Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps
Abstract Photogrammetric measurements of surface movement, 1981–94, on the Muragl glacier forefield (Swiss Alps) are compared to direct current resistivity surveys for the same area. At three locations isolated patches of frozen sediments were inferred, each about 10,000–20,000 m 2 in area. These we...
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crwiley:10.1002/ppp.540 2024-09-15T18:11:34+00:00 Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps Kääb, A. Kneisel, C. 2005 http://dx.doi.org/10.1002/ppp.540 http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.540 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.540 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 17, issue 1, page 79-85 ISSN 1045-6740 1099-1530 journal-article 2005 crwiley https://doi.org/10.1002/ppp.540 2024-08-22T04:17:11Z Abstract Photogrammetric measurements of surface movement, 1981–94, on the Muragl glacier forefield (Swiss Alps) are compared to direct current resistivity surveys for the same area. At three locations isolated patches of frozen sediments were inferred, each about 10,000–20,000 m 2 in area. These were deforming at surface velocities of up to 50 cm per year. The locations where creep was observed coincide well with areas where two‐dimensional (2D) resistivity surveys suggest ice is present within the ground. Copyright © 2005 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 17 1 79 85 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Photogrammetric measurements of surface movement, 1981–94, on the Muragl glacier forefield (Swiss Alps) are compared to direct current resistivity surveys for the same area. At three locations isolated patches of frozen sediments were inferred, each about 10,000–20,000 m 2 in area. These were deforming at surface velocities of up to 50 cm per year. The locations where creep was observed coincide well with areas where two‐dimensional (2D) resistivity surveys suggest ice is present within the ground. Copyright © 2005 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Kääb, A. Kneisel, C. |
spellingShingle |
Kääb, A. Kneisel, C. Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps |
author_facet |
Kääb, A. Kneisel, C. |
author_sort |
Kääb, A. |
title |
Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps |
title_short |
Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps |
title_full |
Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps |
title_fullStr |
Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps |
title_full_unstemmed |
Permafrost creep within a recently deglaciated glacier forefield: Muragl, Swiss Alps |
title_sort |
permafrost creep within a recently deglaciated glacier forefield: muragl, swiss alps |
publisher |
Wiley |
publishDate |
2005 |
url |
http://dx.doi.org/10.1002/ppp.540 http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.540 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.540 |
genre |
Ice permafrost Permafrost and Periglacial Processes |
genre_facet |
Ice permafrost Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 17, issue 1, page 79-85 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.540 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
17 |
container_issue |
1 |
container_start_page |
79 |
op_container_end_page |
85 |
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1810449165094748160 |