The Barrancas rock-avalanche, of northern Neuquén Province (Argentina): Its relation to the outburst flood of December 29, 1914

At some unknown time in the past, instability of the slope of C° Pelán resulted in a rock-avalanche that blocked the Barrancas valley as a landslide dam and formed the Carrilauquen lagoon. It is suggested that the trigger was a seismic shock, that resulted in complex movement of a proximal planar sl...

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Autores principales: González Díaz, E.F., Giaccardi, A.D., Costa, C.H.
Formato: JOUR
Materias:
dam
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v56_n4_p466_GonzalezDiaz
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