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Erne Craigs

Cliff
Erne Craigs
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What is recorded here

Erne Craigs is a sea cliff composed primarily of Devonian sandstone, formed around 400 to 360 million years ago through sedimentary deposition in a shallow marine environment. The site is notable for its well-exposed stratigraphy, which provides insights into the geological history of the Scottish mainland's coastal regions.

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Photo: Scott Cormie · CC BY-SA 2.0