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Date G-26a G-26b CR-12 <br />06/19/95 pH - 6.9 No Flow pH - 6.7 <br /> Temp - 8.9 Temp - 9.4 <br /> Cond - 764 Cond - 1044 <br /> gpm - 13.64 gpm - 60 <br />07/21/95 pH - 7.6 No Flow pH - B.1 <br /> Temp - 10.2 Temp - 12.0 <br /> Cond - 720 Cond - 1220 <br /> gpm - 8.20 gpm - 12 <br />08/13/95 pH - 8.2 No Flow pH - 8.5 <br /> Temp - 14.5 Temp - 20.3 <br /> Cond - 699 Cond - 1265 <br /> gpm - 3.75 gpm - 9 <br />09/03/95 pH - 8.0 No Flow pH - 8.4 <br /> Temp - 13.2 Temp - 15.6 <br /> Cond - 1192 Cond - 209 <br /> gpm - 3 gpm - 10 <br />10/11/95 pH - 8.1 No Flow pH - 8.7 <br /> Temp - 9.2 Temp - 9.4 <br /> Cond - 940 Cond - 1120 <br /> gPm - 3 4Pm - 5 <br />11/07/95 pH - 8.2 No Flow pH - 8.8 <br /> Temp - 7.4 Temp - 8.8 <br /> Cond - 1000 Cond - 980 <br /> gpm - 2.63 qpm - 0.94 <br />Spring G-26a and CR-12 had significant flow during the year. <br />An unusually wet spring contributed to the high flows. Sprinq G- <br />26b was dry all year. There is not enough data on these springs to <br />draw any conclusions regarding mining impact. <br />6 <br />