Zur Gliederung, Bildung und Altersstellung des Kalksteinschutts am Trauf der westlichen Schwäbischen Alb

Dieter Weippert
The steep slope to the NW of the Schwäbische Alb, the Albtrauf, is covered with thick layers consisting of limestone pebbles and cobbles. Because of the difference in grain size and in the percentage of loam, sand and silt mixed in, we can distinguish several different types of rubble: the pieces of the mountain screes, the „coarse rubble" an the „fine rubble". The „coarse rubble" and the „fine rubble" came into being during the Würm-glaciation....