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Falcon Clints

Cliff
Falcon Clints
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What is recorded here

Falcon Clints is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. The feature is notable for its well-exposed clint and gully structures, which result from differential erosion and provide insight into the region's geological history.

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Other information

Photo: Mick Garratt · CC BY-SA 2.0