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Ceann Sléibhe

Headland
Ceann Sléibhe
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What is recorded here

Ceann Sléibhe is a headland composed primarily of basalt, formed during the Paleogene period through volcanic activity associated with the opening of the North Atlantic. It is notable for its columnar jointing, a result of the rapid cooling of lava flows, and its role in the dramatic coastal landscape of southwest Ireland.

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Other information

Photo: Gerd Eichmann · CC BY-SA 4.0