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<br />The Quality of Streams and <br />Rivers is Affected by <br />Historical Mining Activities <br /> <br />Streams affected by mine drain- <br />age, from abandoned/inactive <br />mines, are present throughout <br />much of the Rocky Mountains of <br />Colorado. Metal mining in the <br />UCOL has been an important part <br />of the economy of Colorado since <br />the late 1800s. As a result, many <br />streams in the upper part of the <br />basin contain heavy metals and <br />other toxic elements that affect <br />stream-water quality. Knowledge <br />of mine-drainage effects on a body <br />of water is essential for assessing <br />water quality with regard to human <br />consumption, recreation, and <br />aquatic life. <br /> <br />Because of the potential expo- <br />sure of aquatic organisms to trace <br />elements in streambed sediment, <br />trace-element concentrations in <br />streambed sediment serve as an <br />indicator of potential toxicity to <br />aquatic life. Sampling trace ele- <br /> <br />ments in streambed sediment can <br />be used to identify stream reaches <br />affected by mining and can be <br />used to determine sources of trace <br />elements. The occurrence and <br />distribution of trace elements were <br />characterized by collecting <br />streambed-sediment samples at <br />29 sites in mining districts (fig. 6 <br />and table I) and at 8 background <br />(non-mining) sites in the Southern <br />Rocky Mountains. <br /> <br />Concentrations of cadmium, <br />copper, lead, and zinc in <br />streambed sediment were high at <br />some sites downstream from <br />mining areas (Deacon and Driver, <br />1999). Median concentrations of <br />cadmium (Cd) and zinc (Zn) in <br />samples from most mining districts <br />exceeded the Canadian Sediment <br />Quality Guidelines Probable Effect <br />Level (PEL), which is a sediment <br />guideline (fig. II). The PEL <br />defines the concentration level <br />above which adverse effects to <br />aquatic biota are predicted to occur <br /> <br />Table 1. Mining districts and sampling sites in the Southern Rocky Mountains <br /> <br />Mining district1 <br /> <br />River/Stream [site number(s) in <br />figure 6f <br /> <br />Hunter Creek (24) <br /> <br />Blue River. French Gulch, Swan River <br />(7,10, II, 12. 13, 14, 15, 16, 17) <br /> <br />Tenmile Creek (18) <br /> <br />Oh-Be-Joyful Creek, Coal Creek, <br />Slate, East Rivers (25, 26, 27, 28) <br /> <br />Cross Creek, Eagle River (22,23) <br /> <br />Lake Fork of the Gunnison River, <br />Hensen Creek (3 I, 32) <br /> <br />Peru Creek, Snake River (4, 5, 6) <br /> <br />Canyon Creek, Red Mountain Creek, <br />Uncompahgre River (33,34,35,36, <br />37) <br /> <br />South Fork of Williams Fork, <br />Williams Fork (2, 3) <br /> <br />IInformation from Davis and Streufert (1990). <br />2Background (non-mining) sites 1,8,9,19,20.21.29.30. <br /> <br />Aspen <br />Breckenridge <br /> <br />Climax <br /> <br />Crested Butte <br /> <br />Gilman <br /> <br />Lake City (Carson, Burrows, Sherman <br />Districts) <br /> <br />Montezuma <br /> <br />Ouray (Red Mountain, Sneffels, <br />Uncompahgre Districts) <br /> <br />Urad-Henderson <br /> <br /> <br />Mining land use in the Southern Rocky <br />Mountains. (Photograph by Jeffrey Deacon, <br />U,S. Geological Survey,) <br /> <br />frequently (Canadian Council of <br />Ministers of the Environment, <br />1999). National sediment concen- <br />tration guidelines have not been <br />established for the United States. <br />Concentrations of copper and lead <br />were also elevated and exceeded <br />the PEL in several mining districts. <br />The mining and mineralized areas <br />of the UCOL generally result in <br />higher trace-element concentra- <br />tions in streambed sediment than <br />are detected in other areas studied <br />within the NAWQA Program <br />(p. 12). <br />Collecting samples from sev- <br />eral types of media provides a <br />better understanding of trace ele- <br />ments in the environment. In <br />addition to streambed sediment, <br />which can store trace elements, the <br />overlying stream water can also <br />be a source of trace-element expo- <br />sure to aquatic organisms. Because <br />invertebrates are continuously <br />exposed to water-quality condi- <br />tions, these organisms integrate <br />effects of contaminants over time <br />and provide a measurement of <br />water quality. Invertebrate indica- <br />tors of streams contaminated by <br />trace elements include reduced <br />abundance and a shift in commu- <br /> <br />Major Findings 11 <br />