EL MODELADO GLACIAR EN LA VERTIENTE ORIENTAL DE LA SIERRA DE ANCARES (NOROESTE DE LA PENISULA IBÉRICA)
Abstract
The east valleys of Sierra de Ancares (NW Iberia) have been affected by the last glacial period. In this paper we describe many forms and deposits of three glacial complexes. The main ice sheets reached up to 13 Km. long and 280 m. depth. The location of deposits allow us to define three glacial stages in this part of the Cantabrian rangeDownloads
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