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Tripcock Ness

Headland
Tripcock Ness
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What is recorded here

Tripcock Ness is a headland composed primarily of London Clay, a marine sedimentary rock formed during the Eocene epoch, around 56 to 34 million years ago. The feature is notable for its coastal exposure of this geological formation, which provides insight into the region's ancient marine environment.

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Photo: Marathon · CC BY-SA 2.0