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GENERAL41890
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Last modified
8/24/2016 8:10:17 PM
Creation date
11/23/2007 11:29:04 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982054
IBM Index Class Name
General Documents
Doc Date
7/5/1983
Doc Name
PROPOSED DECISION AND FINDINGS OF COMPLIANCE
Permit Index Doc Type
FINDINGS
Media Type
D
Archive
No
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-7- <br /> <br />GENERAL DESCRIPTION OF THE EXISTING ENVIRONMENT <br />The proposed operation is located in southwestern Colorado, approximately <br />2 1/2 miles southeast of Durango (Figure 1). Elevation of the area <br />ranges from approximately 6500 feet to 7400 feet. <br />There are no documented cultural properties in the proposed permit area. <br />The proposed Carbon Junction Mine will be located in the upper drainage <br />basin of Carbon Junction Canyon. This is an intermittent tributary to <br />the Animas River. The total drainage basin of Carbon Junction Canyon is <br />0.8 square miles. This drainage has a steep gradient and, through much <br />of its reach, is contained within steep valley walls. <br />The Carbon Junction Mine permit area is located on the northern edge of <br />the San Juan Structural Basin in Southwestern Colorado. The sedimentary <br />rock strata dip 26 to 30 degrees to the southeast and strike N45oE. No <br />major faults exist in the permit and adjacent areas. <br />The rock units exposed in the permit and adjacent areas are all <br />Cretaceous in age. These units include the Lewis Shale, the Pictured <br />Cliffs Sandstone, the Fruitland Formation and the Kirtland Shale. The <br />Carbon Junction Mine will extract coal from the Lewis coal seam ("C" <br />seam), Carbonero seam ("B" seam) and the Shamrock seam ("A" seam) within <br />the Fruitland Formation. <br />Ground water within the general area of the mine occurs in the Pictured <br />Cliffs Sandstone, the interbedded and lenticular sandstones, and the <br />coals of the Fruitland Formation, the Quaternary terrace deposits, and <br />the alluvium of the Animas River. <br />Ground water movement in the rock strata is controlled by the geologic <br />structure and the stratigraphy. Ground water within sandstone and coal <br />units flows down the dip of the strata and through fracture zones. <br />Bedrock aquifers are recharged at their outcrops and subcrops. These <br />aquifers discharge at lower elevations, primarily in stream valleys. <br />Lenticular and interbedded sandstones support only localized ground water <br />flows. <br />There are no alluvial valley floor deposits within the permit area. <br />The climate of the area is relatively moderate, with a monthly low mean <br />temperature of 25.3oF in January and a monthly high mean temperature of <br />67.O~F in July. Record temperature extremes range from a high of <br />99oF, recorded in August, to lows of -27oF, recorded in January and <br />February. Annual precipitation averages 18.04 inches, with a maximum of <br />2.36 inches in August and a minimum of 0.98 inches in November. The <br />average snowfall is 65.3 inches, with the highest amount in January (21.2 <br />inches), followed by December (14.8 inches). The average wind direction <br />is generally from the west, with an average speed of less than one knot. <br />
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