Measurement of Firn Motion by a Magnetic Prospecting Method

Abstract The compaction and flow within névé can be studied by means of magnetized steel tubes buried in vertical pits. The locations of the tubes, their distances from the surface, down to a depth of 10 m., and their angles with the vertical can be determined from measurements made with a B.M.Z. ma...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Lliboutry, L.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1961
Subjects:
Earth-Surface Processes
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s002214300002726x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300002726X
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spelling crcambridgeupr:10.1017/s002214300002726x 2024-03-03T08:46:04+00:00 Measurement of Firn Motion by a Magnetic Prospecting Method Lliboutry, L. 1961 http://dx.doi.org/10.1017/s002214300002726x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300002726X en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 29, page 879-881 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1961 crcambridgeupr https://doi.org/10.1017/s002214300002726x 2024-02-08T08:41:37Z Abstract The compaction and flow within névé can be studied by means of magnetized steel tubes buried in vertical pits. The locations of the tubes, their distances from the surface, down to a depth of 10 m., and their angles with the vertical can be determined from measurements made with a B.M.Z. magnetometer. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 3 29 879 881
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Lliboutry, L.
Measurement of Firn Motion by a Magnetic Prospecting Method
topic_facet Earth-Surface Processes
description Abstract The compaction and flow within névé can be studied by means of magnetized steel tubes buried in vertical pits. The locations of the tubes, their distances from the surface, down to a depth of 10 m., and their angles with the vertical can be determined from measurements made with a B.M.Z. magnetometer.
format Article in Journal/Newspaper
author Lliboutry, L.
author_facet Lliboutry, L.
author_sort Lliboutry, L.
title Measurement of Firn Motion by a Magnetic Prospecting Method
title_short Measurement of Firn Motion by a Magnetic Prospecting Method
title_full Measurement of Firn Motion by a Magnetic Prospecting Method
title_fullStr Measurement of Firn Motion by a Magnetic Prospecting Method
title_full_unstemmed Measurement of Firn Motion by a Magnetic Prospecting Method
title_sort measurement of firn motion by a magnetic prospecting method
publisher Cambridge University Press (CUP)
publishDate 1961
url http://dx.doi.org/10.1017/s002214300002726x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300002726X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 3, issue 29, page 879-881
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s002214300002726x
container_title Journal of Glaciology
container_volume 3
container_issue 29
container_start_page 879
op_container_end_page 881
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