniquel,
Laugerie Basse, Gourdan, Mas d'Azil, and Teyjat.
The chief weapon of Late Magdalenian times is the harpoon
with the double row of barbs, which is found at all the principal
discovery sites extending from stations in southwestern and
southern France far to the east. Besides the double-rowed
harpoon, the cylindrical chisel of reindeer-horn frequently occurs,
often pointed at the end and with a small curve at the side ; this,
like other bone implements, was richly decorated with engraving.
This late Magdalenian level is distinguished everywhere by the
rich decoration of all the bone implements and weapons, as well
as of the 'batons de commandement.' The quantity of bone
needles, more numerous in this stage than ever before, attests
the greater refinement of finish in the preparation of clothing.
This was the culminating point both in Magdalenian indus-
try and art, and probably also in the morale and modes of living.
Characteristic types of this late Magdalenian culture are found
at La Madeleine, Les Eyzies, and Teyjat, and extend into the
northern Pyrenees, at Lourdes, Gourdan, and Mas d'Azil. Their
easterly geographical distribution will be described on a later
page. The microlithic flints now reach their culminating point;
to the small bladed flakes with blunted backs are added little
feather-shaped flint blades, and still others with oblique ends,
which begin to suggest the geometric forms of the succeeding
Tardenoisian industry. Among the flint borers we notice a
prevalent type with a stout central point, also the so-called
' parrot-beak' borer; for the preparation of skins, scrapers are
made, as before, of thin flakes, slightly retouched at both ends
to give a rounded or rectangular form.
Following the late or high Magdalenian stage is a period of
decline in industry. In southern France18 both flint and bone
implements show unmistakable indications of the approach
either of the succeeding Tardenoisian or Azilian stage. In the
Pyrenees both the flints and the great polishers of deer-horn begin
to resemble those which occur in the post-Magdalenian levels.
MAGDALENIAN INDUSTRY 389
This industrial stage corresponds broadly with the period of
decline in art, and with the change both in the industrial habits
and in the artistic spirit of the Cro-Magnons.
The divisions of the Magdalenian are, therefore, as follows :
5. Decline of the Magdalenian art and industry.
4. Late Magdalenian typified at La Madeleine, Dordogne.
3. Middle Magdalenian typified at La Madeleine, Dordogne.
2. Early Magdalenian typified at La Madeleine, Dordogne.
1. Proto-Magdalenian typified at Placard, Charente.
Flint and Bone Industry
Through the four successive stages of development which we
have already traced (p. 382) there are perceived certain general
tendencies and characteristics which clearly separate the Mag-
dalenian from the preceding Solutrean culture.
Compared with Solutrean times, when the art of flint work-
ing reached its high-water mark, the Magdalenian palaeoliths
show a marked degeneracy in technique, having neither the sym-
metry of form nor the finely chipped surfaces which distinguish
the Solutrean types ; indeed, they do not even equal the grooved
marginal retouch of the best Aurignacian work. The Magdalenian
retouch shows no influence of the Solutrean; it is even more blunt
and marginal than the late Aurignacian. In compensation for
this decadence in the art of retouch, the Cro-Magnons now show
extraordinary skill in producing long, narrow, thin flakes of flint,
struck off the nucleus with a single blow; these 'blades,' which
are very numerous, are often not retouched at all ; occasionally
a few hasty touches are used to attain a rounded or oblique end ;
in other cases a very limited marginal chipping along the sides
or the development of an elongated pedicle {sole) produces very
effective implements for graving and sculptural work.
For the art of engraving perfect burins, burin-grattoirs, and
burins doubles were rapidly made from these thin flakes ; also
burins with oblique terminal edge and with the ' parrot-beak '
end. For industrial purposes some of the flints were denticu-
lated around the border, doubtless for the preparation of fibres
390
MEN OF THE OLD STONE AGE
and of thin strips of leather for the attachment of clothing
to the body and for binding of the flint and bone lance-heads
to wooden shafts. Extremely fine percoirs have been found
adapted to perforating the bone needles ; the grattoir, single
or double, was also fashioned out of these flakes, and the nu-
cleus of the flint was used as a hammer. Hammers of simple
rounded stones are also found.
But the notable feature of Magdalenian industry is the ex-
tensive and unprecedented use of bone, horn, and ivory. From
the antlers of the reindeer are early developed the sagaies or
Fig. 194. Types of the flint blade with denticulated edge, a characteristic
industrial tool of Magdalenian times, from Bruniquel, Les Eyzies, and
Laugerie Basse. After Dechelette, by permission of M. A. Picard, Librai-
rie Alphonse Picard et Fils.
javelin points of varying size, usually ornamented along the sides
and with several forms of attachment to the wooden shaft,
either forked, bevelled, or rounded. The ornamentation consists
of engraved elongate lines or beaded lines, and of deep grooves
perhaps intended for the insertion of poisonous fluids or the out-
let of blood.
Of all the Magdalenian weapons the most characteristic is
the harpoon, the chief fishing implement, which now appears for
the first time marked by the invention of the barb or point retro-
verted in such a manner as to hold its place in the flesh. The
barb does not suddenly appear like an inventive mutation, but
it very slowly evolves as its usefulness is demonstrated in prac-
tice. The shaft is very rarely perforated at the base for the
attachment of a line ; it is cylindrical in form, adapted to the
MAGDALENIAN INDUSTRY
391
capture of the large fish of the streams. That a barbed weapon
was also used in the chase seems to be indicated by drawings
in the grotto of Niaux and lines engraved on the teeth of the
bear, but these drawings indicate the form of an arrow rather
than of a harpoon. The length varies from two to fifteen inches.
The harpoons may have been projected by means of the so-called
propulseurs or dart-throwers, which resemble implements so
10 cm
I
1
s
Fig. 195. Bone needles from the grotto of Lacave, Lot. After Vire.
employed by the Eskimo and Australians of to-day. These
dart-throwers are often beautifully carved, as in the case of one
found at Mas d'Azil, ornamented with a fine relief of the ibex.
Then there were batons de commandement, carved with scenes
of the chase and with spirited heads of the horse and other
animals, which quite probably were insignia of office. Reinach
has suggested that batons were trophies of the chase, and accord-
ing to Schoetensack they may have been used as ornaments to
fasten the clothing. The discovery of mural painting and en-
graving suggests the possibility that these batons were believed
to have some magical influence, and were connected with mys-
terious rites in the caverns, for a great variety of such ceremonial
392 MEN OF THE OLD STONE AGE
staffs is found among primitive peoples. Geographically, the
batons spread from the Pyrenees into Belgium and eastward
into Moravia and Russia.
Slender bone needles brought to a fine point on stone polish-
ers indicate great care in the preparation of clothing. Associated
with the borers are many other bone implements : awls, hammers,
chisels, stilettos, pins with and without a head, spatulas, and pol-
ishers; the latter may have been employed in the preparation
of leather. The borers, pins, and polishers appear from the very
beginning of the period of sculpture. The name of poniard
(poignard) is given to long points of reindeer-horn ; one of these
was found at Laugerie Basse.
History or Upper Paleolithic Art
Following the pioneer studies of Lartet, the history of the
art of the Reindeer Period, as manifested in bone, ivory, and the
engraved and sculptured horns of the deer, occupied the last
thirty-five years of the life of Edouard Piette,19 a magistrate
of Craonne who pursued this delightful subject as an avoca-
tion. He was a pioneer in the interpretation of Vart mobilier, the
mobile art. It must be remembered that in Piette's time the
fourfold divisions of Upper Palaeolithic culture so familiar to us
were only partly perceived ; his studies, in fact, related chiefly to
the mobile art of Magdalenian times, and he undertook to fol-
low its modifications in every successive grotto, beginning with
his brochure La Grotte de Gourdan, in 1873, in which he first an-
nounced the idea which underlay all his later conclusions, that
sculpture preceded line engraving and etching. He divided the
art into a series of phases ; that of the red deer (Cervus elaphus)
he termed Elaphienne, that of the reindeer Tarandienne, that of
the horse Hippiquienne, and that of the wild cattle Bovidienne.
In concluding this early work of 1873, he remarked: "To write
the history of Magdalenian art is to give the history of primi-
tive art itself." He observed that in sculpturing the horn of the
reindeer the artist was obliged to work in the hard exterior bone
and to avoid the spongy interior ; this defect in material suggested
UPPER PALAEOLITHIC ART 393
the invention of the bas-relief. The statuette he regarded as
the assemblage of two bas-reliefs, one on either side of the bone.
Thus he described the ivory head of the woman of Brassempouy,
the only human face of Upper Palaeolithic times which is even
fairly well represented; also the two imperfect feminine torsos
in ivory. In 1897, at the age of seventy, Piette undertook his
last excavations, and the sum of his labors is preserved for us in
the magnificent volume entitled VArt pendant Vdge du Renne,
published in 1907.
The pupil and biographer of Piette, l'Abbe Henri Breuil, ob-
serves that his scheme of art evolution is exact along its main
lines.20 It is true that human sculpture appears for the first time
in the lower Aurignacian, that it survives the Solutrean, and
even extends into middle Magdalenian times, but this enormous
period cannot be placed in one archaeological division as Piette
supposed ; in truth, he did not suspect the prolonged gestation
of Quaternary art, but contracted into one small division the
documents of numerous phases. At the same time, Piette was
right in attributing the flower of the art of engraving accom-
panied by contours of animal forms in relief to the second and
third levels of the Magdalenian industry, but he had no idea
that this development had been preceded by a long period in
which engraving had been practised in a timid and more or
less sporadic manner as a parietal art on the walls of the cav-
erns as well as on bone and stone. It is also true that a con-
siderable facility in sculpture preceded the art of engraving, but
it was arrested in its progress while engraving slowly developed ;
in the early choice of subjects the sculptors of middle and late
Aurignacian times showed a preference for the human form,
while later, in Solutrean and early Magdalenian times, they in-
clined principally toward animal figures, so that sculpture was
not suddenly eclipsed. The first engravings made with fine
points of flint on stone are hardly less ancient than the first sculp-
tures, and modestly co-exist beside them up to the moment
where engraving, greatly multiplied, largely supplants sculpture.
Finally, observes Breuil, it is one of the glories of Edouard Piette
394
MEN OF THE OLD STONE AGE
to have understood that the painted pebbles of Mas d'Azil rep-
resented the last prolongation of the dying Quaternary art.
It is fortunate that the mantle of Piette fell upon a man of
the artistic genius and appreciation of Breuil, to whom chiefly
we owe our clear understanding of the chronological development
of Upper Palaeolithic art. In the accompanying table (p. 395)
are assembled the results of the observations of Piette, Sautuola,
Riviere, Cartailhac, Capitan, Breuil, and many others, largely in
the order of sequence determined through the labors of Breuil.
Fig. 196. Geographic distribution of the more important Palaeolithic art stations of
Dordogne, the Pyrenees, and the Cantabrian Mountains. After
Breuil and Obermaier.
We are far from 1880, observes Cartailhac,21 when the dis-
covery by Sautuola of the paintings on the roof of the cavern of
Altamira was met with such scepticism and indifference. Know-
ing the artistic instincts of the Upper Palaeolithic people from
their engraving and carving in bone and ivory, we should have
been prepared for the discovery of a parietal art. The publica-
tion of the engravings in the grotto of La Mouthe by Riviere22
in April, 1895, was the first warning of our oversight, and imme-
diately Edouard Piette recalled Altamira to the memory of the
workers on prehistoric art. The discovery of Sautuola ceased
to be isolated. Led by the engravings found in La Mouthe,
Sculpture
Incised Figures
Painted Figures
AZILIAN.
VI. No animal draw-
ings.
VI. Conventional Azilian
decoration. Flat pebbles
(galets) colored in red and
black. Mas d'Azil, Mar-
soulas, Pindal.
Late
Magdalenian.
Middle
Magdalenian.
Early
Magdalenian.
Slender human
figurines in ivory
and bone.
Animal forms in
reindeer and stag
horn on implements
of the chase and
ceremonial insignia.
Animal sculpture.
Bisons of Tuc d' Au-
doubert; hi^h re-
liefs of horses, Cap-
Blanc.
V. Entirely wanting.
IV. Graffites feebly
traced; fine lines indi-
cating hair predominate
in the drawings, as at
Font-de-Gaume and
Marsoulas. Perfected
animal outlines and de-
tails.
Fine animal outlines,
Grotte de la Mairie,
Marsoulas.
Perfected engraving
on bone and ivory.
III. Deeply incised
fines followed by light
graffite contour lines.
Incised outlines and
hair, e. g., mammoths
of Combarelles. Stri-
ated drawings, Castillo,
Altamira, Pasiega.
V. No animal art. Vari-
ous schematic and conven-
tional figures and signs
(bands, branches, lines,
punctuated surfaces sug-
gesting the Azilian galets).
IV. Polychrome animal
figures with the contour in
black and interior modelling
obtained through a mingling
of yellow, red, and black
color. Constant association
of raclage and of inci-
sions with painting. Mains
stylisees. Great, brilliant
polychrome frescos of
Marsoulas, Font-de-Gaume,
Altamira.
Animal outlines in black,
Niaux.
III. Figures of a flat tint
and Chinese shading with-
out modelling, also dotted
animal figures as at Font-
de-Gaume, Marsoulas, Al-
tamira, Pasiega.
SOLUTREAN.
Bone sculpture in
high relief; Isturitz,
Pyrenees. Animal
sculpture^ in the
round, P"ed:n3st.
Engravings.
Late
aurignacian.
Early
aurignacian.
Heavy human
statuettes (idals) of
Mentone, Brass 2 m-
pouy, Willendjrf,
Briinn. Human bas-
reliefs of Lauss^l.
Heavy human fig-
urines of Sireuil,
Pair-non-Pair.
Animals in low
relief.
II. Animal and hu-
man figures, at first very
deeply incised, then less
so; four limbs generally
figured. Designs vigor-
ous, somewhat awk-
ward, as at La Mouthe,
then more characteristic
as at Combarelles.
I. Figures deeply in-
cised, heavy, in abso-
lute profile; stiff in form
as at Pair-non-Pair, La
Greze, La Mouthe, Gar-
gas, Bernifal, Hornos de
la Pena, Marsoulas, Al-
tamira.
Archaic animal out-
lines of Castillo.
II. Filling in lines at first
feeble, then more and more
strong, finally associated
with contour modelling
which ultimately covers the
entire silhouette. Incised
lines associated with paint-
ing as at Combarelles, Font-
de-Gaume, La Mouthe, Mar-
soulas, Altamira.
I. Linear tracings in mono-
chrome, single black or red
lines, indicating only a sil-
houette. Two limbs out of
four are ordinarily figured.
The most ancient paintings
of Castillo, Altamira, Pindal,
Font-de-Gaume, Marsoulas,
La Mouthe, Combarelles,
Bernifal.
Statuary and bas-
relief.
Mobile and parietal
art in line.
Parietal and mobile art in
color.
STAGES IN THE DEVELOPMENT OF UPPER PALAEOLITHIC ART
396 MEN OF THE OLD STONE AGE
Daleau discovered the engravings in the grotto of Pair-non-Pair,
Gironde. In 1902 there was the double discovery of the en-
gravings in the grotto of Combarelles, and of the paintings in the
grotto of Font-de-Gaume, communicated by Capitan and Breuil.
Discoveries at Marsoulas, Mas d'Azil, La Greze, Bernifal, and
Teyjat soon followed.*
In 1908 Dechelette listed eight caverns in Dordogne, six in
the Pyrenees, and seven along the Cantabrian Pyrenees of
northern Spain, but there are now upward of thirty caverns in
which traces of parietal art have been found, and doubtless the
number will be greatly enlarged by future exploration, because
the entrances of many of the grottos have been closed, and the
remote recesses in which drawings are placed, as in the recent
discovery of Tuc d'Audoubert, are very difficult to explore.
The chief divisions of Upper Palaeolithic art are as follows :
1. Drawing, engraving, and etching with nne flint points on surfaces of
stone, bone, ivory, and the limestone walls of the caverns.
2. Sculpture in low or high relief, chiefly in stone, bone, and clay.
3. Sculpture in the round in stone, ivory, reindeer and stag horn.
4. Painting in line, in monochrome tone, and in polychromes of three
or four colors, usually accompanied or preceded by line engraving, with
flint points or low contour reliefs.
5. Conventional ornaments drawn from the repetition of animal or
plant forms or the repetition of geometric lines.
Drawings axd Engravings of the Early Magdalenian
We have already traced the art of engraving, as it first ap-
pears in late Aurignacian times, into the Solutrean ; in the
latter it is but feebly represented. Its further development in
early Magdalenian times is found in the engravings made with
more delicate or more sharply pointed flint implements, capable
of drawing an excessively fine line ; these were doubtless the early
Magdalenian microliths. The animal outlines, with an indication
* The whole history of these successive discoveries, beginning with the finding of an
engraved bone, in 1834, in the grotto of Chaffaud, and concluding with the discoveries
of Lalanne. and of Becouen. in 1012. is summarized in the admirable little handbook
by Salomon Reinach.' This convenient volume also includes outline tracings of the
more important drawings and sculptures found in western Europe up to the present time.
MAGDALENIAN ENGRAVINGS
397
of hair, are frequently sketched with such exceedingly fine lines
as to resemble etchings ; the figures are often of very small
dimensions and marked by much closer attention to details,
such as the eyes, the ears, the hair both of the head and the
Fig. 197. Primitive outline engravings of woolly mammoths of Aurignacian
or early Magdalenian times, from the walls of the cavern of
Combarelles. After Breuil.
Fig. 198. Engraved outlines and hair underlying the painting of one of the
mammoths, from the wall of the Galerie des Fresqucs, Font-de-Gaume.
After Breuil.
mane, and the hoofs ; the proportions are also much more exact,
so that these engravings become very realistic. Breuil ascribes
to the early Magdalenian the engraved mammoth tracings of
Combarelles. Engravings of this period are also found in the
grottos of Altamira in Spain, and of Font-de-Gaume in Dor-
MEN OF THE OLD STONE AGE
dogne, and to this stage belongs the group of does at Altamira,
distinguished by the peculiar lines of the hair covering the face.
The subjects chosen are chiefly the red deer, reindeer, mammoth,
horse, chamois, and bison. The striated drawings of Castillo
and Altamira, which partly represent hair and are partly indica-
tions of shading, belong to this period.
Fig. 199. Charging mammoth engraved on a piece of ivory tusk, from the station of
La Madeleine. After E. Lartet. For the sake of showing this figure clearly, other
outlines in this drawing, which were probably designed to indicate a herd of charging
mammoths, are omitted or represented by dotted lines. This classic engraving, de-
scribed on pages 384 and 385, is one of the most lifelike Palaeolithic representations
known of an animal in action.
The engravings in the grotto of La Mouthe were discovered
by Riviere, in 1895, and were the means of directing attention
afresh to the long-forgotten parietal art found in Altamira by
Sautuola in 1880. The drawings at La Mouthe begin about
270 feet from the entrance and may be traced for a distance of
100 feet, scattered in various groups ; they manifestly belong to
a very primitive stage, probably early Magdalenian, the point
of chief interest being that, while the greater part of the engrav-
ings are in simple incised lines, here and there the contour is
enforced by a line of red or black paint ; this is the beginning of
MAGDALENIAN ENGRAVINGS
399
a method pursued throughout the Magdalenian parietal art, in
which the artist carefully sketches his contours with sharp-
pointed flints before he applies any color. This treatment, at
first limited to the simple outlines, led to tracing in many of the
details with engraved lines, the eyes, the ears, the hair; thus
Breuil has shown that in its
final development a carefully
worked-out engraving under-
lies the painting. In the La
Mouthe drawings the propor-
tions are very bad ; they repre-
sent the reindeer, bison, mam-
moth, horse, ibex, and urus;
spots of red are sometimes
splashed on the sides of the
animals ; here and there is a
bit of superior work, such as
the reindeer in motion.
The cavern of Combarelles,
discovered in 1901, in Dor-
dogne, near Les Eyzies, con-
tains by far the most remark-
able record of early Magdale-
nian art ; there are upward of
four hundred drawings and en-
gravings representing almost
every animal of early Magdalenian times, among them the horse,
rhinoceros, mammoth, reindeer, bison, stag, ibex, lion, and wolf ;
there are also between five and six representations of the men of
the time, both masked and unmasked ; the style is more recent
than that of the oldest drawings in Font-de-Gaume, but much
more ancient than the period of polychrome art.* The gallery
is 720 feet long, and barely 6 feet broad; the drawings begin
about 350 feet from the entrance, and are scattered at irregular
Fig. 200. Engraved outlines believed to
represent human grotesques or masked
figures found on the cavern walls of
Marsoulas, Altamira, and Combarelles.
After Obermaier.
* Only a few drawings from this cavern have as yet been published, such as the famous
mammoth of Combarelles ; the entire work is in the hands of Breuil.
400
MEN OF THE OLD STONE AGE
intervals to the very end. In general the art is very fine and
evidently largely the work of one artist ; representations of the
woolly rhinoceros and of the mammoth are very true to life;
there is a pair of splendid lions, male and female ; the drawings
of the horse are abundant, and side by side we have a represen-
FiG. 201. Entrance to the cavern of Combarelles near Les Eyzies, Dordogne, where
upward of four hundred wall engravings have been discovered.
Photograph by Belves.
tation of several types of horses, the pure forest type with the
arched forehead, the small, fine-headed Celtic type, and a larger
type reminding us of the kiang, or wild ass. Here the greater
part of the work is engraving, as contrasted with the painted
outlines in the cavern of Niaux and with the etched outlines of
the Grotte de la Mairie.
Even a large cavern like Combarelles offers comparatively
few surfaces favorable to these engraved lines; but, small or large,
such surfaces were eagerly sought, sometimes near the floor,
sometimes on. the walls, and again on the ceilings; even with
MAGDALENIAN ENGRAVINGS
401
the brilliant light of an acetylene lamp it is now difficult to dis-
cover all these outlines, some of which are drawn in the most
unlooked-for places. If the
extremely fine incisions, such
as those representing the hair
of the mammoth, are so diffi-
cult to detect with a powerful
illuminant, one may imagine
the task of the Cro-Magnon
artists with their small stone
lamps and wick fed by the
melting grease. One such lamp
has been found in the grotto
of La Mouthe, about 50 feet from the entrance ; the workman's
pick broke it into four pieces, only three of which were re-
covered. The shallow bowl contained some carbonized matter,
Fig. 202. Cave-bear engraved in outline,
from the cavern of Combarelles.
After Breuil.
Fig. 203. Stone lamp of Magdalenian age discovered in the -grotto of La Mouthe by E.
Riviere. It is cut in sandstone and ornamented on the lower surface with the head
and horns of the ibex. Such lamps were doubtless used by the artists to light the
deep recesses of the caverns. After Riviere, redrawn by Erwin S. Christman. One-
third actual size. (Compare PI. VII.)
an analysis of which led Berthelot, the chemist, to conclude that
an animal fat was used for lighting purposes. Like most other
implements, this lamp is decorated — in this instance by an en-
402
MEN OF THE OLD STONE AGE
graving of the head and horns of the ibex. Three of these lamps
have been found in Charente and Lot, and it is noteworthy that
lamps similar to those of the Magdalenian period are used in
Dordogne at the present day.
Fig. 204. Entrance to the cavern of La Pasiega, not far from Castillo. The seated
figure with the staff is M. l'Abbe Henri Breuil, the present leader in the
study of Upper Palaeolithic art. Photograph by N. C. Nelson.
In the great cavern of Castillo,* at Puente-Viesgo, discovered
in 1903 by Alcalde del Rio, which is entered by the majestic
grotto already described on p. 162, the animal drawings are
mostly of an archaic character, belonging to the very beginnings
* The stations of Castillo, of Pasiega, and of Altamira were visited by the writer,
under the guidance of Doctor Hugo Obermaier, in August, 1912.
MAGDALENIAN ENGRAVINGS
403
of early Aurignacian parietal art. The most abundant subjects
are horses and deer, which entirely replace the reindeer drawings
so abundant in central France, outlines of the stag and of the
doe being very numerous; on the other hand, the bison and the
ox are rarely drawn. Belonging to the category of most primi-
'/'*![
tive painting are the simple
outlines in black of a horse and
of a mammoth, the two limbs
of one side being represented as
inverted triangles, terminating
in a sharp point, like the draw-
ings of children. Of more re-
cent style are the rather crude
polychrome bisons, numerous
hands outlined in red, and a
vast number of tectiform signs
and symbols which represent
inferior work of the middle
Magdalenian period.
On the other side of the
same mountain is the grotto of
Pasiega, discovered in 191 2 by
Doctor Hugo Obermaier. This
small grotto, about 500 feet
above the river, receives its
name as a retreat of the shepherds. In the floor is a very narrow
opening through which one rapidly descends by means of a tube
of limestone barely large enough to admit the passage of the
body. The interior is very labyrinthine. After passing through
the Galerie des Animaux and the Galerie des Inscriptions, one
reaches, after a most difficult detour, the terminal chamber,
which Obermaier has called the Salle du Trone, the throne-
room; here there is a natural seat of limestone, with supports
at the sides for the arms, and one can still see the discolora-
tion of the rock by the soiled hands of the magicians or of the
artists. In this salle there are a few drawings and engravings
Fig. 205. Carefully engraved half-figure
of a bison, from the cavern of Marsoulas;
an example of the engraver's work pre-
ceding the application of color. After
Breuil. One-eighth actual size.
404
MEN OF THE OLD STONE AGE
on the walls, and a few pieces of flint have been discovered. In
no other cavern, perhaps, is there a greater sense of mystery
as to the influence, whether religious, magical, or artistic, which
impelled men to seek out and enter these dangerous passages,
the slippery rocks illumined at best by a very imperfect light,
leading to the deep and dangerous recesses below, where a mis-
step would be fatal. The impulse, whatever it may have been,
was doubtless very strong, and in this, as in other caverns,
x\
v- \ r- ■' '• "
Fig. 206. Herd of horses engraved on a small slab of stone, found in the grotto of Chaf-
faud, Vienne, France. After Cartailhac. This impressionistic grouping and perspec-
tive is very exceptional in Palaeolithic design. About nine-tenths actual size.
almost every surface favorably prepared by the processes of
nature has received a drawing. No industrial flints have been
found at the entrance to this cavern, but some have been traced
into the interior. The art is considered partly of late Aurigna-
cian, perhaps of Solutrean, and certainly in part of early Mag-
dalenian times ; in general it is much more recent than that of
Castillo. It consists both of engravings and painted outlines,
with proportions usually excellent and sometimes admirable.
The paintings of deer are in yellow ochre, of the chamois in
red. There are altogether 226 paintings and 36 engravings, in
which are represented 50 roe-deer, 51 horses, 47 tectiforms, 16
MAGDALENIAN ENGRAVINGS
405
Bos, 15 bison, 12 stags, 9 ibexes, 1 chamois, and 16 other forms,
distributed in all parts of the cave. The outlines are in solid
red color or in stripes of red or black, or there is a series of spots ;
the subjects are chiefly the stag, the doe, the wild cattle (which
are rather common), the bison (which are less common), the
ibex, and the chamois. Among the numerous representations
of the horse there are two small engravings of a type with erect
mane, both the feet and the hair being indicated with great
care, the limbs well designed and of excellent proportions, clearly
in early Magdalenian style. Of the utmost interest is the dis-
covery here of two horses drawn with rounded forehead and
drooping mane, the only instance in which the drooping mane
$0i
^ fty~
Fig. 207. Impressionistic design of a herd of reindeer engraved on the radius of an
eagle nearly eight inches in length, found in the upper Magdalenian layers of the
Grotte de la Mairie. After Capitan and Breuil.
of the modern type of horse (Equus caballus) has been observed
in the cavern drawings.
In the advanced development of middle or high Magdalenian
art, parietal engraving with finely pointed flint implements pre-
sents a nearer approach to the truth both of proportion and of
detail than do the earlier stages. In this stage the engravings
seem to consist chiefly of independent animal figures and to
furnish a prelude to the application of color. A simple but
striking example of approaching perfection of technique is seen in
the bison (Fig. 205) engraved in the cavern of Marsoulas, where
the profile is outlined and great shaggy masses of hair beneath
the neck are admirably indicated. In these drawings the com-
plicated details of the feet, with their characteristic tufts of hair,
and of the head show far more careful observation. In the
406
MEN OF THE OLD STONE AGE
great series of bison at Font-de-Gaume the entire animal is
sketched in with these finely engraved lines, as brought out
through the wonderfully close observation and studies of Breuil.
This is quite similar to the practice of the modern artist who
sketches his figure in crayon or charcoal before applying the
color.
There are two quite different styles in this engraving, one
seen in the deep incised lines of the reindeer head in the cavern
Fig. 208. Stag and salmon engraved on an antler, from Lorthet, Hautes-
Pyrenees. After Piette. This design is believed to represent a herd of
stag crossing a stream, one of the very rare Palaeolithic attempts at
composition.
of Tuc d'Audoubert (Fig. 232), a complete design in itself, an-
other seen in the deep incisions in the limestone outlining the
horses and the bison as observed in the cavern of Niaux
(Fig. 174). Here the engraved line is followed by the appli-
cation of a black painted line, the effect being to bring out the
body in the surrounding rock so as to give the silhouette a
high relief.
In the drawings in the large on these curved wall surfaces,
only part of which could be seen by the eye at one time, the
difficulties of maintaining the proportions were extreme, and
one is ever impressed by the boldness and confidence with which
the long sweeping strokes of the flint were made, for one rarely
if ever sees any evidences of corrected outline. Only a lifelong
MAGDALENIAN ENGRAVINGS 407
observer of the fine points which distinguish the different pre-
historic breeds of the horse could appreciate the extraordinary
skill with which the spirited, aristocratic lines of the Celtic are
executed, on the one hand, and, on the other, the plebeian and
heavy outlines of the steppe horse. In the best examples of
Magdalenian engraving, both parietal and on bone or ivory, one
can almost immediately detect the specific type of horse which
the artist had before him or in mind, also the season of the year,
Fig. 209. Outlines of a lioness and a small group of horses of the Celtic or Arab type,
a delicate wall engraving in the Diverticule final of the cavern of Font-
de-Gaume. After Breuil.
as indicated by the representation of a summer or winter coat
of hair.
The realism of most of the parietal art passes into the im-
pressionism of the excessively fine engravings on bone or reindeer
horn, executed with a few strokes, of a herd of horses or of rein-
deer (Fig. 207), or where a herd of deer is seen (Fig. 208) cross-
ing a stream full of fishes, as in the well-known engravings on
reindeer horn found in the grotto of Lorthet, in the Pyrenees.
This is one of the very rare instances in Palaeolithic art, either
engraving or painting, which shows a sense of composition or the
treatment of a subject or incident involving more than one figure.
Others are the herd of parsing reindeer found engraved on a bit
of schist in the grotto of Laugerie Basse, the lion facing a group
of horses engraved on a stalagmite at Font-de-Gaume, and the
procession of mammoths engraved upon a procession cf bison in
the same cavern.
408
MEN OF THE OLD STONE AGE
Beginnings of Painting
The beginnings of painting in Aurignacian times, consisting
of simple contours and crude outlines in red or black, with little
or no attempt at shading, pass in early Magdalenian time24 into
a long phase of mono-
chromes, either in black
or red, in which the tech-
nique pursues a number
of variations, from simple
linear treatment, contin-
uous or dotted, to half
tints or full tints, grad-
ually encroaching on the
sides of the body from
the linear contour. Of
this order are the figures
in flat tints and shading,
resembling those of the Chinese, without modelling; also the
figures entirely covered with dots, such as are seen at Marsoulas,
Fig. 210. Early painting. A small horse of the
Celtic or Arab type, with painted outline and
body colored in black, from a wall of the cavern
of Castillo, Spain. After Breuil.
-
FlG. 21 r. Early painting Galloping horse of the Celtic or of the steppe type painted
in black and white, from a wall of the cavern of Font-de-Gaume. After Breuil.
Font-de-Gaume, and Altamira. The tints, as in the drawing of
the galloping steppe horse, pass inward from the black outline
MAGDALENIAN PAINTING
409
to enhance the effect of roundness or relief. In the splendid
series of paintings in the cavern of Niaux there is little more than
the black outline of the body, but the covering of the sides with
lines, indicating the hair, lends itself to the rounded presentation
of form. A somewhat similar effect is sought in the lines of the
woolly rhinoceros painted in red in the cavern of Font-de-Gaume,
which Breuil attributes to the Aurignacian stage, but which also
suggests the early Magdalenian.
Fig. 212. Opening (cross) of the cavern of Niaux, in the Pyrenees, near Tarascon.
Drawings in Various Caverns of the Early and
Middle Magdalenian
The grandest cavern thus far discovered in France is that of
Niaux (1906), which from a small opening on the side of a lime-
stone mountain and 300 feet above the River Vic de Sos extends
almost horizontally 4,200 feet into the heart of the mountain.25
Not far from Tarascon on the Ariege it lay near one of the most
accessible routes between France and Spain. Passing through
the long gallery beyond the borders of the subterranean lake
which bars the entrance, at a distance of half a mile we reach a
410
MEN OF THE OLD STONE AGE
great chamber where the overhanging walls of limestone have
been finely polished by the sands and gravels transported by
the subglacial streams; on these broad, slightly concave panels
of a very light ochre color are drawings of a large number of
bison and of horses, as fresh and brilliant as if they were the
work of yesterday ; the outlines drawn with black oxide of man-
ganese and grease on the smooth stone resemble coarse lithog-
raphy. The animals are drawn in splendid, bold contours, with
no cross-hatching, but with solid masses of bright color here and
there ; the bison, as the most admired animal of the chase, is
Fig. 213. Engraved and painted horse, apparently of the Celtic type and
with heavy winter coat, from the cavern of Niaux. There is a mark behind
the right shoulder which has been interpreted as the sign of an arrow or
spear head. After Cartailhac and Breuil. (Compare Fig. 174.)
drawn majestically with a superb crest, the muzzle most per-
fectly outlined, the horns indicated by single lines only, the eyes
with the defiant expression highly distinctive of the animal
when wounded or enraged. Here for the first time are re-
vealed the early Magdalenian methods of hunting the bison, for
upon their flanks are clearly traced one or more arrow or spear
heads with the shafts still attached ; the most positive proof of
the use of the arrow is the apparent termination of the wooden
shaft in the feathers which are rudely represented in three of
the drawings. There are also many silhouettes of horses which
strongly resemble the pure Asiatic steppe type now living in
the desert of Gobi, the Przewalski horse, with erect mane and
with no drooping forelock ; in contrast to the bison, the eyes are
rather dull and stupid in expression. There are also drawings
THE ART OF THE CAVERNS
411
of other types of horses, a very fine ibex, a chamois, a few out-
lines of wild cattle, and a very fine one of the royal stag ; we find
no reindeer or mammoth represented. In some of the narrower
passages the rock has been beautifully sculptured by water, and
Fig. 214. Professor Emile Cartailhac at the entrance of the cavern of Le Portel, Ariege.
Photograph by H. F. Osborn.
the artists have been quick to take advantage of any natural
lines to add a bit of color here or there and thus bring out the
outline of a bison.
Presenting the widest possible contrast to Niaux is the cavern
of Le Portel, west of Tarascon, with its contracted entrance and
a very rapidly descending passage hardly broad enough to admit
the body. This narrow and tortuous cave terminates in an ex-
412
MEN OF THE OLD STONE AGE
tremely small passage, so narrow as barely to admit the athletic
and determined artist explorer, the Abbe Breuil. Here, as in
Font-de-Gaume and other caverns, is one of the greatest myster-
ies of the cave art, namely, that these terminal and dangerous
diverticules finals were wrought with some of the most careful
and artistic designs. Le Portel, like Niaux, reveals a single style,
but one altogether different. Very numerous bison are drawn in
outline both in red and black ; the sides of the body are often
Fig. 215. Finely engraved outlines of the Celtic horse and of the reindeer, in the Grotte
de la Maine, near Teyjat, Dordogne. After Capitan and Breuil.
dotted with red or hatched in close parallel lines. On a long
horizontal panel are seen many bison in red, and one observes
here a finery drawn pair of bison feet in the best Magdalenian
style. The horse as represented here is of a quite different type
with thin upper tail and a tail-tuft resembling that of the wild
ass, so that one is almost tempted to believe that the kiang is
intended, but the ears are too short ; it has a high rump and a
high, splendidly arched neck, like that of the stallion, and the eye
is better drawn ; the body is covered with long vertical or oblique
lines which might be mistaken for stripes, but this hatching is a
matter of technique only. Again, the mane is erect, and there is
no forelock ; in fact, none of these Magdalenian artists has rep-
resented the horse with the forelock, indicating that this char-
THE ART OF THE CAVERNS
413
acter of the modern horse was unknown in western Europe and
probably came in during Neolithic times.
Of an entirely different type are the beautifully engraved
miniature figures of animals discovered in 1903 in the Grotte de
Fig. 216. Reindeer, cave-bear, and two horses of the large-headed forest type with
arched forehead, engraved on a panel about twenty inches in length in the
Grotte de la Mairie. After Capitan and Breuil.
la Mairie.26 The outlines, from 18 to 20 inches in length, are
sharply engraved on the limestone stalagmites ; they are all in
the middle Magdalenian style and include the stag, reindeer,
Fig. 217. Wild cattle, bull and cow (Bos primigenius) , engraved in the Grotte de la
Mairie, each figure being about twenty inches in length. After Capitan and Breuil.
bison, cave-bear, lion, wild cattle, and two very distinct types
of horses: one of these types is large-headed with an arched
forehead; this is probably the forest type and perhaps represents
414 MEN OF THE OLD STONE AGE
the horse most abundant at the Solutre encampment (see p. 288) ;
the other horse is small-headed, with a perfectly flat, straight
forehead, corresponding with the Arab or Celtic pony type.
Drawings and Paintings of the End of the
Middle Magdalenian
The fourth and final developmental phase of painting flowers
out toward the end of middle Magdalenian times in the grand
period of polychromes. These are first etched with underlying
Fig. 218. Outline of one of the bison in the Galerie des Fresques at Font-
de-Gaume, showing the preliminary etching or engraving preparatory
to the polychrome fresco painting. After Breuil.
lines engraved with flint, the surface of the limestone having
been previously prepared by the thinning or scraping of the
borders (r adage) to heighten the relief of the drawing; then a
very strong contour is laid down in black, and this may be fol-
lowed by a further contour line in red (the use of black and red
is very ancient) ; an ochreous brown color is mixed in, conform-
ing well with what we know to be the tints of the hairy portions
of the bison. Thus gradually a complete polychrome fresco art
develops. The final stage of this art follows, in which the filling
out of various tones of color requires the use of black, brown, red,
and yellowish shades. The underlying or preliminary engraving
now begins to recede, being retained only for the tracing in of
the final details of the hair, the eyes, the horns, and the hoofs.
2 p
1-i
3*3
03
3s J
POLYCHROME PAINTING
415
The early stages of this art are seen in the cavern of Marsoulas.
and its height is reached in the mural frescos of Font-de-Gaume
and in the ceiling of Altamira, the latter still in a perfect and
brilliant state of preservation.
To prepare the colors, ochre and oxide of manganese were
ground down to a fine powder in stone mortars; raw pigment
Fig. 219. Entrance on the right to the grotto leading to the great cavern of Font-de-
Gaume on the Beune. Photograph by N. C. Nelson.
was carried in ornamented cases made from the lower-limb bones
of the reindeer, and such tubes still containing the ochre have
been found in the Magdalenian hearths; the mingling of the
finely ground powder with the animal oils or fats that were used
was probably done on the flat side of the shoulder-blade of the
reindeer or on some other palette. The pigment was quite per-
manent, and in the darkness of the Altamira grotto it has been
so perfectly preserved that the colors are still as brilliant as if
they had been applied yesterday.
The art of the grotto of Marsoulas, in the Pyrenees, is both
416
MEN OF THE OLD STONE AGE
of an earlier and of a later period ; the engraved lines, as of
the head and front of a bison, are beautifully done in advanced
Magdalenian style, deep incisions representing the larger out-
lines and finer incisions representing the hair ; here the outlines
are also traced in color, and there are several masks or grotesques
of the human face ; these last are treated with a total disregard
of the truth which characterizes the animal work. Among the
few bison represented here, some are covered with dots or
splashes of color, others show the painted outline which begins
Rubicon
/
Grande Galerie
des Fresques
PLAN de la GROTTE
OE
FONTDEGAUME
r el eve pan
le Dr CAP/TAN.
Echelle J,
Fig.
220. Map of the cavern of Font-de-Gaume, showing the 'Rubicon,' the Grande
Galerie des Fresques, in which the chief polychrome paintings are found, and
the Diverticule final. After Capitan.
to extend over the surface with gradations of tint, anticipating
the color effects attained in the finished paintings of Altamira and
of Font-de-Gaume. All the details of the early technique are
found here : the artist outlines the form with an engraved line ;
he traces in black color the contours of the head and of the body;
he begins to apply masses of red over the figure. This beginning
of polychrome art at Marsoulas is a step toward coloring the en-
tire surface with red ochre and black, as in the finished paintings
of a later period.
The grand cavern of Font-de-Gaume,27 on the Beune, not far
from Les Eyzies, contains the most complete record of Upper
Palaeolithic art, especially from the close of Aurignacian to the
Fig. 221. Narrow passage in the cavern of Font-de-Gaume, known as the 'Rubicon.'
On the left wall at this point are two painted bison, and on both walls are
marks left by the claws of the cave-bear. After Lassalle.
POLYCHROME PAINTING
419
close of Magdalenian times. There are crude Aurignacian
drawings, simple outlines painted in black, outlines supplemented
by the indication of hair (examples of the early stages in the de-
velopment of polychrome work as well as of the very highest
stages), compositions like the lion and the group of horses, and
the murals in the Galerie des Fresques, which show a general com-
position in the processions of animals, as well as some special
compositions such as the reindeer and bison facing each other.
The life depicted is largely that of the tundras, mammoths,
rhinoceroses, and reindeer, but it also includes the steppe or
Celtic type of horse, represented galloping (Fig. 211), and a
^^U Wft
r-\
Fig.
222. Plan of a portion of the left wall decoration in the Galerie des Fresques at
Font-de-Gaume, showing reindeer and the procession of bison. After Breuil.
small group of horses of the Arab or Celtic type. Of the meadow
fauna the bison is generally represented in preference to the
wild ox or urus.
Throughout the cavern the favorable surfaces of the walls
are crowded with engravings, and in the Galerie des Fresques,
beyond the narrow passage known as the ' Rubicon' (Fig. 221),
we see altogether the finest examples of Upper Palaeolithic art.
On each side of this gallery is a peculiarly advantageous mural
surface, broad, relatively smooth, and gently concave (PL VII),
probably the best which any cavern afforded, and here we ob-
serve great processions of mammals superposed upon each other,
like the records of a palimpsest, as if such a surface was so rare
that it was visited again and again. The most imposing series
is that of the bison, done in the finest polychrome style, mostly
420
MEN OF THE OLD STONE AGE
headed in one direction. The reindeer form another series and
in some instances face each other, although mainly arranged in
a long procession facing to the left. This superposition of draw-
ing upon drawing ends with the latest superposition in finely
incised lines of a great procession of mammoths upon that of
the polychrome bisons. It is somewhat difficult to reconcile a
religious or votive interpretation with the multiplication of these
Fig. 223. Another portion of the left wall decoration of the Galerie des Fresques, show-
ing the preliminary engraving (above), and the painting (below) of the great proces-
sion of mammoths, superposed upon drawings of the bison, reindeer, and horse. This
section is about fourteen feet in length. After Breuil.
drawings upon each other. Moreover, it appears to be incon-
sistent with the reverent spirit which pervades the work in this
and in all other caverns, for what impresses one most is the ab-
sence of trivial work or meaningless drawings.
It seems as if at every stage in their artistic development
these people were intensely serious about their work, each draw-
ing being executed with the utmost possible care, according to
the degree of artistic development and appreciation.
In the great gallery of frescos we find not less than eighty
t
POLYCHROME PAINTING
421
figures, in some cases partly covered by a fine sheen of stalag-
mitic limestone ; these include 49 bison, 4 reindeer, 4 horses, and
15 mammoths. The bison polychromes have suffered somewhat
in color and are far less brilliant than those at Altamira. In
the polychromes the color is applied either in long lines of red
or black surrounding the contours of the animal or in flat tints
placed side by side, or again the two colors are mingled and give
PIg. 224. Detail of the engraving of the central group of figures on the left wall decora-
tion of the Galerie des Fresques (see Fig. 223), showing the etching of a mammoth
superposed upon that of a bison, superposed in turn upon those of a reindeer and of
a wild boar. These figures are on different scales, and in the present faded condition
of the frescoes are difficult to detect. After Breuil.
intermediate tints with striking effect. On one of the finest of
these bison is the underlying drawing of a reindeer, a wild boar,
and the superposition of an excellent engraving of a mammoth,
which is represented on an altogether different scale, so that it
falls well within the body lines of the bison (Fig. 224). In each
of these mammoths the grotesque but truthful contour is pre-
served in the drapery of hair which almost completely envelops
the limbs; the emphasizing of the sudden depression of the
dorsal line behind the head is everywhere the same and un-
doubtedly conforms very closely to nature.
422
MEN OF THE OLD STONE AGE
After passing the Galerie des Fresques we penetrate to the
final recess called the Diver ticule final, through excessively nar-
FlG. 225. Entrance to the cavern of Altamira, showing the proximity of the roof of
the cavern to the present surface of the earth. Photograph by N. C. Nelson.
row tubular openings barely admitting the body, and we are
again overcome with the mystery as to what impulse carried this
art into the dark, deep portions of the caverns. If it were due
POLYCHROME PAINTING
423
to a feeling partly religious which regarded the caverns with
special awe, why do we find equally skilful and conscientious
work on all the mobile utensils of daily life and of the chase,
apart from the caverns ? The superposition of one drawing upon
another, which is especially characteristic of this cavern, does not
seem to strengthen the religious interpretation.
It would appear that the love of art for art's sake, akin in a
very rudimentary form to that which inspired the early Greeks,
together with the fine spaces which these caverns alone afforded
for larger representations, may be an alternative explanation.
Fig. 226. Plan showing the grouping of bison, horses, red deer, and wild boar, in the
polychrome paintings on the ceiling of Altamira. After Breuil.
There is no evidence that numbers of people entered these cav-
erns. If this had been the case there would be many more ex-
amples of inartistic work upon the walls. It is possible that the
Cro-Magnon artists constituted a recognized class especially
gifted by nature, quite distinct from the magician class or the
artisan class. The dark recesses of the caverns opening back
of the grottos may have been held in awe as mysterious abodes.
In line with this theory is the suggestion that the artists may
have been invited into the caverns by the priests or medicine-
men to decorate the walls with all the animals of the chase.
The polychromes of the ceiling of Altamira in northern Spain,
which rank in the crude art of Palaeolithic times much as the
ceiling of the Sistine Chapel does in modern art, are somewhat
424
MEN OF THE OLD STONE AGE
more conventional in technique than those of Font-de-Gaume, but
they are manifestly the work of the same school, and prove that
the technique of art spread like that of engraving, of sculpture,
and of the preparation of flint and bone implements all over
southwestern Europe. One could not have more striking proof
of the unity of race, of a community of life, and of an inter-
^^^BMjMBBlPlI
m
KflBi
'JB^^I
Fig. 227. The ceiling of Altamira, showing the round projecting bosses of limestone on
which the recumbent figures of the bison are painted. After Lassalle.
change of ideas among these nomadic people than the close re-
semblance which is observed in the art of Altamira, Spain, and
that of Font-de-Gaume, 290 miles distant, in Dordogne.
Very picturesque is the account of the discovery of this
wonderful ceiling, made not by the Spanish archaeologist Sautuola
himself, but by his little daughter, who, while he was searching
for flints on the floor of the cavern, was the first to perceive the
paintings on the ceiling and to insist upon his raising his lamp
aloft. This was in 1879, l°ng before the discovery of parietal
art in France. The ceiling is broad and low, within easy reach
of the hand, and the oval bosses of limestone (Fig. 227), from
POLYCHROME PAINTING
425
4 to 5 feet in length and from 3 to 4 in width, led to the develop-
ment here of one of the most striking characteristics of all Palae-
olithic art, namely, the artist's adaptation of the subject to his
medium and to the character of the surface upon which he was
working. It seems to show a high order of creative genius that
each of these projecting bosses was chosen for the representation
of a bison lying down, with the limbs drawn up in different posi-
tions beneath the body (Fig. 228) and very carefully designed,
Fig. 228. Female bison lying down with the limbs drawn beneath the body, so that
only the horns and tail project beyond the convex surface of the limestone
boss on the ceiling of Altamira. After Breuil.
and with the tail or the horns alone projecting beyond the con-
vex surface to the surrounding plane surface. This is the only
instance known where the bison are represented as lying down,
in most lifelike attitudes, showing the soles of the hoof, observed
with the greatest care and represented by a few strong and sig-
nificant lines. Thus while the Altamira coloring inclines to con-
ventionality, the pose of these animals indicates the greatest
freedom of style and mastery of perspective anywhere observed.
In this wonderful group there is also a bison bellowing, with his
back arched and his limbs drawn under him as if to expel the
air. One striking feature in all these paintings is the vivid rep-
426
MEN OF THE OLD STONE AGE
resentation of the eye, which in every case is given a fierce and
defiant character, so distinctive of the bison bull when enraged.
We also observe a wild boar in a running attitude and several
spirited representations of the horse and of the female deer.
The cavern of Altamira, besides this chef-d'oeuvre, contains work
of a very advanced character, as indicated in the imposing en-
Fig. 229. The royal stag (Cervus elaphus) engraved on the ceiling of the cavern
of Altamira. About twenty-six inches in length. After Breuil.
One-eighth actual size.
graving of the royal stag (Fig. 229), which is altogether the finest
representation of this animal which has thus far been discovered
in any cavern.
Altamira, like Font-de-Gaume, presents many phases of the
development of art in Magdalenian times. There is a Solutrean
layer in the foyer of this great cavern, but Breuil is not inclined
to attribute any of the art to this period. The first entrance of
Altamira by the Cro-Magnon artists is dated by the discovery
of engravings on bone of the female red deer, which are identical
MAGDALENIAN SCULPTURE
427
with those on the walls and which belong to very ancient Magda-
lenian times, the period at which the caverns of Castillo and La
Pasiega were also entered.28
Sculpture
Animal sculpture in the round, which is indicated by the
few statuettes found with the burial at Briinn, Moravia, and by
\>-^
Fig. 230. Statuette of a mammoth in reindeer horn from the Abri de Plantade at Bruni-
quel. After Piette. "A statuette presenting the general form of the mammoth with
some fantastic features. It formed part of a pendant of which the shank, terminating
with a perforation, has been broken. The tusks were laid against this shank and
strengthened it. The incisions bordered by notches suggest the nostrils of some im-
aginary monster. The trunk seems to grow out of the neck, not the head. The tail
having been broken off in Palaeolithic times, the owner made a hole in the back and
inserted one there. The material was too thin to admit of representing the proper
thickness of the animal. It was made to be viewed from the side."
the ivory mammoth statuette found at Pfedmost, continued into
early Magdalenian times and certainly constitutes one of the
most distinctive features of the art of that period, because in
the later Magdalenian it took a different trend in the direction of
decorative sculpture. Only two fine examples of early Mag-
dalenian animal sculpture have been found, but these are of
such a remarkable character as to indicate that modelling in
the round was widely pursued at this time. These are the bisons
discovered in 191 2 in the cavern of Tuc d'Audoubert near Mon-
428
MEN OF THE OLD STONE AGE
tesquieu, in the Pyrenees, and the fine bas-reliefs of horses at the
shelter of Cap-Blanc, on the Beime, in Dordogne.
In company with Professor Cartailhac the writer had the
good fortune to enter the cavern of Tuc d'Audoubert a few days
after its discovery by the Comte de Begouen and his sons ; it
is still in the making, for out from the entrance flows a stream of
Fig. 231. Entrance to the cavern of Tuc d'Audoubert, near Montesquieu- Avantes in
the Pyrenees. This is one of the rare instances in which the stream that formed the
cavern is still flowing from the entrance. Photograph by N. C. Nelson.
water large enough to float a small boat, by which the first of
a series of superbly crystallized galleries is reached. After pass-
ing through a labyrinth of passageways and chambers a favorable
surface was found where the Begouen party showed us a whole
wall covered with low-engraving reliefs, very simply done, fine
in execution, with sure and firm outlines of the bison, the favorite
subject as in all other caverns ; horses fairly well executed and
of the same steppe type as those in the near-by cavern of
MAGDALENIAN SCULPTURE 429
Niaux ; one superbly engraved contour of the reindeer, with its
long, curved horns ; the head of a stag with its horns still in
the velvet ; and a mammoth. All this work is engraved ; there
are no drawn outlines, but here and there are splashes of red
Fig. 232. Head of a reindeer deeply incised or engraved in the limestone wall of the
cavern of Tuc d'Audoubert. After Begouen.
and black color. Shortly afterward a great discovery was made
in this cavern ; it is described as follows by the Comte de Be-
gouen :* " To-day I am happy to give you excellent news from
the cavern Tuc d'Audoubert. As you were the first to visit
* Letter of October 23, 191 2.
430
MEN OF THE OLD STONE AGE
this cavern, you will also be the first to learn that in an upper
gallery, very difficult of access, at the summit of a very narrow
ascending passage, and after having been obliged to break a
number of stalactites which completely closed the entrance, my
son and myself have found two superb statuettes in clay, about
60 cm. in length, absolutely unbroken, and representing bison.
W:'--:< ''■ ' "*
■Br
... -«bS
1
*\ ~ "■sBi
~ .' \
■ "}■■: i ^' 4:
' i '«>/
^^
1 > >, 1 E^NllijH
>- ■" ':!T >
^K»MM^l.l| ^Ml
^ :?t
:^ml
m_ l
'• IB
!<^J^i>:.
.'■■■'•'■■:'":"" ■/'•''
it* - .« ' '
-'•>T™1
W&';%
- ,' ' :ir
mS
IB
•
i&\\$&* $#&***
*^%\
-.i&^
«?*•*"";"*
^
V
•
■ SnKmL1;
A .'
Fig. 233. Two bison, male and female, modelled in clay, discovered in the cavern of
Tuc d'Audoubert. The length of each of these models is about two feet.
After Begouen.
Cartailhac and Breuil, who have come to see them, were filled
with enthusiasm. The ground of these chambers was covered
with imprints of the claws of the bear, skeletons of which were
buried here and there. The Magdalenians have passed through
this ossuary and have drawn out all the canine teeth to make
ornaments of them. Their steps left their fine impressions on
the humid and soft clay, and we still see the outlines of several
bare human feet. They had also lost several flakes of flint and
the tooth of an ox pierced at the neck ; we have collected them,
:
M
AGDALENIAN SCULPTURE
431
and it seems as if they had only dropped yesterday ; the Mag-
dalenians also left an incomplete model of a bison and some
lumps of kneaded clay which still carry the impression of their
ringers. We produce the proof that in this period all branches
of art were cultivated." This model of the male and female
bison in clay has been described by Cartailhac as of perfect
workmanship and of ideal art.
The procession of six horses cut in limestone under the shel-
tering cliff of Cap-Blanc is by far the most imposing work of
Fig. 234. One of a series of horses of the high-bred Celtic type, sculptured in high
relief on the wall of the cliff shelter known as Cap-Blanc. The actual length of
each of these sculptures is about seven feet. After Lalanne and Breuil.
Magdalenian art that has been discovered. The sculptures are
in high relief and of large size and are in excellent proportion ;
they appear to represent the high-bred type of desert or Celtic
horse, related to the Arabian, so far as we can judge from the
long, straight face, the slender nose, the small nostrils, and the
massive angle of the lower jaw ; the ears are rather long and
pointed, and the tail is represented as thin and without hair;
they were found partly buried by layers containing implements
of middle Magdalenian industry, and they are therefore assigned
to an early Magdalenian date in which animal sculpture in the
round reached its climax.
432
MEN OF THE OLD STONE AGE
From the early to the middle Magdalenian period animal sculp-
ture in bone, horn, and ivory was followed as decorative art in
a bold and highly naturalistic manner. Adaptation of the animal
Fig. 235. Head of a horse sculptured on a reindeer antler, from the Magdalenian layer of
Mas d'Azil on the right bank of the Arize. After Piette. Actual size.
figure to the surface and to the material employed is nowhere
shown in a more remarkable way than in the batons, the dart-
throwers, and the poniards. Of all the work of the Upper
Palaeolithic, these decorative heads and bodies are, perhaps, the
Fig. 236. Statuette carved on a fragment of mammoth tusk, representing a horse of
Celtic type with mane erect, from the grotto of Les Espelugues, Lourdes.
After Piette. About one and one-third actual size.
MAGDALENIAN SCULPTURE
433
most highly artistic creations in the modern sense. The famous
horse found in the late Magdalenian levels of Mas d'Azil (Fig.
235) and the small horses from the grotto of Espelugues, of the
middle Magdalenian, are full of movement and life and show
such certainty and breadth of treatment that they must be re-
garded as the masterpieces of Upper Palaeolithic glyptic art.
The ibex carved on the dart-thrower from the grotto of Mas
d'Azil (Fig. 178) indicates observation and a striking power of
Fig. 237. Head of a woman with head-dress sculptured in ivory, from the Magdalenian
levels of Brassempouy. After Piette. One and one-fifth actual size.
expression; while all the details are noted, the treatment is
very broad,
The continuation of animal sculpture in the round is seen in
the well-known horse statuette from the grotto of Lourdes ; the
partly decorative striping is a step in the direction of conventional
treatment. The sculptured reindeer discovered by Begouen in
the grotto of Enlene is treated in a somewhat similar style.
Small human figurines again appear in the form of statuettes
in bone or ivory, representing the renaissance of the spirit of
human sculpture. Some of this work is apparently in search of
beauty and with altogether different motives from the repellent
feminine statuettes of middle and late Aurignacian times, for
434 MEN OF THE OLD STONE AGE
the subjects are slender and the limbs are modelled with relative
skill. As in the earlier works, there is a partial failure to portray
the features, which is in striking contrast to the lifelike treat-
ment of animal heads. Very few examples of this work have
been found, and most of them have been broken. To this period
belong the Venus statuette of Laugerie Basse and the head of a
girl carved in ivory found at Brassempouy (Fig. 237) with the
features fairly suggested and an elaborate head-dress.
Geographic Distribution of the Magdalenian Culture
In Magdalenian times the Cro-Magnon race undoubtedly
reached its highest development and its widest geographic dis-
tribution, but it would be a mistake to infer that the boundaries
of the Magdalenian culture also mark the extreme migration
points of this nomadic people, because the industries and inven-
tions may well have spread far beyond the areas actually inhabited
by the race itself.
Absence of Magdalenian influence around the northerly
coasts of the Mediterranean is certainly one of the most surpris-
ing facts. Breuil has suggested that Italy remained in an Aurig-
nacian stage of development throughout Magdalenian times and
indicates that there is much evidence that Magdalenian culture
never penetrated into this peninsula, for in Italy the Aurignacian
industrial stage is succeeded by traces of the Azilian. This geo-
graphic gap, however, may be filled at any time by a fresh dis-
covery. In Spain, also, the Magdalenian culture is known only
in the Cantabrian Mountains, but never farther south, one of
the earliest sites found in this region being the grotto of Pena la
Miel, visited by Lartet in 1865, and one of the most famous the
cavern of Altamira, discovered by Sautuola in 1875 ; to the north-
east is the station of Banyolas. So far the eastern provinces of
Spain have not yielded any implements of engraved or sculptured
bone.
In contrast to this failure to reach southward, the Magdalenian
culture is widely extended through France, Belgium, England,
EXTENT OF THE MAGDALENIAN CULTURE
435
Germany, Switzerland, Austria, and as far east as Russia. It
would appear either that the men of Magdalenian times wan-
dered far and wide or that there was an extensive system of
barter, because the discovery of shells brought for personal
adornment from the Mediterranean seashores to various Mag-
STATIONS
OF
THE
VEZERE
iox»#
,•8 .13 ,,
® CEREMONIAL BURIALS
>X HUMAN FOSSILS \
\-Corge d' Enfer 9-Liveyre
2-Laugcrie Basse. W-La Mouth*
3-Laugerie Haute \\-Fonl-de-Gaun
4-LA MADELEINE \1-CombmlUs
5-Le Ruth
6-Longuerocke
1-Les Eyzies
A-Crosle Biscol
13-Cazet/e
V^-Bernifal
15- Cap Blanc
Vo-Laussel
ES
1- Trou de Sureau
5- Trou de Chaleux
Z-Goyet
6~ Trou de Frontat
3- Engis
Trou des Nutons
ArTroti Mag r tie
Trou de Praule
STATIONS OF THE DANUBE
fiG. 238. Geographic distribution of the principal Magdalenian industrial stations in
western Europe.
dalenian sites in France and in central Europe seems to indicate
a wide-spread intercourse among these nomadic hunters and a
system of trade reaching from the coasts of the Mediterranean
and the Atlantic to the valley of the Neckar in Germany and
along the Danube in Lower Austria. Another proof of this inter-
course is the wide distribution not only of similar forms of im-
plements but of very similar decorations ; as an instance, Breuil
notes the likeness of schematic engravings on reindeer horn in
436 MEN OF THE OLD STONE AGE
the two primitive Magdalenian layers of Placard, Charente, to
those found in the Polish cavern of Maszycka, near Ojcow, and
to others in the corresponding layers of Castillo, near Santander,
of Solutre on the Saone, and of various sites in Dordogne. A
very distinctive geometric decoration on bone is that of broken
zigzag lines with little intercalated transverse lines, which we
notice at Altamira, in northern Spain, and which also occurs here
and there in Dordogne and in Charente and extends to the grottos
of d'Arlay in the Jura. Another style of ornament, with deep
pectinate and punctuate lines, found in the very ancient Mag-
dalenian of Placard, also occurs in the most ancient layers of
Kesslerloch, Switzerland. Spiral ornaments like those on the
bone weapons of Dordogne, of Arudy, and of Lourdes are found
at Hornos de la Pena, in the Cantabrian Mountains. The spread
of analogous decoration is still more striking when we find it
occurring in the details of sculpture or in a certain type of dart-
thrower (propulseur), which extended from the Pyrenees east-
ward to the Lake of Constance. Inventions like that of the
harpoon and fashions like those of the decorative motifs were
carried from point to point.
This influence does not lead to identity. Some of the phases
of art and of decoration are confined to certain localities; for
example, the engravings of deer on the bone shoulder-blades in
the caverns near Santander, Spain, are not duplicated in France ;
also there are numerous local styles witnessed in the forms and
decorations of the javelin, the lance, and the harpoon ; these vari-
ations, however, do not conceal the element of community of
culture and of similar fluctuations of industry and art between
widely distant stations.
Many Magdalenian stations were crowded around the shel-
tered cliffs of Dordogne (Fig. 238). Besides these, we observe
the Magdalenian sites of Champs, Ressaulier, and the grotto of
Combo-Negro in Correze ; south of Dordogne and Correze are
other stations along the Garonne and the Adour. Some of the
finest examples of Magdalenian art have come from Bruniquel,
on the Aveyron. near the boundary between Tarn-et- Garonne
EXTENT OF THE MAGDALENIAN CULTURE 437
and Tarn, where no less than four important sites have been
excavated.
The culture map of France in Magdalenian times is covered
from north to south with these ancient camp sites, either clus-
tered along the river borders, where erosion has created shelters,
or in the great outcrops of limestone along the northern slopes of
Fig. 239. Necklace of marine shells, from the cave of Cro-Magnon^ mostly periwinkles,
some related to species now living in the North Sea, Purpura, Turitella, and Fusus.
After E. Lartet. The Cro-Magnon grotto dwellers used shells belonging to existing
species, while in the deposits at La Madeleine and Laugerie Basse fossil shells are found.
The use of seashore shells as ornaments in various parts of the interior of Europe indi-
cates that they were brought long distances in trade. The remains of such ornaments
were found with the skeleton of Aurignacian age from Paviland, Wales. Necklaces
were also made of small plates of ivory and the perforated teeth of the cave-bear.
One-third actual size.
the Pyrenees, where the exposure of the limestone has led to the
formation of grottos and caverns, or on the plateaus where game
abounded or flint could be found for the rapidly declining flint
industry. Near the Gulf of Lyons are the stations of Bise,
Tournal, Narbonne, and Crouzade ; extending westward toward
the headwaters of the Ariege are La Vache, Massat, and the great
tunnel station of Mas d'Azil, formed by the River Arize; here
the Magdalenian levels discovered by Piette have yielded some
438 MEN OF THE OLD STONE AGE
of the most notable Magdalenian works of art, including animal
statuettes, bas-reliefs, and engravings with incised contours.
Farther west, on the headwaters of the Garonne, is Gourdan,
where Piette began his remarkable excavations in 187 1 and dis-
covered two of the ancient Magdalenian phases of sculpture ;
then comes the more westerly group of Aurensan, Lor the t, and
Lourdes, the latter a grotto which has yielded one of the finest
examples of the horse sculptured in ivory, and which has since
become famous as the site of a miracle and of modern pilgrimage.
Between the Garonne and the Bay of Biscay lie the stations of
Duruthy and the Grotte du Pape of Brassempouy, the latter
occupied in Magdalenian times, but best known as a centre of
late Aurignacian sculpture of statuettes.
To the northeast, in the very heart of the mountainous region
of Auvergne, is the station of Neschers, where a flow of lava from
Mount Tar tare t descended over the slopes of Mont-Dore and
covered a Mousterian industrial deposit with its mammoth
fauna and then, after a lapse of time, became the site of a Mag-
dalenian industrial camp, so that Boule has been able to deter-
mine the geologic age of the most recent volcanic eruptions in
France, those of the Monts d'Auvergne, as having occurred be-
tween the periods of Mousterian and Magdalenian industry.
In view of the frequent occurrence of Aurignacian and Solu-
trean camps as well as of Neolithic stations in southeastern
France, we are surprised at the extreme rarity there of Magda-
lenian flint implements. However, Capitan has recognized a
Magdalenian station at Solutre, near the headwaters of the Saone,
and not far from this site is the station of Goulaine, which has
yielded an enormous flint scraper or anvil, the largest Upper
Palaeolithic implement ever found ; it is carefully chipped around
the entire curved edge and weighs over 4^ pounds. To the
north of the Dordogne is the celebrated grotto of Placard, in
Charente, where the dawn of the Magdalenian industry has been
discovered, and again directly north of this is the grotto of Chaf-
faud, at Savigne, where the first engraved bone of the 'Rein-
deer Age' was discovered in 1834 ; not far from this is the shelter
<1
>vtvcve~-i
tZM
2.1
<^..U:
<2>
<*N
f
DUSS
n-s
__BL __
^/
HANOVER
O
w
*^s
tarunshdhlem
.—H
SSELDORF
- ygf Neanderthal ralverk'(Skle-
| COLOGNEi
^Vildsbheu
L*fVi/dAaus
Balttnannshohlem
in
■'>•
\
\
V
V
JVeimar
LEIPSIC
| £krmgsdL]*-f-!'tbad?
| JVrJte_Scheuer+
A
Mymenhetmm \j ' Z«ffenkaus\nm
Ahenh,- rsA. S7UTTQTO*Cannstatt
I
pfanhJno
| XSdL/jg
' Oberilarg*
Niedernauk
WinterlinLn
\StrassbeX+
%ropstlr
RauberhokL
mO/net
[rpfelhohjg s^rr"
• J /TJanube
Tuneingen
Scfoueisersbild
+Holjmtein
rtein
Oberilargm ObasTe
[SWABIA
^Ww/r;-: ;.'.'/*. ..••-r-'''::'*.""' -.
iWzJdkirliili:
10
53
52
51
50
49
48
| PALsEOLITHfC STATIONS Q CITIES OF MODERN GERMANY
Fig. 240. Geographic distribution of the Magdalenian and other Palaeolithic stations on
the upper waters of the Rhine and of the Danube. The chief Magdalenian stations are:
Andernach, Bockstein, Buchenloch, Ganscrsfelsen, Hohlefels bei Hiitten, Hohlefeh bei
Schelklingen, Hohlestein, Kartstein, Kastlhdnghohle, Kesslerloch, Martinshohle, Mnn-
zingen, Niedernau, Oberlarg, Ofnet, Propstfels, Schmiechenfels, Schnssenqnelle, Schweizers-
bild, Sirgenstein, Strassberg, Wildhaus, Wildscheuer, and W inter lin gen. After R. R
Schmidt, modified and redrawn.
440 MEN OF THE OLD STONE AGE
of Garenne, near St. Marcel (Indre), which has afforded a fine
figure of a galloping reindeer.
These geographic and artistic records are of intense interest
as carrying the Perigord or Dordogne culture northward. Some-
what to the east, on the headwaters of the Cure, a tributary of
the Yonne, there is an important group including over sixty open
shelters formed in the Jurassic limestone, in which characteristic
Magdalenian bone implements have been found. Of these the
most famous are the Grotte des Fees, and the Grotte du Tri-
lobite, both of which were first entered by the Neanderthals in
Mousterian times and were again sought by the Cro-Magnons
in Magdalenian times. Passing still farther north, the Cro-
Magnons visited the borders of the Somme and sought the his-
toric flint station of St. Acheul, which had been frequented by
races of men for thousands of years previous, back to Pre-
Chellean times.
To the northeast are the stations of Belgium, chiefly made
known through the labors of Dupont, distributed along the val-
leys of the Lesse and of the Meuse and yielding characteristic
Magdalenian flints as well as a number of engravings on bone.
We may be sure that this region was under Cro-Magnon rule and
that their control extended over into Britain, where, it will be
recalled, a Cro-Magnon skeleton was found at Paviland, in
western Wales. Here, again, in Magdalenian times the Cro-
Magnon race was probably wide-spread over southern Britain.
At Bacon's Hole, near Swansea, Wales, there is a wall decoration
consisting of ten red bands, which, according to Breuil and Sollas,
may possibly be of Palaeolithic age. More definite is the Magda-
lenian industry observed at the Cresswell Crags, in Derbyshire ;
while near Torquay, Devonshire, is the famous station of Kent's
Hole, discovered in 1824, in which a bone needle has been found
and several harpoons with double rows of barbs belonging to the
late Magdalenian industry.
In Germany, whereas only three Solutrean stations have
been discovered,29 there are no less than fourteen Magdalenian
stations to attest the wide spread of that culture. Thus the
EXTENT OF THE MAGDALENIAN CULTURE 441
favorite grotto of Sirgenstein, near the centre of the Magda-
lenian stations on the upper waters of the Danube, although
abandoned in Solutrean times, was again entered by man during
the early Magdalenian culture stage. Coincident with the return
of man to this great grotto was the arrival of the banded lem-
ming {My odes torquatus), the herald of the cold tundra wave of
life in the far north. At the very same time man with the banded
lemming arrived at Schweizersbild, near the Lake of Constance ;
Fig. 241. Reindeer engraved around a piece of reindeer antler, from Kesslerloch, Switz-
erland. This is a unique instance of the portrayal of landscape in Palaeolithic
art. After Heim. Slightly more than three-quarters actual size.
at a slightly earlier period, with the dawn of Magdalenian cul-
ture, man entered the sister station of Kesslerloch. It certainly
appears that a cold moist climate accompanying the Buhl ad-
vance influenced all the Cro-Magnon peoples of this region just
north of the Alpine glaciers and compelled them to seek the
grottos and shelters. There are, however, some open stations
in this general region, for example, at Schussenried, Wiirttem-
berg; the Magdalenian culture layer is not found in a grotto, but
lies under a deposit of peat mingled with the remains of the
reindeer, horse, brown bear, and wolf. Again, among the best-
442 MEN OF THE OLD STONE AGE
known sites along the middle Rhine is the open-air station of
Andernach. Demonstrating the eastward distribution of the
art of engraving on ivory and bone is the presence in An-
dernach and in the grotto of Wildscheuer, near Steeten, on
the Lahn, of engravings of this character. Thus far these are
the only German stations in which such engravings have been
found.
Of especial interest also is the open Magdalenian c loess' sta-
tion of Munzingen, on the upper Rhine, because it proves that
the highest layers of the 'upper loess/ corresponding with the
dry or steppe period of climate, were contemporaneous with the
advanced or late Magdalenian industry, also because this final
' upper loess' stage about corresponds with the period when the
last of the arctic tundra mammals began to abandon central
Europe. It was at this critical geologic time that the late Mag-
dalenian culture began to draw to a close. Kesslerloch, Switzer-
land, has yielded a considerable number of engravings on bone,
including one of the finest examples of a browsing reindeer
(Fig. 241), and Schweizersbild also has yielded a considerable
number of rather crude engravings.
Frequented in Magdalenian times was that part of the Swabian
Jura lying between the headwaters of the Neckar and of the
Danube ; along the course of the Danube, from Propstfels, near
Beuron, in the southwest, to Ofnet, in the northeast, extend
the other stations of Hohlefels bei Hiitten, Schmiechenfels, and
Bocksteinhohle.
West of the Danube the industry was carried into the present
region of Bavaria, as indicated by the recent discovery of Kastl-
hang.30 Here, beginning with the early Magdalenian (Gourdanien
injerieur of the French school) and extending to the middle or
high Magdalenian (Gourdanien superieur), we find a complete
series of Magdalenian stations; the middle Magdalenian layer
is of exactly the same type as that found in the Abri Mege of
Dordogne and in the lower levels of the Grotte de la Mairie ;
the same culture stage is again observed in southern Germany
in the stations of Schussenquelle and of Hohlefels, and it extends
EXTENT OF THE MAGDALENIAN CULTURE 443
eastward into Austria in the station of Gudenushohle as well as
into several Moravian stations, for example, that of Kostelik.
These facts are of extraordinary interest, for they show that
the civilization, such as it was, of the Upper Palaeolithic was
very widely extended. This marks an important social charac-
teristic, namely, the readiness and willingness to take advantage
of every step in human progress, wherever it may have originated.
At this point, therefore, it is interesting to compare the Mag-
dalenian industry of Germany with that of France.31 Germany
shows the same technical and stylistic tendencies and the same
evolutionary direction as France. The mammalian life was, of
course, the same in both countries, for in each region the giant
types of mammals still survived, and the banded lemming of the
arctic appears in the sheltered valleys of the Dordogne as well
as in Belgium and in Germany. The vicissitudes of climate were
undoubtedly the same ; we observe the alternation of cold moist
climate in the early Magdalenian along the upper Danube as
well as in the early Magdalenian of the type station of La Made-
leine, Dordogne. Again, we observe the transition into the dry
cold climate in the steppe character of the fauna both along the
upper Rhine, at Munzingen, and also beneath the shelter station
of La Madeleine, as recorded by Peyrony.
More vital still for this community of industrial culture was
the community of race, for at Obercassel we find the same Cro-
Magnon type as that discovered beneath the sheltering cliffs of
Dordogne. It appears probable that the inventions of the cen-
tral region of Dordogne travelled eastward when we note the fact
that none of the prototypes of early forms of the harpoon which
were common in southern France occur in any of the stations
of central Europe, but the single-rowed harpoon is characteristic
of the middle Magdalenian all over Germany. Other primitive
Magdalenian bone implements, such as the bone spear point
with the cleft base, the batons, and the needles, are also of rare
occurrence in the German stations. In late Magdalenian times,
however, a complete community of culture is established, for the
industry of both countries in flint and bone appears to be very
444
MEN OF THE OLD STONE AGE
similar : flint microliths appear in increasing number and variety ;
beside the small flint flakes with blunted backs, numerous feather-
shaped flakes of Pre-Tardenoisian type are found, as well as the
types of graving flints. Some specialties of French Magdalenian
culture did not find their way into Germany; for example, the
graver of the ' parrot-beak ' type has been found in France but
has not been traced far eastward. In both countries, however,
Fig. 242. Entrance to the grotto of Kesslerloch, near Lake Constance. Photograph
by N. C. Nelson.
are found upper Magdalenian chisels of reindeer horn and per-
fected bone needles, batons, and harpoons with double rows of
barbs. On the other hand, works of art and decorative designs
in horn and bone are almost entirely wanting in German locali-
ties, with the exception of the stations of Andernach and Wild-
scheuer previously mentioned. In late Magdalenian times, both
in Germany and France, we find the Furasiatic forest fauna be-
coming more abundant.
The two famous Swiss stations of Kesslerloch and Schweizers-
EXTENT OF THE MAGDALENIAN CULTURE 445
bild, near Lake Constance, appear throughout Magdalenian times
to have been in very close touch with the cultural advances of
Dordogne. Kesslerloch32 has yielded 12,000 flints of small
dimensions, resembling in their succession those of the type
Fig. 243. The famous shelter station of Schweizersbilcl, under a protecting cliff of
limestone, near Lake Constance, Switzerland. On the right stands Dr. Jakob
Niiesch, who has devoted three years to the excavation and study of this site. Pho-
tograph by N. C. Nelson.
station of La Madeleine ; also needles, single and double har-
poons, dart-throwers, batons, as well as the fine engravings men-
tioned above ; bone sculpture is represented here in the unique
head of a musk-ox (Ovibos moschatus), in carvings of the reindeer
and of other animals on the batons and weapons of the chase.
Kesslerloch lies on the edge of a moderately wide valley, trav-
ersed by a brook ; in this sheltered, well-watered, hilly region, the
trees flourished and harbored the forest animals, while the gla-
ciers, retreating and leaving damp and stony areas, were closely
446 MEN OF THE OLD STONE AGE
followed by the tundra fauna ; the woolly rhinoceros and mam-
moth persisted here longer than in other parts of Europe ; the
horse of Kesslerloch is said to show resemblances to the Przewal-
ski horse of the desert of Gobi, in central Asia, and is consequently
referred to the steppe type. The development of the flints takes
place step by step with that of the sister cavern of Schweizersbild,
and in early Magdalenian times these flints are found associated
with the arrival of the great migration of the arctic tundra rodents,
the banded lemmings (My odes torquatus). A hearth with ashes
and coals and many charred bones of old and young mammals,
including the woolly rhinoceros, has been found here ; the animal
life altogether includes twenty-five species of mammals, among
them the woolly mammoth, woolly rhinoceros, reindeer, and
lion.
Less than four miles distant from Kesslerloch, in a small
valley about two miles north of Schaflhausen, is the other famous
Swiss station of Schweizersbild. The Cro-Magnons were at-
tracted to this spot by the protecting cliff of isolated limestone
rock rising sheer from the meadow-land, at the base of which is
a shelter facing southwest, with an entrance of about 30 feet
in height, commanding a wide view of the distant valley. In
the accumulations at the base of this shelter we find a complete
prehistory of the human, industrial, faunal, and climatic changes
of this region of Switzerland from early Magdalenian into Neo-
lithic times. It was not until the true early Magdalenian, after
both the Aurignacian and Solutrean stages had closed, that man
first found his way here during the Bilhl advance, the period of
the deposition of the Upper Rodent Layer with its cold arctic
and steppe fauna ;33 but from this time the grotto was occupied
at intervals until full Neolithic times. The beginning of these
industrial deposits is estimated by Nuesch as having occurred
between 24,000 and 29,000 years ago, but we have adopted a
somewhat lower and more conservative estimate. In descending
order the various layers of this shelter, as studied by Nuesch, are
as follows :
EXTENT OF THE MAGDALENIAN CULTURE 447
Section or the Schweizersbild Deposits
Neolithic
6. Layer of humous earth, between 15 and 19 inches in thickness, con-
taining Neolithic implements.
5. Gray culture layer, about 15 inches in thickness, including many fire-
hearths, ornaments of shell, polished Neolithic flints, and unglazed pottery.
The true forest fauna includes the brown bear, badger, marten, wolf, fox,
beaver, hare, squirrel, short-horned wild ox (Bos taurus brachyceros) , and
reindeer, also the domesticated goat and sheep.
Upper Palceolithic
4. Thin layer of forest-living rodents, principally squirrels. Split
bones and worked flints ; no carvings in bone or horn ; industry of late
Magdalenian or close of Magdalenian Upper Palaeolithic age ; evidences
that climate was changing, steppe conditions passing away, and forests be-
coming more dominant ; only a few steppe species ; the forest species in-
clude the reindeer, hare, pika, squirrel, ermine, and marten.
3. Yellow culture layer, steppe period, rich in fire-hearths and yielding
14,000 flints of middle [ ? and late] Magdalenian age ; engravings on rein-
deer antlers, ornaments of shells and teeth. Mixed fauna with steppe and
forest types predominant; of the few tundra forms, reindeer very abundant
and also arctic fox, but banded lemming and other tundra types entirely
lacking ; steppe and desert fauna includes the kiang, Persian maral deer,
P alias's cat (Felis manul), steppe horse, and steppe suslik; of alpine type,
the ibex ; numerous forest species, pine marten, beaver, squirrel, red deer,
roe-deer, and wild boar.
2. Arctic tundra rodent layer, 20 inches in thickness ; period of the
Buhl Postglacial advance; the banded lemming (Myodes torquatus) most
abundant, mingled with early Magdalenian flint and bone implements ; one
fire-hearth ; abundant tundra fauna, including all tundra types except the
Obi lemming, and the musk-ox (Ovibos moschatus) which is found in Kess-
lerloch; indications of a very cold, moist climate; the banded lemming,
arctic fox, arctic hare, reindeer, wolverene, ermine, also such forest forms
as the wolf, fox, bear, weasel, and a number of northern birds.
1. GraVel bed and old river deposit, recognized by Boule as belonging
to the moraines of the fourth glaciation.
This wonderful deposit of human artifacts and animal re-
mains gives us a complete registration of the changes of climate
in this region accompanying the changes of culture and the de-
velopment of the Magdalenian race.
448
MEN OF THE OLD STONE AGE
Turning our survey to the course of the Danube, we note
that several Magdalenian stations extend into the provinces of
Lower Austria, chief among them being both the open 'loess'
station of Aggsbach, and that of Gobelsburg; there is also the
Hundssteig near Krems, better known as the station of Krems,
and the cavern known as the Gudenushohle ; in the latter sta-
Fig. 244. The open loess station of Aggsbach, on the Danube, near Krems. After
Obermaier.
tion the characteristic batons, javelins, and bone needles have
been found.*
The cavern district of Moravia attracted a relatively large
population, and among the numerous stations are the grottos of
Kfiz, Zitny, Kostelik, Byciskala, Schoschuwka, Balcarovaskala,
Kulna, and Lautsch. Near the Russian border bone imple-
ments like those of Gudenushohle on the Danube have been
found at the station of Kulna, and the industrial stratification of
* J. Bayer34 has lately expressed the opinion that the industry of the open ' loess '
stations of Munzingen, Aggsbach, and Gobelsburg is not really of Magdalenian age, but
represents an atypical Aurignacian.
DECLINE OF THE MAGDALENIAN CULTURE 449
Sipka is very clear. Not far from Cracow, across the Russian
border, the caverns in the region of Ojcow were entered by men
carrying the Magdalenian culture. Another
site in Russia is the grotto of Maszycka, and
characteristic Magdalenian harpoons, needles,
and batons de commandement with other im-
plements have also been found to the eastward,
in the neighborhood of Kiev, in the Ukraine.
Decline of the Magdalenian Culture
e.v'-.i;
%\
hif.'
litim
I
pi
'i:\i
y r-
The highest point touched by the Cro-
Magnon race in the middle or high Magda-
lenian appears to correspond broadly with the
cold arid period of climate in the interval be-
tween the Buhl and Gschnitz advances in the
Alpine region, during which the steppe mam-
mals spread widely over southwestern Europe.
The saiga antelope, for example, a highly
characteristic steppe type, is represented in
one of the most skilful bone carvings found
in the late Magdalenian layers of Mas d'Azil ;
also the steppe type of horse is frequently re-
presented in the most advanced engravings of
late Magdalenian times. How far this cold,
relatively dry climate influenced the artistic
and creative energy of the Cro-Magnons is
largely a matter of conjecture. The entirely
independent records of La Madeleine, of
Schweizersbild, and of Kesslerloch concur
in associating the highest stage of Magda-
lenian history of art with the predominance
of the steppe fauna and evidences of a cold
dry climate. That the mammoth still
abounded is seen in the mammoth engravings
which are superposed on those of the bison in Font-de-Gaume.
The succeeding life period is that of the retreat of the tundra
Fig. 245. Front and
side views of a saiga
antelope carved upon
a bone dart-thrower
from the Magdale-
nian deposits of Mas
d'Azil. After Piette.
450 MEN OF THE OLD STONE AGE
and steppe mammals and of the increasing rarity of the reindeer
and of the mammoth in southwestern Europe ; it corresponds
broadly with the returning cold and moist climate of the second
Postglacial advance known in the Alps as the Gschnitz stage.
With the spread of the forests and the retreat to the north of the
reindeer, the principal source both of the supply of food and
clothing and of all the bone implements of industry and of the
chase, a new set of life conditions may have gradually become
established. If it is true, as most students of geographical con-
ditions and of the climate maintain, that Europe at the same time
became more densely forested, the chase may have become more
difficult, and the Cro-Magnons may have begun to depend more
and more upon the life of the streams and the art of fishing. It
is generally agreed that the harpoons were chiefly used for fish-
ing and that many of the microlithic flints, which now begin to
appear more abundantly, may have been attached to a shaft for
the same purpose. We know that similar microliths were used
as arrow points in predynastic Egypt.
Breuil35 observes very significant industrial changes in clos-
ing Magdalenian times : first, the beginning of small geometric
forms of flints suggesting the Tardenoisian types ; second, the
occasional use of stag horn in place of reindeer horn ; third, a
modification in the form of bone implements toward the pat-
terns of Azilian times ; fourth, the rapid decline— one may almost
say sudden disappearance — of the artistic spirit. Schematic and
conventional designs begin to take the place of the free realistic
art of the middle Magdalenian.
Thus the decline of the Cro-Magnons as a powerful race may
have been due partly to environmental causes and the aban-
donment of their vigorous nomadic mode of life, or it may be
that they had reached the end of a long cycle of psychic develop-
ment, which we have traced from the beginning of Aurignacian
times. We know as a parallel that in the history of many civi-
lized races a period of great artistic and industrial development
may be followed by a period of stagnation and decline without
any apparent environmental causes.
CRO-MAGNON DESCENDANTS 451
Cro-Magnon Descendants in Modern Europe
We might attribute this great change, which affected all of
western Europe, to the extinction of the Cro-Magnon race were
it not for the existing evidence that the race survived throughout
the Azilian-Tardenoisian or close of the Upper Palaeolithic. On
the close of the Palaeolithic the race broke up throughout western
Europe into many colonies, which can perhaps be traced into
Neolithic and even into recent times. The anatomical evidence
for this survival theory chiefly consists of the highly character-
istic form of the head.
In Europe a very broad face and a long, narrow cranium is
such an infrequent combination that anthropologists maintain
that it affords a means of identifying the descendants of the pre-
historic Cro-Magnon race wherever they persist to-day. Since
Dordogne was the geographic centre of the race in Upper Palae-
olithic times, is it merely a coincidence that Dordogne is still
the centre of a similar type ? Ripley^ has given us a valuable
resume of our present knowledge of this subject. The most
significant trait of the long-headed people of Dordogne is that in
many cases the face is almost as broad as in the normal Alpine
round-headed type ; in other words, it is strongly disharmonic ;
in profile the back part of the head rises and in front view the
head is narrowed at the top ; the skull is very low-vaulted ; the
brow ridges are prominent ; the nose is well formed ; the cheek-
bones are prominent, and the powerful cheek muscles give a
peculiarly rugged cast to the countenance. The appearance,
however, is not repellent, but more often open and kindly. The
men are of medium height, but very susceptible to environment
as regards stature ; they are tall in fertile places, and stunted in
less prosperous districts. They are not degenerate at all, but
keen and alert of mind. The present people of Dordogne agree
with but one other type of men known to anthropologists, namely,
the ancient Cro-Magnon race. The geographical evidence that
here in Dordogne we have to do with the survivors of the real
Cro-Magnon race seems to be sustained by a comparison of the
452 MEN OF THE OLD STONE AGE
characteristics of the prehistoric skulls found at Cro-Magnon,
Laugerie Basse, and elsewhere in Dordogne, with the heads of
the types of to-day. The cranial indices of the prehistoric skulls,
varying from 70 per cent to 73 per cent, correspond with indices
of the living head of 72 per cent to 75 per cent. None of the
people of Dordogne are quite so long-headed as this, the aver-
age index of the living head in an extreme district being 76
per cent ; but within the whole population there are much lower
indices.
The probability of direct descent becomes stronger when we
consider the disharmonic low-skulled shape of the Cro-Magnon
head and the remarkable elongation of the skull at the back.
In the prehistoric Cro-Magnons the brows were strongly devel-
oped, the eye orbits low, the chin prominent. The facial type
has been characterized by de Quatrefages37 as follows: "The
eye depressed beneath the orbital vault ; the nose straight rather
than arched ; the lips somewhat thick, the jaw and the cheek-
bones strongly developed, the complexion very brown, the hair
very dark and growing low on the forehead — a whole which,
without being attractive, was in no way repulsive."
In southern France we observe a continuity not only of the
head form but of the prevalence of black hair and eyes. Why
should this Cro-Magnon type have survived at this point and
have disappeared elsewhere ? In order to consider the particular
cause of this persistence of a Palaeolithic race, we must, with
Ripley, broaden our horizon, and consider the whole southwest
from the Mediterranean to Brittany as a unit.
The survival is partly attributed to favorable geographical
environment and partly to geological and racial barriers. On
the north the intrusion of the Teutonic race was shut off and
competition was narrowed down to the Cro-Magnon and Alpine
types.
If the people of Dordogne are veritable survivors of the Cro-
Magnons of the Upper Palaeolithic, they certainly represent the
oldest living race in western Europe, and is it not extremely
significant that the most primitive language in Europe, that of
CRO-MAGNON DESCENDANTS 453
the Basques of the northern Pyrenees, is spoken near by, only
200 miles to the southwest? Is there possibly a connection
between the original language of the Cro-Magnons, a race which
once crowded the region of the Cantabrian Mountains and the
Pyrenees, and the existing agglutinative language of the Basques,
which is totally different from all the European tongues? This
hypothesis, suggested by Ripley,38 is very well worth considering,
for it is not inconceivable that the ancestors of the Basques con-
quered the Cro-Magnons and subsequently acquired their lan-
guage.
The prehistoric Cro-Magnon men would seem, therefore, to
have remained in or near their early settlements through all the
changes of time and the vicissitudes of history. "It is, per-
haps," observes Ripley, "the most striking instance known of
a persistency of population unchanged through thousands of
years."
The geographic extension of this race was once very much
wider than it is to-day. The classical skull of Engis, Belgium,
belongs to this type. It has been traced from Alsace in the east
to the Atlantic in the west. Ranke asserts that it is to be found
to-day in the hills of Thuringia, and that it was a prevalent
type there in the past. Verneau considers that it was the type
prevailing among the extinct Guanches of the Canary Islands.
Collignon39 has identified it in northern Africa, and regards
the Cro-Magnons as a subvariety of the Mediterranean race,
an opinion consistent at least with the archaeological evidence
that this race came into Europe with the Aurignacian culture,
which was circum-Mediterranean in distribution. Traces of Cro-
Magnon head formation are found among the living Berbers.
At present, however, this race is believed to survive only in
a few isolated localities, namely, in Dordogne, at a small spot
in Landes, near the Garonne in southern France, and at Lan-
nion in Brittany, where nearly one- third of the population is
of the Cro-Magnon type. It is said to survive on the island
of Oleron off the west coast of France, and there is evidence of
similar descent to be found among the people of the islands
454 MEN OF THE OLD STONE AGE
of northern Holland. The people of Trysil, on the Scandina-
vian peninsula, are characterized as having dishannonic fea-
tures, possibly representing an outcrop of the Cro-Magnon
type.
Our interest in the fate of the Cro-Magnons is so great that
the Guanche theory may also be considered; it is known to
be favored by many anthropologists: von Behr, von Luschan,
Mehlis, and especially by Verneau. The Guanches were a race
of people who formerly spread all over the Canary Islands and
who preserved their primitive characteristics even after their
conquest by Spain in the fifteenth century. The differences
from the supposed modern Cro-Magnon type may be mentioned
first. The skin of the Guanches is described by the poet Viana
as light-colored, and Verneau considers that the hair was blond
or light chestnut and the eyes blue; the coloring, however, is
somewhat conjectural. The features of resemblance to the an-
cient Cro-Magnons are numerous. The minimum stature of the
men was 5 feet 7 inches, and the maximum 6 feet 7 inches;
in one locality the average male stature was over 6 feet. The
women were comparatively small. The most striking char-
acters of the head were the fine forehead, the extremely long
skull, and the pentagonal form of the cranium, when seen from
above, caused by the prominence of the parietals — a Cro-Mag-
non characteristic. Among the insignia of the chiefs was the
arm-bone of an ancestor ; the skull also was carefully preserved.
The offensive weapons in warfare consisted of three stones, a
club, and several knives of obsidian ; the defensive weapon was
a simple lance. The Guanches used wooden swords with great
skill. The habitation of all the people was in large, well-shel-
tered caverns, which honeycombed the sides of the mountains;
all the walls of these caverns were decorated ; the ceilings were
covered with a uniform coat of red ochre, while the walls were
decorated with various geometric designs in red, black, gray,
and white. Hollowed-out stones served as lamps. We may
conclude with Verneau that there is evidence, although not of
a very convincing kind, that the Guanches were related to the
CRO-MAGNON DESCENDANTS
455
Cro-Magnons.40 His observations on these supposed Cro-Mag-
nons of the Canary Islands are cited in the Appendix, Note V.
We regret that Verneau in his memoir41 does not present his
more recent views in regard to the prehistoric distribution of
this great race.
(i) Breui], 191 2.7, p. 203.
(2) Op. cit., p. 205.
(3) James, 1902. 1.
(4) Heim, 1 894.1, p. 184.
(5) Schmidt, 1912.1, p. 262.
(6) Fraunholz, 191 1.1.
(7) Geikie, 1914.1, pp. 25, 26.
(8) Boule, 1 899. 1.
(9) Breuil, 191 2.7, pp. 203-205.
(10) Obermaier, 191 2.1, pp. 341, 342.
(11) Martin, R., 1914.1, pp. 15, 16.
(12) Verworn, 191 4.1.
(13) Op. cit., p. 646.
(14) Breuil, 1912.7, p. 201.
(15) Lartet, 1875. 1.
(16) Breuil, 1912.7, p. 213.
(17) Schmidt, 191 2.1, p. 136.
(18) Breuil, op. cit., pp. 216, 217.
(19) Breuil, 1909.3.
(20) Op. cit., p. 410.
(21) Cartailhac, 1906. 1, pp. 227, 228.
(22) Riviere, 1897. 1; 1897.2.
(23) Reinach, 1913.1.
(24) Breuil, 191 2.1, p. 202.
(25) Cartailhac, 1908. 1.
(26) Capitan, 1908. 1, pp. 501-514.
(27) Ibid., 1910.1, pp. 59-132.
(28) Breuil, 1912.1, pp. 196, 197.
(29) Schmidt, 1912.1, p. 116.
(30) Fraunholz, 1911.1.
(31) Schmidt, 1912.1, p. 154.
(32) Dechelette, 1908. 1, vol. I, pp.
191-194.
(33) Nehring, 1 880.1; 1 896.1.
(34) Bayer, 1912.1, pp. 13-21.
(35) Breuil, 1912.7, pp. 212, 216.
(36) Ripley, 1899. 1, pp. 39, 165, 173,
174-179, 211, 406.
(37) Op. cit., p. 176.
(38) Op. cit., p. 181.
(39) Collignon, 1 890.1.
(40) Verneau, 1891.1.
(41) Ibid., 1906. 1.
North Africa and Spain
Before continuing with Chapter VI the reader should care-
fully study the note on the Capsian flint industry (see Ap-
pendix, Note XI, p. 514) of Spain and northwest Africa, of
which the type station is Gafsa, a place about 180 miles south-
west of the city of Tunis in the region lying between Tripoli
and Algiers now known as Tunis. It would appear that this
part of Africa was probably the home of the Tardenoisian in-
dustry described on p. 465.
The connection between Spanish and North African life in
Palaeolithic times has recently been fully described by Hugo
Obermaier in his very interesting work, El Hombre fosil, pub-
lished in Madrid in 19 16.
CHAPTER VI
CLOSE OF THE OLD STONE AGE — INVASION OF NEW RACES —
HISTORY OF THE MAS D'AZIL, OF FERE-EN-TARDENOIS — FOREST
ENVIRONMENT AND LIFE — ORIGIN OF THE AZILIAN-TARDENOI-
SIAN CULTURE — CHARACTERS AND CUSTOMS OF THE NEW RACES
— TRANSITION TO THE NEOLITHIC AND RELATIONS OF THE OLD
AND NEW RACES — APPARENT CHIEF LINES OF HUMAN DESCENT
AND OF HUMAN MIGRATION INTO WESTERN EUROPE.
We have now reached the very close of the Old Stone Age,
a period which is believed to extend between 10,000 and 7,000
years before the present era. The entrance to the final cultures
of the Upper Palaeolithic, known as the Azilian-Tardenoisian,
marks a transition even more abrupt than that witnessed in any
preceding stage. It is not a development; it is a revolution.
The artistic spirit entirely disappears ; there is no trace of animal
engraving or sculpture ; painting is found only on flattened
pebbles or in schematic or geometric designs on wall surfaces.
Of bone implements only harpoons and polishers remain, and
even these are of inferior workmanship and without any trace
of art. The flint industry continues the degeneration begun in
the Magdalenian and exhibits a new life and impulse only in
the fashioning of the extremely small or microlithic tools and
weapons known as 'Tardenoisian.' Both bone and flint weapons
of the chase disappear, yet the stag is hunted and its horns are
used in the manufacture of harpoons. This is the 'Age of the
Stag,' the final stage of the 'Cave Period' in western Europe, and
is subsequent to the 'Age of the Reindeer' in the south.
It would appear as if the very same regions formerly occu-
pied by the great hunting Cro-Magnon race from Aurignacian
to Magdalenian times were now inhabited by a race or races
largely employed in fishing. The country is thickly forested.
456
INVASION OF NEW RACES 457
The climate is still cold and extremely moist, and human life
everywhere is in the grottos or entrances to the caverns.
Invasion of Four New Races in Closing Upper Paleolithic
Times
How far this revolution is due to the decline of the Cro-
Magnon race and how far to the invasion of one or more new
races is very difficult to determine in the absence of the anatom-
ical evidence derived from skeletal remains. Two new races
had certainly found their way along the Danube as shown in
the burials of Of net, in eastern Bavaria ; one is extremely broad-
headed and perhaps of central Asiatic origin, while the other is
extremely long-headed and perhaps of southerly or Mediter-
ranean origin. It is possible that these two races correspond
respectively with the easterly and southerly industrial influences
which are observed in the Azilian-Tardenoisian stage. The
former is the first brachy cephalic race to enter western Europe,
for it will be recalled that all the previous races, the Cro-Magnons,
the Briinns, and the Neanderthals, are dolichocephalic. The
long-headed race found at Ofnet is very clearly distinguished
from the disharmonic long-headed Cro-Magnon race by the nar-
rowness of the face ; in other words, it is an harmonic type of
head and face, which may have been Mediterranean in origin,
like the so-called ' Mediterranean race' of Sergi.
This fresh invasion of western Europe by two races arriving
by one or more of the great migration routes from the vast
Eurasiatic mainland to the east, races with a relatively high brain
development, is certainly one of the most surprising features of
the close of the Palaeolithic Period, for we have long been accus-
tomed to think that these fresh easterly and southerly invasions
began only in Neolithic times.
As the Upper Palaeolithic draws to an end, there is, according
to Breuil, still another industrial influence making itself felt:
it comes from the northeast along the shores of the Baltic.
Putting together all the fragmentary evidence which we
possess, we may regard western Europe at the close of the Old
458 MEN OF THE OLD STONE AGE
Stone Age as peopled by four and possibly by five distinct races,
as follows :
5. Arriving late in Palaeolithic times, a race along the shores of the
Baltic, known only by its Maglemose industry; possibly a Teutonic race.
4. A south Mediterranean race, known only by its Tardenoisian in-
dustry, migrating along the northern shores of Africa and spreading over
Spain; with a conventional and schematic art; probably an advance wave
of the true 'Mediterranean' race of Sergi; possibly identical with race 3
below. (The same as Race 4, p. 278.)
3. A long-headed race found at Of net, in eastern Bavaria; possibly
a branch of the true ' Mediterranean ' race 4 above, but not related to the
Briinn. (Possibly the same as Race 4.)
2. The newly arriving Furfooz-Grenelle race, broad-headed; known
along the Danube at Of net, in eastern Bavaria, and northward in Belgium;
possibly a branch of the 'Alpine' race. (The same as Race 5, p. 278.)
1. The surviving Cro-Magnons, in a stage of industrial decline, pur-
suing the Azilian industry, probably inhabiting France and northern Spain.
The broad-headed Ofnet race mentioned above is apparently
the same as the Furfooz-Grenelle race, and may also correspond
with the existing Alpine- Celtic race of western Europe. The
long-headed race of Ofnet may correspond with the existing
1 Mediterranean ' race of Sergi.
The presence of the Cro-Magnon race in western Europe
during Azilian-Tardenoisian times is not sustained, so far as we
know, by any anatomical evidence, but is suggested by the mode
of burial of two skeletons found by Piette in the Azilian deposits
of the station of Mas d'Azil. This burial, like that of Ofnet, is
typical of Upper Palaeolithic and not of Neolithic times. These
skeletons lay in the ' Azilian' layer (VI) described below. As
the smaller bones were missing, Piette concluded that the re-
mains had been for some time exposed to the weather before
burial, and that the larger bones had been scraped and cleaned
with flint knives, and then colored red with oxide of iron before
interment. According to other authorities, the traces of scrap-
ing and cleaning are doubtful ; there can be no question, how-
ever, that the separation of the bones of the skeleton and the
use of coloring matter constitute strong evidence that this
Azilian burial was the work of members of the Cro-Magnon race.
MAS D'AZIL 459
In addition to what we have said as to the survival of the
Cro-Magnon race in the preceding chapter, the opinion of Car-
tailhac1 may be cited: "The race of Cro-Magnon is well de*
termined. There is no doubt about their high stature, and To-
pinard is not the only one who believes that they were blonds.
We have traced them through the 'Reindeer Period ' into the
Neolithic Epoch, where they were widely distributed and posi-
tively related either to the ancient or actual populations of mod-
ern France, being especially characteristic of our region [France]
and of the western Mediterranean. While the race of Cro-Mag-
non predominated in the south and in the west, that of Furfooz
predominated in the northeast of France and in Belgium. These
brachycephals were probably brown-haired or of dark coloring."
But before observing further the characters of these four or
five races, let us examine their industries.
Discovery of the Azilian Type Station
As remarked above, it is believed that these industries pre-
vailed between 7,000 and 10,000 years before our era, that is,
between the close of Magdalenian times and the beginning of the
Neolithic or New Stone Age. This transition period corresponds
with the interval in which the Azilian-Tardenoisian culture swept
all over western Europe and completely replaced the Magda-
lenian. From Castillo in the Cantabrian Mountains of northern
Spain to Ofnet on the upper Danube there is a complete replace-
ment by this new culture. The Magdalenian culture does not
linger anywhere ; it is totally eliminated ; the suddenness of
the change both in the animal life and in the industry is nowhere
more clearly indicated than at the type station of Mas d\\zil in
southern France, which may now be described.
In 1887 Edouard Piette commenced his exploration of the
deposits in the great cavern of Mas d'Azil. This station takes
its name from the little hamlet of Mas d'Azil in the foot-hills of
the Pyrenees about forty miles southwest from Toulouse. Here
the River Arize winds for a quarter of a mile through a lofty
natural tunnel traversed by the highway from St. Girons to
460
MEN OF THE OLD STONE AGE
Carcassonne. A rich layer of Magdalenian deposits first at-
tracted Piette's attention, and he found here some of the finest
examples of late Magdalenian art, but above these deposits he
discovered a hitherto unrecognized industrial stage, to which
he gave the name Azilian. The Azilian layers yielded over one
thousand specimens of flattened and double-barbed harpoons
Fig. 246. Western entrance to the great station of Mas d'Azil. "Here the River Arize
winds for a quarter of a mile through a lofty natural tunnel traversed by the high-
way from St. Giroi\s to Carcassonne." Photograph by N. C. Nelson.
made of the horns of the stag, thus widely differing from the late
Magdalenian harpoons which are rounded and made of the horns
of the reindeer. The entire succession of deposits, as explored
by Piette, is an epitome of the prehistory of Europe from early
Magdalenian times to the Age of Bronze, and should be compared
with the successive deposits of Castillo (p. 164), Sirgenstein (p.
202), Ofnet (p. 476), and Schweizersbild (p. 447).
The Mas d'Azil section is as follows:
MAS D'AZIL 461
Prehistoric and Neolithic
LX. Iron implements, pottery of the Gauls. At the top Gallo-Roman
remains, glass and glazed pottery.
VIII. Middle Neolithic and Age of Bronze; layer of pottery, polished
stone implements, traces of copper and of bronze.
VII. Dawn of the Neolithic. Fauna includes the horse, urus, stag,
and wild boar. Chipped and polished flints, awls and polishers in bone;
harpoons rare. Beginnings of pottery.
Upper Paleolithic
VI. Azilian, red archaeological layer, masses of peroxide of iron. Ex-
tremely moist climate. Broad flat harpoons of stag horn perforated at the
base, numerous flattened and painted pebbles (galets), flints of degenerate
Magdalenian form, especially small rounded planers and knife flakes, awls
and polishers in bone. No trace of reindeer in the fire-hearths ; stag abun-
dant, also roe-deer and brown bear; wild boar, wild cattle, beaver, a variety
of birds. No trace of polished stone implements. Interred in this layer,
beneath the deposits of streaked cinders and quite undisturbed, two human
skeletons were found, which Piette believed had been macerated with flints
and then colored red with peroxide of iron.
V. Sterile finely stratified loam layer, a flood deposit of the River Arize.
IV. Late Magdalenian culture layer; twelve double-rowed harpoons
made of reindeer horn, a few fashioned from stag horn; numerous engrav-
ings and sculptures in bone. Remains of the reindeer rare in the hearths;
those of the royal stag (Cervus elaphus) abundant.
III. A sterile flood deposit of the River Arize.
II. Middle and Early Magdalenian culture layers, with barbed
harpoons of reindeer horn; flint implements of early Magdalenian type,
bone needles. Bones of the reindeer abundant.
I. Gravel deposits. Interspersed fire-hearths.
The total thickness of these culture deposits is 8.03 m., or
26 feet 4 inches. The Azilian type layer (VI) containing flat
harpoons of stag horn and painted pebbles, intercalated between
the deposits of the Reindeer Age and the Neolithic layers, is, on
account of its stratigraphic position, the most interesting and
instructive of all the sites representing this phase of transition ;
and Piette was fully justified in giving to the corresponding cul-
ture period the name of Azilian.2
The transformation of art and industry, indicated in the
Azilian culture layer, is as decided as that in the animal life.
462
MEN OF THE OLD STONE AGE
We observe in this layer no trace of the animal engravings or
sculptures which occur so abundantly in the late Magdalenian
layer below ; the use of pigments is confined to the paintings of
schematic or geometric figures on the flattened pebbles. There
is no suggestion of art in any of the bone implements, and the
harpoons of stag horn are rudely fashioned ; this type of harpoon
appears to be the chief survivor of the rich variety erf imple-
:291 288 290 287
Fig. 247. Typical Azilian harpoons of stag horn. After de Mortillet. 287. A single-
rowed harpoon from Mas d'Azil. 288. Harpoon with perforated base from the shelter
of La Tourasse, Haute-Garonne. 289. Double-rowed harpoon from the same shelter.
290. A similar harpoon with the barbs alternate instead of opposite, from Mas d'Azil.
291. Harpoon with triangular base and round perforation from the Grotte de la Vache,
near Tarascon. All one- third actual size, except 291, which is four-ninths actual size.
ments noted in the Magdalenian layer below. The stag horn
harpoon, moreover, is fashioned with far less skill than the
beautiful Magdalenian harpoons ; like them it has two rows of
barbs, but they are not cut with the same delicacy and exactness.
As to the form of the new model, it is explained by the nature of
the new material ; the interior of the stag horn being composed
of a spongy tissue, could not be utilized as could the harder and
more compact interior of the reindeer horn; the craftsman,
therefore, was obliged to fashion his harpoon out of the exterior
of one side of the stag horn, and in consequence to make it flat.
There are no bone needles, no javelins or sagaies; nor are there
any of the beautifully carved weapons of bone. There is also a
MAS D'AZIL 463
reduction in the uses to which the split bones are put, such as
the large lissoirs or polishers. The bone implements appear to
be derived from an impoverished late Aurignacian stage; the
same is true of the flint implements, for we observe a return of
the keeled scraper (grattoir carene). There is also a return of
certain types of graving tools and of the knife-like form of the
flake ; even some of the small geometric types of flints resemble
those of the Aurignacian levels.
The many shells of the moisture-loving snail Helix nemoralis,
found in the fire-hearths of Mas d'Azil are proofs of the humidity
of the climate, a fact confirmed by the contemporary flood de-
posits of the Arize. The frequent and heavy rains drove the
last few representatives of the steppe fauna away to the north.
These climatic conditions favored the formation of peat-bogs,
so frequent to-day in the north of France, and also the growth
of vast forests, inhabited by the stag, which extended over the
whole country.
The pebbles of Mas d'Azil are painted on one side with per-
oxide of iron, a deposit of which is found in the neighborhood of
the cave. The color, mixed in shells of Pecten, or in hollowed
pebbles or on flat stones, was applied either with the finger or
with a brush. The many enigmatic designs consist chiefly of
parallel bands, rows of discs or points, bands with scalloped
edges, cruciform designs, ladder-like patterns (scalariform) such
as are found in the 'Azilian' engravings and paintings of the
caverns, and undulating lines. These graphic combinations re-
semble certain syllabic and alphabetic characters of the iEgean,
Cypriote, Phoenician, and Greco-Latin inscriptions. However
curious these resemblances may be, they are not sufficient to
warrant any theory connecting the signs on the painted pebbles
of the Azilians with the alphabetic characters of the oldest known
systems of writing.3 Piette attempted to explain some of the
exceedingly crude designs on these pebbles as a system of nota-
tion, others as pictographs and religious symbols, and some few
as genuine alphabetical signs, and suggested that the cavern of
Mas d'Azil was an Upper Palaeolithic school where reading, reck-
(•) cS^i> ^^
(J) I* Ol *mm
Fig. 248. Azilian gahls colories, flat, painted pebbles, from the type station of Mas
d'Azil. After Piette.
FERE-EN-TARDENOIS 465
oning, writing, and the symbols of the sun were learned and
taught. The very wide distribution of these symbolic pebbles
and the painting of similar designs on the walls of the caverns
certainly prove that they had some religious or economic signif-
icance, which may be revealed by subsequent research.
The Tardenoisian Type Station
Turning from the region of the Pyrenees in Azilian times, we
observe the region lying between the Seine and the Meuse in
northern France as the scene of a contemporary industry. At
the station of Fere-en-Tardenois, in the Department of the
Aisne, is found an especially large number of the pygmy flints f
these present various geometric forms, including the primitive
triangular, as well as the rhomboidal, trapezoidal, and semicir-
cular; together, they were designated by de Mortillet as Tar-
denoisian flints, and in 1896, in monographing this microlithic
flint industry, he traced them throughout France, Belgium, Eng-
land, Portugal, Spain, Italy, Germany, and Russia, also along
the southern Mediterranean through Algiers, Tunis, Egypt, and
eastward into Syria and even India.
These geometric flints were at first attributed to a primitive
invasion which was supposed to have occurred at the beginning
of Neolithic times; thus the Tardenoisian industry was con-
sidered as contemporaneous with that of the Campignian, which
is early Neolithic. It was further observed that the topograph-
ical location of the stations closely followed the borders of
ocean inlets, or of river courses, and when the food materials
found in the hearths were compared, it appeared that these
flints were used principally by fishermen or tribes subsisting
upon fish. From an examination of the flints, it would appear
that a very large number of them were adapted for insertion in
small harpoons, or that those of grooved form might even have
been used as fish-hooks. Thus the picture was drawn of a popu-
lation of fishermen. The Tardenoisian, therefore, was for a
long time regarded as contemporaneous with the early Neolithic
466 MEN OF THE OLD STONE AGE
rather than with the close of Palaeolithic times, but as explora-
tion proceeded it was found that neither the remains of domestic
animals nor any traces of pottery occur in any of these Tarde-
noisian deposits, which consequently have nothing in common
with the true Neolithic culture.
The problem was finally solved in 1909, when the grotto of
Valle near Gibaja, Santander, in northern Spain, was discovered
by Breuil and Obermaier.5 Here was a classic Azilian deposit
containing all the well-known Azilian types of bone implements,
such as fine harpoons, carvings in deer horn, bone javelins, polish-
ers of deer bone, flint flakes resembling those of the late Magda-
lenian, also microlithic flints of typical geometric Tardenoisian
form. This discovery established the fact that the lower levels
of the Tardenoisian industry were not really to be distinguished
from the Azilian, for here beneath layers with painted pebbles
and harpoons of Azilian style were harpoons with single and
double rows of barbs of Magdalenian pattern, but cut in stag
horn instead of reindeer horn.
The mammalian life in this true Azilian-Tardenoisian layer
includes the chamois, roe-deer, wild boar, and urus, or wild cattle.
In a layer just below, which represents the close of the Magda-
lenian industrial period, there are found, although rarely, remains
of the reindeer, an animal hitherto unknown in this part of
Spain, also the wild boar, the bison, the ibex, and the lynx.
After this discovery it could no longer be questioned that the
Azilian and Tardenoisian were contemporary.
As to the relation of these two industries, Breuil remarks6
that the prolongation of the Tardenoisian types of flints is ob-
served in Italy and in Belgium, but neither the term 'Tarde-
noisian' nor the term 'Azilian' is sufficiently comprehensive to
embrace the totality of these little industries, which will finally
be distinguished clearly from each other. Of the two the Azilian
represents the prolongation of an ancient period of industry, the
progress of which was apparently from south to north, as we can
trace the distribution of the characteristic flat harpoons of deer
horn from the Cantabrian Mountains and the Pyrenees, through
AZILIAN-TARDENOISIAN CULTURE
467
southern and central France, to Belgium, England, and the
western coast of Scotland. The later industrial phase, the Tar-
denoisian, with its geometric trapeziform flints, originally ap-
pears along the southern Mediterranean in Tunis and to the
Fig. 249. Small geometric flints characteristic of the Tardenoisian industry. After de
Mortillet. 295 to 303, 321, 322, 326. From various sites in northern France. 311.
Uchaux, Vaucluse, France. 305, 315, 320. Valley of the Meuse, Belgium. 312,
313. Cabeco da Arruda, Portugal. 304, 314. Italy. 317, 318, 329. Tunis. 325.
Egypt. 306, 310, 324, 328. Kizil-Koba, Crimea. 307 to 309, 316, 319, 323, 327.
India. All one-half actual size.
eastward in the Crimea, while in France it represents a final
phase of the Palaeolithic, closely approaching the period of
the earliest Neolithic or pre-Campignian hearths common along
the Danube and observed in the vicinity of Liege. Thus the
most comprehensive term by which to designate the ensemble
of these implements, in Europe at least, would be Azilian-
Tardenoisian.
468 MEN OF THE OLD STONE AGE
Environment and Mammalian Life
It appears that the chief geographic change during this period
was a subsidence of the northern coasts of Europe and an ad-
vance of the sea causing the circulation of warm oceanic currents
and a more humid climate favorable to reforestation.
To the north, in Belgium, the tundra fauna lingered during the
extension of the early Tardenoisian industry, for here we still
find remains of the reindeer, the arctic fox, and the arctic hare
mingled in the fire-hearths with flints of Tardenoisian type.
This, observes Obermaier, constitutes proof that the Tarde-
noisian, with the Azilian, must be placed at the very close of
Postglacial time and with the final stage of Upper Palaeolithic
industry.
To the south, in the region of Dordogne and the Pyrenees,
the tundra fauna had entirely disappeared, as well as that of the
steppes and of the alpine heights ; the prevailing animal in the
forests is the royal stag, adapted to forests of temperate type
and associated with the Eurasiatic forest and meadow fauna
which now dominated western Europe.
The only survivor of the great African- Asiatic fauna is the
lion, which appears in the late Palaeolithic stations in the region
of the Pyrenees; the arctic wolverene also gives the fauna a
Postglacial aspect, for, like the lion, it is never found in central
or western Europe after the close of Upper Palaeolithic times.
Other enemies of the herbivorous fauna were the wolf and the
brown bear.
Besides the red deer, or stag, the forests at this time were filled
with roe-deer. To the south in the Pyrenees the moose still sur-
vived, and to the north there were still found herds of reindeer
which survived in central Europe as late as the twelfth century.
Wild boars were numerous, and in the streams were found the
beaver and the otter. In the forest borders and in the meadows
hares and rabbits were abundant. Through the forests and
meadows of southern France and along the borders of the Danube
ranged the wild cattle (Bos primigenius) . It would appear from
MAMMALIAN LIFE 469
our limited knowledge of the life of Azilian-Tardenoisian times
that bison were found chiefly in the northern parts of Europe.
There is little direct evidence in regard to the wild horse, the re-
mains of which do not occur in the hearths of Azilian times.
Our knowledge of the life of the Spanish peninsula at a period
closely succeeding this is indirectly derived from the animal
frescos in certain caverns of northern Spain, which have been
attributed to the early Neolithic but are now referred rather
to the late Palaeolithic. Here are found representations of
the ibex, the stag, the fallow deer, the wild cattle, and also of
the wild horses. This would indicate that wild horses were still
roaming all over western Europe at the close of Upper Palae-
olithic times. The presence of the moose in late Palaeolithic
times at Alpera, on the high plateaus of Spain, has been deter-
mined ; this animal has also been found in the Pyrenees during
the Azilian stage.7
The great contrast between the mammalian life of Magda-
lenian and that of Azilian-Tardenoisian times is witnessed in
the stations along the upper Danube, as described by Koken.8
In Hohlefels, Schmiechenfels, and Propstfels, associated with
implements of the late Magdalenian industry, are found ten
types of animals belonging to the forests and four characteristic
of the forests and meadows, or fourteen species altogether.
With these are mingled two alpine forms, the ibex and the alpine
shrew; also two types of mammals belonging to the steppes,
and no less than six mammals and birds from the tundras, namely,
the reindeer, the arctic fox, the ermine, the arctic hare, the
banded lemming, and the arctic ptarmigan.
In wide contrast to this assemblage of late Magdalenian life
on the upper Danube, there appear in Azilian times along the
shores of the middle Danube in the stations of Of net and of
Istein the following characteristic forest forms : Sus scrofa ferus
(wild boar), Cervus elaphus (stag), Capreolus capreolus (roe-deer),
Bos (?) primigenius (urus), Lepus (rabbit or hare), Ursus arctos
(brown bear), Felis leo (lion), Gulo luscus (common wolverene),
Lynchus lynx (lynx), Vulpes (fox), Mustela martes (marten),
470 MEN OF THE OLD STONE AGE
Castor fiber (European beaver), Mus (field-mouse), Turdus
(thrush). It thus appears that the alpine, the steppe, and the
tundra faunae had entirely disappeared from this region.
Origin and Distribution of the Azilian-Tardenoisian
Industry
This industry represents the last stage of the Old Stone Age.
The decline in the art of fashioning flints, begun in Magdalenian
times, appears to continue in the Azilian-Tardenoisian. As to
the tiny symmetrical flints which are characteristic of this period,
among the microliths of almost all the late Magdalenian stations
pre-Tardenoisian forms are found which may be regarded as
prototypes of the geometric Tardenoisian flints ; 9 this represents
a new fashion established in flint-making under influences com-
ing from the south.
There was also a natural or local Azilian evolution from the
Magdalenian types and technique. In general the flint imple-
ments which had so long prevailed in western Europe become
smaller in diameter and more carelessly retouched, showing
marked deterioration even from the late Magdalenian stages.
For the preparation of hides and the fashioning of bone we dis-
cover unsymmetrical planing tools (grattoirs), also small, well-
formed oval scrapers (racloirs), and microlithic scrapers. Borers
(perqoirs) with oblique ends and gravers (burins) made of small
flakes are the types of implements which most frequently occur,
but the great variety of borers, so characteristic of the Aurig-
nacian and the Magdalenian industries, had entirely disappeared
in Azilian times.
The marks of industrial degeneration are also conspicuous in
the bone implements, which show a very great deterioration in
number and quality as compared with the Magdalenian, and
which are principally confined to three types — the harpoons, the
awls (poinqons), and the smoothers (lissoirs), together with very
small bone borers (pcrqoirs). The distinctive feature of the
Azilian bone industry is the flat harpoon of stag horn ; it is known
that the use of stags' antlers for fashioning harpoons began in
AZILIAN-TARDENOISIAN INDUSTRY
471
the late Magdalenian, when most of them were still being fash-
ioned from reindeer horn. These flat Azilian harpoons succeed
the type of the double-rowed, cylindrical harpoons of the late
Magdalenian, and are found mainly where the rivers, lakes, or
pools offered favorable conditions for fishing. Thus the Azilian
Fig. 250. Geographic distribution of the principal Azilian and Tardenoisian industrial
stations in western Europe, also Campigny and Robenhausen.
bone-harpoon industry, like the Tardenoisian microlithic flint in-
dustry, was largely pursued by fisherfolk.
We may imagine that the gradual disappearance of the rein-
deer, an animal much more easily pursued and killed than the
stag, was one of the causes of the substitution of the various
arts of fishing for those of hunting.
It is to the excessively small or microlithic flints that the
name Tardenoisian especially applies, and it is the vast multi-
plication of these microliths and their wide distribution over the
472 MEN OF THE OLD STONE AGE
whole area of the Mediterranean and of western Europe which
constitutes the most distinctive feature of this industrial stage.10
The triangular flint (Fig. 249) is certainly the most ancient
Tardenoisian type. It occurs in the Azilian stations of the
Cantabrian Mountains and of the Pyrenees, accompanied by
the painted pebbles and with other flints of Azilian type, but
without the graving-tools ; to the east it is found in the stations
of Savoy; and along the Danube it occurs at Of net, associated
with remains of the lion and the moose, also with ornamental
necklaces composed of the perforated teeth of the deer, identical
with those found in the type station of Mas d'Azil in the Pyrenees.
To the north this typical early Azilian culture extends to Istein,
in Baden, where it includes the microlithic flint flakes, the grav-
ers, and the little round scrapers associated here also with the
stag and the prehistoric forest and meadow fauna of western
Europe. Exactly the same stage of industrial development
occurs in the grotto of Hohlefels, near Nuremberg, and in the
shelter station of Sous Sac, Ain. We invariably find proofs of
the variety of these pygmy flints as well as of their continuity
from one station to another. All these facts compel us to assign
a very long period of time to the spread of these industrial types.
The question which arises as to the sources of this special
Tardenoisian industry again finds archaeologists divided.
Schmidt inclines to the autochthonous theory and regards the
microlithic flint industry as an outgrowth of tendencies already
well developed in the Magdalenian. Breuil, on the other hand,11
dwells strongly on the evidence for circum-Mediterranean sources.
In putting the questions, Who were the Azilians? Whence did
they come? What were their ancestors? he is disposed to give
the answer already quoted, that, whichever industry is exam-
ined, we are always obliged to look toward the south, toward
some point along the Mediterranean, for the origin of these
microlithic flints. In Italy, which he believes to have remained
in an Aurignacian industrial stage throughout all the long period
of Magdalenian time, he finds at Mentone a layer overlying the
Aurignacian and containing small flints recalling the geometric
AZILIAN-TARDENOISIAN INDUSTRY
473
forms of the Azilian, as well as a multitude of the small round
scrapers (racloirs) characteristic of Azilian times. The upper
layers at Mentone on the Riviera are paralleled by those ob-
served near Otranto, in Sicily. It is certain, he continues, that
1 1 1
£^> o
Q
10
11
Fig. 251. Azilian stone implements of types surviving from the Magdalenian and ear-
lier Palaeolithic times. After R. R. Schmidt. 1. Finely flaked point from the large
cave of Ofnet. 2, 3. Small Azilian grattoirs, or planing tools, from Istein. on the upper
Danube. 4. Slender blade from Kleinkems. 5. Borer from Wiiste Scheuer. 6. Poly-
hedral borer from Wiiste Scheuer. 7. Incurved scraper from Istein. 8, 9, 10. Gravers
or borers from Istein. n. Double graver or borer with points at the right and left
of the upper end. 1 to 4, actual size; 5 to 11, one-half actual size.
474
MEN OF THE OLD STONE AGE
all around the Mediterranean there was a number of distinct
centres where microlithic implements of geometric form appeared,
and where the accompanying industries, in different stages of
development, were related to an Upper Palaeolithic culture con-
sisting of a continuous Aurignacian type.
The labors of de Morgan, Capitan, and
others have thrown great light on the Palaeo-
lithic of Tunis, where a flint culture was de-
veloped only slightly different from that of
the Azilian of Valle, Santander, of the Mas
d'Azil, Ariege, and of Bobache, Drome. A
resemblance is also found in Portugal; and
southern Spain, despite its poverty of typical
implements, shows a similar evolution. Near
Salamanca, northwest of Madrid, Spain, the
grottos contain schematic figures and colored
pebbles resembling the Azilian. In Portugal
the hearths of Mugem and Cabeco da Arruda
are distinguished by their triangular microliths
and are undoubtedly Pre-Neolithic, because
there is neither pottery nor any trace of domes-
ticated animals, excepting, possibly, the dog.
To the north of Europe the discoveries in
Belgium have especial importance, for typical
Azilian implements, including small round
scrapers, lateral gravers, elongated triangular
microliths, and knife flakes are found associated
with the remains of the reindeer in the grotto of Remouchamp
and at Zonhoven. It appears in Belgium, as in Italy, that the
use of the Tardenoisian microlithic flint types is prolonged into
a later time than that of the typical Azilian flint implements
— the scrapers, gravers, borers, and knife flakes — which, as we
have seen, appear at the end of the true Magdalenian.
On the other side of the English Channel we again find these
flints always unmingled with pottery and usually distributed
along the sea or river shores. The best-known stations are those
Fig. 252.
Azilian
double-rowed har-
poons of stag horn,
from Oban, on the
west coast of Scot-
land. After Boule.
THE BURIALS AT OFNET 475
of Hastings, directly across the Channel opposite Boulogne, and
of Seven Oaks, near London ; in Settle, Yorkshire, is the Victoria
Cave station. To the north, in Scotland, four Azilian stations
have been discovered around Oban, on the western coast near
the head of the Firth of Lome, while Azilian harpoons have also
been found on the Isle of Oronsay, at its entrance.
Thus the spread of the very small Tardenoisian flint imple-
ments in the final stages of the Palaeolithic precedes the southern
advent of the Neolithic.
In Germany only six Azilian-Tardenoisian stations have thus
far been discovered: two to the east of Dusseldorf, one in the
neighborhood of Weimar, two on the headwaters of the Rhine,
near Basle, and, by far the most important, the large and small
grottos of Ofnet, on a small tributary of the Danube northwest
of Munich. This last is exceptionally important because it is
the only station where skeletons have been found buried with
Azilian-Tardenoisian flints, thereby enabling us positively to
determine the contemporary human races.
Burials in Azilian-Tardenoisian Times
The strange interment which gives Ofnet its distinction be-
longs to the period of Azilian-Tardenoisian industry.12 This con-
clusion is not weakened by the absence of Azilian harpoons or
painted pebbles, because at this time the cave of Ofnet served
its frequenters only as a place of burial ; there are no hearths or
flint workshops to indicate continued residence, as during earlier
Upper Palaeolithic times.
This great ceremonial burial seems to afford the only positive
evidence to be found in all western Europe of the kind of people
who were pursuing the Azilian industry. The larger Ofnet grotto
opens toward the southwest and has a length of 39 feet and a
width of 36 feet. It was first entered in early Aurignacian
times and shows successive layers of Aurignacian, early Solu-
trean, and late Magdalenian cultures, above which lies a thick
deposit of the Azilian-Tardenoisian, in which is found the most
remarkable interment of all Palaeolithic times.
476
MEN OF THE OLD STONE AGE
This is a ceremonial burial of thirty-three skulls of people
belonging to two distinct races: respectively, brachy cephalic and
dolichocephalic, and certainly not related in any way to the
Cro-Magnon race. In one group twenty-seven skulls were found
embedded in ochre and arranged in a sort of nest, with the faces
all looking westward. As the skulls in the centre were more
Fig. 253. Section across the entrance of the great grotto of Ofnet near the Danube,
occupied at various times from the beginning of the Upper Palaeolithic to the close of
the Bronze Age. After R. R. Schmidt. IX. Deposits of the Middle Ages and cf
the La Tene and Hallstatt cultures. VIII. Deposits of the Upper Neolithic. VII.
Azilian layer containing the great burial of 33 skulls. VI. Late Magdalenian layer
containing the banded lemmings of the tundras. V. Late Solutrean layer with typical
laurel-leaf spear points. IV, III. Deposits of late and early Aurignacian age, 777
containing arctic rodents. II. Dolomite sand with a few teeth of the mammoth and
bones of the woolly rhinoceros marked by the teeth of hyaenas.
closely pressed together and crushed than those on the outside,
it seems probable that these skulls were added one by one from
time to time, those on the outside being the most recent addi-
tions. About a yard distant a similar nest was found, contain-
ing six more skulls embedded and arranged in exactly the same
manner. The interment probably took place shortly after death
and certainly before the separate bones had been disintegrated
by decomposition, for not only the lower jaw but a number of
the neck vertebrae were found with each skull. The heads had
THE BURIALS AT OFNET
477
been severed from the necks by a sharp flint, the marks of which
are plainly visible on some of the vertebrae.
It is noteworthy that most of these skulls are those of women
and young children, there being only four adult male skulls. On
this account some advance the theory of cannibalism; others
that, being taken captive by a tribe of enemies, these unfortunate
Fig. 254.
Burial nest of six skulls, all facing westward, from the large grotto of Ofnet.
After R. R. Schmidt.
people were offered in sacrifice, in which case decapitation was
the means of death. But, then, how explain the abundant orna-
ments of stag teeth and snail shells (Helix nemoralis) with which
the skulls of the women and little children were decorated,
and the treasured implements of flint with which all save one of
the men and a few of the women and children were provided?
There are precedents for all these singular features of the
Ofnet interment in other Upper Palaeolithic burials, namely, the
embedding in ochre, the offerings of ornaments of teeth and of
THE NEW RACES 479
shells, the separate interment of the skull — all these were customs
more or less characteristic of the Upper Palaeolithic, but never
observed in Neolithic times.
It will be recalled that the custom of burying the entire body,
as well as that of embedding the body in ochre, is first observed
among the late Neanderthals and obtained throughout the en-
tire Upper Palaeolithic from the Aurignacian burials of Grimaldi
to the Azilian of Mas d'Azil. No other case, however, is known
of the westward turning of the face: in most of the Upper Pa-
laeolithic burials the face of the departed looks toward the open-
ing of the grotto; but, although the grotto of Of net opens toward
the southwest, the skulls, without exception, were facing exactly
to the west and looking toward the wall rather than toward the
entrance of the cavern.
The New Broad-Headed and Narrow-Headed Races of
Ofnet
The burials at Ofnet are the first observed in western Europe
which present a mingling of races. This in itself is a fact of
great interest ; it is a prelude to what characterizes all the popu-
lations of western Europe at the present time, namely, the pres-
ence of races widely separated in origin and in anatomical struc-
ture, but closely united by similar customs, industries, and
beliefs.
A second fact of even greater importance is the proof of
the arrival in western Europe toward the close of Palaeolithic
times of two entirely new human stocks ; one broad-headed, re-
sembling the modern Alpine or Celtic type; the other narrow-
headed, resembling the modern 'Mediterranean' type of Sergi.
Beside these pure types there are several blended forms which
are intermediate or mesaticephalic.
Of the eight brachycephalic heads, six are those of children ;
the two adult brachycephalic crania belong to young women
and are, therefore, not quite so characteristic as male skulls
would be, for in general racial type is more strongly marked in
480 MEN OF THE OLD STONE AGE
men than in women ; the remaining skulls are either of a blended
form or purely dolichocephalic.
The relationship of the broad-headed race to other prehis-
toric and existing broad-headed races of western Europe is also
a matter of very great interest. The Ofnet brachycephals are
regarded by Schliz13 as closely similar to the type skull of the
so-called Grenelle race, which, in turn, is closely similar to the
Furfooz type. Thus the cephalic index of one (Fig. 255) of
these broad, flattened skulls of Ofnet is 83.33 Per cent; the face
is relatively narrow, the zygomatic index being low — 76.34 per
cent; the brain capacity of the female skulls does not exceed
1,320 c.cm. The skull is further described as small, smooth,
and delicately modelled, with a correspondingly feeble dentition,
the teeth being small; the processes of muscular attachment
are slightly developed, all of which characters indicate that the
skull belonged to a woman about twenty-five years of age. The
forehead is low, broad, and prominent. It is altogether typically
parallel to the ' skull of Grenelle,' as well as to the female ' skull
of Au vernier' described by Kollmann. The peculiarity of this
broad-headed race, like that of Grenelle and of Furfooz, is that,
while the forehead is of only moderate breadth, the posterior
part of the skull is extremely broad. The broad-headed people
of Ofnet are thus definitely considered by Schliz14 as members
of the Furfooz- Grenelle race.
The narrow-headed race of the Ofnet burials is distinct in
every respect and presents resemblances to the branch of the
1 Mediterranean' race found in the foreground of the Alpine re-
gions to-day, in which the head is of a pear-shaped type. The
best preserved of these dolichocephalic skulls (Fig. 255) presents
an index of 70.50 per cent, with a brain capacity in the male of
1,500 c.cm., while the smallest brain capacity is that found in
one of the female skulls with 1,100 c.cm. Among the five adult
purely dolichocephalic skulls the face is not in the least of the
broad or disharmonic Cro-Magnon type, but is in proportion
with the cranium, and is thus truly harmonic. The resemblance
of this narrow-headed Ofnet skull to that of the Briinn race,
THE NEW RACES 481
which we have described as occurring in Moravia in Solutrean
times, is only partial, and Schliz concludes that among the narrow-
headed people of Ofnet we have a form of dolichocephaly which
is not identical with any of the known early dolichocephalic forms
of western Europe, but which pursues an independent line of
development similar to the narrow-headed races in the borders
of the Alpine region of the present day. Thus this head type,
of a uniform elliptic contour, seems to have become a stable
racial element of the Alpine population, since we meet it again
in later prehistoric times in the region of the southern and west-
ern foreground of the Alps. Among the children's skulls, two
are of the narrow-headed, pear-shaped type similar to the Alpine
dolichocephals of to-day, that is, with a narrow forehead and very
broad posterior portions of the skull.
Central Origin of the Broad-Headed (Alpine?)
Races
The affinity of the broad-headed Azilian-Tardenoisian tribes
of the Danube to those found in the Upper Palaeolithic of north-
western Europe seems to be clearly established. The latter are
sometimes known as the Grenelle race and sometimes as the Fur-
fooz race. Boule15 observes in regard to the skeletal remains
of Grenelle which were found in the alluvium near Paris, in 1870,
that it is quite impossible now, forty years after their discovery,
to demonstrate their geologic antiquity. This is not the case
with the Furfooz broad-heads, the age of which we regard as
well established, but since the head type appears to be the
same in both cases, we may speak of this race as the Furfooz-
Grenelle.
In a cave near Furfooz, in the valley of the Lesse, Belgium,
sixteen skeletons were discovered by Dupont in 1867. With the
bones were found implements of reindeer horn and remains of
the late Pleistocene fauna of northern Europe.16 The reindeer
and the tundra fauna of Belgium were contemporaneous with the
early Tardenoisian culture and with the stag and forest fauna
482
MEN OF THE OLD STONE AGE
Fig. 256. Broad-headed skull of uncertain archaeologic age, either Palaeolithic or Neo-
lithic, discovered at Grenelle, near Paris, in 1870. After de Quatrefages
and Hamy. One-quarter life size.
of southern France, so that the skeletons of Furfooz may safely
be referred to Azilian-Tardenoisian times.
Only two of the Furfooz skulls were preserved in good shape ;
they are of brachycephalic or sub-brachycephalic form, and, fol-
FiG. 257. Opening of the grotto of Furfooz on the Lesse, a tributary of the Meuse, near
Namur, Belgium, where the skeletal remains of 16 individuals and the type skulls
of the broad-headed Furfooz race were discovered in 1867. After Dupont.
THE NEW RACES
483
Fig. 258. Section of the grotto of Furfooz, showing the burial of 16 skeletons of
the Furfooz race and the entrance of the grotto blocked by a
, mass of stone. After Dupont.
lowing the suggestion of de Quatrefages and Hamy, these skulls
have been spoken of as belonging to the ' brachy cephalic Furfooz
race.' The men of this race may certainly be regarded as be-
longing to Upper Palaeolithic times, whereas the brachycephalic
Fig. 259. One of the type skulls of the broad-headed Furfooz race, from the burial
grotto of Furfooz, Belgium. After de Quatrefages and Hamy. One-
quarter life size.
484
MEN OF THE OLD STONE AGE
"race found at Grenelle, near Paris, is probably Neolithic. This
by no means prevents the Furfooz and the Grenelle types belong-
ing to the same general brachy cephalic race ; it is altogether
probable that they do, and that with them may be included the
Ofnet broad-heads.
There are several opinions regarding the geographic centres
from which these broad-heads entered Europe; it is generally
Fig. 260. Restoration of the broad-headed man of Grenelle, modelled
by Mascre, under the direction of A. Rutot. This type of head is similar
to that of Ofnet.
believed that they came from the high plateaus of central Asia.
By Giuffrida-Ruggeri the Furfooz race is identified with the
existing broad-headed Alpine race {Homo sapiens alpinus), and
is mistakenly adduced as proof that the Alpine race originated
in Europe and is not in any way related to the Mongolian races
of central Asia. A more conservative view17 is that the recent
European broad-headed types commonly included under the
Alpine race cannot yet be traced back to the Furfooz- Grenelle
ancestors, because their connection is too problematical. Schliz,
THE NEW RACES 485
on the other hand, considers that the Furfooz-Grenelle race sur-
vived in northwestern Europe and corresponds with that which
became the builders of the megalithic dolmens of Neolithic times,
the latter being but slightly modified descendants of the original
Furfooz race ; he believes, moreover, that these broad-headed
peoples first occupied central Europe and then extended to west-
ern Europe, where they correspond to the Alpine race, at least in
part ; that they also migrated to the north and were the basis
of the broad-headed races now found in Holland and Denmark.
Southern Origin of the Narrow-Headed
(Mediterranean?) Races
While it seems probable that the broad-heads represent a cen-
tral migration from Eurasia, evidence of an industrial and cul-
tural character indicates that the narrow-heads came from the
south ; this is seen both in the south Mediterranean origin of
the Tardenoisian flint industry and in the new schematic influ-
ences on the decadent art of Upper Palaeolithic times.
It seems, observes Breuil, as if the schematic influences in
art during Upper Palaeolithic times always extend from the
south toward the north; they predominate entirely in the
painted rocks of Andalusia, in the Pyrenees, and in Dordogne.
In the grotto of Marsoulas, Haute-Garonne, the Azilian motifs
are clearly superposed upon the Magdalenian polychromes. This
purely schematic phase, which abruptly follows the figure art
of middle Magdalenian times, first made itself felt in the late
Magdalenian. There was a sudden loss of realism which does
not indicate affiliation but rather the infiltration of strange ele-
ments from the south ; the precursors of the destructive invasion
of the Azilian-Tardenoisian tribes who were driven from their
Mediterranean homes by the westward advance of the conquer-
ing Neolithic races. We imagine18 that in southern Spain there
dwelt in Upper Palaeolithic times a population differing from the
Magdalenians of France and of the Cantabrian Mountains in
their lower artistic tastes. It would therefore appear that the
486 MEN OF THE OLD STONE AGE
schematic art had its home toward the south of the peninsula
of Spain about the time of the invasion of the Azilian culture in
France.
Northern Origin of the Baltic (Teutonic?) Races
For the first time the retreat of the Scandinavian ice-fields
and the less severe climate permitted a northern migration route
along the shores of the Baltic. This is the first known migra-
tion of any tribes along this route, which throughout all glacial
times had been blocked by the vicinity of the Scandinavian and
Baltic ice-fields, but which was now opened by the approach of
the more genial climate which succeeded the long Postglacial
Stage. Whether this Baltic invasion was the advance wave of
a northern long-headed Teutonic race is wholly a matter of
conjecture.
"Other peoples/' observes Breuil,19 "known at present only
from their industries, were advancing toward the close of the
Upper Palaeolithic along the northern and southern shores of the
Baltic and persisted for an appreciable time before the arrival of
the tribes introducing the early Neolithic Campignian culture
which accumulated in the kitchen-middens along the same shores.
Like the southern races of Azilian-Tardenoisian times, . these
northerly tribes were truly Pre-Neolithic, ignorant both of agri-
culture and of pottery; they brought with them no domesti-
cated animals excepting the dog, which is known at Mugem,
at Tourasse, and at Oban, in northwestern Scotland. In the use
of bone harpoons of elegant form and in the taste displayed in
fine decorations engraved upon bone, these tribes suggest the
culture of the Magdalenians, but a close examination shows that
it could not have been derived from the Magdalenian type.
The community of style with the painted and engraved figures
found in western Siberia and in the central Ural region and
north of the Altai Mountains denotes rather an Asiatic and
Siberian origin.
"The decorative designs of these Baltic peoples were very
different from those of the Cro-Magnons in Magdalenian times,
THE NEW RACES
487
and are not schematic ; the conception of the animal figures, al-
though naturalistic, is as crude as that of the early Aurignacian
figures, and is far inferior to that of the Magdalenian stage." "it
is probable," continues Breuil, "that in these northerly regions
the closing cultures of the Upper Palaeolithic developed along
Fig. 261. Implements and decorations showing the conventional and crude animal
designs of the art of the Baltic, from Maglemose, Denmark. After Reinecke and
Obermaier. The implements include bone harpoons, fish-hooks, horn chisels, awls,
spear points, and smoothers. About one-fifth actual size.
more or less parallel lines with those observed in the south in
giving rise to ethnographic elements which travelled along the
littoral regions of the northern seas."
This race and culture is described by Obermaier20 as follows:
When primitive man took possession of Denmark the sea-
coast was so remote that he could also reach southern Scandi-
navia. The station of Maglemose in the 'Great Moor,' discov-
ered and described by F. L. Sarauw, of Copenhagen, in 1900, is
488 MEN OF THE OLD STONE AGE
near the harbor of Mullerup on the western coast of Zealand
and not far from the shore of an ancient freshwater lake forma-
tion. These people were lake-dwellers, living perhaps on rafts
but not on dwellings supported by piles. From these rafts it is
supposed the implements dropped into the lake. The 88 1 flint
implements found here include scrapers, borers, cleavers, and
knives, as well as microlithic flints. They show no trace of the
Neolithic art of polishing, merely suggesting certain chipped
styles observed in the 'kjoddenmoddings.' (See Figs. 263, 264,
and 265.) The influence of the Palaeolithic is much stronger,
especially in the case of the microlithic Tardenoisian types. In
the industrial culture of Maglemose, however, far more impor-
tant than stone are implements of horn and bone. These the
Maglemose folk obtained from the wild ox, moose, stag, and roe-
deer, fashioning them into tools of various types, some of which
are shown in Fig. 261. Many of these tools are ornamented
with conventional designs or very crude animal outlines on one
or both surfaces.
The forests of this time consisted of the characteristic north-
ern flora including numerous evergreens, the birch, aspen, hazel,
and elm, but without any trace of the oak. There is absolutely
no trace of pottery in the Maglemose deposits. Of great inter-
est is the fact that skeletal remains of the domestic dog are found
here.
The Maglemose culture of the Baltic region is regarded as
contemporary with the Azilian and Tardenoisian in the south.
It contains types, not of flint but of bone, which are prophetic of
the Neolithic. Traces of this culture have been found through-
out northern Germany, in Denmark, and in southern Sweden,
as well as to the east and in the Baltic provinces. Although no
human remains have as yet been discovered, it is highly prob-
able that these people belonged to the northern Teutonic races.
ANCESTRY OF EUROPEAN RACES 489
Conclusion as to the Relationships of the Paleolithic
Races
Thus in southern, central, and northern Europe the close of
Upper Palaeolithic times is marked by the invasion of new Eura-
siatic races, all in a Pre-Neolithic stage of industry and art. It
is not improbable that these races were advance waves from the
same geographic regions as the Neolithic tribes which followed
them.
From the earliest Palaeolithic to Neolithic times it does not
appear that western Europe was ever a centre of human evolu-
tion in the sense that it gave rise to a single new species of man.
The main racial evolution and the earlier and later branches of
the human family were established in the east and successively
found their way westward ; nor is there at present any ground
for believing that any very prolonged evolution or transforma-
tion of human types occurred in western Europe.
We should regard as wholly unproved the notion that either
of these Palaeolithic races of western Europe gave rise to others
which succeeded them in geologic time; the only sequence of
this sort to which some degree of probability may be attached is
that the Heidelberg race was ancestral to the Neanderthal race.
In most instances, such races as the Piltdown, the Cro-Magnon,
the Brunn, the Furfooz-Grenelle, and the Mediterranean arrived
fully formed, with all their mental and physical attributes and
tendencies very distinctly developed. There is some evidence,
but not of a very conclusive kind, that the modification of cer-
tain of these races in western Europe was partly in the nature of
a decline ; this was apparently the case both with the Neander-
thals and with the Cro-Magnons.
We may therefore imagine that the family tree or lines of
descent of the races of the Old Stone Age consisted of a number
of entirely separate branches, which had been completely formed
in the great Eurasiatic continent, a land mass infinitely larger
and more capable of producing a variety of races than the dimin-
utive peninsular area of western Europe.
490
MEN OF THE OLD STONE AGE
A review of these races in descending order, in respect to
stature, the cephalic index, and brain capacity, is presented in
the following table :
Recent.
(H. sapiens).
European (average)
Upper Paleolithic.
Ofnet Race (brachyce-
phalic)
Ofnet Race (dolichoce-
phalic)
Cro-Magnon Race (old
man of Cro-Magnon
type)
Grimaldi (Cro-Ma-
gnons)
Chancelade
Aurignac
Grimaldi Race.
Grimaldi type (ne-
groid)
Briinn Race.
Briinn I
Lower Paleolithic.
Neanderthal Race (H.
Neanderlhalensis) .
La Chapelle
Spy II
Spy I
La Ferrassie I
La Ferrassie II
La Quina
Krapina D
Neanderthal
Gibraltar
Pre-Neanderthaloids
Piltdown Race.
Piltdown
Trinil Race (Pithecan-
thropus)
Anthropoid Apes.
Apes (maximum) ,
Frontal
Angle
90
75
65
67
57-5
66
62
66 or
73-74
52. 5
56
Height of
Skull
59
51.22
42.2
40.4
40
34-2
37-7
Cephalic
Index
86.21
70.50
73-76
.'63-
? 76.27
72.02
65.7
69.27
65 • 7 or
68.2
75
75-7
7o
?83.7
73-9
77-9
? 78 or
?79
73 -4 or
7o
Brain
Capacity
ccm.
1 400- 1 500
1400
1500
I590
1775-1880
1700
1580
I350
1626
? 1723
? 1562
1367
(approx.)
1408
1250 or
1296
? 1300
? 1500
850-1000
900
600
Height
ft. in.
5 7
6
5 ">#-
6 4%
4 11
5 3
5 1
5 3
5 3
5 4
5 5
4 103
5 4
5 7
Comparative
Length of Arm
and Leg
69.73'
66.05%-
69%
63.12'
?68%
68%
104%
(chimpanzee
minimum.)
The chief authorities for these
ward, Boule, Sollas, Sera, Klaatsch,
measurements are Schwalbe, Dubois, Keith, Smith Wood-
Fraipont, Makowsky, Verneau, Testut, and Broca.
RECENT
NEOLITHIC 2. l.'lo
If
If
%
t
%
\
%
— %_
1 Races b&lon&ini
t*
tgmg
{Existing Species of Mo
He
UJ
o
0£
*B* belbnginjt \
, . r .•*° * *-
ill* jExttyct Stfecles
\ ' l°ff
V
Cdmnvon Ancestors
of
Extinct anal Existing Species bj Man
lomo isatnens
$
t
0
$
/
/
Fig. 262. Tree showing the main theoretic lines of descent of the chief Pre-Neolithic
races discovered in western Europe. (The Grimaldi race is omitted on account of its
aberrant character. The northern Teutonic long-heads are also omitted.) The
Trinil, Heidelberg, and Neanderthal races are represented as offshoots of one great
branch. The Piltdown race is represented as an independent branch of quite unknown
relations to the other races. It is probable that the five or six branches of Homo sapiens
discovered in the Upper Palaeolithic separated from each other in Lower Palaeolithic
times in Asia. Of these the Briinn race is by far the most primitive.
492 MEN OF THE OLD STONE AGE
The migration routes of invasion of the successive Lower
Palaeolithic races — the Piltdown, the Heidelberg, and the Nean-
derthal— are entirely unknown ; we can only infer from the wide
distribution of the Chellean and Acheulean cultures to the south,
along the northern African coast, as well as to the east, that
these races may have had a southerly or circum-Mediterranean
origin. This does not mean that either of these Lower Palaeolithic
races were of negroid or Ethiopian affinity, because the Neander-
thals show absolutely no negroid characters. In fact, through-
out all Palaeolithic time the solitary instance of the two Grimaldi
skeletons furnishes the sole anatomical evidence we possess of
the entrance of a negroid people into Europe, which contrasts
widely with the overwhelming evidence of the dominance in
western Europe first of the non-negroid Neanderthals, and then
of the Cro-Magnons who probably belonged to the Caucasian
stock.
The evidence as to the sources and migrations of the Upper
Palaeolithic races is also indirect. The theory of the Cro-Magnons
entering Europe by the southerly or Mediterranean route we
have seen to rest upon purely cultural or industrial grounds,
namely, the spread of the Aurignacian industry around the
Mediterranean shores. On the other hand, the succeeding cul-
ture, the Solutrean, and the succeeding race to enter Europe, the
Briinn, both appear to be of central or of direct easterly origin.
It is only toward the close of the Upper Palaeolithic that an-
other southerly or Mediterranean invasion occurs, bringing in
the microlithic Tardenoisian culture, which, although anatomical
evidence is wanting, would appear to be an advance wave of the
great invasion of the true 'Mediterranean' race. During the
Upper Palaeolithic Epoch another invasion apparently occurs
from the east along the central migration route, namely, that of
the broad-headed Furfooz-Grenelle races.
Thus in surveying the whole period of the Old Stone Age
we find that there is some evidence for the theory of an alterna-
tion of southerly, of easterly, and finally of northeasterly inva-
sions of races bringing in new industries and ideas.
TRANSITION TO THE NEOLITHIC
493
Transition to the Neolithic. The Campignian.
The Robenhausian
Apart from the special and somewhat debated question of
the place of the Campignian culture in the prehistory of Europe
we may close our survey of the Upper Palaeolithic by pointing
out some of its contrasts with the Neolithic.
The arrival of the Neolithic cultures and industries in
western Europe marks one of the most profound changes in all
Fig. 263. Stages in the manufacture of the Neolithic stone ax, or hache. After de Mor-
tillet. 534. Hache of flint, roughly flaked into shape, from Olendon, Calvados. 535.
Hache of flint from Oise, ready for polishing. It has been finely chipped to a shape
of perfect symmetry, with especial care to smooth out and reduce the large facets made
by the preliminary flaking. 536. Hache of flint after the first polishing, from Abbeville,
on the Somme. The cutting edge has been completely polished, but along the sides
the facets made by flaking are plainly visible. 537. Hache of flint completely polished,
from Le Vesinet, Seine-et-Oise. In this last stage one scarcely notices the faint traces
of facets which show that this hache has passed through all the preceding stages.
Two-ninths actual size.
prehistory and introduces us to a new period which must be
treated in an entirely different historic spirit. This new era
began between 7,000 to 10,000 years ago, or with the close of
the Daun stage, the last geologic feature of Postglacial times.
There are two theories regarding the close of Upper Palaeo-
lithic and the beginning of Neolithic times. The older theory,
which still has some adherents, is that the Upper Palaeolithic
races and industries suddenly gave way before the arrival of
new and superior races bringing in the Neolithic culture. The
newer theory is that there are evidences of gradual transfusions
494
MEN OF THE OLD STONE AGE
from the Upper Palaeolithic into the Neolithic cultures and that
these are found in some of the oldest Neolithic sites.
In 1898 there appeared an ar-
ticle21 by Philippe Salmon, d'Ault
du Mesnil, and Capitan, entitled,
"Le Campignien," defending the
theory of an early and transitional
Neolithic stage, the Campignian.22
The type station of this early cul-
ture was pointed out by Salmon in
1886 ; it lies a little more than a
mile northwest of the village of
Bresle, on a site well
The remains of the
Fig. 264. Stone hatchet, or tranchet,
from the type station of Campigny,
after Salmon, d'Ault du Mesnil, and
Capitan. One-half actual size.
Blangy, on the River
placed for natural defense,
hut-dwellings of this camp and of various indus-
trial objects appear to indicate that this station
belongs to the earliest phase of the Neolithic
Period. These Campignians owe little to the
culture or industry of the races which previously
occupied this region of western Europe ; they
are entire strangers, purely Neolithic in type.
While this is the age of polished, as dis-
tinguished from chipped, stone, the axe (hache)
of polished stone is still very rare in the Cam-
pignian. There prevail flaked flint types com-
mon to all the previous stages of the Stone Age,
such as the knives (couteaux), planers (grattoirs),
and spear or dart heads (pointes de sagaie), but
we notice the appearance of two entirely new
flint implements : first, the triangular knife or
stone hatchet (tranchet), of the type (Fig. 264)
common in the Danish kitchen-middens ; this
knife has a broad, sharp cutting edge flaked on
one side; second (Fig. 265), there is a sort of
elongated axe or pick (pic) with chipped sides and an end more
or less conical in shape.23 These people also made use of large
Fig. 265. Stone
pick, or pic, from
the type station of
Campigny, after
Salmon, d'Ault du
Mesnil, and Capi-
tan. About one-
half actual size.
TRANSITION TO THE NEOLITHIC 495
flakes of flint. If we regard the Campignian as a prolonged
industrial stage in northern Europe, it certainly precedes the
appearance of abundant axe heads of polished flint. In France
it seems to appear occasionally as a local phase of the
Neolithic.
Fig. 266. Restoration of the Neolithic man of Spiennes, Belgium, modelled
by Mascre under the direction of A. Rutot.
The prevailing opinion at present is that the Campignian
distinctly precedes the typical Neolithic of the Swiss lake-
dwellings, a stage known as the Robenhausian. Thus the Neo-
lithic culture becomes fully established in the period of the
Swiss Lake Dwellings, remains of which are found at Moossee-
dorf, Wauwyl, Concise on Lake Neufchatel, and Robenhausen
on Lake Pfaefhkon. The latter is the Robenhausian type
station.
496 MEN OF THE OLD STONE AGE
Distinctive Features of the Neolithic Epoch
The first of these is the presence of implements of polished
stone which find their way gradually into western Europe.
The neoliths at first are greatly outnumbered by chipped and
flaked implements, and some of the latter show a survival of
the familiar types of the Old Stone Age, while others belong to
entirely distinct types which had an independent development
in the far East.
The chief economic change is seen in the rudimentary knowl-
edge of agriculture and in the use of a variety of plants and seeds,
accompanied by the gradual appearance of implements for the
preparation of the soil and for harvesting the crops. This new
source of food supply leads to the establishment of permanent
stations and camps and more or less to the abandonment of
nomadic modes of life. Near the ancient camp sites and villages,
therefore, are found implements for the preparation of skins and
hides, because the chase was still maintained for purposes of
clothing as well as for food.
Still more distinctive of the Neolithic is the introduction of
pottery, which is at first used in the preparation of food. In
the hearths or kitchen-middens and in the refuse heaps of the
camps we no longer find evidence of the splitting of the jaws of
mammals and of the long and short bones of the limbs, or even
of the larger foot bones, in search of marrow, which is such a
universal feature of the Upper Palaeolithic deposits.
The artistic impulse of the north is very crude and natural-
istic. In the Spanish peninsula, accompanying and following the
schematic period described in the early part of this chapter, there
was a long stage of development in which men were painting on
rocks, mostly in the form of silhouettes, naturalistic figures of
animals and of people.24
The presence of the moose in these drawings concurs with
that of the two bison represented in the cavern of Cogul and
would tend to indicate that these paintings belong to Upper
Palaeolithic times, and it is now considered that they are
NEOLITHIC CULTURE
497
of late Palaeolithic age. The character of these animal designs
is totally different from that of the Magdalenian period in the
north and is analogous rather to that of the Bushmen of South
Africa. The authors of these frescos represent not only the
ibex, stag, and wild cattle but also the horse, moose, fallow deer,
wolf, and occasionally the birds. There are many features in
this art which show its absolute independence of origin from
Fig. 267. Fresco from the rock shelter of Alpera, Albacete, Spain, painted in dark red
and representing a stag hunt, the hunters being armed with bows and arrows. Attrib-
uted to southern races arriving in late Palaeolithic times. After Breuil and Obermaier.
that of the Magdalenian of the north, among them the fre-
quent presence of composition and the almost invariable pres-
ence of human figures.
The frescos in the Spanish caverns of Alpera and of Cogul
recall those of southern France but are almost always grouped
in series of the chase, of encampment, and perhaps of war. This
frequency of human figures, the representations of the bow and
arrow, and the presence of a small animal which may be recog-
nized as the domesticated dog are indications of an entirely dis-
tinct race coming from the south and bringing in a new spirit
in art which has no relation whatever to that of the Magdalenian.
498 MEN OF THE OLD STONE AGE
Neolithic Mammalian Life
Even in the oldest Neolithic deposits no trace of the horse
as an object of food appears. The domestication of this animal
was introduced from the east, and thus it ceased to be an object
of the chase. The newly arriving tribes were undoubtedly at-
tracted by the abundance of horses, both of the forest and Celtic
types, which had survived from Upper Palaeolithic times. A
very distinctive feature of the modern horses, however, should
be mentioned, that is, the presence of a forelock covering the
face, no trace of which is indicated in any of the Upper Palaeo-
lithic carvings or engravings.
The wild animal life of western Europe at this time is a direct
survival of the great Eurasiatic forest and meadow fauna which
we have traced from the earliest Palaeolithic times. It includes
the bison, the long-horned urus, the stag, the roe-deer, the
moose, the wild boar, the forest horse, the Celtic horse, the
beaver, the hare, and the squirrel. The fallow deer (Cervus dama)
also appears more abundantly. Among the carnivora are the
brown bear, the badger, the marten, the otter, the wolf, the
fox, the wildcat, and the wolverene. The lion has disappeared
entirely from western Europe. The reindeer survives only in
the north.
As observed above, two of these wild animals were early
chosen by the invaders for domestication, namely, the plateau
or Celtic horse and the forest horse. The former type is found
in the Neolithic deposits of Essex, England. The wild urus (Bos
primigenius) was hunted but was not domesticated.
Two new varieties of domestic cattle appear, neither of which
has been previously observed in western Europe. The first of
these is the 'Celtic shorthorn' (Bos hmgijrons), the probable
ancestor of the small breeds of British short-horned and horn-
less cattle. The second is the 'longhorn' (Bos taurus), which
shows some points of resemblance to the ' urus ' (Bos primigenius)
but is not directly related to it. Direct wild ancestors of this
latter animal are said to occur in the Pleistocene of Italy. A
NEOLITHIC FAUNA
499
new type of pig also appears, the so-called turf pig (Sus scrofa
palustris) .
The Neolithic invaders, or men of the New Stone Age, thus
brought with them, or domesticated from among the animals
which they found in the forests of western Europe, a great variety
of the same types of animals as those domesticated to-day,
namely, cattle, sheep, goats, pigs, horses, and dogs.
Fig. 268. Map showing the geographic distribution of the three principal cranial types
of man inhabiting western Europe at the present time. Prepared after Ripley's maps
in his Races of Europe. Also the restricted area neighboring the Vezere valley, where
the supposed descendants of the disharmonic type of the Cro-Magnons are still to be
found. Other small Cro-Magnon colonies are not represented. The heavy-faced lines
show those districts where the race indicated is most numerous and found in the greatest
perfection of type.
The Prehistoric and Historic Races of Europe
Before the close of Neolithic times all the direct ancestors
of the modern races of Europe had not only established them-
500
MEN OF THE OLD STONE AGE
selves, but had begun to separate into those larger and smaller
colonies which now mark out the great anthropological divisions
of western Europe. It is therefore interesting to glance at the
cranial distinctions of the men who successively entered western
Europe in Upper Palaeolithic and Neolithic times. The upper
part of the table corresponds with that of Ripley.25
Type
Head
Face
Hair
Eyes
Stature
Nose
Cephalic
Index
Average
per cent
VI.
Teutonic
(? Baltic).
Long,
narrow.
High,
narrow.
Very
light,
Blue.
Tall.
Narrow,
aquiline.
75
V.
Mediter-
ranean
(POfnet).
Long,
narrow.
High,
narrow.
Dark
brown or
black.
Dark.
Medium,
slender.
Rather
broad.
75
IV.
Alpine,
Celtic
(POfnet).
Round.
Broad.
Light
chestnut.
Hazel-
gray.
Medium,
stocky.
Varia-
ble;
rather
broad;
heavy.
87
III.
Ftjrfooz-
Grenelle
(POfnet).
Broad.
Medium.
?
?
?
?
79-85
II.
Brunn-
Predmost
(Moravia).
Long.
Low,
medium.
?
?
?
?
68.2
or
65.7
I.
Cr5-
Magnon.
Long.
Low and
broad.
?
?
Tall to
medium.
Narrow,
aquiline.
?63-
? 76.27
MODERN, NEOLITHIC, AND UPPER PALEOLITHIC EUROPEAN RACES
OF THE EXISTING SPECIES OF MAN {HOMO SAPIENS)
It would appear that five out of these six great racial types
had entered Europe before the close of Upper Palaeolithic times,
namely, I to V in the above table.
How about the sixth type ; the narrow-headed, light-haired
people of the north, the modern Teutonic type? This question
cannot be answered at present We have, however, high au-
CONCLUSIONS 501
thority for the invasion of a new northern race, which may
have been of the Teutonic type, as occurring before the close
of Palaeolithic times. These were the people described above,
migrating along the shores of the Baltic with a new northern
Maglemose culture and crude naturalistic art.
Conclusions as to the Old Stone Age
The above outline of the beginnings of the Neolithic Age
shows that the Palaeolithic represents a complete cycle of human
development ; we have traced its rise, its perfection, its decline.
During this dawning period of the long prehistory of Europe
the dominant features are the very great antiquity of the spirit
of man and the fundamental similarity between the great steps
of prehistory and of history.
The rise of the spirit of man through the Old Stone Age can-
not be traced continuously in a single race because the races
were changing ; as at the present time, one race replaced another,
or two races dwelt side by side. The sudden appearance in Eu-
rope at least 25,000 years ago of a human race with a high
order of brain power and ability was not a leap forward but
the effect of a long process of evolution elsewhere. When the
prehistoric archaeology of eastern Europe and of Asia has been
investigated we may obtain some light on this antecedent de-
velopment.
During this age the rudiments of all the modern economic
powers of man were developed : the guidance of the hand by the
mind, manifested in his creative industry ; his inventive faculty ;
the currency or spread of his inventions; the adaptation of
means to ends in utensils, in weapons, and in clothing. The
same is true of the aesthetic powers, of close observation, of the
sense of form, of proportion, of symmetry, the appreciation of
beauty of animal form and the beauty of line, color, and form
in modelling and sculpture. Finally, the schematic representa-
tion and notation of ideas so far as we can perceive was alpha-
betic rather than pictographic. Of the musical sense we have
at present no evidence. The religious sense, the appreciation of
502 MEN OF THE OLD STONE AGE
some power or powers behind the great phenomena of nature,
is evidenced in the reverence for the dead, in burials apparently
related to notions of a future existence of the dead, and espe-
cially in the mysteries of the art of the caverns.
All these steps indicate the possession of certain generic facul-
ties of mind similar to our own. That this mind of the Upper
Palaeolithic races was of a kind capable of a high degree of edu-
cation we entertain no doubt whatever because of the very ad-
vanced order of brain which is developed in the higher members
of these ancient races ; in fact, it may be fairly assumed from
experiences in the education of existing races of much lower
brain capacity, such as the Eskimo or Fuegian. The emer-
gence of such a mind from the mode of life of the Old Stone Age
is one of the greatest mysteries of psychology and of history.
The rise and fall of cultures and of industries, which is at
this very day the outstanding feature of the history of western
Europe, was fully typified in the very ancient contests with
stone weapons which were waged along the borders of the Somme,
the Marne, the Seine, and the Danube. No doubt, each inva-
sion, each conquest, each substitution of an industry or a cul-
ture had within it the impelling contest of the spirit and will of
man, the intelligence directing various industrial and warlike
implements, the superiority either of force or of mind.
(i) Cartailhac, 1903. 1, pp. 330, 331. (13) Schliz, 1912.1, pp. 242-244.
(2) Dechelette, 1908. 1, vol. I, pp. (14) Op. cit., p. 252.
314-320. (15) Boule, 1913.1, p. 210.
(3) Op. cit., p. 320. (16) Dupont, 1871.1.
(4) Op. cit., pp. 505-510. (17) Fischer, 1913.1, p. 356.
(5) Breuil, 1912.6, pp. 2-6. (18) Breuil, 1912.5.
(6) Ibid., 1912.7, pp. 232, 233. (19) Ibid., 1912.7, PP- 235, 236.
(7) Ibid., 191 2.6, p. 20. (20) Obermaier, 191 2.1, pp. 467-469.
(8) Koken, 1912.1, pp. 172, 173, 176- (21) Salmon, 1898. 1.
178, 180, 181, 201. (22) Munro, 1912.1, pp. 275-277.
(9) Schmidt, 1912.1, p. 40. (23) Dechelette, iqoS.i, vol. I, p. 326.
(10) Breuil, 191 2.7, p. 225. (24) Breuil, 1912.5, p. 560.
(11) Op. cit., p. 233. (25) Ripley, 1899. 1, p. 121.
(12) Schmidt, 1912.1, p. 41.
APPENDIX
NOTE I
LUCRETIUS AND BOSSUET ON THE EARLY EVOLUTION OF MAN
Lucretius's conception* of the gradual development of human culture
undoubtedly came from Greek sources beginning with Empedocles. His
indebtedness is beautifully expressed in the opening lines of Book III of
his De Rerum Natura :
"0 Glory of the Greeks! who first didst chase
The mind's dread darkness with celestial day,
The worth illustrating of human life —
Thee, glad, I follow — with firm foot resolved
To tread the path imprinted by thy steps;
Not urged by competition, but, alone,
Studious thy toils to copy; for, in powers,
How can the swallow with the swan contend?
Or the young kid, all tremulous of limb,
Strive with the strength, the fleetness of the horse;
Thou, sire of science ! with paternal truths
Thy sons enrichest: from thy peerless page,
Illustrious chief ! as from the flowery field
Th' industrious bee culls honey, we alike
Cull many a golden precept — golden each —
And each most worthy everlasting life.
For as the doctrines of thy godlike mind
Prove into birth how nature first uprose,
All terrors vanish; the blue walls of heaven
Fly instant — and the boundless void throughout
Teems with created things."
The same conceptionf of the early periods in the development of human-
ity is found in the Histoire universelle of Bossuet, in a curious passage un-
doubtedly suggested by Lucretius:
"Tout commence: il n'y a point d'histoire ancienne ou il ne paraisse,
non seulement dans ces premiers temps, mais encore longtemps apres, des
vestiges manifestes de la nouveaute du monde. On voit les lois s'etablir,
* Lucretius, On the Nature of Things, metrical version by J. M. Good. Bohn's Classical
Library, London, 1890.
f Bossuet, Jacques Benigne, Discours sur V Histoire universelle (first published in 168 1),
pp. 9, 10. Edition conforme a celle de 1700, troisieme et derniere edition revue par l'au-
teur. Paris, Librairie de Firmin Didot Freres, 1845.
503
504 APPENDIX
les mceurs se polir, et les empires se former: le genre humain sort peu a,
peu de l'ignorance; l'experience l'instruit, et les arts sont inventes ou per-
fectionnes. A mesure que les hommes se multiplient, la terre se peuple
de proche en proche: on passe les montagnes et les precipices; on traverse
les fleuves et enfin les mers, et on etablit de nouvelles habitations. La terre,
qui n'etait au commencement qu'une foret immense, prend une autre forme;
les bois abattus font place aux champs, aux paturages, aux hameaux, aux
bourgades, et enfin aux villes. On s'instruit a prendre certains animaux,
a apprivoiser les autres, et a les accoutumer au service. On eut d'abord
a combattre les betes farouches: les premiers heros se signalerent dans ces
guerres; elles firent in venter les armes, que les hommes tournerent apres
contre leurs semblables. Nemrod, le premier guerrier et le premier con-
querant, est appele dans Fecriture un fort chasseur. Avec les animaux,
l'homme sut encore adoucir les fruits et les plantes; il plia jusqu'aux metaux
a son usage, et peu a peu il y fit servir toute la nature."
NOTE II
HORACE ON THE EARLY EVOLUTION OF MAN
Horace* also adopted the Greek conception of the natural evolution
of human culture:
"Your men of words, who rate all crimes alike,
Collapse and founder, when on fact they strike:
Sense, custom, all, cry out against the thing,
And high expedience, right's perennial spring.
When men first crept from out earth's womb, like worms,
Dumb speechless creatures, with scarce human forms,
With nails or doubled fists they used to fight
For acorns or for sleeping-holes at night;
Clubs followed next; at last to arms they came,
Which growing practice taught them how to frame,
Till words and names were found, wherewith to mould
The sounds they uttered, and their thoughts unfold;
Thenceforth they left off fighting, and began
To build them cities, guarding man from man,
And set up laws as barriers against strife
That threatened person, property, or wife.
'Twas fear of wrong gave birth to right, you'll find,
If you but search the records of mankind.
Nature knows good and evil, joy and grief,
But just and unjust are beyond her brief:
Nor can philosophy, though finely spun,
By stress of logic prove the two things one,
To strip your neighbor's garden of a flower
And rob a shrine at midnight's solemn hour."
*The Satires, Epistles and Ars Poetica of Horace, the Latin Text with Conington's
Translation, pp. 29, 31. George Bell & Sons, London, 1904.
APPENDIX 505
NOTE III
.ESCHYLUS ON THE EARLY EVOLUTION OF MAN
iEschylus, in Prometheus Bound,* presents one of the earliest known as
well as one of the noblest conceptions of the natural development of the
human faculties:
"And let me tell you — not as taunting men,
But teaching you the intention of my gifts,
How, first beholding, they beheld in vain,
And hearing, heard not, but, like shapes in dreams,
Mixed all things wildly down the tedious time,
Nor knew to build a house against the sun
With wicketed sides, nor any woodwork knew,
But lived, like silly ants, beneath the ground
In hollow caves unsunned. There came to them
No steadfast sign of winter, nor of spring
Flower-perfumed, nor of summer full of fruit,
But blindly and lawlessly they did all things,
Until I taught them how the stars do rise
And set in mystery, and devised for them
Number, the inducer of philosophies,
The synthesis of Letters, and, beside,
The artificer of all things, Memory
That sweet Muse-mother."
NOTE IV
'UROCHS,' OR ' AUEROCHS,' AND ' WISENT '
Kobeltf discusses the habits of the wild cattle and of the bison as fol-
lows:
"One is inclined to consider the ancient wild cattle of Europe, the
Urochs, or Auerochs, as the inhabitants of boggy forests. The Auerochs
survived to the seventeenth century in the forests of Poland and then be-
came extinct. It is described as of a black color with a light stripe along
the back.
" The bison, or Wisent, is generally regarded as the inhabitant of the
open steppe, or at least of dryer, opener woods; it differs so little from the
American bison that both can be considered only as races of one species,
the Bison priscus of Pleistocene times, which spread over the temperate zone
of both hemispheres. The American bison has always avoided the woods
and roamed the prairies in countless herds. But all reliable historic records
describe the Wisent as a forest animal, and its few remaining survivors are
* iEschylus, Prometheus Bound. Elizabeth Barrett Browning. Poetical Works of
Elizabeth Barrett Browning, pp. 148, 149- Oxford edition, 1906. Henry Frowde, London,
Edinburgh, Glasgow, New York, and Toronto.
f Kobelt, W., Die Verbreitung der Tierwelt, pp. 403-7. C. H. Tauchnitz, Leipsic, 1902.
506 APPENDIX
entirely limited to the forests. Apparently it was never so widely and gen-
erally distributed as the Auerochs and reached western Europe later, for
it is not found in the north, and never in conjunction with the mammoth
and rhinoceros. Remains of the bison have also been found in Asia Minor.
In Lithuania the bison lives together in herds, resenting the approach of
all strangers. In the Caucasus it lives wild in certain high valleys and here
it is a true mountain animal, its favorite haunts being the forests of beech,
hornbeam, and evergreens from 4,000 to 8,000 feet above sea-level. Only
in winter does it descend to lower levels. It is uncertain whether the
Wisent does not also occur in Siberia. Kohn and Andree assert positively
that it is found in large numbers in the wooded mountains of Sajan, in
Siberia (1895)."
According to Kobelt, much confusion in the nomenclature of these
animals has resulted from the fact that, after the extinction of the
'Urochs,' or 'Auerochs,' in the seventeenth century, the term 'Auerochs'
was frequently used by writers as synonymous with ' Wisent,' or bison, an
entirely different animal.
NOTE V
"In the museums of the Grand Canary, Teneriffe, and Palma a con-
siderable number of prehistoric vessels are preserved. Anthropologists are
agreed that the natives of the archipelago at the time of its conquest, in
the fifteenth century, were a composite people made up of at least three
stocks: a Cro-Magnon type, a Hamitic or Berber type, and a brachyce-
phalic type. These natives were in a Neolithic stage of civilization. Their
arms were slings, clubs, and spears. Most of the people went naked, ex-
cept for a girdle round the loins, and there was no intercommunication be-
tween the islands. Their stone implements were of obsidian or of basalt.
Only four polished axes are known from the Grand Canary and one from
Gomera. The axes are of chloromelanite, and of a type contemporary
with megalithic structures in France. The first colonists probably brought
the knowledge of making pottery with them, but each island developed an
individuality of its own. Even the painted ware of the Grand Canary
appears to be of local origin and not due to external influence. Although
undoubted Lybian inscriptions in the Grand Canary and lava querns of
Iron Age type prove that the archipelago was visited before its conquest
by the Spaniards without affecting the general civilization of its inhabitants."
* Abercromby, Hon. John, The Prehistoric Pottery of the Canary Islands and Its
Makers. Royal Anthropological Institute, November 17, 1914. Nature, December 3,
1914, p. 383;
APPENDIX 507
GUANCHE CHARACTERISTICS RESEMBLING CRO-MAGNON*
The following excerpts are quoted from the account given by the dis-
tinguished anthropologist, Dr. Rene Verneau, of his observations during
a five years' residence in the Canary Islands.
Page 22.
" Without doubt the race that has played the most important role in
the Canaries is the Guanche. They were settled in all the islands, and in
Teneriffe they preserved their distinctive characteristics and customs
until the conquest by Spain in the fifteenth century.
"The Guanches, who at that time were described as giants, were of
great stature. The minimum measure of the men was 1.70 m. (5 ft. 7 in.).
"I myself met a number of men in the various islands who measured
over 1.80 m. (5 ft. 11 in.). Some attained a height of 2 m. (6 ft. 62 in.).
At Fortaventure the average height of the men was 1.84 m. (6 ft. i3o in.),
perhaps the greatest known in any people.
"It is a curious fact that the women who gave birth to such men were
comparatively small — I observed a difference of about 20 cm. (8 in.) in
che heights of the two sexes.
"Their skin was light colored — if we may believe the poet Viana — ■
and sometimes even absolutely white. Dacil, the daughter of the last
Guanche chief of Teneriffe, the valiant Bencomo, who struggled so heroi-
cally for the independence of his country, had a very white complexion and
her face was quite freckled. The hair of the true Guanche should be blond
or light chestnut, and the eyes blue.
"The most striking characteristic of the Guanche race was the shape
of the head and the features of the face. The long skull gave shape to a
beautiful forehead, well developed in every way. Behind, above the
occipital, one notices a large plane contrasting strongly with the marked
prominence of the occipital itself. In addition, the parietal eminences,
placed very high and very distinct from each other, combined to give the
head a pentagonal j or m."
Page 29.
"The Guanche chiefs were much respected. At Teneriffe the corona-
tion of the chief took place in an enclosure surrounded with stones (the
Togaror), in the presence of nobles and people. One of his nearest kins-
men brought him the insignia of power. According to Viera y Clavijo,
this was the humerus of one of his ancestors, carefully preserved in a case
of leather; according to Viana, it was the skull of one of his predecessors.
"The chief (Menceg) placed the relic on his head, pronouncing the
sacramental formula: 'I swear upon the bone of him who has borne this
royal crown, that I will imitate his acts and work for the happiness of my
* Verneau, Dr. R., Cinq annees de sejour aux ties Canaries. (Ouvrage couronne par
PAcademie des sciences, 1801.)
508 APPENDIX
subjects.' Each noble, in turn, then received the bone from the hands of
the chief, placed it upon his shoulder and swore fidelity to his sovereign. . . .
These chiefs led a very simple life: their food was like that of the people,
their apparel but little more elaborate, and their dwellings — like those of
their subjects — consisted of caves, only theirs were a little larger than those
of the common people. They did not disdain to inspect their flocks or
their harvests in person, and were, indeed, no richer than the average
mortal."
Page 31.
"Above all, the ancient Canarians sought to develop strength and
agility in their children. From an early age the boys devoted themselves
to games of skill in order to fit them to become redoubtable warriors. The
men delighted in all bodily exercises and, above all, in wrestling. At
Gran Canaria (Grande Canarie) they often held veritable tourneys, which
were attended by an immense number of people. These could not take
place without the consent of the nobles and of the high priest.
" Permission obtained, the combatants presented themselves at the
place of meeting. This was a circular or rectangular enclosure, surrounded
by a very low wall, allowing free view of the details of the combat. Each
warrior took his place upon a stone of about 40 cm. diameter (15! in.).
His offensive weapons consisted of three stones, a club, and several knives
of obsidian: his defensive weapon was a simple lance. The skill of de-
fense consisted in evading the stones by movements of the body, or parry-
ing the blows with the lance, without moving from the stone on which
stand had been taken. These combats often resulted fatally for one of
the combatants."
Page 34.
"The Guanche understood the use of the sword, and although it was
of wood (pine), it could cut, they say, as if it were of steel.
"To parry blows, they used a lance, as mentioned above, but they
also had shields made of a round of the dragon-tree (Draccena draco).
"The Guanches were, essentially shepherds. While their flocks pas-
tured they played the flute, singing songs of love or of the prowess of
their ancestors. Those songs which have come down to us show them
to have been by no means devoid of poetic inspiration.
"When the care of their stock permitted, they employed their leisure
in fishing. For this they employed various means — sometimes nets,
sometimes fish-hooks, sometimes a simple stick."
Page 47.
"The Guanches were above all troglodytes — that is to say, they lived
in caves. There is no lack of large, well-sheltered caves in the Canary
Islands. The slopes of the mountains and the walls of their ravines are
honeycombed with them. The islanders may have their choice.
APPENDIX 509
"The caves are almost never further excavated. They are used just
as they are.
" Here is a description of one of these caves, the Grotto of Goldar:
"The interior is almost square — 5 m. (16 ft. 4 in.) along the left side,
5.50 m. (18 ft.) along the right. The width at the back is 4.80 m. (15 ft.
6 in.). A second cave, much smaller, opens from the right wall. All
these walls are decorated with paintings. The ceiling is covered with a
uniform coat of red ochre, while the walls are decorated with various
geometric designs in red, black, gray, or white. High up runs a sort of
cornice painted red, and on this background, in white, are groups of two
concentric circles, whose centre is also indicated by a white spot. On
the rear wall the cornice is interrupted by triangles and stripes of red."
Page 61.
"The Guanches never polished their stone weapons."
Page 168.
"Inhabited caves are very numerous at Forta venture. The popula-
tion in certain parts — Mascona, for example — must be quite numerous to
judge by the number of these caves. At a little distance, in the place
known as Hoya de Corralejo, one may still see the Togaror, or tribal meet-
ing place. It is an almost circular enclosure about 40 m. (131 ft. 2 in.) in
diameter, surrounded by a low wall of stones. Six huts, from 2.50 to 4 m.
(8 ft. 2\ in. — 13 ft. ii in.) in diameter, designed no doubt for the sacred
animals, stood near the Togaror."
Page 245.
"A great number of Canarians still live in caves. Near Caldera de
Bandama (Gran Canaria) there is a whole village of cave dwellers."
Page 264.
At Teneriffe Dr. Verneau received hospitality in a cabin worthy of the
Palaeolithic Age.
"I had no need to make any great effort to imagine myself with a
descendant of those brave shepherds of earlier times. My host was an
example of the type — even though the costume was lacking — and his
dwelling completed the illusion. The walls, which gave free access to the
wind, supported a roof composed of unstripped tree trunks covered with
branches. Stones piled on top prevented the wind from tearing it off.
"Hung up on poles to dry were goatskins, destined to serve as sacks
for the gofio (a kind of millet), bottles for water, and shoes for the family.
A reed partition shut off a small corner where the children lay stretched
out pell mell on skins of animals. For furniture, a chest, a hollowed-out
stone which served as a lamp, shells which served the same purpose, a water
jar, three stones forming a hearth in one corner, and that was all."
(And this host was the most important personage in the place.)
510 APPENDIX
Page 289.
Another time, also at Teneriffe, Dr. Verneau had a similar experience.
"An old shepherd invited me to his house and offered me some milk.
What was my surprise on seeing the furnishing of his hut ! In one corner
was a bed of fern, near by a Guanche mill and a large jar, in all points
similar to those used by the ancient islanders. A reed flute, a wooden bowl
and a goatskin sack full of gofio completed the appointments of his home.
I could scarcely believe my eyes on examining the jar and the mill. See-
ing my astonishment, the old man explained that he had found them in
a cave where 'the Guanches' lived, and that he had used them for many
years. I could not persuade him to part with these curiosities. To my
offers of money he answered that he needed none for the short time he had
still to live."
NOTE VI
THE LENGTH OE POSTGLACIAL TIME AND THE ANTIQUITY OF THE AURIGNA-
CIAN CULTURE
The most recent discussion on the length of Postglacial time was that
held at the Twelfth International Congress of Geology, in Ottawa, in 1913
(Congres Geologique International, Compte-rendu de la XII Session, Canada,
1913, pp. 426-537). The notes abstracted by Dr. Chester A. Reeds from
the various papers are as follows:
" American estimates of Postglacial time have been made chiefly from the
recession of waterfalls since the final retreat of the great ice-fields in North
America. The retreat of the Falls of St. Anthony, Minnesota, has been
estimated by Winchell at 8,000 years and by Sardeson at 30,000 years.
The retreat of the Falls of Niagara has been estimated as requiring from
7,000 to 40,000 years; it has proved a very uncertain chronometer, because
of the great variation in the volume of water at different stages in its his-
tory. The recession of Scarboro Heights and other changes due to wave
action on Lake Ontario have been estimated by Coleman as requiring from
24,000 to 27,000 years. Fairchild has estimated that 30,000 years have
elapsed since the ice left the Lake Ontario region of New York.
" In Europe the most accurate chronology is that of Baron de Geer on
the terminal moraines and related marine clays of northern Sweden. For
the retreat of the ice northward over a distance of 370 miles in Sweden
5,000 years were allowed; for the time since the disappearance of the ice
in Sweden, 7,000 years; for the retreat of the ice from Germany across the
Baltic, 12,000 years; giving a total of 24,000 years as compared with a
total of between 30,000 and 50,000 years allowed by Penck for the retreat
of the ice-fields of the Alps."
APPENDIX 511
NOTE VII
THE MOST RECENT DISCOVERIES OF ANTHROPOID APES AND SUPPOSED
ANCESTORS OF MAN IN INDIA
It is possible that within the next decade one or more of the Tertiary
ancestors of man may be discovered in northern India among the foot-hills
known as the Siwaliks. Such discoveries have been heralded, but none have
thus far been actually made. Yet Asia will probably prove to be the
centre of the human race. We have now discovered in southern Asia prim-
itive representatives or relatives of the four existing types of anthropoid
apes, namely, the gibbon, the orang, the chimpanzee, and the gorilla,
and since the extinct Indian apes are related to those of Africa and of
Europe, it appears probable that southern Asia is near the centre of the
evolution of the higher primates and that we may look there for the ances-
tors not only of prehuman stages like the Trinil race but of the higher and
truly human types.
As early as 1886 several kinds of extinct Old World primates, including
two anthropoid apes related to the orang and to the chimpanzee, were re-
ported from the Siwalik hills in northern India, and recently Dr. Pilgrim,
of the Geological Survey, has described three new species of Siwalik apes
resembling Dryopithecus of the Upper Miocene of Europe, also an anthro-
poid which he has named Sivapithecus and regards as actually related to
the direct ancestors of man, a conclusion which may or may not prove to
be correct. Another extinct Indian ape, Palceopithecus, is of very general-
ized type and is related to all the anthropoid apes.
NOTE VIII
ANTHROPOID APES DISCOVERED BY CARTHAGINIAN NAVIGATORS*
The Periplus of Hanno purports to be a Greek translation of a Cartha-
ginian inscription on a tablet in the "temple of Chronos" (Moloch) at
Carthage, dedicated by Hanno, a Carthaginian navigator, in commemora-
tion of a voyage which he made southward from the Strait of Gibraltar
along the western coast of Africa as far as the inlet now known as Sherboro
Sound, the next opening beyond Sierra Leone.
Hanno is a very common Carthaginian name, but recent writers think
it not improbable that this Hanno was either the father or the son of that
Hamilcar who led the great Carthaginian expedition to Sicily in 480 B. C.
In the former case the Periplus might be assigned to a date about 520 B. C;
in the latter, some fifty years later.
The narrative was certainly extant at an early period, for it is cited in
the work on Marvellous Narratives ascribed to Aristotle, which belongs to
*Bunbury, E. H. History of Ancient Geography, vol. I, pp. 3^~333- Jonn Murray,
London, 1879.
512 APPENDIX
the third century B.C., and Pliny also expressly refers to it. The authen-
ticity of the work is now generally conceded.
According to the narrative the farthest limit of Hanno's voyage, which
was undertaken for purposes of colonization, brought him and his com-
panions to an island containing a lake with another island in it which was
full of wild men and women with hairy bodies, called by the interpreters
gorillas. The Carthaginians were unable to catch any of the men, but they
caught three of the women, whom they killed, and brought their skins back
with them to Carthage. " Pliny, indeed, adds that the skins in question
were dedicated by Hanno in the temple of Juno at Carthage, and continued
to be visible there till the destruction of the city. There can be no diffi-
culty in supposing these 'wild men and women' to have been really large
apes of the family of the chimpanzee, or pongo, several species of which are
in fact found wild in western Africa, and some of them, as is now well
known, attain a stature fully equal to that of man."
NOTE IX
THE JAW AND SKULL OF THE PILTDOWN MAN
The skull and jaw fragments, as described on pages 130-144, on which
were founded the new genus and species of the human race, Eoanthropus
dawsoni, have aroused a wide difference of opinion among anatomists
which is still (February, 19 18) unsettled.
Many anatomists questioned the association of the Piltdown jaw with
the Piltdown skull. Some anatomists held that the jaw is not prehuman
and does not belong with the skull at all. After reconsidering the origi-
nal discovery and subsequent geological and anatomical evidence, Dr. A.
Smith Woodward still (letter of January 27, 1917) feels convinced that the
jaw and skull fragments are prehuman and belong to a single individual
of the Piltdown race. His opinion is supported by W. P. Pycraft, D. M.
S. Watson, and other British anatomists who have made a very careful
investigation and comparison of the original Piltdown specimens with
similar bones of anthropoid apes.
On the other hand, Gerrit S. Miller, Jr.,* from a careful comparative
study of a cast of the Piltdown jaw with the jaws of various types of chim-
panzee, still maintains that the portions of the Piltdown jaw preserved,
including the upper eye-tooth, or canine, are generically identical with
those of an adult chimpanzee. This new species of chimpanzee, which
Miller believes to be characteristic of the European Pleistocene, he names
Pan veins. If Miller's theory be correct it would deprive the Piltdown
specimen of its jaw and incline us to refer the Piltdown skull to the genus
Homo rather than to the supposed more ancient genus Eoanthropus.
* Miller, Gerrit S., Jr., The Jaw of the Piltdown Man. Smithsonian Institution,
Washington, November 24, [915.
APPENDIX
513
Miller's theory, however, has not been strengthened by the recent re-
searches of the British Museum above alluded to, nor by the additional
excavations of Smith Woodward near the locality where the jaw was
found, both of which are said to confirm the original opinion of Dawson
and Smith Woodward that the jaw belongs with the skull.
EAST
3miles
Fig. 269. Geologic section of the valley of the Ouse River at Piltdown, England, show-
ing earlier (1, 2) and present (3) river levels. The cross indicates the location of the
Piltdown quarry and theoretic former level of the River Ouse which has since cut a
deep valley nearly 100 ft. below its level when the Piltdown skull was deposited.
Drawn by C. A. Reeds.
As to the geological age of the Piltdown race, if confirmed by future
discovery, the presence in Germany near Taubach, Weimar, of teeth
similar to those in the Piltdown jaw, found in Sussex, England, would tend
to confirm the opinion expressed in the first edition of this work that the
Piltdown race belongs to Third Interglacial times.
NOTE X
FAMILY SEPULTURE OF LA FERRASSIE, FRANCE
The only instance of the knee-flexed burial position known in the Lower
Palaeolithic is the unique family sepulture at the Mousterian station of La
Ferrassie, in Dordogne, discovered by D. Peyrony in the years 1909-1911.
It includes the remains of two adults and two children. One of the adult
skeletons lay upon its back with the legs strongly flexed. The body lay
upon the floor of the cave without any sign of a cavity to contain it. The
head and shoulders had been protected and surrounded by slabs of stone,
while the rest of the body may have been covered by pelts or woven
branches. The second skeleton was that of a woman with the arms folded
upon the breast, while the legs were pressed against the body, indicating
that they were bound with cords or thongs. Two children were interred
in shallow graves.
This sepulture, like that of Spy, Belgium, of late Mousterian times,
was apparently a case of genuine burial, testifying to the ancient reverence
for the dead, joined, perhaps, with the belief in a life after death. In the
Ferrassie burial, close to the children's remains, there was a grave filled
514 APPENDIX
with ashes and bones of the wild ox. Similarly, in the interment at La
Chapelle-aux-Saints there was a cavity containing a bison horn and a
second cavity where large bones of the same animal were found, indicating
possibly the remains of sacrificial offerings or funeral feasts.
NOTE XI
PALAEOLITHIC HISTORY OF NORTHWESTERN AFRICA AND SOUTHERN
SPAIN
The flint workers of Lower and Upper Palaeolithic times who inhabited
the existing geographic regions of Morocco, Algeria, and Tunis sought the
flint-bearing limestones for the manufacture of their implements and fash-
ioned them into forms which are closely similar to those found in Spain
and France. As a result of the explorations of J. de Morgan, L. Capitan,
and P. Boudy between 1907 and 1909* it appears that Palaeolithic man in
Africa became acquainted with fewer types of implements than his contem-
poraries in Europe. It is true that we find the Lower Palaeolithic repre-
sented by typical Chellean coups de poing, and there were also true
Acheulean implements and true Mousterian implements marking the
close of Lower Palaeolithic time.
As to the great antiquity of man in these regions, it appears likely that
there was a kind of pre-Chellean industry at Gafsa, as at St. Acheul in
France, with flakes roughly adapted to the functions of racloirs, points,
knives, etc. It is, in fact, very possible so to interpret the very coarse
flakes found by Boudy in such abundance in the lower deposits of hill 328
at Gafsa. The Chellean and then the Acheulean culture would have
succeeded to this earliest stage, being characterized by an industry strik-
ingly similar for these two epochs. The Mousterian, with its predomi-
nance of racloirs, points, and discs, appears in Tunis to have been only a
modality, a stage of the great Chelleo-Mousterian period, just as it was
in Europe.
Then follows the Aurignacian, the first stage of the Upper Palaeolithic
cultures, in which the forms of the flints are, in the opinion of Capitan,
extremely similar to those of the Lower Aurignacian of northern Spain and
of France. It was at this time, it is believed, that the great wave of indus-
trial migration and perhaps the men of the Cro-Magnon race passed from
these northwestern African stations into Spain and France; for it has
been noted that the Lower Aurignacian of western Europe comes from the
south and not from the east of Europe. The flint-making stations during
the long Lower Palaeolithic are widely distributed, as indicated by the
black dots of the accompanying map (Fig. 270).
* J. de Morgan, L. Capitan, and P. Boudy, "Stations pn'historiques du sud Tunisien,"
Rev. VEcole d'Anthr., 1910, pp. 105-136, 206-221, 267-286, 335-347; 1911, pp. 217-228.
APPENDIX
515
But now a very important change occurs, as indicated in the stations
marked by a crossed circle, in the genesis of new modes of fashioning the
flints which are for a long time peculiar to this region and which — centring
Fig. 270. Extension of the Early Palaeolithic and Capsian industries throughout Spain
and northwest Africa. It is supposed that at this time there was a land connection
across the Straits of Gibraltar. Stations too closely grouped to be shown separately
are as follows:
Africa. — At Mostaganem (8) are the eight stations of Aboukir , Aiin-bou-Brahim , Karouba,
Ouled Zerifa, Ain-el-Bahr, Oued Melah, Oued Ria, and Mazouna. Near Mascara
are the sites of Ain-Hadjar, Ain-Ksibia, Palikao, and Ain-Harca.
Spain. — At Velez Blanco are the three stations of Ambrosio, Cueva Chiquita de los
Treinta, and Fuente de los Molinos; at the Cuevas de Vera are the three caves known
as Serron, Zajara, and Humosa; while the figure 8 marks the eight caves of Palo-
marico, Las Pemeras, Bermeja, Las Palomas, Tazona, Ahumada, Cueva de los
Tollos, and Cueva del Tesoro. Only the Capsian stations of Spain are named here.
For the names of others see Fig. 272, p. 519.
■receive
the
in the stations crowded around Gafsa in the heart of Tunis
name of CAPSIAN.
The explanation of the life and art of the Capsian is probably that of a
climatic change in this region of Africa from a moist and semiforested con-
dition favorable to the larger kinds of game to an arid condition in which
516 APPENDIX
the larger kinds of game became less numerous and the chase was aban-
doned. This is Capitan's opinion, that the Capsian corresponds to new
climatic conditions in northern Africa; for in the depths of the limestone
caves it appears that men's food partly consisted of the animals of the
chase, but more commonly of edible land snails belonging to species still
existing in this region and occurring in great abundance during the winter
and spring rains. This change of climate came after the close of Mous-
terian time, namely, the period which we estimated (p. 281) at about
25,000 years B. C. on the theory that the Fourth Glaciation closed not less
than 25,000 years ago (p. 41).
LOWER PALEOLITHIC OF AFRICA
When we consider that the genuine Chellean industry is completely
lacking in central Europe* we are driven to the conclusion that this in-
dustry came to France and England not from the east but from Africa in
the south. Therefore it becomes clear why, in passing to the aforesaid
countries from northern Africa, this industry was more widely distributed in
Spain than in Italy. Without doubt the same conditions of migration pre-
vailed throughout the entire Lower Palaeolithic, The Acheulean and
Mousterian industries followed the same route, for both are typically rep-
resented in northern Africa and there is no convincing evidence of these
industries having followed any different course.
THE CAPSIAN — UPPER AND LOWER
The succeeding Aurignacian industry of the Mediterranean also had
its centre of dispersion in the northwestern part of Africa — a centre known
through the labors of de Morgan, Capitan, and Boudy, and, more recently,
through those of Pallary, Gobert, and Breuil. Obermaier regards the
Lower Capsian as presenting an industry containing only the Lower Aurig-
nacian (types of Chatelperron) and Upper Aurignacian (types of La Gra-
vette) and considers that the Middle Aurignacian is wanting in northern
Africa. This Middle Aurignacian culture is regarded as of French origin,
having apparently extended southward only in the Cantabrian region,
where it is typically represented at Castillo, Hornos de la Pena, and the
Cueva del Conde.
The Upper Capsian, then, is regarded as extending from Post-Aurig-
nacian time through the entire epoch of the Solutrean and the Magdalenian
of western Europe. Thus for a very long period of time there was no
contact whatever between the industry of northwestern Africa and of
southwestern Europe. During this period the Capsian itself developed
* Obermaier, Hugo, El 1 1 ombre fusil, 1916, p. 203.
APPENDIX
517
its peculiar forms, and toward the close of the Upper Palaeolithic this
industry spread into Spain as indicated by the dotted area and arrows in
the accompanying map (Fig. 271, B).
In the development of the Capsian itself* it is found that the in-
dustry varies according to the sites, each with its own evolution of types.
For example, at the rock shelter of El Mekta flint knives with blunted
backs were of large size, probably because they were used to cut the flesh
of game. At Sidi-Mansour, on the contrary, the dwellers, being snail-
eaters, used only blades as fine as needles and of a type found also at El
Mekta, but fewer in number. This, then, is the origin of the microlithic
flints which were first discovered at the station of Fere-en-Tardenois, in
Capsiense superior;
fer^y-TyVj Solutreo-Magdaleniense.
Capsiense final-Tardenoisiense.
23 Aziliense.
Fig. 271. Maps showing the supposed migration routes into Spain of the:
A. Solutrean and Magdalenian industries from France.
B. Late Capsian (Tardenoisian) industry from Africa. After Obermaier.
France, and hence received the name of Tardenoisian. If the conclusions
of de Morgan, Capitan, and Boudy are well founded, the Upper Capsian
industry of Africa is the true parent of the Tardenoisian of France.
On the other hand, the identity of the Lower Capsian with the Aurig-
nacian in Europe is strongly insisted upon by the same authors. The
Lower Capsian is a Tunisian phase of the Aurignacian of Europe and ab-
solutely identical with it. The forms from the rock shelters of Redeyef,
Foum-el-Maza, and, above all, El Mekta are absolutely typical. In the
latter station occur, moreover, forms closely paralleling those distinctive
of the Aurignacian of Europe, Lower, Middle, and Upper — the great picks;
the large flakes finely retouched; the long, fine blades retouched on one or
both sides, often curved, with blunted backs; the notched blades; the
* Obermaier, Hugo, El Hombre fosil, 1916, pp. 346, 347.
518
APPENDIX
nuclei with edges worked into grattoirs; and, above all, the blades with
square-edged grattoirs across the ends, often presenting a lateral burin,
so characteristic of the Aurignacian. Thus these authors conclude that
human evolution and probably the human stock in Tunis was uniform
with that of Europe throughout all Aurignacian time until its very close,
and that, following this, an independent evolution in North Africa took place.
Little is known of the anatomy of these Lower Capsian workmen. In
an abri about two kilometres from Redeyef, and associated with a flint in-
dustry characteristic of the Lower Capsian, there were found numerous
fragments of human bones much altered, friable, and with very irregular
surfaces. Recognizable among this skeletal debris were a decidedly thick
cranial vault, and portions of two large thigh-bones (femora) and of shin-
bones (tibias) which are also thick and very much flattened (platycnaemic).
It is interesting to recall that the abundant skeletal remains found at
Grimaldi were chiefly of the well-known Cro-Magnon type with markedly
platycnaemic tibias, and were associated with flint implements characteristic
of the Aurignacian culture, which Capitan considers identical with the Lower
Capsian.
INDUSTRIES OF NORTH AFRICA GEOGRAPHIC CONDITIONS
INDUSTRIES OF EUROPE
Upper Capsian
(Late Upper Palaeolithic)
(final phase of Capsian =
Tardenoisian)
Reunion with Spain and Close of the Upper Palaeo-
France lithic
Tardenoisian and Azilian
Stages
(Middle Upper Palaeolithic)
Separation from Spain Solutrean and Magdalenian
and France Stages
Lower Capsian
(Beginning of the Upper
Palaeolithic)
Union with Spain Aurignacian Stage
and France
Lower Palaeolithic
Mousterian, Acheulcan, and
Chellean Stages
Union with Spain and Lower Palaeolithic
France Mousterian, Acheulean,
and Chellean Stages
PALAEOLITHIC HISTORY OF SPAIN
Having now considered northern Africa, it is interesting to look at
Spain as influenced by Africa on the south, by the industrial and artistic
life of France on the north, and as having an important independent evo-
lution of its own. These conditions are fully described in Hugo Ober-
maier's recent work, El II ombre fosil* to which the reader is referred.
Over eighty Palaeolithic stations have been discovered in Spain. Spain
shares with the greater part of Africa (including Egypt), with Syria, Meso-
potamia, and parts of India, the extraordinarily wide distribution of in-
* Obermaier, Hugo, /:/ II ombre fosil, 1916.
APPENDIX
519
Fig. 272. Upper and Lower Palaeolithic stations of Spain and Portugal. Stations too
closely grouped to be shown separately on this map are as follows:
North. — 5, Cueva del Conde, Cueva del Rio, Coilubil, Viesca, La Cuevona; 4, Cueto
de la Mina, Balmori, Arnero, Fonfria; 14 (also marked 'Castillo'), four symbols
represent the fourteen closely grouped stations of Castillo, Altamira, Homos de la
Pefia, Camargo, Cueva del Mar, Truchiro, Astillero, Nuestra Sefiora de Loreto,
Villanueva, Pendo, Cobalejos, San Felices de Buelna, Pefia de Carranceja. and El
Cuco. A little west of Fuente del Frances is San Vitores.
West. — At Oporto are the three stations of Pacos, Ervilha, and Castello do Queijo.
In or near Lisbon are the fifteen stations of Agonia, Alto do Duque, Amoreira, Bica,
Boticaria, Casal da Serra, Casal das Osgas, Casal do Monte, Estrada de Aguda-
Queluz, Leiria, Moinho das Cruzes, Pedreiras, Pefias Alvas, Rabicha, and Serra de
Monsanto.
Southeast. — At Velez Blanco are the three stations of Ambrosio, Cueva Chiquita de los
Treinta, and Fuente de los Molinos; at the Cuevas de Vera are the three caves known
as Serron, Zajara, and Humosa; while between the two sites marked 8 are the eight
caves of Palomarico, Las Perneras, Bermeja, Las Palomas, Tazona, Ahumada,
Cueva de los Tollos, and Cueva del Tesoro.
dustries resembling those of the three Lower Palaeolithic stages — the
Chellean, the Acheulean, and the Mousterian.
By what types of man these industries were pursued in these different
countries it would be premature to say. At the beginning of the Upper
Palaeolithic a profound change occurs, for in the Aurignacian industry we
have to do with a Mediterraneo-European culture exhibiting advances in
technique which are not developed elsewhere.
5^0
APPENDIX
IMPORTANT PALEOLITHIC SITES IX SPAIN AND PORTUGAL
Provinces and Stations
SPAIN
GUIPUZCOA
Altzbitarte (Landarbaso)
YIZCAYA
Armina
Balzola
SANTANDER
Miron, El
Valle
Otero
Salitre
Rascafio
Fuente del Frances
Astillero
Nuestra Sefiora de Loreto
Castillo
Pendo, Cueva del (San Pantaleon) . .
Cobalejos (Puente Arce)
Camargo
Hornos de la Pena
Altamira
OVIEDO
Panes
Cueto de la Mina"
Conde, Cueva del
Paloma, Cueva de la
SORIA
Torralba
MADRID
San Isidro
CORDOBA
Posadas-Almodovar del Rio
JAEN
Campos de Olivar de Puente Mocho.
CADIZ
Laguna de la Janda
BARCELONA
Abrich Romanl
GERONA
Scrinya
I.I.KIDA
Cogul
almeri'a
\elcz Blanco (three stations).
MURCIA
Benneja, Cueva de la
VLBACETE
Alpera
VALENCl \
Parpallo, Cueva del
Maravillas, Cueva de la
'I rue he (Tun he), .\l>ri.u'<> de la
POK I l (. \L
Mugem, in the valley of the Tagus (four stations
Purninha
Lisbon and environs (fifteen stations)
Paleolithic Cultures
Lower
Upper
+■
+ I +
+:
+
+
+?
+
+
+
+
+
+
+
+
+
+
+
+
+o
+
+
+
r-y-i
+?
Capsian
f
+
+
APPENDIX 521
At the close of Upper Aurignacian time the community of culture
ceases in Spain itself, and this country divides sharply into two regions,
namely, northern and southern.
In the northern region we observe a close similarity with the industrial
evolution of France during the entire period of Solutreo-Magdalenian time.
The true Solutrean extended from France throughout the northern part
of the Iberian Peninsula. In Cantabria, Early Solutrean is represented by
laurel-leaf points found at Castillo, Hornos de la Pena, and elsewhere;
while Late Solutrean types — shouldered points, and laurel-leaf and willow-
leaf points with concave base — appear at Altamira, Camargo, and the
Cueva del Conde. True Solutrean strata have not yet been discovered in
the east of Spain, although the discovery — made by H. Breuil — of a willow-
leaf point at El Arabi would seem to indicate that there may have been
some slight infiltration of the Solutrean along the seacoast. Implements
suggesting the Solutrean found in Almeria (Cueva Chiquita de los Treinta)
and Murcia (Cueva de las Perneras) are doubtful, as it is very possible
that they represent Neolithic types. The true Magdalenian appears also
to be an intrusion restricted to the northern part of the peninsula. It
is found in the east in the provinces of Gerona and Barcelona, but occurs
chiefly in the Whole Cantabrian region. The homogeneity of the Mag-
dalenian in these parts with that of France is very marked, not only in the
stratification and types of Palaeolithic implements but also in the objects
of mobiliary art.
SOUTHERN AND EASTERN SPAIN — THE CAPSIAN
At the same time the southern and eastern regions of Spain were com-
pletely under the influence of the Upper Capsian industry of northern
Africa and in these regions the typical forms of the Lower Capsian ( =
Lower and Upper Aurignacian) tend to become reduced in size and to
evolve toward the geometric forms until they finally acquire the aspect
of the Tardenoisian microliths. Thus we find that in the Upper Capsian
of eastern and southern Spain, as in northern Africa, true Solutrean and
Magdalenian implements are unknown. These implements are replaced
by the microlithic industry, chiefly characterized by trapezoidal forms which
can be traced eastward along the coast of Africa to Egypt, Phoenicia, and
even to the Crimea. A notable part of this industry found its way also
into Sicily.
The final phase of the Upper Capsian of Spain is essentially identical
with the Tardenoisian of France. Certain discoveries have been made in
Guadalajara, in Murcia, and in Albacete (Alpera). To these must be added
other Azilio-Tardenoisian stations no less important found in Portugal
in the valley of the Tagus. At Mugem and at other stations heaps of
sea-shells of a great variety of species prove that when the Upper Capsian
men were living they sought the same kinds of food in Spain as in northern
5W APPENDIX
Africa. In these heaps the trapezoidal forms of implements predominate,
closely similar to those of the Tardenoisian. The animal life of these de-
posits does not include any sort of domestic animal except the dog.
Of great interest are the numerous burials — chiefly of women and chil-
dren, more rarely of men — in which the skeletons occur most often in the
folded position. The human type has not been determined, but long-
headed (dolichocephalic) skulls greatly predominate, while short-headed
(brachycephalic) skulls occur but rarely. It is probable, therefore, that
these people belonged to the small, long-headed, dark-skinned Mediter-
rean race.
Inasmuch as the origins of the Tardenoisian of France are found in
the final Capsian stage of Spain, reinforced by African elements, Ober-
maier regards the Spanish Tardenoisian as somewhat older than the French.
CAPSIAN AND AZILIO-TARDENOISIAN ART
Obermaier observes that it is as yet impossible to determine the period
of the commencement of this peculiar art of central and southern Spain,
but considers that a transition from the naturalistic art of the Quaternary
to the conventionalized schematic art was effected by almost impercept-
ible degrees. This would imply that no sudden changes took place at
this time in the population of Spain, but that the tribes of Upper Capsian
culture evolved in situ into the Azilio-Tardenoisian stage, and eventually,
owing to the influence of exterior civilizations, into the Neolithic. Final
phases of this schematic art contain idols and representations of faces which
coincide absolutely with Neolithic idols in the collections of L. Siret, F.
de Motos, and others. Moreover, they present similarities to certain designs
from the dolmens of the final Neolithic.
This art is characterized by its numerous reproductions of the human
figure. In almost all the important rock shelters of the eastern region
(Alpera) it has been possible to distinguish layers of more recent designs
painted over the classic Quaternary paintings, and classified — on account
of their superposition — as "Post-Palaeolithic." Of these a small portion
are .figures still retaining the naturalistic style — representations of animals
and men — but poor in conception, stiff and lifeless, in most cases bearing
no comparison with the vigor and abandon of the figures of Alpera. The
greater part of these designs consist of geometric or conventionalized signs
or figures.
Still purer in style and more abundant are the instances of this con-
ventionalized mural art in southern Spain, where M. de Gongora, Vilanova,
Jimenez de la Espada, Gonzalez de Linares, M. Gomez Moreno, F. de
Motos, H. Breuil, J. Cabre, and E. Hernandez-Pacheco have devoted
themselves sedulously to its study. Numerous painted rock shelters are
known, but almost all without the slightest trace of Palaeolithic art and
with numerous conventionalized (schematic) petroglyphs, in Andalusia
APPENDIX 523
(Velez Blanco, Ronda, and Tarifa) and throughout the Sierra Morena
(Fuencaliente). In many cases it would be difficult to guess the deriva-
tion of these designs of human or animal figures, were it not for the exist-
ence of gradations in conventionalization from the naturalistic design to
the final geometric scheme. With these, arranged in a regular manner,
there occur further a great number of ramiform, pectiniform, stelliform,
serpentine, and alphabet-like signs, with designs in zigzags, circles, and dots.
Another important centre is found in western Spain (Estremadura)
the notable designs of which are mentioned by Lope de Vega in 1597 —
Fig. 273. Detail from the Late Palaeolithic designs painted on the sides of two natural
recesses in the rock shelter of Alpera. After Obermaier.
doubtless referring to the paintings of Canchal de las Cabras in Las
Batuecas.
Slight infiltrations of the same art have been recognized in northern
Spain at Castillo, Santander, and at the open station of Pena Tu, near
Vidiago, Oviedo. As a notable exception to the naturalistic art prevail-
ing north of the Pyrenees we may mention the paintings in this same geo-
metric style found in the cave of La Vache, near Tarascon, Ariege, in south-
ern France.
524
APPENDIX
Of equally great interest is the explanation which this art affords of
the remarkable painted pebbles of Mas d'Azil which are now seen to be
partly pictographic in origin, chiefly schematized representations of the
human figure which gradually begin to assume shapes closely resembling
those of the Phoenician alphabet. As early as 191 2 Henri Breuil was con-
sidering this pictographic theory and beginning to refer to the 'Azilian
signs' at Las Batuecas as reminiscent both of the painted pebbles of Mas
dAzil and of the mural paintings of Andalusia. But chiefly he made clear
the importance of the "dotted lines, ramiform, pectiniform, and stelli-
form signs, zigzags, circles, and figures vaguely resembling alphabetic
forms." A very ingenious study of these schematic Azilian signs has been
made by Obermaier in El Hombre fosil, where he endeavors to trace the
conventionalized descendants of the human figure of the ancient natural-
istic style as shown in Fig. 274. The demonstration of this theory may in
ffei/ftS^ft^
f
M. d. A.
Fig. 274. Figures from Piedra Escrita (a-e) and from Cimbarillo de Maria Antonia (/),
compared with a design occurring on the painted pebbles of Mas d'Azil, showing a
progressive conventionalization of the human figure. After Obermaier.
good time make possible a logical interpretation of a great part of these
same painted pebbles of the Azilian. Obermaier feels confident that they
should be considered as religious symbols, and that these petroglyphs of
Spain will supply a proof that many of the designs on these pebbles plainly
show conventionalized human figures.
Some years ago A. B. Cook drew attention to the fact that a native
tribe in central Australia, the Arunta, is distinguished by each clan having
a deposit of ' churingas' in a cave. There the churinga of each individual
of the clan, be it man or woman, is the object of vigilant protection. They
are made of wood or stone, and in the latter case show a striking resem-
blance in form and decoration to the Azilian pebbles. The Australian sees
in each churinga the incarnation of one of his ancestors, whose spirit has
passed to him and whose qualities he has inherited. It is noteworthy that,
according to Australian beliefs, they can acquire the gift of speech by
means of the 'bull-roarer,' an amulet of stone or bone.
By analogy with the preceding, it is possible that some of the Azilian
pebbles represent such 'stones of the ancestors,' an incarnation of mas-
culine or feminine forefathers whose symbols were the objects of an es-
pecial cult. F. Sarasin found in the cave of Birseck, near Arlesheim,
Switzerland, a typical Azilian deposit with painted pebbles which had all
APPENDIX
515
been intentionally broken, without exception. He advanced the not im-
probable theory that this evidenced an act of the extremest hostility
against the sanctuary of a tribe, performed in order to despoil its members
forever of the protection of their ancestors, seeking in this way to subju-
gate or annihilate them.
In the Capsian silhouettes there is little likeness to the naturalistic
art of the Cro-Magnons in the north of Spain and in France. We are re-
minded rather of the rock paintings of the Bushmen and of the hunting-
scenes depicted by North American Indians, but on the whole there is
greater tendency to grouping and composition of standing figures, mascu-
line and feminine, in ceremonies and in the chase. The male figures are
mostly nude, and occasionally have head ornaments of feathers; while the
Fig. 275. Various types of bows and arrows shown in the paintings of the'Cueva de la
Vieja ' at Alpera. After J. Cabre.
female figures are represented with kirtles, head-dresses, and ornaments
on the body, arms, and ankles. Masculine figures in the chase are ac-
companied by hunting-dogs and exhibit the bow and arrow. If these
drawings are correctly assigned to the close of the Upper Palaeolithic, this
is the most ancient representation of this primitive weapon of the chase
of which we have record. The arrow seems to be single-barbed, as shown
in the accompanying cut from Alpera. It may have been pointed with
flint fastened on one side to the shaft. We recall that double-barbed
arrow-heads were in use in Magdalenian times, as shown in the cavern
of Niaux.
BIBLIOGRAPHY
A
Agassiz, L.
1 83 7. i Discours prononce a l'ouverture des seances de la Societe Helvetique
des Sciences Naturelles a Neuchatel le 24 Juillet, 1837, par L.
Agassiz, President. Actes, Soc. Helvetique, Sci. nat., 22^ Sess. ,
1837, pp. v-xxxii.
1 840. 1 Etudes sur les glaciers. Ouvrage accompagne d'un atlas de 32
planches. 8vo. Neuchatel, 1840.
1840.2 On Glaciers and Boulders in Switzerland. Rept. 10th Meeting, Brit.
Assoc. Adv. Sci., Glasgow, 1840, pp. 113, 114 (Trans. Sections).
Alcalde del Rio, H.
191 2. 1 Les cavernes de la region cantabrique (Espagne). (With Breuil and
Sierra.) See Breuil, H., 1912.2.
1913.1 La Pasiega. (With Breuil and Obermaier.) See Breuil, H., 1913.1.
Anthony, R.
1910.1 L'encephale de l'homme fossile de La Chapelle-aux-Saints. (With
M. Boule.) C. R. Acad. Sci., Paris, tome 150, 1910, pp. 1458-1461.
191 1.1 L'encephale de rhomme fossile de La Chapelle-aux-Saints. (With
M. Boule.) See Boule, M., 1911.1.
191 2.1 L'encephale de l'homme fossile de La Quina. C. R. Acad. Sci.,-
Paris, tome 155, 1912, pp. 91-93.
Arcelin, A.
1869. 1 L'Age du Renne en Maconnais, etc. (With Ferry, H.) See Ferry,
H., 1869. 1.
d'Ault du Mesnil, G.
1896. 1 Note sur le terrain quaternaire des environs d' Abbeville. Rev.
de VEcole d'Anthropol., Paris, 1896, annee VI, pp. 284-296.
1898. 1 L'Age de la Pierre. (With Salmon, P., et Capitan.) See Salmon, P.,
1898. 1.
Avebury, Lord (Sir John Lubbock).
1913.1 Prehistoric Times as Illustrated by Ancient Remains and the Man-
ners and Customs of Modern Savages. Seventh edition, thor-
oughly revised and entirely reset. (Henry Holt & Co.) 8vo, 1913.
B
Bachler, E.
191 2. 1 Das Wildkirchli, die alteste prahistorische Kulturstation der Schweiz
und ihre Beziehungen zu den altsteinzeitlichen Niederlassungen
des Menschen in Europa. Schr. Ver. fur Geschichte des Bodensees,
Heft XLL
527
528 BIBLIOGRAPHY
Bardon, L.
1909. i Decouverte d'un squelette humain mousterien a, la Bouffia de La
Chapelle-aux-Saints (Correze). (With Bouyssonie.) See Bouys-
sonie, A., 1909. 1.
Bayer, J.
191 2. 1 Das geologisch-archaologische Verhaltnis im Eiszeitalter. Zeitschr.
fur Ethnol., 44 Jahrgang, Heft 1, 191 2, pp. 1-22.
Begouen, Le Comte.
191 2.1 Les statues d'argile prehistoriques de la caverne du Tuc d'Audou-
bert (Ariege). C. R. Acad. Inscrip. et Belles-Lettres, 191 2, pp.
532-538.
191 2.2 Une nouvelle grotte a gravures dans l'Ariege, la caverne du Tuc
d'Audoubert. Congr. Internal. d'Anlhropol. et d'Archeol. prehist.,
XIVe Sess., Geneve, 1912, pp. 489-497.
Berry, R. J. A.
1 9 14. 1 The Place in Nature of the Tasmanian Aboriginal as Deduced from
a Study of his Calvaria. — Part II, His Relation to the Australian
Aboriginal. (With A. W. D. Robertson.) Proc. R. Soc. Edin-
burgh, vol. XXXIV, part II, 1914, pp. 144-189.
Blanckenhorn, M.
191 1.1 Die Pithecanthropus-Schichten aus Java. (With Selenka, L.) See
Selenka, L., 1911.1.
Bonareili, G.
1909. 1 Paleoanthropus (n. g.) heidelbergensis (Schoet.). Perugia Riv. ital.
Palaeont., vol. 15, 1909, pp. 26-31.
Bonnet, R.
1914.1 Diluviale Menschenfunde in Obercassel bei Bonn. (With Verworn
and Steinmann.) Ill, Die Skelete. See Verworn, M., 1914.1.
Boucher [de Crevecceur] de Perthes, J.
1 846. 1 Antiquites celtiques et antediluviennes: Memoire sur l'industrie
primitive ou des arts a, leur origine. Tome I, 1846. Tome II,
1857. Tome III, 1864. Paris, 8vo.
Boule, M.
1 888. 1 Essai de paleontologie stratigraphique de l'homme. Rev. d' Anthropoid
1888, ser. 3, tome III, pp. 129-144, 272-297, 385-411, 647-680.
1899. 1 Sur l'existence d'une faune d'animaux arctiques dans la Charente a
l'epoque quaternaire. (With Chauvet, G.) C. R. Acad. Sci.,
Paris, tome 128, pp. 1188-1190.
1905. 1 L'origine des eolithes. L'Anthropol., tome XVI, 1905, pp. 1-11.
1906. 1 Les Groltes dc Grimaldi (Baousse-Rousse). Tome I, fasc. II — ■
Geologic et Paleontologie. Publiees sous les auspices de S. A.
S. Albert Icr, Prince de Monaco. Monaco, 4to.
1908. 1 L'homme fossile de La Chapelle-aux-Saints (Correze). C. R. Acad.
Sci., Paris, 1908, tome 147, pp. 1349-1352.
BIBLIOGRAPHY 529
1908.2 L'homme fossile de La Chapelle-aux-Saints. V Anthropoid tome
XIX, 1908, pp. 519-525.
1909. 1 L'homme fossile de La Chapelle-aux-Saints (Correze). UAnthropol.,
tome XX, 1909, pp. 257-271.
1910.1 L'encephale de l'homme fossile de La Chapelle-aux-Saints. (With
R. Anthony.) C. R. Acad. ScL, Paris, tome 150, 1910, pp. 1458-
1461.
1910.2 Les Grottes de Grimaldi (Baousse-Rousse). Tome I, fasc. Ill — ■
Geoiogie et Paleontologie (suite). Monaco, 1910.
1911.1 L'encephale de l'homme fossile de La Chapelle-aux-Saints. (With
R. Anthony.) U Anthropol., tome XXII, 191 1, pp. 129-196.
191 2. 1 La taille et les proportions du corps de VHomo ncandcrthalcnsis.
C. R. Inst, franq. Anthrop., 1912, pp. 57-60.
1913.1 L'homme fossile de La Chapelle-aux-Saints. Ext. Ann. Pal., tome
VI, 1911, pp. m-172 [1-64], PL XVII-XX [PL I-IV]; tome VII,
1912, pp. 21-192 [65-208], PL IV-XIX [PL V-XVI]; tome VIII,
1913, pp. 1-70 [209-278], Paris, 4to.
Bourgeois, l'Abbe.
1 86 7. 1 Decouverte d'instruments en silex dans le depot a Elephas meridionalis
de Saint-Prest, aux environs de Chartres. C. R. Acad. Set.,
Paris, tome 64, pp. 47, 48.
Bourrinet.
1906. 1 L'Abri Mege, une station magdalenienne a Teyjat (Dordogne).
(With Capitan, Breuil, and Peyrony.) See Capitan, 1 906.1.
1908. 1 La grotte de la Mairie a Teyjat (Dordogne). Fouilles d'un gise-
ment magdalenien. (With Capitan, Breuil, and Peyrony.) See
Capitan, 1908. 1.
191 2. 1 Les gravures sur cascade stalagmitique de la grotte de la Mairie a
Teyjat (Dordogne). (With Capitan, L., Breuil, and Peyrony.)
See Capitan, L., 1912.1.
Bouyssonie, les Abbes A. et J.
1909. 1 Decouverte d'un squelette humain mousterien a la Bouffia de La
Chapelle-aux-Saints (Correze). (With Bardon.) V Anthropol.,
tome XIX, 1909, pp. 513-518.
Breuil, l'Abbe H.
1906. 1 L'Abri Mege, une station magdalenienne a Teyjat (Dordogne).
(With Capitan, Bourrinet, and Peyrony.) See Capitan, L., 1906. 1.
1906.2 La caverne d'Altamira a Santillane pres Santander (Espagne).
(With Cartailhac.) See Cartailhac, E., 1906. 1.
1908.1 La grotte de la Mairie a Teyjat (Dordogne). Fouilles d'un gise-
ment magdalenien. (With Capitan, Bourrinet, and Peyrony.)
See Capitan, 1 908.1.
1908.2 Les peintures et gravures murales des cavernes pyreneennes. (With
Cartailhac.) See Cartailhac, E., 1908. 1.
1909.1 L'Aurignacien presolutreen. Epilogue d'une controverse. Rev.
prehist., annee 4, 1909, pp. 5-46.
530 BIBLIOGRAPHY
1909.2 Cranes paleolithiques faconnes en coupes. (With Obermaier, H.)
V Anthropoid tome XX, 1909, pp. 523-53°-
1909.3 L'evolution de l'art quaternaire et les travaux d'Edouard Piette.
Rev. ArcheoL, ser. 4, tome XIII, pp. 378-411.
1910.1 La caverne de Font-de-Gaume aux Eyzies (Dordogne). (With
Capitan and Peyrony.) See Capitan, L., 1910.1.
1910.2 Les peintures et gravures murales des cavernes pyreneennes. IV—
Gargas, Cne. d'Aventignan (Hautes-Pyrenees). (With Car-
tailhac.) See Cartailhac, E., 1910.1.
191 1.1 L'abri sculpte de Cap-Blanc a Laussel (Dordogne). (With Lalanne.)
V Anthropol., tome XXII, 191 1, pp. 385-408.
191 2.1 L'age des cavernes et roches ornees de France et d'Espagne. Rev.
ArcheoL, tome XIX, 191 2, pp. 193-234.
191 2.2 Les cavernes de la region cantabrique (Espagne). (With Alcalde
del Rio, and R. P. K. Sierra.) See Alcalde del Rio, 191 2.1.
191 2.3 Les gravures sur cascade stalagmitique de la grotte de la Mairie a,
Teyjat (Dordogne). (With Capitan, L., Peyrony, and Bourrinet.)
See Capitan, L., 1912.1.
191 2.4 La statuette de mammouth de Pfedmost. (With Maska and Ober-
maier.) See Maska, 191 2.1.
191 2.5 Les peintures rupestres d'Espagne. (WTith Serrano Gomez and
Cabre Aguilo.) IV — Les Abris del Bosque a Alpera (Albacete).
V Anthropol., tome XXIII, 191 2, pp. 529-562.
191 2.6 Les premiers travaux de l'lnstitut de Paleontologie humaine. (With
Obermaier.) V Anthropol., tome XXIII, 191 2, pp. 1-27.
191 2.7 Les subdivisions du paleolithique superieur et leur signification.
Congr. Intern.. d'Anthrop. d' 'ArcheoL prehist., C. R., XI Ve Sess.,
Geneve, 1912, pp. 165-238.
1913.1 Travaux executes en 191 2. (With Obermaier.) Travaux de l'ln-
stitut de Paleontologie humaine. V Anthropol., tome XXIV,
1913, pp. 1-16.
1913.2 La Pasiega a Puente-Viesgo (Santander, Espagne). (With Ober-
maier and Alcalde del Rio.) Peintures et gravures murales des
cavernes paleolithiques. Institut de Paleontologie humaine.
Monaco, 4to, 1913.
Broca, P.
1868. 1 Sur les cranes et ossements des Eyzies. Bull. Soc. dJ Anthropol.,
Paris, ser. 2, tome III, pp. 350-392.
1875. 1 Instructions craniologiques et craniometriques de la Societe d'An-
thropologie de Paris. Ext. Mem. Soc. d' Anthropol., tome II,
ser. 2, 203 pp., 6 Pis., Paris, Masson et Cie., 8vo., 1875.
Bruckner, E.
1909. 1 Die Alpen im Eiszeitalter. See Penck, A., 1909. 1.
Biichner, L. W. G.
1914.1 A Study of the Curvatures of the Tasmanian Aboriginal Cranium.
Communicated by Professor R. J. A. Berry. Proc. R. Soc. Edin-
burgh, vol. XXXIV, part II, 19 14, pp. 128-143.
BIBLIOGRAPHY 531
Buckland, W.
1823. i Reliquiae Diluvianae; or, Observations on the Organic Remains con-
tained in Caves, Fissures, and Diluvial Gravel, and on Other
Geological Phenomena, attesting the action of an Universal
Deluge. London, 4to, 1823.
Butler, S.
191 1.1 Evolution, Old and New; or, the Theories of Buffon, Dr. Erasmus
Darwin, and Lamarck, as compared with that of Charles Darwin.
With a Preface by R. A. Streatfield (dated October, 191 1), New
York (Dutton), 8vo.
c
Cabre Aguilo, J.
191 2. 1 Les peintures rupestres d'Espagne. (With Breuil and Serrano
Gomez.) See Breuil, H., 1912.5.
Capitan, L.
1898. 1 L'Age de la Pierre. (With Salmon, P., and d'Ault du Mesnil.) See
Salmon, P., 1898. 1.
1 906. 1 L'Abri Mege, une station magdalenienne a Teyjat (Dordogne).
(With Breuil and Peyrony.) Rev. de VEcole d'Anthropol., annee
VI, 1906, pp. 196-212.
1908. 1 La grotte de la Mairie a Teyjat (Dordogne). (With Breuil, Bour-
rinet and Peyrony.) Fouilles d'un gisement magdalenien. Rev.
de VEcole d'Anthropol., annee XVIII, 1908, pp. 153-173.
1910.1 La caverne de Font-de-Gaume aux Eyzies (Dordogne). (With
Breuil and Peyrony.) Peintures et gravures murales des cavernes
paleolithiques publiees sous les auspices de S. A. S. le Prince
Albert Ier de Monaco. Monaco, 4to, 19 10.
191 2. 1 Les gravures sur cascade stalagmitique de la grotte de la Mairie a
Teyjat (Dordogne). (With Breuil, Peyrony, and Bourrinet.)
Congr. Intern. d'Anthropol. et d'Archeol. prehist., C. R., XIV* Sess.,
Geneve, pp. 498-514.
191 2.2 Station prehistorique de la Ferrassie, Commune de Savignac-du-
Bugue (Dordogne). (With Peyrony.) Rev. Anthropol., annee
XXI, no. i, 191 2, pp. 29-50.
Cartailhac, E.
1903. 1 La France prehistorique d'apres les sepultures et les monuments.
Deuxieme edition, avec 162 gravures dans le text. Paris, 8vo,
1903.
1 906. 1 La caverne d'Altamira a Santillane pres Santander (Espagne).
(With Breuil.) Peintures et gravures murales des cavernes pale-
olithiques publiees sous les auspices de S. A. S. Prince Albert Ier
de Monaco. Monaco, 4T.0, 1906.
1908. 1 Les peintures et gravures murales des cavernes pyreneennes. (With
Breuil.) Ill — Niaux (Ariege). V Anthropoid tome XIX, 1908,
pp. 15-46.
532 BIBLIOGRAPHY
1910.1 Les peintures et gravures murales des cavernes pyreneennes. (With
Breuil.) IV — Gargas, die. d'Aventignan (Hautes-Pyrenees).
V Anthropoid tome XXI, 1910, pp. 129-150.
191 2.1 Les Grottes de Grimaldi (Baousse-Rousse). Tome II, fasc. II —
Archeologie. Peintures et gravures murales des cavernes pale-
olithiques publiees sous les auspices de S. A. S. Prince Albert Ier
de Monaco. Monaco, 4to, 191 2.
Chamberlin, T.
1895. 1 Glacial Studies in Greenland. Ill — Coast Glaciers between Disco
Island and Inglefield Gulf. Joum. Geol., vol. Ill, 1895, pp. 61-69.
1905. 1 Geology. .(With Salisbury, R. D.) American Science Series, Ad-
vanced Course, vols. I and II. Second edition, revised, New
York, 8vo, 1905.
de Charpentier, J.
1 84 1. 1 Essai sur les glaciers et sur le terrain erratique du bassin du Rhone.
Lausanne, 8vo, 1841.
Chauvent, G.
1899. 1 Sur l'existence d'une faune d'animaux arctiques dans la Charente
a l'epoque quaternaire. (With Boule, M.) See Boule, M., 1899. 1.
de Christol.
1 8 29. 1 Notice sur les ossemens humains fossiles des cavernes du departement
du Gard. Ext. [Acad. Montpellier], 25 pp. et planche. Mont-
pellier, 8vo, 1829.
Christy, H.
1875. 1 Reliquiae Acquitanicae. (With Lartet, E.) See Lartet, E., 1875. 1.
Collignon, R.
1 890. 1 L'anthropologie au conseil de revision; methode a suivre. Son
application a l'etude des populations des C6tes-du-Nord. Bull.
Soc. dWnthropol., Paris, ser. 4, tome I, 1890, pp. 736-805.
Commont, V.
1906. 1 Les decouvertes recentes a Saint- Acheul, PAcheuleen. Rev. de VEcole
d'Anthropol., Paris, annee XVI, 1906, pp. 228-241.
1908. 1 Les industries de l'ancien Saint-Acheul. V Anthropoid tome XIX,
1908, pp. 527-572.
1 909. 1 L'industrie mousterienne dans la region du nord de la France. Congr.
Prehist. de France, Ve Sess., 1909, pp. n 5-1 57.
1909.2 Saint-Acheul et Montieres. Notes de geologie, de paleontologie et
de prehistoire. Mem. Soc. Geol. du Nord, tome VI, iii.
191 2. 1 Mousterien a faune chaude dans la vallee de la Somme a Montieres-
les-Amiens. Congr. Intern. dWnthropol. et d'Archeol. prehist.,
C. R., XIVC Sess., Geneve, 191 2, pp. 291-300.
Cope, E. D.
1893. 1 The Genealogy of Man. Amer. Nat., vol. XXVII, 1893, pp. 321-335.
BIBLIOGRAPHY 533
D
Dana, J.
1875. i Manual of Geology: Treating of the Principles of the Science with
Special Reference to American Geological History. Second edi-
tion, New York, 8vo, 1875.
Darwin, C.
1871.1 The Descent of Man and Selection in Relation to Sex. Vols. I and
II. London (Murray), 8vo, 1871.
1909. 1 The Descent of Man and Selection in Relation to Sex. Second edi-
tion, revised and enlarged, New York (Appleton), 8vo, 1909.
1909.2 The Origin of Species by Means of Natural Selection, or the Preser-
vation of Favored Races in the Struggle for Life. With additions
and corrections. From sixth and last English edition, New York
(Appleton), 8vo, 1909.
Dawkins, W. Boyd.
1880. 1 Early Man in Britain and His Place in the Tertiary Period. London,
1880.
1883. 1 On the Alleged Existence of Ovibos moschatus in the Forest-Bed, and
on its Range in Space and Time. Quart. Journ. Geol. Soc, Lon-
don, 1883, vol. XXXIX, pp. 575-581.
Dawson, C.
1913.1 On the Discovery of a Palaeolithic Human Skull and Mandible in a
Flint-Bearing Gravel overlying the Wealden (Hastings Beds) at
Piltdown, Fletching (Sussex). With an Appendix by Prof. G.
Elliot Smith. (With A. S. Woodward.) Quart. Journ. Geol. Soc,
London, vol. LXIX, part I, 1913, pp. 117-151, Pis. 15-21.
1913.2 Prehistoric Man in Sussex. Zoologist, ser. 4, vol. 17, pp. 33-36.
1914.1 Supplementary Note; On the Discovery of a Palaeolithic Human
Skull and Mandible in a Flint-Bearing Gravel, etc. (With A. S.
Woodward.) With an Appendix by Prof. Grafton Elliot Smith.
Quart. Journ. Geol. Soc, vol. LXX, 1914, pp. 82-99, Pis. 14, 15.
Dechelette, J.
1908. 1 Manuel d'archeologie prehistorique celtique et gallo-romaine. Tome
I — Archeologie prehistorique (1908). Tome II — Archeologie celti-
que ou protohistorique. Premiere partie — Age du Bronze (1910).
Deuxieme partie — Premier Age du Fer ou Epoque de Hallstatt
(1913). Appendices (1910). Appendices (Supplement) (1912).
Paris, 8vo, 1910-1913.
Desnoyers, J.
1863. 1 Note sur des indices materiels de la coexistence de l'homme avec
VElephas meridionalis dans un terrain des environs de Chartres,
plus ancien que les terrains transport quaternaires des vallees
de la Somme et de la Seine. C. R. Acad. Set., Paris, tome 56, 1863,
pp. 1073-1083.
534 BIBLIOGRAPHY
Dietrich, W. O.
1910.1 Neue fossile Cervidenreste aus Schwaben. Jahreshefte, Ver. vaterl.
Naturk., Wiirttemberg, 66 Jahrg., 1910, pp. 318-336.
Dubois, E.
1 894. 1 Pithecanthropus ertctus, erne Menschenaehnliche Uebergangsform
aus Java., Batavia, 4to, 1894.
Dupont, E.
1 866. 1 Etudes sur les fouilles scientifiques executees pendant l'hiver de
1 86 5-1 866 dans les cavernes des bords de la Lesse. Bull. Acad.
R. de Belgique, ser. 2, tome XXII, 1866, pp. 31-54.
1 87 1. 1 Les temps antehistoriques en Belgique. L'homme pendant les ages
de la pierre dans les environs de Dinant-sur-Meuse. Deuxieme
edition. Bruxelles (Muquardt), 8vo, 187 1.
E
Eccardus, J. G.
1 7 50. 1 De Origine et Moribus Germanorum eorumque vetustissimis colonis,
migrationibus ac rebus gestis. (Ioh. Guil. Schmidii), 4to, Goet-
tingae, do h ccl (1750).
Elbert, J.
1 908. 1 Uber das Alter der Kendeng-Schichten mit Pithecanthropus erectus
Dubois. N. Jahrb. Mineral. Geol. u. Pal., XXV Beil.-Bd., 1908,
pp. 648-662.
Ewart, J. C.
1904. 1 The Multiple Origin of Horses and Ponies. Trans. Right. Agri. Soc.
Scotland, 1904, pp. 1-39.
1 907. 1 On the Skulls of Horses from the Roman Fort at Newstead, near
Melrose, with Observations on the Origin of the Domestic Horses.
Trans. R. Soc. Edinburgh, vol. XLV, part III, no. 20, 1907, pp.
555-587.
1 909. 1 The Possible Ancestors of the Horses Living under Domestication.
Science, n. s., vol. XXX, no. 763, August 13, 1909, pp. 219-223.
F
de Ferry, H.
1 869. 1 L'Age du Renne en Maconnais. Memoire sur le gisement archeol-
ogique du clos du Charnier a Solutre, Departement de Saone-et-
Loire. (Compte rendu des fouilles operees en 1867 et 1868 par
MM. H. de Ferry et A. Arcelin.) Trans. Intern. Congr. Prehist.
Archeol., IIP Sess., London, 1868 (published 1869), pp. 319-350,
Pis. I, II.
Fischer, E.
1913.1 Fossile Hominiden. Sondcrabd. Handworterbuch Naturwiss., Bd. IV,
PP- 332-360, Jena, 8vo, 1913.
BIBLIOGRAPHY 535
Fraipont, J.
1887. i La race de Neanderthal ou de Canstadt en Belgique. (With Lohest
M.) Arch. Biol., tome VII, 1887, pp. 587-757.
Fraunholz, J.
191 1.1 Die Kastlhang-Hohle, eine Renntierjagerstation im bayerischen
Altmiihltale. Mit einem Beitrag von Max Schlosser. (With
Obermaier.) Beitrdge, Anthropol. u. Urgesch. Bayerns, Bd. XVIII,
191 1. (Unpaged separate.)
G
Gaudry, A.
1876. 1 Materiaux pour l'histoire des temps quaternaires. Fasc. I. Paris,
4to, 1876.
1 890. 1 Le Dryopitheque. Mem. Soc. Geol. de France, Pal. Mem. no. 1.
Paris, 4to, 1890.
Geikie, J.
1 894. 1 The Great Ice Age and Its Relation to the Antiquity of Man. Third
edition, largely rewritten. London, 8vo, 1894.
1 914. 1 The Antiquity of Man in Europe, being the Munro Lectures, 1913.
Edinburgh, 8vo, 19 14.
Godwin-Austen.
1840. 1 On the Geology of the Southeast of Devonshire. Trans. Geol. Soc,
ser. 2, vol. VI, pp. 433-489, PI. XLII.
Gorjanovic-Kramberger, K.
1 901. 1 Der palaolithische Mensch und seine Zeitgenossen aus dem Diluvium
von Krapina in Kroatien. Mitt. Anthrop. Gesell. Wien, Bd. 31,
pp. 163-197, 4 Pis., 13 Figs.
1 903. 1 Nachtrag (to the above). Mitt. Anthrop. Gesell. Wien, Bd. 32, pp.
189-216, 4 Pis., 17 Figs.
1906. 1 Der diluviale Mensch von Krapina in Kroatien. Ein Beitrag
zur Palaoanthropologie. Studien iiber Entwicklungsmechanik
des Primatskelettes mit besonderer Berucksichtigung der Anthro-
pologic und Descendenzlehre. . . . Herausgegeben von Dr. Otto
Walkhoff, Wiesbaden, 4to, 1906.
1909. 1 Der vordere Unterkieferabschnitt des altdiluvialen Menschen in
seinem genetischen Verhaltnis zum Unterkiefer des rezenten
Menschen und den der Anthropoiden. Zeitschr. Abstammungs-
u. Vererbungsl., Bd. I, pp. 411-439.
Gregory, W. K.
The Dawn Man of Piltdown, England. Am. Mus. Jour., vol. XIV,
May, 1914.
H
Harle, E.
1 899. 1 Notes sur la Garonne. Bull. Soc. d'Hist. Nat. Toulouse, annee
XXXII (Oct., 1899), pp. 149-198.
1908.1 Faune quaternaire de la province de Santander (Espagne). Bull.
Soc. Geol. de France, ser. 4, tome VIII, 1908, pp. 82-83.
■(
536 BIBLIOGRAPHY
1910.1 Les mammiferes et oiseaux quaternaries connus jusqu'ici en Portugal.
Memoire suivi d'une liste generate de ceux de la Peninsule Iberique.
Ext. tome VIII, " ' Communicacoes," Service Geol. du Portugal.
Haug, E.
1907. 1 Traite de Geologic Tome I — Les Phenomenes geologiques (1907).
Tome II — Les Periodes geologiques (191 1). Paris, 8vo.
Hauser, O.
1909. 1 Homo aurignacensis Hauseri, etc. See Klaatsch, H., 1909. 1.
Heim, A.
1 894. 1 Ueber das absolut Alter der Eiszeit. Vierteljahrschrif. naturf. Gesell.
Zurich, Bd. 39, 1894, pp. 180-186.
Hilzheimer.
1 913. 1 Studienreise zu den palaolithischen Fundstellen der Dordogne. See
Wiegers, 1913.1.
Hrdlicka, Dr. A.
1914.1 The Most Ancient Skeletal Remains of Man. Report, Smithsonian
Institution, etc., 1913, pp. 491-552, Pis. 1-41. Publication 2300.
Government Printing Office, Washington, 8vo, 1914.
Huntington, E.
1 907. 1 The Pulse of Asia.' New York, 8vo, 1907.
J
James, W.
1902.1 The Varieties of Religious Experience. A Study in Human Nature.
Being the Gifford Lectures on Natural Religion delivered at
Edinburgh in 1901-1902. New York, 8vo, 1902.
Johnson, J. P.
1913.1 The Stone Implements of the Tasmanians. Nature, vol. 92, no. 2298,
November 13, 1913, p. 320.
K
Keane, A. H.
1901.1 Ethnology. Cambridge Geographical Series. Stereotyped edition.
Cambridge, 8vo. 1901.
Keith, A.
1911.1 Ancient Types of Man. Harper's Library of Living Thought. New
York, 121110. 191 1.
191 1.2 Discovery of the Teeth of Palaeolithic Man in Jersey. Nature, vol.
86, no. 2169, May 25, 191 1, p. 414.
191 1.3 The Early History of the Gibraltar Cranium. Nature, vol. 87, no.
2184, September 7, 191 1, pp. 313, 314.
BIBLIOGRAPHY 537
191 2.1 Cranium of the Cro-Magnon Type found by Mr. W. M. Newton in
a Gravel Terrace near Dartford. Rpt. 82d Meeting, Brit. Assoc.
Adv. Sci., Dundee, 191 2, pp. 516, 517.
191 2.2 Hunterian Lecture on Certain Phases in the Evolution of Man.
(Abstract.) Brit. Med. Joum., 191 2, vol. I, pp. 734-737, 788-790.
1913.1 The Piltdown Skull and Brain Cast. Nature, vol. 92, no. 2294,
October 16, 1913, pp. 197-199.
1913.2 The Piltdown Skull and Brain Cast. Nature, vol. 92, no. 2297,
November 6, 1913, p. 292.
1913.3 The Piltdown Skull and Brain Cast. Nature, vol. 92, no. 2299,
November 20, 1913, pp. 345, 346.
Kennard, A. S.
1913.1 [Discussion of] On the Discovery of a Palaeolithic Human Skull and
Mandible . . . at Piltdown, Fletching (Sussex). See Dawson, C,
1913.1, p. 150.
King, W.
1 864. 1 The Reputed Fossil Man of the Neanderthal. Quart. Joum. Sci.,
vol. I, pp. 88-97, Pis. I, II.
Klaatsch, H.
1 909. 1 Homo aurignacensis Hauseri, ein palaolithischer Skeletfund aus dem
unteren Aurignacien der Station Combe- Capelle bei Montf errand
(Perigord). (With Hauser.) Prdhist. Zeitschr., Bd. I, 1909
(Heft 3-4, 1910), pp. 273-338.
Koken, E.
1912.1 Die diluviale Vorzeit Deutschlands, von R. R. Schmidt. II — Geolo-
gischer Teil von Ernst Koken. Die Geologie und Tierwelt der
palaolithischen Kulturstatten Deutschlands. See Schmidt, R. R.,
1912.1.
Kraemer, H.
Weltall und Menschheit. Geschichte der Erforschung der Natur
und der Verwertung der Naturkrafte im Dienst der Volker. Band
II. Berlin, n. d.
L
Lalanne, G.
191 1. 1 L'abri sculpte de Cap-Blanc a Laussel (Dordogne). (With BreuiL
H.) See Breuil, H., 1911.1.
Lamarck, J.
1809. 1 Philosophic Zoologique. Paris (Duminil-Leseur), 8vo, 1909.
181 5.1 Histoire naturelle des animaux sans vertebres. . . . Tomes 1-7
(1815-1822). Paris (Verdiere), 8vo, 1815-1822.
Lartet, E.
1861.1 Nouvelles recherches sur la coexistence de l'homme et des grands
mammiferes fossiles reputes caracteristiques de la derniere periode
538 BIBLIOGRAPHY
geologique. Ann. Sci. Nat., ser. 4, Zoologie, tome XV, 1861, pp.
177-253, PL X.
1875. 1 Reliquiae Acquitanicae. (With Christy.) Being Contributions to
the Archaeology and Palaeontology of Perigord and the Adjoining
Provinces. Edited by Rupert Jones. London, 4to, 1875.
Leverett, F.
1 910. 1 Comparison of North American and European Glacial Deposits.
Zeitschr. fiir Gletscherk., Bd. IV, 1910, pp. 241-316.
Lubbock, Sir J. (See Avebury, Lord).
1 86 2. 1 On the Evidences of the Antiquity of Man afforded by the Physical
Structure of the Somme Valley. Nat. Hist. Rev., 1862, pp.
244-269.
Lyell, Sir C.
1 863. 1 The Geological Evidences of the Antiquity of Man with Remarks
on the Theories of the Origin of Species by Variation. Second
revised edition. London (Murray), 8vo, 1863.
1 86 7. 1 Principles of Geology or the Modern Changes of the Earth and Its
Inhabitants Considered as Illustrative of Geology. Tenth and
entirely revised edition. Vol. I, 1867. Vol. II, 1868. London
(Murray), 8vo, 1867-1868.
1 87 7. 1 Principles of Geology or the Modern Changes of the Earth and its
Inhabitants Considered as Illustrative of Geology. Eleventh and
entirely revised edition. Vol. I, 1877. Vol. II, 1872. New
York (Appleton), 8vo, 1872-1877..
M
MacCurdy, G. G.
1 905. 1 The Eolithic Problem. Evidences of a Rude Industry Antedating
the Paleolithic. Amer. Anthropol., n. s., vol. VII, no. 3, 1905,
pp. 425-479-
Mahudel.
1 740. 1 Sur les pretendues pierres de foudre. Hist. Acad. R. Inscript. et
Belles-Lettres, Paris, tome XII, 1740, pp. 163-168.
Makowsky, A.
1892. 1 Der diluviale Mensch im Loss von Briinn. Mitt. Anthropol. Gesell.
Wien, Bd. XXII (N. F. Bd. XIII), pp. 73-84.
Marett, R. R.
Anthropology. Home University Library of Modern Knowledge.
New York (Henry Holt & Co.), i2mo, n. d.
Martin, H.
1910.1 Astragale humain du Mousterien moyen de La Quina. (Ext., Bull.
Soc. prehist. de France, 19 10, p. 391.) [Reviewed by M. Boule.]
U Anthropol., tome XXII, 1911, pp. 312, 313.
BIBLIOGRAPHY 539
Martin, R.
1 9 14. i Lehrbuch der Anthropologic in systematischer Darstellung. Mit
besonderer Beriicksichtigung der anthropologischen Methoden.
Fur studierende Arzte und Forschungsreisende. Jena, 8vo,
1914.
Martins, C.
1 847. 1 Recherches sur la periode glaciaire et l'ancienne extension des glaciers
du Mont-Blanc depuis les Alpes jusqu'au Jura. Rev. deux mondes
1847, tome 17, pp. 919-942.
Maska, K.
1886. 1 Fund des Unterkiefers in der Schipka-Hohle. Verh. Berliner Gesell.
f. Anthropol., Ethnol. u. Urgesch., 1886, pp. 341-350.
191 2. 1 La statuette de mammouth de Pfedmost. (With Obermaier and
Breuil.) V Anthropol., tome XXIII, 191 2, pp. 273-285.
Massenat, E.
1869. 1 Objets graves et sculptes de TAugerie Basse (Dordogne). Mater,
pour Vhist. de Vhomme, annee V, ser. 2, pp. 348-356.
Morlot, A.
1854. 1 Notice sur le Quaternaire en Suisse. Bull. Soc. Vaudoise, Set. nat.,
1854, pp. 41-45.
de Mortillet, A.
1 869. 1 Essai d'une classification des cavernes et des stations sous abri,
fondee sur les produits de l'industrie humaine. C. R. Acad. Sci.,
Paris, tome 68, 1869, pp. 553-555-
de Mortillet, G.
1872. Classification des ages de la pierre. Classification des di verses periodes
de l'age de la pierre. C. R. Congr. Intern, d' Anthropol., d'Archeol.
Prehist., VP Sess. Bruxelles, 1872, pp. 432-444.
Munro, R.
1 893. 1 [On the Relation between the Erect Posture and the Physical and
Intellectual Development of Man.] Rpt. 63d Meeting, Brit. Assoc.
4dv. Sci., Nottingham, 1893, Presidential Address, Section of
Anthropology, pp. 885-889.
191 2. 1 Palaeolithic Man and the Terramara Settlements in Europe. Being
the Munro Lectures in Anthropology and Prehistoric Archaeology
in connection with the University of Edinburgh. Edinburgh,
8vo, 1912.
N
Nehring, A.
1 880. 1 Ubersicht iiber vierundzwanzig mitteleuropaische Quatar-Faunen.
Zeitschr. deutsch. geolog. Gesell., 1880, pp. 468-509,
yl
.540 BIBLIOGRAPHY
1896. i Die kleineren Wirbeltiere vom Schweizersbild bei Schaffhausen.
N. Denkschr. allg. schweiz. Gesell. gesam. Naturwiss., Bd. XXXV,
1896, pp.- 40-77-
Neumeyer, M.
1890. 1 Erdgeschichte. Band I, 1895. Band II, 1890. Leipzig, R. 8vo,
1890-1895.
Nicolle, E. T.
1910.1 Report on the Exploration of the Palaeolithic Cave-Dwelling known
as La Cotte, St Brelade, Jersey. (With Sinel, J.) Man, 1910,
nos. 101-102, pp. 185-188.
Niezabitowski, E.
191 1.1 Die Uberreste des in Starunia in einer Erdwachsgrube mit Haut und
Weichteilen gefundenen Rhinoceros antiquitatis Blum, (tichorhinus
Fisch.). Bull. Acad. Sci. Cracovie, Classe des Sci. Mathemat., etc.,
191 1, ser. B; Sci. nat., pp. 240-266.
Niiesch, J.
1902. 1 Das Schweizersbild, eine Niederlassung aus palaeolithischer und neo-
lithischer Zeit. Die praehistorische Niederlassung am Schwei-
zersbild bei Schaffhausen. Die Schichten und ihre Einschliisse.
N. Denkschr. allg. schweiz. Gesell. gesam. Naturwiss., Bd. XXXV,
zweite Verbesserung, pp. 1-120.
o
Obermaier, H.
1909. 1 Cranes paleolithiques faconnes en Coupes. (With Breuil.) See
Breuil, H., 1909.2.
1909.2 Les formations glaciaires des Alpes et l'homme paleolithique. V An-
thropol., tome XX, 1909, pp. 497-522.
1909.3 Die Aurignacienstation von Krems (N.-O.). (With Strobel.) See
Strobel, 1909. 1.
191 1.1 Die Kastlhang-Hohle, eine Renntierjagerstation im bayerischen
Altmuhltale. (With Fraunholz und Schlosser.) See Fraunholz,
J., 1911.1.
191 2.1 Der Mensch der Vorzeit. Munchen, R. 8vo, 1912.
1 9 1 2 . 2 Les premieres travaux de l'lnstitut de Paleontologie humaine. (With
Breuil.) See Breuil, H., 1912.6.
191 2.3 La statuette de mammouth de Pfedmost. (With MaSka et Breuil.)
See MaSka, 1912.1.
1913.1 La Pasiega a Puente-Viesgo (Santander, Espagne). (With Breuil
and Alcalde del Rio.) See Breuil, H., 1913.2.
Osborn, H. F.
1894. 1 From the Greeks to Darwin. An Outline of the Development of
the Evolution Idea. New York, 8vo, 1894.
1910.1 The Age of Mammals in Europe, Asia and North America. New
York, 8vo, 1910.
BIBLIOGRAPHY 541
P
Penck, A.
1908. i Das Alter des Menschengeschlechts. Zeitschr. fur Ethnol., Jahrg. 40,
Heft 3, 1908, pp. 390-407.
1 909. 1 Die Alpen im Eiszeitalter. (With Bruckner, E.) Band I, II, III.
Leipzig, R. 8vo, 1909.
Peyrony, M.
1908. 1 La grotte de la Mairie a Teyjat (Dordogne). (With Capitan and
Breuil.) See Capitan, L., 1908. 1.
1910.1 La caverne de Font-de-Gaume aux Eyzies (Dordogne). (With
Breuil and Capitan.) See Capitan, 1910.1.
191 2.1 Les gravures sur cascade stalagmitique de la grotte de la Mairie a
Teyjat (Dordogne). (With Breuil, Bourrinet, and Capitan.) See
Capitan, 1912.2.
Piette, E.
1907. 1 L'art pendant l'Age du Renne. Album de cent planches dessinees
par J. Pilloy. Paris, small folio, 1907.
Pilgrim, G.
1 913. 1 The Correlation of the Siwaliks with Mammal Horizons of Europe.
Records, Geol. Survey India, vol. XLIII, part 4, pp. 264-326, Pis.
26-28.
0
Quatrefages, A.
1884. 1 Hommes fossiles et hommes sauvages. Etudes d'Anthropologie.
Paris, 8vo, 1884.
R
Reeds, C. A.
191 5. 1 The Graphic Projection of Pleistocene Climatic Oscillations. Bull.
Geol. Soc. Amer., vol. 26, no. 1, 1915, pp. 106-109.
Reid, C.
1908. 1 The Pre-Glacial Flora of Britain. (With E. M. Reid.) Joum.
Linn. Soc. Botany, vol. XXXVIII, 1908, pp. 206-227.
1913.1 [Discussion of] On the Discovery of a Palaeolithic Human Skull and
Mandible ... at Piltdown . . . Sussex. See Dawson, C,
1913.1.
Reinach, S.
1889. 1 Antiquites nationales. Description raisonnee du Musee de Saint-
Germain-en-Laye. I — Epoque des alluvions et des cavernes.
Paris, 8vo [1889], 322 pp.
1913.1 Repertoire de l'Art quaternaire. Paris, i2mo, 1913.
542 BIBLIOGRAPHY
Retzius, A.
1 864. i Ethnologische Schriften. Ill — Ueber die Form des Knochengeriistes
des Kopfes bei verschiedenen Volkern. Stockholm, 4to, 1864.
Rigollot,
1 8 54. 1 Memoires sur des instruments en silex trouvees a Saint- Acheul.
Amiens, 1854.
Ripley, W. Z.
1899. 1 The Races of Europe. A Sociological Study. (Lowell Institute
Lectures.) Accompanied by a Supplementary Bibliography of
the Anthropology and Ethnology of Europe, etc. New York,
8vo, 1899.
Riviere, E.
1897. 1 La grotte de La Mouthe (Dordogne). Bull. Soc. d'Anthropol.,
Paris, ser. 4, tome VIII, 1897, pp. 302-329; 484-490; 497-501.
1897.2 La grotte de La Mouthe (Dordogne). C. R. assoc. franq. pour
V"avanc. sci., 26me Sess., Saint-Etienne, 1897, pp. 669-687.
Robertson, A. W. D.
1914.1 The Place in Nature of the Tasmanian Aboriginal as Deduced from
a Study of his Calvaria. (With Berry, R. J. A.) See Berry, R.
J. A., 1914.1.
Rutot, A.
1 902. 1 Les industries primitives. Defense des eolithes. Les actions natu-
relies possibles sont inaptes a produire des effets semblables a la
retouche intentionelle. Bull, et Mem. Soc. Anthropol., Bruxelles,
tome XX (1902), mem. III.
1 907. 1 A fin de la question des eolithes. Bull. Soc. Beige Geol., Proces-
Verbal, 1907, tome XXI, pp. 211-217.
Rzehak, Prof. A.
1906. 1 Der Unterkiefer von Ochos. Ein Beitrag zur Kenntnis des altdi-
luvialen Menschen. Verhandl. naturf. Ver., Briinn, Bd. XLIV
(1905), pp. 91-114. Published in 1906.
s
Salisbury, R. D.
1905. 1 Geology. (With Chamberlin, T. C.) See Chamberlin, T., 1905. i„
Salmon, P.
1898. 1 Age de la pierre: habitations neolithiques. (With d'Ault du Mesnil
and Capitan.) Le Campignien. Rev. de VEcole d'Anthropol., annee
VIII, 1898, pp. 365-408.
de Sautuola, M.
1 880. 1 Breves apuntes sobre algunos objetos prehistoricos de la provincia
de Santander. Madrid, 1880, 4 pi.
BIBLIOGRAPHY 543
Schaaffhausen, D.
1 85 7. i Theilen des menschlichen Skelettes im Neanderthale bei Hochdal.
Sitzungsber. niederrhein. Gesellsch. f. Natur u. Heilkunde, Bonn,
1857, pp. xxxviii-xlii.
1858. 1 Zur Kenntniss der altesten Rassenschadel. Miilleis Archiv, Jahrg.
1858, pp. 453-478.
Schliz, A.
1912.1 Die diluviale Vorzeit Deutschlands, von R. R. Schmidt. Teil III —
Anthropologischer Teil. Die diluvialen Menschenreste Deutsch-
lands. See Schmidt, R. R., 1912.1.
Schlosser, M.
191 1.1 Die Kastlhang-Hohle, eine Renntierjagerstation im bayerischen Alt-
miihltale. (With Fraunholz und Obermaier.) See Fraunholz,
1911.1.
Schmerling, P.-C.
1 833. 1 Recherches sur les Ossemens Fossiles decouvertes dans les cavernes
de la province de Liege. Liege, 4X0, 1833.
Schmidt, R. R.
1912.1 Die diluviale Vorzeit Deutschlands. I — Archaologischer Teil: Die
diluvialen Kulturen Deutschlands, R. R. Schmidt. II — Geologi-
scher Teil: Die Geologie und Tierwelt der palaolithischen Kultur-
statten Deutschlands, Ernst Koken. Ill — Anthropologischer
Teil: Die diluvialen Menschenreste Deutschlands, A. Schliz.
Stuttgart, 4to, 191 2.
Schoetensack, O.
1 908. 1 Der Unterkiefer des Homo heidelbergensis aus den Sanden von Mauer
bei Heidelberg. Ein Beitrag zur Palaontologie des Menschen.
Leipzig, 4to, 1908.
Schuchert, C.
1913.1 Climates of Geologic Time. Reprint, Carnegie Inst, of Washington,
Publication No. 192, pp. 263-298.
Schuchhardt, C.
1 9 13. 1 Palaolithische Fundstellen der Dordogne. (With Wiegers und Hilz-
heimer.) See Wiegers, 1913.1.
Schwalbe, G.
1897. 1 Ueber die Schadelformen der altesten Menschenrassen mit besonderer
Beriicksichtigung des Schadels von Egisheim. Mitt. Philomat.
Gesell. Elsass-Lothringen, Jahrg. 5 (1897), Heft III, pp. 72-85.
1899. 1 Studien liber Pithecanthropus erectus Dubois. Zeitschr. f. Morph.
u. Anthropoid Bd. I, Heft I, pp. 16-22, Pis. I-III.
1901.1 Der Neanderthalschadel. Bonner Jahrb., no. 106, Bonn, pp. 1-72.
1901.2 tJber die specifischen Merkmale des Neanderthalschadels. Verh.
Anat. Gesell., Bonn, 1901, pp. 44-61.
1904.1 Die Vorgeschichte des Menschen. Braunschweig, 8vo, 1904.
544 BIBLIOGRAPHY
1 906. i Das Schadelfragment von Briix und verwandte Schadelformen.
Zeitschr. fiir Morphol. und Anthropol., Sonderheft, 1906, pp. 81-182,
Pis. I-IL
1914.1 Kritische Besprechung von Boule's Werk: "L'homme fossile de La
Chapelle-aux-Saints " mit eigenen Untersuchungen. Zeitschr.
Morph. u. Anthropol., Bd. XVI, Heft 3, pp. 527-610.
19 14. 2 Uber einen bei Ehringsdorf in der Nahe von Weimar gefundenen
Unterkiefer des Homo primigenius. Anat. Anzeiger, Band 47,
nos. 13-17. Oktober,' 1914, pp. 337~345-
Selenka, L.
191 1.1 Die Pithecanthropus-Schichten auf Java. (With Blanckenhorn.)
Geologische und palaontologische Ergebnisse der Trinil-Expedition
( 1 907-1 908). Herausgegeben von M. Lenore Selenka und Prof.
Max Blanckenhorn, Leipzig, 4to, 191 1.
Serrano Gomez, P.
191 2. 1 Les peintures rupestres d'Espagne. (With Breuil and Cabre Aguilo.)
See Breuil, 1912.5.
Sierra, R. P. L.
1 91 2. 1 Les cavernes de la region cantabrique (Espagne). (With Alcaldfc
del Rio and Breuil.) See Alcalde del Rio, 191 2.1.
Smith, G. E.
191 2.1 Presidential Address to the Anthropological 'Section (B. A. A. S.).
Rpt. S20I Meeting, Brit. Assoc. Adv. Sci., Dundee, 1912, pp. 575-598.
1913.1 The Controversies concerning the Interpretation and Meaning of
the Remains of the Dawn-Man Found near Piltdown. [Abstract.]
Meet. Manchester Lit. and Philosoph. Soc, November 18, 1913.
1913.2 On the Discovery of a Palaeolithic Human Skull and Mandible in a
Flint-Bearing Gravel overlying the Wealden (Hastings Beds) at
Piltdown, Fletching (Sussex). With an Appendix by Prof.
Grafton Elliot Smith. See Dawson, C, 1913.1.
1913.3 The Piltdown Skull. Nature, vol. 92, no. 2292, October 2, 1913,
p. 131.
1913.4 The Piltdown Skull and Brain Cast. Nature, vol. 92, no. 2296,
October 30, 1913, pp. 267, 268.
1914.1 Supplementary Note on the Discovery of a Palaeolithic Human Skull
and Mandible at Piltdown (Sussex). (With Dawson and Wood-
ward.) With an Appendix by Prof. Grafton Elliot Smith. See
Dawson, C, 1914.1.
Smith, W.
1894. 1 Man the Primeval Savage. His Haunts and Relics from the Hill-
Tops of Bedfordshire to Blackwall. London, 8vo, 1894.
Sollas, W. J.
1 900. 1 Evolutional Geology. Presidential Address to the Geological Sec-
tion (B. A. A. S.). Rpt. 70th Meeting, Brit. Assoc. Adv. Sci., Brad-
ford, 1900, pp. 711-730.
BIBLIOGRAPHY 545
191 i.i Ancient Hunters and Their Modern Representatives. London, 8vo.
1911.
1913.1 Paviland Cave: An Aurignacian Station in Wales. (The Huxley
Memorial Lecture for 1913.) Joum. R. AnthropoL Inst, of Gr.
Brit. fr Ireland, vol. XLIII, 1913, pp. 325-373.
Steinmann, C.
1914.1 Diluviale Menschenfunde in Obercassel bei Bonn. (With Verworn
and Bonnet.) IV — tJber das geologische Alter der Fundstelle.
See Verworn, M., 1914.1.
Strobel, J.
1909. 1 Die Aurignacienstation von Krems (N.-C3.). (With Obermaier, H.)
Mit einem Anhang von Oskar von Troll. Jahrb. Alter tumskunde,
Bd. Ill, 1909, pp. 129-148, Pis. XI-XXI.
T
Tomes, C. S.
1914.1 A Manual of Dental Anatomy, Human and Comparative. Edited
by H. W. Marett Tims and A. Hopewell-Smith. Seventh edition.
(J. and A. Churchill.) London, 8vo, 1914, 616 pp.
von Troll, O.
1909. 1 Die Aurignacienstation von Krems (N.-O.). (With Strobel and
Obermaier.) Mit einem Anhang von Oskar von Troll. See
Strobel, J., 1909. 1.
u
Upham, W.
1 893. 1 Estimates of Geologic Time. Artier. Joum. Sci., vol. XLV, 1893,
pp. 209-220.
V
Verneau, R.
1886. 1 La race de Cro-Magnon. Rev. AnthropoL, ser. 3, tome I, 1886, pp.
10-24.
1 89 1. 1 Cinq annees de sejour aux iles Canaries. Paris, 1891.
1906. 1 Les Grottes de Grimaldi (Baousse-Rousse). Tome II, fasc. I—
Anthropologic Monaco, 4to, 1906
Verworn, M.
1914.1 Diluviale Menschenfunde in Obercassel bei Bonn. (With Bonnet
and Steinmann.) I — Fundbericht, Verworn. II — Die Kulturstufe
des Fundes, Verworn. Ill— Die Skelete, Bonnet. IV— Uber das
geologische Alter der Fundstelle, Steinmann. Die Naturwisscn-
schaften, Heft 27, Jahrg. 2, 3 Juli 1914, pp. 645-650.
546 BIBLIOGRAPHY
de Vibraye.
1864. i Note sur des nouvelles preuves de l'existence de Thornine dans le
centre de la France a, une epoque ou. s'y trouvaient aussi divers
animaux qui de nos jours n'habitent pas cette contree. C. R.
Acad. Sci., Paris, tome 58, 1864, pp. 409-416.
Villeneuve, L.
1906. 1 Les Grottes de Grimaldi (Baousse-Rousse). Tome I, fasc. I— His-
torique et Description. Monaco, 4to, 1906.
Volz, W.
1 907. 1 Das geologische Alter der Pithecanthropus-Schichten bei Trinil,
Ost-Java. N. Jahrb. Miner., Geol. u. Paldontol., Festband, 1907,
pp. 256-271.
w
Walcott, C. D.
1 893. 1 Geologic Time as Indicated by the Sedimentary Rocks of North
America. Amer. Geol., vol. XII, no. 6, 1893, pp. 343-368, PL XV.
Wiegers, F.
1913.1 Eine Studienreise zu den palaolithischen Fundstellen der Dordogne.
(With Schuchhardt and Hilzheimer.) Zeitschr. f. Ethnol., Jahrg.
45, Heft I, 1913, pp. 126-160.
Wilser, L.
1898. 1 Menschenrassen und Weltgeschichte. Naturwiss. Wochenschr., Band
XIII, Heft 1, 1898.
Woodward, A. S.
19 13. 1 On the Discovery of a Palaeolithic Human Skull and Mandible in a
Flint-Bearing Gravel overlying the Wealden (Hastings Beds) at
Piltdown, Fletching, Sussex. (With Dawson, C.) With an
Appendix by Prof. Grafton Elliot Smith. See Dawson, C., 1913.1.
1 914. 1 Supplementary Note on the Discovery of a Palaeolithic Human Skull
and Mandible at Piltdown (Sussex). (With Charles Dawson.)
With an Appendix by Prof. Grafton Elliot Smith. See Dawson,
C., 1914.1.
1914.2 On the Lower Jaw of an Anthropoid Ape (Dryopithecus) from the
Upper Miocene of Lerida (Spain). Quart. Journ. Geol. Soc.,
London, vol. LXX, pp. 316-320, PI. XLIV.
191 5. 1 A Guide to the Fossil Remains of Man in the Department of Geology
and Palaeontology in the British Museum (Natural History),
Cromwell Road, London, S. W. With 4 plates and 12 text-figures.
Printed by order of the trustees of the British Museum. 8vo,
1915, 33 PP.
INDEX
INDEX*
Abbeville, 109, 116, 124, 125, 127, 149, 152,
156, 166, 167, 244, 331
Abri Audit, 245, 246, 248, 255, 269, 277,
305, 3o7, 309, 3ii5 3i4
Abri Dufaure, 471
Abri Mege, 435, 442
Abris, see Rock Shelters
Achenheim, 30, 160, 161, 167, 176, 195, 284,
3i4
Achenschwankung, see Postglacial Stage
Acheulean, 14-16, 18, 30; chronology, 33,
41, 89; climate, 112, 117, 118, 165, 166,
173, 174, 175-177, 186; fauna, 144-148,
165; geography (physical), 166; human
fossils, 24, 181-185; industry, 14, 16,
18, 41, 108, 113, 122-124, 169-173, 177-
180, 270, 280, 362; stations, 151, 158-
162, 166-169; see Origin
iEschylus, on the prehistory of man, 3, 505
Aggsbach, 29, 435, 448
Agriculture, 2, 486, 496
Aiguille, needle, 271, 310, 313, 387, 388,
391, 392, 440, 443-445, 449, 46i, 462
Alactaga jaculus, 373, 374; see Jerboa
Alces, 187, 287, 369; latifrons, 70, see Moose
Alento, 167
Alpera, 469, 497
Alpine fauna, see Fauna
Alpine race, 278, 458, 479, 480, 481, 484,
485, 49i, 499, 5oo
Alpine vole, 371, see Arvicola nivalis
Altamira, 17, 319, 321, 331, 332, 346, 368,
385, 394, 395, 399, 408, 415, 416, 422-427,
434, 435, PL VIII
Ancestry of Man, see Man
Ancona, 167
Andernach, 160, 195, 279, 372, 378, 435
Anthropoid Apes, 3, 21; ancestry, 49-61;
brain, 52-60; compared with Grimaldi,
266, with Neanderthal, 9, 217, 230-233,
237-240, with Piltdown, 140, 141, with
Pithecanthropus, 9, 77-79; known to
Carthaginians, 511, 512; recent dis-
coveries, 511
Anthropology, rise of, 3-10
A.itilope saiga, see Saiga antelope
Anvils, bone, 211, 253, 256, 271; see Com-
presseur
Apes, see Anthropoid
Arboreal life, effects of, 56, 57
Archaeology, rise of, 10-18
Archer, 329
Arctomys marmotta, 182, 370; see Marmot
Arcy-sur-Cure, 214, 219, 435
Argali sheep, 46, 285, 287, 37 rf see Ovis
argaloides
Arrow, 214, 258, 270, 272, 344, 353, 354, 410,
45o, 497
Art, 13, 14, 17, 21, 315-330, 332, 347-350,
392-434, 449, see Aurignacian, Magda-
l^nian, Solutrean, Engraving, Painting,
Sculpture, Industry; implements used in,
270, 309-312, 321, 329, 330, 385, 396, 415,
463; means of dating, 317-320
Arudy, 435, 436
Arvicola, amphibius, 147; gregalis, 373;
nivalis, 370, 371
Ascoli Piceno, 167
Ass, wild (kiang), see Horse
Aurensan, 435, 438, 471
Aurignac, 5, 13, 14, 16, 275, 279, 290, 294,
3i4
Aurignacian, 14-16, 18, 275, 276; art, 315-
330, 403, 404, 408; burial customs, 302-
305; chronology, 33, 41, 35 1 5 climate, 123,
281-286; fauna, 285-289; human fossils,
289-305; industry, 16, 18, 41, 108, 269-
271, 275-277, 280, 305-313, 329, 330,
362; stations, 275, 283, 284, 289, 307,
313-315; see Origin
Aurignacian race, see Combe-Capelle man
Aurochs, see Bos primigenius and Cattle
Australian head type, 136, 228, 232, 234
Awl, see Poinqon
Axe, 493, 494
Azilian, see Azilian-Tardenoisian
Azilian-Tardenoisian, 16, 275, 451, 456;
art, 456; burial customs, 475-479; chro-
nology, 275, 456, 459; climate, 463, 468;
fauna, 463, 466, 468-470, 471, 472, 474;
: Authors' names are given in the bibliography and in the reference lists at the end of each chapter.
549
550
INDEX
human fossils, 461, 475-485; industry
(Azilian), 15, 16, 18, 270, 271, 275, 276,
456, 459-465, 466, 470-475, (Tardenoi-
sian) 16, 18, 270, 271, 450, 456, 465-468,
470-472, (painted pebbles) 394,456,461,
463-465; stations, 459, 463, 466, 467,
472-475; see Origin
B
Badegoule, 279, 331, 336, 435
Badger, 165, 201, 343, 367, 447, 498; see
Meles taxus
Ballahohle, 279, 331, 336
Baltic race, 458, 486, 500; see Maglemose
Balverhohle, 471
Baousse Rousse, see Grimaldi, Grottes de
Baousso da Torre, see Grimaldi, Grottes de
Barma Grande, see Grimaldi, Grottes de
Baton de commandement, 271, 311, 312, 345,
358, 359, 388, 391, 432, 443-445, 449
Baumannshohle, 160, 195, 245, 247, 248,
439
Bear, 43, 44, 62, 95, 96, 165, 213, 245, 264,
287, 288, 333, 343, 348, 367, 378, 430, 441,
447, 461, 468, 498; see Cave-bear and
Ursus
Beaver, 63, 95, 134, 165, 182, 288, 348, 367,
447,461,468, 498, see Castor; giant, in,
155, see Trogontherium
Bernifal, 321, 395, 396, 435
Billancourt, 109, 149, 152
Bison, Wisent, 13, 43, 44, 69, 71, 95, 98, 106,
125, 147, 165, 192, 194, 196, 202, 206, 211,
223, 287, 288, 317, 321, 333, 348, 353, 356,
364, 368, 372, 385, 403, 405, 406, 410, 414,
420, 421, 423-428, 430, 431, 449, 466, 469,
496, 498, 505, 506, Pis. VII and VIII; see
Bison
Bison, antiquus, 69; prisons, 71, 95, 148, 368,
see Bison
Blade, see Couteau and Lame
Bleville, 167
Boar, wild, 2, 3, 43, 44, 76, 95, 264, 265, 421,
426, 447, 461, 466, 468, 498; see Sus
Bockstein, 285, 314, 435, 442
Bois Colombes, 109, 149, 152
Borer, drill, see Per coir
Bos, 71, 369, 405; longifrons, 498; primi-
genius, 71, 94, 222, 368, 413, 468, 469,
498; taurus, 447, 498; see Cattle
Bossuet, on the prehistory of man, 503, 504
Brachycephaly, 7, 8, 78, 183, 457, 458, 478-
485
Brain, anthropoid, 51, 52, 56, 59; Briinn,
334, 490; Combe-Capelle, 236, 302, 490;
Cro-Magnon, 272, 292, 294, 299, 490;
evolution of, 8, 9, 56-60; Grimaldi, 269,
490; Modern, 56-59, 83, 84, 140, 235,
303, 490; Neanderthal, 9, 58, 59, 235-
237, 490; Ofnet, 480, 490; Piltdown, 58,
59, i39_I4i, 236, 490; Pithecanthropus
9, 58, 59, 83, 84, 490
Brassempouy, 14, 279, 314, 322, 331, 347,
355, 393, 395, 433~435, 438
Brive, 307, 314
Bronze Age, 12, 18, 21, 202, 267, 460, 461,
. 476
Bruniquel, 279, 348, 388, 427, 435, 436
Briinn, 279, 315, 322, 331, 334~337, 395, PL
II; race, 23, 257, 276, 278, 302, 331, 333,
334-338, 480, 489-491, 500; see Briix,
Galley Hill, Pfedmost, Human fossils,
and Origin
Briix, 334; see Briinn race
Buchenloch, 245, 314, 435
Buffon, G. L. L., 3
Biihl, see Postglacial Stage
Burial customs, 24, 215, 221-223, 27°, 271,
302, 303-305, 337, 376-380, 475-479
Burin, graver, 270, 306-308, 310, 386, 389,
470
Cabeco da Arruda, 467, 471, 474
Camargo, 279, 294, 314, 331, 435
Campignian, 493"495
Campigny, 471; see Campignian
Camps, open, 29, 30, 176, 283, 284, 314,
334, 337, 341-343, 442, 448
Canary Islands, 453, 454, 506-510
Canis, lagopus, 193, 206, see Fox, arctic;
neschersensis, 333; suessi, 147; see Dog,
Jackal, and Wolf
Cannibalism, 184, 477
Cannstatt, 10, 105, 218, 220, 331
Cap-Blanc, 317, 395, 428, 431, 435
Capreolus, 70, 147, 367, 469; see Deer,
roe-
Capri, 167, 168
Caramanico, 167
Castillo, 33, 150, 162-165, 167, 245, 246,
279, 3X4, 319, 320, 324, 325, 331, 342, 349,
395, 402, 408, 435, 436, 459, 460, 471
Castor, 69; fiber, 147, 183, 470; see Beaver
Cattle, wild (Aurochs, Urochs, urus), 43, 44,
62, 66, 76, 95, 98, 106, 119, 125, 148, 165,
182, 192, 206, 211, 214, 245, 265, 284, 288,
325, 333, 348, 356, 368, 372, 392, 405, 413,
461, 466, 468, 469, 497, 498, 505, 506; see
Bos and Leptobos
INDEX
551
Cave-bear, 10, n, 13, 182, 194, 197, 201,
202, 206, 210, 211, 212, 213, 218, 287, 401,
413; see Ursus spelceus
Cave-hyaena, 11, 212, 218, 265, 287, 288;
see Hycena crocuta spclcea
Cave-leopard, 206, 287; see Felis pardus
spelcea
Cave-lion, 201, 206, 265, 287; see Felis leo
spelcBa
Caverns, 24; formation of, 30-33, 212; life
in, 2, 30, 32, 211-213, 457
Cavillon, Grotte de, see Grimaldi, Grottes
de
Cazelle, 435
Cephalic index, 8, 480, 490
Ceppagna, 167
Cergy, 109, 149, 152
Cervus,camutomm, ji',dama,4g8;dicranius,
71; elaphus, 70, 94, 147, 367, 392, 426,
461, 469; maral, 367, 447; sedgwicki, 69,
71; see Deer and Stag
Chaflaud, Grotte du, 396, 404, 435, 438
Chaleux, Trou de, 435
Chamois, Rupicapra, 44, 46, 201, 264, 265,
357, 365, 366, 369, 37i, 466
Champs, 435, 436
Champs Blancs, 331, 348, 435
Chancelade, 279, 376-378, 382, 435
Chapelle-aux-Saints, La, 7, 9, 203, 214, 222-
224, 226-232, 235-238, 241-243, 245, 246
Chatelperron, 305, 307, 314; see Points
Chellean, 14-16, 18; chronology, 33, 34,
113-115, 120; climate, 117, 118; fauna,
144-148; geography (physical), 115, 116,
I54-I575 industry, 12, 14, 16, 18, 41, 108,
114, 148-154, 270, 280, 362; stations, 149,
152, 154-158; see Origin
Chelles, 16, 109, m, 116, 149, 152, 154,
167, 244
Chimpanzee, 3, 8, 49, 52-56, 58, 59, 78, 140,
227, 231, 235, 490, 511, 512
Chipping, see Flint
Chisel, see Ciseau
Chronology, 10, 12-14, I0\ 18-24, 41, 510;
tables, 18, 21, 22, 23, 33, 41, 43, 54, 108,
280, 362, 395, 491; means of estimating,
19, 20, 22-24, 317-320
Ciseau, chisel, 270, 271, 388, 392, 444
Climate, effect on fauna, 46, 47, 192, 194,
205, 284-287; effect on man, 33, 297, 332,
372, 382; glacial, 20, 29, 34, 37-43, 64-66,
89, 104, 105, 114, 117, 188-194, 202, 205,
281, 285; interglacial, 20, 29, 30, 33, 34,
37-41, 43, 67, 90, 91, 95, 103, 112, 117,
118, 186-188; Pliocene, 63; Postglacial,
23, 41, 43, 276, 281-284, 361-363
Clothing, 2, 178, 186, 213, 388, 392, 496
Cogul, 394, 497
Colombes, 109, 149, 152
Combarelles, 319, 395~397, 399~40i, 435
Combe-a-Roland, 331
Combe- Capelle, 167, 192, 196, 197, 199, 211,
245, 248, 249, 252, 253, 255, 279, 314;
man {Homo aurignacensis) , 302, 303, 338
Combo-Negro, 435, 436
Compresseur, 271; see Anvils
Continental outline, 19, 34-37, 64, 65, 71,
86, 92, 105, 115, 116, 155, 156, 166, i89,(
190, 281, 282, 288, 362
Cotte de St. Brelade, La, 214, 225, 245
Cottes, Les, 213, 314
Coup de poing, 113, 114, 121, 129, 130, 152-
154, 169-173, 177-180, 222, 251-254, 256,
270
Couteau (knife, blade), 130, 172, 177, 180,
270, 306, 308, 310, 386, 389, 488, 494
Crayford, 198, 245
Creteil, 109, 149, 152
Cricetus phceus, 373, 374; see Hamster
Cro-Magnon, 279, 291, 314, 331, 437, PL
II; man, 7, 273, 279, 291-294, 300, 301;
race, 7, 23, 54, 240, 257, 258, 260, 261,
263, 265-276, 278, 280-282, 284, 289-
305, 336, 35i, 358, 376-382, 434, 44o,
443, 449-454, 457-459, 489-492, 499, 5oo,
506-510, PL VII
Cromer, Forest Bed of, 64, 67, 68, 71
Crosle Biscot, 435
Crouzade, 331, 341, 435, 437
Culture, see Industry
Cyon alpinus fossilis, 201
Dart-thrower, see Propulseur
Daun, see Postglacial Stage
Deer, 44, 125, 134, 245, 265, 356, 426, see
Cervus; Axis, 62, 71, 76, 102; fallow, 265,
469, 497, see Cervus dama; giant, 43, 94,
96, 165, 187, 206, 211, 213, 288, 335,
see Mcgaceros; polycladine, 63, 102, see
Cervus dicranius and sedgwicki; red, 44,
287, 426, 447, see Cervus elaphus and
Stag; roe-, 44, 94, 95, 165, 264, 265, 287,
404, 447, 466, 468, 488, 498, see Capre-
olus; rusa, 76
Dicerorhinus (R.), antiquitatis, 46, 106, 285,
see Rhinoceros, woolly; etruscus, 41, 63,
69, see Rhinoceros, Etruscan; merckii,
41, 92-94, 117, 148, 263, see Rhinoceros,
Merck's
Dog, domestic, 474, 486, 488, 497, 499
552
INDEX
Dolichocephaly, 7, 8, 78, 220, 230, 231, 266,
268, 334, 336, 338, 457, 478-481
Domestic Animals, 447, 466, 474, 486, 488,
497-499
Drill, see Ferqoir
Dryopithecus, 6, 49, 50, 511
Durnten, 20, 117, 119
Durntenian, 107, 119
Duruthy, see Sorde
E
Ehringsdorf, 167, 181, 214
Elasmothere, E. sibiricum, 46, 286, 373
Elephant, 38, 43, 44, 47, 72, 76, 86, 91-95,
102, 117, 119, 123, 124, 147, 148, 155, 157,
161, 174, 177, 186, 187, 192, 205, 245, 264;
see Elephas
Elephas, antiquus, 27, 41, 47, 72, 76, 92-94,
96, 117, 123, 125, 148, 165, 263; hysudri-
cus, 76; meridionalis , 26, 27, 41, 62, 69, 72,
92, 125; planifrons, 62; primigenius, 26,
46, 106, 285; trogontherii, 41, 93, 102, 117;
see Elephant and Mammoth
Elevation, see Continental outline
Enfants, Grotte des, see Grimaldi, Grottes
de, and Grimaldi race
Engis, 435, 453
Engraving, 317, 319-324, 326, 348, 349, 353,
355, 356, 358, 392-407
Eoanthropus dawsoni, 138, see Piltdown
Eolith, n, 68, 84-86, 135
Eolithic, Era, 17, 18; industry, 17
Equus, caballus celticus, 367-369, 400, 408,
412, 419, 431, 432, 498; przewalski, 194,
367, 373, 408, 410, 419; stcnonis, 27, 62,
63, 69, 72; see Horse
Erect attitude, 4, 57-60, 73, 74, 82, 241-244
Ermine, Mustela erminia, 46, 207, 370, 447,
469
Etruscan rhinoceros, see Rhinoceros
Eyzies, Les, 13, 249, 279, 331, 378, 388, 394,
435
F
Fate, Grotte delle, 245, 247
Fauna, 19-21, 38-47, 61-64, 66, 69, 108;
Achculean, 117, 147, 148, 165, 177, 182;
African-Asiatic, 43, 44, 47, 62, 63, 71, 72,
86, 91-94, 205, 206, 287; alpine, 44, 46,
206, 287; Aurignacian, 284-289; Azilian-
Tardenoisian, 466, 468-470, 472; Chel-
lean, 117, 125, 144-148; forest, 44, 71,
206, 287; glacial, 105, 106, 117, 190-194,
196, 197, 205-214, 265; interglacial, 69-
72, 91-98, 101-103, 108-112, 117, 119,
123-125, 186-188, 265; Magdalenian,
364-376, 385, 397-434, 449, 466, 469;
meadow, 44, 71, 206, 287; Mousterian,
117, 186-188, 190-194, 196, 197, 199-
214, 218, 221-223, 225, 263, 264; Plio-
cene, 54, 61-64, 144; Postglacial, 281,
364, 468, 469, 498, 499; Pre-Chellean,
108-112, 117, 125; Siwalik, 76; Solu-
trean, 332, 333, 343, 348; steppe, 44, 46,
194, 206, 281, 287, 362-366, 373-376,
449, 450; tundra, 44, 46, 190-194, 206-
211, 281, 285, 287, 348, 361, 362-366,
370-373; migrations of, 19, 34-37, 62-
64, 71, 72, 202, 205-210, 287; represented
in Palaeolithic art (list), 366; see Climate,
for effect of, and Faunal lists
Faunal lists, 95, 125, 147, 206, 207, 287,
366
Faune chaude, 39, 91, 192; see Mousterian
fauna
Faune froide, see Mousterian fauna
Faustkeil, see Coup de poing
Fees, Grotte des, 279, 435
Felis, leo, 72, 92, 469; leo antiqua, 147; leo
spelcsa, 47, 188; manul, 447; pardus
spelcea, 201; see Cave-leopard, Cave-
lion, Leopard, Lion, and Wildcat
Femur (thigh-bone), 73, 74, 77,80, 237-241,
266, 298, 376, 380
Fere-en-Tardenois, 16, 465, 471
Ferrassie, La, 7, 214, 216, 219, 224, 232, 237,
245, 246, 269
Fire, use of, 2, 165, 212, 213
First Glacial Stage, see Glacial Epoch
First Interglacial Stage, see Glacial Epoch
Fishing, 355, 385, 390, 450, 465, 471
Flake, see Levallois
Flaking, see Flint
Flint, chipping, 170; cleavage, 171; flaking,
169
Floors, Mousterian, 198, 199
Flora, 20; Acheulean, 117, 118, 174, 175;
Chellean, 117, 118; glacial, 65, 108, 117-
119, 191, 192, 202, 208; interglacial, 20,
67, 90, 91, 117-119; Mousterian, 199;
Pliocene, 61, 63; Postglacial, 361, 372,
375, 463, 488; Pre-Chellean, 117, 118;
Pre-Neolithic, 488
Font-de-Gaume, 283, 314, 318, 319, 321,
325, 33i, 349, 356, 358, 365, 372, 395-
397, 399, 406-409, 412, 414-424, 435,
449
Font Robert, 277, 311, 314, 331, 340, 344
Forcsti;ui, Upper, 362; Lower, 282
Forests, see Flora
INDEX
553
Foro, 167
Fourth Glacial Stage, see Glacial Epoch
Fox, 43, 63, 71, 206, 265, 287, 333, 343, 348,
366, 447, 498, see Vulpes.; arctic, 44, 46,
193, 207, 287, 289, 348, 370, 447, 468,
469, see Canis lagopus.
Freudenthal, 279, 435 .
Frileuse, 167
Frontal, Trou de, 435
Fuente del Frances, 435
Furfooz, 7, 279, 481-483, PL Horace, 278,
458, 480, 482-485, 489, 491, 492, 500; see
Grenelle, Ofnet, and Origin
Furninha, 167, 168
Galley Hill, 28, 302, 337, 338; see Briinn
race
Gansersfelsen, 435
Garenne, 435, 440
Gargano, 167
Gargas, 31, 307, 314, 317, 325, 327, 349, 394,
395
Germolles, 307, 314
Gibbon, 49-54, 58,61,63,77, 511; seeHylob-
ates
Gibraltar skull, 7, 9, 140, 214, 215, 216, 219,
226, 228, 232, 233, 236
Glacial Epoch, 18-23, 33, 40, 41, 43, 54;
chronology, 18-23, 4°, 41, IQ8, 188, 280,
362; see Climate, Continental outline,
Fauna, Glaciers; First Glacial Stage
(Giinz), 23, 25, 26, 37, 38, 41, 43, 64-66;
Second Glacial Stage (Mindel), 23, 25,
26, 33, 37, 38, 41, 43, 65, 86-90; Third
Glacial Stage (Riss), 23, 25, 26, 33, 37-
39, 41, 43, 94, 104-106, 115; Fourth
Glacial Stage (Wiirm), 18, 22, 23, 25, 26,
30, 32, 33, 36-38, 41, 43, 107, 108, 117,
160, 188-195, 205, 206, 280, 281, 284, 285,
362, Lanfenschwankung, 41, 108, 280, 362;
First Interglacial Stage (Gunz-Mindel or
Norfolkian), 23, 26, 29, 33-35, 38, 41, 43,
66-72, 84, 95, 115; Second Interglacial
Stage (Mindel-Riss), 23, 25, 29, 33, 38,
40, 41, 43, 69, 90-95, 109-111, 114, 115;
Third Interglacial Stage (Riss-Wlirm),
23, 25, 29, 33, 34, 36, 38-41, 43, 69, 94,
107, 108, 112, 113, 115-119, 186-188, 280,
362; Postglacial Stage, 18-23, 29, 32, 33,
36, 41, 43, 108, 280-284, 362, 468, 510,
Buhl, 23, 25, 26, 41, 108, 276, 280, 281,
361, 362, 370, 372, 446, 447, 449, Gschnitz,
23, 41, 108, 276, 280, 281, 362, 363,372,
449, 450, Daun, 23, 41, 108, 276, 280, 281,
362, 363, Achenschwankung, 25, 26, 281,
282, 284
Glaciers, 64-66, 89, 90, 94, 104-106, 118,
189, 190, 361-363
Glutton, see Gulo luscus and Wolverene
Gobelsburg, 435, 448
Goccianello, 167, 168
Gorge d'Enfer, 331, 435
Gorilla, 49, 52, 54-56, 511, 512
Goulaine, 435, 438
Gourdan, 214, 279, 331, 341, 369, 388, 392,
435, 438
Goyet, 435
Grattoir, 129, 130, 177, 254, 270, 306-310,
386, 390, 470, 473, 494; carene, 308, 309,
463
Graver, see Burin
Gravette, etching tool, 270
Gravette, La, 277, 311, 314
Gray's Thurrock, 28, 109, 116, 128, 149,
152, 156, 157
Greek conception of nature and of the pre-
history of man, 1-3
Grenelle, 279, 481, 482, 484; race, see
Furfooz
Greze, La, 314, 317, 327, 331, 395, 396
Grimaldi, Grottes de (Baousse Rousse), 245,
247, 262-265, 279, 294, 295, 312-314, 321,
323, 380; Baousso da Torre, 263, 294;
Barma Grande, 263, 294; Cavillon,
Grotte de, 263, 294; Enfants, Grotte
des, 263-265, 292, 294-297, see Grimaldi
race; Prince, Grotte du, 262, 263
Grimaldi race, 7, 19, 245, 260, 262-269,
278, 279, 294, 301, 314, 490-492
Gschnitz, see Postglacial Stage
Guanches, 453-455, 5°7-510
Gudenushohle, 245, 248, 279, 307, 314, 435,
448
Gulo luscus, 469; borealis, 193; see Wol-
verene
Giinz, see Glacial Epoch
Hachette (tranchette, chopper, cleaver), 270,
488, 494
Hammer-stone, see Percuteur
Hamster, 46, 63, 147, 165, 287, 362, 364,
374
Hand-axe, see Coup de poing
Hand-stone, see Coup de poing
Hare, 289, 333, 368, 447, 468, 498, see
Lepus (timidus); arctic, 46, 207, 287,
348, 370, 447, 468, 469, see Lepus vari-
abilis; tailless, see Lagomys and Pika
554
INDEX
Harpoons, 355, 383-385, 387, 388, 390, 391,
440, 443-445, 449, 450, 456, 460-462, 465,
466, 470, 474, 486, 487
Hastings, 471, 475
Heidelberg man, Mauer, 7, 23, 24, 40, 41,
53, 54, 90, 95-iQi, 114, 138, 143, 144, 214,
228, 229, 489, 491, 492, PL II
Heidelberg race, see Heidelberg man and
Origin
Helin, 109, 116, 127, 128, 149, 152, 166, 167
Helvetian, see Durntenian
Hermida, La, 435
Hippopotamus, H. major, 38, 39, 41, 43, 44,
47, 69, 71, 86, 91, 92-94, 102, 117, 123-
125, 134, 147, 148, 155, 157, 165, 174, 177,
186, 192, 199, 263, 264
Hohlefels bei Hutten, 435, 442
Hohlefels bei Schelklingen, 435, 442
Hohlestein, 314, 435
Hommes, Grotte des, 279, 435
Homo, aurignacensis , see Combe-Capelle
man; heidelbergensis, see Heidelberg man;
mousteriensis, see Neanderthal race;
neanderthalensis , see Neanderthal race;
sapiens, 7, 9, 10, 54, 230-234, 257, 260,
261, 278, 334, 484, 490, 491, 500
Horace, on the prehistory of man, 3, 504
Hornos de la Pefia, 245-247, 314, 331, 395,
435, 436
Horse,. 45, 165, 182, 192, 225, 284, 355, 385,
392, 404, 405, 407, 408, 410, 412-414, 431,
432, 469, 498; Desert, Plateau or Celtic,
see Equus caballus celticus; Forest or Nor-
dic, 95, 147, 288, 289, 367, 369, 400, 498;
Hipparion, 63; kiang or wild ass, 194,
285-287, 366, 367, 372-374, 400, 447;
Solutre, 288, 289, 414; Steno's, 34, 96,
no, in, 125, see Equus stenonis ; Steppe,
see Equus przewalski
Hoteaux, Les, 279, 378, 379, 435
Hoxne, 158
Human figures, 317, 321-323, 328, 329, 337,
357, 393, 395, 399, 433, 434, 497
Human fossils, 4, n; distribution of, 214,
279; tables of, 7, 219, 294, 336, 378, 490;
see Lists
Human races, see Lists and Origin
Hunting, 2, n, 166, 202, 211-214, 283, 372,
456, 47i, 496, 497
Hyaena, 43, 62, 76, no, 147, 148, 155, 165,
188,214, 245,265,317,356, 476; see Cave-
hyaena and Hycena
Hycena, brevirostris, 125; crocuta, 102, 147;
crocuta spelcea, 47, 102, 188; striata, 92,
102; see Hyaena
Hylobates, 6; see Gibbon
Ibex, Ibex priscus, 44, 46, 201, 206, 264, 265,
287, 289, 321, 348, 357, 369, 37i, 39i, 401,
405, 433, 447, 466, 469, 497
Ice Age, see Glacial Epoch
Ice-fields, 19, 22; see Glaciers
Implements, 11, 27-30, 130, 270, 271; art,
270, 329, 330; see Eolith, Flint, Industry,
Lists, Neolith, Palaeolith
Industry, 4,11,1 2-14, 19, 33, see Acheulean,
Aurignacian, Azilian-Tardenoisian, Chel-
lean, Campignian, Magdalenian, Mous-
terian, Neolithic, Pre-Chellean, Solu-
trean; see Lists and Implements
Interglacial Stages, see Glacial Epoch
Iron Age, 12, 18, 21, 202, 267
Irpfelhohle, 245, 248
Istein, 469, 471-473
Isturitz, 347, 395
J
Jackal, 43, 44; see Canis neschersensis
Javelin point, see Sagaie
Jerboa, 46, 194, 287, 364; see Alactaga ja-
culus
K
Karlich, 314
Kartstein, 245, 248, 314, 435
Kastlhang, 370, 435, 442
Kent's Hole, 10, 152, 244, 245, 435, 440
Kesslerloch, 279, 286, 355, 361, 364, 378,
383, 435, 436, 44i, 442, 444-446, 449
Kiang, wild ass, see Horse
Kleinkems, 471
Knife, blade, see Couteau and Lame
Knight, Charles R., see Restorations
Kostelik, 435, 448
Krapina, 7, 162, 167, 181-185, 214, 219, 220,
228, 229, 256
Krems, 119, 248, 289, 307, 314, 435, 448
Lacave, 279, 331, 340, 345, 347, 391 ^
Lagomys, 63; pusillus, 202, 370, see Pika
Lagopus, see Ptarmigan
Lamarck, on man, 4
Lame, blade, 271
Lampe, lamp, 270, 401, 402
Laufenschwankung, see Glacial Epoch
Laugerie Basse, 13, 14, 275, 279, 331, 348,
376-378, 385, 388, 392, 407r434, 435, 47i
Laugerie Haute, 13, 14, 279, 294, 296, 314,
33i, 346, 352, 435
Laussel, 245, 246, 249, 275, 313, 314, 317,
326-329, 331, 352, 395, 435
INDEX
555
Lauterach, 314
Lemming, 46, 191, 193, 194, 202, 207, 281,
287, 333, 348, 361, 364, 37o, 469, 476;
see Myodes
Leopard, 265, 348; see Cave-leopard and
Felis pardus spelcea
Leptobos, 71; elatus, 62; etruscus, 63; see
Cattle
Lepus, 469; cuniculus, 364, see Rabbit;
timidus, 364, see Hare ; variabilis, 206,
see Hare, arctic
Levallois, 167, 179
Levallois flake, 167, 168, 179, 180, 199, 250,
Limeuil, 279, 435
Lion, 43, 86, 94-96, 98, 148, 165, 188, 281,
317, 348, 356, 365, 378, 400, 407, 446, 468,
472, 498; see Cave-lion and Felis leo
Lissoir, polisher, smoother, 270, 271, 380,
388, 392, 456, 463, 466, 470
Lists and Tables, chronology, 18, 21, 22, 23,
33,41,54,108,280, 362; climatic changes,
38, 39, 4i, 43, "7, 191, 192, 275, 281, 284,
361-364; fauna, 21, 41, 43, 54, 62, 95,
125, 147, 206, 207, 287; human fossils, 7,
9, 219, 236, 237, 239, 266, 294, 295, 336,
378, 490; human races, 41, 54, 108, 278,
280, 362, 458, 490, 491, 499, 500; indus-
tries, divisions of, 18, 113, 114, 248, 249,
252, 340, 389, succession of, 12, 13, 14, 16,
17, 18, 33, 41, IQ8, 280, 362; implements,
130, 172, 254, 270, 271, 306, 308, 310
Liveyre, 331, 435
Loam, 5, 24, 27, 28
Loess, 5, 23-25, 29, 30, 36, 38, 46, 97, 103,
112, 115, 117-119, 122-124, 151, 159, 161,
162, 174, 176, 181, 252, 281, 282, 284, 286,
314, 334, 337, 364, 376, 442,448; stations,
see Camps, open
Longueroche, 435, 471
Lorthet, 406, 407, 435, 438, 471
Lourdes, 279, 388, 432, 435, 436, 438, 471
Lower Rodent Layer, see Rodent Layers
Lucretius on the prehistory of man, 1, 2, 503
Lussac, 279, 435
Lutra vulgaris, 147; see Otter
Lynchus lynx, 469; see Lynx
Lynx, 43, 63, 206, 287, 367, 466; see Lyn-
chus lynx
M
Macaque, 54, 61, 63, 69, 76
Macerata, 167
Machcsrodus, 41, 69, 244; see Sabre-tooth
tiger
Madeleine, La, 13, 16, 279, 351, 383-389,
398, 435, 443, 445, 449, 47*
Magdalenian, 14-16, 18, 276, 277, 351-360;
art, 351-357, 365, 366, 393, 395-434; bur-
ial customs, 376-380; chronology, 18, 33,
41, 108, 276, 280, 281, 351, 361-364; cli-
mate, 276, 360-364, 370-376, 443, 447,
449, 45°; fauna, 361-376, 443, 445-447,
449, 450; human fossils, 376-382; indus-
try, 14-16, 270, 271, 275, 276, 351-356,
358, 382-392, 436, 440, 443-450; stations,
351, 434-449; see Origin and Rodent
Layers
Maglemose, 458, 471, 487,488, 501
Magrite, Trou, 314, 331, 344, 435
Mairie, Grotte de la, 317, 395, 400, 405, 412,
413, 435, 442
Malarnaud, 214, 219
Mammoth, 10, 43, 102, 109, 117, 134, 147,
148, 177, 187, 194, 200, 202, 205, 206, 213,
218, 281, 288, 289, 316, 317, 321, 324-326,
333, 337, 348-350, 356, 364, 372, 385, 401,
403, 420, 421, 427, 429, 449, 450, 476, see
Elephas; woolly, 13, 40, 41, 43, 106, 117,
174, 187, 190-192, 196, 205, 207, 208, 210,
218, 221, 285-289, 334, 335, 363, 370, 372,
384, 397, 398, 420, 427, 446, see Elephas
primigenius
Man, ancestry of, 3-7, 49-64, 491, 511
Mantes-la- Ville, 167
Marcilly-sur-Eure, 214
Mare-au-Clercs, La, 167
Marignac, 109, 126, 149, 152
Markkleeberg, 167
Marmot, Arctomys marmotta, 182, 201, 206,
265, 37o
Marsoulas, 314, 319, 321, 328, 373, 394, 395,
396, 399, 403, 405, 4i5, 4i6, 435, 471, 485
Marten, 71^ 165, 201, 265, 367, 380, 447,
498; see Mustela martes
Martinshohle, 435, 471
Mas d'Azil, 15, 16, 279, 319, 357, 375, 380,
385, 388, 391-396, 432, 433, 435, 437, 449,
458-465, 47i, 472, 474
Massat, 437, 471
Mastodon, 62, 70, 134
Maszycka, 435, 436, 449
Mauer, see Heidelberg man
McGregor, J. Howard, see Restorations
Mediterranean race, 261, 278, 457, 458,
479, 480, 485, 489, 491, 492, 499, 500
Megaceros, 45, 68, 70, 106, 147, 182, 196,
287, 367; see Deer, giant
Meles taxus, 147; see Badger
Mentone, 247, 322, 395, 472, 473; see Gri-
maldi, Grottes de
556
INDEX
Merck's Rhinoceros, see Dicerorhinus and
Rhinoceros
Mesaticephaly, 8, 479
Metternich, 284, 314
Micoque, La, 113, 167, 168, 179, 192, 196,
245, 246, 248, 249
Microlith, see Microlithique
Microlithique, microlith, 270, 306, 308, 310,
388, 396, 450, 470-472
Migration, of fauna, see Fauna; of human
races and industries, see Origin
Mindel, see Glacial Epoch
Miskolcz, 245, 248, 331
Mommenheim, 245, 247, 248
Monkeys, 54, 61-63
Montconfort, 279, 331, 435
Montfort, 341, 471
Monthaud, 331, 346
Montieres, 109, 127, 149, 152, 186, 244, 245,
283, 3i4, 33i
Moose, 44, 94, 96, 265, 281, 348, 366, 468,
469, 472, 488, 496-498; see Alces
Moulin de-Laussel, 331
Mousterian, 14-16, 18, 30, 186-188, 248-
250; burial customs, 222, 223, 271;
chronology, 18, 33, 41, 108, 280, 362;
climate, 117, 123, 188-199, 202, 205, 207;
fauna, 117, 190-194, 196, 199-214; flora,
199; human fossils, 218-226; industry,
14-16, 113, 248-256, 270, 271; stations,
194-202, 244-248; see Caverns, life in,
Floors, and Origin
Moustier, Le, 13, 16, 196-199, 214, 245, 246,
251, 253, 255; man, 7, 196, 214, 221-223,
226, 228, frontispiece
Mouthe, La, 17, 246, 279, 314, 317, 320,
• 321, 394, 395, 398, 399, 401
Mugem, 471, 474, 486
Munzingen, 160, 195, 435, 439, 442, 443
Murals, see Painting
Musk-ox, 42-44, 46, 65, 66, 187, 191, 193,
207, 285, 287, 289, 348, 362, 366, 370;
see Ovibos moschatus
Mustela, erminea, see Ermine; martes, 147,
469, see Marten.
Myodes, lemmus, 210; obensis, 206,285,370;
torquatus, 193, 202, 206, 285, 370, 441,
446, 447; see Lemming
Narbonne, 435, 437
Naulette, La, 7, 214, 221, 228
Neanderthal, cave, 31, 214, 216, 217, PI.
1 1 ; burial customs, see Mousterian; man,
5, 7, 9, 56, 181, 216-219, 490; race, fron-
tispiece, 5-7, 9, 23, 40, 41, 54, 136, 182,
191, 196, 211-244, 256, 258, 263, 272,491,
492, anatomical features, 53-56, 183, 184,
203, 219-223, 226-244, 490, chronology,
41, 108, 257, 262, 280, 491, compared
with Cro-Magnon, 297, 298, discoveries,
181-185, 215-226, distribution of, 214,
219; see Origin
Necklace, 302, 304, 376, 378, 437, 472
Needle, see Aiguille
Negroid race, 261, 262, 266-269, 278, 301,
302, 321, 492
Neolith, 11, 496
Neolithic, New Stone Age, 10, 13, 18, 19, 21,
41, 108, 280, 362, 447, 482, 484-486, 488,
493-50I
Neopithecus, 49
Neschers, 245, 435, 438
Niaux, 314, 319, 353, 373, 391, 394, 395, 400,
406, 409-411, 412, 429, 435
Niedernau, 370, 435
Norfolkian, see First Interglacial Stage
and Forest Bed of Cromer
Nutons, Trou des, 435
Oban, 474, 475, 486
Obercassel, man, 7, 279, 353, 378, 380-382,
435, 443
Oberlarg, 435
Ochos, 214, 219, 221, 228, 245, 248
Ofnet, 279, 285, 314, 331, 370, 435, 469, 471,
473, 475-48i; races, 442, 457~46o, 480,
481, 490, 491, 500; see Furfooz race and
Origin
Ojcow, 331, 436, 449
Ondratitz, 331
Orang, 3, 49, 52-54, 56, 77, 5"
Origin, of industries, Acheulean, 261, 492,
Aurignacian, 261, 289, 305-307, 322, 492,
Azilian-Tardenoisian, 457, 470-472, 492,
Chellean, 126, 261, 492, Magdalenian,
35I-353, 3%3j Mousterian, 261, Pre-
Chellean, 126. Solutrean, 330, 331, 340,
353, 492; of human races, Alpine, 458,
484, 485, Briinn, 331, 492, Cro-Magnon,
261, 322, 492, Furfooz, 492, Grimaldi,
262, Heidelberg, 492, Mediterranean, 492,
Neanderthal, 492, Ofnet, 457, 484, 485,
Piltdown, 492, Teutonic, 486
Otter, 63, 71, 76, 165, 201, 287, 468, 498;
see Lutra vulgaris
Ovibos, 376; mnschatus, 193, 445, 447, see
M usk-ox
Ovis argaloides, 369; see Argali sheep
INDEX
551
Painted Pebbles, see Azilian-Tardenoisian
industry
Painting, 305, 316-318, 320, 321, 324, 325,
327, 328, 330, 358, 365, 394-396, 404-406,
408-429, 464, 465, 474, 496, 497
Pair-non-Pair, 279, 307, 314, 317, 320-322,
33i, 336, 394-396
Palaeolith, 11, 24, 84, 85, 109, in, 158, 389
Palaeolithic, Old Stone Age, 13, 16, 18, 19,
21, 28, 33, 41, 108, 160, 280, 362; Lower
Palaeolithic, 14^ 41, 108,' 11,3, 114, 214,
280, 362, 490, 491; Upper Palaeolithic,
14, 41, 108, 214, 275, 276, 278, 280, 362,
395, 396, 490, 491, 500; chronology, 18,
41, 108, 280, 362, 456
Palceopithecus, 49, 511
Parietal Art, see Painting
Pasiega, La, 319, 395, 402-405
Pataud, 245, 246, 331
Paviland, 279, 289, 290, 294, 314, 440
Pech de l'Aze, 214, 219, 245
Percoir, drill, borer, 130, 135, 153, 172, 179,
253, 254, 270, 306, 308, 310, 311, 344,
346, 385, 386, 388, 390, 392, 470, 473,
488
Percuteur, hammer-stone, 130, 254, 270,
3°6
Pescara, 167
Petit Puymoyen, 214, 245, 246
Pic, pick, 494
Pierre de jet, throwing stone, 130, 172, 213,
. 254, 270, 306
Pika, 46, 362, 447; see Lagomys (pusillus)
Piltdown, 109, 116, 128, 130-135, 149, 152,
214, PL II; industry, 127, 128, 133-135;
man (Eoanthropus) , 7, 23, 24, 40, 50, 53,
54, 56, 130-145, 214, 489-491; race, see
Piltdown man and Origin
Pindal, 314-316, 325, 349, 394, 395
Pithecanthropus, Trinil race, 7, 23, 24, 40,
53, 54, 86, 491, 511, PL II; anatomical
features, 9, 10, 53, 56, 74, 77-84, 233, 234,
240, 490; discovery, 73-77
Placard, 279, 331, 333, 334, 340, 345~348,
352, 353, 355, 378-380, 383, 385, 389, 435,
436, 438
Planing tool, see Grattoir
Pleistocene, see Glacial Epoch
Pliohylobates , 49, 54
Pliopithecus, 49, 54
Poignard, dagger, poniard, 271, 392, 432
Poincon, awl, 271, 308, 346, 392, 470
Pointe, point, knife, lance head, spear head,
15, 113, 153, 172, i77, i79, 248-255, 270,
306,308,310, 311,473; Chatelperron, 306,
307, 311; pointe a cran, shouldered, 270,
308, 310, 313, 334, 340, 342, 345, 346, 352;
pointe a face plane, 341; pointe de lance,
271, 306; pointe de laurier, laurel leaf, 15,
270, 310-312, 334, 337, 339-341, 344, 345,
347, 348, 352; pointe de sagaie, javelin
point, 271, 308, 340, 346, 354, 355, 361,
364, 37o, 383, 387; 39°, 442, 449, 462, 494;
pointe de saule, willow leaf, 340, 344, 347;
pointe a soie, 270, 310, 311, 313, 340,
345
Polisher, see Lissoir
Portel, Le, 319, 394, 411, 412
Postglacial Stage, see Glacial Epoch
Pottery, 461, 466, 474, 486, 488, 496
Praule, Trou de, 435
Pre-Chellean, 16, 18, 36, 41; chronology,
18, 33, 40, 41, 90, 107-115, 280, 362;
climate, 108, 112, 114, 117, 118, 123;
fauna, 108-112, 117, 124, 125; industry,
40. 114, 120-130, 270; stations, 109, 116,
122-128, 149, 150-152, 158, see Conti-
nental outline and Origin
Pfedmost, 257, 279, 331, 341, 345, 348, 349,
366, 395, 427; see Briinn race; mam-
moth hunters, 279, 337
Primates, 3-10, 40, 49-64, 73-84, 86, 140,
141, 217, 219, 227, 231, 233-235, 237-240,
490, 491
Prince, Grotte du, see Grimaldi, Grottes de
Pro pliopithecus, 49, 54
Propstfels, 372, 435, 442, 469
Propulseur, spear thrower, dart thrower,
271, 355, 39i, 432, 433, 436, 445, 449
Ptarmigan, Lagopus, 44, 206, 207, 287, 289,
37o, 37i, 375, 469
Quartz, 166
Quartzite, 163, 164, 265
Quina, La, 9, 113, 211, 213, 214, 245, 246.
248, 253-256; man, 7, 9, 214, 216, 217,
219, 221, 225, 236, 237, 248
Rabbit, 265, 343, 368, 468; see Lepus
cuniculus
Racloir, scraper, 113, 114, 130, 135, 172, 178,
209, 248, 250, 251, 253-255, 270, 306, 387,
388, 470, 472, 473, 488
Rangifer tarandus, 193, 209, 210, 285; see
Reindeer
Rauberhohle, 245, 247, 248, 314
558
INDEX
Raymonden, 340, 376, 388, 435
Reilhac, 331, 471
Reindeer, 13, 41, 43, 44, 46, 102, 103, 187,
191-194, 196, 197, 202, 205, 206, 209,
210-212, 214, 221, 223, 225, 284, 285,
286-289, 314, 317, 332, 333, 365, 366,
37o, 372, 385, 392, 399, 405, 407, 411-
413, 415, 419-421, 429, 433, 440, 441,
445, 447, 461, 462, 468, 469, 47i, 474,
481, 498; see Rangifer
Reindeer Epoch, Period, 13, 14, 102, 192,
275, 286, 363, 375, 392, 438, 456, 459
Religion, 272, 358-360, 463, 465, 501
Remouchamp, 471, 474
Ressaulier, 435, 436
Restorations, Knight, Charles R., frontis-
piece, 358; McGregor, J. Howard, 9,
79-82, 87, 137, 140, 142, 143, 145, 203,
242, 243, 273, 293, 300, 301; Rutot-
Mascre, 73, 101, 484, 495
Retouch, 169-172, 248, 269, 306, 308, 3IOj
33i, 332, 338, 339, 358, 389
Key, 331
Rhens, 284, 314
Rhinoceros, 38, 39, 43, 44, 62, 76, 123, 221,
245, 289, 337, 356, 365, see Dicer or hinus ;
Etruscan, 34, 95-97, 101, 109, 110-112,
117, 125, 134, 144, see D. etruscus;
Merck's (broad-nosed), 27, 43, 47, 93,
94, 97, 102, 109, 119, 124, 125, 134, 147,
148, 151, 155, 157, 161, 164, 165, 177,
182, 186, 187, 192, 205, 263-265, see D.
merckii; woolly, n, 13, 40, 41, 117, 148,
174, 187, 190, 191, 196, 199, 205, 206,
208-210, 213, 218, 223, 225, 281, 285-288,
314, 319, 324-326, 348, 363, 366, 372,
400, 409, see D. antiqidtatis
Riss, see Glacial Epoch
River-drifts, 5, n, 12, 23; formation, 24-
27, 90, 119, 154-157, 186; stations, 114-
116, 1 19-124, 154-156; terraces, 20, 23,
24-28, 34, 85, 90, 104, 154-157, 162
Robenhausen, 471, 495
Roccamorice, 167
Roche au Loup, 307, 314
Rochette, La, 245, 246
Rock Shelters, 32, 33
Rodent Layers, 447; Lower, 206, 207,
211, 281, 314; Upper, 281, 361, 363,
446
Romanelli, 306, 314
Riiderbach, 167
Riidersheim, 167
Rupicapra, see Chamois
Ruth, Le, 314, 331, 435
Rutot-Mascre, see Restorations
Sablon, 162, 167
Sabre-tooth tiger, 34, 43, 62, 69, 70, 72, 94,
102, 110-112, 117, 125, 144, 147; see
Machcerodus
Sagaie, javelin point, see Pointe de sagaie
Saiga antelope, 44, 46, 194, 287, 289, 333,
357, 362, 366, 373, 374, 376, 449
Saiga tartarica, see Saiga antelope
Salitre, 435
Saint Acheul, 5, 14, 16, 109, 116, 1 19-124,
127-129, 149-152, 155, 162, 163, 166, 167,
170, 244, 245, 249, 283, 314, 331, 435, 440
Saint Lizier, 435
Saint Martin d'Excideuil, 331
Saint Prest, 17, 67-69
San Isidro, 109, 126, 149, 152, 167, 245, 246
Sciurus vulgaris, 367; see Squirrel
Schmiechcnfels, 372, 435, 469
Schussenquelle, 372, 435, 442
Schussenried, 435, 441; see Schussenquelle
Schweizersbild, 286, 361, 364, 370, 435, 441,
442, 444-447, 449, 460
Scraper, see Racloir
Sculpture, 317, 320-323, 328, 329, 347~349,
356-358, 392, 393, 395, 396, 427-434
Second Glacial Stage, see Glacial Epoch
Second Interglacial Stage, see Glacial Epoch
Seven Oaks, 471, 475
Shelters, abris, see Rock Shelters
Sipka, 214, 219, 221, 228, 245, 247, 248, 435,
449
Sireuil, 314, 322, 395
Sirgenstein, 201, 202, 245, 248, 285, 314,
33i, 37o, 372, 435, 44i, 460
Sivapithecus , 511
Siwalik, see Fauna
Solutre, 16, 279, 283, 286, 288, 294, 314, 330,
33i, 341-345, 373, 435, 436, 438
Solutrean, 14-16, 18, 41, 270, 271, 276, 278,
280; art, 347-350, 357; burial customs,
332; chronology, 18, 33, 41, 108, 280, 362;
climate, 41, 108, 276, 280, 281, 332, 333;
fauna, 332-334, 343, 348, 366; human
fossils, 279, 334-337; industry, 275-278,
330-332, 334, 338-348, 351, 352, 354, 358;
stations, 326-328, 331, 337, 340-348, see
Origin
Somme River, 12, no, 112, 114-117, 119,
i2o, 122-125, 127, 162, 252, 276
Sorde, 279, 378, 435, 438
Souzy, 435
Spermophilus rnfescens, 194, 373; see Sus-
lik
Spear-point, see Pointe
INDEX
559
Speech, power of, 4, 58, 60, 139, 140
Spiennes, 127, 128, 495
Spy, 162, 214, 244, 245, 311, 314, 331; man,
7, 181, 214, 218-220, 226, 228, 229, 231-
233, 235-237, 244, 256, 257, 490
Squirrel, 447, 498; see Sciurus vulgaris
Stag, 43, 44, 95, 106, 119, 187, 201, 202, 264,
265, 288, 333, 364, 367, 370, 372, 405, 426,
429, 456, 461, 463, 468, 469, 481, 488, 497,
498; see Cervus elaphus and Deer, red
Stegodon, 76, 134
Strassberg, 435
Stratification of Castillo, 164; Enfants,
Grotte des, 265; Heidelberg, 97; Made-
leine, La, 385; Mas d'Azil, 461; Ofnet,
476; Piltdown, 133; Placard, 333~334;
Saint Acheul, 122, 123, 150; Schweizers-
bild, 447; Slrgenstein, 202
Subsidence, see Continental outline
Sureau, Trou du, 435
Sus, arvernensis, 63; scrofa, 71; scrofa
ferus, 147, 165, 368, 469; scrofa palustris,
499; see Boar
Suslik, 206, 289, 447; see Spermophilus
rufesce is
Tables, see Lists
Tardenoisian, see Azilian-Tardenoisian
Tasmanian compared with Neanderthal,
232, 233; see Neanderthal
Taubach, 119, 167, 214
Tectiforms, 283, 284, 403, 404
Terraces, see River-drifts
Teutonic race, 458, 486, 488, 499-501
Teyjat, 388, 394, 396, 435; see Mairie,
Grotte de la, and Abri Mege
Thiede, 314
Third Glacial Stage, see Glacial Epoch
Third Interglacial Stage, see Glacial Epoch
Throwing stone, see Pierre de jet
Thumb, opposable, 55, 58, 60, 240
Tibia, shin-bone 237-239, 241, 266, 298
Tilloux, 109, 149, 152, 167
Torralba, 109, 126, 149, 152
Tourasse, La, 471, 486
Trilobite, Grotte du, 314, 324, 326, 331, 340,
341, 344, 347, 440
Trinil race, see Pithecanthropus
Trogontherium, 45, 69, 94; see Beaver, giant
Tuc d'Audoubert, 32, 395, 396, 406, 427-
43i, 435
Tundra, see Climate, glacial; see Fauna
Turbarian, Lower, 361; Upper, 363
Upper drift, 191
Upper Rodent Layer, see Rodent Layers
Urochs, Aurochs, see Bos primigenius and
Cattle
Ursus, arctos, 102, 147, 211, 469; arvemen-
sis, 63,94, 102; deningeri, 102; spelV.V. AJt^f
■ 1
mmfflBSffiSI
BBH