Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion
In the middle of last century, Agassiz, Tyndall and others showed that a glacier flowed faster at its centre than at its margin. Partly from experiments and partly from the assumption that it behaved like a river, it became generally accepted that it also flowed faster at the surface than lower down...
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Language: | English |
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Cambridge University Press (CUP)
1947
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Online Access: | http://dx.doi.org/10.1017/s0022143000001088 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001088 |
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crcambridgeupr:10.1017/s0022143000001088 2024-03-03T08:46:09+00:00 Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion Seligman, G. 1947 http://dx.doi.org/10.1017/s0022143000001088 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001088 en eng Cambridge University Press (CUP) Journal of Glaciology volume 1, issue 01, page 12-21 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1947 crcambridgeupr https://doi.org/10.1017/s0022143000001088 2024-02-08T08:38:15Z In the middle of last century, Agassiz, Tyndall and others showed that a glacier flowed faster at its centre than at its margin. Partly from experiments and partly from the assumption that it behaved like a river, it became generally accepted that it also flowed faster at the surface than lower down. This belief was held until ten or fifteen years ago although search through earlier literature shows that evidence was accumulating which might disprove this. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 1 01 12 21 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Seligman, G. Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion |
topic_facet |
Earth-Surface Processes |
description |
In the middle of last century, Agassiz, Tyndall and others showed that a glacier flowed faster at its centre than at its margin. Partly from experiments and partly from the assumption that it behaved like a river, it became generally accepted that it also flowed faster at the surface than lower down. This belief was held until ten or fifteen years ago although search through earlier literature shows that evidence was accumulating which might disprove this. |
format |
Article in Journal/Newspaper |
author |
Seligman, G. |
author_facet |
Seligman, G. |
author_sort |
Seligman, G. |
title |
Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion |
title_short |
Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion |
title_full |
Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion |
title_fullStr |
Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion |
title_full_unstemmed |
Extrusion Flow in Glaciers: A description of tests to prove the hypothesis and some details regarding its influence on glacial erosion |
title_sort |
extrusion flow in glaciers: a description of tests to prove the hypothesis and some details regarding its influence on glacial erosion |
publisher |
Cambridge University Press (CUP) |
publishDate |
1947 |
url |
http://dx.doi.org/10.1017/s0022143000001088 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001088 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 1, issue 01, page 12-21 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000001088 |
container_title |
Journal of Glaciology |
container_volume |
1 |
container_issue |
01 |
container_start_page |
12 |
op_container_end_page |
21 |
_version_ |
1792502127615016960 |