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' wells are plotted on Figure 20. The dissolved solids average 2200 to 3000 <br /> mg/1 and range in value from 1950 to 4725 mg/1. The water is a <br /> calcium-sulfate type with high bicarbonate and low SAR. The water is higher <br /> <br /> in dissolved solids than the background bedrock levels but lower than most <br />' of the spoil spring discharges. The data does not indicate any significant <br /> changes in the trace metals concentrations. They all have relatively high <br />' manganese levels. <br />1 <br /> <br /> <br />1 <br />1 <br /> <br /> <br />1 <br />1 <br /> <br /> <br />1 <br /> <br />1 <br /> - 5 - <br /> <br />