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...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Rose, J., Letzer, J. M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1977
Subjects:
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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spelling 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
institution Open Polar
collection Cambridge University Press
op_collection_id 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
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