Deforming-bed origin for southern Laurentide till sheets?

Abstract The widespread, uniform till sheets of the southern margin of the Laurentide ice sheet were deposited by fast-moving, wet-bedded ice over relatively short periods of time. Characteristics of these till sheets are entirely consistent with deposition from deforming subglacial sediment layers;...

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Published in:Journal of Glaciology
Main Author: Alley, Richard B.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1991
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000042817
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000042817
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spelling crcambridgeupr:10.1017/s0022143000042817 2024-09-15T18:12:18+00:00 Deforming-bed origin for southern Laurentide till sheets? Alley, Richard B. 1991 http://dx.doi.org/10.1017/s0022143000042817 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000042817 en eng Cambridge University Press (CUP) Journal of Glaciology volume 37, issue 125, page 67-76 ISSN 0022-1430 1727-5652 journal-article 1991 crcambridgeupr https://doi.org/10.1017/s0022143000042817 2024-07-31T04:04:38Z Abstract The widespread, uniform till sheets of the southern margin of the Laurentide ice sheet were deposited by fast-moving, wet-bedded ice over relatively short periods of time. Characteristics of these till sheets are entirely consistent with deposition from deforming subglacial sediment layers; it is difficult (although not impossible) to explain their origin through debris transport in basal ice. Careful estimation of debris budgets and studies of sorted sediments contained in the till sheets may clarify their origin further. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 37 125 67 76
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The widespread, uniform till sheets of the southern margin of the Laurentide ice sheet were deposited by fast-moving, wet-bedded ice over relatively short periods of time. Characteristics of these till sheets are entirely consistent with deposition from deforming subglacial sediment layers; it is difficult (although not impossible) to explain their origin through debris transport in basal ice. Careful estimation of debris budgets and studies of sorted sediments contained in the till sheets may clarify their origin further.
format Article in Journal/Newspaper
author Alley, Richard B.
spellingShingle Alley, Richard B.
Deforming-bed origin for southern Laurentide till sheets?
author_facet Alley, Richard B.
author_sort Alley, Richard B.
title Deforming-bed origin for southern Laurentide till sheets?
title_short Deforming-bed origin for southern Laurentide till sheets?
title_full Deforming-bed origin for southern Laurentide till sheets?
title_fullStr Deforming-bed origin for southern Laurentide till sheets?
title_full_unstemmed Deforming-bed origin for southern Laurentide till sheets?
title_sort deforming-bed origin for southern laurentide till sheets?
publisher Cambridge University Press (CUP)
publishDate 1991
url http://dx.doi.org/10.1017/s0022143000042817
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000042817
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 37, issue 125, page 67-76
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000042817
container_title Journal of Glaciology
container_volume 37
container_issue 125
container_start_page 67
op_container_end_page 76
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