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1. The proposed mining operations would not interrupt, discontinue, or <br />preclude farming on the alluvial valley floor. The surface facilities <br />associated with the mine are located outside of the area designated as <br />ailuvtal valley floor. The proposed operation would undermine portions <br />of the area designated as alluvial valley floor but this is not expected <br />to affect farming activities. The applicant has proposed limited mining <br />(the extraction ratio wail be between 50 and 55 percent), and, <br />therefore, no significant surface effects from subsidence are expected. <br />In addition, the applicant has proposed a subsidence monitoring plan <br />tSection 2.05.6(6)(f)(1i)(c) of the permit application) to verify the <br />predicted effect. <br />The proposed mining operation would not materially damage the quantity <br />or quality of surface and ground water which supply the alluvial valley <br />floor. During mining operations, the proposed underground mine would <br />slightly deplete flows in the stream/alluvial aquifer system, and the <br />discharge of water from the underground workings would affect water <br />quality in the Carbon Ditch and in Ward Creek. After mining <br />operations, when the natural ground water flow pattern is restored, <br />water passing through the underground workings would affect water <br />quality in the Williams Creek and Ward Creek streamlalluvial aquifer <br />system. A quantitative assessment of these effects is provided in the <br />discussion of probable hydrologic consequences contained in this <br />findings document. That assessment predicts the streamflow depletion to <br />be less than 2 percent of the average streamflow in Ward Creek, and less <br />than 7 percent of the lowest streamflow observed in Ward Creek. The <br />predicted water quality resulting from the mining activities would not <br />prevent the use of surface water for flood irrigation. <br />The essential hydrologic functions of the alluvial valley floors would <br />be preserved. The most important characteristics of the Williams Creek <br />and Ward Creek alluvial valley floors are the integrity of the present <br />irrigation system and the ability of the surface water system to supply <br />sufficient irrigation water to farming activities on the alluvial valley <br />floors. As discussed above, surface disturbances would be located <br />outside of the alluvial valley floors, and mining would be limited to <br />50-55 percent extraction to minimize surface subsidence effects. Any <br />surface effects are anticipated to be minor, and capable of remedy. The <br />operator has committed to promptly regrading depressions, swells or <br />cracks if any develop as a result of subsidence. As a result, the <br />surface topography and the integrity of the existing irrigation system <br />would be preserved. Since no significant effect to the quantity or <br />quality of the water which supplies the alluvial valley floor is <br />expected, the supply of irrigation water would also be preserved. <br />_pl_ <br />