Abtragungs- und Bodenbildungsphasen im Rißlöß

Erhard Bibus
In the following article an attempt is made to establish a stratigraphie division of the Riss-loess, which is situated between the first and second fossil "Parabraunerde" (leached brown soil). The Riss-loess can be stratified by poorly developed soils, and by intercalated erosional phases. During the younger Riss strong sedimentation of loess prevailed. At the same time, at least six cold and more humid phases led to the formation of a corresponding number of poorly developed...