Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska

Crevasse initiation is linked to strain rates that range over three orders of magnitude (0.001 and 0.163 a–1) as a result of the temperature-dependent nonlinear rheological properties of ice and from water and debris inclusions. Here we discuss a small cold glacier that contains buried crevasses at...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Campbell, Seth, Roy, Samuel, Kreutz, Karl, Arcone, Steven A, Osterberg, Erich C, Koons, Peter
Format: Text
Language:unknown
Published: Dartmouth Digital Commons 2013
Subjects:
Online Access:https://digitalcommons.dartmouth.edu/facoa/461
https://doi.org/10.3189/2013AoG63A266