Department of Civil Engineering, Universidad Catolica de la Ssma Concepcion

dc.creatorAránguiz, R.,
dc.creatorVillagrán, M.
dc.date2020-03-11T20:29:43Z
dc.date2022-07-07T23:55:46Z
dc.date2020-03-11T20:29:43Z
dc.date2022-07-07T23:55:46Z
dc.date2012
dc.date.accessioned2023-08-22T11:42:34Z
dc.date.available2023-08-22T11:42:34Z
dc.identifier15110017
dc.identifier15110017
dc.identifierhttps://hdl.handle.net/10533/238891
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8345189
dc.descriptionThe 2010 Chile tsunami affected the entire coast of the Biobio Region, where several bays were flooded, and seawater surged hundreds of meters into rivers. However, no inundation occurred in the 2km wide Biobio River, located at the northern entrance of t
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.9753/icce.v33.currents.5
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleThe effect of a submarine canyon on tsunami propagation in the gulf of Arauco, Chile
dc.titleDepartment of Civil Engineering, Universidad Catolica de la Ssma Concepcion
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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