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Rubha nan Trì Chlach

Headland

What is recorded here

Rubha nan Trì Chlach 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 nan Trì Chlach is a basaltic sea cliff or headland, likely formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. It is notable for its resistant basalt rock, which has withstood coastal erosion, and may represent part of a larger volcanic complex in the region.

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