Hostname: page-component-7b7567c8c-2n9c9 Total loading time: 0 Render date: 2026-11-14T16:40:34.176Z Has data issue: false hasContentIssue false
  • English
  • Français

Eyjabakkajökull

Published online by Cambridge University Press:  30 January 2017

W. V. Lewns
W. V. Lewns*
Affiliation:
Department of Geography, Cambridge
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.

Information

Type
Correspondence
Information
Journal of Glaciology , Volume 1 , Issue 9 , 1951, pp. 503
Copyright
Copyright © International Glaciological Society 1951

Sir,

In the discussion on the The Origin of Glacial Drifts (Journal of Glaciology, Vol. 1, No. 8, 1950, p. 435) I suggested that the date of the readvance of Eyjabakkajökull, which caused the interesting folds in the moraine, was either 1750–60 or 1840–50. My reason was that these were the dates of two very well marked advances of the glaciers in Iceland.

Mr. J. N. Jennings has since very kindly drawn my attention to a reference by Th. Thoroddsen (Island, Grundriss der Geographie und Geologie, p. 199) giving the date of the Eyjabakkajökull advance as 1889–90, with which I am fully prepared to agree.