The information on this page is a summary description.
The full formal description is available here: Lommel Member
| Abbreviation | StL |
| Parent unit | Sterksel Formation |
| Child units | |
| Lithological 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. |
| Age | Mostly post-Jaramillo Early Pleistocene. |
| Thickness | |
| Area of occurrence | Lower Meuse Valley. |
| Type locality | Sand quarry Houthalen. |
| 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 Lommel Member, 01/01/2001. National Commission for Stratigraphy Belgium. http://ncs.naturalsciences.be/lithostratigraphy/Lommel-Member |
