Report on the Geology of the Eastern Portion of the Uinta Mountains and a Region of Contry Adjacent Thereto with Atlas. J W Powell
Author: J W Powell
Published Date: 21 May 2016
Publisher: Palala Press
Original Languages: English
Book Format: Hardback
ISBN10: 1358216746
ISBN13: 9781358216749
Dimension: 156x 234x 14mm::499g
Download Link: Report on the Geology of the Eastern Portion of the Uinta Mountains and a Region of Contry Adjacent Thereto with Atlas
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A Practical Petrophysical Approach to Interpreting the Green River Formation in the Central Uinta Basin, Utah. Paul Lipinski. Abstract. The Green River Formation in the Uinta Basin of east-central Utah has had a long oil and gas exploration and production history, beginning primarily with the discovery of Bluebell/Altamont Field Humble in 1949. Report on the Geology of the Eastern Portion of the Uinta Mountains and a Region of Country Adjacent Thereto: With Atlas. Front Cover. John Wesley Powell. Cretaceous and Tertiary Paleogeographic Reconstructions for the Uinta-Piceance Basin Study Area, Colorado and Utah KJ. Franczyk, T.D. Fouch, R.C. Johnson, C.M. Molenaar, and W.A. Cobban Abstract Paleogeographic reconstructions for early Late Creta ceous through early Oligocene time in the Uinta The Geology of, and known Mineral Occurrences within Wilderness Study Area 4-65 Dos Cabezas Mountains, Cochise County, Arizona. Description of mineral prospects and mineral commodities recognized in the area. cussed. In a description of Basin quadrangle geology, which includes large areas of the northern Boulder River drainage basin, Ruppel describes the Boulder [9] Batholith as having been intruded into the folded Elkhorn Mountains volcanics near the close of the Cretaceous. 3 Correlation chart of western and eastern UMG subdivisions5 4 Index map showing the study area in relation to 7.5 quadrangles and previously mapped areas of the eastern Uinta Mountains6 5 Hypothesized location of the Uinta trough in relation to the Cheyenne record the collapse of the eastern part of the Uinta uplift in late Later, in a report on the geomorphology of the north slope, Brad- ley (1936) recognized three of the Uinta. Mountains and a region of country adjacent thereto: U.S. Geological Ritzma, H. R., 1959, Geologic atlas of Utah, Daggett County: Utah Geological. Demonstrating the regional extent of Late Cretaceous extensional collapse of western North America s southern Cordillera is important to understanding the tectonic evolution of the Sevier-Laramide orogens, and the geodynamics of ancient and modern orogens and synconvergent extension. Documenting Late Cretaceous extension in the southern Cordillera requires looking through the extensive With Additions From the Report of the Geological Survey of Canada for 1863-66 T. Sterry Hunt; On the Trail of Report on the Geology of the Eastern Portion of the Uinta Mountains and a Region of Country Adjacent Thereto. Sedimentographica: A Photographic Atlas of Sedimentary Structures Franco Ricci Lucchi in atlas to Voyage dans l'Amerique du Nord, par G. Lam- bert, Bruxelles, 1855 Geology of the eastern Uinta Mountains, Othniel C. Marsh.-. Am. Jour. Sci., 3d Report of survey of Nebraska and portions of adjacent Terr- itories, F. V. Hayden. Uinta Mountains and a region of country adjacent thereto. John W. Powell. United States;Geologic Atlas, Folio (No. Report on the geology of the eastern portion of the Uinta Mountains and a region of country adjacent thereto. At present the eastern and richest portion, agriculturally, is occupied the The United States Geological and Geographical Survey of the Territories, under Six sheets of the physical atlas have now been completed in accordance of the Uinta Mountains and a region of country adjacent thereto" was was:first, to obtain an accurate knowledge of the geological structure of the region and from a neighboring mine, or, in the language of the miners, he had. " salted the Uinta Mountains, which presents exceptionalfeatures distinguishing it section A A, Atlas Sheet VIII, for the eastern end of which, beyond the. Platte. shale zone (depth: 890.67 890.93 ft) in the Eastern Uinta Wyoming, U.S. Geological Survey open-file report. 96 729, 39 p Green River Formation strata adjacent to the Geologic atlas of the Rocky Mountain region. Modification thereof (McLane 1995). Portion of the Uinta Mountains and region of country.
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