Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology
Abstract The tectonic effects of a glacier surge differ from those of steady state because flow is driven by longitudinal stresses rather than shear stresses. The orientations of recently formed crevasses, indicating the directions of the principal stresses, have been used to investigate tectonic pr...
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Language: | English |
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Cambridge University Press (CUP)
1994
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Online Access: | http://dx.doi.org/10.1017/s0022143000012430 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012430 |
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crcambridgeupr:10.1017/s0022143000012430 2024-09-15T18:07:55+00:00 Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology Richard, Hodgkins Dowdeswell, Julian A. 1994 http://dx.doi.org/10.1017/s0022143000012430 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012430 en eng Cambridge University Press (CUP) Journal of Glaciology volume 40, issue 136, page 553-560 ISSN 0022-1430 1727-5652 journal-article 1994 crcambridgeupr https://doi.org/10.1017/s0022143000012430 2024-07-24T04:03:42Z Abstract The tectonic effects of a glacier surge differ from those of steady state because flow is driven by longitudinal stresses rather than shear stresses. The orientations of recently formed crevasses, indicating the directions of the principal stresses, have been used to investigate tectonic processes in glacier surges recorded by repeat aerial photography. Long-term, large-magnitude shifts in stress regime are demonstrated, as are short-term propagation features. Two types of tide-water glacier advance are identified, depending on the position of the surge front relative to a low effective-pressure zone at the glacier terminus. Article in Journal/Newspaper glacier Journal of Glaciology Svalbard Cambridge University Press Journal of Glaciology 40 136 553 560 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract The tectonic effects of a glacier surge differ from those of steady state because flow is driven by longitudinal stresses rather than shear stresses. The orientations of recently formed crevasses, indicating the directions of the principal stresses, have been used to investigate tectonic processes in glacier surges recorded by repeat aerial photography. Long-term, large-magnitude shifts in stress regime are demonstrated, as are short-term propagation features. Two types of tide-water glacier advance are identified, depending on the position of the surge front relative to a low effective-pressure zone at the glacier terminus. |
format |
Article in Journal/Newspaper |
author |
Richard, Hodgkins Dowdeswell, Julian A. |
spellingShingle |
Richard, Hodgkins Dowdeswell, Julian A. Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology |
author_facet |
Richard, Hodgkins Dowdeswell, Julian A. |
author_sort |
Richard, Hodgkins |
title |
Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology |
title_short |
Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology |
title_full |
Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology |
title_fullStr |
Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology |
title_full_unstemmed |
Tectonic processes in Svalbard tide-water glacier surges: evidence from structural glaciology |
title_sort |
tectonic processes in svalbard tide-water glacier surges: evidence from structural glaciology |
publisher |
Cambridge University Press (CUP) |
publishDate |
1994 |
url |
http://dx.doi.org/10.1017/s0022143000012430 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012430 |
genre |
glacier Journal of Glaciology Svalbard |
genre_facet |
glacier Journal of Glaciology Svalbard |
op_source |
Journal of Glaciology volume 40, issue 136, page 553-560 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000012430 |
container_title |
Journal of Glaciology |
container_volume |
40 |
container_issue |
136 |
container_start_page |
553 |
op_container_end_page |
560 |
_version_ |
1810445281478574080 |