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Selley, R. C. (1965) The Torridonian Succession on the Islands of Fladday, Raasay, and Scalpay, Inverness-shire. Geological Magazine, 102 (5) 361-369 doi:10.1017/s0016756800053632

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Reference TypeJournal (article/letter/editorial)
TitleThe Torridonian Succession on the Islands of Fladday, Raasay, and Scalpay, Inverness-shire
JournalGeological Magazine
AuthorsSelley, R. C.Author
Year1965 (October)Volume102
Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800053632Search in ResearchGate
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Mindat Ref. ID249550Long-form Identifiermindat:1:5:249550:1
GUID0
Full ReferenceSelley, R. C. (1965) The Torridonian Succession on the Islands of Fladday, Raasay, and Scalpay, Inverness-shire. Geological Magazine, 102 (5) 361-369 doi:10.1017/s0016756800053632
Plain TextSelley, R. C. (1965) The Torridonian Succession on the Islands of Fladday, Raasay, and Scalpay, Inverness-shire. Geological Magazine, 102 (5) 361-369 doi:10.1017/s0016756800053632
In(1965, October) Geological Magazine Vol. 102 (5) Cambridge University Press (CUP)
Abstract/NotesAbstractThe succession of the Torridonian rocks seen on the islands of Fladday, Raasay, and Scalpay is described. Three lithological fades indicative of three distinct sedimentary environments are recognized. Breccias and grits, believed to be sub-aerial in their lower part, are overlain, or pass laterally into, grey shales and sandstones of lacustrine or shallow water marine origin. These are succeeded by red fluviatile sandstones and shales, which, except near the base, are coarse grained and pebbly throughout much of the succession. Three cases of lateral facies variation are described and their significance discussed with regard to the Torridonian succession elsewhere in the Inner Hebrides and on the mainland.


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