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r <br /> III IIIIIIIIIIIIIIII <br />STATE OF COLORADO <br />DIVISION OF MINERALS AND GEOLOGY <br />Drpanmem of Natural Resources <br />I 1 L{ Sherman 51 , RUIIDI 215 ~, <br />+tlk <br /> <br />Denver, (~ulnoulo 01103 I <br />~ <br />` <br />Phunc' (f U { I Hfi L- { S o, III <br />FA%: I ill 4111 L'~If I UU <br /> DEPARTMENT OF <br /> NATURAL <br />DATE: October 16, 1996 RESOURCES <br />TO: Erica Crosby Roy Romer <br /> Governor <br /> <br />FROM: Susan Burgmaier lames 5. LochheaA <br />Execmive DveOO~ <br /> <br />RE: Seneca II-W Mine (C-82-057) Michael 0. long <br />Division Dnerlo~ <br />1995 Annual Hydrology Report <br />I have completed a review of the 1995 AHR for the Seneca 11-W Mine. I reviewed water <br />quantity and quality data, but not sampling frequency compliance since you already did that part. <br />Following are my comments on the report. <br />1. The approved permit application package, in Tab 17 (Probable Hydrologic <br />Consequences), predicts there will be little or no impact on surface water quantity. An <br />increase in Total Dissolved Solids (TDS) is expected on Dry Creek (114%) and Sage <br />Creek (7%). Ground water 9uality is expected to undergo a 7-9% increase in TDS, and <br />a slight drawdown, which will be Ilmited to the area within the permit boundary, is <br />expected. <br />2. Ground water levels exhibited typical seasonal fluctuations. Water levels were higher <br />than normal in the Spring, due to the unusually wet weather in the mine area. <br />3. TDS is increasing in the Hubberson Gulch alluvium. Hubberson Gulch is tributary to <br />Dry Creek. The downstream surface water monitoring site on Dry Creek indicates the <br />increases in surface water TDS, to date, are still below the predicted increase. Increases <br />in surface water TDS were lessened by the higher than normal precipitation during the <br />year. <br />4. Hydrographs for Hubberson Gulch, Dry Creek, and Sage Creek show seasonal <br />fluctuations consistent with baseline data. Data from the Spring shows higher flows than <br />normal, again due to higher precipitation in the early part of the year. <br />4. TDS is increasing in the Sage Creek alluvium, but there have not yet been discharges to <br />Sage Creek, since Pond 009 has not discharged. The increase, then, is not likely mine <br />related. <br />5. Tables 3 and 10 of the AHR should be revised in future reports to note the date <br />monitoring was discontinued at any given site. [f a casing faded, a well was mined <br />through, beavers dammed the flow, etc., the date of that occurrence should be noted. A <br />considerable amount of time is spent each year trying to figure out when a monitoring <br />site was dropped. <br />6. Monitoring was discontinued at well GW-S2W-7A1 when the casing was destroyed. Will <br />Seneca Coal Company be replacing this well? <br />7. It would be helpful if, in future reports, Seneca Coal Company would include tables of <br />cumulative data for certain parameters at certain sites. Tables of all data to date for <br />