Fig. 8From: Multiple Quaternary erosion and infill cycles in overdeepened basins of the northern Alpine forelandOutcrop at Herrenwies with cross-bedded fluvial gravels (LFA7.1, internal stratification indicated in b) interpreted as channel or scour-pool fills deposited in a glacial outwash plain. These gravels are correlated to Formation I. For location see Fig. 2a, label DBack to article page