Chapter II: The Palaeolithic Age (1)

[Sidenote: Reasons for devoting a chapter to the Palaeolithic Age.]

A chapter devoted to Palaeolithic Man may perhaps appear irrelevant to a work the aim of which is to serve as an introduction to English history; for it has been questioned whether in this country he left any descendants, and therefore whether he exercised even the smallest influence upon the later immigrants. But in France, if not here, the Palaeolithic merged, perhaps by a long period of transition, into the Neolithic Age:[17] the neolithic inhabitants of Britain were of course descended from palaeolithic ancestors; and in every part of the world in which it existed the palaeolithic culture was apparently much the same. There are therefore other reasons besides that of sentiment for attempting in this book to describe the life of primitive men and the surroundings in which they lived: yet sentiment has its weight; for no one who is not heedless of the past would forget the efforts of those who, in hard struggle with nature and with fierce beasts, were the unconscious founders of European civilization. Without the faith of the Shinto ancestor-worshipper one may share his daily repeated pious gratitude,--‘Ye forefathers of the generations, and of our families, and of our kindred, unto you, the founders of our homes, we utter the gladness of our thanks.’[18]

[Sidenote: Tertiary man.]

The palaeolithic people had acquired a degree of skill in the manufacture of stone tools which is only attainable by the most practised modern imitators. But the progress which they made during the incalculably long period of their existence was so small that they must have needed ages to ascend to the level at which we are able to observe them. Therefore, although no skeletons, no implements have yet been found which can be referred, in the opinion of all experts, to the Tertiary Period, the most sceptical are willing to believe that man, even if he did not deserve the appellation of _Homo sapiens_, did then wander upon the face of the earth.[19] But how, when he had assumed the erect position and had begun to make intelligent use of the hands which gave him such an advantage in contending with other carnivorous animals more powerful than himself, he learned slowly and by repeated efforts to chip the flints that he picked up into serviceable shapes; how in the struggle for a livelihood the stronger or the more cunning prevailed; how with developing intelligence came keener susceptibility to pain as well as to pleasure; how men’s fancies were quickened by light and darkness, sun, moon, and stars, and their fears excited by storm and flood and fire; how they strove to communicate to each other their alarms, their desires, and their joys--these things may only be imagined; and the imagination of those who have read most wisely and have most observantly studied the ways of modern savages will lead them least astray.

[Sidenote: The Ice Age.]

The Tertiary was merging into the Quaternary or Pleistocene Period when the climate which had before fostered the palms and crocodiles whose fossils have been discovered in the London Clay,[20] but had been gradually changing, became intensely cold. Snow fell thickly upon the mountains of Scandinavia; glaciers began to creep down the valleys; and gradually the ice accumulated until it overspread the whole of Northern Europe, filled the basins of the Baltic and the North Sea, hid mountains and uplands in Scotland, and choked the dales of Northern England, of the Midlands, and of Wales; while isolated glaciers were formed even so far southward as the valleys of the Beaujolais and the Lyonnais. The ice has left its record upon the Highland and Cumbrian mountains, whose rugged crags it moulded into flowing curves; upon rocks which were scratched by stones embedded in slowly moving glaciers; in the mud, stiff and tenacious, which they deposited as they grided over many kinds of rocks, and which, being interspersed with stones, large and small, is called boulder-clay; in rocks which they transported and dropped far from their native sites, and by which the directions that they followed can still be traced; in moraines which mark the limits of their descent and their recession; in lakes that were formed, after the ice had disappeared, in glens which moraines had dammed;[21] in the Arctic plants which survive on mountains, and in those whose fossil remains have been found in Norfolk near the level of the sea. In many places the boulder-clay lies in two or more layers, separated by stratified sands and gravels, from which it has been generally inferred that the Ice Age was interrupted by a period--here and there by short intervals--during which the climate was mild. Told briefly and in general terms, the tale which a learner might piece together from geological textbooks[22] is something like this. The cold was most intense during the earlier stage, when the lower boulder-clay was being deposited, and, little by little, Britain rose until it became one with the Continent, with Ireland, and with Scandinavia, and extended far westward into the Atlantic Ocean. Then, we are told, the ice-sheet that covered Scandinavia was six thousand feet thick; and though it became thinner as it advanced southward, it shrouded the hill-tops in Scotland, where boulders were lifted right over the water-parting, and dropped on the western side, and scored its marks upon rocks in the Lake District at heights of two thousand five hundred feet; while, spreading over Ireland, it went out to sea beyond Cork and Kerry, where the wall of ice broke off and floated away in bergs. Then the land slowly sank until in the interglacial period only the hills stood out above the sea, and Great Britain became an archipelago. Again the movement was upward, though often interrupted and perhaps not general in extent: the climate was again becoming severe; and, although the rigours of the first period were not repeated, local glaciers crept down the higher valleys north of the Midlands, while icebergs floated over the parts that remained submerged and over the North Sea. Now too, as in the earlier period, the cold was not everywhere continuous: there were oscillations during which the glaciers alternately advanced and retreated. As the Ice Age was beginning to near its end, the land continued to rise until the North Sea, the English Channel, and the Irish Sea once more disappeared. In the latest stage of all, when Arctic conditions were about to vanish even in our northern latitudes, there was a gradual subsidence: Scotland was lowered about one hundred feet beneath the present level of the sea, as the highest ‘raised beach’ along the shores of the great estuaries testifies; and the waters rushed in over the sinking valley of the Dover Strait.

Such was the orthodox faith: but the rising geologists have discarded some of its articles; and even among the faithful there are pious doubters. Many authorities deny that the sea-shells which are found on hills in North Wales, Cheshire, and elsewhere, prove that they were once submerged: those shells, they insist, were ploughed up by glaciers out of the sea-floor; and they require us to believe that they were carried up the sides of the hills to heights of thirteen hundred and fifty feet above the sea-level.[23] But although these shells are probably not in their original position, and the mere presence of marine organisms is no sufficient proof of former submergence, shells have been found near Inverness, five hundred feet above the sea, in the very place where they lived and died. Still, it does not follow that the submergence which they attest was interglacial.[24] Some inquirers believe that the glaciers advanced and retreated once and no more;[25] that there was only one slight elevation of the land and one slight subsidence: others that Britain was not only elevated twice, but also twice partially submerged; others that it was finally severed from the Continent in the earlier part of the Ice Age, when the drainage of Northern Europe, pouring into the North Sea and barred by the ice-sheet from escaping northwards, cut for itself a channel across the isthmus which now lies below the Dover Strait.[26] One expert still insists that when man first entered Britain the whole country stood at least six hundred feet above its present level:[27] another, in the same work, denies that its greatest elevation was more than seventy feet;[28] and their editor looks helplessly on. One writer suggests that there may never have been an Ice Age, in the strictest sense of the term, at all, but only local glaciers, such as now exist in Greenland.[29] Another has laboured to show that the accumulation of ice-sheets ‘merely marked one or more culminating epochs in a period when the climate was at least as commonly temperate as Arctic’.[30] Others even now maintain that not one only, but five interglacial periods interrupted the intense cold;[31] others again that there was no interglacial period at all, but only local ameliorations of climate.[32] Another fertile theme of controversy has been the origin of the boulder-clays. But the confession of a Fellow of the Royal Society, who, as a member of the Geological Survey, lived in Norfolk for eight years, studying its geology, suggests that, after all, a sense of humour may compensate for inability to fathom the mysteries of the Ice Age. ‘After spending about a year in Norfolk,’ he says, ‘I began to believe I knew all about the drifts, but during the following seven years of my sojourn in that county, as I moved from place to place, I somehow seemed to know less and less, and I cannot say what would have been the result, but fortunately the geological survey of the county came to an end.’[33] Fortunately, too, it is not essential to our study of palaeolithic man to decide in every case between the theories of rival geologists. All admit that in Britain the Thames was the extreme southern limit of glacial movement, although even in the southern fringe Arctic conditions prevailed; that glaciers covered a large part of the country north of the Thames, and on the higher regions coalesced into ice-sheets: the view that the lower boulder-clay was a _moraine profonde_ has at last been generally adopted;[34] while almost all agree that there was at least one interglacial period, and that there were climatic variations in certain tracts. Nevertheless one of the ablest and most experienced of our field geologists has recently given weighty reasons for his own conviction that even this solitary age of amelioration should not be regarded as an established fact.[35]

[Sidenote: Continental Britain.]

But, if we are to study the Palaeolithic Age intelligently, we must endeavour to test for ourselves the dogma that Britain was then continental. That dogma has recently been questioned by geologists who have minutely re-examined in the field the phenomena of the Glacial Epoch. Mr. Clement Reid, for instance, holds that in the Palaeolithic Age England never rose more than seventy feet above its present level,[36] and that men first entered it across a narrow strait which was formed in the earlier period of glaciation.[37] It is certain that the sea then washed the coast of Sussex and the western counties; for near Selsea there is a patch of boulder-clay--the only one south of the Thames--which must have been deposited by shore-ice, and there are rocks belonging to Bognor or the Isle of Wight, to the Channel Islands, and to Brittany, which were transported by icebergs and dropped when they melted under the summer sun.[38] Again, before the first English boulder-clay was formed Arctic plants flourished near Cromer; and, says Mr. Reid,[39] ‘as these occur just above the present sea-level, and lie evenly on the strata below without deeply channelling them, the height of the land at the commencement of the Glacial Epoch, in Norfolk at any rate, must have been almost the same as it is now’. The same observer assures us that in Southern Britain the first intense cold was succeeded, after an interval of which geology has nothing to tell, by an interglacial period in which the land sunk about one hundred and forty feet below its present level, so that shingle was deposited on what is now Portsdown Hill;[40] and that it then gradually rose until, long before the second glaciation began, its level, marked by fresh-water and estuarine deposits, once more virtually coincided with the present line.[41] But, he tells us, at some time after the disappearance of the ice which deposited the latest boulder-clay of Norfolk the land stood rather higher than now;[42] and he holds that even in the early part of the Neolithic Age Britain must have been almost connected with the Continent, for many of the river valleys were excavated to depths of from sixty to seventy feet below the present level of the sea.[43] The submerged forests of Devonshire, Cornwall, and the Bristol Channel, which contain traces of neolithic handiwork, flourished at a time when the land stood from fifty to seventy feet above its present elevation.[44]

But there are other facts which demonstrate that at some time after the first period of intense cold--perhaps in that interval of which geology has nothing to tell--the Continent must have included Britain. As we shall presently see, not only the mammoth, the woolly rhinoceros, the glutton, and other Arctic animals, but also many species which prefer a temperate climate, and others which are now tropical, lived in this country side by side with palaeolithic man. Nearly all of them had been represented here before the earliest glaciers of Scotland were formed.[45] But even on the southern side of the Thames the cold was so intense during the earlier part of the Ice Age that none of the tropical, none even of the temperate species could there have lived: since the land was barren, treeless, and frozen,[46] even the mammoth, protected though it was by its woolly coat, could have found little food;[47] and large herds of Arctic animals travelled as far southward as Italy and Spain.[48] It is therefore evident that the beasts of tropical and of temperate climes whose remains have been found in the river-drift and in caves along with palaeolithic implements must have entered Britain after the coldest period had ceased.[49] Moreover, vast quantities of bones of Pleistocene mammals, some of which, such as the reindeer, have never been found in Britain in preglacial deposits, have been dredged up out of the bed of the North Sea, principally from the Dogger Bank;[50] and it is therefore clear that at some time after the climax of the Glacial Period that sea or a large part of it did not exist. It cannot indeed be proved that the men of the river-drift and the caves entered Britain as soon as the other animals;[51] and possibly the Dover Strait may have existed as a narrow channel at the time of their arrival: but since the bones that were raised from the Dogger Bank appear to belong to the time when the Thames was laying down the gravels in which men’s tools have been found,[52] it seems probable that the land bridge was standing in some part of the Palaeolithic Age.

[Sidenote: The relation of palaeolithic man to the Ice Age.]

It has been demonstrated that palaeolithic men were living in East Anglia after glaciers had finally disappeared from that part of the country. The valleys of the Ouse and its tributaries, in the gravels of which their implements are to be found, were worn down through boulder-clay.[53] Excavations at Hoxne in Suffolk have shown that the people who left their tools there lived at a time which was separated by two climatic waves, attested by the flora of two sets of strata, from the age in which the latest boulder-clay of that district had been deposited.[54] Moreover, in many cases in which evidence has been adduced to show that palaeolithic remains are of glacial or interglacial date, doubts have arisen either as to the artificial character of the flints or as to the age of the beds in which they were found.[55] When, for instance, a member of the Geological Survey announced that he had found palaeolithic implements at Brandon in Suffolk in three interglacial beds, separated by layers of boulder-clay,[56] Sir John Evans suggested that the clay was not in its original position, but had slipped down from a higher level.[57] Again, Dr. Henry Hicks and Sir Joseph Prestwich were convinced that the cave of Cae Gwyn in the Vale of Clwyd had been inhabited before the climax of the Ice Age.[58] Here a flint flake was taken out of earth separated by a superincumbent bed of clay from a layer of sand and gravel, above which again rested boulder-clay that, in Hicks’s judgement, showed no sign of having ever been disturbed, and which, in the opinion of Mr. Clement Reid,[59] must have been deposited before the last glaciation of the district. Even this evidence, however, is not unanimously accepted. Flints have also been found in the Cromer Forest Bed at East Runton, which was certainly preglacial; but Sir John Evans cannot see on them the faintest marks of human workmanship.[60]

Nevertheless, it is not improbable that when the hunters whose tools have been exhumed from the drift of South-Eastern Britain were living in a comparatively mild climate, Scotland, the Lake Country, and the highlands of Yorkshire and Wales may still have been partially buried beneath ice.[61] The high-level drift of the Thames valley, which has yielded so many implements, is believed by eminent geologists to have been laid down at a time when ice spread over Northern Britain;[62] and in support of this view it has been contended that in those regions no palaeolithic implements have been found.[63] The argument cannot be easily set aside; but it has been pointed out that in the northern districts, owing to the extreme scarcity of flint, stone tools could only have been made of harder rocks, on which it is not so easy to detect marks of human agency; that the alluvial deposits in those parts are not readily accessible to search; and that, if they are patiently explored, implements may yet be recovered from them.[64] Some years, however, have elapsed since this suggestion was made; and it has not yet been verified. Moreover, the absence from the country north of Yorkshire, save in a few preglacial deposits, of such bones as have been found with palaeolithic remains seems to indicate that the animals contemporary with palaeolithic man were unable to find food in Northern Britain owing to the continuance of an Arctic climate.[65] Man was undoubtedly living in Southern Britain in the cold period that succeeded the so-called interglacial period of Sussex and Hampshire; for the plateau gravels that cap the Bournemouth cliffs, in which his tools have been found, are older than the valley gravels of the Hampshire Avon and the Stour, which were formed towards the end of the Ice Age by torrents that streamed over frozen chalk downs impervious to water and swept away the fragments of their crumbling surface.[66] Furthermore, stone implements have been found at Caddington below, and near London embedded in, a stratum known as ‘contorted drift’, which is believed to have been formed in a period of great cold;[67] and it is merely a question of words whether this period is to be included in the last phase of the Ice Age.[68]

[Sidenote: ‘Eolithic’ man?]

But there is one district from which evidence has been obtained that has convinced many who sought conviction, that there were men in Britain before the first British palaeolithic tool was made. In the village of Ightham, near Sevenoaks, lives a tradesman, named Benjamin Harrison, whose discoveries have caused much searching of heart, if they have not revolutionized our knowledge of the life of early man. In 1885 he began to search for old stone implements on the chalk plateau between the valleys of the Medway and the Darent. There, embedded in patches of gravel that must have been drifted on to the plateau from hills higher still, which had been already worn down by denudation even when palaeolithic hunters were roaming among herds of mammoths in the valley of the Thames, he found flints of divers shapes which seemed to him to bear sure traces of man’s handiwork, and which have been termed ‘eoliths’, or stone implements of a dawning age. Nearly all of them, indeed, were so rude that the chipping on their edges has been ascribed by sceptics to the action of nature. But if even a small fraction of them could be proved to be authentic, the contention of their finder would be established. They recur, again and again, in certain well-defined and peculiar shapes; the chips have in many cases been removed not from the exposed parts but from concave sides which, he would have us believe, natural agents could hardly have affected;[69] if Sir John Evans and other experts are unable to accept them as artificial, Canon Greenwell,[70] Pitt-Rivers,[71] and Prestwich[72] were convinced that they had been wrought by man; even the labourers who picked them out of the gravel hardly ever failed to distinguish them from the surrounding flints;[73] and, if we may believe the champions of their authenticity, those who assert that they were shaped by nature have failed to produce stones of similar forms from the valley-drift.[74] Now when the hunters of the Thames valley were making their tools, Britain had the same main features of hill and dale that it has to-day; but when the gravels were being drifted on to the Kentish plateau, Thames and Medway were yet unborn; and, filling the great valley that now lies between the North Downs and the Lower Greensand hills, some five miles further south, the plateau rose southward to Central Wealden uplands two thousand feet or more above the sea. With no special knowledge of geology the antiquary who spends a holiday in walking from Sevenoaks or Wrotham on to the plateau may satisfy himself that this is true. Mingled with the eoliths in the patches of drift are fragments of chert that must have been washed down from the Lower Greensand at a time when it rose high above the plateau’s level; for south of the eolithic area, inclining upward below the chalk and below the Upper Greensand, the outcrop of the Lower Greensand shows itself still. The plateau drift lies upon rock of preglacial age;[75] and although there is no evidence that it is itself older than the Pleistocene period, some geologists hold that it was deposited soon after, perhaps before, British glaciers began to form.[76]

But assuming that the eoliths are artificial, does it follow that they are older than the oldest palaeoliths, or that they were wrought by a race different from the men of the valleys? Mr. Clement Reid has pointed out that the gravel at Alderbury, some three miles below Salisbury, in which multitudes of eoliths have been found, is on exactly the same level as that of a gravel three miles lower down the valley, where Prestwich picked up a palaeolithic implement which had fallen from a yet higher elevation.[77] If the position of this implement was an index of its age, eoliths were being used in Wiltshire after palaeoliths had begun to be manufactured.[78] On the other hand, it is asserted that eoliths have lately been found in Tertiary deposits on the high plateau above the Avon;[79] and one geologist, who rejects all eoliths, would argue that Benjamin Harrison’s labours have not been vain. Many palaeolithic implements have been found on the Kentish plateau, but never embedded in association with eoliths: most of them are unworn, and look as if they had remained on the very spot where they were lost; and it is easy to see that they are far less ancient than the eoliths. But certain implements have also been found there which, although they were not lying in the gravels, appeared to bear marks of having been derived from them and washed down in the same drift that contains the eoliths. Like the latter they were stained deep brown, covered with glacial scratches, and coated with the white deposit of silica.[80] If this argument had been generally accepted, one might conclude that the greater antiquity of British man does not depend for its proof upon the authenticity of the eoliths. What all admit is that in France flints of eolithic form have been found even in Tertiary beds.[81]

But while the extreme antiquity of many eoliths is certain, the question of their authenticity has recently been debated with renewed and redoubled vigour. About two years ago an eminent French palaeontologist, Monsieur Marcellin Boule, announced that in the process of manufacturing cement at Mantes many flints had been converted into eolithic forms;[82] and it has been contended that the conditions which were actually observed in the factory were analogous to those of the torrential streams by which flints may have been dashed hither and thither as they were swept on to the Kentish plateau in primaeval times.[83] An ardent advocate of the authenticity of eoliths insisted that some of the Kentish types would be looked for in vain among the machine-made specimens from Mantes;[84] but a sceptic affirmed that he had himself found an eolith, manifestly untouched by man, with its notch accurately fitting against another stone, the two having been ground together by a natural process which he described as the slipping, sliding, and foundering of the insoluble surface material from higher to lower levels.[85] Although it was objected that certain rectangular eoliths with blunt edges could not have been produced except by art,[86] it is permissible to doubt whether the human origin of eoliths will ever be established beyond dispute; and he who reflects that they have been met with not only in Tertiary beds but in those immeasurably later deposits which were contemporary with or but little older than palaeolithic man[87] will leave them for the present without regret to the consideration of enthusiasts.

[Sidenote: The environment of palaeolithic man in Britain.]

Let us then try to conceive of the environment of those palaeolithic hunters of whose culture we have clearer indications in a late phase of the Ice Age, when the glaciers of Southern Britain had passed away. Then the configuration of the country was very different from that which we behold. The chalk ranges of Kent and of Picardy were unbroken. The Thames, fed sometimes by torrential rains, flowing rapidly and fitfully in the broad shallow valley which it was excavating, was depositing gravels on the slopes that bordered it, a hundred feet above the level of its existing waters,[88] and wandering far eastward across a plain from whose now sunken surface bones of mammoth and reindeer, of hyena and bear have been dredged, to swell that greater Rhine which found no outlet till it reached a far northern sea. Mammoths, woolly rhinoceroses, and giant elks with antlers ten feet across, roamed in the forests; hippopotamuses swam in the streams;[89] brown bears and grizzly bears and lions and hyenas made their dens in caves, and dragged into their dark and sinuous recesses the prey which they had torn down in the open.

[Sidenote: Whence did he come?]

The earlier palaeolithic immigrants, impelled perhaps by scarcity of game, had crossed the valley of the Dover Strait doubtless from the nearer parts of France or Belgium; but the original home of the race is unknown, for palaeolithic tools have been found not only in this island and almost every European country except Scandinavia, but also in North Africa, in the valley of the Nile,[90] in Palestine and Asia Minor, the Euphrates Valley, Somaliland, India, and North America: as a high authority has remarked, they are ‘so identical in form and character with British specimens that they might have been manufactured by the same hands’;[91] and the same may be said of those which were wrought by the Tasmanians, who, fifty years ago, had not yet been exterminated by the pioneers of Christian civilization.[92]

[Sidenote: Chronological puzzles.]

Many attempts have been made to calculate the number of millenniums that have elapsed since our Palaeolithic Age began and since it came to its end. Croll, the author of the astronomical theory of the Ice Age, finally concluded that that epoch ceased about eighty thousand years ago;[93] and Sir Archibald Geikie laboured in his youth to estimate the time which the rivers would have taken to excavate their valleys from the days when they were depositing the high-level gravels to the era when they reached their present depth.[94] But any one who uses his powers of reflection will see how many elements of uncertainty must stultify such a method as this;[95] and, since the cause of the Ice Age remains unknown, the calculations of Croll were futile.[96] Indeed, if it were possible to prove that eighty thousand years have passed since the beginning or since the end of the Palaeolithic Age, not much would be gained; for whose mind can conceive what such a period means? The wiser archaeologists have given up the quest of chronological precision; and they know that the imagination may be stimulated by more legitimate means. Go to Caversham and stand upon the gravels washed down by the Thames in his lusty youth:[97] one hundred and twenty feet below he is flowing now; think of the ages that passed while his waters were hollowing out that valley, which was as it is still before the Palaeolithic Age had passed away. Walk along the cliff near Bournemouth, and look out over the Solent Sea. That cliff was once a river bank; and even the cautious geologist who has described how Hampshire was wrought into its present form is willing to believe that man had then appeared in our land. Where you see salt water he would have seen dry land, bounded far away by a range of hills which linked the downs of the Isle of Wight to those that rise behind Weymouth Bay, and of which the Needles remain as lonely relics: he would have seen the Solent flow, a mighty river, enriched by the tribute of the Stour, the Avon, the Itchen, and the Test.[98] Ascend the hill on which stands Dover Castle, and gaze upon Cape Grisnez. Let the waters beneath you disappear: across the chalk that once spanned the Channel like a bridge men walked from the white cliff that marks the horizon to where you stand. No arithmetical chronology can spur the imagination to flights like these.[99]

[Sidenote: Palaeolithic skeletons.]

The dwellers on the plateau, if they did exist in preglacial times, have left us no memorial save their tools: but can we picture to ourselves the lineaments of the palaeolithic hunters who came after them? Human bones, including two perfect skulls, closely associated with the bones of hyenas, have been recovered from a cave near Plymouth. The average height of the people to whom they belonged was little more than five feet: the skulls have hardly been described with sufficient accuracy to enable us to compare them with others of the same period; but, in regard to breadth and to the degree of projection of the lower jaw, they were not very different from the majority of modern British skulls.[100] Two other human skulls have been found in England for which palaeolithic age has been claimed--one near Swanscombe in Kent, the other near Bury St. Edmunds; but the former may not be as old as the bed from which it was unearthed; and the other was so broken that its contour could hardly be restored.[101] But almost all the older palaeolithic skulls that have been found in Western Europe belong to the same type, which is generally called after the famous specimen that was exhumed nearly half a century ago in the Neander valley in Rhenish Prussia, and of which the most characteristic examples were derived from a cavern at Spy in the province of Namur. The Swanscombe skull has somewhat similar characters; and it has been supposed that the earlier palaeolithic inhabitants of Britain belonged to the Neanderthal race. Unfortunately, however, the dates of the Neanderthal and Spy specimens cannot be fixed. The latter may belong to the comparatively advanced period in which the best palaeolithic stone implements of France were manufactured: the former was not seen in place by a competent observer, and its age is quite uncertain.[102] If the very few skeletons that we possess are typical, these men were short, big-boned, and powerfully built. Their heads were long and narrow, their foreheads amazingly low and retreating, and their jaws heavy and projecting. But their most striking features were enormously massive and outstanding brow ridges. Although the Neanderthal skull was described by Huxley as the most ape-like of all human skulls, and although for some time after its discovery it was the subject of animated discussion, it and its congeners were thenceforward regarded by all anatomists until the beginning of the present century as human in the strictest sense of the word. Within the last few years, however, a German anthropologist has endeavoured to prove that it and the two skulls of Spy may only be called human in a limited sense: he refuses to class them under the head of _Homo sapiens_, and refers them to an older species, which he calls _Homo primigenius_. This view, however, has not made influential converts: the Neanderthal skull was capacious enough to lodge a brain as large as that of many a living savage; and trained observers have pointed out that skulls of like contour have belonged in modern times to men of considerable mental power.[103] A considerable number of skeletons have lately been discovered in Moravia, which, although like the Neanderthal race they had long skulls and prominent brows, belonged to a higher type, and, as the length of their thigh-bones showed, were of great stature;[104] while the caves of Baoussé-Roussé, near Mentone, were the resting-place of very ancient men, in whose skeletons anatomists have detected certain negroid characteristics, although their skulls must have contained a large volume of brain.[105]

But the Palaeolithic Age was of such vast duration that before its close Britain may well have been invaded by new races. In the latest period there were living in the Riviera a people whose physical features connect them with the earliest French neolithic race; and in South-Western France skulls of like type have been found at Laugerie-Basse and Chancelade in the valley of the Lozère.[106] The relics of these men which have been discovered in the caves in which they dwelled show that some of them were worthy to be called forerunners of Pheidias and Praxiteles. With their tools of flint or chert they carved ivory dagger-handles, or, as we are now assured, objects of uncertain use,[107] adorning them with figures of the heads of reindeer, and scratched on horns or tusks drawings of mammoths, deer, horses, and hunters spearing salmon, of which the finer examples are recognized by modern artists as true works of art.[108] A single specimen, found in the Robin Hood Cave in Creswell Crags, is all that we can show:[109] but implements with which it was associated present points of likeness to those of the French caves which justify the assumption that the primitive artists of France sent emigrants to our land.

[Sidenote: Range of the palaeolithic hunters in Britain.]

The palaeolithic nomads, whether of the earlier or the later race, pushed their way as far north as Lincolnshire, Derbyshire, and Denbighshire, perhaps even into the East Riding of Yorkshire; and as far west as Glamorganshire, Caermarthenshire and Devonshire:[110] but almost all the remains of their handiwork have been found in the south-eastern district of England,--in Kent, especially the neighbourhood of Reculver, Sussex, Hampshire, Essex, Middlesex, and Surrey, Hertfordshire, Buckinghamshire, and Northamptonshire, Oxfordshire and Berkshire, Cambridgeshire, Norfolk, and Suffolk.

[Sidenote: Where their tools have been found.]

The places in which these relics lay buried may be grouped in four classes,--the plateau gravels, already described; gravels which were apparently deposited not by rivers but by heavy rains which, falling upon frozen chalk downs, destroyed the shattered surface and swept it away in floods;[111] the river-drift, and caves; and, unlike the belongings of the neolithic herdsmen, those of the older inhabitants are not to be found, except in special cases, on or near the surface of the earth. The amateur who has acquired the rudiments of geology and has learned to discern stone implements among the fragments of rock which surround them, knows that in the gravels and sands which rivers deposited at various elevations when they were flowing now here now there in higher and wider channels he may hope to find specimens to add to his collection. Common sense too teaches him that in the same valley the higher terraces were formed before the lower, and that the tools which they contain, however closely they may resemble those which are embedded below, are nevertheless, as a rule, far older.[112] If he asks himself how they found their way into these gravel beds, reflection will soon suggest the answer. It would seem that although the palaeolithic hunters dwelled sometimes near lakes or ponds, they usually settled on the banks of streams. Fishing, hunting, wading through fords, warned by swiftly rising floods to quit their habitations, they lost or abandoned the weapons which now serve our purpose instead of theirs. But in some cases beds which contained palaeolithic remains are so situated that a tiro would never suppose that they had been deposited by running water at all. Few even of professed geologists would have thought of searching on the hill-tops at Caddington, near Dunstable; yet old stone implements have been found there in profusion. When the men who made them were alive the hills were valleys, and the valleys which now lie below the hills did not exist. Nor would it have occurred to any but a geologist that the tools which were espied lying at the foot of the cliffs between Reculver and Herne Bay had fallen from the gravels which line their summit.[113]

[Sidenote: Inhabited caves.]

Kent’s Cavern and the Brixham Cave, near Torquay, the Wookey Hole ‘Hyena Den’, near Wells, the Long Hole Cave in Glamorganshire, and the caves of Creswell Crags, on the north-eastern border of Derbyshire, are perhaps the most famous of their class. Heaps of bones have been found in all of them, which proved that the men who, from time to time, inhabited them were contemporary, like those whose tools are recovered from the river-drift, with animals of which some, like the mammoth, the straight-tusked elephant, and the ‘sabre-toothed’ tiger, have disappeared from the face of the earth, and many have long been extinct in Britain. Generally in the lower strata the stone tools are exactly like those found in the river-drift; while in the higher they are as a rule more elaborately finished, and are associated with needles, harpoons, and other implements of bone. The same sequence is discernible in the palaeolithic caves of France and Belgium.[114]

[Sidenote: Cave implements and river-drift implements.]

Let us compare in some museum the sets of tools and weapons which have been taken from caves with those of the river-drift. Are the latter older than the former, and is it possible to establish in either or in both a chronological succession of types? Taken by itself, the form of palaeolithic implements, at least in this country, is not generally a criterion of their age; but neither the forms of those that have come from the caves nor the bones which accompanied them forbid us to believe that the oldest are at least as old as any that belonged to the drift. Generally speaking, the fauna of the caves and of the river gravels are identical.[115] It is therefore certain that, although in general aspect a collection of implements derived from the former source is unlike one from the latter because the two were deposited in different circumstances, some of the deposits in the drift and in the caves were contemporaneous.[116] Since a few implements of river-drift form have been found in caves along with those of higher types, it seems reasonable to conclude that the same men possessed both; and if those which are characteristic of the caves are almost entirely absent from the drift, is not the explanation partly that they were more perishable, partly that many of them would not have been used in the field? In other words, there is no reason to believe that the later occupants of the caves were men of different race or of different habits from the contemporary hunters whose lost tools have been given up by the drift.[117] Long ago Monsieur de Mortillet framed a chronological classification of French and Belgian palaeolithic implements according to their types, which, though of late years it has been modified, has been provisionally accepted; but in this country it has been found impossible to follow his example: the same types exist here, but the relative antiquity of the specimens can seldom be determined; for implements of the oldest French types have been found in deposits which belong to the close of our Palaeolithic Age.[118] Even when implements from the high-level terraces are compared with those of the lower, no marked distinction is observed. In certain cases of course a local classification has been established. Thus the stone implements in the upper strata of two of the caves of Creswell Crags belonged to the advanced type which is called after the settlement of Solutré in the department of Saône-et-Loire;[119] and the implements of North-East London which, from their position at the bottom of the excavations as well as their colour, were evidently the oldest, were also inferior in workmanship to newer specimens found above them some twelve feet beneath the surface, and far inferior to the newest of the same district, which were recovered from an old land-surface, two or three feet below the existing ground, generally called the ‘Palaeolithic Floor.’[120] Again, in the brick-fields of Caddington excavation revealed an ancient land-surface on which a palaeolithic colony had made their tools. At a later time a new surface about two feet higher was formed by brick-earth, which must have been swept down by heavy rains from the hills above; and on this more implements appeared. Above it again is a bed of contorted drift, containing implements whose deep ochreous colour would seem to show that of the three series they are the oldest: evidently they were washed down from the hill-tops on which perhaps lived the earliest inhabitants of the district, and which, as they were gradually worn away, formed a deposit in what were then valleys, but are now in their turn hills. The lowest implements, which were of course older than those next above them, belong to the type called after the cave of Le Moustier in the valley of the Vezère, which is itself later than the type associated with the high-level gravels of the Somme.[121] It has been suggested that when the evidence of plants or of strata is wanting, the relative age of palaeolithic implements may be provisionally estimated by the animal remains with which they are found. The straight-tusked elephant, the ‘big-nosed’ rhinoceros, and the hippopotamus were characteristic, we are told, of the earliest palaeolithic times;[122] the mammoth, the woolly rhinoceros, the cave-bear, and the hyena of a later period; and the reindeer was specially abundant towards the close of the age. But it is now generally recognized that if this orderly succession of fauna existed in Aquitaine, it cannot be distinguished either in our island or in Northern Gaul. When we find Arctic and tropical animals commingled, when we see that the bones of big-nosed rhinoceros and woolly rhinoceros, of straight-tusked elephant and hyena and reindeer have been dug out of the same beds,[123] we may conclude that it is hardly worth while to gauge the antiquity of the works of palaeolithic craftsmen by such tests as these.

On a general review it should seem that the French chronological classifications of palaeolithic implements, even applied to England, contain a measure of truth. The implements which are commonly found in the river-drift and other deposits in the open field undoubtedly began to be manufactured before those which are characteristic of the caves; and those of Mousterian type were first made, both in England and in France, long before the development of the elegant Solutrean forms and the period in which flourished the artists of South-Western France.[124] But both in France and in England Mousterian implements were still used during the later period;[125] and even drift implements of the oldest kind continued to be used by palaeolithic hunters of the latest generation.[126]

[Sidenote: Divers forms of tools.]

In order to apprehend the culture of the palaeolithic races, it is necessary to be conversant with the forms of their tools. The great majority were made of flint; but in places where flint was scarce or difficult to obtain other stones, for example, chert, quartzite pebbles, sandstones, and felstone, were used. The principal forms were flint flakes, which were probably intended to serve as knives, sometimes even as saws (for a few of them are serrated),[127] and, in certain instances, as scrapers for dressing hides; implements or weapons, pear-shaped or tongue-shaped in outline, more or less acutely pointed, and more or less truncated at the butt, some of which look like spear-heads, though they may have been grasped in the hand; and oval, almond-shaped, and occasionally heart-shaped or triangular implements, which have a cutting edge all round. Each of these forms of course comprises many varieties, not only in contour but also in the mode of chipping; and a few tools of abnormal shapes have also been found, as well as natural blocks of flint, called ‘hammer-stones’, which were used in the process of manufacture, and most of which were slightly trimmed in order to make them more serviceable. Near Ipswich a lady has recently discovered a tiny implement which, it has been fondly suggested, some hunter may have wrought as a toy for his child.[128] Among the bone implements were harpoons, barbed sometimes on one, sometimes on both sides, which have been found in Kent’s Cavern and other caves, and which closely resemble those that are used by the Eskimos of our own day; and needles drilled by bone awls, with eyes so small that the threads of reindeer sinew which they received could hardly have exceeded a thirtieth of an inch in diameter. Moreover, it is more than probable that clubs, wooden tools, and utensils and vessels of skin were also used, which, from their perishable nature, have long since disappeared.[129]

[Sidenote: Palaeolithic workshops.]

The explorations of antiquaries have revealed more than one of the open-air workshops in which the primitive tool-makers plied their trade. Near Crayford, on a sandy beach beneath an old chalk cliff that overhung the Thames when on its southern side its bed was nearly two miles wider, excavation discovered the surface, strewn with flint flakes, in actual contact with mammoths’ bones, on which the workers had lived and toiled until a great flood drove them away, leaving the sediment which for countless ages concealed their remains. The inferior quality of the flint showed that they had not known how to win it by mining from the rock, but had been obliged to content themselves with such stray blocks as they could find. The enthusiast who discovered the site was actually able to fit many of the flakes together, and to reconstruct the original blocks from which they had been struck off.[130] At Caddington, where hammer-stones and punches, great blocks of flint which had been used as anvils, and innumerable flakes and cores bore their silent testimony, Mr. Worthington Smith inferred from the confusion in which finished and unfinished tools were left that the settlers, terrified perhaps by some violent storm, had suddenly quitted their abode. He found an implement which had been ruined by an ill-directed blow of the hammer, and one which had been re-flaked and re-pointed by a later worker; and his practised eye detected that the craftsmen had flaked their tools differently from those of Crayford.[131] Speaking generally, however, the methods of working were the same as those which are still followed by the ‘knappers’ of Brandon in Suffolk, who manufacture gun-flints for African savages. The flakes which were to be used as knives or scrapers were detached from the blocks by a stone hammer; and the larger implements were trimmed into the various shapes which have been described, by blows along their edges, which chipped off small splinters. The effect of the hammer was to produce on the flake, just below the point where the blow was delivered, a protuberance, which is called the ‘bulb of percussion’, and which of course left a corresponding cavity on the block from which the flake was detached. This bulb is the mark by which a manufactured flint may be recognized; but on tools whose artificial origin is manifest even to an untrained eye it has often been obliterated by the process of chipping.[132]

[Sidenote: Handles.]

Inquisitive antiquaries have raised the question whether any palaeolithic implements were furnished with handles. The Tasmanians simply grasped their tools in their hands;[133] and there is little evidence that the Britons mounted theirs:[134] but the triangular sharply-pointed flints which have been already described might sometimes have been used as arrow-points or javelin-heads.[135] Some were doubtless missiles and nothing more.

[Sidenote: Uses of tools.]