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Cúinne an Mhionnáin

Headland
Cúinne an Mhionnáin
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What is recorded here

Cúinne an Mhionnáin 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 for its coastal exposure that highlights the region's volcanic geological history.

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