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: Edward Arnold 2019
Subjects:
Online Access:http://hdl.handle.net/10852/72510
http://urn.nb.no/URN:NBN:no-75628
https://doi.org/10.1177/0959683618798165
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spelling ftoslouniv:oai:www.duo.uio.no:10852/72510 2023-05-15T17:57:27+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 2019-01-10T11:10:17Z http://hdl.handle.net/10852/72510 http://urn.nb.no/URN:NBN:no-75628 https://doi.org/10.1177/0959683618798165 EN eng Edward Arnold http://urn.nb.no/URN:NBN:no-75628 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. The Holocene. 2018, 28(12), 1841-1854 http://hdl.handle.net/10852/72510 1653886 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=The Holocene&rft.volume=28&rft.spage=1841&rft.date=2018 The Holocene 28 12 1841 1854 https://doi.org/10.1177/0959683618798165 URN:NBN:no-75628 Fulltext https://www.duo.uio.no/bitstream/handle/10852/72510/2/Hilger_etal2018_Multiple%2Brock-slope%2Bfailrues%2Bfrom%2BMannen_TheHolocene_Sept.pdf 0959-6836 Journal article Tidsskriftartikkel Peer reviewed AcceptedVersion 2019 ftoslouniv https://doi.org/10.1177/0959683618798165 2020-06-21T08:53:11Z 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. Article in Journal/Newspaper permafrost Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Mannen ENVELOPE(13.520,13.520,68.204,68.204) Norway The Holocene 28 12 1841 1854
institution Open Polar
collection Universitet i Oslo: Digitale utgivelser ved UiO (DUO)
op_collection_id ftoslouniv
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.
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 Edward Arnold
publishDate 2019
url http://hdl.handle.net/10852/72510
http://urn.nb.no/URN:NBN:no-75628
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 0959-6836
op_relation http://urn.nb.no/URN:NBN:no-75628
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. The Holocene. 2018, 28(12), 1841-1854
http://hdl.handle.net/10852/72510
1653886
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https://doi.org/10.1177/0959683618798165
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