Géomorphologie et Quaternaire en Tarentaise. Etat actuel des connaissances
Bibliographic Data
| ID | 9266293 |
|---|---|
| Authors | Yves Bravard (corresponding author) |
| Year | 1969 |
| Volume | 57 |
| Issue | 3 |
| Pages | 571-592 |
| Publication date | 1969-01-01 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Revue de géographie alpine (JOURNAL) |
| Journal identifiers | ISSN: 0035-1121 • E-ISSN: 1760-7426 |
| Publisher | PERSEE Program (PUBLISHER) |
| DOI | 10.3406/rga.1969.3427 |
| OpenAlex | W2085301791 |
| Language | FR |
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 velocity | historical |
|---|---|
| Highly cited | No |