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<br />I <br /> <br />\ <br />I <br />I <br />i <br />i <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />001742 <br /> <br />7 <br /> <br />Straightforward interpretation of the differences between <br />class I and class 2 could easily lead to the conclusion that <br />Coal Creek below Louisville is presently a class 2 warmwater <br />system because of the virtual absence of fish. In addition, <br />Coal Creek just above Louisville, although in somewhat better <br />condition with respect to fish than the lower part of Coal <br />Creek, would also appear to be a definite class 2 system. It <br />is even questionable whether the higher reaches of Coal Creek <br />around Highway 93 would qualify as a class 1 system because of <br />very low flow at certain times of the year. <br /> <br />It appears to me that Coal Creek consists of three <br />distinct segments. Segment I extends from the upper boundary <br />of the warmwater segment (exact biological boundary unknolO1l) <br />to a point 2-4 kilometers above Louisville, has a reasonably <br />good rocky bottom, shows indications of good water quality <br />(although no data are available), and has relatively abundant <br />warm\o/at er fish populat ions. Defic ienc ies of th is por t ion of <br />the stream include low seasonal flow due to water diversions <br />and almost complete lack of game fish. The second segment of <br />Coal Creek extends from 2-4 kilometers above Louisville to the <br />Louisville discharge point. This segment is characterized by <br />lower abundance of fish, very turbid water, unionized ammonia <br />levels exceeding the .06 mg/l proposed standard on at least <br />some occasions, and poor streambed quality. The third segment <br />of Coal Creek extends from the Louisville discharge down, <br />including two other point discharges. This third segment lS <br />characterized by virtual absence of fish, at least at the <br />present time, by unionized ammonia levels that exceed the .06 <br />proposed standard in the upper reaches but not in the lower <br />reaches, by very high turbidity, and by very poor stream bed <br />quality. <br /> <br />There is obviously a degradation in stream quality from <br />segments 1 through 3 moving from points well above <br />Louisville toward the confluence of Coal Creek with Boulder <br />Creek. The question of major importance to the City of <br />Louisville is what the City's role might be in contributing to <br />this degradation in quality. <br /> <br />\ <br />I <br />I <br /> <br />First, it is clear that substantial degradation is caused <br />by nonpoint sources, as the decline in quality from segment 1 <br />to segment 2 occurs above all of the point sources on Coal <br />Creek. Unionized ammoni.a above .06 rng/l accompanies the <br />degradation, both just above and just below Louisville, but <br />none of the observed unionized ammonia levels are in my opinion <br />high enough to el iminate the warmwater fish fauna. This is <br />especially true near the confluence of Coal Creek and Boulder <br />Creek, Where the unionized ammonia levels are much below .06 <br /> <br />\ <br />I <br /> <br />I <br />