Mots-clés
Analyse isotopique ; Cycle d'érosion ; Datation ; Erosion glaciaire ; Glaciaire ; Grotte ; Interglaciaire ; Quaternaire ; Royaume-Uni ; Scotland ; Uranium ; Vallée glaciaire ; Vitesse d'érosionCave ; Dating ; Erosion cycle ; Erosion rate ; Glacial erosion ; Glacial features ; Glacial valley ; Interglacial ; Isotope analysis ; Quaternary ; Scotland ; United Kingdom ; UraniumRate of glacial valley deepening during the Late Quaternary in Assynt, Scotland
Special Issue: Geomorphic processes/landscape evolution
Auteur(s) et Affiliation(s)
HEBDON, N.J.
School of Environmental Sciences, University of East Anglia, Norwich, Royaume-Uni
Description :
A dated landscape history of the Allt nan Uamh valley in the Assynt area is constructed, spanning the last 300 ka, using geomorphological analysis, U-series speleothem dating, and existing cave surveys. The mean rate of valley deepening is estimated to lie between 47 and 68 m per glacial/interglacial cycle of 100 ka. This, combined with an estimated duration of glaciation, implies glacial erosion rates in agreement with modern process measurements.
Type de document :
Congrès
Source :
Symposium British Geomorphological Research Group (BGRG), Glasgow, Royaume-Uni, 1996-01-04, Earth surface processes and landforms, issn : 0197-9337, 1997, vol. 22, n°. 3, p. 307-315, Collation : Illustration, Références bibliographiques : 20 ref.
Date :
1997
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)