STRATIFIED BEDS IN TILL, LEITHEN WATER, PEEBLESSHIRE, SCOTLAND.
And again, the same writer says:
"The intercalated beds are remarkable for having yielded an imperfect skull of the great extinct ox (Bos primigenius), and remains of the Irish elk or deer, and the horse, together with layers of peaty matter."[2]
Several of our foremost scientists see in the phenomena of the Drift the evidences of a cataclysm of some sort.
Sir John Lubbock[3] gives the following representation of a section of the Drift at Joinville, France, containing
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SECTION AT JOINVILLE.
[1. "The Great Ice Age," p. 149.
2. Ibid., p. 149.
3. "Prehistoric Times," p. 370.]