Subsurface crevasse formation in glaciers and ice sheets

[1] Crevasses form in response to tensile stresses in glaciers and ice sheets. It has been widely assumed that crevasses initiate at, or near, the surface of the ice, from starter cracks up to a few centimeters long. If the tensile stress is sufficient, these cracks propagate downward into the ice t...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Nath, P.C., Vaughan, D.G.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2003
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/12810/
http://www.agu.org/journals/jb/jb0301/2001JB000453/