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