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Cretaceous and Tertiary Formations of the Wasatch Plateau, Utah
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1925
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EngineeringGeographyCretaceous PeriodArchaeologyGeologyGeological DataCretaceous-paleogene BoundaryColorado PlateauGsa Bulletin 1925Earth ScienceRegional GeologyIntegrated StratigraphyWasatch Plateau
Research Article| September 30, 1925 Cretaceous and Tertiary Formations of the Wasatch Plateau, Utah* EDMUND M. SPIEKER; EDMUND M. SPIEKER Search for other works by this author on: GSW Google Scholar JOHN B. REESIDE, JR. JOHN B. REESIDE, JR. Search for other works by this author on: GSW Google Scholar GSA Bulletin (1925) 36 (3): 435–454. https://doi.org/10.1130/GSAB-36-435 Article history received: 13 Apr 1925 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 EDMUND M. SPIEKER, JOHN B. REESIDE; Cretaceous and Tertiary Formations of the Wasatch Plateau, Utah. GSA Bulletin 1925;; 36 (3): 435–454. doi: https://doi.org/10.1130/GSAB-36-435 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 IntroductionThis paper is intended to present, in summary fashion, some of the results of stratigraphic work by the senior author in the Wasatch Plateau of Utah. In this study he has had the advantage of extensive conference, both in the field and in the office, with the junior author, who contributes to the paper the paleontologie part of the work and many of the comparisons with other regions.General Features of PlateauLOCATION AND SURFACE FEATURESThe Wasatch Plateau lies in central Utah. It is the northeastern unit of the great group of high plateaus that borders the northern part of the Colorado Plateau on the west and separates it from the Great Basin. The plateau is a fairly well-defined tableland, about 90 miles long and 20 to 30 miles broad, whose summits commonly reach elevations 10,000 to 11,000 feet above sealevel and 5,000 to 6,000 feet above Castle . . . 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.