作者: Javier de Pedraza Gilsanz , Miguel A. Sanz , Jane Willenbring , Rosa M. Carrasco , David Domínguez Villar
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摘要: During the period of deglaciation last glacial cycle, a rock avalanche tooks place in cliffs of Los Hermanitos (Cuerpo de Hombre Valley, Sierra Bejar). The material displaced during avalanche fells over ice, was transported towards glacier front and later on deposited as supraglacial meltout till. origin is result decompression slopes valley after they have been liberated ice (paraglacial stress relaxation). Based geomorphological data and the implementation GIS, reconstruction masses main stages have been carried out order to quantify relaxation that produced collapse.