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A Holocene tsunami deposit in eastern Scotland |
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| Authors: | David Long David E. Smith Alastair G. Dawson |
| Abstract: | A thin, regionally extensive, laterally persistent sand layer identified within the Holocene coastal sequences of eastern Scotland, dated to 7000 years BP, is suggested to be a tsunami deposit. The likely source of the tsunami wave is the earthquake induced second Storegga Slide on the Norwegian continental slope at least 750 km northeast of the deposit. |
| Keywords: | Holocene eastern Scotland tsunami deposit North Sea earthquake |