| Lithological Description: |
| Silicate-mudstone, grey, generally smooth to slightly silty, with sporadic beds of argillaceous limestone nodules. Over most of the outcrop (except the Cleveland Basin, where only the upper part is present) it comprises a tripartite succession: lower part (Peterborough Member) silicate-mudstone, mainly brownish-grey, fissile, organic-rich ("bituminous"), with subordinate beds of pale to medium grey, blocky mudstone; middle part (Stewartby Member) silicate-mudstone, mainly pale to medium grey, smooth to slightly silty, blocky, with subordinate beds of silty shell-debris-rich mudstone; upper part (Weymouth Member) mudstone, mainly pale grey, calcareous, smooth, blocky. For more detail see Peterborough, Stewartby and Weymouth members. |
| Definition of Lower Boundary: |
| Generally a fairly sharp but generally conformable junction with silicate-sandstone or sandy mudstone of the underlying Kellaways Formation or, in the Cleveland Basin, sandstone of the underlying Osgodby Formation, overlain by silicate-mudstone. In thicker, expanded successions (Wessex Basin) arbitary boundary drawn at the top of highest substantial silicate-sandstone or sandy mudstone above which the succession is predominantly silicate-mudstone. |
| Definition of Upper Boundary: |
| Upward transition from silicate-mudstone to silty mudstone of the overlying West Walton Formation (Oxford to Market Weighton) or sandy mudstones and calcareous sediments (Dorset to Oxford, and Yorkshire, north of Market Weighton) of the Corallian Group. In Market Weighton area, sharp disconformable contact with chalk (Chalk Group, Hunstanton Formation). In the Westbury to Longleat area, Wiltshire, sharp disconformable contact with sandy micaceous mudstone (Cretaceous, Gault Formation). |
| Thickness: |
| To 185m (perhaps in south Dorest); typically 50 to 70m over much of the East Midlands Shelf. |
| Geographical Limits: |
| Dorset coast (Weymouth area) to North Yorkshire coast. Extensive in onshore subcrop, though absent above the interior of the London Platform. |
| Reference(s): |
| Arkell, W J. 1933. The Jurassic System in Great Britain. [Oxford: Clarendon Press.] |
| Smith, W. 1817. Strata identified by organized fossils, Part 3. [London.] |
| Gallois, R W and Cox, B M. 1977. The stratigraphy of the Middle and Upper Oxfordian sediments of Fenland. Proceedings of the Geologists' Association, Vol.88, 207-228. |
| Phillips, W, 1818. A selection of facts from the best authorities, arranged so as to form an outline of the geology of England and Wales. (London: W Phillips). |
| Cox, B M, Hudson, J D and Martill, D M, 1992. Lithostratigraphic nomenclature of the Oxford Clay (Jurassic). Proceedings of the Geologists' Association, Vol.103, p.343-345. |
| Arkell, W J. 1947. The Geology of Oxford. [Oxford: Clarendon Press.] |
| Gaunt, G D, Fletcher, T P amd Wood, C J. 1992. Geology of the country around Kingston upon Hull and Brigg. Memoir of the British Geological Survey, sheets 80 and 89 (England and Wales). |