JOURNAL of the WATERFORD & SOUTH-EAST of Lreland
JOURNAL OF THE WATERFORD & SOUTH-EAST OF lRELAND ARCHEOLOGICAL SOCIETY. FIRST QUARTER, JANUARY TO MARCH, 1915. SUBSOIL OF (Papers on Elementary. Archazology.) - By Rev, P. POWER. ROM the material at hand it is impossible to specify, even approximately, the duration in Europe of the palaeolithic period. The duration was certainly immense ; some authorities express the number of years in five, others in six, and some in even seven figures. That last period of geologic time-extend- ing forward from, roughly speaking, commencement of the Ice Age, scientists call the Pleistocene. It may be regarded as a sub-division of the Quaternary-the other sub-division being the Recent. A.&hropologists, and indeed archreologists very generally, claim the existence of man in Europe before termination of the Glacial period. On this subject by the way, the reader might consult with much profit a very interesting , article by Rev. Dr. Cooper of Washington in the (American) "Ecclesiastical Review" for ~e~tember.Let us glance over the face of Europe as it appeared in glacial times. In our hasty and beneral survey we need not trouble ourselves about such details as glacial or interglacial epochs. 'This"is what we see:: north of a line drawn along the south coast of helaid, continued across England from the Severn to the Thames, and prolonged midway through the continent to Moscow, a solid ice cap, hundreds of feet thick over the British Isles, and miles thick at its centre which is Scandanavja. The ice coat, by the way, is of generous fit ; it not merely covers Ireland from top to toe but it extends far beyond the western Irish coast into the Atlantic.
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