| Lithological Description: |
| Unsorted clast-supported breccio-conglomerate, weakly cemented; clasts of igneous volcanic and Lower Palaeozoic lithologies. |
| Definition of Lower Boundary: |
| Unconformable on Coal Measures and older rocks. |
| Definition of Upper Boundary: |
| Unconformably overlain by Bridgnorth Sandstone Formation. |
| Thickness: |
| To 75m |
| Geographical Limits: |
| Malvern - Abberley Hills; equates with Clent Breccia of West Midlands. (Mitchell, and others, 1962). |
| Reference(s): |
| Mitchell, G H, Pocock, R W and Taylor, J H, 1962. Geology of the country around Droitwich, Abberley and Kidderminster. |
| Worssam, B C, Ellison, R A, and Moorlock, B S P. 1989. Geology of the country around Tewkesbury. Memoir of the British Geological Survey, Sheet 216 (England and Wales). |
| Groom, T T, 1902. The sequence of the Cambrian and associated beds of the Malvern Hills. Quarterly Journal of the Geological Society of London, Vol.58, p.59-135. |
| Phillips, J, 1848. The Malvern Hills compared with the Palaeozoic districts of Abberley, Woolhope, May Hill, Tortworth and Usk. Memoir of the Geological Survey of Great Britain, Vol.2, Part 1. |