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Càrn Tarmachain

Cliff

Why this matters

Càrn Tarmachain is a sea cliff composed primarily of Silurian greywacke, part of the Dalradian Supergroup, formed around 440–420 million years ago through sedimentation and subsequent metamorphism. It is notable for its exposure of ancient Scottish Highlands basement rocks, which provide insights into the region’s complex geological history.

What is recorded here

Càrn Tarmachain is shown as a cliff on the public map of Perth and Kinross. The saved point is the map point or the centre of its mapped shape.
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