2.8. Mol Formation - Ml
Authors: De Meuter & Laga (1976), after Mourlon (1896).
Description: white pure, coarse and medium fine sand, sometimes lignitic and with some lenses of a micaceous clay; in the type region, lower part very slightly glauconiferous.
Stratotype: sandpits for the exploitation of glass sands.
Area: whole northeastern part of the Campine.
Thickness: 20 m in the Mol area, but up to 70 m and more east of the faults.
Age: late Pliocene.