Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A.
Abstract Modes of formation and rates of collapse have been determined for kame terraces and a fan delta in the Adams Inlet area, Alaska. The hummocky and trenched surface of the kame terrace develops by mass-wasting processes caused by differential melting of buried ice. The dry channels in the col...
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Language: | English |
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Cambridge University Press (CUP)
1987
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Online Access: | http://dx.doi.org/10.1017/s0022143000005347 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005347 |
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crcambridgeupr:10.1017/s0022143000005347 2024-09-30T14:37:51+00:00 Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A. McKenzie, Garry. D Goodwin, Robert G 1987 http://dx.doi.org/10.1017/s0022143000005347 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005347 en eng Cambridge University Press (CUP) Journal of Glaciology volume 33, issue 113, page 55-59 ISSN 0022-1430 1727-5652 journal-article 1987 crcambridgeupr https://doi.org/10.1017/s0022143000005347 2024-09-18T04:03:41Z Abstract Modes of formation and rates of collapse have been determined for kame terraces and a fan delta in the Adams Inlet area, Alaska. The hummocky and trenched surface of the kame terrace develops by mass-wasting processes caused by differential melting of buried ice. The dry channels in the collapsed part of the terrace are formed by melt water during stagnant-ice bursts. Measurements over a period of 17 years indicate that terrace back-wasting averages 4.3 m a −1 . The fan delta is forming near sea-level by streams that derive part of their load from the kame terrace. The fan delta seaward of the retreating kame terrace is undergoing partial collapse to produce kettles ringed by concentric fractures. Vegetation, now as much as 5 m below high tide, suggests a fan-delta collapse rate of about 0.5 m a −1 . Article in Journal/Newspaper Journal of Glaciology Alaska Cambridge University Press Journal of Glaciology 33 113 55 59 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Modes of formation and rates of collapse have been determined for kame terraces and a fan delta in the Adams Inlet area, Alaska. The hummocky and trenched surface of the kame terrace develops by mass-wasting processes caused by differential melting of buried ice. The dry channels in the collapsed part of the terrace are formed by melt water during stagnant-ice bursts. Measurements over a period of 17 years indicate that terrace back-wasting averages 4.3 m a −1 . The fan delta is forming near sea-level by streams that derive part of their load from the kame terrace. The fan delta seaward of the retreating kame terrace is undergoing partial collapse to produce kettles ringed by concentric fractures. Vegetation, now as much as 5 m below high tide, suggests a fan-delta collapse rate of about 0.5 m a −1 . |
format |
Article in Journal/Newspaper |
author |
McKenzie, Garry. D Goodwin, Robert G |
spellingShingle |
McKenzie, Garry. D Goodwin, Robert G Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A. |
author_facet |
McKenzie, Garry. D Goodwin, Robert G |
author_sort |
McKenzie, Garry. D |
title |
Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A. |
title_short |
Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A. |
title_full |
Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A. |
title_fullStr |
Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A. |
title_full_unstemmed |
Development of Collapsed Glacial Topography in the Adams Inlet Area, Alaska, U.S.A. |
title_sort |
development of collapsed glacial topography in the adams inlet area, alaska, u.s.a. |
publisher |
Cambridge University Press (CUP) |
publishDate |
1987 |
url |
http://dx.doi.org/10.1017/s0022143000005347 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005347 |
genre |
Journal of Glaciology Alaska |
genre_facet |
Journal of Glaciology Alaska |
op_source |
Journal of Glaciology volume 33, issue 113, page 55-59 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000005347 |
container_title |
Journal of Glaciology |
container_volume |
33 |
container_issue |
113 |
container_start_page |
55 |
op_container_end_page |
59 |
_version_ |
1811640632700043264 |