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1993-04-19_REVISION - C1981008
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1993-04-19_REVISION - C1981008
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Entry Properties
Last modified
1/26/2021 10:45:17 PM
Creation date
6/11/2010 2:13:54 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981008
IBM Index Class Name
Revision
Doc Date
4/19/1993
Doc Name
PROPOSED DECISION & FINDINGS OF COMPLIANCE FOR RN2
Type & Sequence
RN2
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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The New Horizon Mine 1 produced coal from both the upper and lower Dakota coal <br /> seams . The upper Dakota coal seam ranges in thickness from 1 .6 feet to <br /> 3.3 feet and is separated from the lower Dakota seam by 7 to 11 feet of <br /> interbedded sandstone and shale. The lower Dakota seam varies in thickness <br /> from 5.9 feet to 7.9 feet. The base of the lower Dakota coal is 83 feet above <br /> the top of the Burro Canyon Formation. The coal dips 10 to 20 southwest <br /> and strikes N 250W to N 450 W. <br /> The New Horizon Mine 2 will primarily produce coal from the lower Dakota coal <br /> seam and may utilize the upper Dakota coal seam during subsequent permit terms <br /> if the seam is thick enough and of sufficient quality. The lower Dakota coal <br /> seam at New Horizon Mine 2 ranges in thickness from 4.2 feet to 6.9 feet and <br /> is 99 feet above the top of the Burro Canyon Formation. The coal dips <br /> 4.50 SW along a strike of N 450W. <br /> Surface Water <br /> The San Miguel River has its source in the San Juan Mountains . These <br /> mountains are primarily composed of Tertiary volcanic rocks . Iorns <br /> et. al . (1965a) has shown these waters to be of a calcium bicarbonate - <br /> sulfate type during high flow periods . These waters contain less bicarbonate <br /> during low flows while the calcium and sulfate concentrations increase due to <br /> less dilution from snowmelt runoff. The San Miguel River traverses the <br /> interior portions of a basin that is chiefly underlain by Dakota Sandstones , <br /> the Morrison Formation and Mancos Shales . The Morrison Formation and Mancos <br /> Shale have the greatest potential for influencing the river water chemistry. <br /> The San Miguel River drains an area of 1 ,080 square miles . In addition, <br /> approximately 15,500 acres of irrigated land lies between Placerville and <br /> Naturita, Colorado. It is estimated that 2 .8 tons of Total Dissolved Solids <br /> (TDS) per acre are contributed to the waters annually from this area. This <br /> results in increased levels of magnesium, potassium, sulfate and chloride. <br /> Water quality samples taken from the San Miguel River at Naturita, Colorado, <br /> have a weighted average of 316 milligrams per liter (mg/1 ) TDS. Specific <br /> 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 , <br /> 90 percent of the time , flow in this river exceeds 60 cubic feet per second <br /> (cfs) , while flows exceed 1000 cfs about 10 percent of the time. The mean <br /> discharge of the river is 351 cfs . San Miguel River waters are suitable for <br /> domestic usage except at low flow periods when sulfate levels are high. <br /> The Colorado Cooperative Ditch Company diverts as much as 155 cfs of water <br /> from the San Miguel River approximately ten miles east of the town of Nucla. <br /> The main diversion ditch then flows westerly passing just north of the town of <br /> Nucla and then flows northwestward passing north of the New Horizon Mine 1 . <br /> Diversion ditches distribute water to mainly agricultural users in the area. <br /> Additional uses include domestic , municipal and stock pond consumption. <br /> The New Horizon Mine 1 is located downslope from the main ditch in the gently <br /> sloped upland of Second Park. This is just north of Tuttle Draw and is <br /> totally within its watershed. The New Horizon Mine 2 site is just west of the <br /> town of Nucla and is located in the mildly sloping upland area immediately <br /> north of Calamity Draw, approximately in the middle of First Park. The <br /> above-mentioned parks consist of recent undifferentiated aeolian silts and <br /> sands overlaying the Dakota and Burro Canyon Formations . Since the completion <br /> -5- <br />
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