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Rubha Dubh

Headland
Rubha Dubh
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What is recorded here

Rubha Dubh is shown as a headland on the public map of Argyll and Bute. The saved point is the map point or the centre of its mapped shape.
Rubha Dubh is a basaltic sea cliff or headland formed during the Paleogene period, approximately 60 to 55 million years ago, as a result of volcanic activity associated with the opening of the North Atlantic. It is notable for its resistant basalt rock, which has withstood coastal erosion, and may represent part of a larger igneous complex in the region.

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Photo: Peter Evans · CC BY-SA 2.0