The information on this page is a summary description.
The full formal description is available here: Waimes Member
| Abbreviation | WAI |
| Parent unit | Fooz Formation |
| Child units | |
| Lithological description | Kaolinitic coarse-grained sandstone with few micro-conglomeratic recurrences and siltstone intercalations |
| Age | Uppermost Pridoli |
| Thickness | 12 to 150 metres |
| Area of occurrence | Margins of the Stavelot and Condroz Inliers |
| Type locality | The Waimes quarry and nearby section along the former railway acts as a composite type section for the Waimes Member. |
| Alternative names | Arkose de Waismes (or de Weismes), Grès et arkoses de Gdoumont |
| Authors | Denayer, J. & Mottequin, B. |
| Date | 23/09/2025 |
| Cite as | Denayer, J. & Mottequin, B., 2025. The Waimes Member, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Waimes-Member |
| Additional information |
