Tsunami hazards in the Eastern Mediterranean: strong earthquakes and tsunamis in the East Hellenic Arc and Trench system

G. A. Papadopoulos (1) , E. Daskalaki (1) , A. Fokaefs (1) , N. Giraleas (1)

1 Institute of Geodynamics [Athens]

Data on tsunami phenomena occurring in the East Hellenic Arc and Trench system (HA-T) from antiquity up to the present have been updated, critically evaluated and compiled in the standard GITEC format developed in the last decade for the New European Tsunami Catalogue. New field observations are presented for the tsunamis of 9 February 1948 and 24 March 2002. From the 18 tsunamis reported eight are rather well-documented while another nine remain doubtful. The mean recurrence of strong tsunamis is likely equal to about 142 years. Most of the tsunamis documented are caused by strong earthquakes occurring in the area offshore Rhodes to the east or northeast of the island. However, there are large earthquakes near Rhodes that do not cause tsunamis, like the 1926 and 1957 ones, which is of particular importance for the tsunami hazard assessment.

Domaines: Interfaces continentales, environnement; Océan, Atmosphère; Sciences de la Terre

G. A. Papadopoulos, E. Daskalaki, A. Fokaefs, N. Giraleas. Tsunami hazards in the Eastern Mediterranean: strong earthquakes and tsunamis in the East Hellenic Arc and Trench system. Natural Hazards and Earth System Sciences, 2007, 7 (1), pp.57-64. ⟨hal-00299403⟩