Why this matters
Robinson Crag is a sea cliff composed of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. It is notable for its exposure of sedimentary rock layers that provide insight into ancient tropical sea conditions in the region.
What is recorded here
Robinson Crag is shown as a cliff on the public map of Cumberland. The saved point is the map point or the centre of its mapped shape.
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