IGB

Connexion

(Article of periodic en Anglais - 1995)

Document title

Diversion of the upper Bear River: glacial diffluence and Quaternary erosion, Sierra Nevada, California

published at : Special issue. Glacial geomorphology: process and form development

Authors(s) and Affiliation(s)

JAMES L.A. ;

Abstract

Deep canyon erosion and diversion of more than 300 km[2] of the former upper Bear River is documented with stratigraphic and morphologic evidence. A hypothesis is presented that the channel diversion and much of the local South Yuba valley incision at the site were induced by glacial erosion during the Quaternary period

Source

Thematical fascicle

published at : Geomorphology / ISSN 0169-555X

Editor : Elsevier, Amsterdam - PAYS-BAS (1987)

Millesime : 1995, vol. 14, no 2 [pp. 131-148]

Bibliographic references : 37 ref.

Language

Anglais

INIST-CNRS, Cote INIST : 21151

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1996.
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