Hostname: page-component-cd9895bd7-gxg78 Total loading time: 0 Render date: 2024-12-28T02:18:34.118Z Has data issue: false hasContentIssue false
  • English
  • Français

Theory of glacier variations; reply to Dr. Shumskiy’s letter

Published online by Cambridge University Press:  30 January 2017

J. F. Nye
J. F. Nye*
Affiliation:
H. H. Wills Physics Laboratory, Royal Fort, Bristol 2, England
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content. As you have access to this content, full HTML content is provided on this page. A PDF of this content is also available in through the ‘Save PDF’ action button.
Type
Correspondence
Information
Journal of Glaciology , Volume 6 , Issue 45 , 1966 , pp. 465
Copyright
Copyright © International Glaciological Society 1966

The Editor, Journal of Glaciology

Sir,

It would be interesting to make direct measurements of the direction of ice flow in the region Reference ShumskiyDr. Shumskiy describes (1966). I gather this has not been done, but if the ice should turn out to be flowing due north I should be only too glad to concede Dr. Shumskiy’s point. The surface strain-rates in this region would then be of great interest.

I am content to leave the other points to the judgement of your readers.

References

Shumskiy, P. A. 1966. Theory of glacier variations; reply to Dr. Nye’s letter. Journal of Glaciology, Vol. 6, No. 44, p. 319. [Letter.]Google Scholar