The Role of Stress Concentration in Slab Avalanche Release

Abstract Slab avalanches are shown to be released by brittle fracture. An analogy is drawn in which the snow-pack is considered to be a macroscopic, molecular model of glass. The analogy is examined qualitatively from two viewpoints: the Griffith fracture criterion, and stress concentration theory....

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Published in:Journal of Glaciology
Main Author: Sommerfeld, R. A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1969
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000027039
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027039
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spelling crcambridgeupr:10.1017/s0022143000027039 2024-09-15T18:15:39+00:00 The Role of Stress Concentration in Slab Avalanche Release Sommerfeld, R. A. 1969 http://dx.doi.org/10.1017/s0022143000027039 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027039 en eng Cambridge University Press (CUP) Journal of Glaciology volume 8, issue 54, page 451-462 ISSN 0022-1430 1727-5652 journal-article 1969 crcambridgeupr https://doi.org/10.1017/s0022143000027039 2024-07-31T04:04:10Z Abstract Slab avalanches are shown to be released by brittle fracture. An analogy is drawn in which the snow-pack is considered to be a macroscopic, molecular model of glass. The analogy is examined qualitatively from two viewpoints: the Griffith fracture criterion, and stress concentration theory. The details of fracture propagation in a layered snow-pack are explained by means of stress concentration theory, and many details of slab avalanches are shown to be consistent with the proposed mechanism. The significance of various fracture surface markings is pointed out. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 8 54 451 462
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Slab avalanches are shown to be released by brittle fracture. An analogy is drawn in which the snow-pack is considered to be a macroscopic, molecular model of glass. The analogy is examined qualitatively from two viewpoints: the Griffith fracture criterion, and stress concentration theory. The details of fracture propagation in a layered snow-pack are explained by means of stress concentration theory, and many details of slab avalanches are shown to be consistent with the proposed mechanism. The significance of various fracture surface markings is pointed out.
format Article in Journal/Newspaper
author Sommerfeld, R. A.
spellingShingle Sommerfeld, R. A.
The Role of Stress Concentration in Slab Avalanche Release
author_facet Sommerfeld, R. A.
author_sort Sommerfeld, R. A.
title The Role of Stress Concentration in Slab Avalanche Release
title_short The Role of Stress Concentration in Slab Avalanche Release
title_full The Role of Stress Concentration in Slab Avalanche Release
title_fullStr The Role of Stress Concentration in Slab Avalanche Release
title_full_unstemmed The Role of Stress Concentration in Slab Avalanche Release
title_sort role of stress concentration in slab avalanche release
publisher Cambridge University Press (CUP)
publishDate 1969
url http://dx.doi.org/10.1017/s0022143000027039
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027039
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 8, issue 54, page 451-462
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000027039
container_title Journal of Glaciology
container_volume 8
container_issue 54
container_start_page 451
op_container_end_page 462
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