Short Note on Slab-Avalanche Measurements
Abstract From a study of 205 slab avalanches it is concluded that failure initiates where the slope is 25° or steeper, that slab failure stress is in the range 10 2 N m -2 to 10 4 N m -2 , and that the slab failure plane is most commonly at a temperature of -5°C or warmer. The study also indicates t...
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Cambridge University Press (CUP)
1978
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Online Access: | http://dx.doi.org/10.1017/s0022143000021250 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021250 |
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crcambridgeupr:10.1017/s0022143000021250 2024-03-03T08:45:59+00:00 Short Note on Slab-Avalanche Measurements Perla, R. 1978 http://dx.doi.org/10.1017/s0022143000021250 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021250 en eng Cambridge University Press (CUP) Journal of Glaciology volume 20, issue 82, page 221-222 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000021250 2024-02-08T08:40:23Z Abstract From a study of 205 slab avalanches it is concluded that failure initiates where the slope is 25° or steeper, that slab failure stress is in the range 10 2 N m -2 to 10 4 N m -2 , and that the slab failure plane is most commonly at a temperature of -5°C or warmer. The study also indicates that the shear strength of weak layers varies approximately as the square of the density. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 20 82 221 222 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Perla, R. Short Note on Slab-Avalanche Measurements |
topic_facet |
Earth-Surface Processes |
description |
Abstract From a study of 205 slab avalanches it is concluded that failure initiates where the slope is 25° or steeper, that slab failure stress is in the range 10 2 N m -2 to 10 4 N m -2 , and that the slab failure plane is most commonly at a temperature of -5°C or warmer. The study also indicates that the shear strength of weak layers varies approximately as the square of the density. |
format |
Article in Journal/Newspaper |
author |
Perla, R. |
author_facet |
Perla, R. |
author_sort |
Perla, R. |
title |
Short Note on Slab-Avalanche Measurements |
title_short |
Short Note on Slab-Avalanche Measurements |
title_full |
Short Note on Slab-Avalanche Measurements |
title_fullStr |
Short Note on Slab-Avalanche Measurements |
title_full_unstemmed |
Short Note on Slab-Avalanche Measurements |
title_sort |
short note on slab-avalanche measurements |
publisher |
Cambridge University Press (CUP) |
publishDate |
1978 |
url |
http://dx.doi.org/10.1017/s0022143000021250 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021250 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 20, issue 82, page 221-222 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000021250 |
container_title |
Journal of Glaciology |
container_volume |
20 |
container_issue |
82 |
container_start_page |
221 |
op_container_end_page |
222 |
_version_ |
1792501749699837952 |