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IV.—Notes on “The Great Ice Age” in Relation to the Question of Submergence

Published online by Cambridge University Press:  01 May 2009

Extract

Leaving those local matters, there is a point of some general interest, suggested by several passages of Dr. Geikie's work, which we should like briefly to notice before laying it aside. It is in regard to those repeated depressions and re-elevations of the land which he still favours in connection with the Glacial epoch. Dr. Geikie's latest “scheme” of that epoch seems to include at least five Glacial and four inter-Glacial periods, accompanied by submergences and re-elevations to the extent of between 500 and 600 feet—the maximum being for the present restricted to that amount. Frankly, we confess ourselves unable to see the proofs for so many Glacial and inter-Glacial periods, of which, if they did occur, it would apparently be impossible—on the author's own premises as to glacial erosion—now to discover any traces. Apart from this, we might remark on the inherent improbability of such extensive oscillations of the earth's crust having happened in recent geological times, without leaving more distinct evidence of themselves than the very scanty and doubtful deposits which we have been considering.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1895

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References

page 403 note 1 See “Great Ice Age,” pp. 323–325, 421 and 422. Also “Fragments of Earth Lore,” pp. 319–321.

page 403 note 2 “On Geological Climate,” Trans. Geol. Soc. Glasgow, vol. v.Google Scholar