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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Published in:Journal of Glaciology
Main Author: Perla, R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
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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spelling 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
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