Bemerkungen über Stauch—„End"moränen

Eckhard Grimmel
Push ridges which occur in regions that were covered with continental ice sheets in former times may have different origins: They can be regarded as having originated not only by frontal push, but also by basal push of the expanding ice sheets. As long as there are no clear features, which allow to say whether a certain ridge is the result of frontal or basal push, such a ridge should indifferently be termed push ridge,...