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Post-glacial fault scarps in Jämtland, central Sweden
Högskolan Dalarna, Akademin Utbildning, hälsa och samhälle, Geografi.
2015 (engelsk)Inngår i: GFF, ISSN 1103-5897, E-ISSN 2000-0863, Vol. 137, nr 4, s. 339-343Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Analysis of a light detection and ranging-derived digital elevation model has revealed previously unknown fault scarps in central Jämtland, Sweden. These are interpreted to have been formed by earthquakes at the time of deglaciation, c. 10 ka BP, in an area with current low-magnitude seismicity. The dating is based upon morphology and comparison with similar features at other locations in Sweden but not supported by independent dating. Observed scarps are 0.4–6 km long, 2–8 m high, trending SSW–NNE to WSW–ENE, the northern and western sides uplifted. The dimensions of the scarps suggest an approximate moment magnitude M 7 of the strongest corresponding earthquakes.

sted, utgiver, år, opplag, sider
2015. Vol. 137, nr 4, s. 339-343
Emneord [en]
light detection and ranging, palaeoseismicity, post-glacial fault, Sweden
HSV kategori
Forskningsprogram
Utbildning och lärande
Identifikatorer
URN: urn:nbn:se:du-19797DOI: 10.1080/11035897.2015.1036361ISI: 000367018000008OAI: oai:DiVA.org:du-19797DiVA, id: diva2:862436
Tilgjengelig fra: 2015-10-22 Laget: 2015-10-22 Sist oppdatert: 2017-12-01bibliografisk kontrollert

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