Measurements of Side-slip at Austerdalsbreen, 1959

Abstract Measurements have been made using two different methods of the rate at which the glacier Austerdalsbreen is slipping past its side wall at four sites. The rate of slipping varies from site to site in a way which seems to be connected with the details of glacier flow in the neighbourhood, an...

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Published in:Journal of Glaciology
Main Authors: Glen, J. W., Lewis, W. V.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1961
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000017524
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017524
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spelling crcambridgeupr:10.1017/s0022143000017524 2024-03-03T08:46:06+00:00 Measurements of Side-slip at Austerdalsbreen, 1959 Glen, J. W. Lewis, W. V. 1961 http://dx.doi.org/10.1017/s0022143000017524 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017524 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 30, page 1109-1122 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1961 crcambridgeupr https://doi.org/10.1017/s0022143000017524 2024-02-08T08:36:15Z Abstract Measurements have been made using two different methods of the rate at which the glacier Austerdalsbreen is slipping past its side wall at four sites. The rate of slipping varies from site to site in a way which seems to be connected with the details of glacier flow in the neighbourhood, and in all cases is less than the slip previously measured further up-glacier at the foot of one of the ice falls, and is also a smaller fraction (about one sixth) of the flow rate in the centre of the glacier. One of the methods measured the velocity of the last metre of ice, and this method gave movements which were more erratic than the other method, which measured velocity a few metres from the edge. This suggests that protuberances of rock and boulders lodged between the ice and the rock wall cause local variations in flow which are smoothed out in a few metres. The results are discussed in connection with the process of glacial erosion. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 3 30 1109 1122
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Glen, J. W.
Lewis, W. V.
Measurements of Side-slip at Austerdalsbreen, 1959
topic_facet Earth-Surface Processes
description Abstract Measurements have been made using two different methods of the rate at which the glacier Austerdalsbreen is slipping past its side wall at four sites. The rate of slipping varies from site to site in a way which seems to be connected with the details of glacier flow in the neighbourhood, and in all cases is less than the slip previously measured further up-glacier at the foot of one of the ice falls, and is also a smaller fraction (about one sixth) of the flow rate in the centre of the glacier. One of the methods measured the velocity of the last metre of ice, and this method gave movements which were more erratic than the other method, which measured velocity a few metres from the edge. This suggests that protuberances of rock and boulders lodged between the ice and the rock wall cause local variations in flow which are smoothed out in a few metres. The results are discussed in connection with the process of glacial erosion.
format Article in Journal/Newspaper
author Glen, J. W.
Lewis, W. V.
author_facet Glen, J. W.
Lewis, W. V.
author_sort Glen, J. W.
title Measurements of Side-slip at Austerdalsbreen, 1959
title_short Measurements of Side-slip at Austerdalsbreen, 1959
title_full Measurements of Side-slip at Austerdalsbreen, 1959
title_fullStr Measurements of Side-slip at Austerdalsbreen, 1959
title_full_unstemmed Measurements of Side-slip at Austerdalsbreen, 1959
title_sort measurements of side-slip at austerdalsbreen, 1959
publisher Cambridge University Press (CUP)
publishDate 1961
url http://dx.doi.org/10.1017/s0022143000017524
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017524
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 3, issue 30, page 1109-1122
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000017524
container_title Journal of Glaciology
container_volume 3
container_issue 30
container_start_page 1109
op_container_end_page 1122
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