Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ...

Understanding rock slope kinematics in steep, fractured bedrock permafrost is a challenging task. Recent laboratory studies have provided enhanced understanding of rock fatigue and fracturing in cold environments but were not successfully confirmed by field studies. This study presents a unique time...

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Main Authors: Weber, Samuel, Beutel, Jan, Faillettaz, Jérome, Hasler, Andreas, Krautblatter, Michael, Vieli, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2017
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000161338
http://hdl.handle.net/20.500.11850/179308
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spelling ftdatacite:10.3929/ethz-b-000161338 2024-04-28T08:35:44+00:00 Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ... Weber, Samuel Beutel, Jan Faillettaz, Jérome Hasler, Andreas Krautblatter, Michael Vieli, Andreas 2017 application/pdf https://dx.doi.org/10.3929/ethz-b-000161338 http://hdl.handle.net/20.500.11850/179308 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 article-journal Text ScholarlyArticle Journal Article 2017 ftdatacite https://doi.org/10.3929/ethz-b-000161338 2024-04-02T12:33:25Z Understanding rock slope kinematics in steep, fractured bedrock permafrost is a challenging task. Recent laboratory studies have provided enhanced understanding of rock fatigue and fracturing in cold environments but were not successfully confirmed by field studies. This study presents a unique time series of fracture kinematics, rock temperatures and environmental conditions at 3500 m a. s. l. on the steep, strongly fractured Hörnligrat of the Matterhorn (Swiss Alps). Thanks to 8 years of continuous data, the longer-term evolution of fracture kinematics in permafrost can be analyzed with an unprecedented level of detail. Evidence for common trends in spatiotemporal pattern of fracture kinematics could be found: a partly reversible seasonal movement can be observed at all locations, with variable amplitudes. In the wider context of rock slope stability assessment, we propose separating reversible (elastic) components of fracture kinematics, caused by thermoelastic strains, from the irreversible (plastic) ... : The Cryosphere, 11 (1) ... Article in Journal/Newspaper permafrost DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Understanding rock slope kinematics in steep, fractured bedrock permafrost is a challenging task. Recent laboratory studies have provided enhanced understanding of rock fatigue and fracturing in cold environments but were not successfully confirmed by field studies. This study presents a unique time series of fracture kinematics, rock temperatures and environmental conditions at 3500 m a. s. l. on the steep, strongly fractured Hörnligrat of the Matterhorn (Swiss Alps). Thanks to 8 years of continuous data, the longer-term evolution of fracture kinematics in permafrost can be analyzed with an unprecedented level of detail. Evidence for common trends in spatiotemporal pattern of fracture kinematics could be found: a partly reversible seasonal movement can be observed at all locations, with variable amplitudes. In the wider context of rock slope stability assessment, we propose separating reversible (elastic) components of fracture kinematics, caused by thermoelastic strains, from the irreversible (plastic) ... : The Cryosphere, 11 (1) ...
format Article in Journal/Newspaper
author Weber, Samuel
Beutel, Jan
Faillettaz, Jérome
Hasler, Andreas
Krautblatter, Michael
Vieli, Andreas
spellingShingle Weber, Samuel
Beutel, Jan
Faillettaz, Jérome
Hasler, Andreas
Krautblatter, Michael
Vieli, Andreas
Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ...
author_facet Weber, Samuel
Beutel, Jan
Faillettaz, Jérome
Hasler, Andreas
Krautblatter, Michael
Vieli, Andreas
author_sort Weber, Samuel
title Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ...
title_short Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ...
title_full Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ...
title_fullStr Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ...
title_full_unstemmed Quantifying irreversible movement in steep, fractured bedrock permafrost on Matterhorn (CH) ...
title_sort quantifying irreversible movement in steep, fractured bedrock permafrost on matterhorn (ch) ...
publisher ETH Zurich
publishDate 2017
url https://dx.doi.org/10.3929/ethz-b-000161338
http://hdl.handle.net/20.500.11850/179308
genre permafrost
genre_facet permafrost
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.3929/ethz-b-000161338
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