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An Rubha Crìon

Headland
An Rubha Crìon
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What is recorded here

An Rubha Crìon is a headland composed primarily of basalt, formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. It is notable for its resistant columnar jointing and coastal erosion features, typical of the region’s volcanic landscape.

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Photo: Anne Burgess · CC BY-SA 2.0