Why this matters
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.
What is recorded here
Erne Craigs is shown as a cliff on the public map of Angus. The saved point is the map point or the centre of its mapped shape.
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