Creag a' Chapaill

Creag a' Chapaill is shown as a cliff on the public map of Highland. The saved point is the map point or the centre of its mapped shape.

Creag a' Chapaill is a sea cliff located in the Highland region of Scotland, composed primarily of basaltic rock formed during the Paleogene period, around 60 to 55 million years ago. It is notable as part of the broader geological formation associated with the North Atlantic Igneous Province, resulting from ancient volcanic activity linked to the opening of the North Atlantic Ocean.