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    <dct:description>Skull Valley is a north-trending narmw depression that extends about 50 miles from the vicinity of Lookout Pass in T. 8 S., R. 7 W., northward to the southwestern shore of Great Salt Lake. The Skull Valley drainage basin includes about 880 square miles. In the valley, the main ground-water reservoir is in unconsolidated rocks of late Tertiary and Quaternary age and underlies about 230,000 acres. The source of all water in Skull Valley is precipitation which falls mainly on the Stansbury and Onaqui Mountains. The estimated potential long-term average annual runoff from the uplands is about 32,000 acre-feet of water, but only a small part of this amount flows out of the valley. The remainder becomes recharge or is lost by evapotranspiration within the
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The estimated average annual ground-water recharge and discharge is in the range of 30,000-50,000 acre-feet per year. Ground water is discharged from Skull Valley by evapotranspiration, wells, surface outflow, and underflow from the mouth of the valley. Of these, evapotranspiration accounts for 80-90 percent of the total gmund-water discharge. In 1965, wells discharged only about 5,000 acre-feet of water.</dct:description>
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    <dct:title>Hydrologic Reconnaissance of Skull Valley, Tooele County, Utah </dct:title>
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