Mots-clés
Accumulation fluviatile ; Datation ; Evolution de vallée ; Fluviatile ; Kraków ; Lit fluvial ; Méandre ; Paléovallée ; Plaine d'inondation ; Pologne ; Sédimentologie ; WisłaCracow ; Dating ; Floodplain ; Fluvial deposit ; Fluvial processes ; Meander ; Palaeovalley ; Poland ; River bed ; Sedimentology ; Valley floor evolution ; WisłaThe structure and age of the Drwień depression interrupting the Vistula flood-plain east of Cracow (South Poland)
Auteur :KALICKI, T.
Description :
Flat-floored depressions without traces of paleomeanders occur frequently on the Vistula flood plain within the Sandomierz Basin. One of this, the Drwień depression extends along the southern Vistula valley side between Cracow and Niepołomice. In the depression survived channel deposits laid down by the braided Vistula during the Late Glacial. In the western part the sandy-gravel deposits underlie a thin layer of peats in the eastern part the Younger Dryas and Preboreal channel deposits occur. Since the Preboreal the overbank deposits were sedimented. - (DG)
Type de document :
Article de périodique
Source :
Studia geomorphologica Carpatho-Balcanica, issn : 0081-6434, 1991, vol. 25-26, p. 89-113, Collation : Illustration, Références bibliographiques : 20 réf.
Date :
1991
Editeur :
Pays édition : Pologne, Warszawa, Państwowe Wydawnictwo Naukowe
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)