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Discovering a meaning in scenery

Published online by Cambridge University Press:  01 May 2009

C. H. Crickmay
C. H. Crickmay*
Affiliation:
525 Salem Avenue, Calgary 4, Alberta, Canada
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Summary

A problem is seen in the claim (made ten years ago) that, under certain conditions, either during uplift of the crust or statically at high levels, denudation alone might develop a peneplain. Observations are now brought forward which seem to indicate that uplift, when active, exceeds the rate of stream erosion, which in turn always exceeds the rate of denudation; and from this, doubt arises as to the postulated peneplain origins.

Type
Research Article
Information
Geological Magazine , Volume 109 , Issue 2 , March 1972 , pp. 171 - 177
Copyright
Copyright © Cambridge University Press 1972

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References

Ahnert, F. 1970. Functional relationships between denudation, relief, and uplift in large mid-latitude drainage basins. Am. J. Sci. 268, 243–63.CrossRefGoogle Scholar
Crickmay, C. H. 1959. A preliminary inquiry into the formulation and applicability of the geological principle of uniformity. 50 pp, illus. Publ. by author, Calgary, , Canada.Google Scholar
Crickmay, C. H. 1971. The role of the river. 30 pp. Publ. by author, Calgary, , Canada.Google Scholar
Davis, W. M. 1899. The Peneplain. Am. Geol. 23, 207–39.Google Scholar
Davis, W. M. 1905. The geographic cycle in an arid climate. J. Geol. 13, 381–407.Google Scholar
Kennedy, W. Q. 1962. Some theoretical factors in geomorphological analysis. Geol. Mag. 99, 304–312.CrossRefGoogle Scholar
Penck, W. 1924, transl. 1953. Morphological analysis of land forms. 420 pp., illus. Macmillan, London.Google Scholar
Schumm, S. A. 1963. The disparity between present rates of denudation and orogeny. U.S. Geol. Survey, Prof. paper 454H, 13 pp.CrossRefGoogle Scholar