Mots-clés
Colluvions ; Dynamique de versant ; Etats-Unis ; Glacier rocheux ; Géomorphodynamique ; Montagne ; Paléoclimat ; Paléogéomorphologie ; Pergélisol ; Périglaciaire ; Stratigraphie ; UtahColluvium ; Earth surface processes ; Mountain ; Palaeoclimate ; Palaeogeomorphology ; Periglacial features ; Permafrost ; Rock glacier ; Slope dynamics ; Stratigraphy ; United States of America ; UtahOrigin of fossil rock glaciers, La Sal Mountains, Utah
Auteurs :NICHOLAS, J.W.
GARCIA, J.E.
Description :
This paper presents an investigation of one of several boulder deposits on the northwest flanks of the La Sal Mountains, in Utah. A deductive approach is used to determine the most likely scenario surrounding the formation of one of these lobes. Several alternative scenarios are presented and evaluated in light of available evidence. Evidence consists of surface morphology, subsurface geology, stratigraphic relationships, present and past climatic conditions, and fabric analysis. The lobe was compared to other similar types of deposits, and the AA. conclude that it is a fossil permafrost-derived rock glacier.
Type de document :
Article de périodique
Source :
Physical geography, issn : 0272-3646, 1997, vol. 18, n°. 2, p. 160-175, Collation : Illustration, Références bibliographiques : 49 ref.
Date :
1997
Editeur :
Pays édition : Royaume-Uni, Abingdon, Taylor and Francis
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)