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GENERAL40748
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GENERAL40748
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Last modified
8/24/2016 7:59:53 PM
Creation date
11/23/2007 10:50:45 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981028
IBM Index Class Name
General Documents
Doc Date
3/17/1992
Doc Name
Proposed Decision & Findings of Compliance for RN2
Permit Index Doc Type
Findings
Media Type
D
Archive
No
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Description of the Environment <br />The Keenesburg Mine is approximately 4.5 miles north of Keenesburg, Colorado. <br />Ennis Draw, an ephemeral drainage, is located along the eastern boundary of <br />the permit area. No stream, river, or other body of water lies within the <br />mine site. The post-mining use of the affected land is rangeland. The permit <br />area is located on level to gently rolling topography consisting of fine sand, <br />which is wind-deposited material overlying weathered residual shale. The sand <br />varies in depth from about 5 feet to 20 feet, is highly to moderately <br />permeable, and is highly susceptible to wind erosion. For these reasons, the <br />land capability is classified as VIe for dryland farming and IV for irrigated <br />farming. <br />The proposed non-irrigated site is classified as rangeland by the <br />U.S. Department of Agriculture, Soil Conservation Service, as shown on page 37 <br />of the permit application, general soil map of Weld County, Colorado. The <br />land cannot support a variety of uses under existing technologies and local <br />resources. All attempts at dryland farming on the area have been abandoned, <br />and the damage caused by those attempts will remain evident for many decades. <br />Otherwise, the land is moderately to well stabilized by a sandsage-prairie <br />sandreed plant association that is used primarily for grazing by cattle in <br />summer months. Fort Lupton, which has an average annual precipitation of 12.5 <br />inches, provides the best estimate of precipitation at the area. <br />Previous mining activity at the site extracted the No. 7 coal seam of the <br />Laramie Formation. The flat-lying coal seam is overlain by 60-100 feet of <br />overburden consisting of yellow-brown and gray to blue gray soft carbonaceous <br />shale and clay interbedded with sand and shaley sand. At the base of the <br />Laramie Formation is the Fox Hills member, a cross bedded gray to buff <br />sandstone which is slightly to well cemented. <br />Because of the low relief and deep, well drained soils, there is virtually no <br />surface runoff Therefore, no streams springs or seeps exist in the area. All <br />water flows subsurface through aeolian deposits to Ennis Draw, an ephemeral <br />drainage. Ennis Draw appears to be a complex, braided, ancient stream bed <br />that has been covered by windblown sand. It discharges several miles to the <br />north into Box Elder Creek. <br />Since there is no surface runoff or streams in the area, wildlife is limited <br />to small rodents, primarily field mice, and birds with an occasional spotting <br />of raptors such as hawks and eagles. There are no known endangered species in <br />the area. Deer are rare as are most higher order vertebrates. <br />-~- <br />
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