Ridges on Antarctic Ice Rises
Abstract Satellite pictures have revealed the presence of ridges on the summits of ice rises in Antarctica. Because ice does not exhibit a critical stress it is conclugerd that these ridges must be produced by a snow accumulation process rather than by ice gerformation. A sand-mogerl analogue has be...
| Published in: | Journal of Glaciology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1976
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s002214300003080x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003080X |
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crcambridgeupr:10.1017/s002214300003080x |
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openpolar |
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crcambridgeupr:10.1017/s002214300003080x 2024-03-03T08:37:57+00:00 Ridges on Antarctic Ice Rises Martin, P. J. 1976 http://dx.doi.org/10.1017/s002214300003080x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003080X en eng Cambridge University Press (CUP) Journal of Glaciology volume 17, issue 75, page 141-144 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s002214300003080x 2024-02-08T08:41:37Z Abstract Satellite pictures have revealed the presence of ridges on the summits of ice rises in Antarctica. Because ice does not exhibit a critical stress it is conclugerd that these ridges must be produced by a snow accumulation process rather than by ice gerformation. A sand-mogerl analogue has been used to simulate this behaviour. Article in Journal/Newspaper Antarc* Antarctic Antarctica Journal of Glaciology Cambridge University Press Antarctic Journal of Glaciology 17 75 141 144 |
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Open Polar |
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Cambridge University Press |
| op_collection_id |
crcambridgeupr |
| language |
English |
| topic |
Earth-Surface Processes |
| spellingShingle |
Earth-Surface Processes Martin, P. J. Ridges on Antarctic Ice Rises |
| topic_facet |
Earth-Surface Processes |
| description |
Abstract Satellite pictures have revealed the presence of ridges on the summits of ice rises in Antarctica. Because ice does not exhibit a critical stress it is conclugerd that these ridges must be produced by a snow accumulation process rather than by ice gerformation. A sand-mogerl analogue has been used to simulate this behaviour. |
| format |
Article in Journal/Newspaper |
| author |
Martin, P. J. |
| author_facet |
Martin, P. J. |
| author_sort |
Martin, P. J. |
| title |
Ridges on Antarctic Ice Rises |
| title_short |
Ridges on Antarctic Ice Rises |
| title_full |
Ridges on Antarctic Ice Rises |
| title_fullStr |
Ridges on Antarctic Ice Rises |
| title_full_unstemmed |
Ridges on Antarctic Ice Rises |
| title_sort |
ridges on antarctic ice rises |
| publisher |
Cambridge University Press (CUP) |
| publishDate |
1976 |
| url |
http://dx.doi.org/10.1017/s002214300003080x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003080X |
| geographic |
Antarctic |
| geographic_facet |
Antarctic |
| genre |
Antarc* Antarctic Antarctica Journal of Glaciology |
| genre_facet |
Antarc* Antarctic Antarctica Journal of Glaciology |
| op_source |
Journal of Glaciology volume 17, issue 75, page 141-144 ISSN 0022-1430 1727-5652 |
| op_doi |
https://doi.org/10.1017/s002214300003080x |
| container_title |
Journal of Glaciology |
| container_volume |
17 |
| container_issue |
75 |
| container_start_page |
141 |
| op_container_end_page |
144 |
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1792502991322873856 |