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Evidence of elevation of the sea coast as shown by fossil deltas near Wolfville, N.S.

dc.contributor.authorChurchill, Frederick C.
dc.contributor.authorNova Scotian Institute of Science
dc.date.accessioned2010-07-23T14:58:02Z
dc.date.available2010-07-23T14:58:02Z
dc.date.issued1920
dc.identifier.citationChurchill, F. C. (1920). Evidence of elevation of the sea coast as shown by fossil deltas near Wolfville, N.S. Proceedings and Transactions of the Nova Scotian Institute of Science, 15(3), 137-140.en_US
dc.identifier.urihttp://hdl.handle.net/10222/12904
dc.descriptionRead November 8, 1920en_US
dc.language.isoenen_US
dc.publisherMcAlpine Publishing Co., Ltd.en_US
dc.subjectWolfville (Nova Scotia)en_US
dc.subjectDeltasen_US
dc.subjectSedimentation and depositionen_US
dc.subjectGeologyen_US
dc.subjectEarth scienceen_US
dc.subjectFossilsen_US
dc.subjectBed-rock (Triassic)en_US
dc.titleEvidence of elevation of the sea coast as shown by fossil deltas near Wolfville, N.S.en_US
dc.typeArticleen_US
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