3.1.5. Zutendaal Formation - Zd
Authors: Gullentops & Paulissen, herein.
Description: Sediments from the Meuse when diverted to the northwest, depositing large fans covering the Kempen Plateau. Coarse aggrading gravel, considered fluvio-glacial with ice-rafted blocks, heavily weathered into reddish brown As Soil.
Stratotype: As quarry.
Area: Lower Meuse Valley.
Age: Basal Middle Pleistocene, "Cromerian", probably Glacial B.