Climatic Variations Their Extent And Causes

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Shales with occasional erratics in the Lower Marine Series.
Lochinvar Glacial Beds at the Base of the Lower . Marine Sc- ries.
Again, whatever view may be held on the controversy as to the occurrence of warm iuterglacial periods during the Pleis- 1 There Is some evidence of glacial beds of this period on the cast of the t'ral Mountains.
2 A. Julien. "Ant-lens glaciers de la Feriode Houillore dans le Plateau Central de la France. " Ann. Club Alpin Franeais. Vol. XXI. 1S!4. Pp. Lis.
3 A. E. Kitso
...n. "On the Occurrence of Glacial Beds at Wynyard, near Table Cape. Tasmania. " 1'roc. It. Sue. Victoria, new Ser.. Vol. XV. I'. Mii, 1>. :U.
4 T. W. K. David. "Discoverey of Glaciated I'. Oiilders ai I'. Ase f Permo-CarbonJ ferous System. I.^ehinvar. New South Wales. " Journ. It. Soc. N. S. Wales. Vol. XXXI II. 1889, pp. 154-159.
CLIMATIC VARIATIONS. 19 toeene glaciation of Europe, it will be generally admitted that considerable 1 oscillations occurred in the extent of the ice. Thus the evidence in the British Isles, strongly supports the view that after the maximum glaciation, there was a redaction in the extent of the ice, and then after some interVal^a-fresh advance of valley glaciers'.


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