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Moraine de versant et confluences glaciaires

Etude de morphologie glaciaire sur le plateau de St-Nizier entre Drac et Furon

Bibliographic Data

ID9264426
AuthorsRobert Vivian, Monique Ricq de Bouard
Year1969
Volume57
Issue3
Pages529-543
Publication date1969-01-01
Open AccessYes
TypeARTICLE
VenueRevue de géographie alpine (JOURNAL)
Journal identifiersISSN: 0035-1121 • E-ISSN: 1760-7426
PublisherPERSEE Program (PUBLISHER)
DOI10.3406/rga.1969.3424
OpenAlexW2003387328
LanguageFR

St-Nizier plateau situated at the confluence point of the two big Isère and Drac-Romanche quaternary glaciers is covered with morainic deposits in a discontinuous way. The sedimentological and mineralogical study of these slope morainal deposits makes it clear that most of the plateau bas been worked by the ices of the Isère glacier whereas the influence of the Drac-Romanche glacier was decisive in that part only at the end of the disglaciation period and on the low slopes giving way up to the plateau

Geomorphology · Glacier · Moraine · Plateau (mathematics) · Quaternary · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Paleontology · Pleistocene-Era Hominins and Archaeology

Highly citedNo

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