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<br />Proposed Decision and Findings of Compliance July 2018 <br />Permit Renewal No. 7 P a g e | 55 <br />Lower Taylor Creek, a tributary to Wilson Creek, contains small areas with alluvial deposits, but <br />does not contain enough water to provide for sub-irrigation of croplands. Taylor Creek, which <br />will be mined in its upper reaches, is therefore not considered an alluvial valley floor. <br /> <br />The West Fork of Good Spring Creek was investigated in association with PR-02, and was <br />determined not to be an alluvial valley floor due to the restricted width of the alluvial deposit along <br />most of the reach, and the absence of sub-irrigated or flood irrigated agricultural activity (current <br />or historic). <br /> <br />Other Stream Valleys in the General Area <br /> <br />Various other stream valleys with unconsolidated alluvial deposits in the mine vicinity may meet <br />alluvial valley floor criteria, but have not been evaluated as a part of this review because th ey are <br />located outside the proposed permit boundary or there is no proposed mine disturbance within their <br />watersheds. These valleys include the East and West Forks of Wilson Creek, which are located <br />upstream of any proposed mining, the East Fork of Good Spring Creek, located upstream of any <br />proposed mining, and James Creek, located upstream of any proposed mining. <br />B. Primary Impacts <br /> <br />None of the four designated alluvial valley floors are within the area to be mined; therefore, mining <br />operations will not cause direct disturbance to any alluvial valley floors. Any mining impact that <br />might occur will be indirect in nature. <br />C. Secondary Impacts <br /> <br />It that the areas to be mined presently contribute relatively little water to alluvial valley floors. <br />Any degraded water that might reach an alluvial valley floor would be diluted by other sources. <br />In addition, alluvial valley floors are protected by both stream buffer zones and treatment of runoff <br />from disturbed areas by sediment ponds. <br /> <br />The Gossard Loadout is located near the confluence of Wilson and Taylor Creeks and the alluvial <br />valley floor associated with Wilson Creek. There is a slight potential for waters of degraded <br />quality to reach alluvial materials near the loadout. An alluvial well located near the loadout is <br />monitoring this situation. Runoff from the surrounding areas above the loadout are diverted around <br />the disturbance and waters from the disturbance itself are treated in sediment ponds and must meet <br />CDPS standards before being released. <br /> <br />Waters leaching salts from reclaimed spoils may eventually reach Taylor, Wilson and Good Spring <br />Creeks. It is believed that these spoil waters will still meet CDPS standards and will not contribute <br />salts in levels that would warrant changes in mining and reclamation plans. This situation will be <br />monitored through alluvial wells located on Wilson Creek (near the Gossard Loadout) and on <br />Good Spring Creek and West Fork Good Spring Creek, both above and below mining disturbances. <br />