| Lithological Description: |
| White to pale brown, typically well-sorted medium- to coarse-grained, moderately to highly shell-detrital ooidal grainstone, locally fine- to very coarse-grained; medium to thickly well-bedded and cross-bedded, with thin shell-detrital marl seams and locally calcareous sandstone beds. |
| Definition of Lower Boundary: |
| Top of highest significant mudstone in Fuller's Earth Formation or Sharp's Hill Formation, or passage from finer grained limestone of the Eyford Member, where present. |
| Definition of Upper Boundary: |
| Passage upwards into fine-grained ooidal limestone and marls of Hampen Formation or mudstone, siltstone and limestone of the Rutland Formation. |
| Thickness: |
| 0-11m, locally possibly up to 15m, type area 6 to 8m |
| Geographical Limits: |
| Stroud, Gloucestershire (where passes westwards near Stroud into finer grained limestones of Througham Member (Fuller's Earth Formation) and succeeding Hampen Formation; Sumbler, M G, Barron, A J M and Morigi, A N, 2000. To Brackley, Northants (where passes northeast into Wellingborough Member (formerly Upper Estuarine Limestone) of the Rutland Formation (Horton et al, 1987)). |
| Reference(s): |
| Sumbler, M G, Barron, A J M and Morigi, A N, 2000. Geology of the Cirencester district. Memoir of the British Geological Survey, Sheet 235 (England and Wales). |
| Barron, A J M, 1998. Geology of the Hawling area: 1:10 000 Sheet SP02SE. British Geological Survey Technical Report WA/98/26. |
| Sumbler, M G, 1995. Geological notes and local details for 1:10 000 Sheet SP11NW (Farmington). British Geological Survey Technical Report WA/95/3. |
| Sumbler, M G and Williamson, I T. 1998. Lee's Quarry Taynton: a type locality for the Taynton Limestone Formation (Middle Jurassic, Great Oolite Group). Proceedings of the Cotteswold Naturalists' Field Club, Vol. 41 (2), p. 222 - 229. |