Mechanical and hydrologic basis for the rapid motion of a large tidewater glacier 2. Interpretation
The data presented in part 1 of this paper (Meier et al., this issue) are here used to assess the role of water input/output, water storage, and basal water pressure in the rapid movement of Columbia Glacier, Alaska. Consistently high basal water pressures, mostly in the range from 300 kPa below to...
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
1994
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Subjects: | |
Online Access: | https://doi.org/10.1029/94JB00467 |