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1 <br />' those observed in 1986. This increase probably has occurred from the advancement of the front <br />of high dissolved solids water in the Wadge Overburden aquifer as indicated by the 1986 and <br />' 1988 Inflow Studies. The plot of field conductivity for the Fish Creek Borehole discharge and <br />Fish Creek is presented on Figure 45. No impact on Fish Creek from the discharge is indicated. <br />The discharged water is a mixed cation -sulphate water type. Most metal concentrations are <br />' low. Only iron at Station 109 was relatively high in 1987 to 1990. <br /> <br /> <br /> <br />-11- <br />