3.1.4.2. Lommel Member - StL
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.