Die warmzeitlichen Ablagerungen am Rau de l’Amourette (Trièves, französiche Alpen)

Wilhelmus Gremmen, Christian Hannss & Jean Jacques Puissegur
At least two major climatic warm phases are attested by malacological and palynological evidence in dominantly clayish-silty sediments of the Trièves, an intra-montanic basin south of Grenoble. They belong probably to the Eem-Interglacial as well as to the Early Würm. The layers with the fossiles are found above local limestone gravels and underneath a moraine with cristalline components.