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Subsiding cliff, Park Head

Cliff or headland
Subsiding cliff, Park Head
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What is recorded here

A named place photographed at this map point in Cornwall.
Subsiding cliff at Park Head in Cornwall consists of Devonian slate, formed around 380 million years ago through the compaction of marine sediments. The cliff is notable for its ongoing erosion and subsidence, revealing layered rock formations and contributing to the dynamic coastal landscape of the region.

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Photo: David Hawgood · CC BY-SA 2.0