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Rubha na Sgàth Mòire

Headland

What is recorded here

Rubha na Sgàth Mòire is a basaltic sea cliff or coastal rock feature, likely formed during the Paleogene period (approximately 60–55 million years ago) as part of the North Atlantic Igneous Province. It is notable for its association with the broader volcanic activity that shaped much of the Scottish Highlands' coastline.

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