Flujos densos en los Valles Calchaquies, Andes Centrales de Argentina

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dc.contributor.authorBarrientos, Celia D.
dc.contributor.authorAlonso, Ricardo N.
dc.date.accessioned2014-12-16T12:50:59Z
dc.date.available2014-12-16T12:50:59Z
dc.date.issued2001
dc.description.abstractThe eastern slope of the Central Andes is an interesting geological observatory for the study of mass movements. Giant land-slides, mud-flows, debris-flows and flash-floods occur frequently. During the austral summer season (December to March), Calchaqui Valleys are the theatre of several mud-flows. We have also evidences of several phenomena in the historical time. We report here two localities with past mass movements (San Lucas and Santa Rosa). These localities constitute a site for potential geological hazard mainly during the ENSO (El Niño/ La Niña) yearsen_US
dc.identifier.urihttp://hdl.handle.net/10272/9544
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMud-flowsen_US
dc.subject.otherDebris-flowsen_US
dc.subject.otherSaltaen_US
dc.subject.otherArgentinaen_US
dc.subject.otherCalchaqui Valleysen_US
dc.titleFlujos densos en los Valles Calchaquies, Andes Centrales de Argentinaen_US
dc.titleMud flows in the eastern slope of the Central Andes (Calchaqui Valleys), Argentinaeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 30, (2001)