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.[1][2] It is a Geological Conservation Review site.[3]
| Site of Special Scientific Interest | |
.jpg) | |
| Location | Oxfordshire |
|---|---|
| Grid reference | SP 530 027[1] |
| Interest | Geological |
| Area | 0.5 hectares (1.2 acres)[1] |
| Notification | 1986[1] |
| Location map | Magic Map |
The cutting exposes limestone and clay laid down in mid-Oxfordian stage of the Late Jurassic, around 160 million years ago. The deposit is part of the Stanford Formation, and the clay appears to have been deposited in a channel between coral reefs which then covered the Oxford area.[4][5]
References
edit- ^ a b c d "Designated Sites View: Littlemore Railway Cutting". Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
- ^ "Map of Littlemore Railway Cutting". Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
- ^ "Littlemore (Oxfordian)". Geological Conservation Review. Joint Nature Conservation Committee. Retrieved 26 February 2020.[permanent dead link]
- ^ "Littlemore Railway Cutting citation" (PDF). Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
- ^ "Stanford Formation". British Geological Survey. Retrieved 6 April 2020.