El glaciar noroccidental del Besiberri (Pirineo de Lérida)

The studied complex is a glacial debris system with three different areas: The upper, with an ice core covered by glacial debris and very active periglacial processes; the middle, a black glacier with a semi-covered part; and the lower, a rock glacier in the front of the complex. The end of the dyna...

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Bibliographic Details
Published in:Pirineos
Main Authors: Serrano, E., Martínez de Pisón, E., Martínez, R., Cantarino, I., Navarro, J.
Format: Article in Journal/Newspaper
Language:Spanish
Published: Consejo Superior de Investigaciones Científicas 1991
Subjects:
Online Access:https://pirineos.revistas.csic.es/index.php/pirineos/article/view/197
https://doi.org/10.3989/pirineos.1991.v137.197