Rubha Dubh-Àird

Rubha Dubh-Àird 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 Dubh-Àird 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 for its potential association with the geological formations of the Scottish Highlands, which include extensive basalt flows and columnar jointing from ancient lava eruptions.