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Àird Tharsgabhaig

Headland

Why this matters

Àird Tharsgabhaig is a coastal headland composed primarily of basaltic rock, formed during the Palaeogene period through volcanic activity associated with the North Atlantic Igneous Province. The feature is notable for its dramatic sea cliffs and its location within a region shaped by ancient lava flows and subsequent coastal erosion.

What is recorded here

Àird Tharsgabhaig 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.
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