Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-24T16:46:49.845Z Has data issue: false hasContentIssue false
  • English
  • Français

Alleged thermal erosional structures near Farnham, England

Published online by Cambridge University Press:  01 May 2009

P. Worsley  and
I. D. Bryant
P. Worsley
Affiliation:
Department of Geography, University of Reading, No. 2 Earley Gate, Whiteknights Road, Reading RG6 2AU, 27th May 1982
I. D. Bryant
Affiliation:
Department of Geography, University of Reading, No. 2 Earley Gate, Whiteknights Road, Reading RG6 2AU, 27th May 1982
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Correspondence
Information
Geological Magazine , Volume 120 , Issue 1 , January 1983 , pp. 81 - 82
Copyright
Copyright © Cambridge University Press 1983

References

American Geological Institute, 1962. Dictionary of Geological Terms. New York: Dolphin Books.Google Scholar
Andersson, J. G. 1906. Solifluction; a component of subaerial denudation. J. Geol. 14, 91–112.CrossRefGoogle Scholar
Fisher, P. & Rolls, J. D. 1982. A thermokarst phenomenon on a terrace of the River Wey, near Farnham, Surrey, England. Geol. Mag. 119, 315–18.CrossRefGoogle Scholar
French, H. M. 1976. The periglacial environment. London: Longman.Google Scholar
Washburn, A. L. 1979. Geocryology. London: Arnold.Google Scholar