Snaefell, East Iceland
Abstract The morphology of Snaefell, East Iceland, and the state of its glaciers in 1937 are described. There are four small glaciers. Two of these exist in well-developed cirques incised into the lavas, tuffs and breccias of this Pleistocene volcano. The third receives ice from a summit ice cap, wh...
Published in: | Journal of Glaciology |
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Language: | English |
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Cambridge University Press (CUP)
1952
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Online Access: | http://dx.doi.org/10.1017/s0022143000034109 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034109 |
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crcambridgeupr:10.1017/s0022143000034109 2024-03-03T08:45:19+00:00 Snaefell, East Iceland Jennings, J. N. 1952 http://dx.doi.org/10.1017/s0022143000034109 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034109 en eng Cambridge University Press (CUP) Journal of Glaciology volume 2, issue 12, page 133-137 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1952 crcambridgeupr https://doi.org/10.1017/s0022143000034109 2024-02-08T08:38:15Z Abstract The morphology of Snaefell, East Iceland, and the state of its glaciers in 1937 are described. There are four small glaciers. Two of these exist in well-developed cirques incised into the lavas, tuffs and breccias of this Pleistocene volcano. The third receives ice from a summit ice cap, while the fourth also receives ice from the same source as well as lying in a cirque. The firn line in 1937 is put between 1350 and 1500 m. so that the mass balance of the glaciers is unlikely to have been favourable, although only one showed any abandoned moraines. An explanation of the varying glacial modification of the different slopes of Snaefell is suggested in terms of structural trends, shading from the sun and snow-drifting. Article in Journal/Newspaper Ice cap Iceland Journal of Glaciology Cambridge University Press Journal of Glaciology 2 12 133 137 |
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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 Jennings, J. N. Snaefell, East Iceland |
topic_facet |
Earth-Surface Processes |
description |
Abstract The morphology of Snaefell, East Iceland, and the state of its glaciers in 1937 are described. There are four small glaciers. Two of these exist in well-developed cirques incised into the lavas, tuffs and breccias of this Pleistocene volcano. The third receives ice from a summit ice cap, while the fourth also receives ice from the same source as well as lying in a cirque. The firn line in 1937 is put between 1350 and 1500 m. so that the mass balance of the glaciers is unlikely to have been favourable, although only one showed any abandoned moraines. An explanation of the varying glacial modification of the different slopes of Snaefell is suggested in terms of structural trends, shading from the sun and snow-drifting. |
format |
Article in Journal/Newspaper |
author |
Jennings, J. N. |
author_facet |
Jennings, J. N. |
author_sort |
Jennings, J. N. |
title |
Snaefell, East Iceland |
title_short |
Snaefell, East Iceland |
title_full |
Snaefell, East Iceland |
title_fullStr |
Snaefell, East Iceland |
title_full_unstemmed |
Snaefell, East Iceland |
title_sort |
snaefell, east iceland |
publisher |
Cambridge University Press (CUP) |
publishDate |
1952 |
url |
http://dx.doi.org/10.1017/s0022143000034109 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034109 |
genre |
Ice cap Iceland Journal of Glaciology |
genre_facet |
Ice cap Iceland Journal of Glaciology |
op_source |
Journal of Glaciology volume 2, issue 12, page 133-137 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000034109 |
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Journal of Glaciology |
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2 |
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12 |
container_start_page |
133 |
op_container_end_page |
137 |
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1792500849163894784 |