Abstract
Research Article| January 01, 1901 Geology of Rigaud mountain, Canada OSMOND EDGAR LE ROY OSMOND EDGAR LE ROY *Introduced by F. D. Adams. Search for other works by this author on: GSW Google Scholar GSA Bulletin (1901) 12 (1): 377–394. https://doi.org/10.1130/GSAB-12-377 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation OSMOND EDGAR LE ROY; Geology of Rigaud mountain, Canada. GSA Bulletin 1901;; 12 (1): 377–394. doi: https://doi.org/10.1130/GSAB-12-377 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract IntroductionRigaud mountain is situated in the northwestern part of the county of Vaudreuil, Province of Quebec, Canada, and includes in its area the parish of Saint George and parts of the parishes of Rigaud, Saint Redempteur, and Sainte Marthe. It is the most western of a line of hills of igneous origin, which, in the vicinity of Montreal, forms the principal topographic feature of the eastern part of the Paleozoic plain of central Canada. These hills—locally termed mountains—are at no great distance from the border of the V-shaped Laurentian protaxis, and follow a line of disturbance which is almost at right angles to the trend of the Notre Dame range. In westward succession there are Shefford, Yamaska, Rougemont, Beloeil, Montarville, Mount Royal, and Rigaud. The hills of Brome, lying south of Shefford, and mount Johnson, south of Beloeil, are on another line, but evidently belong to the same series. . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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