Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8090
AuthorsDe Martini, P. M.* 
Barbano, M. S.* 
Pantosti, D.* 
Smedile, A.* 
Pirrotta, C.* 
Del Carlo, P.* 
Pinzi, S.* 
TitleGeological evidence for paleotsunamis along eastern Sicily (Italy): an overview
Issue Date14-Aug-2012
Series/Report no./12 (2012)
DOI10.5194/nhess-12-2569-2012
URIhttp://hdl.handle.net/2122/8090
KeywordsTsunami depostits
tsunami hazard
Eastern Sicily
Subject Classification04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology 
04. Solid Earth::04.04. Geology::04.04.04. Marine geology 
AbstractWe present geological evidence for paleotsunamis along the 230 km-long coast of eastern Sicily (Italy); combining this information with historical data, we reconstruct a unique history of tsunami inundations. We integrate data on 38 paleotsunami deposits (from fine sand layers to boulders) collected at 11 sites (one offshore). The geological data record traces of large tsunamis which have occurred during the past 4 millennia. Chronological constrains include 14C, 210Pb and 137Cs, OSL and tephrochronology. When compatible, the age of the paleotsunami deposits is associated to historical events, but it is also used to highlight unknown tsunamis. Average tsunami recurrence interval (between 320 and 840 yr) and minimum inland tsunami ingressions (often greater than the historical ones) were estimated at several sites. On the basis of this work, the tsunami catalogue is implemented by two unknown tsunamis which occurred during the first millennium BC and by one unknown regional tsunami, which occurred in 650–770 AD. By including this latter event in the eastern Sicily catalogue, we estimate an average recurrence interval for strong tsunamis of ca. 385 yr. Comparison and merging of historical and geological data can definitely contribute to a better understanding of regional and local tsunami potential and provides robust parameters to be used in tsunami hazard estimates.
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