Why this matters
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.
What is recorded here
Tripcock Ness is shown as a headland on the public map of Royal Borough of Greenwich. The saved point is the map point or the centre of its mapped shape.
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