Subglacial floods and the origin of low-relief ice-sheet lobes
Abstract The likely genesis of low-relief ice-sheet lobes is episodic subglacial floods which occur in the form of water sheets hundreds of kilometers wide. During the few weeks prior to termination, when the flood discharge is large, the average thickness of a water sheet beneath the Lake Michigan...
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Cambridge University Press (CUP)
1992
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Online Access: | http://dx.doi.org/10.1017/s0022143000009643 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009643 |
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crcambridgeupr:10.1017/s0022143000009643 2024-09-15T18:12:13+00:00 Subglacial floods and the origin of low-relief ice-sheet lobes Shoemaker, E. M. 1992 http://dx.doi.org/10.1017/s0022143000009643 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009643 en eng Cambridge University Press (CUP) Journal of Glaciology volume 38, issue 128, page 105-112 ISSN 0022-1430 1727-5652 journal-article 1992 crcambridgeupr https://doi.org/10.1017/s0022143000009643 2024-07-24T04:01:47Z Abstract The likely genesis of low-relief ice-sheet lobes is episodic subglacial floods which occur in the form of water sheets hundreds of kilometers wide. During the few weeks prior to termination, when the flood discharge is large, the average thickness of a water sheet beneath the Lake Michigan lobe likely exceeded 1 m and reached thicknesses in excess of 6 m. The release of a part of the basal shear stress during this period produced an elongation of the lobe of tens of kilometers. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 38 128 105 112 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract The likely genesis of low-relief ice-sheet lobes is episodic subglacial floods which occur in the form of water sheets hundreds of kilometers wide. During the few weeks prior to termination, when the flood discharge is large, the average thickness of a water sheet beneath the Lake Michigan lobe likely exceeded 1 m and reached thicknesses in excess of 6 m. The release of a part of the basal shear stress during this period produced an elongation of the lobe of tens of kilometers. |
format |
Article in Journal/Newspaper |
author |
Shoemaker, E. M. |
spellingShingle |
Shoemaker, E. M. Subglacial floods and the origin of low-relief ice-sheet lobes |
author_facet |
Shoemaker, E. M. |
author_sort |
Shoemaker, E. M. |
title |
Subglacial floods and the origin of low-relief ice-sheet lobes |
title_short |
Subglacial floods and the origin of low-relief ice-sheet lobes |
title_full |
Subglacial floods and the origin of low-relief ice-sheet lobes |
title_fullStr |
Subglacial floods and the origin of low-relief ice-sheet lobes |
title_full_unstemmed |
Subglacial floods and the origin of low-relief ice-sheet lobes |
title_sort |
subglacial floods and the origin of low-relief ice-sheet lobes |
publisher |
Cambridge University Press (CUP) |
publishDate |
1992 |
url |
http://dx.doi.org/10.1017/s0022143000009643 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009643 |
genre |
Ice Sheet Journal of Glaciology |
genre_facet |
Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology volume 38, issue 128, page 105-112 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000009643 |
container_title |
Journal of Glaciology |
container_volume |
38 |
container_issue |
128 |
container_start_page |
105 |
op_container_end_page |
112 |
_version_ |
1810449794101936128 |