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I.—The Rôle of Solution in Valley-making

Published online by Cambridge University Press:  01 May 2009

A. J. Jukes-Browne
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Extract

It has recently been suggested that many of the dry valleys which are found in limestone districts owe their formation to subterranean solution, and not to surface-erosion; in other words, that they are the work of subterranean watercourses which, by dissolving the rock substance, have caused subsidence of the surfaces overlying the lines of such watercourses.

Type
Original Articles
Information
Geological Magazine , Volume 5 , Issue 12 , December 1908 , pp. 529 - 534
Copyright
Copyright © Cambridge University Press 1908

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References

page 529 note 1 See “Solution Valleys in the Glyme Area (Oxfordshire),” by the Rev. Spicer, E. C. M.A., F.G.S.: Quart. Journ. Geol. Soc., 1908, vol. lxiv, pt. 3, pp. 335–44, pls. xxxviii, xxxix.CrossRefGoogle Scholar

page 532 note 1 Geographical Magazine for September, 1908, p. 288.

page 532 note 2 Op. cit., p. 277.

page 533 note 1 “The Cretaceous Rocks of Britain”: Mem. Geol. Survey, 1904, vol. iii, p. 418.Google Scholar

page 533 note 2 Quart. Journ. Geol. Soc., 1906, vol. lxii, p. 158.Google Scholar