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dc.contributor.authorRodríguez Vidal, Joaquín 
dc.contributor.authorCáceres Puro, Luis Miguel 
dc.contributor.authorGonzález-Regalado Montero, María Luz 
dc.contributor.authorGómez Gutiérrez, Paula
dc.contributor.authorClemente Pérez, M. J.
dc.contributor.authorRuiz Muñoz, Francisco 
dc.contributor.authorToscano Grande, Antonio 
dc.contributor.authorAbad de los Santos, Manuel 
dc.date.accessioned2015-09-11T10:27:55Z
dc.date.available2015-09-11T10:27:55Z
dc.date.issued2015
dc.identifier.citationRodríguez Vidal, J., Cáceres Puro, L.M., González-Regalado Montero, M.L., Gómez Gutiérrez, P., Clemente Pérez, M.J., Ruiz Muñoz, F., Toscano Grande, A., Abad de los Santos, M.: "Las grietas de acantilado como un nuevo registro de tsunamitas : ejemplo en la costa de Gibraltar". En: Una visión global del Cuaternario. El hombre como condicionante de procesos geológicos (J. P. Galve, J. M. Azañón, J. V. Pérez Peña y P. Ruano, Eds.), págs. 31-32. XIV Reunión Nacional de Cuaternario, Granada (España).
dc.identifier.urihttp://hdl.handle.net/10272/11100
dc.description.abstractMain tsunami records around the world coasts are associated with low-lying sandy coasts or estuarine areas. In the Rock of Gibraltar formed by limestone cliffs these records are less common and they are limited to the lagoon (The Inundation) located at the isthmus that joins the Rock with the mainland. Tsunamigenic deposits filling deep open crevices that record marine events since ca. 3,000 years BP have been studied at the southwestern end, i.e. Rosia Bay. The most represented deposits could be related with both Atlantic and Mediterranean tsunamis occurred in ~1000 BC, 218-209 BC, 60 AD, 365 AD and 1755 AD. These new tsunamite-type evidence represent a complementary tool in the geological analysis and chronology of these high-energy marine events.en_US
dc.language.isospaen_US
dc.publisherAsociación Española para el Estudio del Cuaternarioen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherTsunamitaen_US
dc.subject.otherCosta rocosaen_US
dc.subject.otherHolocenoen_US
dc.subject.otherEstrecho de Gibraltaren_US
dc.subject.otherRock coasten_US
dc.subject.otherHoloceneen_US
dc.subject.otherStrait of Gibraltaren_US
dc.titleLas grietas de acantilado como un nuevo registro de tsunamitas : ejemplo en la costa de Gibraltaren_US
dc.typeinfo:eu-repo/semantics/conferenceObjecten_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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