Glacier Mechanics in the Perfect Plasticity Theory

Abstract The author agrees with Nye’s correction of two errors in a previous paper; but disagrees with his other objections. Evidence is put forward for the significance of a second approximation in the theoretical equation for the profile of a glacier; for instance, it explains why bulges of increa...

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Published in:Journal of Glaciology
Main Author: Lliboutry, Louis
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1958
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000024163
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024163
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spelling crcambridgeupr:10.1017/s0022143000024163 2024-09-15T18:15:39+00:00 Glacier Mechanics in the Perfect Plasticity Theory Lliboutry, Louis 1958 http://dx.doi.org/10.1017/s0022143000024163 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024163 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 23, page 162-169 ISSN 0022-1430 1727-5652 journal-article 1958 crcambridgeupr https://doi.org/10.1017/s0022143000024163 2024-07-17T04:03:49Z Abstract The author agrees with Nye’s correction of two errors in a previous paper; but disagrees with his other objections. Evidence is put forward for the significance of a second approximation in the theoretical equation for the profile of a glacier; for instance, it explains why bulges of increased thickness travel down glacier faster than the ice. Features of the front of the Glacier de Saint-Sorlin are reported. An attempt is made to explain crevasse formation in glaciers and the upturning of blue bands at the foot of an ice fall. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 3 23 162 169
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The author agrees with Nye’s correction of two errors in a previous paper; but disagrees with his other objections. Evidence is put forward for the significance of a second approximation in the theoretical equation for the profile of a glacier; for instance, it explains why bulges of increased thickness travel down glacier faster than the ice. Features of the front of the Glacier de Saint-Sorlin are reported. An attempt is made to explain crevasse formation in glaciers and the upturning of blue bands at the foot of an ice fall.
format Article in Journal/Newspaper
author Lliboutry, Louis
spellingShingle Lliboutry, Louis
Glacier Mechanics in the Perfect Plasticity Theory
author_facet Lliboutry, Louis
author_sort Lliboutry, Louis
title Glacier Mechanics in the Perfect Plasticity Theory
title_short Glacier Mechanics in the Perfect Plasticity Theory
title_full Glacier Mechanics in the Perfect Plasticity Theory
title_fullStr Glacier Mechanics in the Perfect Plasticity Theory
title_full_unstemmed Glacier Mechanics in the Perfect Plasticity Theory
title_sort glacier mechanics in the perfect plasticity theory
publisher Cambridge University Press (CUP)
publishDate 1958
url http://dx.doi.org/10.1017/s0022143000024163
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024163
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 3, issue 23, page 162-169
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000024163
container_title Journal of Glaciology
container_volume 3
container_issue 23
container_start_page 162
op_container_end_page 169
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