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1 <br />' 1s most apparent during the low flow times of the year. This difference is small, <br /> approximately 300 to 400 mg/L. It is probably due to evapotransp~rative effects <br /> and impacts from naturally saline bedrock discharge to Fish Creek as it meanders <br /> through Twentymile Park. Since the underground mine is not presently impacting <br /> Fish Creek the data is presented for baseline purposes o nly. <br /> <br />b'~i'~ l ~`z ~ 4 CJ°~ <br />1 <br />1 <br /> <br /> <br /> <br />1 <br />~~~ <br /> <br />