Rubha na h-Àirde Glaise

Rubha na h-Àirde Glaise 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 Glaise is a headland composed primarily of basaltic rock, formed during the Palaeogene period (approximately 60–55 million years ago) as part of the North Atlantic volcanic province. The feature is notable for its association with the geological activity linked to the opening of the North Atlantic Ocean and the formation of the Scottish Highlands’ volcanic and intrusive complexes.