Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada
Abstract “Avalanche-type” medial moraines are described on four Torngat Mountains glaciers with single, rather than compound, firn basins. They form from debris avalanching down couloirs and are exposed by ice melt to form extensive debris covers on glacier snouts in the Torngat Mountains. The debri...
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Language: | English |
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Cambridge University Press (CUP)
1986
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Online Access: | http://dx.doi.org/10.1017/s0022143000012028 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012028 |
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crcambridgeupr:10.1017/s0022143000012028 2024-03-03T08:44:40+00:00 Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada Rogerson, R.J. Olson, M.E. Branson, D. 1986 http://dx.doi.org/10.1017/s0022143000012028 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012028 en eng Cambridge University Press (CUP) Journal of Glaciology volume 32, issue 112, page 350-354 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1986 crcambridgeupr https://doi.org/10.1017/s0022143000012028 2024-02-08T08:34:04Z Abstract “Avalanche-type” medial moraines are described on four Torngat Mountains glaciers with single, rather than compound, firn basins. They form from debris avalanching down couloirs and are exposed by ice melt to form extensive debris covers on glacier snouts in the Torngat Mountains. The debris may play an important part in helping the glacier survive periods with warm summers and/or dry winters since, in the Torngat Mountains, average ice melt on debris-covered sites is approximately one-third that on exposed ice. Article in Journal/Newspaper glacier* Journal of Glaciology Cambridge University Press Canada Torngat Mountains ENVELOPE(-63.665,-63.665,59.000,59.000) Journal of Glaciology 32 112 350 354 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Rogerson, R.J. Olson, M.E. Branson, D. Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada |
topic_facet |
Earth-Surface Processes |
description |
Abstract “Avalanche-type” medial moraines are described on four Torngat Mountains glaciers with single, rather than compound, firn basins. They form from debris avalanching down couloirs and are exposed by ice melt to form extensive debris covers on glacier snouts in the Torngat Mountains. The debris may play an important part in helping the glacier survive periods with warm summers and/or dry winters since, in the Torngat Mountains, average ice melt on debris-covered sites is approximately one-third that on exposed ice. |
format |
Article in Journal/Newspaper |
author |
Rogerson, R.J. Olson, M.E. Branson, D. |
author_facet |
Rogerson, R.J. Olson, M.E. Branson, D. |
author_sort |
Rogerson, R.J. |
title |
Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada |
title_short |
Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada |
title_full |
Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada |
title_fullStr |
Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada |
title_full_unstemmed |
Medial Moraines and Surface Melt on Glaciers of the Torngat Mountains, Northern Labrador, Canada |
title_sort |
medial moraines and surface melt on glaciers of the torngat mountains, northern labrador, canada |
publisher |
Cambridge University Press (CUP) |
publishDate |
1986 |
url |
http://dx.doi.org/10.1017/s0022143000012028 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012028 |
long_lat |
ENVELOPE(-63.665,-63.665,59.000,59.000) |
geographic |
Canada Torngat Mountains |
geographic_facet |
Canada Torngat Mountains |
genre |
glacier* Journal of Glaciology |
genre_facet |
glacier* Journal of Glaciology |
op_source |
Journal of Glaciology volume 32, issue 112, page 350-354 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000012028 |
container_title |
Journal of Glaciology |
container_volume |
32 |
container_issue |
112 |
container_start_page |
350 |
op_container_end_page |
354 |
_version_ |
1792500156735684608 |