Articles | Volume 18, issue 5
https://doi.org/10.5194/nhess-18-1411-2018
https://doi.org/10.5194/nhess-18-1411-2018
Research article
 | 
23 May 2018
Research article |  | 23 May 2018

Characteristics and frequency of large submarine landslides at the western tip of the Gulf of Corinth

Arnaud Beckers, Aurelia Hubert-Ferrari, Christian Beck, George Papatheodorou, Marc de Batist, Dimitris Sakellariou, Efthymios Tripsanas, and Alain Demoulin

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ED: Publish subject to minor revisions (review by editor) (12 Mar 2018) by Thomas Glade
AR by Aurélia Hubert-Ferrari on behalf of the Authors (22 Mar 2018)  Author's response   Manuscript 
ED: Publish as is (30 Mar 2018) by Thomas Glade
AR by Aurélia Hubert-Ferrari on behalf of the Authors (01 May 2018)  Author's response   Manuscript 
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Short summary
Coastal and submarine landslides occur on average every 30–50 years at the western tip of the Gulf of Corinth. These landslides trigger tsunamis and thus represent a significant hazard. We realized an inventory of the submarine landslide deposits in the western Gulf. Six large events are identified in the last 130 000 years. Such sliding events likely generated large tsunami waves in the whole Gulf of Corinth, possibly larger than those reported in historical sources.
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