The information on this page is a summary description.
The full formal description is available here: Zutendaal Formation
| Abbreviation | Zd |
| Parent unit | Meuse Group |
| Child units | |
| Lithological 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. |
| Age | Basal Middle Pleistocene, “Cromerian”, probably Glacial B. |
| Thickness | |
| Area of occurrence | Lower Meuse Valley. |
| Type locality | As quarry. |
| 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 Zutendaal Formation, 01/01/2001. National Commission for Stratigraphy Belgium. http://ncs.naturalsciences.be/lithostratigraphy/Zutendaal-Formation |
