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Deposits from landslides and avalanches triggered by seismic activity in swedish lapland
Responsible organisation
2010 (English)In: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Geografiska Annaler: Series A, Physical Geography, Vol. 92, no 3, p. 411-420Article in journal (Refereed) Published
Abstract [en]

Abstract.In the mountain area of Swedish Lapland, landforms with semicircular or horse‐shoe ridges encircling hummocky ground occur. They are interpreted as landslide or avalanche deposits directly upon, from or adjacent to down‐wasting ice. Since they are restricted to the vicinity of fault scarps in the Pärvie fault system the releasing factor is suggested to be displacement of bedrock blocks or related seismic activity.

Place, publisher, year, edition, pages
Taylor & Francis , 2010. Vol. 92, no 3, p. 411-420
National Category
Natural Sciences
Identifiers
URN: urn:nbn:se:polar:diva-8175DOI: 10.1111/j.1468-0459.2010.00404.xOAI: oai:DiVA.org:polar-8175DiVA, id: diva2:1289117
Available from: 2019-02-15 Created: 2019-02-15 Last updated: 2019-02-15

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Publisher's full texthttps://doi.org/10.1111/j.1468-0459.2010.00404.x
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Geografiska Annaler. Series A, Physical Geography
Natural Sciences

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