Why this matters
Cùl na Bèinge is a sea cliff or coastal rock feature composed of metamorphic rocks, likely of Precambrian to early Paleozoic age. These rocks were formed through high-pressure and high-temperature deformation of older sedimentary or igneous rocks, typical of the Scottish Caledonides, and the feature is notable for its association with the ancient geological history of the region.
What is recorded here
Cùl na Bèinge 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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