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Rubha na Feundain

Headland
Rubha na Feundain
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What is recorded here

Rubha na Feundain is a headland composed primarily of Devonian-aged sandstone, formed through sedimentary processes around 400 million years ago. It is notable for its resistant rock formations that have withstood coastal erosion, contributing to the dramatic sea cliffs characteristic of the Argyll and Bute coastline.

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Photo: Andy Waddington · CC BY-SA 2.0