NUMERICAL SIMULATION OF THE 7 FEBRUARY 1963 TSUNAMI IN THE BAY OF CORINTH, GREECE

dc.contributor.author	Lobkovsky L.I.
dc.contributor.author	Mazova R.Kh.
dc.contributor.author	Garagash I.A.
dc.contributor.author	Kataeva L.Yu.
dc.date.accessioned	2025-03-22T08:33:32Z
dc.date.available	2025-03-22T08:33:32Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=21518534
dc.identifier.citation	Russian Journal of Earth Sciences, 2006, 8, 5, ES5003
dc.identifier.issn	1681-1208
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/48599
dc.description.abstract	The paper addresses the event that occurred in the Bay of Corinth, Greece, on 7 February 1963. The tsunami was produced by a submarine landslide in the mouth of the local Salmenikos River. The paper presents preliminary numerical results obtained in terms of an elastoplastic model for the surface water waves generated by the landslide and propagated onto the coast. The wave propagation is analyzed as a function of the landslide movement. The inferred results are compared with those obtained in terms of other models.
dc.subject	TSUNAMI GENERATION
dc.subject	SHALLOW WATER EQUATIONS
dc.subject	ASEISMIC TSUNAMI
dc.subject	SEDIMENTARY MASS
dc.title	NUMERICAL SIMULATION OF THE 7 FEBRUARY 1963 TSUNAMI IN THE BAY OF CORINTH, GREECE
dc.type	Статья
dc.identifier.doi	10.2205/2006ES000210

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