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<br />• <br />Hydrologic Monitoring A[tivitiu <br />1990 water year for these sites are presented in <br />Appendix B and Appendix C, respectively. <br />Seasonal (three times per year) water samples were <br />taken at all surface water monitoring stations <br />except the USGS North Fork station. Measured <br />parameters included pH, conductivity, temperature, <br />total dissolved solids, total suspended solids, total <br />iron, and total manganese. Sampling results are <br />summarized in Appendix D. Minimum and maxi- <br />mum information for the baseline monitoring <br />period is compared with water year 1990 data for <br />the Sylvester Gulch and North Fork Upper sta- <br />tions in Appendix E. <br />Spring Water Monitoring <br />Seven springs were monitored during the 1990 <br />water year (Table 2). Their locations are shown on <br />Exhibit I. All known springs in the lease area are <br />shown on Exhibit 2.8.1.B. in Volume 3 oC the M <br />and R Plan. <br />In accordance with U.S. Forest Service (USES) <br />stipulations, a map of USES water resources has <br />been included as Exhibit II1. Table 3 summarizes <br />the resources. Some of the USES water resources <br />are springs. No changes in the USES Water Re- <br />sources Map are necessary for 1990 because no <br />new rights were filed for or new uses made in f990 <br />in the Icase area. <br />Seasonal measurements (three times per year) of <br />pH, conductivity, temperature, total dissolved <br />solids, total suspended solids, total iron, and total <br />manganese were taken at each of the seven springs. <br />Measured (lows, field parameters, and the results <br />o[ laboratory analyses are presented in <br />Appendix F. Maximum and minimum comparisons <br />are presented in Appendix E. Bar graphs depicting <br />spring }lows Crom 1979 to the present have been <br />included as Appendix G. <br />Of the seven springs, only springs G-14, G-16, and <br />G-20, were sampled during 1990. Flows at the <br />other four springs were either nonexistent or <br />insufficient for sampling during all three sampling <br />periods. Consequently, water quality data are <br />available only for springs G-14, G-16, and G-20. <br />Groundwater Monitoring <br />Twenty-three wells were monitored during the <br />1990 water year (Table 4). Their locations are <br />shown nn Exhibit 1. Sampling frequency for water <br />levels and wafer quality was 3 times per year. <br />Monitored parameters included water Icvel, pH, <br />conductivity, temperature, total dissolved solids, <br />'fable 2 Summary of the Spring Monitoring Program at the Mt. Gunnison No. 1 Mine <br /> <br />Location Frequency of Discharge <br />Measurement <br />fir,, y< Frequency of Water Quality <br />Measurement <br />Springs Above the " F' Seam in the North Fork Drainage Basin <br />G-12 3 times per year r 3 times per year <br />G-14 3 times per year F 3 times per year <br />G-16 3 times per year F 3 times per year <br />G-22 3 tinter per year F 3 times per year <br />G-24 3 times per year ~ 3 times per year <br />Springs in or Below the "F' Seam in the North Fork Drainage Basin <br />G-la 3 times per year <br />G-20 3 times per year <br />3 times per year <br />3 times per year <br /> <br />