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Mr. Tom Schreiner <br />May Z5, 2005 <br />Page 4 <br />Colorado water laws and regulations and Colorado water quality laws and regulations (NLRB Rules, <br />§3.1.6(1)(a) and (b)). Also, the Rules require a ground water monitoring program on acase-by-case <br />basis where an adverse impact on ground water quality may be reasonably expected (NLRB Rules, § <br />3.1.7(7)). Additionally, the CMLR Act states "disturbances to the prevailing hydrologic balance ... <br />and to the quality and quantity of water in surface and groundwater systems...shall be minimized <br />(Act 34-32-116(7)). Review of the proposed site indicates the mining operation will directly affect <br />both the surface and ground water systems for the following reasons: <br />The fractured aquifer yield is not poor as claimed by the applicant. Wells developed into this <br />aquifer in the vicinity of the proposed quarry site yield significant ground water (10-100+ <br />gpm). For example, one of Black Hawk's wells (approximately 4 miles northwest) produces <br />130 gpm,Black Hawk/Central City Sanitation District's (BHCCSD) well (within 600 feet of <br />the subject property) produces more than 20 gpm, and the Cleaz Creek Convenience store's <br />well (within 400 feet ofthe proposed quarry entrance) yields 20 gpm. <br />• The fractured aquifer is not classified as nontributary. Pumping tests in the area demonstrate <br />that the fracture system is hydrologically connected to the surface water system and is, <br />therefore, tributary. Furthermore, the State Engineer administers water in this aquifer as <br />tributary and subject to the priority system. <br />• Well data in the vicinity of the proposed quarry site indicate that ground water will be <br />• encountered with mining operations and that dewatering will be necessary. Review of 300 <br />wells within four miles of the site, shows the median depth to water is 120 feet. None ofthe <br />wells have a depth to water greater than 500 feet and only two percent exceed 400 feet. <br />Review of the well data also indicates that the water table is generally parallel to the ground <br />surface. Therefore, 1) the ground water system is recharged in the upland azeas, Z) the <br />ground water flows approximately parallel to the slope of the land, and 3) ground water <br />discharges to the perennial streams in the azea including North Clear Creek (adjacent to the <br />site] and Cottonwood Creek (within the site boundaries). <br />There is a risk that the quality and quantity of local ground water supplies will be adversely <br />affected. The BHCCSD well (permit number 59840-F, Augmentation Case No. 94C W036) <br />and the convenience store well aze completed in the fracture zone of the Black Hawk fault <br />(see Figure 1). This fault zone is hydraulically connected to the fractured aquifer underlying <br />the proposed quarry site. Therefore, the existing wells aze dependent on recharge that <br />currently occurs on the project site and flows across the site to the northeast. Significant <br />dewatering of the quarry will very likely reduce the yield from the existing wells. <br />• There is also a concern that the proposed mining operation (blasting, etc.) may introduce <br />contaminants to the interconnected fractures supplying the water to the nearby wells and <br />negatively impact the water quality. Additionally, the proposed blasting could plug the <br />interconnected fractures and reduce or eliminate the yield from these existing wells. <br />The permit should be denied because: <br />LEONARD RICE ENGINEERS, INC. <br />