Laserfiche WebLink
drained by two perennial streams: Goodspring Creek on the east, North Fork of Goodspring Creek on <br />the South, and Wilson Creek on the west. Taylor Creek, an intermittent stream located just inside and <br />generally parallel to the west boundary of the permit area, and generally pazallel to Wilson Creek, <br />flows into Wilson Creek north of the rail loadout. Several ephemeral drainages occur on the permit <br />area, including the Streeter Drainage. This drainage profile was raised as a result of excess spoil fill <br />in the Streeter Canyon, the deepest fill (the Streeter Fill) neaz the confluence of Streeter Drainage and <br />Goodspring Creek. These drainages are tributazies to Milk Creek, which flows into the Yampa River <br />about seven miles north of the permit area. Precipitation averages 18 inches annually on the property <br />and runoff is limited. Flows in the drainages aze mainly in response to snow melt or intense <br />thunderstorm events. <br />Water sampled from the drainages is quite hard, dominated by calcium and magnesium cations and <br />bicazbonate and sulfate anions. The relatively high alkalinity and pH of the system impedes the <br />solubility and transport of heavy cations, thus minimizing potential toxicity problems associated with <br />heavy metals or acid drainage. <br />Springs and seeps aze abundant in the area, with 59 originally identified during an inventory <br />completed in 1985. More recent inventory and study resulted in additional springs and seeps in the <br />South Taylor and Lower Wilson areas. Four springs were found to be perennial, two tributary to <br />Wilson Creek and two tributary to Good Spring Creek. The locations of all monitored springs and <br />seeps are shown on Map 10A, Volume 14. Spring and seep information is included in Tables <br />2.05.6-1 and 2 in Volume 12 for the South Taylor and Lower Wilson areas. <br />No alluvial valley floors (AVF's) exist within the area to be mined. However, the alluvial deposits of <br />Goodspring Creek, Wilson Creek, and lower Elkhorn Creek meet the geomorphic and irrigation <br />criteria of an AVF and aze discussed in Section B, Item XVII of this document. <br />The Wilson Reservoir, from which water is drawn for mining activities, is an important fishery of the <br />azea. The Wilson Reservoir was built in 1941, and is under the regulatory jurisdiction of the <br />Colorado Division of Water Resources. Except for a pumping station, the Wilson Reservoir is not <br />within the Permit area, and is not a part of the Permit. The pumping station at the reservoir, and the <br />pipeline from the pumping station to the main areas of the Mine, aze included in the Permit. <br />3.2.10 Vegetation <br />Baseline vegetation information is found in Section 2.04.10 Map 4 and Exhibit 10 of the PAP <br />original volumes. Vegetation information associated with the PR-2 Lower Wilson and South Taylor <br />expansion areas can be found in Section 2.04.10 of Volume 12, Exhibit 10 of Volume 13, and Maps <br />3, 4A, and 4B of Volume 14. Six vegetation communities and a small amount of cropland exist <br />within the Mine permit boundary. The major communities are sagebrush and mountain shrub. <br />Communities of lesser extent include a juniper community in the vicinity of Streeter Mountain, <br />aspen groves in the upper reaches of Streeter, Taylor and Wilson Creeks, a limited riparian <br />community along Goodspring, West Fork Goodspring, Wilson, and Taylor Creeks, and a small <br />Proposed Decision and Findings of Compliance 4 May 2007 <br />Permi[ Revision 02 Page 20 <br />