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Exposure dating using cosmogenic 36 Cl demonstrates that the summit plateau of Scafell Pike (978m) in the SW Lake District escaped erosion by glacier ice during the last glacial maximum (LGM; c. 26–21kyr) and probably throughout the Devensian Glacial Stage (MIS 5d-2). Exposure ages obtained for ice-moulded bedrock on an adjacent col at 750–765m confirm over-riding and erosion of bedrock by...
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