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Landslide soils and geomorphology in Bridger-Teton National Forest, Northwest Wyoming

Auteur(s) et Affiliation(s)

ZUNG, A.B.
Dep. of Geography, Univ. Kansas, Lawrence, Etats-Unis
SORENSON, C.J.
Dep. of Geography, Univ. Kansas, Lawrence, Etats-Unis
WINTHERS, E.
USDA Forest Service, Bridger-Teton National Forest, Jackson, Etats-Unis


Description :
In this study, soil and geomorphic properties related to landslide occurence were studied at 18 landslides in the Bridger-Teton National Forest (BTNF). Landslides were categorized as active or inactive based on geomorphic features. Landslide soil characteristics including texture, shrink-swell potential, clay mineralogy, and horizonation were compared on active and inactive landslides. This study shows that soil characteristics and slope geomorphic properties may be useful for assessing landslide frequency. The results support a hypothesis that landslide occurence in the BTNF is related to weathering of soil and unconsolidated material, which affects clay mineralogy.


Type de document :
Article de périodique

Source :
Physical geography, issn : 0272-3646, 2009, vol. 30, n°. 6, p. 501-516, nombre de pages : 16, Références bibliographiques : 2 p.

Date :
2009

Editeur :
Pays édition : Royaume-Uni, Abingdon, Taylor and Francis

Langue :
Anglais
Droits :
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