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Reynolds, S. H., Smith, Stanley (1925) The Old Red Sandstone and Avonian Succession at Westbury-on-Trym. Geological Magazine, 62 (10) 464-473 doi:10.1017/s0016756800106089

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Reference TypeJournal (article/letter/editorial)
TitleThe Old Red Sandstone and Avonian Succession at Westbury-on-Trym.
JournalGeological Magazine
AuthorsReynolds, S. H.Author
Smith, StanleyAuthor
Year1925 (October)Volume62
Issue10
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800106089
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Mindat Ref. ID280733Long-form Identifiermindat:1:5:280733:5
GUID0
Full ReferenceReynolds, S. H., Smith, Stanley (1925) The Old Red Sandstone and Avonian Succession at Westbury-on-Trym. Geological Magazine, 62 (10) 464-473 doi:10.1017/s0016756800106089
Plain TextReynolds, S. H., Smith, Stanley (1925) The Old Red Sandstone and Avonian Succession at Westbury-on-Trym. Geological Magazine, 62 (10) 464-473 doi:10.1017/s0016756800106089
In(1925, October) Geological Magazine Vol. 62 (10) Cambridge University Press (CUP)
Abstract/NotesIn the erection of a new home of rest—St. Monica's, in the grounds of what was formerly Cote House, near the top of Westbury Hill, an interesting section1 of the upper part of the Old Red Sandstone and of the lower Avonian rocks up to the top of Zx was exposed in digging the foundations. Although the section lies only a little over a mile north-east of the Avon section and the general succession of the two is very similar, the Westbury section is of considerable interest, particularly as certain levels were well seen which are not exposed in the Avon section. In all the following tables the strata are described from below upwards.


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