The information on this page is a summary description.
The full formal description is available here: Claminforge Member
| Abbreviation | CLA |
| Parent unit | Rivière Formation |
| Child units | none |
| Lithological description | Fine-grained, fossiliferous and calcareous sandstone and calcareous shale with intercalations of reddish and greenish shale. |
| Age | Eifelian |
| Thickness | 39 m in the type area, rapidly decreasing eastwards. |
| Area of occurrence | Northern limb of the Dinant Synclinorium, fully developed west of the Samson River valley. |
| Type locality | Section along the disused railway south of Aisemont. |
| Alternative names | Macigno de Claminforge |
| Authors | Denayer, J., Coen-Aubert, M., Marion, J.-M. & Mottequin, B. |
| Date | 23/09/2025 |
| Cite as | Denayer, J., Coen-Aubert, M., Marion, J.-M. & Mottequin, B., 2025. The Claminforge Member, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Claminforge-Member |
| Additional information |
