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approaches 50 percent of the total 631 gpm estimated in 1985 as average inflow <br />for the entire No. 5 Mine. The flow from these faults has remained - <br />essentially the same since 1983. The remainder of mine inflow results from <br />more general sources, ie. roof, floor, pillars and coal faces located both in <br />the western and eastern portions of the mine. The present area of activity in <br />the No. 5 Mine, located in the southeast part of the permit area, tends to be <br />the driest part of the operation. <br />Due to the inflow of water into the workings of the Eagle No. 5 Ftirte, the <br />quantity of ground water in adjacent aquifers can be impacted. The Trout - <br />Creek Sandstone lies some 320 to 360 feet below the "F" seam in which the <br />Eagle No, 5 is located. The Eagle No. 6 Mine, to be developed in the "E" seam <br />will be some 40 to 100 feet stratigraphically closer to the Trout Creek <br />sandstone. The Trout Creek Sandstone is under artesian conditions in most of <br />the permit area where it has supplied water for industrial and domestic <br />purposes. Regular monitoring of the Trout Creek aquifer, however, was not <br />conducted until rather recently when the growing body of evidence indicated <br />that the Trout Creek was dewatering into the No. 5 mine by way of the faults <br />encountered in the western mine workings. <br />Empire Energy Corporation produces water for its mining operations from two <br />wells in the Trout Creek aquifer, These wells, the No. 5 and 5A, are located <br />near the Eagle No, 5 Mine portal. Subsequent to encountering the <br />fault-associated inflows in the western mine workings, Empire Energy <br />Corporation reports the No. 5 Mine well experienced a decline in static head <br />which reduced it from a flowing to non-flowing artesian condition, The amount <br />of this past decline cannot be quantified from the existing records. Any <br />future impacts, however, will be documented since both the No. 5 Mine well and <br />the Okie Plaza well, which also produces from the Trout Creek sandstone, will <br />be included in the future hydrologic monitoring plan. A third Trout Creek <br />well, the No, 5A Mine supplemental well, is located within a few feet of the <br />No. 5 Mine well, and will not be monitored as part of the plan. No <br />significant additional impacts on the quantity of water in the Trout Creek <br />sandstone are likely to result from proposed mining of the "E" and "F" seams <br />during the first five permit years, Both the remainder of the work in the <br />Eagle No. 5 Mine and the Eagle No. 6 mining will be conducted in the eastern <br />and southeastern portions of the permit area where current general inflow into <br />the existing No. 5 Mine workings is minimal, where both the No. 5 and No. 6 <br />Mines are separated from the Trout Creek aquifer by significant thicknesses of <br />sedimentary rock, and where no evidence of faulting has been obtained, <br />The Middle sandstone lies approximately 125 feet to 150 feet above the "F" <br />seam and the Eagle No, 5 mining, At one time, the Middle sandstone was <br />believed to be the primary source of the fault associated water inflow <br />encountered in the western mine workings because of the relatively abrupt <br />declines in water levels recorded by Middle sandstone monitoring Wells TR-4, <br />TR-7A, and 81-Oi shortly after the fault zone was reached. As evidence <br />accumulated, however, that the Trout Creek sandstone is the more likely source <br />of the water and since water levels in the Middle sandstone have risen, it is <br />now argued that the earlier water level declines in the Middle sandstone were <br />simply climatic in orgin, related to drier years and periods of low recharge <br />of the aquifer. Whatever was responsible for those abrupt declines, the <br />impact on the quantity of water in the Middle sandstone is diminishing at this <br />time. Whether this lessening of impact will continue in the future as <br />-30- <br />