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RULE 2 PERMITS <br />The Collom Lite pit is likely to be within the watersheds for springs VI, V 10, and V32 (West Fork of <br />Jubb Creek). These springs collectively produce about 0.024 cfs during September, during which <br />monitoring location WFJC was dry, indicating that the spring flow reinfiltrates into the valley fill, or is <br />captured in stock ponds before reaching the monitoring point. The springs contributed about 0.042 cfs in <br />May 2006 to the West Fork of Jubb Creek. Stream flow was measured in May 2005 as 0.10 cfs. No <br />conclusive estimate of the percentage contributed by the springs can be made given the likely difference <br />between hydrologic conditions in those two years. <br />Considering that 0.024 cfs was lost to valley fill or ponds during September, it appears that the <br />contribution of V1, V 10, and V32 to the peak flow at WFJC could be considerably less than the 42 <br />percent implied by a year -to -year comparison. At monitoring point CJC, the May 2005 discharge was <br />0.15 cfs, implying that the affected springs contribute 28 percent of the flow at that location. Since much <br />of the recharge is from undisturbed areas outside of the Collom Lite pit, the probable reduction is likely to <br />be less than half of this amount and not expected to be measurable or statistically significant. Once the <br />mining has been completed and the pit has been saturated, the contributions to surface water from springs <br />originating from infiltration into the Collom Lite pit would return to normal. <br />Collom Lite Pit Hydrology <br />The Collom Lite pit will have a reclaimed surface area of approximately 880 acres and a pit bottom that <br />inclines predominantly toward the north. The low point in the reclaimed pit topography will be at its <br />intersection with the valley of Little Collom Gulch, at an elevation of approximately 7,275 feet amsl. <br />Resaturation of the reclaimed pit backfill will occur from confined groundwater creating static conditions <br />following dewatering, infiltrating precipitation, seepage of surface water, and groundwater inflow from <br />upgradient areas. <br />The mining activity will not cause any decrease in the hydraulic conductivity or transmissivity of the <br />unmined bedrock units downdip (north) of the pit and the capacity of the bedrock units to transmit <br />groundwater will not diminish. Consequently, the recharge and upgradient inflow entering the pit area <br />will re -enter the bedrock units on the downdip side of the pit and flow in directions similar to the pre - <br />mining flow configuration. The ground water in the spoils will flow to the north through the pitwall due <br />to the hydraulic gradient in the area. <br />The first component of the pit spoils resaturation will be the reestablishment of the piezometric surface <br />for the confined conditions (as discussed in the WMC study). This elevation in the northern portion of <br />the Collom Lite pit is approximately 7150 feet (amsl). Once the dewatering pumps have ceased pumping, <br />this level should reestablish within a short time period. Some surface water from precipitation will help <br />the establishment of the saturated level. However, this inflow of ground water from the pitwalls and floor <br />will be much quicker than any recharge from any other source. Thus, the ground water from the pitwalls <br />below an elevation of 7150 feet will come into contact with any spoils much faster than any other ground <br />(or surface) water source. This level will be established before mining ceases in Collom, so all possible <br />pit spoil recharge will occur on top of this level. <br />It is very unlikely that groundwater resaturating the reclaimed pit will accumulate to an elevation high <br />enough to cause it to discharge to the valley fill or to the surface in Little Collom Gulch. That could <br />occur only if the capacity of the bedrock units downdip of the reclaimed pit to transmit groundwater flow <br />were to be diminished compared to the pre- mining condition. A range of time; necessary to resaturate the <br />reclaimed pit backfill to that point can be calculated from the pit topography, the volume of materials to <br />be resaturated, and the rate, of recharge to the reclaimed pit backfill, as describ�.d below. <br />Collom — Rule 2, Page 136 Revision Date: 9/28/11 <br />Revision No.: PR -03 <br />