Mots-clés
Bilan sédimentaire ; British Columbia ; Canada ; Holocène ; Modèle ; Paraglaciaire ; Réseau de drainage ; ValléeBritish Columbia ; Canada ; Drainage network ; Holocene ; Model ; Paraglacial ; Sediment budget ; ValleyBalance sedimentario ; Canada ; Colombia Británica ; Holoceno ; Modelo ; Paraglaciar ; Red de drenaje ; ValleScale variation of post-glacial sediment yield in Chilliwack Valley, British Columbia
Auteur(s) et Affiliation(s)
TUNNICLIFFE, J.F.
Department of Geography, The University of British Columbia, Vancouver, Canada
CHURCH, M.
Department of Geography, The University of British Columbia, Vancouver, Canada
Description :
The Holocene volumetric sediment budget is estimated for coarse textured sediments (sand and gravel) in a large, formerly glaciated valley in southwest British Columbia. Erosion is estimated by compiling volumetric loss estimated in digital elevation models (DEMs) of gullied topography and by applying a non-linear diffusion model on planar, undissected hillslopes. Estimates of steepland yield are based on estimates of post-glacial deposition volumes in fans, cones and deltas at the outlets of low-order tributary catchments. Results are classed by catchment order and compared across scales of contributing area. A simple network routing model emphasizes the significant sediment flux contributions from colluvium, drift blankets and gullies in steeper terrain.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 2011, vol. 36, n°. 2, p. 229-243, nombre de pages : 15, Références bibliographiques : 60 ref.
Date :
2011
Editeur :
Pays édition : Royaume-Uni, Chichester, Wiley
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)