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Smith, Bernard (1924) On the West Cumberland Brockram and its Associated Rocks. Geological Magazine, 61 (7) 289-308 doi:10.1017/s0016756800086441

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Reference TypeJournal (article/letter/editorial)
TitleOn the West Cumberland Brockram and its Associated Rocks
JournalGeological Magazine
AuthorsSmith, BernardAuthor
Year1924 (July)Volume61
Issue7
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800086441
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Mindat Ref. ID280675Long-form Identifiermindat:1:5:280675:8
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Full ReferenceSmith, Bernard (1924) On the West Cumberland Brockram and its Associated Rocks. Geological Magazine, 61 (7) 289-308 doi:10.1017/s0016756800086441
Plain TextSmith, Bernard (1924) On the West Cumberland Brockram and its Associated Rocks. Geological Magazine, 61 (7) 289-308 doi:10.1017/s0016756800086441
In(1924, July) Geological Magazine Vol. 61 (7) Cambridge University Press (CUP)
Abstract/NotesFor many years the breccia of Western Cumberland has been known locally as “ The Conglomerate ”, under which name it figures largely in hundreds of records of borings put down in search of haematite or coal. Since, however, its components consist in general of angular and subangular rather than rounded fragments, the term “ conglomerate ” is misleading; hence the deposit is here referred to as “ Brockram ” (broken rock), a descriptive lithological term applied to rocks of similar origin in the Vale of Eden and of definite significance to British geologists.


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