Instruments and Methods: The Resistograph and the Compressive Strength of Snow

Abstract A recent field comparison of snow strength as measured by the snow resistograph and compressive strength as measured by direct loading to failure indicates good agreement in the range 25–400 g/cm 2 .

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Bradley, Charles C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1968
Subjects:
Earth-Surface Processes
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000020682
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020682
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spelling crcambridgeupr:10.1017/s0022143000020682 2024-03-03T08:46:05+00:00 Instruments and Methods: The Resistograph and the Compressive Strength of Snow Bradley, Charles C. 1968 http://dx.doi.org/10.1017/s0022143000020682 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020682 en eng Cambridge University Press (CUP) Journal of Glaciology volume 7, issue 51, page 499-506 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1968 crcambridgeupr https://doi.org/10.1017/s0022143000020682 2024-02-08T08:36:10Z Abstract A recent field comparison of snow strength as measured by the snow resistograph and compressive strength as measured by direct loading to failure indicates good agreement in the range 25–400 g/cm 2 . Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 7 51 499 506
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Bradley, Charles C.
Instruments and Methods: The Resistograph and the Compressive Strength of Snow
topic_facet Earth-Surface Processes
description Abstract A recent field comparison of snow strength as measured by the snow resistograph and compressive strength as measured by direct loading to failure indicates good agreement in the range 25–400 g/cm 2 .
format Article in Journal/Newspaper
author Bradley, Charles C.
author_facet Bradley, Charles C.
author_sort Bradley, Charles C.
title Instruments and Methods: The Resistograph and the Compressive Strength of Snow
title_short Instruments and Methods: The Resistograph and the Compressive Strength of Snow
title_full Instruments and Methods: The Resistograph and the Compressive Strength of Snow
title_fullStr Instruments and Methods: The Resistograph and the Compressive Strength of Snow
title_full_unstemmed Instruments and Methods: The Resistograph and the Compressive Strength of Snow
title_sort instruments and methods: the resistograph and the compressive strength of snow
publisher Cambridge University Press (CUP)
publishDate 1968
url http://dx.doi.org/10.1017/s0022143000020682
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020682
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 7, issue 51, page 499-506
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000020682
container_title Journal of Glaciology
container_volume 7
container_issue 51
container_start_page 499
op_container_end_page 506
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