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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Cambridge University Press (CUP)
1958
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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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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 |
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Open Polar |
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Cambridge University Press |
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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 |
_version_ |
1810453561407963136 |