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High Pennard

Cliff
High Pennard
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What is recorded here

High Pennard is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. The cliff is notable for its exposure of fossil-rich rock layers, which provide evidence of ancient reef environments and contribute to the geological understanding of the South Wales coalfield region.

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Photo: Bill Boaden · CC BY-SA 2.0