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<br />The world's largest molybdenum mine. located <br />at Climax, Colorado. just north of the head- <br />waters of the East Fork, produces 60 percent of <br />the total mined in the United States and 40 per- <br />cent of that mined in the western world. <br />Molybdenum is essential for plant growth, but at <br />times may accumulate in concentrations high <br />enough to be toxic to livestock (Chappell, 1975 <br />124)). Voegeli and King (1969) 11561 reported <br />that most surface waters in the mountainous <br />areas of Colorado contain less than <br />0.005 mg/L of molybdenum, but according to <br />Chappell (19751 1241 levels of 9 mg/L have <br />been detected in Ten-Mile Creek, which drains <br />the Climax mine. These high levels were found <br />during the spring runoff. <br /> <br />Cadmium <br /> <br />Cadmium is often found in nature as an impurity <br />in zinc-lead ores. There is no evidence that cad- <br />mium is an essential micronutrient and once it <br />enters the body it is likely to remain in animal <br />and human tissue (McKee and Wolf. 1963 <br />[1051 ). Cadmium is extremely toxic and often <br />acts synergistically with other elements (Hublou <br />et aI., 1954 [79] ). Clubb et al. (19751 [27] <br />measured cadmium uptake and elimination in <br />two stoneflies, Pteronarce/la badia and Pteronar- <br />cys california, exposed to subacute levels of <br />cadmium followed by return to cadmium-free <br />water. Uptake was curvilinear in both species <br />while elimination was rapid and linear. The latter <br />result suggests that these insects may be <br />capable of recovering from intermittently high <br />exposures to cadmium. <br /> <br />Cadmium is usually found in fresh waters of the <br />United States in concentrations of less than <br />1.0 /lg/L, but it was not found to be toxic to <br />embryos and larvae of freshwater fish in some <br />waters until levels of 4.0 /lg/L were reached <br />(Eaton et aI., 1978143] I. McKim et al. (19751 <br />[107] found cadmium to be acutely toxic to <br />rainbow trout at 7.0 /lg/L. Mount and Stephan <br />(19671 [115] have shown that fish liver ac. <br />cumulated high concentrations of cadmium <br />during chronic exposure, but accumulated very <br />little following acute exposure; it was suggested <br />that fish liver concentrations exceeding 300 /lg <br />Cd/g dry weight indicate a previous history of <br />chronically damaging cadmium exposure. <br /> <br />Davies and Goettl (19761 [341 suggest that <br />levels of cadmium not exceed 0.4 /lg/L in waters <br /> <br />of less than 100 mg/L hardness (as CaCa,). <br />and not exceed 1.0 /lg/L in waters of less than <br />200 mg/L hardness. The Environmental Protec- <br />tion Agency (19801 [52] recommends that <br />average concentrations of cadmium over a <br />24-hour period should not exceed 0.012, <br />0.025. and 0.051 /lg/L in waters at hardnesses <br />of 50, 100, and 200 mg/L (as CaCa,). respec- <br />tive/y. <br /> <br />METHODS AND MATERIALS <br /> <br />Description of the Area <br /> <br />The study area lies east of the north-south trend- <br />ing Sawatch Range, whose crest forms the Con- <br />tinental Divide. Colorado's highest peak, MI.. <br />Elbert, with an elevation of 4398 m above m.s.1. <br />(mean sea level), is located in this range. The <br />Mosquito Range lies immediately to the east and <br />is generally parallel to the Sawatch Range. The <br />area is characterized as a high mountain basin <br />with a natural dendritic drainage pattern opened <br />to the south. <br /> <br />The Arkansas River in the study area flows in a <br />broad valley which has been subjected to re- <br />peated glaciation. Main uses of the valley today <br />are mining on the upper slopes and grazing in the <br />bottom lands. Some of the Arkansas River tribu- <br />taries originate from small alpine lakes while <br />others, like the river itself, begin on mountain <br />slopes. Flow is characterized by high late-spring <br />and early-summer flows which recede to more <br />stabilized flows for the remainder of the year, al- <br />though diversions from the western slope aug- <br />ment the river's flow considerably below Tur- <br />quoise and Twin Lakes. Many of the natural <br />gulches dry up during the summer and fall, <br />although some are known to carry seepage to <br />creek channels and thus to the Arkansas River <br />(LaBounty et al.. 19751941 ). <br /> <br />The 1979 stream and lake evaluation map of the <br />State of Colorado classifies river drainages <br />according to the existing fishery resources. The <br />upper Arkansas River is given a I rating. which <br />designates it a highest-valued fishery resource. <br />Lake Fork and Halfmoon Creek are given a II <br />rating which designate them high-priority fishery <br />resources. The remaining tributaries to the upper <br />Arkansas River are less important for fish pro- <br />duction. <br /> <br />14 <br />