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Ground-ice wedges interpreted by A. von Bunge (1884) in Siberia

Published online by Cambridge University Press:  30 January 2017

André Cailleux
André Cailleux*
Affiliation:
Centre d'Études Nordiques, Université L aval, Québec 10e, Canada
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Abstract

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Type
Correspondence
Information
Journal of Glaciology , Volume 10 , Issue 60 , 1971 , pp. 410 - 411
Copyright
Copyright © International Glaciological Society 1971

Sir,

It is a good thing that Dr Colhoun has reminded us that as early as 1905-08 J. R. Kilroe interpreted an ice-wedge pseudomorph observed near Londonderry as having been formed when the sands and gravels that it cuts were frozen (Reference Colhoun,Colhoun, 1970).

Dr Colhoun has noted that Kilroe’s interpretation pre-dated “the classic interpretation of ground-ice wedges in Alaska published by (Reference Leffingwell,Leffingwell 1915, Reference Leffingwell,1919)”, which is true. But Leffingwell was by no means the first author to give the proper interpretation. Ice-wedges were first described from East Siberia by Reference Adams,Adams (1815) and Reference Middendorff,Middendorff (1867), and correctly interpreted by von Reference Bunge,Bunge (1884) on the basis of extremely careful field observations. This has been stressed by Reference Troll,Troll (1944) and myself (Reference Cailleux, and Taylor,Cailleux and Taylor, 1954).

References

Adams,, M.F. 1815. De skeleto mammonteo sibirico ad maris glacialis littora anno 1807 effosso. Mémoires de?’Académie Impériale des Sciences de St-Pétersbourg, Tom. 5, p. 406–55.Google Scholar
Bunge,, A. von. 1884. Naturhisorische Beobachtungen und Fahrten im Lena-Delta. Bulletin de l’AcadémieImpériale des Sciences de St-Pétersbourg, Tom. 29, p. 422–75.Google Scholar
Cailleux,, A., and Taylor,, G. 1954. Cryapédotogie: étude des sols gélés. Paris, Hermann. (Actualités Scientifiques etIndustrielles, 1203. Expéditions Polaires Françaises [Travaux], IV.)Google Scholar
Colhoun,, E.A. 1970. Early discoverers. XXIX. Early record and interpretation of ice-wedge pseudomorph in County Londonderry, Northern Ireland, by J. R. Kilroe. Journal of Glaciology, Vol. 9, No. 57, p. 391–92.Google Scholar
Leffingwell,, E. de K. 1915. Ground-ice wedges. The dominant form of ground-ice on the north coast of Alaska. Journal of Geology, Vol. 23, No. 7, p. 635–54.Google Scholar
Leffingwell,, E. de K. 1919. The Canning River region, northern Alaska. U.S. Geological Survey. Professional Paper 109.Google Scholar
Middendorff,, A.T. von. 1867. Reise in den äussersten norden und osten Sibiriens während der Jaltre 1843 und 1844. Bd. 4. Übersicht der Natur Nord- und Ost-Sibiriens. Theil 1. St. Petersburg. Buchdruckerei der Kaiserlichen Akademie der Wissenschaften.Google Scholar
Troll,, C. 1944. Strukturböden, Solifluktion und Froslklimate der Erde. Geologische Rundschau Bd 34 Ht. 7-8, p. 545–694.Google Scholar