Man, Past and Present by Agustus Henry Keane, A. Hingston Quiggin, Alfred Court Haddon (best young adult book series .txt) 📖

of sepulchral monuments the dolmens and the long barrows. But towards the end of the Stone Age a brachycephalic race was already penetrating into the islands. This appears to have been a peaceful infiltration, at any rate in certain districts, where remains of the two types are found side by side and there is evidence of racial intermixture. The brachycephals introduced a new form of sepulture, making their burial mounds circular instead of elongated, whence Thurnam's convenient formula, "long barrow, long skull; round barrow, round skull." But the earlier view that there was a definite transition from long heads, neolithic culture and long barrows, to round heads, bronze culture and round barrows can no longer be maintained. "It is often taken for granted that no round barrows were erected in Britain before the close of the Neolithic Age, and that the earliest of the brachycephalic invaders whose remains have been found in them landed with bronze weapons in their hands[1250]." But there is abundant evidence that the brachycephalic element preceded the knowledge of metals, and a number of round barrows in Yorkshire and further north show no trace of bronze.

Nevertheless the majority of the round barrows belong to the Bronze Age, and the physical type of their builders is sufficiently well marked. The stature is remarkably tall, attaining a height of 1.763 m. or over 5 ft. 9 ins. The skull is brachycephalic with an average index of about 80. It is also characterised by great strength and ruggedness of outline, with (often) a sloping forehead, prominent supraciliary ridges, and a certain degree of prognathism.

According to Rolleston's description "The eyebrows must have given a beetling and probably even formidable appearance to the upper part of the face, whilst the boldly outstanding and heavy cheekbones must have produced an impression of raw and rough strength. Overhung at its root, the nose must have projected boldly forward." And Thurnam adds "the prominence of the large incisor and canine teeth is so great as to give an almost bestial expression to the skull[1251]."

Although this type is conveniently called the Round Barrow type, or even the Round Barrow Race, the round barrows also contain remains of a different racial character. The skull form shows a more extreme brachycephaly, with an index of 84 or 85, and exhibits none of the rugged features associated with the true Round Barrow type. On the contrary, of the two typical groups, one from round barrows in Glamorganshire, and the other from short cists in Aberdeenshire not one of the skulls is prognathous, the supraciliary ridges are but slightly developed, the cheek bones are not prominent, the face is both broad and short and the lower jaw is small. But the greatest contrast is in the height, which averages in the two groups, 1.664 m. and 1.6 m. respectively, i.e. 5 ft. 5-3/4 ins. and 5 ft. 3 ins. All these characters connect this type closely with the Alpine type on the continent.

These round-headed peoples have been the subject of much discussion ably summarised and criticised by Rice Holmes, whose conclusion perhaps best represents the view now taken of their affinities and origins.

"The great mistake that has been made in discussing the question is the not uncommon assumption that the brachycephalic immigrants who buried their dead in round barrows arrived in Britain at one time, and came from one place. Some of them certainly appeared before the end of the Neolithic Age: others may have introduced bronze implements or ornaments; others doubtless came, in successive hordes, during the course of the Bronze Age. Some of those who belonged to the Grenelle race [Alpine type], who certainly came from Eastern Europe and possibly from Asia, and whose centre of dispersion was the Alpine region, may have started from Gaul; others could have traced their origin to some Rhenish tribe; and I am inclined to believe that those who belonged to the characteristic rugged Round Barrow type crossed over, for the most part, from Denmark or the out-lying islands[1252]."

After the passage of the Romans, who mingled little with the aborigines and made, perhaps, but slight impression on the speech or type of the British populations, a great transformation was effected in these respects by the arrival of the historical Teutonic tribes. Hand in hand with the Teutonic invasions went a lust for expansion on the part of the peoples in Ireland. Settlements were effected by them in South Wales and Anglesey, the Isle of Man and Argyll, probably also in North Devon and Cornwall. For many generations the south and east of England were the scenes of fierce struggles, during which the Romano-British civilisation perished. Only in more inaccessible districts, such as the fen country, may a British population have survived, though Celtic languages are not yet dislodged from their mountain strongholds in Wales and Scotland, and lingered for many centuries in Strathclyde and Cornwall. After the strengthening of the Teutonic element by the arrival of the Scandinavians and Normans, all very much of the same physical type, no serious accessions were made to this composite ethnical group, which on the east side ranged uninterruptedly from the Channel to the Grampians. Later the expansion was continued northwards beyond the Grampians, and westwards through Strathclyde to Ireland, while now the spread of education and the development of the industries are already threatening to absorb the last strongholds of Celtic speech in Wales, the Highlands, and Ireland.

Thanks to its isolation in the extreme west, Ireland had been left untouched by some of the above described ethnical movements. It is doubtful whether Palaeolithic man ever reached this region, and but few even of the round-heads ranged so far west during the Bronze Age[1253]. The land oscillations during post-Glacial times appear to have been practically identical over an area including northern Ireland, the southern half of Scotland, and northern England. There was a period of depression followed by one of elevation. The Larne beach-deposits prove that Neolithic man was in existence from almost the beginning of the deposition of that series until after its conclusion. The estuarine clays of Belfast Lough correspond to the depression, and the Neolithic period extended from at least near the top of the lower estuarine clay to the beach-deposit of yellow sand which overlies it, or possibly till later. It is to this period of elevation that the Neolithic sites among the sand dunes of North Ireland belong; those of Whitepark Bay and Portstewart, for example, extend to the maximum elevation. A slight movement of subsidence of about five feet in recent times has left the surface as we now find it. The implements found in the Larne gravels correspond to some extent with those of Danish kitchen-middens; this was not a dwelling site but a quarry-shop or roughing-out place, the serviceable flakes being taken away for further manipulation; it thus belongs to the earliest phase of neolithic times. The sandhill sites were occupied, continuously and occasionally, during neolithic times, through the Bronze Age, and into the Iron and Christian periods[1254]. Nina F. Layard has recently studied the Larne raised beach and exposed a new section. She states that "Taken as a whole the flints certainly do not correspond at all closely either to the Palaeoliths or Neoliths so far found in England.... Some are strongly reminiscent of well-known drift type.... Again, there are shapes that bear a closer resemblance to some of the earliest Neolithic types[1255]." She believes that, from their rolled condition, they were derived from another source.

J. Bigger[1256] described some kitchen-middens at Portnafeadog, near Roundstone, Connemara, which yielded stone hammers but no worked flints, pottery or metal-ware. The chief interest of this paper is due to the fact that it is the first record of the occurrence of vast quantities of the shells of Purpura lapillus, all of which were broken in such a manner that the animal could easily be extracted. There can be no doubt that the purple dye was manufactured here in prehistoric times[1257]. W. J. Knowles[1258] suggests from the close resemblance--in fact identity--of a great number of neolithic objects in Ireland with palaeolithic forms in France (Saint-Acheul, Moustier, Solutre, La Madeleine types), that the Irish objects bridge over the gap between the two ages, and were worked by tribes from the continent following the migration of the reindeer northwards. These peoples may have continued to make tools of palaeolithic types, while at the same time coming under the influence of the neolithic culture gradually arriving from some southern region. The astonishing development of this neolithic culture in the remote island on the confines of the west, as illustrated in W. C. Borlase's sumptuous volumes[1259], is a perpetual wonder, but is rendered less inexplicable if we assume an immense duration of the New Stone Age in the British Isles. The Irish dolmen-builders were presumably of the same long-headed stock as those of Britain[1260], and they were followed by Celtic-speaking Goidels who may have come directly from the continent[1261], and there is evidence in Ptolemy and elsewhere of the presence of Brythonic tribes from Gaul in the east. Since these early historic times the intruders have been almost exclusively of Teutonic race, and Viking invaders from Norway and Denmark founded the earliest towns such as Dublin, Waterford and Limerick. Now all alike, save for an almost insignificant and rapidly dwindling minority, have assumed the speech of the English and Lowland Scotch intruders, who began to arrive late in the 12th century, and are now chiefly massed in Ulster, Leinster, and all the large towns. The rich and highly poetic Irish language has a copious medieval literature of the utmost importance to students of European origins.

In Scotland few ethnical changes or displacements have occurred since the colonisation of portions of the west by Gaelic-speaking Scottic tribes from Ireland, and the English (Angle) occupation of the Lothians. The Grampians have during historic times formed the main ethnical divide between the two elements, and brooklets which can be taken at a leap are shown where the opposite banks have for hundreds of years been respectively held by formerly hostile, but now friendly communities of Gaelic and broad Scotch speech. Here the chief intruders have been Scandinavians, whose descendants may still be recognised in Caithness, the Hebrides, and the Orkney and Shetland groups. Faint echoes of the old Norrena tongue are said still to linger amongst the sturdy Shetlanders, whose assimilation to the dominant race began only after their transfer from Norway to the Crown of Scotland.

Since 1901 the researches of Gray and Tocher[1262] on the pigmentation of some 500,000 school children of Scotland have increased our information as to racial distribution. The average percentage of boys with fair hair is nearly 25 for the whole of the country, and when this is compared with 82 in Schleswig Holstein "we are driven to the conclusion that the pure Norse or Anglo-Saxon element in our population is by no means predominant. There is evidently also a dark or brunette element which is at least equal in amount and probably greater than that of the Norse element" (p. 380). Pure blue eyes for the whole of Scotland average 14.7 per cent., which may be compared with 42.9 in Prussia. The greatest density for fair hair and eyes is to be found in the great river valleys opening on to the German Ocean, and also in the Western Isles. The Tweed, Forth, Tay and Don all show indications of settlements of a blonde race "probably due to Anglo-Saxon invasions," but the maximum is to be found at the mouth of the Spey. The high percentage here and in the Hebrides and opposite coasts, the authors trace to Viking invasions. The percentage of dark hair for boys and girls is 25.2 as compared with 1.3 in Prussian school children, the maximum density as we should expect being in the west. Jet black hair (1.2%) has its maximum density in the central highlands and wild west coast. Beddoe[1263] commenting on Gray and Tocher's