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dc.contributor.authorVilímek, Vit
dc.contributor.authorZapata Luyo, Marco Alfonso
dc.contributor.authorKlimes, Jan
dc.contributor.authorPatzelt, Zdenek
dc.contributor.authorSantillán Portilla, Nelson
dc.coverage.spatialCordillera Blanca
dc.date.accessioned2019-02-11T16:34:29Z
dc.date.available2019-02-11T16:34:29Z
dc.date.issued2005
dc.identifier.citationVilímek, V., Zapata Luyo, M. A., Klimes, J. et al. (2018) Influence of glacial retreat on natural hazards of the Palcacocha Lake area, Peru. Landslides, 2, 107-115. doi: https://doi.org/10.1016/j.gloplacha.2007.11.003es_ES
dc.identifier.issnISSN: 1612-510X (Print) 1612-5118 (Online)es_ES
dc.identifier.urihttps://hdl.handle.net/20.500.12543/3338
dc.descriptionOriginal abstract: In this article we describe natural hazards associated with outburst floods of Palcacocha Lake and landslide events on the slopes of its moraine dam, in Cojup Valley, Cordillera Blanca (Peru). These events occurred in the last 70 years and some of them resulted in disasters, which strongly affected the city of Huar´as. Field investigations and reference expression hydrodynamic tests as well as archive satellite images and aerial pictures were used to describe the evolution of hazards connected with Palcacocha Lake. Expression hydrodynamic tests proved a high permeability of sandy gravels glacial sediments, which form the present-day lake dam. Seepage through the natural dam forming small ponds below the overflow spillways occurs. A retreat of the glacial tongue causing an increase of the lake volume and unloading of the slope toe areas are the most important recent processes that influence the potential hazards affecting the Cojup valley. The research has proved that the climate warming and ongoing deglaciation play a very significant.es_ES
dc.descriptionArtículo en período de embargoes_ES
dc.description.abstractDescribe los peligros naturales asociados con las inundaciones de arroyos del lago Palcacocha y los eventos de deslizamientos de tierra en las laderas de su presa de morrenas, en el valle de Cojup, Cordillera Blanca (Perú). Estos eventos ocurrieron en los últimos 70 años y algunos de ellos resultaron en desastres, que afectaron fuertemente a la ciudad de Huaraz.es_ES
dc.formatapplication/pdfes_ES
dc.language.isoenges_ES
dc.publisherSpringer Berlin Heidelberges_ES
dc.relation.ispartofseriesLandslides, July 2005, Volume 2, pp 107–115es_ES
dc.relation.urihttps://link.springer.com/article/10.1007/s10346-005-0052-6
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourceAutoridad Nacional del Aguaes_ES
dc.sourceRepositorio institucional - ANAes_ES
dc.subjectComportamiento de eventos extremos de origen glaciar y climáticoes_ES
dc.subjectGestión de riesgos de desastres en recursos hídricoses_ES
dc.subjectMonitoreo de lagunas y glaciareses_ES
dc.titleInfluence of glacial retreat on natural hazards of the Palcacocha Lake area, Perues_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.identifier.doihttps://doi.org/10.1016/j.gloplacha.2007.11.003es_ES


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