U.S.
GEOLOGICAL SURVEY
Water-Resources Investigations Report 00-4144
Occurrence and Quality of Surface Water and Ground Water within the Yavapai-Prescott Indian Reservation, Central Arizona, 1994-98
By
G.R. Littin, Margot Truini, H.A. Pierce, and B.M. Baum
ABSTRACT
The Yavapai-Prescott Indian Reservation encompasses about 1,395 acres in central Arizona adjacent to the city of Prescott. From October 1994 to September 1997, the annual average rainfall was 14.9 inches and the total annual streamflow leaving the reservation along Granite Creek was about 430 acre-feet more than the amount of streamflow entering the reservation. The channel-fill and valley-fill sediments within the flood plain of Granite Creek make up the principal aquifer. The only ground-water development is from spring discharge that is being contained for livestock and wildlife use. About 29 acre-feet of ground water leaves the reservation each year after discharging into Granite Creek. Water levels in wells throughout the reservation reflect seasonal variations in rainfall and snowmelt.
Surface water and ground water on the reservation are calcium bicarbonate types.
Specific-conductance field measurements ranged from 187 to 724 microsiemens
per centimeter for surface water and 381 to 990 microsiemens per centimeter
for ground water. Fecal streptococcal bacteria and fecal coliform bacteria in
the surface water make the water unsuitable for domestic use. Some volatile
and semivolatile organic compounds were detected in samples of surface water,
ground water, and streambed sediment. The potential for contamination exists
from point and nonpoint sources on and off the reservation.
Abstract
Principal findings
Introduction
Data collection and analysis
Water resources
Summary
Selected references
Basic data
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