Abstract
Researches carried out on the main glacier of the ovrefjell massif, candes Mountains, orway (62° ; 9° ) point to recent periglacial features which are presently directly developed on the ice. This original location raises the problem of their morphodynamic significance and a hypothesis of ephemeral periglacial activity in a paraglacial context is proposed here.
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Riwan Kerguillec
Riwan Kerguillec, Institut de Géographie et d'Aménagement Régional de l'Université de Nantes, Campus du Tertre, BP 81227, 44-312 Nantes cedex 3, France.
E‐mail: [email protected]