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III IIIIIIIIIIIII III <br />999 <br />STATE OF COLORt~DO <br />DIVISION OE MINERALS AND GEOLOGY <br />DepanmeN of Natural Resources <br />1713 Sherman St., Room 215 Ilye <br />Denver, Colorario 80203 Ily <br />Phune: (3031 866-3567 <br />FAX. (301) 832-8106 <br />DEPARTNIEfYT OF <br />NATURAL <br />RESOURCES <br /> Roy Romer <br /> Governor <br />January 5, ] 998 lames 5. Lochhead <br /> ErecW rvc DirPCbr <br />Mr. Michael G. Altavilla "'i`h'e~ a. `°°F <br />Division Direclw <br />Seneca Coal Company <br />P.O. Drawer D <br />Hayden, CO 81639 <br />RE: Seneca II-W Mine (C-82-057) <br />1996 Annual Hydrology Report & Annual Reclamation Report <br />The Division of Minerals and Geology received the 1996 Annual Hydrology Report (AHR) and <br />Annual Reclamation Report (ARR) for the Seneca II-W Mine on March 3, 1997 and April 4, <br />1997, respectively. <br />The ARR was submitted and is in compliance with Rule 2.04.13. The Division has no comments <br />that need to be addressed by the operator. <br />The AHR was found to be ahigh-quality document, containing the necessary information for <br />analysis. The AHR could be improved by two means. First, Seneca could relate the results to <br />the PHC section of the permit and second, Seneca could use the same scale on the plots where <br />possible. Some are way out of the range of others, but for our purposes, vaziation in TDS content <br />of 100 mg/I at a given sampling location is not significant compared to variations of 2 or 3 orders <br />of magnitude, the range over which we are observing changes at some locations. <br />The Division has a few comments regarding the conformance of the hydrologic system to the <br />predictions in the PHC; <br />Surface Water <br />The quality of the water in the Hubberson Gulch "system" and the Dry Creek "system" have not <br />reached the high dissolved salts levels predicted in the permit. At Hubberson Gulch, the water <br />downstream of NPDES point 006 has increased about 250 mg/1, but has reached a maximum on <br />one occasion of only 1700 mg/I, much less than the predicted post-mining concentration of 2200 <br />mg/l. Most measurements indicate levels about 830 mg/I. At Dry Creek, the NPDES discharge <br />point has seen water increase from 1100 mgJl to nearly 1500 mgll, but at the monitoring site <br />downstream of the confluence of that tributary with Dry Creek, the measurements have fallen <br />within the historic range, 1000 mg/I less than predicted. <br />