Page:Palæolithic Man and Terramara Settlements in Europe.djvu/137
Land Oscillations.
That the lands of Western Europe, subsequent to their submergence in the glacial sea and the deposition of the boulder clay, stood much higher than at the present time, is a matter capable of direct proof. The extent of the elevation was such at one time as to admit of the British Isles being an integral part of the Continent; without which it would be impossible for the fauna of the river-gravels and the bone caves to have spread over the greater part of the British Isles. Moreover, most of these animals found access to several districts which are now islands. In the recently discovered Palæolithic cave in Jersey were found some human teeth, together with bones of the reindeer, woolly rhinoceros, horse, some species of deer and bovidæ, associated with flint implements of Moustérien types a combination of relics which conclusively proves that Jersey was formerly connected with the Continent. (Archæologia), vol. lxxii., p. 454.)
Professor Boyd Dawkins, in describing ossiferous caverns in Pembrokeshire, thus writes:—
I have already referred to bones and teeth of extinct mammalia as having been dredged from the bed of the German Ocean; and also to submerged forests. On the latter point,