Rubha Àird Druimnich

Rubha Àird Druimnich 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 Druimnich is a headland composed primarily of basaltic rock, formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. Its notable columnar jointing and coastal erosion features make it a distinctive and geologically significant coastal landform in the Scottish Highlands.