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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Cambridge University Press (CUP)
1991
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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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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 |
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Open Polar |
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Cambridge University Press |
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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 |
_version_ |
1810449895160545280 |