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February 2000 Chapter 3 Page 3-77 <br />one is on BLM surface (J&B Spring and Pipeline 5). These sites are used for stock watering <br />purposes. <br />Six adjudicated water rights associated with wells are located in or around the Iron Point Coal <br />Lease Tract and Exploration License Area. All but the Blue Ribbon well are located along the <br />!North Fork of the Gunnison River and are apparently installed in saturated alluvium. The Biue <br />Ribbon well is located in Hubbard Creek adjacent to the historic Blue Ribbon Mine. This well is <br />installed in the alluvium of Hubbard Creek and has not been in use since the Btue Ribbon Mine <br />was closed. <br />The King Clay well is located on the West Fork Terror Creek. This shallow well is installed in <br />the alluvium along West Fork Terror Creek and is for domestic use. The Peggy Seabloom well <br />is located on the East Fork Terror Creek, about a mile west of Terror Creek Reservoir. This <br />shallow well is installed in the alluvium along Easf Fork Terror Creek and is for domestic use. <br />Elk Creek Coal Lease Tract -There are no adjudicated water rights associated with springs in <br />the Elk Creek Lease Tract area. <br />Two adjudicated water rights associated with wells are located near the Elk Creek Coal Lease <br />Tract (Bear No. 1 and Somerset Mine wells). These wells are located along the North Fork of <br />the Gunnison River and are apparently installed in saturated alluvium. All other active <br />registered wells without water rights are used only for monitoring. <br />3.6.3 Environmental Consequences <br />Coal mine development in the Iron Point and Elk Creek Coal Lease tracts and exploration <br />activities on the Iron Point Exploration License area could potentialty result in some impacts to <br />area groundwater resources. <br />Longwall mining causes bedrock fracturing and land subsidence above longwall panels. By <br />potentially providing pathways for groundwater to move downward toward the tnihed horizon; <br />fracturing and subsidence may divert water from saturated horizons and surface water bodies <br />above and adjacent to quad areas. Impacts to groundwater systems may potentially result in <br />the decrease in natural discharge rates from springs and seeps or change water levels and <br />yields in area wells. Potential effects include the following. <br />Mining would dewater the coal seam and water-saturated horizons immediately <br />above and below the coal seam. <br />Water quality could be degraded when groundwater flows through active or <br />abandoned mine workings. <br />Transbasin diversion of groundwater resulting from dewatering of the coal seam is a <br />potential impact. <br />Water rights could be affected if area spring flows and associated pond levels and <br />well water levels are diminished. <br />Increased sedimentation of area springs from construction and use of surface <br />facilities (exploration drill pads and associated access roads) could occur. <br />Accidental fuel or solvent spills could impact shallow groundwater locally. <br />