Liège Formation

The information on this page is a summary description.
The full formal description is available here: Liège Formation

Abbreviation Lg
Parent unit Meuse Group
Child units
Lithological description Highest gravel reach, on or just incised in the Tertiary peneplain, weathered into red-yellow podzolic subtropical soils. It comprises the Trainée Mosane from Namur to Liège, consisting of well rounded quartz with silicified ooliths. The Meuse had still an important drainage area in the Paris Basin with a delta fan in the Lower Rhine embayment. The Formation represents the coarse proximal Meuse part of the West European “Kiezelooliet Group”.
Age Miocene to Middle Pliocene, no biostratigraphical elements
Thickness
Area of occurrence Lower Meuse Valley.
Type locality Bouge quarry, laying on marine Oligocene sands.
Alternative names
Authors Gullentops, F., Bogemans, F., De Moor, G., Paulissen, E. & Pissart, A.
Date 01/01/2001
Cite as Gullentops, F., Bogemans, F., De Moor, G., Paulissen, E. & Pissart, A., 2001. The Liège Formation, 01/01/2001. National Commission for Stratigraphy Belgium. http://ncs.naturalsciences.be/lithostratigraphy/Liege-Formation

Quaternary

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