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(Article of periodic en Français - 1981)

Document title

Traces d'activité périglaciaire dans les Vosges moyennes

Authors(s) and Affiliation(s)

VAN VLIET-LANOE B. ; FLAGEOLLET J. C. ;

Abstract

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.

Source

Article of periodic

published at : Biuletyn peryglacjalny Lodz

Editor :

Millesime : 1981, vol. 28 [pp. 209-219]

Bibliographic references : 12réf.

Language

Français

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