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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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Smart, C. C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1986
Subjects:
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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spelling 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
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