Fig. 7
From: Multiple Quaternary erosion and infill cycles in overdeepened basins of the northern Alpine foreland
Outcrops of fluvial or distal fluvioglacial gravels (LFA7.1). a Planar-bedded gravels along the north-eastern edge of the Strassberg Plateau (outcrop B in Fig. 2a) with strong surface cementation. b Weathered gravels at the Oberschwendli outcrop (outcrop C in Fig. 2a). c Broken clasts (example from Oberschwendli) can be found in both outcrops. Both outcrops are correlated to Formation C