The information on this page is a summary description.
The full formal description is available here: Névremont Formation
| Abbreviation | NEV |
| Parent unit | none |
| Child units | none |
| Lithological description | Various well-bedded limestone with shaly intercalation, notably near the base, rather fossiliferous, dolomitic in the upper part. |
| Age | Givetian |
| Thickness | 71 m in the type area, rapidly decreasing eastwards. |
| Area of occurrence | Northern limb of the Dinant Synclinorium, from the Eau dHeure River valley to the Ourthe River valley, Haine-Sambre-Meuse overturned thrusted sheets between the Mons area to the Samson River valley, and Vesdre area. |
| Type locality | Section along the disused railway south of Aisemont. |
| Alternative names | none |
| 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 Névremont Formation, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Nevremont-Formation |
| Additional information |
