The end of the Beinn Eighe range at Ruadh-stac Mor. The Cambrian quartzites overlie the Torridonian - part of the spectacular large-scale geology visible in this area.
The end of the Beinn Eighe range at Ruadh-stac Mor. The Cambrian quartzites overlie the Torridonian - part of the spectacular large-scale geology visible in this area.