Mots-clés
Cône de déjection ; Datation C 14 ; Friuli-Venezia Giulia ; Holocène ; Italie ; Modèle ; Paléogéographie ; Quaternaire ; Structure sédimentaire ; Sédiment lacustre ; ValléeAlluvial cone ; C 14 dating ; Friuli-Venezia Giulia ; Holocene ; Italy ; Lacustrine sediment ; Model ; Palaeogeography ; Quaternary ; Sedimentary structure ; ValleyThe Holocene evolution of a stretch of an Eastern Italian Alpine valley
Auteurs :FRIZ, C.
VILLI, V.
TURRINI, M.C.
Description :
The morphological evolution of a stretch of an alpine valley located in the Eastern Italian Alps is described. This has been conditioned by a great alluvial fan that was formed as a consequence of interconnected events, deriving from large rockfalls which occured in the late glacial period at the head of the Missiaga-Bordina valley, on the left side of the Agordo basin. The aggradation of the alluvial fan blocked the Cordevole valley south of the Agordo basin and produced a lake that is documented by lacustrine sediments. After, an erosional phase began. A series of illustrations depicts the sequence of the fan's development.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 1995, vol. 20, n°. 8, p. 747-757, Collation : Illustration, Références bibliographiques : 22 ref.
Date :
1995
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)