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Structural controls on ground-water conditions and estimated aquifer properties near Bill Williams Mountain, Williams, Arizona

Author: H A Pierce; Williams (Ariz.); Geological Survey (U.S.),
Publisher: Tucson, Ariz. : U.S. Department of the Interior, U.S. Geological Survey, Tucson, Ariz. : U.S. Department of the Interior, U.S. Geological Survey. 2001.
Series: Water-resources investigations report, 01-4058.
Edition/Format:   Print book : National government publication : EnglishView all editions and formats
Summary:
As of 1999, surface water collected and stored in reservoirs is the sole source of municipal water for the city of Williams . During 1996 and 1999, reservoirs reached historically low levels. Understanding the ground-water flow system is critical to managing the ground-water resources in this part of the Coconino Plateau. The nearly 1,000-meter-deep regional aquifer in the Redwall and Muav Limestones, however, makes  Read more...
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Additional Physical Format: Online version:
Pierce, H.A. (Herbert A.), 1951-
Structural controls on ground-water conditions and estimated aquifer properties near Bill Williams Mountain, Williams, Arizona
(OCoLC)680178662
Material Type: Government publication, National government publication, Internet resource
Document Type: Book, Internet Resource
All Authors / Contributors: H A Pierce; Williams (Ariz.); Geological Survey (U.S.),
OCLC Number: 47242836
Notes: Shipping list numbers : 2001-0230-P; 2003-0193-P.
Description: v, 41 pages : illustrations, maps (some color) ; 28 cm.
Series Title: Water-resources investigations report, 01-4058.
Responsibility: by Herbert A. Pierce ; prepared in cooperation with the City of Williams.

Abstract:

As of 1999, surface water collected and stored in reservoirs is the sole source of municipal water for the city of Williams . During 1996 and 1999, reservoirs reached historically low levels. Understanding the ground-water flow system is critical to managing the ground-water resources in this part of the Coconino Plateau. The nearly 1,000-meter-deep regional aquifer in the Redwall and Muav Limestones, however, makes studying or utilizing the resource difficult. Near-vertical faults and complex geologic structures control the ground-water flow system on the southwest side of the Kaibab Uplift near Williams, Arizona. To address the hydrogeologic complexities in the study area, a suite of techniques, which included aeromagnetic, gravity, square-array resistivity, and audiomagnetotelluric surveys, were applied as part of a regional study near Bill Williams Mountain.

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