Zum Problem der saaleeiszeitlichen Terrassenbildungen im Unterlauf der Werre

J. H. Henke
The classification of the fluviatile deposits of the river Werre showing its problematic character in the literature on the subject, caused the author to study the terraces of the lower course of the Werre near Gohfeld and Bad Oeynhausen. The stratigraphy of the layers and the roundings of quartz grains were taken into special consideration. By way of example the terraces near the station of Gohfeld are closely described and examined according to climatic changes...