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Published online by Cambridge University Press: 01 May 2009
Having formed one of a party of sixteen, who have lately further explored the recently discovered caverns at Stainton, notices of which have appeared in the Times and other journals, I wish to furnish a few details of the exploration, which may possibly prove interesting. The caverns are in the Carboniferous Limestone formation, and situated at a point one mile and a quarter south-east of the Dalton station of the Furness Railway, Lancashire.