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Corran a' Chinn Uachdaraich

Headland
Corran a' Chinn Uachdaraich
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What is recorded here

Corran a' Chinn Uachdaraich is a basaltic sea cliff formed during the Paleogene period, approximately 60 to 55 million years ago, as a result of volcanic activity associated with the opening of the North Atlantic. It is notable for its columnar jointing, a characteristic feature of rapidly cooled lava flows, and its contribution to the dramatic coastal landscape of the Scottish Highlands.

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Photo: John Allan · CC BY-SA 2.0