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Availability of ground water in the Bear River valley, Wyoming

Author: Charles Joseph RobinoveDelmar W BerryJohn G ConnorGeological Survey (U.S.)United States. Department of the Interior.All authors
Publisher: [Washington D.C. ] : Geological Survey, Washington, D.C. : U.S. G.P.O. 1963.
Series: Geological Survey water-supply paper, 1539-V.; Contributions to the hydrology of the United States.
Edition/Format:   Print book : National government publication : English
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Genre/Form: Maps
Geological maps
Material Type: Government publication, National government publication, Internet resource
Document Type: Book, Internet Resource
All Authors / Contributors: Charles Joseph Robinove; Delmar W Berry; John G Connor; Geological Survey (U.S.); United States. Department of the Interior.; Wyoming. State Engineer's Office.; Wyoming Natural Resource Board.
OCLC Number: 7022854
Notes: "United States Department of the Interior. Stewart L. Udall, secretary. Geological Survey. Thomas B. Nolan, director."--Verso title page.
Two folded leaves in pocket.
Description: iv, 44 pages, 2 plates : illustrations, maps ; 24 cm.
Cartographic Mathematical Data: Scale 1:63,360; (W 111°02ʹ--W 110°58ʹ/N 41°30ʹ--N 41°00ʹ).
Contents: Map of the Bear River Valley, Wyoming, showing the geology, depth to water, depth of well and location of wells and springs for which records are given --
Hydrograph of Bear River north of Evanston, Wyoming (16-121-13ba), from October 1, 1955, to September 30, 1956, diagrams show chemical composition of water in relation to discharge, (streamflows below 20 CFS are relative and not to log scale).
Series Title: Geological Survey water-supply paper, 1539-V.; Contributions to the hydrology of the United States.
Other Titles: Map of the Bear River Valley, Wyoming, showing the geology, depth to water, depth of well and location of wells and springs for which records are given.
Hydrograph of Bear River north of Evanston, Wyoming (16-121-13ba), from October 1, 1955, to September 30, 1956, diagrams show chemical composition of water in relation to discharge, (streamflows below 20 CFS are relative and not to log scale).
Responsibility: by Charles J. Robinove and Delmar W. Berry ; with a section on chemical quality of the water by John G. Connor ; prepared in cooperation with the Wyoming Natural Resource Board and the State Engineer of Wyoming.

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