Traces d'activité périglaciaire dans les Vosges moyennes

Auteurs :
VAN VLIET-LANOE, B.
FLAGEOLLET, J. C.

Description :
In the middle region of the French Vosges, a compact formation is commonly observed preferentially on south facing slopes. It is a till, usually called the crassin which frequently shows a well developed platy structure. From the Authors'observations the structure, and in part the compaction, result from the growth of segregated ice lenses. It was formed probably under a melting ice sheet or in a periglacial environment.


Type de document :
Article de périodique

Source :
Biuletyn peryglacjalny Lodz, 1981, vol. 28, p. 209-219, Références bibliographiques : 12réf.

Date :
1981