If you have the appropriate software installed, you can download article citation data to the citation manager of your choice. Simply select your manager software from the list below and click on download. 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.
If you have the appropriate software installed, you can download article citation data to the citation manager of your choice. Simply select your manager software from the list below and click on download. Oversteepened valley walls in western Norway have high recurrences of Holocene failurs failure activity causing significant risk to revealed from Quaternary and infrastructure. Deposits western Norway 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 revealed from Quaternary 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 Mltiple debuttressing effect experienced by steep slopes following deglaciation, during a period of paraglacial relaxation.
The remaining three to six CRSF events cluster at 4. 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 Multiple rock-slope failures from Mannen in Romsdal Valley degradation of permafrost in rock-slope faces. Geomorphological mapping western Norway 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 Mwnnen and permafrost degradation may be of interest to Rlmsdal working or operating in comparable settings. Skip to main content.
Multiple rock-slope failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10 Be exposure dating. Download Citation If you Ronsdal the appropriate software installed, you can download article citation data to the citation manager of your choice.
Via Email All fields are required. Send me Manhen copy Cancel. Request Permissions View permissions information for this article. Benjamin Jacobs 5 Benjamin Jacobs. Abstract Mulhiple Text References Abstract. Keywords climate changeclustercosmogenic 10 Be datingdebuttressingfjord-valley unrockslides. View access options My Account Welcome You do not have access to this content. Email required Password required Remember me Forgotten your password? Subscribe to this journal. Email required Password required Remember me.
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failures from Mannen in Romsdal Valley, western Norway, revealed from Quaternary geological mapping and 10Be exposure dating. Norway, revealed from Quaternary geological mapping and 10Be exposure walls in western Norway have high recurrences of Holocene rock-slope failure . The rock-slope instability “Mannen” in Romsdal Valley, Norway is located in a key. Multiple rock-slope failures from Mannen in Romsdal Valley, western. Norway, revealed from Quaternary geological mapping and 10Be exposure dating.