Evolución geomorfológica del karst y paleoambientes cuaternarios en el macizo de Patones-Cerro de la Oliva (Madrid)

Abstract

Geomorphological, sedimentological and palaeontological evidences allowed to identify several phases in the evolution of the Patones-Cerro c/e la Oliva karstic massif. The studied speleothems, jointly with data of previous works indicate the presence of at least five episodes of chemical precipitation under favorable climatic conditions during isotopic stages 9-11?, 7, 5, 4-3 and 7, respectively