Mots-clés
Argile minéral ; Eau souterraine ; England ; Erosion ; Géomorphogenèse ; Lithologie ; Minéralogie ; Royaume-Uni ; Réseau de drainage ; Vallée ; Yorkshire ; Zone tempéréeClay mineral ; Drainage network ; England ; Erosion ; Geomorphogenesis ; Groundwater ; Lithology ; Mineralogy ; Temperate zone ; United Kingdom ; Valley ; YorkshireGroundwater sapping and valley development in the Hackness Hills, North Yorkshire, England
Auteur(s) et Affiliation(s)
NASH, D.J.
Earth and Environmental Science Research Unit, University of Brighton, Brighton, Royaume-Uni
Description :
This paper presents the first study of valley development in the Hackness Hills and, through an analysis of the links between lithological variation and valley morphology, suggests that groundwater sapping processes played a major role in valley formation. As such, this study aims to broaden the knowledge of groundwater erosion processes, particularly in humid temperate areas. The emphasis of this study is predominantly morphological and is intended to provide a basis for future process-oriented investigations.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 1996, vol. 21, n°. 9, p. 781-795, Collation : Illustration, Références bibliographiques : 42 ref.
Date :
1996
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)