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...
Published in: | Annals of Glaciology |
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Main Authors: | , , , , , |
Format: | Text |
Language: | unknown |
Published: |
Dartmouth Digital Commons
2013
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Subjects: | |
Online Access: | https://digitalcommons.dartmouth.edu/facoa/461 https://doi.org/10.3189/2013AoG63A266 |