Das Schlernstadium und der Klimaablauf der Späteiszeit im nördlichen Alpenraum

Carl Rathjens
With the arguments of many own observations and of the most important literature the attempt is made to give a picture of the evolution of climate of the Late Glacial time in the northern Alps, considering especially the geomorphological phenomena. According to that the violent return of coldness in the Younger Dryas period of Central Europe is represented by the Schiern moraines of the Alps, to which the position of a real substage with glaciers...