Der kaltzeitliche Formenschatz im Cleurie-Tal (Südwestvogesen)

Gerd Wenzens
Mapping and profile analysis of glacial and fluvio-glacial forms and deposits in the Cleurie valley allow the following statements concerning this area's glacial history: On basis of criterions like state of conservation, intensity of weathering and incrustation, height and composition three different glacial periods can be distinguished.Because of the thickness of the Mosel- and Moselotte-glacier in the Remiremont/St. Arne basin a large diffluence during the Würm is improbable, it may at most have reached to...