Mots-clés
Dune ; Déglaciation ; Eolien ; Fluvioglaciaire ; Géomorphogenèse ; Norvège ; Sandur ; SédimentologieAeolian features ; Deglaciation ; Dune ; Fluvioglacial features ; Geomorphogenesis ; Norway ; Sandur ; SedimentologyDeglaciación ; Duna ; Eólico ; Fluvioglaciar ; Geomorfogénesis ; Sandur ; SedimentologíaThe eolian landforms and sediment in the valley of River Jømna, east of Elverum, south-east Norway
Auteur(s) et Affiliation(s)
KLEMSDAL, T.
Dep. of Geosciences, Univ., Oslo, Norvege
Description :
Eolian landforms as sandy dunes and dune heaps were mapped by the author in 1979-1980 in a zone where vegetation had been destroyed by a forest fire on 30 June 1976, in an area to the east of Elverum, south-east Norway. The mapped eolian landforms are discussed together with information from 40 samples of the eolian sediment. Winds, mostly from the north and north-west, were responsible for the development of these eolian landforms, utilizing the fluvioglacial sediments accumulated as a sandur during the retreat of the inland ice approximately 10,000 years ago. The winds were active during a short period of time, only a century or so before the area became vegetated.
Type de document :
Article de périodique
Source :
Norsk geografisk tidsskrift, issn : 0029-1951, 2010, vol. 64, n°. 2, p. 94-104, nombre de pages : 11, Références bibliographiques : 19 ref.
Date :
2010
Editeur :
Pays édition : Norvege, Oslo, Norske geografiske selskab ; Universitetsforlaget
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)