What is recorded here

The Dip is shown as a cliff on the public map of Pembrokeshire. The saved point is the map point or the centre of its mapped shape.

The Dip is a sea cliff composed primarily of Carboniferous limestone, formed around 340–325 million years ago through the accumulation of marine sediments. It is notable for its exposure of sedimentary rock layers that provide insights into ancient tropical marine environments.

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