The information on this page is a summary description.
The full formal description is available here: Pont de la Folle Formation
| Abbreviation | PFL |
| Parent unit | none |
| Child units | Fontaine Samart Member, Machenées Member, Hymiée Member |
| Lithological description | Coarse-grained bioclastic limestone massive to well-bedded, dolomitic in place, passing upwards to nodular shale rich in fossils. |
| Age | Early to middle Frasnian |
| Thickness | 90 m in the type area |
| Area of occurrence | North-western part of the DurbuyPhilippeville Anticlinorium, north-western limb of the Dinant Synlinorium. |
| Type locality | Eastern trench of the CharleroiCouvin road (N5E420), on both sides of the railway bridge south of Philippeville, but is largely overgrown nowadays. |
| Alternative names | Marbre Sainte-Anne (p.p.) |
| Authors | Mottequin, B., Denayer, J., Delcambre, B., Marion, J.-M. & Poty, E. |
| Date | 23/09/2025 |
| Cite as | Mottequin, B., Denayer, J., Delcambre, B., Marion, J.-M. & Poty, E., 2025. The Pont de la Folle Formation, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Pont-de-la-Folle-Formation |
| Additional information |
