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