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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ftdartmouthcoll:oai:digitalcommons.dartmouth.edu:facoa-1463 2023-07-16T03:58:33+02:00 Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska Campbell, Seth Roy, Samuel Kreutz, Karl Arcone, Steven A Osterberg, Erich C Koons, Peter 2013-01-01T08:00:00Z https://digitalcommons.dartmouth.edu/facoa/461 https://doi.org/10.3189/2013AoG63A266 unknown Dartmouth Digital Commons https://digitalcommons.dartmouth.edu/facoa/461 doi:10.3189/2013AoG63A266 https://doi.org/10.3189/2013AoG63A266 Dartmouth Scholarship Earth Sciences Glaciology Physical Sciences and Mathematics text 2013 ftdartmouthcoll https://doi.org/10.3189/2013AoG63A266 2023-06-28T10:40:09Z 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 and near an ice divide. Surface-conformable stratigraphy, the glacier’s small size, and cold temperatures argue for limited rheological variability at this site. Surface ice-flow velocities of (1.2–15.5) ???????? 0.472 m a–1 imply classic saddle flow surrounding the ice divide. Numerical models that incorporate field-observed boundary conditions suggest extensional strain rates of 0.003–0.015 a–1, which fall within the published estimates required for crevasse initiation. The occurrence of one crevasse beginning at 50 m depth that appears to penetrate close to the bed suggests that it formed at depth. Field data and numerical models indicate that a higher interior stress at this crevasse location may be associated with steep convex bed topography; however, the dynamics that caused its formation are not entirely clear. Text glacier Alaska Dartmouth Digital Commons (Dartmouth College) Mount Hunter ENVELOPE(-62.400,-62.400,-64.083,-64.083) Annals of Glaciology 54 63 200 208 |
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Open Polar |
collection |
Dartmouth Digital Commons (Dartmouth College) |
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ftdartmouthcoll |
language |
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topic |
Earth Sciences Glaciology Physical Sciences and Mathematics |
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Earth Sciences Glaciology Physical Sciences and Mathematics Campbell, Seth Roy, Samuel Kreutz, Karl Arcone, Steven A Osterberg, Erich C Koons, Peter Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska |
topic_facet |
Earth Sciences Glaciology Physical Sciences and Mathematics |
description |
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 and near an ice divide. Surface-conformable stratigraphy, the glacier’s small size, and cold temperatures argue for limited rheological variability at this site. Surface ice-flow velocities of (1.2–15.5) ???????? 0.472 m a–1 imply classic saddle flow surrounding the ice divide. Numerical models that incorporate field-observed boundary conditions suggest extensional strain rates of 0.003–0.015 a–1, which fall within the published estimates required for crevasse initiation. The occurrence of one crevasse beginning at 50 m depth that appears to penetrate close to the bed suggests that it formed at depth. Field data and numerical models indicate that a higher interior stress at this crevasse location may be associated with steep convex bed topography; however, the dynamics that caused its formation are not entirely clear. |
format |
Text |
author |
Campbell, Seth Roy, Samuel Kreutz, Karl Arcone, Steven A Osterberg, Erich C Koons, Peter |
author_facet |
Campbell, Seth Roy, Samuel Kreutz, Karl Arcone, Steven A Osterberg, Erich C Koons, Peter |
author_sort |
Campbell, Seth |
title |
Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska |
title_short |
Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska |
title_full |
Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska |
title_fullStr |
Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska |
title_full_unstemmed |
Strain-rate estimates for crevasse formation at an alpine ice divide: Mount Hunter, Alaska |
title_sort |
strain-rate estimates for crevasse formation at an alpine ice divide: mount hunter, alaska |
publisher |
Dartmouth Digital Commons |
publishDate |
2013 |
url |
https://digitalcommons.dartmouth.edu/facoa/461 https://doi.org/10.3189/2013AoG63A266 |
long_lat |
ENVELOPE(-62.400,-62.400,-64.083,-64.083) |
geographic |
Mount Hunter |
geographic_facet |
Mount Hunter |
genre |
glacier Alaska |
genre_facet |
glacier Alaska |
op_source |
Dartmouth Scholarship |
op_relation |
https://digitalcommons.dartmouth.edu/facoa/461 doi:10.3189/2013AoG63A266 https://doi.org/10.3189/2013AoG63A266 |
op_doi |
https://doi.org/10.3189/2013AoG63A266 |
container_title |
Annals of Glaciology |
container_volume |
54 |
container_issue |
63 |
container_start_page |
200 |
op_container_end_page |
208 |
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1771545705845882880 |