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Brady's Crag

Named rock
Brady's Crag
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What is recorded here

Brady's Crag is a coastal rock feature in Northumberland, composed of basalt and formed during the Palaeogene period, around 60 to 55 million years ago, as a result of volcanic activity associated with the North Atlantic Igneous Province. It is notable for its resistant basaltic structure, which has withstood coastal erosion, and may represent part of a larger volcanic complex in the region.

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Photo: Karl and Ali · CC BY-SA 2.0