Geomorphological evidences of paleosurge activity in Lake Viedma Lobe, Patagonia, Argentina

The valley of Lake Viedma represents one of the main ice flow axes during the Quaternary glaciations of Patagonia. Geomorphological mapping of the eastern sector of the lake, between the shoreline and the end moraine systems attributed to the Last Glaciation, allowed us to recognize a large number o...

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Detalles Bibliográficos
Autores principales:	Ponce, J.F., González Guillot, M., Díaz Balocchi, L., Martínez, O.
Formato:	JOUR
Materias:	Glacial geomorphology Last glaciation Paleosurge activity Patagonia geomorphological mapping glaciation ice flow ice margin last glaciation moraine subglacial environment
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_0169555X_v327_n_p511_Ponce
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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