Mots-clés
Argile minéral ; Champs de pierres ; Cycle gel-dégel ; Déglaciation ; Erosion chimique ; Expérimentation ; Granulométrie ; Géomorphogenèse ; Modèle ; Météorisation ; Norvège ; Zone froideChemical erosion ; Clay mineral ; Cold area ; Deglaciation ; Experimentation ; Freeze-thaw cycle ; Geomorphogenesis ; Grain size distribution ; Model ; Norway ; WeatheringBlockfields, old or new? Evidence and implications from some plateaus in northern Norway
Auteur(s) et Affiliation(s)
REA, B.R.
Queen's University Belfast, School of Geosciences, Belfast BT7 1NN, Royaume-Uni
Description :
Evidence is presented from investigations on plateau-top blockfields in still-glaciated regions of north Norway. They are of considerable age and probably have been forming since pre-Pleistocene times. They are composite landforms produced by a combination of deep weathering under warmer conditions and sorting by frost heaving processes under periglacial conditions. Overall, the findings presented here allow a re-evaluation of the significance of blockfields and their formative conditions but also allude to the need to fully recognise pre-glacial conditions for glacier erosion.
Type de document :
Article de périodique
Source :
Geomorphology (Amsterdam), issn : 0169-555X, 1996, vol. 15, n°. 2, p. 109-121, Collation : Illustration, Références bibliographiques : 42 ref.
Date :
1996
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)