Mots-clés
Action anthropique ; Aménagement hydraulique ; Chenal anastomosé ; Cours d'eau ; Datation C 14 ; Dynamique fluviale ; GPR ; Géométrie hydraulique ; Géophysique ; Holocène ; Méandre ; Obra ; Paléogéographie ; Paléogéomorphologie ; Pologne ; Pologne de l'Ouest ; Proglaciaire ; TélédétectionBraided channel ; C 14 dating ; Channel geometry ; Fluvial dynamics ; Geophysics ; Ground penetrating radar ; Holocene ; Human impact ; Hydraulic works ; Meander ; Palaeogeography ; Palaeogeomorphology ; Poland ; Proglacial features ; Remote sensing ; Stream ; Western polandAcción antrópica ; Aprovechamiento hidráulico ; Canal anastomosado ; Corriente de agua ; Datación Carbono 14 ; Dinámica fluvial ; Geofísica ; Geometria hidráulica ; Holoceno ; Meandro ; Paleogeografía ; Paleogeomorfología ; Polonia ; Proglaciar ; TeledetecciónReconstructing of anastomosing river
Auteur(s) et Affiliation(s)
SŁOWIK, M.
Dept. of Geographic and Geologic Sciences, Adam Mickiewicz Univ., Poznán, Pologne
Description :
Intensive hydro technical works were conducted in the middle course of the Obra River (Poland) at the beginning of the nineteenth century. The natural river course (functioning before the major construction works) was transformed into 3 artificial canals. Ground-penetrating radar investigations, ground-truthed with coring and remote sensing surveys, were conducted to reconstruct the course taken by the river prior to the hydro technical works. This work demonstrated that the Obra formerly had an anastomosing planform. Radiocarbon dating indicated that the earliest of the retraced channels were active before 9000 BP. The retraced river system was formed in a proglacial stream valley perpendicularly cut by remains of subglacial tunnels, now partly filled with lakes. The planform consisted of one or two major channels and a number of secondary channels formed by avulsions. During the last 2000 years, some of the avulsions may have been caused by anthropogenic interventions. Valley sections with meandering anabranches, anastomosing patterns with traces of a lateral migration and traces of a transition from meandering to anastomosing planform were distinguished.
Type de document :
Article de périodique
Source :
Geografiska annaler. Series A. Physical geography, issn : 0435-3676, 2014, vol. 96, n°. 2, p. 195-216, nombre de pages : 22, Références bibliographiques : 64 ref.
Date :
2014
Editeur :
Pays édition : Suede, Stockholm, Svenska sällskapet för antropologi och geografi
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)