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Author: Gullentops, herein.

Description: Attracted by the antithetic down warping along the Rauw Fault, Rhine sands were deposited in a deep southern bend and cover the western part of the Kempen. Different mineralogy probably due to superficial weathering.

Stratotype: Sand quarry Houthalen.

Area: Lower Meuse Valley.

Age: Mostly post-Jaramillo Early Pleistocene.