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<br />The alluvia of Trout Creek and its tributaries are important sources of ground water. The alluvial bodies <br />are used as water supplies, provide subirrigation to vegetation, and supply base flow to the streams. The <br />alluvial bodies are recharged by both the streams and the bedrock aquifers. <br />The mine is located in the upper reaches of the Yampa River Basin. The proposed permit revision area <br />and adjacent areas are drained by Foidel Creek, an intermittent stream ,and Fish Creek and Middle <br />Creeks, both perennial streams. Fish Creek drains east into Trout Creek whereas Foidel Creek runs <br />northeast to Middle Creek before joining Trout Creek. The quality of water in the Fish Creek and Foidel <br />Creek drainages have been affected previously by surface mining upstream and downstream of the <br />underground mine's existing surface facilities. Alluvial valley floors are identified downstream of the <br />proposed mining area at the confluence of Foidel and Middle Creek, and on Trout Creek from its <br />confluence with Middle Creek downstream to the Yampa River. Permit Revision No. 3 declassified <br />portions of Foidel and Middle creeks previously classified as AVF's. Detailed discussion concerning <br />alluvial valley floors can be found in Section B, part XVII of this document. <br />The climate within the area is semi-arid with a mean annual precipitation of 14.6 inches. Approximately <br />45 percent of this precipitation occurs during the growing season of April though September. High <br />temperatures generally range from 70-80oF in the summer months to below freezing in the winter months. <br />Normally, a significant snowpack resides on the ground for 4-5 months during the winter. <br />Two broadly classified soil complexes exist within the permit area. These are Typic Paleoborolls - <br />Borollic Camborthids and Argic Cryoborolls - Cryic Paleoborolls. However, prior to mining, the Typic <br />Paleoborolls - Borollic Camborthids soils covered the disturbed area. They occur primarily on uplands <br />and are formed in materials weathered in place from soft shale. These clayey soils are moderately deep to <br />deep, well drained and usually contain less than 35 percent rock fragments. Permeability is slow, <br />shrink-swell potential is high and potential frost action is moderate to high. These soils are used for <br />rangeland, non-irrigated cropland, and irrigated hay and pastureland. <br />Vegetation in the vicinity of the mine is characterized by four major communities: grassland, mountain <br />shrub, big sagebrush, and cropland; and by two sub-types: aspen and mountain shrub-rock outcrop. <br />Within the Foidel Creek Mine disturbed area, the prominent vegetation types prior to disturbance were big <br />sagebrush and cropland (dryland small grains). <br />Numerous wildlife species inhabit the general area. The most predominant are elk, mule deer and grouse. <br />Other wildlife species include: black bear, cougar, rabbit, coyote, bobcat, red fox, rodents, bats, skunks, <br />waterfowl, amphibians and reptiles. Two golden eagle nests are located on sandstone cliffs adjacent to the <br />disturbed area within the permit boundary for CYCC Permit No. C-81-071. There is critical winter habitat <br />for elk, an elk migration corridor and elk calving grounds and critical sage grouse habitat within and <br />adjacent to the proposed permit area. Sage grouse critical habitat is located outside of the disturbed area. <br />Cultural and historic resources within the permit area include three historic sites and one prehistoric or <br />protohistoric site. Two of the historic sites are undistinguished homesteads with no important architectural <br />features and which are not associated with persons important in history. The other historic site, the Foidel <br />Canyon Schoolhouse, is listed in the National Register of Historic Places, and is located in the general area <br />of the main facilities along Foidel Creek. It will not be undermined or subsided and is protected <br />appropriately. The prehistoric site (SRT345) is a rock art site located on the outcrop of the Twentymile <br />Sandstone directly north of the main mine facility area. Mining approved under PR-02 (Southwest Mining <br />District) undermined and subsided SRT345. Stipulation No. 33 was attached to the PR-02 approval and <br />the required appropriate measures, as determined by the BLM, were taken prior to undermining this site. <br />