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<br />49 <br /> <br />permit area. Mining activities will not have a significant effect on <br />snowmelt runoff. Overland runoff passes over disturbed areas within the <br />permit area to one of the eight sedimentation ponds, mentioned <br />previously in this section. This water may be discharged to the North <br />Fork or stored when water rights are in priority. <br /> <br />During Water Year 1982, MCC’s conditional right to withdraw water <br />from the North Fork was deemed absolute. When this water right is in <br />priority, water can be pumped from the intake point to the 10 acre-foot <br />freshwater pond. This water right is expected to be out of priority from <br />July to September. Average withdrawals from the North Fork of the <br />Gunnison are not expected to exceed 400,000 gallons per day (gpd) and <br />are likely to be on the order of 200,000 gpd. The freshwater pond is <br />filled during spring runoff and kept full until water rights are out of <br />priority. The water is either treated to meet potable and sanitary water <br />requirements, used and then treated as sanitary waste water, or is <br />withdrawn for dust suppression in the mine and becomes mine water. <br /> <br />The potential effects of MCC’s water diversion on North Fork flows <br />have been projected for flow rates and flow volumes. With the existing <br />pump capacity, 450 gallons per minute (gpm), the diversion would result <br />in a measurable change in flow during low flows having return periods of <br />about 200 years or greater, and would be less than 5 percent. During <br />extreme low flow periods, MCC's water rights would be out of priority <br />and diversion would not be undertaken. <br /> <br />Although subsidence fractures that develop over and next to mine <br />workings have the potential to dewater streams and ponds, Section <br />2.05.6(6) of the permit application explains that dewatering is unlikely to <br />occur because subsidence cracks that develop at the surface will not <br />extend deep enough to intersect fractures propagating upward from the <br />caved and fractured zones. Also, the stratigraphic sequence in stream <br />valleys is resistant to fracturing due to the presence of interbedded fine- <br />grained units. These beds would more likely undergo ductile <br />deformation (bed bending), rather than brittle deformation (bed <br />fracturing). Stream flows and local channel elevations will continue to <br />be monitored in the permit area, as set forth in the permit application. <br />Subsidence magnitudes of stock ponds will also be monitored. Specific <br />measures MCC will employ for assessing and protecting the Minnesota <br />Creek water supply are described in Exhibit 58 of the permit application <br />titled, "Protection of Minnesota Creek Water Supply." Possible <br />subsidence impacts to streams and ponds are discussed in the following <br />Subsidence Control section. <br /> <br />Underground mine workings will come within 800 ft. of the Monument <br />Dam and Minnesota Reservoir. MCC explains in Section 2.05.6(6) of <br />the permit application that the reservoir is unlikely to be affected by <br />mining because the dam and reservoir are outside the predicted angle of