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...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Kamb, Barclay, Engelhardt, Hermann, Fahnestock, Mark, Humphrey, Neil, Meier, Mark, Stone, Dan
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 1994
Subjects:
Online Access:https://doi.org/10.1029/94JB00467