On the Disintegration of Ice Shelves: The Role of Fracture
Abstract Crevasses can be ignored in studying the dynamics of most glaciers because they are only about 20 m deep, a small fraction of ice thickness. In ice shelves, however, surface crevasses 20 m deep often reach sea-level and bottom crevasses can move upward to sea-level (Clough, 1974; Weertman,...
| Published in: | Journal of Glaciology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1983
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| Online Access: | http://dx.doi.org/10.1017/s0022143000005177 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005177 |