Some Observations on Subglacial Ground-Water flow
Abstract Conduit and regelation water are inferred to drain as ground water from up to 130 km 2 of Columbia Icefield. Subglacial conduits appear to be generally occupied by free surface streams. Ground-water flow will allow exchange between the regelation film and conduits. Present-day discharge fro...
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Language: | English |
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Cambridge University Press (CUP)
1986
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Online Access: | http://dx.doi.org/10.1017/s0022143000015550 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015550 |
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crcambridgeupr:10.1017/s0022143000015550 2024-03-03T08:46:09+00:00 Some Observations on Subglacial Ground-Water flow Smart, C. C. 1986 http://dx.doi.org/10.1017/s0022143000015550 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015550 en eng Cambridge University Press (CUP) Journal of Glaciology volume 32, issue 111, page 232-234 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1986 crcambridgeupr https://doi.org/10.1017/s0022143000015550 2024-02-08T08:36:10Z Abstract Conduit and regelation water are inferred to drain as ground water from up to 130 km 2 of Columbia Icefield. Subglacial conduits appear to be generally occupied by free surface streams. Ground-water flow will allow exchange between the regelation film and conduits. Present-day discharge from beneath the accumulation zone carries little sediment, and past injections of sediment appear to correspond to ancient interglacials. Transport of sediment through cave passages may be analogous to transport through basal conduits. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 32 111 232 234 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Smart, C. C. Some Observations on Subglacial Ground-Water flow |
topic_facet |
Earth-Surface Processes |
description |
Abstract Conduit and regelation water are inferred to drain as ground water from up to 130 km 2 of Columbia Icefield. Subglacial conduits appear to be generally occupied by free surface streams. Ground-water flow will allow exchange between the regelation film and conduits. Present-day discharge from beneath the accumulation zone carries little sediment, and past injections of sediment appear to correspond to ancient interglacials. Transport of sediment through cave passages may be analogous to transport through basal conduits. |
format |
Article in Journal/Newspaper |
author |
Smart, C. C. |
author_facet |
Smart, C. C. |
author_sort |
Smart, C. C. |
title |
Some Observations on Subglacial Ground-Water flow |
title_short |
Some Observations on Subglacial Ground-Water flow |
title_full |
Some Observations on Subglacial Ground-Water flow |
title_fullStr |
Some Observations on Subglacial Ground-Water flow |
title_full_unstemmed |
Some Observations on Subglacial Ground-Water flow |
title_sort |
some observations on subglacial ground-water flow |
publisher |
Cambridge University Press (CUP) |
publishDate |
1986 |
url |
http://dx.doi.org/10.1017/s0022143000015550 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015550 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 32, issue 111, page 232-234 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000015550 |
container_title |
Journal of Glaciology |
container_volume |
32 |
container_issue |
111 |
container_start_page |
232 |
op_container_end_page |
234 |
_version_ |
1792502133096972288 |