Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A.
Abstract Mount Redoubt, a volcano located west of Cook Inlet in Alaska, erupted from 1966 to 1968. This eruptive cycle removed about 6 × 10 7 m 3 of glacier ice from the upper part of Drift Glacier and decoupled it from the lower part during a sequence of jökulhlaups which originated in the Summit C...
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Cambridge University Press (CUP)
1986
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Online Access: | http://dx.doi.org/10.1017/s002214300001203x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001203X |
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crcambridgeupr:10.1017/s002214300001203x 2024-03-03T08:44:33+00:00 Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A. Sturm, Matthew Benson, Carl MacKeith, Peter 1986 http://dx.doi.org/10.1017/s002214300001203x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001203X en eng Cambridge University Press (CUP) Journal of Glaciology volume 32, issue 112, page 355-362 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1986 crcambridgeupr https://doi.org/10.1017/s002214300001203x 2024-02-08T08:40:37Z Abstract Mount Redoubt, a volcano located west of Cook Inlet in Alaska, erupted from 1966 to 1968. This eruptive cycle removed about 6 × 10 7 m 3 of glacier ice from the upper part of Drift Glacier and decoupled it from the lower part during a sequence of jökulhlaups which originated in the Summit Crater and flooded Drift River. The same events blanketed the lower part of the glacier with sand and ash, reducing ice ablation. Normal snowfall, augmented by intense avalanching, regenerated the upper part of the glacier by 1976, 8 years after the eruptions. When the regenerated glacier connected with the rest of Drift Glacier, it triggered a kinematic wave of thickening ice accompanied by accelerating surface velocities in the lower part of the glacier. Surface velocities increased by an order of magnitude and were accompanied by thickening of 70 m or more. At the same time, parts of the upper glacier thinned 70 m. The glacier appears to be returning to its pre-eruption equilibrium condition. Article in Journal/Newspaper glacier Journal of Glaciology Alaska Cambridge University Press Drift River ENVELOPE(-97.082,-97.082,58.222,58.222) Journal of Glaciology 32 112 355 362 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Sturm, Matthew Benson, Carl MacKeith, Peter Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A. |
topic_facet |
Earth-Surface Processes |
description |
Abstract Mount Redoubt, a volcano located west of Cook Inlet in Alaska, erupted from 1966 to 1968. This eruptive cycle removed about 6 × 10 7 m 3 of glacier ice from the upper part of Drift Glacier and decoupled it from the lower part during a sequence of jökulhlaups which originated in the Summit Crater and flooded Drift River. The same events blanketed the lower part of the glacier with sand and ash, reducing ice ablation. Normal snowfall, augmented by intense avalanching, regenerated the upper part of the glacier by 1976, 8 years after the eruptions. When the regenerated glacier connected with the rest of Drift Glacier, it triggered a kinematic wave of thickening ice accompanied by accelerating surface velocities in the lower part of the glacier. Surface velocities increased by an order of magnitude and were accompanied by thickening of 70 m or more. At the same time, parts of the upper glacier thinned 70 m. The glacier appears to be returning to its pre-eruption equilibrium condition. |
format |
Article in Journal/Newspaper |
author |
Sturm, Matthew Benson, Carl MacKeith, Peter |
author_facet |
Sturm, Matthew Benson, Carl MacKeith, Peter |
author_sort |
Sturm, Matthew |
title |
Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A. |
title_short |
Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A. |
title_full |
Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A. |
title_fullStr |
Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A. |
title_full_unstemmed |
Effects of the 1966–68 Eruptions of Mount Redoubt on the Flow of Drift Glacier, Alaska, U.S.A. |
title_sort |
effects of the 1966–68 eruptions of mount redoubt on the flow of drift glacier, alaska, u.s.a. |
publisher |
Cambridge University Press (CUP) |
publishDate |
1986 |
url |
http://dx.doi.org/10.1017/s002214300001203x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001203X |
long_lat |
ENVELOPE(-97.082,-97.082,58.222,58.222) |
geographic |
Drift River |
geographic_facet |
Drift River |
genre |
glacier Journal of Glaciology Alaska |
genre_facet |
glacier Journal of Glaciology Alaska |
op_source |
Journal of Glaciology volume 32, issue 112, page 355-362 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s002214300001203x |
container_title |
Journal of Glaciology |
container_volume |
32 |
container_issue |
112 |
container_start_page |
355 |
op_container_end_page |
362 |
_version_ |
1792500043713871872 |