The information on this page is a summary description.
The full formal description is available here: Heusy Member
| Abbreviation | HEU |
| Parent unit | Pepinster Formation |
| Child units | none |
| Lithological description | Arkosic and conglomeratic sandstone beds and conglomerate, usually pinkish with pink quartz pebble. |
| Age | Eifelian |
| Thickness | 24 m in the type area |
| Area of occurrence | Northern limb of the Dinant Synclinorium, east of the Hoyoux River valley, Vesdre area and Theux Window. |
| Type locality | The original stratotype along the E42 motorway is overgrown but a neostratotype is defined in the Gileppe River valley at Goé. |
| 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 Heusy Member, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Heusy-Member |
| Additional information |
