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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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) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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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 |
_version_ |
1797567751642939392 |