Rubha Àird Treisnis

Rubha Àird Treisnis 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 Àird Treisnis is a basaltic sea cliff or coastal rock feature, likely formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. It is notable as part of the rugged coastal landscape shaped by erosion and tectonic processes in the Scottish Highlands.