A | B | C | D | E | F | G | H | CH | I | J | K | L | M | N | O | P | Q | R | S | T | U | V | W | X | Y | Z | 0 | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9
Site of Special Scientific Interest | |
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Location | Oxfordshire |
---|---|
Grid reference | SU 326 941[1] |
Interest | Geological |
Area | 2.6 hectares (6.4 acres)[1] |
Notification | 1986[1] |
Location map | Magic Map |
Shellingford Crossroads Quarry is a 2.6-hectare (6.4-acre) geological Site of Special Scientific Interest west of Stanford in the Vale in Oxfordshire.[1][2] It is a Geological Conservation Review site.[3]
This site exposes rocks of the Corallian Group, dating to the Oxfordian stage of the Late Jurassic, around 160 million years ago. It has many fossils of corals and reef-dwelling bivalves, and it is also important as it provides an example of the complexity of Oxfordian stratigraphy.[4]
References
- ^ a b c d "Designated Sites View: Shellingford Crossroads Quarry". Sites of Special Scientific Interest. Natural England. Retrieved 8 April 2020.
- ^ "Map of Shellingford Crossroads Quarry". Sites of Special Scientific Interest. Natural England. Retrieved 8 April 2020.
- ^ "Shellingford Crossroads (Oxfordian)". Geological Conservation Review. Joint Nature Conservation Committee. Retrieved 26 February 2020.[permanent dead link]
- ^ "Shellingford Crossroads Quarry citation" (PDF). Sites of Special Scientific Interest. Natural England. Retrieved 8 April 2020.
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