The information on this page is a summary description.
The full formal description is available here: Linchamps Conglomerate Bed
| Abbreviation | |
| Parent unit | Fépin Formation |
| Child units | |
| Lithological description | Poorly sorted conglomerate with dark quartzitic sandstone and quartz boulders and pebbles in an argillaceous sandstone matrix. |
| Age | Upper Pridoli to lowermost Lochkhovian |
| Thickness | 0 to 20 metres |
| Area of occurrence | Margins of the Caledonian inliers of Rocroi, Serpont and Givonne |
| Type locality | The Linchamps Conglomerate is defined in the disused quarry at Muno. |
| Alternative names | Poudingue de Fépin, Poundingue de Muno, Poudingue de Tournavaux |
| Authors | Denayer, J. & Mottequin, B. |
| Date | 23/09/2025 |
| Cite as | Denayer, J. & Mottequin, B., 2025. The Haybes Bed, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Linchamps-Conglomerate-Bed |
| Additional information |
