The archæology and prehistoric annals of Scotland

by Sir Daniel Wilson

CHAPTER I.—THE PRIMEVAL TRANSITION.

The closing epoch of geology, which embraces the diluvial formations, is that in which archæology has its beginning. In a zoological point of view, it includes man and the existing races of animals, as well as the extinct races which appear to have been contemporaneous with indigenous species. Archæology also lays claim to the still more recent alluvium, with all its included relics pertaining to the historic period. Within the legitimate scope of this department of investigation are comprehended the entire evidence of changes on the geographical features of the country, on its coasts and harbours, its estuaries, rivers, and plains: all properly coming within the limits of Archæology, though too extensive to be embraced in the present review of its elements. This much, however, we learn from an examination of the detritus and its included fossils, that at the period immediately preceding the occupation of the British Islands by their first colonists the country must have been almost entirely covered with forests, and overrun by numerous races of animals long since extinct. Much has been done in recent years to complete the history of British fossil mammalia; and though less attention has been paid to the question in which we are here most deeply interested, as to what portion of them are to be considered as having been contemporaneous with man, yet on this also some interesting light has been thrown. The most extensive discoveries of mammalian remains and recent shells generally occur along the valleys by which the present drainage of the country takes place, and hence we infer that little change has taken place in its physical conformation since their deposition. These, however, include the mammoth, elephant, rhinoceros, cave tiger, with other extinct species, and are referrible to the earlier portion of an epoch, with the close of which we have alone to deal. They belong to that period in which our planet was passing through its very latest stage of preparation prior to its occupation by man; a period on which the geologist, who deals with phenomena of the most gigantic character, and with epochs of vast duration, is apt to dwell with diminished interest, but which excites in the thoughtful mind a keener sympathy than all that preceded it. The general geographical disposition of the globe was then nearly as it still remains. Our own island was, during a great portion of it, insulated, as it is now. Yet it is of this familiar locality that the palæontologist remarks:—"In this island, anterior to the deposition of the drift, there was associated with the great extinct tiger, bear, and hyæna of the caves, in the destructive task of controlling the numbers of the richly developed order of the herbivorous mammalia, a feline animal, (the Machairodus Latidens,) as large as the tiger, and, to judge by its instruments of destruction, of greater ferocity."[20] It was within the epoch to which these strange mammals belong, and while some of them, and many other contemporaneous forms of being, still animated the scene, that man was introduced upon this stage of existence, and received dominion over every living thing.

It has been supposed by more than one intelligent naturalist, that the gigantic fossil elk (Megaceros Hibernicus) co-existed with the human race. Dr. Hart has produced what he conceived to be conclusive evidence on this subject, derived from the appearance of a rib, pierced with an oval opening near its lower edge, "with the margin depressed on the outer and raised on the inner surface, round which there is an irregular effusion of callus; in fact, such an effect as would be produced by the head of an arrow remaining in a wound after the shaft was broken off." This conclusion Professor Owen has disputed, apparently on satisfactory grounds.[21] By a similar line of argument, however, to which he has yielded his assent,[22] it has been shewn that the north of Europe was occupied by the human race at a time when the Bos primigenius, the Bison priscus, and the Ursus spelæus, existed.[23] Of the Ursus spelæus, or great cave bear, a skeleton is preserved in the museum of Lund, found in a peat-bog in Scania, under a gravel or stone deposit, and alongside of primitive implements of the chase. Though no such direct evidence has yet been observed here, similar conclusions have been arrived at. Mr. Owen, after referring the period of existence of the great cave bear to earlier geological epochs, adds, as the conclusion from present evidence, "that the genus surviving, or under a new specific form reappearing, after the epoch of the deposition and dispersion of those enormous, unstratified, superficial accumulations of marine and fresh-water shingle and gravel, called drift and diluvium, has been continued during the formation of vast fens and turbaries upon the present surface of the island, and until the multiplication and advancement of the human race introduced a new cause of extermination, under the powerful influence of which the Bear was finally swept away from the indigenous fauna of Great Britain."[24] To these native mammals may be added the horse, the roebuck, the red deer, the wild boar, the brown bear, the wolf, and the beaver, all of which have undoubtedly existed as wild animals in this country, and been gradually domesticated or extirpated by man.[25]

The most interesting of all the species for our present inquiry are those adapted for domestication, among which the Bovidæ occupy a prominent place. Of these, the great fossil ox (Bos primigenius) is very frequently found in Scotland. Dr. Fleming describes a skull of one in his possession measuring 27½ inches in length,[26] and a still larger one from Roxburghshire, now in the Scottish Antiquarian Museum, measures 28 inches in length. No evidence leads us to conclude that any attempt was made by the native Britons to domesticate either of the two kinds of gigantic oxen, the bison or great urus, which the Romans discovered on first penetrating into the north of Europe. But besides these there was also a smaller primitive wild species, the Bos Longifrons, of the domestication of which in Britain we have abundant proof, at least at the period of the Roman invasion. Soon after this it appears to have become extinct, so that we are rather led to assume that it may have been the domesticated ox of the native population prior to the intrusion of the Romans. Mr. Woods refers to the discovery of the skull and horns of the great urus in a tumulus on the Wiltshire Downs, along with bones of deer and boars, and fragments of native pottery, in proof of the existence in this country originally of a "very large race of taurine oxen, although most probably entirely destroyed by the aboriginal inhabitants before the invasion of Britain by Cæsar." Professor Owen has discussed the probable influence of Roman occupation on the wild herds and the breeds of domesticated oxen, with much sagacity, though somewhat too much influenced by the views so generally entertained of the barbarian state of the native Britons prior to the intrusion of Roman colonists.[27] Scarcely less interesting is the evidence which British fossil mammalia furnish of the existence of the horse among the native wild animals of the country, since we find proof, both in the early tumuli and the subterranean dwellings, not only of its domestication, but also of its being used for food.

This very slight glance at the most prominent indications of the primeval state of the country, will suffice to convey some idea of the circumstances under which the aboriginal colonists entered on the possession of the British Isles. Other portions of the same line of argument, derived from the fossil mammalia, and the circumstances under which they are discovered, will come under review in the course of our inquiries. The fossil Cetacea, especially, furnish most interesting and conclusive evidence of the very remote period at which the presence of a human population is discoverable in Scotland, while the beaver, (Castor Europæus,) which is frequently found in a fossil state, is also proved to have existed as a living species, both in Scotland and Wales, down to the twelfth century, and is even referred to so late as the fifteenth century. To the abundance of wild animals which continued to occupy the moors and forests of Scotland, long after the primitive states of society had entirely passed away, we shall also have occasion hereafter to refer. The same causes which exterminated the huge urus, the cave bear, and others of the largest and most intractable of the wild denizens of the British forests, ultimately led to the extinction of the greater number of those which either supplied objects of the chase, or were inimical to the social progress of man. Thus we observe, in the economy of nature, that one species after another disappears, to make way for newer occupants, until at length the last of those huge preadamite races of being give place, before the gradual advancement of man to assume possession of terrestrial dominion. Yet on this point also those questions in historic chronology, which tend to determine more precisely the lapse of centuries intervening between the Adamic creation and the earliest era of authentic history, exercise an important influence. Geology leaves no room for questioning the fact, that man did not enter upon this earth after some tremendous cosmical revolution, which made way for an entirely new race of beings, but that he was introduced as the lord of an inheritance already in possession of many inferior orders of creation. Contemporary with the most remarkable cave fossils are found the remains of many historic, or still existing species, and the precise line has yet to be drawn which shall determine how many of these were extinct, at the period when the Creator, at length satisfied with his inferior works, said, "Let us make man in our image, after our likeness." The remains, both of the large cave hyæna, (Hyæna spelæa,) and of the great cave tiger, (Felis spelæa,) occur not only in ossiferous caverns, but have also been found in superficial unstratified deposits. Considerable portions of the skeleton of the latter were discovered in 1829, along with remains of the mammoth, rhinoceros, ox, stag, and horse, in a marl-pit near North Cliff, Yorkshire. Under precisely similar geological circumstances the Bos primigenius has very frequently been brought to light in Scotland. It is of this animal that Sir R. I. Murchison remarks, in a letter to Professor Owen, descriptive of an example already referred to, found in a bog in Scania: "This urus is most remarkable in exhibiting a wound of the apophysis of the second dorsal vertebra, apparently inflicted by a javelin of one of the aborigines, the hole left by which was exactly fitted by Nillson with one of the ancient stone javelins.... This instrument fractured the bone, and penetrated to the apophysis of the third dorsal vertebra, which is also injured. The fractured portions are so well cemented, that Nillson thinks the animal probably lived two or three years after. The wound must have been inflicted over the horns, and the javelin must have been hurled with prodigious force." Of the existence, therefore, of the Bos primigenius within the historic epoch, we can entertain no doubt, and it is accordingly requisite to give full weight to the influence which its presence must have exercised on the general condition of our island. Professor Owen remarks, after showing the erroneous nature of the usually received opinion, that the lion, the tiger, and the jaguar, are peculiarly adapted to a tropical climate:—"A more influential, and, indeed, the chief cause or condition of the prevalence of the larger feline animals, in any given locality, is the abundance of the vegetable feeding animals in a state of nature, with the accompanying thickets or deserts unfrequented by man. The Indian tiger follows the herds of antelope and deer, in the lofty Himalayan chain, to the verge of perpetual snow. The same species also passes that great mountain barrier, and extends its ravages with the leopard, the panther, and the cheetah, into Bocharia, to the Altaic chain, and into Siberia, as far as the fiftieth degree of latitude; preying principally, according to Pallas, on the wild horses and asses."[28] No change, therefore, of climate, nor any remarkable geological revolution is needful to account for the disappearance of the huge British carnivora, the remains of which abound in the ossiferous caves. They pertain to the closing transition-period of the preadamite earth, and, as in other transition-periods which we shall have to consider, some traces of them survived among the inheritors of the new era. It is therefore a legitimate source of interest to the archæologist, to observe the mingling of extinct and familiar species among the fossil mammals found in the superficial deposits, wherein so much of the evidence of his own science must be sought. It discovers to him the precise link by which his pursuits take hold of the great chain of truth, and in a new sense shews man, not as an isolated creation, but as the last and best of an order of animated beings, whose line sweeps back into the far removed shadow of an unmeasured past. "Phenomena like these," says Professor Sedgwick, when referring to the discoveries at the North Cliff, Yorkshire, in 1829, "have a tenfold interest, binding the present order of things to that of older periods, in which the existing forms of animated nature seem one after another to disappear."[29]

Thus much is apparent from the most superficial glance at the geological evidence of the primeval state of Britain within the historic era, that though corresponding in its great geographical outlines to its present condition, it differed, in nearly every other respect, as widely as it is possible for us to conceive of a country capable of human occupation. A continuous range of enormous forests covered nearly the whole face of the country. Vast herds of wild cattle, of gigantic proportions and fierce aspect, roamed through the chase, while its thickets and caves were occupied by carnivora, preying on the herbivorous animals, and little likely to hold in dread the armed savage who intruded on their lair. The whole of these have existed since the formation of the peat began, and therefore furnish some evidence of the very remote antiquity to which we must refer the origin of some of the wastes that supply, as will be seen in subsequent chapters, an important element in the elucidation of primitive chronology. Upon this singular arena Archæology informs us that the primeval Briton entered, unprovided with any of those appliances with which the arts of civilisation arm man against such obstacles. Intellectually, he appears to have been in nearly the lowest stage to which an intelligent being can sink; morally, he was the slave of a superstition, the grovelling character of which will be traced in reviewing his sepulchral rites; physically, he differed little in stature from the modern inheritors of the same soil, but his cerebral development was poor, his head small in proportion to his body, his hands, and probably his feet, also small; while the weapons with which he provided himself for the chase, and the few implements that ministered to his limited necessities, indicate only the crude development of that inventive ingenuity which first distinguishes the reason of man from the instincts of the brutes. The evidence from which such conclusions are deduced, forms the subject of the following chapters.