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- W2048602784 abstract "Abstract Ralston, D.R. and Williams, R.E., 1979. Groundwater flow systems in the western phosphate field in Idaho. In: W. Back and D.A. Stephenson (Guest-Editors), Contemporary Hydrogeology — The George Burke Maxey Memorial Volume. J. Hydrol., 43: 239-264. The complex geologic setting of the western phosphate field in Idaho provides the environment for equally complex groundwater flow systems. This research was initiated in 1974 to provide general and detailed hydrologic data on specific areas to aid in understanding the water-resource systems in the western phosphate field. Geologic, hydrogeologic and hydrologic data were collected in Little Long Valley and Lower Dry Valley in the Blackfoot River basin. Two groundwater flow systems are important in relation to the present and proposed mining in Little Long Valley: (1) the local shallow flow systems in the western ridge; and (2) the intermediate flow system in the Dinwoody Formation on the eastern ridge. The baseflow of Angus Creek in Little Long Valley is dependent on the groundwater flow systems in both ridges during the first one or two months following snow melt. The baseflow of the stream is almost completely dependent on the intermediate flow system in the eastern ridge for the rest of the year. Three groups of groundwater flow systems have been delineated in the Lower Dry Valley study area: (1) flow systems in the Thaynes and Dinwoody Formations along Schmid Ridge; (2) local flow systems in the shallow unconsolidated material on the east slope of Schmid Ridge; and (3) a Dry Valley—Slug Creek Valley flow system in the Wells Formation. The locations of the springs that discharge from the Thaynes and Dinwoody Formations are largely controlled by the axis of the Schmid Syncline and by small E—W-trending faults. The interbasin Dry Valley—Slug Creek Valley flow system is postulated based upon the geologic configuration formed by the Schmid Syncline, the loss of surface water on the floor of Dry Valley, the downward gradient in groundwater potential in the Phosphoria Formation in Lower Dry Valley and the existence and flow pattern of springs in the Slug Creek Valley. Care must be taken to avoid creating groundwater flow systems in any waste piles constructed as part of the mining activity. Drainage from a waste-pile flow system would probably be poorer quality than water from natural flow systems in the area." @default.
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- W2048602784 date "1979-10-01" @default.
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- W2048602784 title "Groundwater flow systems in the western phosphate field in Idaho" @default.
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- W2048602784 doi "https://doi.org/10.1016/0022-1694(79)90175-6" @default.
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