| Lithological Description: |
| Pale grey, quartz-cemented sandstones and interbedded conglomerates. Conglomerates contain mainly quartz pebbles, but also Malverns Complex and volcanic lithologies. |
| Definition of Lower Boundary: |
| Unconformable or in faulted contact with the Precambrian Malverns Complex. |
| Definition of Upper Boundary: |
| Conformable junction with Hollybush Sandstone. |
| Thickness: |
| Difficult to estimate, but possibly up to 60m (Worssam and others, 1989). |
| Geographical Limits: |
| Malvern Hills area, Hereford and Worcester. |
| Reference(s): |
| 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. |
| Stubblefield, C J, 1966. The Malvern Lower Cambrian strata. Nature, London, Vol.209, p.1121. |
| Groom, T T, 1899. The geological structure of the southern Malvern Hills and of the adjacent areas to the west. Quarterly Journal of the Geological Society of London, Vol.55, p.129-169. |