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<br />I <br />I, <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br />I, <br />I <br />l <br />[ <br />I <br />t, <br />I <br />\, <br />~ <br /> <br />r=1794 <br /> <br />3. Historic Impacts: Mining, Flow Augmentations, and Project <br />Reach Land Use <br /> <br />3.1. Mining Impacts <br /> <br />The Leadville mining district has produced in excess of $800 million in silver, lead, zinc, <br />gold, and copper since the mid 1800's (Collins and Collins, 1986), Smelting operations <br />have also utilized significant quantities of manganese, bismuth, and iron, Mining in the <br />area commenced around 1860 on California Gulch when placer gold was discovered, By <br />1875, the gold mining had essentially ceased, in part due to the difficulty of processing a <br />heavy gray mineral that was present in high concentrations in the placer deposits, This <br />material was identified as cerussite (lead carbonate) in 1876, which is a common lead ore <br />that forms upon the interaction of carbonated waters with galena (lead sulfide; Hurlbut <br />and Klein, 1977), The cerussite ore also contained large amounts of silver. The lead- <br />silver ore was mined extensively until about 1902, From about 1903 to after WWI, large <br />quantities of zinc carbonate ore were mined in the Leadville district. Since about 1923, <br />base metal complex sulfide ores have constituted the primary mining activity in the <br />region, Between 1859 and 1966, approximately 24 million tons of ore were produced in <br />the Leadville district (Studzinski, 1996), Some local mines have actively produced gold <br />ore in recent years (Collins and Collins, 1986), <br /> <br />Mining waste generated in the Leadville region over the past 150 years has been directly <br />disposed of on the Arkansas River floodplain, and has been transported down the <br />Arkansas River project reach via upstream tributaries including California Gulch (BOR, <br />1999), These tailings are located along the channel margin and floodplain within the <br />project reach, and consequently constitute a potential source of contaminants for the <br />active channel (URS, 1977), As the channel course has shifted laterally through time, <br />many tailing deposits are located away from the main channel in relict channel features <br />and on the adjacent floodplain or low terrace surfaces, Additional concern has been <br />expressed that mine tailings have been transported though irrigation ditches and <br />deposited in broad fields in the valley bottom, Within the project reach, some of the <br />tailings have been identified as phytotoxic, such that vegetative reinforcement of channel <br />banks and floodplain surface is locally limited (URS, 1997), <br /> <br />The delineation and geochemical analyses of tailings within the project reach is ongoing, <br />To date, approximately 90,000 cubic yards of tailings have been mapped and <br />geochemically evaluated along the project reach CURS 1997; 1998), Treatment strategies <br />for the tailings were undergoing feasibility evaluations at the time of this investigation, <br /> <br />Sediment control measures have been implemented on California Gulch to reduce the <br />quantity of tailings delivered to the project reach, Whereas historic sediment loading out <br />of California Gulch likely consisted of substantial quantities of sand and finer grained <br />material, sediment control measures will reduce both the size and volume of sediment <br />introduced in the future, <br /> <br />May 7, 1999 <br /> <br />Fluvial Geomorphological Assessment <br />Upper Arkansas River <br /> <br />Page 8 <br />