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The New Horizon Mine 1 produced coal from both the upper and lower Dakota coal seams. The <br />upper Dakota coal seam ranges in thickness from 1.6 feet to 3.3 feet and is separated from the lower <br />Dakota seam by 7 to 11 feet of interbedded sandstone and shale. The lower Dakota seam varies in <br />thickness from 5.9 feet to 7.9 feet. The base of the lower Dakota coal is 83 feet above the top of the <br />Burro Canyon Formation. The coal dips 1° to 2° southwest and strikes N 25"W to N 45° W. <br />The New Horizon Mine 2 primazily produces coal from the Lower Dakota coal seam and will utilize <br />the Upper Dakota coal seam when the seam is thick enough and of sufficient quality. The lower <br />Dakota coal seam at New Horizon Mine 2 ranges in thickness from 4.2 feet to 6.9 feet and is 99 feet <br />above the top of the Burro Canyon Formation. The. coal dips 4.5° SW along a strike of N 45° W. <br />Surface Water <br />The San Miguel River has its source in the San Juan Mountains. These mountains are primazily <br />composed of Tertiary volcanic rocks. Ioms et. al. (1965a) has shown these waters to be of a calcium <br />bicarbonate-sulfate type during high flow periods. These waters contain less bicazbonate during low <br />flows while the calcium and sulfate concentrations increase due to less dilution from snowmelt <br />runoff. The San Miguel River traverses the interior portions of a basin that is chiefly underlain by <br />Dakota Sandstones, the Morrison Formation and Mancos Shales. The Morrison Formation and <br />Mancos Shale have the greatest potential for influencing the river water chemistry. The San Miguel <br />River drains an azea of 1,080 squaze miles. In addition, approximately 15,500 acres of irrigated land <br />lies between Placerville and Naturita, Colorado. It is estimated that 2.8 tons of Total Dissolved <br />Solids (TDS) per acre aze contributed to the waters annually from this area. This results in increased <br />levels of magnesium, potassium, sulfate and chloride. Water quality samples taken from the San <br />Miguel River at Naturita, Colorado, have a weighted average of 316 milligrams per liter (mg/1) TDS. <br />Specific conductance varies between 318 and 730 millimhos (mmhos). The mean sodium <br />adsorption ratio (SAR) is about 0.7 at Naturita. Water curves indicate that, 90 percent of the time, <br />flow in this river exceeds 60 cubic feet per second (cfs), while flows exceed 1000 cfs about 10 <br />percent of the time. The mean discharge of the river is 351 cfs. San Miguel River waters aze <br />suitable for domestic usage except at low flow periods when sulfate levels aze high. <br />The Colorado Cooperative Ditch Company diverts as much as 145 cfs of water from the San Miguel <br />River approximately ten miles east of the town of Nucla. The main diversion ditch then flows <br />westerly passing just north of the town of Nucla and then flows northwestwazd passing north of the <br />New Horizon Mine 1. Diversion ditches distribute water to mainly agricultural users in the area. <br />Since the completion of the irrigation system for this area in about 1910, these areas have been <br />intensively reworked for irrigated agriculture. Additional uses include domestic, municipal and stock <br />pond consumption. <br />The New Horizon Mine 1 is located downslope from the main ditch in the gently sloped upland of <br />Second Pazk. This is just north of Tuttle Draw and is totally within its watershed. The Second Pazk <br />Lateral Irrigation Ditch is in continuous operation from mid-April through mid-October. While this <br />water is primarily used for irrigation, important secondary uses include maintaining water levels in <br />stock ponds and domestic cisterns. During the non-imgation season [he ditch is occasionally turned <br />on to maintain the water levels in the stock ponds and cisterns. <br />