A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams

The deformation and state of stress at the confluence of two glacier streams are analysed using the techniques of slip-line theory. The valley walls are taken to be vertical parallel planes and the deformation is supposed independent of depth. The mechanical behavior of ice is modeled by the ideal r...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Collins, I. F.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1970
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000023510
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023510