What is recorded here

Graig-y-fuches-las is shown as a cliff on the public map of Conwy. The saved point is the map point or the centre of its mapped shape.

Graig-y-fuches-las is a sea cliff located in the area of Conwy, composed primarily of Silurian greywacke and slates, formed around 440–420 million years ago through sedimentation and subsequent tectonic compression. It is notable for its exposure of ancient volcanic and sedimentary rocks that are part of the Caledonide mountain-building event.

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