@incollection{brebbia_jubaguerra_2004,
	address = {Southampton},
	series = {Management {Information} {Systems}},
	title = {The {Jubaguerra} stream event: analysis of a mass movement connected with a flash flood phenomenon and its application to other areas in the {Gredos} {Mountains} ({Central} {Spain})},
	volume = {9},
	isbn = {1470-6326 1-85312-736-1},
	shorttitle = {The {Jubaguerra} stream event: analysis of a mass movement connected with a flash flood phenomenon and its application to other areas in the {Gredos} {Mountains} ({Central} {Spain})},
	url = {://000226374700030},
	abstract = {Mass movements have been a predominant shaping process on the Jerte Valley slopes (Gredos Mountains, Spain) during the Quaternary time. The present day activity of these mass movements is characterized as either 'first-time failures' (shallow debris slides and debris flows) or 'reactivations' of pre-existing landslide deposits. The Jubaguerra event, a debris slide which took place on January the 24(th), 1996, is a good example of these 'first-time failures' and its associated hazard. In this paper, a hydrogeotechnical and morphological characterisation of the Jubaguerra failure is made. Once these factors were defined, they were input in a GIS, and a prospective model, applicable to the Gredos Mountains, has been made. In this model, areas with the same characteristics of the Jubaguerra failure are mapped.},
	language = {English},
	booktitle = {Risk {Analysis} {Iv}},
	publisher = {Wit Press},
	author = {Pedraza, J. and Carrasco, R. M. and Bodoque, J. M. and Sanz, M. A. and Martin-Duque, J. F. and Gonzalez, A. and Diez, A.},
	editor = {Brebbia, C. A.},
	year = {2004},
	keywords = {\#nosource, LANDSLIDES, MODEL, SURFACE SATURATION, Spanish, VALLEY, centralsSystem, debris slide, flash flood, natural hazards, zones},
	pages = {345--358},
}

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F.","Gonzalez, A.","Diez, A."],"bibdata":{"bibtype":"incollection","type":"incollection","address":"Southampton","series":"Management Information Systems","title":"The Jubaguerra stream event: analysis of a mass movement connected with a flash flood phenomenon and its application to other areas in the Gredos Mountains (Central Spain)","volume":"9","isbn":"1470-6326 1-85312-736-1","shorttitle":"The Jubaguerra stream event: analysis of a mass movement connected with a flash flood phenomenon and its application to other areas in the Gredos Mountains (Central Spain)","url":"://000226374700030","abstract":"Mass movements have been a predominant shaping process on the Jerte Valley slopes (Gredos Mountains, Spain) during the Quaternary time. The present day activity of these mass movements is characterized as either 'first-time failures' (shallow debris slides and debris flows) or 'reactivations' of pre-existing landslide deposits. The Jubaguerra event, a debris slide which took place on January the 24(th), 1996, is a good example of these 'first-time failures' and its associated hazard. In this paper, a hydrogeotechnical and morphological characterisation of the Jubaguerra failure is made. Once these factors were defined, they were input in a GIS, and a prospective model, applicable to the Gredos Mountains, has been made. 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