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• located further downstream on Foidel above the confluence with Middle Creek. Former site 304 was located <br />further downstream of 900. Site 304 was eliminated in 2003 per TR03-42. <br />Tables 33 through 36 provide summaries of the 2009 Water Year data collected at each site. Tables 33a, 34a, and <br />35a provide POR statistical summaries of collected data at each site. Figures 52 to 59 and 102 to 105 provide <br />graphical representations of water levels and selected water quality parameters recorded at each site. Typical <br />flow patterns were exhibited at these sites with spring runoff periods accounting for the peak flows observed. At <br />all of these sites, the inverse relationship between flow and field conductivity continues to be evident. Water <br />quality parameters for these sites were within previously established ranges. <br />Fish Creek: Nine surface flow monitoring sites are utilized on Fish Creek. Site 16A replaced site 16 in 2000, <br />and is located upstream of the Fish Creek Borehole discharge site 115. Historical data for site 16 may be found in <br />previous AHRs. Site 307 is located approximately one mile downstream of the Fish Creek Borehole mine <br />dewatering site and is monitored in conjunction with alluvial well 006-AZ-3. Site 302 is located approximately <br />two miles downstream of the Fish Creek Borehole mine dewatering site. Site 305 is located upstream of the Fish <br />Creek Tipple and is monitored in conjunction with alluvial well 008-AU-3. Site 27A is located immediately <br />upstream of the Fish Creek Tipple discharge (a.k.a. CDPS discharge site 62). Site 1003 is located downstream of <br />the Fish Creek Tipple site 62. <br />Monitoring requirements at sites 307 and 305 require monthly water level measurements (March through <br />• September), and semi-annual field parameters. However, per PR03-06, site 305 now requires semi-annual water <br />quality testing. <br />Three relatively new surface sites were added in conjunction with the new Fish Creek Alluvium well sites (AVF- <br />13, AVF-14, and AVF-15), in order to evaluate potential subsidence impacts in the area. These are surface sites <br />SW-13, SW-14 (both added in August 2001), and SW-15 (added in June 2002). These sites require quarterly <br />water level measurements (March through September), and semi-annual field parameters and water quality <br />sampling. <br />Tables 37 through 45 provide summaries of the 2009 Water Year data collected at Fish Creek surface flow sites. <br />Tables 37a through 45a provide some historical summaries of collected data at each site for comparison. Figures <br />60 through 91 provide graphical representations of water levels and selected water quality parameters recorded at <br />each site. Again, typical flow patterns were exhibited at these sites with spring runoff periods accounting for the <br />peak flows observed. In general, an inverse relationship between flow and field conductivity was evident. 2006 <br />water quality parameters for these sites were generally within previously established ranges. <br />New surface sites SW-13, SW-14, and SW-15 (Tables 43-45, Figures 66-77) indicated elevated concentrations <br />for total recoverable (TR) iron in early June 2003, however iron concentrations dropped dramatically (about an <br />order of magnitude) by August 2003. With the exception of TR iron, none of the values recorded during the <br />• initial sampling episode fell outside the typical historical range of other surface sites on Fish Creek. In 2009 iron <br />values ranged between 340 ug/L to a high of 27400 ug/L. This is typical for historical seasonal fluctuations, with <br />11