Why this matters
Aaron Crags is a sea cliff located in Cumberland, composed primarily of Carboniferous limestone, formed approximately 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
Aaron Crags 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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