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III.—On Subaërial Denudation, and on Cliffs and Escarpments of the Chalk and Lower Tertiary Beds

Published online by Cambridge University Press:  01 May 2009

William Whitaker
Affiliation:
Geological Survey of England.

Extract

For some years geologists have more or less agreed in the view that the present features of the earth, whether hill, valley, or plain (with some small exceptions, as volcanic outbursts) have been formed directly by denudation; though indirectly disturbances, whether faults upheavals or sinkings, have of course had their effect in determining the flow, so to speak, of the denuding agent.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1867

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References

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page 449 note 8 I believe that: Professor Ramsay started this argument against the marine origin of escarpments.—W. W.Google Scholar

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1 Professor Ramsay has noticed the great thickness of solid rock that must have been denuded in Wales (Mem. Geol. Surv. vol. i. p. 297, and plates. 4, 5, 1846; and vol. iii. p. 236, and pl. 28, 1866). I believe that the former of these was the first attempt at showing the vast amount of denudation that has taken place.Google Scholar