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-41- <br /> The quality and quantity of the alluvial aquifers of Fourmile Creek, Thompson <br /> Creek and Coal Creek will not be cumulatively impacted during the first 5-year <br /> permit period of the three mines. There is a possibility of quality and <br /> quantity impacts on Coal Creek in the distant future when, and if, the north <br /> Thompson Creek Mines progress into the Coal Creek Drainage. <br /> There is a minor potential for the Coal Basin Mine load-out and the North <br /> Thompson Creek Mine load-out to cumulatively impact the quality and quantity <br /> of ground water in the Roaring Fork alluvium, since both load-outs are located <br /> on this alluvial body. However, both of these load-outs have limited surface <br /> disturbance, small amounts of disturbed drainage to handle, and much of the <br /> disturbed drainage water is going into total containment lined ponds. <br /> Therefore, that minor amount of polluted drainage which may escape from the <br /> drainage control system will negligibly impact the quality of the vast amounts <br /> of Roaring Fork alluvial water. <br /> The greatest cumulative ground water impact will be the indirect depletion of <br /> surface water flow through the ground water system to the mine workings. <br /> Since the impacts are to surface water, they are quantitatively discussed <br /> below in the Surface Water section of this Cumulative Impacts Study. The <br /> mechanism of stream depletion has been discussed in the general description of <br /> ground water. <br /> Cumulative Impacts - Surface Water <br /> One of the potential cumulative impacts that has been effectively mitigated is <br /> unnatural sediment loads generated by the operations. The sediment control <br /> systems in use at all mines and the strict effluent limitations imposed on all <br /> discharges will keep sediment loads near natural levels. It also should be <br /> noted that all three mines considered in this assessment are underground mines <br /> with minimal surface disturbance. Total surface disturbance is only 0.06% of <br /> the 1451 square mile Roaring Fork River Basin. Because of these facts, <br /> cumulative sediment loads are not expected to be significant. <br /> The cumulative effect of impounding water in sediment ponds at all three mines <br /> will also be insignificant. Because of the small relative surface disturbance <br /> at each mine, pond storage volumes are likewise small . Sedimentation ponds at <br /> all mines are dewatered within 72 hours to minimize any water loss to the <br /> hydrologic system. <br /> The total worse case depletion to the Roaring Fork River by mine inflows is <br /> small . If all mine inflows were consumed and not discharged back to the <br /> receiving stream, a total of 456 acre-feet/year would be depleted from the <br /> Roaring Fork. This is only 0.06% of the total flow. Even during the low flow <br /> of 179 cfs for the period of record on Roaring Fork, the total depletion would <br /> be 0.4%. This amount is insignificant to the surface water system. (Refer to <br /> Table 4. ) <br />