The Structure of Moraines in Lyngsdalen, North Norway
Abstract The structure of some moraines in and around two glaciers in northern Norway was studied by the method of fabric analysis. It was found that englacial material tends to lie parallel to the direction of movement of the ice, and material in lateral and terminal moraines shows orientations whi...
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Language: | English |
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Cambridge University Press (CUP)
1956
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Online Access: | http://dx.doi.org/10.1017/s0022143000024989 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024989 |
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crcambridgeupr:10.1017/s0022143000024989 2024-03-03T08:46:09+00:00 The Structure of Moraines in Lyngsdalen, North Norway Galloway, R. W. 1956 http://dx.doi.org/10.1017/s0022143000024989 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024989 en eng Cambridge University Press (CUP) Journal of Glaciology volume 2, issue 20, page 730-733 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1956 crcambridgeupr https://doi.org/10.1017/s0022143000024989 2024-02-08T08:36:10Z Abstract The structure of some moraines in and around two glaciers in northern Norway was studied by the method of fabric analysis. It was found that englacial material tends to lie parallel to the direction of movement of the ice, and material in lateral and terminal moraines shows orientations which appear to be related to the conditions under which it was deposited. Article in Journal/Newspaper Journal of Glaciology North Norway Northern Norway Cambridge University Press Norway Lyngsdalen ENVELOPE(20.093,20.093,69.448,69.448) Journal of Glaciology 2 20 730 733 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Galloway, R. W. The Structure of Moraines in Lyngsdalen, North Norway |
topic_facet |
Earth-Surface Processes |
description |
Abstract The structure of some moraines in and around two glaciers in northern Norway was studied by the method of fabric analysis. It was found that englacial material tends to lie parallel to the direction of movement of the ice, and material in lateral and terminal moraines shows orientations which appear to be related to the conditions under which it was deposited. |
format |
Article in Journal/Newspaper |
author |
Galloway, R. W. |
author_facet |
Galloway, R. W. |
author_sort |
Galloway, R. W. |
title |
The Structure of Moraines in Lyngsdalen, North Norway |
title_short |
The Structure of Moraines in Lyngsdalen, North Norway |
title_full |
The Structure of Moraines in Lyngsdalen, North Norway |
title_fullStr |
The Structure of Moraines in Lyngsdalen, North Norway |
title_full_unstemmed |
The Structure of Moraines in Lyngsdalen, North Norway |
title_sort |
structure of moraines in lyngsdalen, north norway |
publisher |
Cambridge University Press (CUP) |
publishDate |
1956 |
url |
http://dx.doi.org/10.1017/s0022143000024989 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024989 |
long_lat |
ENVELOPE(20.093,20.093,69.448,69.448) |
geographic |
Norway Lyngsdalen |
geographic_facet |
Norway Lyngsdalen |
genre |
Journal of Glaciology North Norway Northern Norway |
genre_facet |
Journal of Glaciology North Norway Northern Norway |
op_source |
Journal of Glaciology volume 2, issue 20, page 730-733 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000024989 |
container_title |
Journal of Glaciology |
container_volume |
2 |
container_issue |
20 |
container_start_page |
730 |
op_container_end_page |
733 |
_version_ |
1792502110489673728 |