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The crags of Raw Head in the Bickerton Hills are a geological Site of Special Scientific Interest. The sandstone was deposited in the Triassic era, 250 million years ago.
Credit: Vertigogen (16 November 2008)
The crags of Raw Head in the Bickerton Hills are a geological Site of Special Scientific Interest. The sandstone was deposited in the Triassic era, 250 million years ago.
Credit: Vertigogen (16 November 2008)