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<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 />I <br />I <br />I <br />I <br />I <br /> <br />Water Resources. At this location the bankfull discharges of the Alamosa River is 656 <br />cfs with bankfull dimensions of 49 feet in width, 2.9 feet in depth, a cross sectional area <br />of 140 square feet and mean velocity of 4.5 fUsee. There is also a gaging station 1 mile <br />above Terrace Reservoir (Gage number 08236000). CDPHE has several temporary <br />gaging stations to support the Summitville Mine Superfund Project. Figures 4 and 5 <br />provide hydrographs for the Alamosa River above and below Terrace Reservoir (25). <br />Attachment 4 provides hydrographs for these two gaging stations for water years 1998, <br />1999 and 2000. <br /> <br />4.2 Groundwater <br /> <br />Basic Groundwater Quality Standards for the State of Colorado (Regulation 41) are <br />applicable to the groundwater conditions in the Alamosa River Watershed. The <br />groundwater use classifications in the state are as follows: <br /> <br />. Domestic Use <br />. Agricultural <br />· Surface Water Quality Protection <br />. Potentially Usable Quality <br />. Limited Use <br /> <br />The groundwater in the Alamosa River Watershed is of sufficient quality to support all of <br />the groundwater classifications listed above. No site-specific exemptions exist in the <br />watershed. Specific numeric and narrative standards for groundwater are provided in <br />Attachment 5 (26). <br /> <br />There are no known routine groundwater monitoring programs in the Alamosa River <br />Watershed. There are no public water supplies that come from groundwater sources <br />that would require routine monitoring and reporting to CDPHE. The watershed is <br />dominated by individual, private wells for domestic drinking and for agriculture. <br /> <br />The most extensive groundwater monitoring program performed in the Alamosa River <br />Watershed was part of the Summitville Mine Superfund Project by EPA and CDPHE. In <br />1993, a comprehensive study was performed by Ecology and Environment, Inc. for the <br />EPA to determine baseline conditions and if contamination from the mine had occurred <br />in the aquifer. Twenty-one domestic wells were sampled, three upstream and 18 <br />downstream of Terrace Reservoir. The results of the 1993 groundwater sampling <br />showed that some wells contained metals sueh as copper, zinc and occasionally <br />arsenic; none of these concentrations exceeded the Maximum Concentration Level <br />(MCL) or secondary MCLs for drinking water established by EPA (27). <br /> <br />Similar metal concentrations in groundwater were found in 1998 after 24 wells in the <br />Alamosa River Watershed were sampled and tested. No drinking water MCLs were <br />exceeded in this study, but it was noted that two wells exceeded standards for iron and <br />manganese (secondary MCLs). High concentrations of iron and manganese cause <br />visual staining on clothes or fixtures and are not generally associated with human <br />toxicity. CDPHE initiated a groundwater monitoring study of 21 wells in June 1999. <br />Copper, an indicator of acid mine drainage, was not detected above MCLs in any <br /> <br />4-2 <br />