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_ _ _ <br />,~ ~ • ~ III ~II~II~II~~II III <br />sss <br />STATE OF COLORADO <br />DIVISION OF MINERALS AND GEOLOGY <br />Department of Natural Resources <br />1313 Sherman 51., Room 215 <br />Denver, CO 80203 <br />Phone: 13031 866-3567 <br />FAX: (3031 832-8106 <br />January 13, 1993 <br />TO: Steve Wathen/~ <br />FM: Shawn Smith <br />Re: Preliminary Adequacy Review for HG Loadout Application <br />HG Peabody (C-92-081) <br />Dear Steve: <br />OF. ~~(O <br />~~., q <br />Nom. % ~ 0 <br />M <br />•~ +RSe~ ~ <br />~ X876 <br />Ruy Rumer <br />Governor <br />Michael 8. LnnF <br />Drvuion Direcio~ <br />I have reviewed the following sections of the permit application <br />from Peabody for PAR concerns per Larry's request dated 1/8/93. <br />2.04.5 - General Description of Geology and Hydrology <br />2.04.6 - Geology Description <br />2.04.7(1) - Ground Water Information <br />2.05.6(3) - Protection of the Hydrological Balance <br />2.06.8 - Alluvial Valley Floors demonstration and <br />investigation <br />In addition, I have reviewed both Volumes I and II of the permit <br />application with the pertinent sections, hydrological data <br />submitted for 1982-1984 for baseline studies on the alluvial wells <br />on the loadout site, and the Seneca II-W permit; Volume 11, Tab 16 <br />pg 13-20 for the Keammerer Ecological Consultants and Golder <br />Associates study on Dry Creek as a potential AVF. <br />All geological descriptions are complete, with stratigraphy and <br />structural analysis provided. <br />General surface and ground water hydrologic trends and parameters <br />have been provided. All ground water information has been found to <br />be accurate and complete with records of well chemistry data from <br />5/87 to 10/91 provided which compares to baseline data of 1982-84. <br />Since the background TDS and sulfate levels are so high, any impact <br />by the loadout will be masked. The two alluvial wells, HGDAL 1 and <br />2 (upstream and downstream respectively) were drilled in late 1981 <br />into the Lewis shale member. Evidently, from baseline data <br />gathered 1982-84, the Lewis shale is responsible for the extreme <br />salinity and high metal chemistry illustrated. TDS ranges in HGDAL <br />1 run from highs of 76,000 in fall to lows of 750 mg/1 with 37,000 <br />mg/1 the average. Well HGDAL 2 shows somewhat lower TDS levels, <br />with high of 67,000 and low of 330 with 30,000 the average. There <br />