Mots-clés
Charge solide ; Cumbria ; Ecoulement fluvial ; England ; Fluviatile ; Géométrie hydraulique ; Hydrodynamique ; Lit fluvial ; Paléohydrologie ; Royaume-UniChannel geometry ; Cumbria ; England ; Fluvial processes ; Hydrodynamics ; Palaeohydrology ; River bed ; Sediment load ; Stream flow ; United KingdomFlow-separation berms downstream of a hydraulic jump in a bedrock channel
Auteur :CARLING, P.A.
Description :
The purpose of this paper is to report the first direct observation of the phenomenon of gravel berm formation, downstream of a hydraulic jump. As the observations were fortuitous, detailed measurements of hydraulic conditions were not possible but estimates were obtained. These observations are compared with laboratory experiments and theory. The deposits have significance in constraining flood palaeoflow reconstructions as the presence of berms determines the former location of hydraulic jumps.
Type de document :
Article de périodique
Source :
Geomorphology (Amsterdam), issn : 0169-555X, 1995, vol. 11, n°. 3, p. 245-253, Collation : Illustration, Références bibliographiques : 27 ref.
Date :
1995
Editeur :
Pays édition : Pays-Bas, Amsterdam, Elsevier
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)