Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska
The hundredfold speedup in glacier motion in a surge of the kind that took place in Variegated Glacier in 1982-1983 is caused by the buildup of high water pressure in the basal passageway system, which is made possible by a fundamental and pervasive change in the geometry and water-transport charact...
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American Association for the Advancement of Science (AAAS)
1985
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Online Access: | http://dx.doi.org/10.1126/science.227.4686.469 https://www.science.org/doi/pdf/10.1126/science.227.4686.469 |
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craaas:10.1126/science.227.4686.469 2024-09-15T18:07:31+00:00 Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska Kamb, Barclay Raymond, C. F. Harrison, W. D. Engelhardt, Hermann Echelmeyer, K. A. Humphrey, N. Brugman, M. M. Pfeffer, T. 1985 http://dx.doi.org/10.1126/science.227.4686.469 https://www.science.org/doi/pdf/10.1126/science.227.4686.469 en eng American Association for the Advancement of Science (AAAS) Science volume 227, issue 4686, page 469-479 ISSN 0036-8075 1095-9203 journal-article 1985 craaas https://doi.org/10.1126/science.227.4686.469 2024-08-29T04:01:01Z The hundredfold speedup in glacier motion in a surge of the kind that took place in Variegated Glacier in 1982-1983 is caused by the buildup of high water pressure in the basal passageway system, which is made possible by a fundamental and pervasive change in the geometry and water-transport characteristics of this system. The behavior of the glacier in surge has many remarkable features, which can provide clues to a detailed theory of the surging process. The surge mechanism is akin to a proposed mechanism of overthrust faulting. Article in Journal/Newspaper glacier Alaska AAAS Resource Center (American Association for the Advancement of Science) Science 227 4686 469 479 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
The hundredfold speedup in glacier motion in a surge of the kind that took place in Variegated Glacier in 1982-1983 is caused by the buildup of high water pressure in the basal passageway system, which is made possible by a fundamental and pervasive change in the geometry and water-transport characteristics of this system. The behavior of the glacier in surge has many remarkable features, which can provide clues to a detailed theory of the surging process. The surge mechanism is akin to a proposed mechanism of overthrust faulting. |
format |
Article in Journal/Newspaper |
author |
Kamb, Barclay Raymond, C. F. Harrison, W. D. Engelhardt, Hermann Echelmeyer, K. A. Humphrey, N. Brugman, M. M. Pfeffer, T. |
spellingShingle |
Kamb, Barclay Raymond, C. F. Harrison, W. D. Engelhardt, Hermann Echelmeyer, K. A. Humphrey, N. Brugman, M. M. Pfeffer, T. Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska |
author_facet |
Kamb, Barclay Raymond, C. F. Harrison, W. D. Engelhardt, Hermann Echelmeyer, K. A. Humphrey, N. Brugman, M. M. Pfeffer, T. |
author_sort |
Kamb, Barclay |
title |
Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska |
title_short |
Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska |
title_full |
Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska |
title_fullStr |
Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska |
title_full_unstemmed |
Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, Alaska |
title_sort |
glacier surge mechanism: 1982-1983 surge of variegated glacier, alaska |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1985 |
url |
http://dx.doi.org/10.1126/science.227.4686.469 https://www.science.org/doi/pdf/10.1126/science.227.4686.469 |
genre |
glacier Alaska |
genre_facet |
glacier Alaska |
op_source |
Science volume 227, issue 4686, page 469-479 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.227.4686.469 |
container_title |
Science |
container_volume |
227 |
container_issue |
4686 |
container_start_page |
469 |
op_container_end_page |
479 |
_version_ |
1810444901081415680 |