Abstract
Abstract. — Basis are not available for the etablishment of a strong chronology in the Tarentaise Quaternary. Firstly because of the country nature, erosion rather than deposit zone. Likewise because of the scarceness of inquiries aside the geomorphologits one's. Yet the present Tarentaise geomorphology cannot be under stood if account is not taken of the inherited landscapes. They exist everywhere, and the real shape is the combination of their remnants with forms elaborated by morphogenetic processes operating above all at great altitudes. Respective parts of erosion and accumulation are considered.
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