Chantry Mill is a 8.7-hectare (21-acre) geological Site of Special Scientific Interest in Storrington in West Sussex.[1][2] It is a Geological Conservation Review site.[3]

This site provides the best exposure of the junction between the Gault and Folkestone Beds of the Wealden Group, dating to around 140 million years ago in the Early Cretaceous.[4]

A public footpath runs along the south-western edge of the site.

References

  1. ^ a b c d "Designated Sites View: Chantry Mill". Sites of Special Scientific Interest. Natural England. Retrieved 19 April 2019.
  2. ^ "Map of Chantry Mill". Sites of Special Scientific Interest. Natural England. Retrieved 19 April 2019.
  3. ^ "Chantry Mill (Aptian-Albian)". Geological Conservation Review. Joint Nature Conservation Committee. Retrieved 6 April 2019.
  4. ^ "Chantry Mill citation" (PDF). Sites of Special Scientific Interest. Natural England. Retrieved 19 April 2019.

50°54′47″N 0°26′42″W / 50.913°N 0.445°W / 50.913; -0.445

Allikas: https://en.wikipedia.org/wiki/Chantry_Mill
No tags for this post.