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-25- <br /> Mid-Continent will be undermining the headwaters of Muddy Creek, a tributary <br /> of the North Fork of the Gunnison. The underground workings at that point <br /> will be over 2,000 feet below the ground surface. There is no surface <br /> disturbance in this watershed and subsidence effects are projected to be <br /> small , therefore, this portion of the Coal Basin mining operation will not be <br /> considered in the cumulative hydrologic impact assessment. The other two <br /> mines are entirely within the Roaring Fork drainage basin. <br /> All three mining operations in the general area are underground operations. <br /> The life-of-mine areas of these mines are plotted on Figure 3. In addition, <br /> the coal seams to be mined, the area of surface disturbance, the area to be <br /> undermined during the first 5-year permit period and the area to be undermined <br /> during the life-of-mine are tabulated in Table 1. This assessment is divided <br /> into the three major subsections: Description of the Hydrologic Environment, <br /> Probable Hydrologic Consequences of Mining and Cumulative Hydrologic Impact <br /> Assessment. <br /> Description of the Hydrologic Environment <br /> The first part of this assessment describes the hydrology of the Roaring Fork <br /> River Drainage Basin. This includes a regional description of 1) topography, <br /> 2) precipitation and runoff, 3) geology, 4) ground water, and 5) surface water. <br /> Topography <br /> The topography of the Crystal-Roaring Fork Drainage Basin consists of broad <br /> flood plains and terraces in the lowland river valleys flanked by steep walled <br /> canyons and of broad park areas along the tributary streams. The topography <br /> is strongly controlled by the erosional resistance of the sedimentary rock <br /> strata along the Grand Hogback. Resistant sandstone strata form steep sloped <br /> water gaps along stream channels, and form prominent ridges and cliffs. <br /> Erosive shale strata form the broad river valleys and intra-mountain parks. <br /> The tributaries that flow through the mine sites have steep relief and steep <br /> stream gradients. Fourmile Creek varies in elevation from 10,361 feet at Bald <br /> Mountain to 7,831 feet at the Sunlight Mine to 5,950 feet at the Roaring Fork <br /> River. Thompson Creek varies from 10,927 feet at Twin Peaks to 7,500 feet at <br /> the North Thompson Creek Mines to 6,350 feet at the Crystal River. Coal Creek <br /> varies from 11,852 feet at Huntsman Ridge to 8,000 feet at the surface <br /> facilities of the Coal Basin Mines to 7,165 feet at the confluence with the <br /> Crystal River. <br /> Precipitation and Runoff <br /> Mean annual precipitation varies with elevation and slope attitude, that is <br /> precipitation is orographically controlled. The mean annual precipitation at <br /> Glenwood Springs (lowest end of the Roaring Fork watershed) is 16 inches per <br /> year; at the Sunlight Mine, it is about 18 inches; at Basalt, Colorado, it is <br /> 15 inches; at the Coal Basin Mines, it is 26.4 inches; and, at the upper <br /> elevations along Huntsman Ridge, the mean annual precipitation is in excess of <br /> 40 inches. <br />