Bottom Crevasses in the Ross Ice Shelf
Bottom crevasses were detected at many locations in the southern portion of the Ross Ice Shelf during the 1973-74 austral summer. The crevasses which extended up about 100 m from the bottom of the shelf were detected by radio-echo sounding. These linear features were mapped in some detail at the RIS...
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Language: | English |
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Cambridge University Press (CUP)
1975
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Online Access: | http://dx.doi.org/10.1017/s0022143000034560 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034560 |
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crcambridgeupr:10.1017/s0022143000034560 2024-03-03T08:45:29+00:00 Bottom Crevasses in the Ross Ice Shelf Clough, John W. 1975 http://dx.doi.org/10.1017/s0022143000034560 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034560 en eng Cambridge University Press (CUP) Journal of Glaciology volume 15, issue 73, page 457-458 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000034560 2024-02-08T08:42:50Z Bottom crevasses were detected at many locations in the southern portion of the Ross Ice Shelf during the 1973-74 austral summer. The crevasses which extended up about 100 m from the bottom of the shelf were detected by radio-echo sounding. These linear features were mapped in some detail at the RISP Camp. Wide-angle reflection velocity measurements, airborne radio-echo sounding, and other results of the R1GGS program will be included in the discussion. Article in Journal/Newspaper Ice Shelf Journal of Glaciology Ross Ice Shelf Cambridge University Press Austral Ross Ice Shelf Journal of Glaciology 15 73 457 458 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Clough, John W. Bottom Crevasses in the Ross Ice Shelf |
topic_facet |
Earth-Surface Processes |
description |
Bottom crevasses were detected at many locations in the southern portion of the Ross Ice Shelf during the 1973-74 austral summer. The crevasses which extended up about 100 m from the bottom of the shelf were detected by radio-echo sounding. These linear features were mapped in some detail at the RISP Camp. Wide-angle reflection velocity measurements, airborne radio-echo sounding, and other results of the R1GGS program will be included in the discussion. |
format |
Article in Journal/Newspaper |
author |
Clough, John W. |
author_facet |
Clough, John W. |
author_sort |
Clough, John W. |
title |
Bottom Crevasses in the Ross Ice Shelf |
title_short |
Bottom Crevasses in the Ross Ice Shelf |
title_full |
Bottom Crevasses in the Ross Ice Shelf |
title_fullStr |
Bottom Crevasses in the Ross Ice Shelf |
title_full_unstemmed |
Bottom Crevasses in the Ross Ice Shelf |
title_sort |
bottom crevasses in the ross ice shelf |
publisher |
Cambridge University Press (CUP) |
publishDate |
1975 |
url |
http://dx.doi.org/10.1017/s0022143000034560 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034560 |
geographic |
Austral Ross Ice Shelf |
geographic_facet |
Austral Ross Ice Shelf |
genre |
Ice Shelf Journal of Glaciology Ross Ice Shelf |
genre_facet |
Ice Shelf Journal of Glaciology Ross Ice Shelf |
op_source |
Journal of Glaciology volume 15, issue 73, page 457-458 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000034560 |
container_title |
Journal of Glaciology |
container_volume |
15 |
container_issue |
73 |
container_start_page |
457 |
op_container_end_page |
458 |
_version_ |
1792501045404893184 |