Mots-clés
Connecticut ; Estuaire ; Etats-Unis ; Holocène ; Niveau marin ; Paléogéographie ; Plaine d'inondation ; Quaternaire ; Stratigraphie ; Transport sédimentaireConnecticut ; Estuary ; Floodplain ; Holocene ; Palaeogeography ; Quaternary ; Sea level ; Sediment transport ; Stratigraphy ; United StatesResponse of the Connecticut River estuary to late Holocene sea level rise
Special issue : Geomorphic systems
Auteurs :PATTON, P. C.
HORNE, G. S.
PHILLIPS, J. D.
RENWICK, W. H.
Description :
The purpose of this paper is to describe the late Holocene development of the Connecticut River. This analysis is based on studies of water circulation and sediment transport in the modern estuary and the Holocene stratigraphy preserved below sea level. The goal of the study is to construct a model of the past estuarine landscape, and from this model to evaluate the degree to which an earlier inherited morphology controls the functioning of the modern estuary and its future evolution.
Type de document :
Congrès
Source :
Proceedings of the 23rd Binghamton Symposium in geomorphology, Inconnu, 1992-09-25/1992-09-27, Geomorphology (Amsterdam), issn : 0169-555X, 1992, vol. 5, n°. 3-5, p. 391-417, Collation : Illustration, Références bibliographiques : 52 réf.
Date :
1992
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)