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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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Richard, Hodgkins, Dowdeswell, Julian A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1994
Subjects:
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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spelling 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
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