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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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Carter, Adams, Atherton, David
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1961
Subjects:
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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spelling 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
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