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littlemore+railway+cutting Latitude and Longitude:

51°43′16″N 1°14′02″W / 51.721°N 1.234°W / 51.721; -1.234
From Wikipedia, the free encyclopedia
Littlemore Railway Cutting
Site of Special Scientific Interest
LocationOxfordshire
Grid reference SP 530 027 [1]
InterestGeological
Area0.5 hectares (1.2 acres) [1]
Notification1986 [1]
Location map Magic Map

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]

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

  1. ^ a b c d "Designated Sites View: Littlemore Railway Cutting". Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
  2. ^ "Map of Littlemore Railway Cutting". Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
  3. ^ "Littlemore (Oxfordian)". Geological Conservation Review. Joint Nature Conservation Committee. Retrieved 26 February 2020.[ permanent dead link]
  4. ^ "Littlemore Railway Cutting citation" (PDF). Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
  5. ^ "Stanford Formation". British Geological Survey. Retrieved 6 April 2020.

51°43′16″N 1°14′02″W / 51.721°N 1.234°W / 51.721; -1.234


littlemore+railway+cutting Latitude and Longitude:

51°43′16″N 1°14′02″W / 51.721°N 1.234°W / 51.721; -1.234
From Wikipedia, the free encyclopedia
Littlemore Railway Cutting
Site of Special Scientific Interest
LocationOxfordshire
Grid reference SP 530 027 [1]
InterestGeological
Area0.5 hectares (1.2 acres) [1]
Notification1986 [1]
Location map Magic Map

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]

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

  1. ^ a b c d "Designated Sites View: Littlemore Railway Cutting". Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
  2. ^ "Map of Littlemore Railway Cutting". Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
  3. ^ "Littlemore (Oxfordian)". Geological Conservation Review. Joint Nature Conservation Committee. Retrieved 26 February 2020.[ permanent dead link]
  4. ^ "Littlemore Railway Cutting citation" (PDF). Sites of Special Scientific Interest. Natural England. Retrieved 6 April 2020.
  5. ^ "Stanford Formation". British Geological Survey. Retrieved 6 April 2020.

51°43′16″N 1°14′02″W / 51.721°N 1.234°W / 51.721; -1.234


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