The information on this page is a summary description.
The full formal description is available here: Bois des Collets Member
| Abbreviation | BCO |
| Parent unit | Wépion Formation |
| Child units | |
| Lithological description | Very coarse-grained to conglomeratic sandstone beds separated by shale. |
| Age | Emsian |
| Thickness | 40 metres in the type locality |
| Area of occurrence | North and eastern margins of the Dinant Synclinorium, up to the Mormont Fault. |
| Type locality | Abandoned Bois des Collets quarry at Wépion in the Meuse River valley. |
| Alternative names | Poudingue du Bois des Collets |
| Authors | Denayer, J. & Mottequin, B. |
| Date | 23/09/2025 |
| Cite as | Denayer, J. & Mottequin, B., 2025. The Bois des Collets Member, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Bois-des-Collets-Member |
| Additional information |
