Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating

Oversteepened valley walls in western Norway have high recurrences of Holocene rock-slope failure activity causing significant risk to communities and infrastructure. Deposits from six to nine catastrophic rock-slope failure (CRSF) events are preserved at the base of the Mannen rock-slope instabilit...

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Published in:The Holocene
Main Authors: Hilger, Paula, Hermanns, Reginald, Gosse, John C, Jacobs, B, Etzelmüller, Bernd, Krautblatter, Michael
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2018
Subjects:
Online Access:http://hdl.handle.net/11250/2586526
https://doi.org/10.1177/0959683618798165
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spelling ftntnutrondheimi:oai:ntnuopen.ntnu.no:11250/2586526 2023-05-15T17:57:32+02:00 Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating Hilger, Paula Hermanns, Reginald Gosse, John C Jacobs, B Etzelmüller, Bernd Krautblatter, Michael 2018 http://hdl.handle.net/11250/2586526 https://doi.org/10.1177/0959683618798165 eng eng SAGE Publications The Holocene. 2018, 28 (12), 1841-1854. urn:issn:0959-6836 http://hdl.handle.net/11250/2586526 https://doi.org/10.1177/0959683618798165 cristin:1653886 1841-1854 28 The Holocene 12 Journal article Peer reviewed 2018 ftntnutrondheimi https://doi.org/10.1177/0959683618798165 2019-09-17T06:54:52Z Oversteepened valley walls in western Norway have high recurrences of Holocene rock-slope failure activity causing significant risk to communities and infrastructure. Deposits from six to nine catastrophic rock-slope failure (CRSF) events are preserved at the base of the Mannen rock-slope instability in the Romsdal Valley, western Norway. The timing of these CRSF events was determined by terrestrial cosmogenic nuclide dating and relative chronology due to mapping Quaternary deposits. The stratigraphical chronology indicates that three of the CRSF events occurred between 12 and 10 ka, during regional deglaciation. Congruent with previous investigations, these events are attributed to the debuttressing effect experienced by steep slopes following deglaciation, during a period of paraglacial relaxation. The remaining three to six CRSF events cluster at 4.9 ± 0.6 ka (based on 10 cosmogenic 10Be samples from boulders). CRSF events during this later period are ascribed to climatic changes at the end of the Holocene thermal optimum, including increased precipitation rates, high air temperatures and the associated degradation of permafrost in rock-slope faces. Geomorphological mapping and sedimentological analyses further permit the contextualisation of these deposits within the overall sequence of post-glacial fjord-valley infilling. In the light of contemporary climate change, the relationship between CRSF frequency, precipitation, air temperature and permafrost degradation may be of interest to others working or operating in comparable settings. acceptedVersion © 2018. This is the authors' accepted and refereed manuscript to the article. The final authenticated version is available online at: https://journals.sagepub.com/doi/10.1177/0959683618798165 Article in Journal/Newspaper permafrost NTNU Open Archive (Norwegian University of Science and Technology) Mannen ENVELOPE(13.520,13.520,68.204,68.204) Norway The Holocene 28 12 1841 1854
institution Open Polar
collection NTNU Open Archive (Norwegian University of Science and Technology)
op_collection_id ftntnutrondheimi
language English
description Oversteepened valley walls in western Norway have high recurrences of Holocene rock-slope failure activity causing significant risk to communities and infrastructure. Deposits from six to nine catastrophic rock-slope failure (CRSF) events are preserved at the base of the Mannen rock-slope instability in the Romsdal Valley, western Norway. The timing of these CRSF events was determined by terrestrial cosmogenic nuclide dating and relative chronology due to mapping Quaternary deposits. The stratigraphical chronology indicates that three of the CRSF events occurred between 12 and 10 ka, during regional deglaciation. Congruent with previous investigations, these events are attributed to the debuttressing effect experienced by steep slopes following deglaciation, during a period of paraglacial relaxation. The remaining three to six CRSF events cluster at 4.9 ± 0.6 ka (based on 10 cosmogenic 10Be samples from boulders). CRSF events during this later period are ascribed to climatic changes at the end of the Holocene thermal optimum, including increased precipitation rates, high air temperatures and the associated degradation of permafrost in rock-slope faces. Geomorphological mapping and sedimentological analyses further permit the contextualisation of these deposits within the overall sequence of post-glacial fjord-valley infilling. In the light of contemporary climate change, the relationship between CRSF frequency, precipitation, air temperature and permafrost degradation may be of interest to others working or operating in comparable settings. acceptedVersion © 2018. This is the authors' accepted and refereed manuscript to the article. The final authenticated version is available online at: https://journals.sagepub.com/doi/10.1177/0959683618798165
format Article in Journal/Newspaper
author Hilger, Paula
Hermanns, Reginald
Gosse, John C
Jacobs, B
Etzelmüller, Bernd
Krautblatter, Michael
spellingShingle Hilger, Paula
Hermanns, Reginald
Gosse, John C
Jacobs, B
Etzelmüller, Bernd
Krautblatter, Michael
Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating
author_facet Hilger, Paula
Hermanns, Reginald
Gosse, John C
Jacobs, B
Etzelmüller, Bernd
Krautblatter, Michael
author_sort Hilger, Paula
title Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating
title_short Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating
title_full Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating
title_fullStr Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating
title_full_unstemmed Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating
title_sort multiple rock-slope failures from mannen in romsdal valley, western norway, revealed from quaternary geological mapping and 10be exposure dating
publisher SAGE Publications
publishDate 2018
url http://hdl.handle.net/11250/2586526
https://doi.org/10.1177/0959683618798165
long_lat ENVELOPE(13.520,13.520,68.204,68.204)
geographic Mannen
Norway
geographic_facet Mannen
Norway
genre permafrost
genre_facet permafrost
op_source 1841-1854
28
The Holocene
12
op_relation The Holocene. 2018, 28 (12), 1841-1854.
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container_title The Holocene
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