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February 9, 2001 <br /> Page 3 of 4 Pages <br /> It is possible that present and future mining activities may slightly reduce the flow of ground water <br /> moving through the coals towards the Piceance Basin (permit, page 3-49). There is no monitoring <br /> associated with groundwater flows to the Piceance Basin. <br /> No adverse impact is inferred to regional groundwater,but not distinctly stated (permit, page 3-60). <br /> There is no monitoring of regional groundwater flows. <br /> A soil loss comparison, pages 4-19i through4-19iii of the permit, concludes that untreated drainage <br /> (surface) from reclaimed areas would contribute slightly fewer suspended solids that untreated <br /> drainage from the natural surrounding areas. There is no monitoring associated with this conclusion. <br /> A statement is made that water quality will not be impacted by suspended solids during reclamation <br /> or after a large precipitation event (permit, page 4-105). "No discharge" reports (Refuse and Pond <br /> 9 sedimentation ponds) indicate performance within this prediction. An analysis after a vegetation <br /> survey performed during July 1992 demonstrated that untreated drainage from the reclaimed mine <br /> site does not contribute additional suspended solids above natural conditions. No monitoring is <br /> accomplished for small areas that have exemptions from sediment pond treatments. <br /> Seals (portals) were designed to withstand anticipated hydrostatic heads of flooded mines (permit, <br /> page 4-66). However, the seals at Portal 1 did not prevent seepage of mine water, and drainpipes at <br /> Portal 3 allow for drainage of mine water. <br /> "The flow in North Thompson Creek will not be significantly affected by impoundments, surface <br /> disturbances, or surface facilities."(permit, page 4-109) Monitoring through 1985 did not establish <br /> depletion to the North Thompson Creek and Middle Thompson Creek, and monitoring was <br /> discontinued in 1986 (permit, page 5-115b). <br /> "---the effects of the altered infiltration and evapotranspiration rates on the entire watershed's flow <br /> rates would be imperceptible due to the minor percentage of watershed area involved." (permit,page <br /> 4-110) Monitoring through 1985 did not establish depletion to the North Thompson Creek and <br /> Middle Thompson Creek, and monitoring was discontinued in 1986 (permit, page 5-115b). <br /> "The refuse pile would have a minimal impact on the water quality of North Thompson Creek." <br /> (permit,page 4-114) Surface runoff is directed into the Refuse Pile Sedimentation Pond, discussed <br /> earlier. Data obtained for monitor well (refuse pile piezometer, directly below the pile) D-1 A <br /> indicates conductivities nearly double those of piezometer D-2A (located to the west of the pile). <br /> Impacts on North Thompson Creek, however, are difficult to evaluate. No groundwater flow <br /> information of the Refuse Pile is available. North Thompson Creek experiences rise in total <br /> dissolved solids across the site (described as primarily from leaching of geologic formations <br /> undisturbed by mining operations formations and treated mine water discharges in the PAP). The <br /> AHR refers to baseline monitoring data and the discharges from Portal 2 (Abandoned Mined Lands <br /> peat bog water treatment system) for explanation for the increases. <br />