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• III Illlllllllllllll <br /> 5TATE OF COLOMDO <br /> DIVISION OF MINERALS AND GEOLOGY <br /> Department of Natural Resources <br /> 1313 Sherman St.,Room 215 <br /> Denver,Colorado 80203 D I V I S I O N O F <br /> Phone:(303)866-3567 M I N E R A L S <br /> FAX:(303)832-8106 & <br /> GEOLOGY <br /> RECLAMATION <br /> MINING-SAFETY <br /> Date: June 11, 1999 <br /> Bill Owens <br /> Governor <br /> To: Wally H. Erickson Greg E.Watcher <br /> Executive Director <br /> From: Harry H. Posey Michael Long <br /> Division Director <br /> Subject: Monitoring parameter changes; Howardsville Mill; M-84-049. <br /> This letter reviews your April 12, 1999 letter from Jerry Sandell, Court Appointed Receiver for <br /> Tusco, Inc., Howardsville Mill, and recalls our conversation regarding same. <br /> Mr. Sandell proposes to reduce ground and surface water monitoring parameters at <br /> Howardsville. With some exceptions, I concur with his recommended parameters list. The <br /> attached table compares the analytical parameters already measured to those proposed by Tusco <br /> and bears a list of recommended parameters. If the recommended list seem inadequate in your <br /> view, please discuss with me further. <br /> The table of ground and surface water analyses which you prepared reveals some interesting <br /> points about the hydrologic system at Howardsville. Several wide geochemical variations cannot <br /> be ascribed to seasonal fluctuations alone. Rather, they seem to reflect a mix of physical and <br /> chemical conditions including changes in site conditions that took place during sampling. <br /> Changing site conditions and consequent fluctuations in groundwater composition are related <br /> most probably to (a) disturbances in groundwater chemistry through excavation of pre-law <br /> tailings by Sunnyside Gold Corporation; (b) inhomogeneous contact between groundwater, <br /> waste rock and tailings of different compositions along discrete flow paths; (c) surface water <br /> discharges from the Sunnyside disturbance; and (d) chemical changes, including manganese <br /> mobilization, caused by interaction with low Eh, neutral pH, low carbonate waters in the <br /> wetlands. All combined, the significant variations in local geochemistry and groundwater flow <br /> make it impossible to define the background conditions with any reliability. Thus, it will be <br /> challenging, if not impossible, to define background conditions. <br /> Short of having the operator start over with the monitoring program, I believe DMG is obligated <br /> to make the best of the highly variable system. To that end, I would agree with your <br /> recommendation that the operator monitor for a short list of parameters for three more periods. <br /> The Operator's proposed twice-yearly sampling should be adequate. Once the background <br /> situation is better defined, the short list of parameters may be shortened even further to monitor <br /> only for evidence of contamination related to future operations. <br />