Sròn Ghlas

Headland

Why this matters

Sròn Ghlas is a headland composed primarily of basaltic rock, formed during the Paleogene period through volcanic activity associated with the opening of the North Atlantic. Its columnar jointing and coastal erosion features make it a notable example of igneous landforms along the Scottish coast.

What is recorded here

Sròn Ghlas 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.

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