.
ny clay, called 'till' or 'hard-pan.' Through
r the till consists more
it, will be found to be the s
e earth, it is unfossiliferous. That is to say, it con
sider it, is an e
up, and not contain any evidences of life? It is as if one were to say that he had col
two places have shells ever been obtained, with certainty, from a bed in the true till of Scotland. They occur here and there in bowlder-clay, and
ift is entirely destitut
at even the stratified drift
nd, and Wales, I might add throughout the northern hemisphere, on both sides of the Atla
Ice Age," G
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