Experience with Shear Frames

Abstract The shear frame is a simple in situ device for indexing the shear strength of thin weak layers. The index is sensitive to shear-frame geometry, rate-of-pull, and shear-frame mass. It is time-consuming to carefully align the device on the Gleitschicht (shear failure plane) in a slab avalanch...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Perla, R., Beck, T. M. H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1983
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000030380
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030380
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spelling crcambridgeupr:10.1017/s0022143000030380 2024-03-03T08:46:04+00:00 Experience with Shear Frames Perla, R. Beck, T. M. H. 1983 http://dx.doi.org/10.1017/s0022143000030380 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030380 en eng Cambridge University Press (CUP) Journal of Glaciology volume 29, issue 103, page 485-491 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1983 crcambridgeupr https://doi.org/10.1017/s0022143000030380 2024-02-08T08:40:23Z Abstract The shear frame is a simple in situ device for indexing the shear strength of thin weak layers. The index is sensitive to shear-frame geometry, rate-of-pull, and shear-frame mass. It is time-consuming to carefully align the device on the Gleitschicht (shear failure plane) in a slab avalanche zone. The ratio shear frame index/shear stress of the Gleitschicht has a high variance, and may not be a fundamental measure of slab avalanche stability. Corrections for the normal stress on the Gleitschicht reduce the variance only slightly. Despite these limitations, the shear frame is a useful tool for gathering statistical data on strength distributions and anisotropies of the Gleitschicht until a more fundamental technique is developed. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 29 103 485 491
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Perla, R.
Beck, T. M. H.
Experience with Shear Frames
topic_facet Earth-Surface Processes
description Abstract The shear frame is a simple in situ device for indexing the shear strength of thin weak layers. The index is sensitive to shear-frame geometry, rate-of-pull, and shear-frame mass. It is time-consuming to carefully align the device on the Gleitschicht (shear failure plane) in a slab avalanche zone. The ratio shear frame index/shear stress of the Gleitschicht has a high variance, and may not be a fundamental measure of slab avalanche stability. Corrections for the normal stress on the Gleitschicht reduce the variance only slightly. Despite these limitations, the shear frame is a useful tool for gathering statistical data on strength distributions and anisotropies of the Gleitschicht until a more fundamental technique is developed.
format Article in Journal/Newspaper
author Perla, R.
Beck, T. M. H.
author_facet Perla, R.
Beck, T. M. H.
author_sort Perla, R.
title Experience with Shear Frames
title_short Experience with Shear Frames
title_full Experience with Shear Frames
title_fullStr Experience with Shear Frames
title_full_unstemmed Experience with Shear Frames
title_sort experience with shear frames
publisher Cambridge University Press (CUP)
publishDate 1983
url http://dx.doi.org/10.1017/s0022143000030380
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030380
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 29, issue 103, page 485-491
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000030380
container_title Journal of Glaciology
container_volume 29
container_issue 103
container_start_page 485
op_container_end_page 491
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