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Some Theoretical Factors in Geomorphological Analysis

Published online by Cambridge University Press:  01 May 2009

W. Q. Kennedy
W. Q. Kennedy
Affiliation:
Geology Department, University of Leeds.
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Abstract

Consideration of the relative rates of uplift-erosion and erosion-denudation leads to the recognition of nine cases which define the conditions of geomorphological evolution. It is concluded that a peneplanated surface may develop during active tectonic uplift, and that the total volume of clastic sediments produced during any stage is inversely proportional to the rate of uplift.

Type
Articles
Information
Geological Magazine , Volume 99 , Issue 4 , August 1962 , pp. 304 - 312
Copyright
Copyright © Cambridge University Press 1962

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References

REFERENCES

Davis, W. M., 1899. The Geographical Cycle. Geographical Journal, 14, 481–504. Reprinted in Geographical Essays, Boston, 1909, 249–278.CrossRefGoogle Scholar
Penck, W. (translated by Czech, H. and Boswell, K. C.), 1953. Morphological Analysis of Land Forms. Macmillan, London.Google Scholar