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Dipton Crags

Cliff
Dipton Crags
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What is recorded here

Dipton Crags is a sea cliff composed primarily of Carboniferous sandstone, formed around 300 million years ago through sedimentary deposition in a shallow marine environment. The crags are notable for their exposure of resistant rock layers and their role in the coastal landscape of Northumberland, offering insights into the region's geological history.

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Photo: Clive Nicholson · CC BY-SA 2.0