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(Article of periodic en Anglais - 1997)

Document title

Evidence for cirque glaciation in the Colorado Front Range during the Younger Dryas chronozone

Authors(s) and Affiliation(s)

MENOUNOS B. (1) ; REASONER M.A. ;
(1) Inst. Artic and Alpine Research, Dep. Geography, Univ. Colorado, Boulder, ETATS-UNIS

Abstract

The AA. present evidence that indicates a limited advance of alpine glaciers occured in the Colorado Front Range Mountains during the Younger Dryas Chron. Sky Pond was selected for this study because it is situated directly downvalley from a moraine with relative-age features similar to those of early Holocene to late Pleistocene glacial landforms in the Colorado Front Range

Source

Article of periodic

published at : Quaternary research / ISSN 0033-5894 / CODEN QRESAV

Editor : Elsevier, San Diego, CA - ETATS-UNIS (1970)

Millesime : 1997, vol. 48, no1 [pp. 38-47]

Bibliographic references : 60 ref.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 15739

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1997.
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