Deglacial paleoseismicity in Sweden: the 9663 BP Iggesund event

Nils-Axel Mörner (Lead / Corresponding author), Per Einar Tröften, Rabbe Sjöberg, Douglas Grant, Sue Dawson, Christian Bronge, Ole Kvamsdal, Alf Sideén

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33 Citations (Scopus)

Abstract

The Iggeesund event is an example of the high seismicity which occurred in Fennoscandia during deglaciation as a function of the high rate of glacial isostatic uplift. This event is dated to varve 9663 BP. The Iggesund-Hudiksvall area is represented by intensive postglacial fracturing of the bedrock recorded over an area of at least, 50 x 50 km. The most remarkable locality is the Boda cave system; a hill fractured into a field of large detached blocks with a cave system of more than 2 km length. In the varve-year 9663 BP, an extensive turbidite was spread over an area of 210 x 80 km. Liquefaction structures are recorded over an area of 80 x 30 km and can be assigned to the same varve year. Structures and deposits of a tsunami are recorded over 80 x 50 km.

Original languageEnglish
Pages (from-to)1461-1468
Number of pages8
JournalQuaternary Science Reviews
Volume19
Issue number14-15
Early online date22 Sep 2000
DOIs
Publication statusPublished - 1 Oct 2000

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    Mörner, N-A., Tröften, P. E., Sjöberg, R., Grant, D., Dawson, S., Bronge, C., Kvamsdal, O., & Sideén, A. (2000). Deglacial paleoseismicity in Sweden: the 9663 BP Iggesund event. Quaternary Science Reviews, 19(14-15), 1461-1468. https://doi.org/10.1016/S0277-3791(00)00095-0