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Tsunamis as Paleoseismic Indicators

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Synonyms

High-energy deposits; Tsunami deposits; Tsunamigenic layers; Tsunamiites; Tsunamites

Introduction

Tsunami waves are the result of a large mass of water being displaced by different processes. Earthquake-induced tsunamis have small wave heights offshore and very long wavelengths up to several hundred kilometers (line source tsunami). This is in contrast to tsunamis caused by mass movements (subaerial or underwater origin), volcanic eruptions and explosions, glacier calvings, or meteorite impacts, which have very high waves and very short wavelengths close to the origin (point source tsunami).

More than 85 % of tsunamis have tectonic causes such as fault movements (5 % are caused by volcanic activity, 5 % by landslides, and 5 % by a combination of all other causes; impact tsunamis are very rare), and 80 % of these occur in the Pacific Ocean; other oceans and seas have also been affected by tsunamis like the Mediterranean Sea. Tsunami evidence has also been found on the...

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Correspondence to Klaus Reicherter .

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Reicherter, K. (2021). Tsunamis as Paleoseismic Indicators. In: Beer, M., Kougioumtzoglou, I., Patelli, E., Au, IK. (eds) Encyclopedia of Earthquake Engineering. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-36197-5_26-1

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  • DOI: https://doi.org/10.1007/978-3-642-36197-5_26-1

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