Why this matters
Craigie Doubs is a sea cliff composed primarily of Silurian greywacke, formed around 430 million years ago through sedimentation and subsequent lithification in a deep marine environment. The cliff is notable for its resistant rock type, which has withstood coastal erosion to form a prominent and enduring coastal feature.
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Craigie Doubs 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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