| Lithological Description: |
| Grey or pinkish grey quartzose sandstone. Quartzose conglomerate beds are common at the base of the formation, increasing in thickness and clast size towards the north. |
| Definition of Lower Boundary: |
| The basal conglomerate of the Trenchard Formation rests unconformably upon the quartzitic sandstone of the Cromhall Sandstone Formation. |
| Definition of Upper Boundary: |
| Taken at the base of the lowermost sandstone of "Pennant"- type (lithic arenite) of the Pennant Sandstone Formation, resting conformably above coarse-grained sandstone of the Trenchard Formation. This is a significant change to the Trotter (1942), who included all strata below the Coleford High Delf as part of his Trenchard Group. |
| Thickness: |
| Up to 120 m thick in the north of the Forest of Dean Coalfield. |
| Geographical Limits: |
| Restricted to the northern part of the Forest of Dean coalfield, approximately north of a line from Mailscott Wood, Coleford (SO 562 142) to Ruspidge, Cinderford (SO 649 119). |
| Reference(s): |
| Cleal, C and Thomas, B A. 1996. British Upper Carboniferous stratigraphy. Geological conservation review series No. 11. [London: Chapman and Hall]. |
| Waters, C N, Barclay, W J, Davies, J R and Waters, R A. In press. Stratigraphical framework for Carboniferous successions of Southern Great Britain (Onshore). British Geological Survey Research Report, RR/05/06. |
| Jones, P C. 1972. Quartzarenite and litharenite facies in the fluvial foreland deposits of the Trenchard Group (Westphalian), Forest of Dean, England. Sedimentary Geology, Vol. 8, 177-198. |
| Trotter, F M. 1942. Geology of the Forest of Dean Coalfield. Memoir of the British Geological Survey. |