Record-breaking height for 8000-year-old tsunami in the North Atlantic

One of the largest Holocene sub‐marine slides mapped on Earth is the Storegga slide offshore Norway [Bugge, 1987] (Figure 1). Approximately 3500 km3 material slid out and generated a huge tsunami dated to about 7300 14C yr BP [Bondevik et al., 1997a], or ca 8150 calendar years BP. The tsunami is kno...

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Bibliographic Details
Published in:Eos, Transactions American Geophysical Union
Main Authors: Bondevik, Stein, Mangerud, Jan, Dawson, Sue, Dawson, Alastair, Lohne, Øystein
Format: Article in Journal/Newspaper
Language:English
Published: 2003
Subjects:
Online Access:https://discovery.dundee.ac.uk/en/publications/1807a2c7-c984-4ae5-affb-e5e14f9eb6a9
https://doi.org/10.1029/2003EO310001
http://www.scopus.com/inward/record.url?scp=70449906372&partnerID=8YFLogxK
Description
Summary:One of the largest Holocene sub‐marine slides mapped on Earth is the Storegga slide offshore Norway [Bugge, 1987] (Figure 1). Approximately 3500 km3 material slid out and generated a huge tsunami dated to about 7300 14C yr BP [Bondevik et al., 1997a], or ca 8150 calendar years BP. The tsunami is known from onshore deposits in Norway [Bondevik et al., 1997a], on the Faroe Islands [Grauert et al., 2001], and in Scotland [Dawson et al., 1993]. Of these, the tsunami deposits in western Norway reaches the highest elevation, indicating a runup of 10–12 m. In this article, we demonstrate that at the Shetland Islands between Norway and Scotland (Figure 1), this tsunami reached onshore heights at least 20 m above the sea level of that time.