Fig. 10From: Distribution, geometry, age and origin of overdeepened valleys and basins in the Alps and their forelandCross-section through the “Wintermoorer Rinne” near Buxtehude, northern Germany, as an example of a tunnel valley formed during the Elster Glaciation at the southern margin of the Scandinavian Ice Sheet (modified after Kuster and Meyer 1979). The “Lauenburger Ton” unit is, at its type location, overlain by deposits of the Holsteinian (Meyer 1965)Back to article page