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Mine removed coal from the F seam in the lower Williams Fork. The No. 6 Mine portal was <br />used to access and mine coal from the E seam in the lower Williams Fork. (The adjacent surface <br />pits of the Trapper Mine take coal from the upper Williams Fork. The I seam of Trapper <br />probably correlates to the P seam of the Williams Fork Mines, No. 5. mine) <br />Geologic Structural Setting. The Williams Fork Mines are situated on the northeast flank of the <br />northwest plunging Moffat Anticline. The Moffat Anticline is part of the larger -scale Axial <br />uplift that extends northwestward across northwest Colorado to the Uinta Mountains in northeast <br />Utah. The northeast limb of the Moffat Anticline dips northward into the Big Bottom syncline. <br />Although only small - displacement gravity faults have been found in the permit area, the large <br />displacement Moffat thrust fault probably lies several thousand feet beneath the ground surface <br />of the permit area. The surface trace of the Moffat thrust is two miles southwest of the permit <br />area. <br />Local Coal Mining History. Previous mining within the Williams Fork Mines permit area <br />included: the Fields Mine which operated in the E seam during the 1930s; the Wise Mine and the <br />Wise Hill No. 2 which operated in the C seam (below the E seam) in the 1940s and 1950s; the <br />Leo White and Baker Mines which operated in the Hart seam (between the F seam and <br />Twentymile sandstone); and the Wise Hill Nos. 3 and 4, which operated in the Hart seam during <br />the 1970s. <br />Surface Water Features. Drainages within and adjacent to the permit area (on the north- facing <br />slope) are ephemeral and generally extend south to north down the slope in a dendritic pattern. <br />These drainages flow primarily in response to snowmelt or heavy rains. Flows in these drainages <br />that do not infiltrate into the ground or evaporate eventually enter the Williams Fork River, and <br />then flow the short distance to the confluence with the Yampa River in the northwest corner of <br />the permit area. <br />Yampa River Flows. Flow in the Yampa River depends primarily on snowmelt from the winter <br />snowpack on the high mountain slopes surrounding the drainage basin. The lower intermittent <br />and ephemeral drainages produce only a small part of the total water yield of the basin (Colorado <br />Water Conservation Board, 1969). About 64 percent of the flow occurs in May and June with up <br />to 84 percent occurring from April to July at selected gaging stations within the drainage basin <br />(Steele, et al., 1979). Minimum flows generally occur from August through February. Irons, et <br />al. (1965) reported that summertime flows in streams of the basin from July through October <br />generally include a large component of ground water discharge. Extremes recorded at the <br />Maybell Gaging Station are a maximum flow of 17,900 cfs on May 19, 1917, and a minimum of <br />2.0 cfs on July 17 -19, 1934. Annual variation in yield may also be great. Historical annual yield <br />has varied from 345,000 acre -feet in 1977 to 2,135,000 acre -feet for the Yampa River in 1917. <br />Average annual yield amounts to 1,116,000 acre -feet. <br />Williams Fork River Flows. The Williams Fork River is a major tributary of the Yampa River. <br />The Williams Fork drains approximately 350 square miles, or ten percent of the Yampa River <br />Valley. The Williams Fork fluctuates seasonally like the Yampa, but is more dependent on <br />snowmelt, and there is less ground water discharge to sustain the flows of the river during low <br />flow periods. Flows in the Williams Fork in the permit area typically range between 2500 cfs <br />during spring runoff and less than 100 cfs during low flow. <br />Williams Fork Mines 6 Permit Renewal 06 <br />C- 1981 -044 December 8, 2014 <br />