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Published online by Cambridge University Press: 14 March 2018
Last Easter, when I was with Professor Hughes and his geological students at Torquay, I found some very perfectly preserved pseudomorphs of hæmatite after iron pyrites. They occur in the calcareous red shale in the most northerly part of Saltern Cove, Torquay, where the unconformity of the Trias and the Devonian is well shown.