Mots-clés
Appalachian Mountains ; Bassin-versant ; Distribution spatiale ; Erosion ; Etats-Unis ; Evolution post-orogénique ; Lit fluvial ; Modèle ; Modèle conceptuel ; Mouvement de masse ; North Carolina ; Pente de versant ; Profil longitudinal ; Rupture de penteAppalachian Mountains ; Conceptual model ; Erosion ; Knickpoint ; Longitudinal section ; Mass movement ; Model ; North Carolina ; Post-orogenic evolution ; River bed ; Slope gradient ; Spatial distribution ; United States of America ; WatershedAppalaches ; Carolina del Norte ; Cauce ; Cuenca hidrográfica ; Distribución espacial ; Erosión ; Estados Unidos ; Inclinación de la vertiente ; Modelo ; Modelo conceptual ; Movimiento de masa ; Perfil longitudinalHillslope response to knickpoint migration in the Southern Appalachians: implications for the evolution of post-orogenic landscapes
Auteur(s) et Affiliation(s)
GALLEN, S.F.
Dep. of Marine, Earth, and Atmospheric Sciences, North Carolina State Univ., Raleigh, Etats-Unis
WEGMANN, K.W.
Dep. of Marine, Earth, and Atmospheric Sciences, North Carolina State Univ., Raleigh, Etats-Unis
FRANKEL, K.L.
School of Earth and Atmospheric Sciences, Georgia Inst. of Technology, Atlanta, Etats-Unis
HUGHES, S.
Dep. of Marine, Earth, and Atmospheric Sciences, North Carolina State Univ., Raleigh, Etats-Unis
LEWIS, R.Q.
Dep. of Marine, Earth, and Atmospheric Sciences, North Carolina State Univ., Raleigh, Etats-Unis
LYONS, N.
Dep. of Marine, Earth, and Atmospheric Sciences, North Carolina State Univ., Raleigh, Etats-Unis
PARIS, P.
Dep. of Marine, Earth, and Atmospheric Sciences, North Carolina State Univ., Raleigh, Etats-Unis
ROSS, K.
Dep. of Marine, Earth, and Atmospheric Sciences, North Carolina State Univ., Raleigh, Etats-Unis
BAUER, J.B.
North Carolina Geological Survey, Swannanoa, Etats-Unis
WITT, A.C.
North Carolina Geological Survey, Swannanoa, Etats-Unis
Description :
Values of normalized hypsometry, hypsometric integral, and mean slope vs elevation are used in south-western North Carolina for 14 tributary basins and the Cullasaja basin as a whole to characterize landscape evolution following upstream knickpoint migration. Results highlight the existence of a transient spatial relationship between knickpoints present along the fluvial network of the Cullasaja basin and adjacent hillslopes. This transient effect of knickpoint-driven channel incision on basin hillslopes is captured by measuring the relief, mean slope steepness, and mass movement frequency of tributary basins and comparing these results with the distance from major knickpoints along the Cullasaja River. A conceptual model of area–elevation and slope distributions is presented that may be representative of post-orogenic landscape evolution.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 2011, vol. 36, n°. 9, p. 1254-1267, nombre de pages : 14, Références bibliographiques : 2 p.
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)