THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T.
SUMMARY The drumlin‐like landforms that Tyrre'll described in 1896 as lrdrumlinoidstl are themost characteristic features of glacial origin in the Barren Grounds. Their widespread distribution throughout the glacial‐drift covered portions of this region, as well as manyother regions in more sou...
Published in: | Canadian Geographies / Géographies canadiennes |
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Online Access: | http://dx.doi.org/10.1111/j.1541-0064.1953.tb01722.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1953.tb01722.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1953.tb01722.x |
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crwiley:10.1111/j.1541-0064.1953.tb01722.x 2024-06-02T08:08:18+00:00 THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T. Dean, W.G. 1953 http://dx.doi.org/10.1111/j.1541-0064.1953.tb01722.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1953.tb01722.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1953.tb01722.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Canadian Geographies / Géographies canadiennes volume 1, issue 3, page 19-30 ISSN 0008-3658 1541-0064 journal-article 1953 crwiley https://doi.org/10.1111/j.1541-0064.1953.tb01722.x 2024-05-03T11:05:53Z SUMMARY The drumlin‐like landforms that Tyrre'll described in 1896 as lrdrumlinoidstl are themost characteristic features of glacial origin in the Barren Grounds. Their widespread distribution throughout the glacial‐drift covered portions of this region, as well as manyother regions in more southerly lati‐tudes covered by glacial materials, implies that thedrumlinoids are a rather significant landform developed under a continental glaciation. A yet, the pro‐cesses involved in their formation can only be speculated upon, or at best, drumlinoids might be regarded as being related to drumlins and therefore formed in a similar manner. There are a number of glaciological and geomorphological factors apparently affecting theirformation. Some of these are discussed here, but, until more detailed investigations have been carried out especially in field surveys, and a definite classification of such features has been evolved, drumlinoids can only be definitely described as widespread features which re‐sulted frc TI both depositional and erosional processes of a continental ice sheet Further study concerning the nature and orientations of the drumlfnoids in the BarrenGrounds, and elsewhere, dong with an investigation into the pro‐cesses involved En their origin should bring to light much useful Information. Such information would not only concern glacial geology and geomorphology, but also glaciology, and, indirectly, glacial climatology. Article in Journal/Newspaper Ice Sheet Wiley Online Library Canadian Geographies / Géographies canadiennes 1 3 19 30 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
SUMMARY The drumlin‐like landforms that Tyrre'll described in 1896 as lrdrumlinoidstl are themost characteristic features of glacial origin in the Barren Grounds. Their widespread distribution throughout the glacial‐drift covered portions of this region, as well as manyother regions in more southerly lati‐tudes covered by glacial materials, implies that thedrumlinoids are a rather significant landform developed under a continental glaciation. A yet, the pro‐cesses involved in their formation can only be speculated upon, or at best, drumlinoids might be regarded as being related to drumlins and therefore formed in a similar manner. There are a number of glaciological and geomorphological factors apparently affecting theirformation. Some of these are discussed here, but, until more detailed investigations have been carried out especially in field surveys, and a definite classification of such features has been evolved, drumlinoids can only be definitely described as widespread features which re‐sulted frc TI both depositional and erosional processes of a continental ice sheet Further study concerning the nature and orientations of the drumlfnoids in the BarrenGrounds, and elsewhere, dong with an investigation into the pro‐cesses involved En their origin should bring to light much useful Information. Such information would not only concern glacial geology and geomorphology, but also glaciology, and, indirectly, glacial climatology. |
format |
Article in Journal/Newspaper |
author |
Dean, W.G. |
spellingShingle |
Dean, W.G. THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T. |
author_facet |
Dean, W.G. |
author_sort |
Dean, W.G. |
title |
THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T. |
title_short |
THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T. |
title_full |
THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T. |
title_fullStr |
THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T. |
title_full_unstemmed |
THE DRUMLINOID LAND FORMS OF THE “BARREN GROUNDS”, N.W.T. |
title_sort |
drumlinoid land forms of the “barren grounds”, n.w.t. |
publisher |
Wiley |
publishDate |
1953 |
url |
http://dx.doi.org/10.1111/j.1541-0064.1953.tb01722.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1953.tb01722.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1953.tb01722.x |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Canadian Geographies / Géographies canadiennes volume 1, issue 3, page 19-30 ISSN 0008-3658 1541-0064 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1541-0064.1953.tb01722.x |
container_title |
Canadian Geographies / Géographies canadiennes |
container_volume |
1 |
container_issue |
3 |
container_start_page |
19 |
op_container_end_page |
30 |
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1800753514900619264 |