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Rubha h-Uamha-saile

Headland
Rubha h-Uamha-saile
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What is recorded here

Rubha h-Uamha-saile is a headland composed primarily of Devonian sandstone, formed around 400 million years ago through sedimentary deposition in a shallow marine environment. It is notable for its resistant rock formations that have withstood coastal erosion, contributing to the rugged topography of the Argyll and Bute coastline.

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Photo: Andrew Spenceley · CC BY-SA 2.0