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Géomorphologie et Quaternaire en Tarentaise. Etat actuel des connaissances

Bibliographic Data

ID9266293
AuthorsYves Bravard (corresponding author)
Year1969
Volume57
Issue3
Pages571-592
Publication date1969-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueRevue de géographie alpine (JOURNAL)
Journal identifiersISSN: 0035-1121 • E-ISSN: 1760-7426
PublisherPERSEE Program (PUBLISHER)
DOI10.3406/rga.1969.3427
OpenAlexW2085301791
LanguageFR

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

Aside · Chronology · Erosion · Geography · Geomorphology · Quaternary · Geological and Geophysical Studies Worldwide · Geology · Geology and Paleoclimatology Research · Geotourism and Geoheritage Conservation · Paleontology · Philosophy

Citation velocityhistorical
Highly citedNo

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