Milton Mt. Mckinley Range Expedition, 1960
Abstract The paper describes the expedition’s work on the north fork of the Eldridge Glacier, which is found to be of the temperate alpine type. Velocity profiles show both slip at the glacier’s edge and shear in the adjacent layers. A summer accumulation pattern is demonstrated which makes the glac...
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Language: | English |
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Cambridge University Press (CUP)
1961
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Online Access: | http://dx.doi.org/10.1017/s0022143000017536 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017536 |
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crcambridgeupr:10.1017/s0022143000017536 2024-03-03T08:46:06+00:00 Milton Mt. Mckinley Range Expedition, 1960 Carter, Adams Atherton, David 1961 http://dx.doi.org/10.1017/s0022143000017536 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017536 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 30, page 1123-1132 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1961 crcambridgeupr https://doi.org/10.1017/s0022143000017536 2024-02-08T08:37:11Z Abstract The paper describes the expedition’s work on the north fork of the Eldridge Glacier, which is found to be of the temperate alpine type. Velocity profiles show both slip at the glacier’s edge and shear in the adjacent layers. A summer accumulation pattern is demonstrated which makes the glacial balance unusually delicate. It is concluded that glaciers in this region are near their recent maxima because the high altitude accumulation offsets the shrinking of the lower tributary glaciers. Examination of an ice-dammed lake shows the main Eldridge Glacier to be near the maximum of the last major advance which raised the level of the ice at least 60 m. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Milton ENVELOPE(-84.800,-84.800,-78.800,-78.800) Dammed Lake ENVELOPE(-68.258,-68.258,68.496,68.496) North Fork ENVELOPE(161.250,161.250,-77.533,-77.533) Journal of Glaciology 3 30 1123 1132 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Carter, Adams Atherton, David Milton Mt. Mckinley Range Expedition, 1960 |
topic_facet |
Earth-Surface Processes |
description |
Abstract The paper describes the expedition’s work on the north fork of the Eldridge Glacier, which is found to be of the temperate alpine type. Velocity profiles show both slip at the glacier’s edge and shear in the adjacent layers. A summer accumulation pattern is demonstrated which makes the glacial balance unusually delicate. It is concluded that glaciers in this region are near their recent maxima because the high altitude accumulation offsets the shrinking of the lower tributary glaciers. Examination of an ice-dammed lake shows the main Eldridge Glacier to be near the maximum of the last major advance which raised the level of the ice at least 60 m. |
format |
Article in Journal/Newspaper |
author |
Carter, Adams Atherton, David |
author_facet |
Carter, Adams Atherton, David |
author_sort |
Carter, Adams |
title |
Milton Mt. Mckinley Range Expedition, 1960 |
title_short |
Milton Mt. Mckinley Range Expedition, 1960 |
title_full |
Milton Mt. Mckinley Range Expedition, 1960 |
title_fullStr |
Milton Mt. Mckinley Range Expedition, 1960 |
title_full_unstemmed |
Milton Mt. Mckinley Range Expedition, 1960 |
title_sort |
milton mt. mckinley range expedition, 1960 |
publisher |
Cambridge University Press (CUP) |
publishDate |
1961 |
url |
http://dx.doi.org/10.1017/s0022143000017536 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017536 |
long_lat |
ENVELOPE(-84.800,-84.800,-78.800,-78.800) ENVELOPE(-68.258,-68.258,68.496,68.496) ENVELOPE(161.250,161.250,-77.533,-77.533) |
geographic |
Milton Dammed Lake North Fork |
geographic_facet |
Milton Dammed Lake North Fork |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 3, issue 30, page 1123-1132 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000017536 |
container_title |
Journal of Glaciology |
container_volume |
3 |
container_issue |
30 |
container_start_page |
1123 |
op_container_end_page |
1132 |
_version_ |
1792501994864246784 |