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<br />Division of Minerals and Geology <br />9 November 2000 <br />Page 2 <br />Exhibit G -Water Information <br />Section 8.02 -Surface Water System <br /> <br />1. Reference to the flood boundary was incorrectly stated as appearing on Exhibit C (Pre- <br />mising Plan) map. The flood boundary is depicted on the air photomap designated as <br />Exhibit G (Water Information Map). Additional flood boundary information, as well as <br />responses to technical adequacy items 2a and 2b under this section, are being sent under <br />separate cover from Pickett Engineering, Inc. <br />Section 8.03 -Groundwater System <br />Dewatering trenches are typically located around the perimeter of the current mining <br />phase. Settling will occur in the trenches, and if necessary, settling ponds will be <br />constructed at a point prior to discharge. Discharges will be to the Cache La Poudre <br />River at various points as designated within the NPDES Permit for this site. As indicated <br />in our application, a copy of the NPDES permit will be submitted to DMG when the <br />permit is issued. <br />2. The proposed gravel mining operations will impact the alluvial groundwater aquifer at the <br />proposed facility. This is because dry mining operations are proposed to a depth below <br />ground surface of 30 fl. <br />The alluvial aquifer system at the proposed facility is in close proximity to the Cache La <br />Poudre River. The aquifer is generally characterized by coarse, well graded gravels <br />extending from a few feet below ground surface to a total depth of approximately 70 feet. <br />Within these alluvial materials, groundwater generally occurs between 8 and 10 feet <br />below ground surface. Therefore, there appears to be an approximately 62 foot saturated <br />thickness within the alluvial aquifer in the vicinity of the facility. Groundwater gradients <br />and horizontai flow direction are somewhat difficult to determine based on existing well <br />data. This is because existing well data indicate a relatively flat groundwater surface in <br />the vicinity of the facility. However, it can reasonably assumed that there is a gentle <br />horizontal gradient toward the Cache La Poudre River in the vicinity of the facility. <br />Aquifer ttansmissivity is estimated based on a total samrated aquifer thickness of <br />approximately 62 feet and assumed hydraulic conductivity of the gravel materials of 1 x <br />10-2 cm/sec. This yields a calculated aquifer transmissiviry of approximately 19 cm/sec. <br />3. The applicant proposes to use "Option C" to demonstrate that impacts to surface and <br />groundwater will be minimized both during mining and reclamation for the proposed <br />facility. The applicant commits to mitigating any adverse impacts to ground water levels <br />surrounding the facility during operation and reclamation of the facility. Because the mine <br />plan calls for dry mining down to 30 feet, it is anticipated that this dry mining will <br />produce the maximum groundwater drawdown in the vicinity of the proposed facility <br />\\DEN Vnnunon\PRO)ECrS\20167 Greeley\RCSpon< io iech Rev2.da <br />