What is recorded here

Clogwyn y Barcut is shown as a cliff on the public map of Gwynedd. The saved point is the map point or the centre of its mapped shape.

Clogwyn y Barcut is a sea cliff composed primarily of Silurian greywacke and mudstone, formed around 440–420 million years ago through sedimentation and subsequent tectonic uplift. It is notable for its exposure of ancient marine sediments and its location within the scenic and geologically significant coastline of Gwynedd.

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