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RULE 2 PERMITS <br />area, and thus Taylor Creek is examined as a separate drainage in this presentation. The principal <br />drainages within the permit revision area described below. <br />Good Spring Creek --The Good Spring Creek watershed encompasses an area of about 35 square miles. <br />The drainage is characterized by steep sloping upland areas and narrow flat valley bottoms. Slopes <br />approaching or exceeding 50 percent are common, primarily due to the preponderance of exposed <br />bedrock strata (CDM, 1985b). Incision has created deep gullies in reaches locally within the permit <br />revision area, and bank sloughing is contributing to channel widening. Other, more stable reaches are <br />armored along the channel bottom by cobbles or exposed bedrock. Good Spring Creek has a higher <br />baseflow than other area creeks in part due to flow contributions from perennial springs in the West Fork <br />of Good Spring Creek. <br />Wilson Creek - The Wilson Creek watershed encompasses an area of about 20 square miles. Similar to <br />Good Spring Creek, the Wilson Creek drainage is characterized by narrow upland areas, steeply sloping <br />hillsides, and flat valley bottoms. The tributary channels are incised into bedrock. The valley bottom <br />exhibits morphologic evidence of historic landslide debris accumulation, which serves as a transporting <br />media for bedrock groundwater discharge and side valley runoff to recharge surface water flows (CDM, <br />1985b). This recharge mechanism is illustrated by seeps along the banks of the stream. <br />Taylor Creek — The Taylor Creek watershed encompasses an area of about 7.22 square miles. Slopes are <br />variable, ranging from 20 to 25 percent in the broad upland area in the highest portion of the watershed, <br />and generally steeper throughout the remainder of the basin leading to the valley bottom. Bedrock <br />stability in the area inhibits the accumulation of mass -wasting debris (CDM, 1985b). The channel is <br />relatively steep, typically greater than ten percent, and incision and bank sloughing are limited due to the <br />bedrock control. <br />Surface Water Quantity — The South Taylor/Lower Wilson permit revision area extends from <br />Colowyo's existing mining operations in the Good Spring Creek watershed into the Wilson Creek, Taylor <br />Creek, and Jubb Creek watersheds. Baseline monitoring was conducted from September 1996 through <br />September 1997 in each of these drainages. Additional baseline monitoring was conducted in March <br />1999 through August 2000 in Good Spring Creek. The Colorado Mined Land Reclamation Division's <br />Guidelines for the Collection of Baseline Water Quality Data were utilized during the baseline <br />monitoring. Water quality sampling and laboratory analyses were conducted in accordance with Rule <br />2.03.3(4) for analytes defined in Rule 2.04.7(2) and for analytes also listed in the Division'sGuidelines for <br />the Collection of Baseline Water Quality and Overburden Geochemistry. Field measurements for pH, <br />electrical conductivity, temperature, dissolved oxygen, and flow were monitored monthly. Quarterly <br />monitoring included a full suite of analyses at each location. Analysis for metals included only total <br />recoverable concentrations. <br />Baseline surface water monitoring data are presented in Table 2.04.7-34 and Table 2.04.7-35. <br />Streamflow hydrographs for representative surface water monitoring locations in these drainages are <br />presented in figures 2.04.7-22 to 2.04.7-28. Surface water quality as measured by specific conductance is <br />also illustrated to show seasonal variability with respect to stream flows. <br />Good Spring Creek — Flow measurements obtained from surface water monitoring locations in Good <br />Spring Creek in 1996/97 ranged from 0.85 cfs at New Upper Good Spring Creek (NUGSC) to 17.0 cfs at <br />Lower Good Spring Creek (LGSC). Flows increased in the late spring and early summer months, <br />corresponding to periods of high snowmelt and surface runoff. Flows measured in 1999/2000 ranged <br />from 0.2 to 13.0 cfs at EFGSC, 0.26 to 7.0 cfs at Lower West Fork Good Springs Creek (LWFGSC), and <br />0.18 to 6.5 cfs at Upper West Fork Good Springs Creek (UWFGSC), respectively. Flows also increased <br />in the late spring and early summer months. <br />South Taylor/Lower Wilson — Rule 2, Page 27 Revision Date: 4/7/17 <br />Revision No.: RN -07 <br />