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dc.contributor.authorMuller, Cyril
dc.contributor.authorDel Potro, R.
dc.contributor.authorBiggs, Juliet
dc.contributor.authorGottsmann, Joachim
dc.contributor.authorVan der Laat, R.
dc.contributor.authorEbmeier, S. K.
dc.date.accessioned2021-03-25T18:29:23Z
dc.date.available2021-03-25T18:29:23Z
dc.date.issued2011
dc.identifier.urihttp://hdl.handle.net/11056/18989
dc.description.abstractHere we present initial conclusions of a one year-long combined geodesy campaign on Arenal Volcano, in Costa Rica (2008-2009). Our data shows evidence for an active local tectonic surrounding, and a 7cm/yr displacement field of the western flank of the volcano edifice that is in general agreement with recent INSAR studies. The study shows that a rigorous combination of simultaneous GPS, EDM (Electronic Distance Measurements) and triangulation measurements provide a time-cost effective approach to volcanic monitoring.es_ES
dc.language.isoenges_ES
dc.rightsAcceso abiertoes_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.titleCombined GPS, EDM and triangulation surveys of the rapid downslope motion of the western flank of Arenal Volcano, Costa Ricaes_ES
dc.typehttp://purl.org/coar/resource_type/c_8544es_ES
dc.description.procedenceUniversity of Bristoles_ES
dc.description.procedenceObservatorio Vulcanológico y Sismológico de Costa Rica (OVSICORI), Universidad Nacional.es_ES
dc.identifier.codproyectoV53C-2639


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