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dc.creatorMora Fernández, Mauricio
dc.creatorPeraldo Huertas, Giovanni
dc.date2010-06-16
dc.date.accessioned2016-05-03T14:24:39Z
dc.date.available2016-05-03T14:24:39Z
dc.identifierhttp://revistas.ucr.ac.cr/index.php/geologica/article/view/3445
dc.identifier10.15517/rgac.v0i44.3445
dc.identifier.urihttps://hdl.handle.net/10669/22424
dc.descriptionThis research integrates information from documents and testimonies about the effects of the Buenavista Earthquake, July 3rd 1983 (Ms = 6,1) in Costa Rica. From this documentation, it has been possible to reconstruct a local intensity map, and furthermore to understand the perception and social representations that the population draw as explanations about the earthquake source. Maximum intensities occurred northward of Rivas town (VIII-IX), showing an elongated pattern striking NNW. The integration of all primary and secondary information which has been taken and analyzed, suggests a seismic source striking E-W or NW-SE, located north of Buenavista town. The social interpretations to explain the Buenavista Earthquake were focused on ?divine punishment? (?the final judgement?), volcanic activity or collapsing caverns.es-ES
dc.formatapplication/pdf
dc.languagespa
dc.publisherUniversidad de Costa Ricaes-ES
dc.relationRevista Geológica de América Central;
dc.rightsCopyright (c) 2014 Revista Geológica de América Centrales-ES
dc.sourceRevista Geológica de América Central; Revista Geológica de América Central: Número 44en-US
dc.sourceRevista Geológica de América Central; Revista Geológica de América Central: Número 44es-ES
dc.source2215-261X
dc.source0256-7024
dc.titleAnálisis macrosísmico del terremoto de buena vista de Pérez Zeledón, 3 de julio de 1983 (ms = 6,1), Costa Ricaes-ES
dc.typeartículo original
dc.coverageCRCes-ES


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