Superimposed Drumlins
Abstract Drumlins in parts of central Scotland and east Cumbria form two populations according to their size. In certain cases the small features are superimposed on the large. Drumlins, superimposed drumlins, and megadrumlins are considered to be part of a continuum of glacier bed forms, which is t...
Published in: | Journal of Glaciology |
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Language: | English |
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Cambridge University Press (CUP)
1977
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Online Access: | http://dx.doi.org/10.1017/s0022143000021146 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021146 |
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crcambridgeupr:10.1017/s0022143000021146 2024-06-23T07:54:15+00:00 Superimposed Drumlins Rose, J. Letzer, J. M. 1977 http://dx.doi.org/10.1017/s0022143000021146 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021146 en eng Cambridge University Press (CUP) Journal of Glaciology volume 18, issue 80, page 471-480 ISSN 0022-1430 1727-5652 journal-article 1977 crcambridgeupr https://doi.org/10.1017/s0022143000021146 2024-06-05T04:04:44Z Abstract Drumlins in parts of central Scotland and east Cumbria form two populations according to their size. In certain cases the small features are superimposed on the large. Drumlins, superimposed drumlins, and megadrumlins are considered to be part of a continuum of glacier bed forms, which is the product of changes in the stress applied by glaciers and the strength of bed material. Glacier behaviour can be inferred on the basis of this interpretation. Drumlins in parts of central Scotland and east Cumbria form two populations according to their size. In certain cases the small features are superimposed on the large. Drumlins, superimposed drumlins, and megadrumlins are considered to be part of a continuum of glacier bed forms, which is the product of changes in the stress applied by glaciers and the strength of bed material. Glacier behaviour can be inferred on the basis of this interpretation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 18 80 471 480 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Drumlins in parts of central Scotland and east Cumbria form two populations according to their size. In certain cases the small features are superimposed on the large. Drumlins, superimposed drumlins, and megadrumlins are considered to be part of a continuum of glacier bed forms, which is the product of changes in the stress applied by glaciers and the strength of bed material. Glacier behaviour can be inferred on the basis of this interpretation. Drumlins in parts of central Scotland and east Cumbria form two populations according to their size. In certain cases the small features are superimposed on the large. Drumlins, superimposed drumlins, and megadrumlins are considered to be part of a continuum of glacier bed forms, which is the product of changes in the stress applied by glaciers and the strength of bed material. Glacier behaviour can be inferred on the basis of this interpretation. |
format |
Article in Journal/Newspaper |
author |
Rose, J. Letzer, J. M. |
spellingShingle |
Rose, J. Letzer, J. M. Superimposed Drumlins |
author_facet |
Rose, J. Letzer, J. M. |
author_sort |
Rose, J. |
title |
Superimposed Drumlins |
title_short |
Superimposed Drumlins |
title_full |
Superimposed Drumlins |
title_fullStr |
Superimposed Drumlins |
title_full_unstemmed |
Superimposed Drumlins |
title_sort |
superimposed drumlins |
publisher |
Cambridge University Press (CUP) |
publishDate |
1977 |
url |
http://dx.doi.org/10.1017/s0022143000021146 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021146 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 18, issue 80, page 471-480 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000021146 |
container_title |
Journal of Glaciology |
container_volume |
18 |
container_issue |
80 |
container_start_page |
471 |
op_container_end_page |
480 |
_version_ |
1802646336816807936 |