Ketton Quarries is a 115.6-hectare (286-acre) biological and geological Site of Special Scientific Interest east of Ketton in Rutland. It is a Geological Conservation Review site, and an area of 27.5 hectares is managed by the Leicestershire and Rutland Wildlife Trust.
The White Limestone Formation is a Bathonian geologic formation in the United Kingdom, dating to the Middle Jurassic, 168.3 to 166.1 million years ago. Fossil sauropod tracks have been reported from the formation. It is the lateral equivalent of the Blisworth Limestone. It predominantly consists of grey-yellow limestone, typically wackestone and packstone with subordinate ooidal grainstone. The Woodeaton Quarry locality has yielded microvertebrates.
Hornsleasow Quarry is a 3.5-hectare (8.6-acre) geological Site of Special Scientific Interest in Gloucestershire, notified in 1974. The site is listed in the 'Cotswold District' Local Plan 2001-2011 as a Regionally Important Geological Site (RIGS).
The Rutland Formation is a geologic formation in England. It preserves fossils dating back to the late Bajocian to Bathonian stages in the Jurassic period, about 169 million years ago. It is the lateral equivalent of the Sharp's Hill Formation and the Fuller's Earth Formation. The "Rutland Dinosaur" specimen of Cetiosaurus is known from the formation.
Roade Cutting is a 15.2-hectare (38-acre) geological Site of Special Scientific Interest along the West Coast Main Line north from Roade in Northamptonshire. It is a Geological Conservation Review site.
Blisworth Rectory Farm Quarry is a 1.0-hectare (2.5-acre) geological Site of Special Scientific Interest west of Blisworth in Northamptonshire. It is a Geological Conservation Review site.
Finedon Top Lodge Quarry, also known as Finedon Gullet is a 0.9-hectare (2.2-acre) geological Site of Special Scientific Interest east of Wellingborough in Northamptonshire. It is a Geological Conservation Review site revealing a sequence of middle Jurassic limestones, sandstones and ironstones, and is the type section for a sequence of sedimentary rocks known as the 'Wellingborough Member'. It was created by quarrying for the underlying ironstone for use at Wellingborough and Corby Steelworks; the ore was transported by the 1,000 mm gauge Wellingborough Tramway.
Cranford St John SSSI is a 2.8-hectare (6.9-acre) geological Site of Special Scientific Interest in Cranford St John, east of Kettering in Northamptonshire. It is a Geological Conservation Review site.
Shipton-on-Cherwell and Whitehill Farm Quarries is a 30-hectare (74-acre) geological Site of Special Scientific Interest north of Kidlington in Oxfordshire. It is a Geological Conservation Review site.
Dry Sandford Pit is a 4.2-hectare (10-acre) biological and geological Site of Special Scientific Interest north-west of Abingdon-on-Thames in Oxfordshire. It is a Geological Conservation Review site and it is managed as a nature reserve by the Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust.
Hook Norton Cutting and Banks is a 6.7-hectare (17-acre) biological and geological Site of Special Scientific Interest south of Hook Norton in Oxfordshire. The site is in three areas, two of which are managed as a nature reserve called Hook Norton Cutting by Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust. and are designated a Geological Conservation Review site.
Kirtlington Quarry is a 3.1-hectare (7.7-acre) geological Site of Special Scientific Interest west of Kirtlington in Oxfordshire. It is a Geological Conservation Review site, and it is part of the 7.4-hectare (18-acre) Kirtlington Quarry Local Nature Reserve.
Rock Edge is a 1.7-hectare (4.2-acre) geological Site of Special Scientific Interest in Oxford in Oxfordshire. It is a Geological Conservation Review site and a Local Nature Reserve
Ardley Cutting and Quarry is a 40.1-hectare (99-acre) biological and geological Site of Special Scientific Interest north-west of Bicester in Oxfordshire. It is a Geological Conservation Review site and an area of 11 hectares is managed by the Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust as Ardley Wood Quarry. The site contains a Scheduled Monument, Ardley Wood moated ringwork, a Norman defended enclosure.
Horsehay Quarries is a 8.4-hectare (21-acre) geological Site of Special Scientific Interest west of Bicester in Oxfordshire. It is a Geological Conservation Review site.
Littlemore Railway Cutting is a 0.5-hectare (1.2-acre) geological Site of Special Scientific Interest on the southern outskirts of Oxford in Oxfordshire. It is a Geological Conservation Review site.
Lyehill Quarry is a 2.8-hectare (6.9-acre) geological Site of Special Scientific Interest east of Oxford in Oxfordshire. It is a Geological Conservation Review site.
Sharp's Hill Quarry is a 2.4-hectare (5.9-acre) geological Site of Special Scientific Interest west of Banbury in Oxfordshire. It is a Geological Conservation Review site.
Kermackodon is an extinct genus of allotherian mammal, known from the Middle Jurassic of England. It combines features of multituberculates with those of euharamyidans. The remains of type species, K. multicuspis were collected from Kirtlington Quarry in Oxford, England, by a team lead from UCL led by Professor Kenneth Kermack after whom the taxon is named, from sediments of the Forest Marble Formation, dating to the Bathonian stage of the Middle Jurassic. The genus and species were named by Percy M. Butler and Jerry Hooker in 2005. The remains comprise a left upper molar (M2), a lower last premolar, initially considered a left but later considered more likely to be right (p4), and an incomplete non-last upper premolar. A second species, K. oxfordensis, from Kirtlington and also sediments of the White Limestone Formation at Woodeaton Quarry was assigned to the genus in 2022, originally placed in the separate genus Eleutherodon. A 2020 study considered it to be more closely related to mutlituberculates than to euharamiyidans, while the 2022 study considered it to be a member of Euharamiyida.
