. The ore deposits of Utah. B. POLISHED SURFACE OF SPECIMEN SHOWN IN A. Veinlets of metallic pold; dark areas, brown carbonate containinga little limonile. Enlarged 4 2). SPECIMEN SHOWN IN C, WITH CROSSED 30 diameters. ORE DEPOSITS OF UTAH. 599 UINTA MOUNTAINS. By B. S. The Uinta Mountains have yielded relativelysmall amounts of metals and have thereforebeen httle studied l)y the WTiter m preparationfor this paper. In September, 1913, he spenttwo days m a trip from Vernal to the Dyermine, and the same month he and F. L. Hessvisited prospects in
. The ore deposits of Utah. B. POLISHED SURFACE OF SPECIMEN SHOWN IN A. Veinlets of metallic pold; dark areas, brown carbonate containinga little limonile. Enlarged 4 2). SPECIMEN SHOWN IN C, WITH CROSSED 30 diameters. ORE DEPOSITS OF UTAH. 599 UINTA MOUNTAINS. By B. S. The Uinta Mountains have yielded relativelysmall amounts of metals and have thereforebeen httle studied l)y the WTiter m preparationfor this paper. In September, 1913, he spenttwo days m a trip from Vernal to the Dyermine, and the same month he and F. L. Hessvisited prospects in the vicinity of BrownsPark. The followmg statements concerningthe geology of the range are largely a com-pilation. PHYSIOGRAPHY. The Uinta Range extends from the WasatchRange in the northeastern part of Utah east-ward into Colorado, a distance of about 150mQes, with an average width of approximately35 miles. Its glacial features have been de-scribed in detail by Atwood,^ and its topog-raphy and physiography have been summarizedby BoutweU ^ as follows: The general form of the range is an elongated, broad,flat-topped arch. As the main east-west divide lies northof the cent
Size: 1584px × 1577px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookdecade1920, booksubjectminesandmineralresou
