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~., -J- <br />III IIIIIIIIIIIII III <br />DIVISION OF MINERALS AND GEOLOGY <br />Depanmenl of Natural Resources <br />1313 Sherman SI., Room 215 <br />Denver, Colorado 80203 <br />Phone: 13031 866-3 567 <br />FAX: (3031 8328106 <br />February 5, 1999 <br />Jim Stover <br />MINREC, INC. <br />2768 Compass Drive, Suite 101 <br />Grand Junction, CO 81506 <br />STATE OF COLORADO <br />RE: Phase II and III Bond Release Evaluation <br />Red Canyon Mine (Permit C-81-034) <br />Dear Mr. Stover. <br />This letter addresses issues pertaining to hydrologic impacts and subsidence effects which were <br />not resolved during the bond release inspection of December 1, 1998, nor in the inspection <br />report issued pursuant to that inspection, on December 17, 1998. <br />Hydroloaic Impacts <br />In the review of the 1997 Annual Hydrology Report, DMG identified a potential concern with <br />respect to rising water levels in monitoring well E-1, and questioned whether the water level rise <br />was associated with mine inflows. Based on E-1 water quality, the operator has speculated that <br />well E-1 may contain a mixture of water from the E-seam and the overlying alluvium, which <br />might explain the higher than expelled water level in the well. This assertion regaring the <br />source of increasing head in well E-1 has not been adequately documented. The mixing of <br />alluvial water and coal seam water could occur if the well was improperty constructed or has <br />perforated casing installed across both the alluvial aquifer and the wal seam. Information in the <br />permit application package (PAP) regarding well E-1 completion is incomplete and somewhat <br />contradictory. Accurate well completion information is important for understanding potential <br />sources of inflow to the well casing/borehole. Given the available information, potential sources <br />for the rising water inGude recharge from the glaciaUalluvial aquifer, inflow from the E-Seam <br />workings, and possibly infiltration from an irrigation ditch located adjacent to well E-1. Infiltration <br />from the irigation ditch is unlikely unless there is no surface casing or the surface casing is <br />damaged. <br />The Division is concerned that if the rising water level in well E-1 is associated with mine inflow, <br />there is the potential that the sealed and backfilled E-seam portals may discharge to the surface <br />in the future. surtace discharge from the portals was not projected in the permit application, and <br />as such the permit did not inGude provisions for safely handling and treating (if necessary) mine <br />discharge. Likewise, the probable hydrologic consequences evaluation (PHC) did not address <br />the potential impacts of surtace discharge from the portals. The PHC was based on the <br />projection that postmining discharge would be to the glaciaUalluvial aquifer, and eventually to <br />Ward Creek via the alluvial aquifer. <br />The operator will need to provide information to demonstrate that ultimate water level in the <br />abandoned workings will not result in discharge from the portals. Installation of a well into the <br />workings may be required. If it cannot be verified that surtace discharge will not occur, the <br />following measures will need to be taken: <br />~~ <br />DEPARTMENT OF <br />NATURAL <br />RESOURCES <br />Roy Romer <br />Governor <br />lames 5. Lochhead <br />Ezecuiive Director <br />Michael B. Long <br />Division Dueaor <br />