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-56- <br />Effects of the Bear Coal Company Mining on Operations on Surface Water <br />The proposed Bear No. 3 mine plan is designed to minimize the impacts of the project <br />on the surface water hydrology of the region. The surface disturbance at the Bear <br />No. 3 will be limited to approximately 8 acres. Drainage from the disturbed area <br />will be routed to a sediment pond and will meet NPDES permit requirements prior <br />to discharge. All discharges will be monitored for pH, total suspended solids <br />(TSS), total dissolved solids, iron, manganese, and oiI and grease content. The <br />19 acre disturbed area at the Bear No. 1 and No. 2 portals will be revegetated in <br />the fall of 1982, and runoff rates and quality of runoff from the area should <br />approximate that from adjacent areas in succeeding years. The hydrologic consequence <br />of the Bear mine operation on the North Fork of the Gunnison are minimal. For a <br />detailed discussion of the potential impacts on surface water in the permit and <br />adjacent area, please see the Section VII, Alluvial Valley Floors. <br />Cumulative Hydrologic Impact Assessment <br />Impacts on Ground Water <br />The six underground mines along the North Fork of the Gunnison may impact ground <br />water quantity by one or more of the following: <br />- induced inflows into the mines through faults and fractures which provide <br />communication between the mine and overlying and underlying aquifers and <br />surface waters; <br />- dewatering of the coal, roof and floor with the advance of mining; and <br />- subsidence induced flows into the mines. <br />Faults and Fractures <br />Faults and fractures produce a localized increase in porocity within the strata <br />cut by them. If the faults and fractures do not become sealed by clays, they <br />may become conduits for the flow of ground and surface water. When encountered <br />within the mine, faults and fractures will dewater. The amount of water flowing <br />into the mine from these sources depends on porocity and permeability of faults <br />or fractures, and on the open vertical connection within the faults and fractures <br />between the coal seam and sources of ground or surface water. <br />Fault and fracture controlled inflows have been noted and mapped in the U.S. Steel <br />Corporation Somerset mine application (Exhibit E8-366), the Western Slope Carbon <br />Hawk's Nest mine permit application (Exhibit 2.04.7(1) or W-1006), and the Western <br />Associated Coal, Blue Ribbon mine application (Exhibit-T), Colorado Westmoreland, <br />Inc. has not mapped inflows to date. However, they have noted inflows in faulted <br />areas. No inflow mapping is available at present for the Bear mines. However the <br />company states that it is not presently experiencing any mine inflows. The Mt. <br />Gunnison No. 1 mine has encountered only minor inflows from fractures in the <br />number one portal. <br />