Abstract
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.
Original language | English |
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Pages (from-to) | 289-293 |
Number of pages | 6 |
Journal | Eos, Transactions American Geophysical Union |
Volume | 84 |
Issue number | 31 |
DOIs | |
Publication status | Published - 5 Aug 2003 |
ASJC Scopus subject areas
- General Earth and Planetary Sciences