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The Holocene Storegga Slide tsunami in the United Kingdom

Smith, D.E. and Shi, S. and Cullingford, R.A. and Dawson, Alastair G. and Dawson, S. and Firth, C.R. and Foster, Ian D.L. and Fretwell, P.T. and Haggart, B.A. and Holloway, L.K. and Long, D. (2004) The Holocene Storegga Slide tsunami in the United Kingdom. Quaternary Science Reviews, 23 (23-24). pp. 2291-2321. ISSN 0277-3791

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Official URL: http://dx.doi.org/10.1016/j.quascirev.2004.04.001

Abstract

All currently known sites in the United Kingdom with evidence for the Holocene Storegga Slide tsunami are described. Information on the altitude, distribution, stratigraphical context, age, particle size profile and microfossil characteristics of the deposits is presented. The tsunami involved a greater area than previously described, reaching a coastline over 600 km long. The ubiquitous sand layer which forms the main deposit associated with the event is shown to exhibit a consistent morphology and a particle size profile marked by fining-upwards sequences. An analysis of new and previously published radiocarbon dates indicates that from evidence in the United Kingdom, the event took place sometime around 7100 radiocarbon years BP (7900 calibrated years BP). A new isobase model for mainland Scotland and adjacent areas, providing a preliminary estimate of land uplift since the tsunami, is presented. The model estimates contemporary sea surface level offshore at 14 m below the present day mean high water spring tides. Tsunami sediment run-up is greatest in inlets, where it reaches at least 25 m on Shetland and at least 5 m along the mainland coastline to the south, and run-up of the tsunami would have exceeded these values. The tsunami sediments identified here are considered particularly valuable as a synchronous marker horizon.

Item Type:Article
Research Community:University of Westminster > Life Sciences, School of
ID Code:6069
Deposited On:19 Feb 2009 14:53
Last Modified:16 Dec 2009 12:40

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