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Deposits from landslides and avalanches triggered by seismic activity in swedish lapland
Ansvarlig organisasjon
2010 (engelsk)Inngår i: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Geografiska Annaler: Series A, Physical Geography, Vol. 92, nr 3, s. 411-420Artikkel i tidsskrift (Fagfellevurdert) 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.

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Taylor & Francis , 2010. Vol. 92, nr 3, s. 411-420
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URN: urn:nbn:se:polar:diva-8175DOI: 10.1111/j.1468-0459.2010.00404.xOAI: oai:DiVA.org:polar-8175DiVA, id: diva2:1289117
Tilgjengelig fra: 2019-02-15 Laget: 2019-02-15 Sist oppdatert: 2019-02-15

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Forlagets fullteksthttps://doi.org/10.1111/j.1468-0459.2010.00404.x
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