Submarine evidence of glacier surges
Surges constitute a common form of glacier advance on the Svalbard archipelago (Liestd 1969), northwestern Barents Sea. The Austfonna ice cap (8100 km2) covers most of Nordaustlandet, the second largest island in the archipelago (Fig. 1). It has its entire southern and eastern front grounded in the...
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Norwegian Polar Institute
1986
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ftjpolarres:oai:journals.openacademia.net:article/2497 2023-05-15T15:33:55+02:00 Submarine evidence of glacier surges Solheim, Anders 1986-01-05 application/pdf https://polarresearch.net/index.php/polar/article/view/2497 https://doi.org/10.3402/polar.v4i1.6925 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2497/5748 https://polarresearch.net/index.php/polar/article/view/2497 doi:10.3402/polar.v4i1.6925 Copyright (c) 2018 Polar Research Polar Research; Vol. 4 No. 1 (1986); 91-95 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1986 ftjpolarres https://doi.org/10.3402/polar.v4i1.6925 2021-11-11T19:12:43Z Surges constitute a common form of glacier advance on the Svalbard archipelago (Liestd 1969), northwestern Barents Sea. The Austfonna ice cap (8100 km2) covers most of Nordaustlandet, the second largest island in the archipelago (Fig. 1). It has its entire southern and eastern front grounded in the sea under open, marine conditions. Between 1937 and 1938 the Brdsvellbreen glacier, which is part of the Austfonna ice cap, had a major surge which is well documented from aerial photography (Hoe1 & Werenskiold 1962: 73-74; Schytt 1969). Since 1938, the glacier has retreated several kilometres. Article in Journal/Newspaper Austfonna Barents Sea glacier Ice cap Nordaustlandet Polar Research Svalbard Polar Research (E-Journal) Svalbard Barents Sea Svalbard Archipelago Nordaustlandet ENVELOPE(22.400,22.400,79.800,79.800) Austfonna ENVELOPE(24.559,24.559,79.835,79.835) Polar Research 4 1 91 95 |
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Open Polar |
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Polar Research (E-Journal) |
op_collection_id |
ftjpolarres |
language |
English |
description |
Surges constitute a common form of glacier advance on the Svalbard archipelago (Liestd 1969), northwestern Barents Sea. The Austfonna ice cap (8100 km2) covers most of Nordaustlandet, the second largest island in the archipelago (Fig. 1). It has its entire southern and eastern front grounded in the sea under open, marine conditions. Between 1937 and 1938 the Brdsvellbreen glacier, which is part of the Austfonna ice cap, had a major surge which is well documented from aerial photography (Hoe1 & Werenskiold 1962: 73-74; Schytt 1969). Since 1938, the glacier has retreated several kilometres. |
format |
Article in Journal/Newspaper |
author |
Solheim, Anders |
spellingShingle |
Solheim, Anders Submarine evidence of glacier surges |
author_facet |
Solheim, Anders |
author_sort |
Solheim, Anders |
title |
Submarine evidence of glacier surges |
title_short |
Submarine evidence of glacier surges |
title_full |
Submarine evidence of glacier surges |
title_fullStr |
Submarine evidence of glacier surges |
title_full_unstemmed |
Submarine evidence of glacier surges |
title_sort |
submarine evidence of glacier surges |
publisher |
Norwegian Polar Institute |
publishDate |
1986 |
url |
https://polarresearch.net/index.php/polar/article/view/2497 https://doi.org/10.3402/polar.v4i1.6925 |
long_lat |
ENVELOPE(22.400,22.400,79.800,79.800) ENVELOPE(24.559,24.559,79.835,79.835) |
geographic |
Svalbard Barents Sea Svalbard Archipelago Nordaustlandet Austfonna |
geographic_facet |
Svalbard Barents Sea Svalbard Archipelago Nordaustlandet Austfonna |
genre |
Austfonna Barents Sea glacier Ice cap Nordaustlandet Polar Research Svalbard |
genre_facet |
Austfonna Barents Sea glacier Ice cap Nordaustlandet Polar Research Svalbard |
op_source |
Polar Research; Vol. 4 No. 1 (1986); 91-95 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/2497/5748 https://polarresearch.net/index.php/polar/article/view/2497 doi:10.3402/polar.v4i1.6925 |
op_rights |
Copyright (c) 2018 Polar Research |
op_doi |
https://doi.org/10.3402/polar.v4i1.6925 |
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Polar Research |
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4 |
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1 |
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91 |
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95 |
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1766364502811475968 |