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Rubha na h-Àirde

Headland

What is recorded here

Rubha na h-Àirde is shown as a headland on the public map of Highland. The saved point is the map point or the centre of its mapped shape.
Rubha na h-Àirde is a headland composed primarily of basalt, formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. It is notable for its dramatic coastal cliffs and potential links to the broader geological history of the Scottish Highlands.

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