What is recorded here

Dove Crag is shown as a cliff on the public map of Northumberland. The saved point is the map point or the centre of its mapped shape.

Dove Crag is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. It is notable for its exposure of fossil-rich rock layers, which provide insights into ancient marine environments and contribute to the geological significance of Northumberland’s coastal landscape.

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