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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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Galloway, R. W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1956
Subjects:
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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spelling 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
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