Why this matters
Craig Ogwr is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. The cliff is notable for its exposure of sedimentary rock layers that provide insight into ancient tropical sea conditions and may contain fossil remains of marine life from the Carboniferous period.
What is recorded here
Craig Ogwr is shown as a cliff on the public map of Bridgend. The saved point is the map point or the centre of its mapped shape.
The public map does not by itself grant access. Check current paths, opening conditions and ownership before entering.