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Published online by Cambridge University Press: 01 May 2009
In his posthumous paper on the geology of the Island of Raasay H. B. Woodward (1) remarks: “On the fore-shore south of Oskaig Point, the modern beach is cemented into a conglomerate.” The unique mineralogical composition of this conglomerate, which has been collected in the course of a study of the Tertiary igneous rocks of Raasay and neighbouring islands, warrants the following note.