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Mine water inflow into the Sanborn Creek Mine and Sanborn East Tract is estimated to be 425 gpm or less. The old Somerset Mine had an inflow rate of 0.15667 gpm/acre for the 1,500 acres of development in the mine that was below the level of the North Fork River. Projecting this rate to the 2,600 acres of the Sanborn Mine and Sanborn East Tract yields an inflow of 407 gpm. The operator has rounded this figure t0 425 gpm in the permit document. The operator has also projected an additional 235 gpm discharge from the old Somerset Mine, which might reach the North Fork via the alluvial system. This is considered to be extremely unlikely; however, the projection is used in the CHIS to allow for absolute worst-case prediction. The following are potential sources for inflow: The North Fork of the Gunnison River is 750 feet to the south and 100 feet above the proposed B-seam workings and 40 feet above the C-seam workings. Groundwater is expected to travel downdip from the river through the coal and overburden into the mine workings. Because of the low permeability of the coal and overburden, calculations have shown that these flows should be minor. The flows can be expected occur with a considerable lag time. There will be a comparable diminution of flow in the North Fork but mine pumpage will return this amount to the river, minus that used in the mine. The cone of depression from dewatering of the strata will only extend to the boundary of the North Fork and will not adversely impact any wells. 2. There is the potential that the mine may encounter water inflow from faults and fractures. The location of these faults are unknown. The largest fault that the old Somerset Mine encountered had a sustained inflow of 120 gpm, ~.vhich contributed 50 percent of the total inflow. The Somerset Mine has committed to conducting a study of the potential for mine inflow from the faults and fractures in the Coal Gulch area. 3. The Sanborn Creek Mine will undermine portions of two abandoned mines - the Oliver Mine and the Hawk's Nest Mine. The Oliver Mine :gas mined in the 1930's and is known to be completely flooded. An exposure of the workings adiacent to the old county road is discharging water at a rate of a few ga~lons oer minute. About 90 percent of the workings of this mine lie downdip of the discharge point. The riawk's Nest Mine lies north of the Oliver .•?ine and is stratigraohically higher than the Olver D seam. Hawk's Nest mined in both the E and F seams. The workings of this mine are probably not flooded, as indicated by measurements in an old drill hole. Also, curing cceration of the Ha~.vk's Nest Kline, therz '.vas very little inflow. because there i5 the potential that subsidence could cause fiacturing of the interburden bet.+een the B seam and the _tQ_