Till Texture in Drumlins
Abstract Drumlin till has often been described as clay-rich. Drumlins in Ontario are composed of sandy till. Additional examples from north-eastern North America show that sandy till is common in drumlins. It is suggested that the widely accepted association between drumlins and clay till was foster...
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Language: | English |
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Cambridge University Press (CUP)
1981
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Online Access: | http://dx.doi.org/10.1017/s0022143000011540 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011540 |
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crcambridgeupr:10.1017/s0022143000011540 2024-03-03T08:45:57+00:00 Till Texture in Drumlins Karrow, P. F. 1981 http://dx.doi.org/10.1017/s0022143000011540 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011540 en eng Cambridge University Press (CUP) Journal of Glaciology volume 27, issue 97, page 497-502 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1981 crcambridgeupr https://doi.org/10.1017/s0022143000011540 2024-02-08T08:34:04Z Abstract Drumlin till has often been described as clay-rich. Drumlins in Ontario are composed of sandy till. Additional examples from north-eastern North America show that sandy till is common in drumlins. It is suggested that the widely accepted association between drumlins and clay till was fostered by the use of such terms as “boulder clay” and “glacial clay”. Also, because till in drumlins may be finer than other glacial materials in such areas as the Appalachian region, a loose and exaggerated description of such material as being clay-rich arose. More careful description of drumlin till is advocated. It is suggested that grain-size distribution of till may have had a role in drumlin formation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 27 97 497 502 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Karrow, P. F. Till Texture in Drumlins |
topic_facet |
Earth-Surface Processes |
description |
Abstract Drumlin till has often been described as clay-rich. Drumlins in Ontario are composed of sandy till. Additional examples from north-eastern North America show that sandy till is common in drumlins. It is suggested that the widely accepted association between drumlins and clay till was fostered by the use of such terms as “boulder clay” and “glacial clay”. Also, because till in drumlins may be finer than other glacial materials in such areas as the Appalachian region, a loose and exaggerated description of such material as being clay-rich arose. More careful description of drumlin till is advocated. It is suggested that grain-size distribution of till may have had a role in drumlin formation. |
format |
Article in Journal/Newspaper |
author |
Karrow, P. F. |
author_facet |
Karrow, P. F. |
author_sort |
Karrow, P. F. |
title |
Till Texture in Drumlins |
title_short |
Till Texture in Drumlins |
title_full |
Till Texture in Drumlins |
title_fullStr |
Till Texture in Drumlins |
title_full_unstemmed |
Till Texture in Drumlins |
title_sort |
till texture in drumlins |
publisher |
Cambridge University Press (CUP) |
publishDate |
1981 |
url |
http://dx.doi.org/10.1017/s0022143000011540 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011540 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 27, issue 97, page 497-502 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000011540 |
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Journal of Glaciology |
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27 |
container_issue |
97 |
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497 |
op_container_end_page |
502 |
_version_ |
1792501687769890816 |