A Mechanism of Basal Ice-Layer Formation Involving Major Ice-Fabric Changes

Abstract An opportunity to analyse the mechanism for the formation of a basal ice layer was provided by Glacier de Tsanfleuron in the Swiss Alps. This glacier has some lateral subglacial cavities in which a basal ice layer forms on the bedrock floor and is subsequently incorporated at the base of th...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Tison, J.-L., Lorrain, R.D.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1987
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000005323
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005323
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Summary:Abstract An opportunity to analyse the mechanism for the formation of a basal ice layer was provided by Glacier de Tsanfleuron in the Swiss Alps. This glacier has some lateral subglacial cavities in which a basal ice layer forms on the bedrock floor and is subsequently incorporated at the base of the glacier. Petrographic and crystallographic analyses of the different types of ice have provided a means of investigating the successive stages of the process. These analyses show major structural changes which provide field confirmation of the deformation mechanisms studied by several authors in laboratory experiments.