A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams
The deformation and state of stress at the confluence of two glacier streams are analysed using the techniques of slip-line theory. The valley walls are taken to be vertical parallel planes and the deformation is supposed independent of depth. The mechanical behavior of ice is modeled by the ideal r...
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Language: | English |
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Cambridge University Press (CUP)
1970
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Online Access: | http://dx.doi.org/10.1017/s0022143000023510 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023510 |
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crcambridgeupr:10.1017/s0022143000023510 2024-03-03T08:44:41+00:00 A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams Collins, I. F. 1970 http://dx.doi.org/10.1017/s0022143000023510 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023510 en eng Cambridge University Press (CUP) Journal of Glaciology volume 9, issue 56, page 169-193 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1970 crcambridgeupr https://doi.org/10.1017/s0022143000023510 2024-02-08T08:40:23Z The deformation and state of stress at the confluence of two glacier streams are analysed using the techniques of slip-line theory. The valley walls are taken to be vertical parallel planes and the deformation is supposed independent of depth. The mechanical behavior of ice is modeled by the ideal rigid/perfectly plastic material. Detailed solutions are presented for the deformation at the confluence of one or more tributaries with a main stream and of two main streams. Attention is concentrated on predicting the number, position and magnitude of the bands of intense shear which emanate from some of the junction corners. The predictions of this idealized theory are compared with field data from a confluence on the Kaskawulsh Glacier, Yukon Territory, Canada. Article in Journal/Newspaper glacier* Journal of Glaciology Yukon Cambridge University Press Yukon Canada Kaskawulsh Glacier ENVELOPE(-139.104,-139.104,60.749,60.749) Journal of Glaciology 9 56 169 193 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Collins, I. F. A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams |
topic_facet |
Earth-Surface Processes |
description |
The deformation and state of stress at the confluence of two glacier streams are analysed using the techniques of slip-line theory. The valley walls are taken to be vertical parallel planes and the deformation is supposed independent of depth. The mechanical behavior of ice is modeled by the ideal rigid/perfectly plastic material. Detailed solutions are presented for the deformation at the confluence of one or more tributaries with a main stream and of two main streams. Attention is concentrated on predicting the number, position and magnitude of the bands of intense shear which emanate from some of the junction corners. The predictions of this idealized theory are compared with field data from a confluence on the Kaskawulsh Glacier, Yukon Territory, Canada. |
format |
Article in Journal/Newspaper |
author |
Collins, I. F. |
author_facet |
Collins, I. F. |
author_sort |
Collins, I. F. |
title |
A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams |
title_short |
A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams |
title_full |
A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams |
title_fullStr |
A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams |
title_full_unstemmed |
A Slip-Line Field Analysis of the Deformation at the Confluence of two Glacier Streams |
title_sort |
slip-line field analysis of the deformation at the confluence of two glacier streams |
publisher |
Cambridge University Press (CUP) |
publishDate |
1970 |
url |
http://dx.doi.org/10.1017/s0022143000023510 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023510 |
long_lat |
ENVELOPE(-139.104,-139.104,60.749,60.749) |
geographic |
Yukon Canada Kaskawulsh Glacier |
geographic_facet |
Yukon Canada Kaskawulsh Glacier |
genre |
glacier* Journal of Glaciology Yukon |
genre_facet |
glacier* Journal of Glaciology Yukon |
op_source |
Journal of Glaciology volume 9, issue 56, page 169-193 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000023510 |
container_title |
Journal of Glaciology |
container_volume |
9 |
container_issue |
56 |
container_start_page |
169 |
op_container_end_page |
193 |
_version_ |
1792500159455690752 |