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. Rounded stones of non-alpine origin, found in the south of the early pleistocene Danube current in the eastern Iller-Lech-Platte (plateau) are assumed to be displaced last remnants of gravel deposits, accumulated by a pliocene Danube. They give first references to her current about 35 or 40 km more southern. The Dinkelscherbener Altwasserscheide (old watershed), till now regarded as a tertiary remnant, can be formed not earlier than in the pleistocene and probably must not be elongated beyond the Staufenberg to NNE.

Erste Hinweise auf eine pliozäne Donau in der östlichen Iller-Lech-Platte (Bayerisch Schwaben)