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1996-06-25_GENERAL DOCUMENTS - C1980007
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1996-06-25_GENERAL DOCUMENTS - C1980007
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Last modified
2/17/2021 10:45:05 AM
Creation date
11/23/2007 5:42:34 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
General Documents
Doc Date
6/25/1996
Doc Name
Proposed Decision & Findings of Compliance for RN3
Permit Index Doc Type
FINDINGS
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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of the coal lease area. Minnesota Creek enters the North Fork of the Gunnison River near <br /> Paonia. The overall drainage exhibits a dendritic drainage pattern with steep channels. <br /> Horse Creek and South Prong of the East Fork of Minnesota Creek are perennial streams, <br /> while Lick Creek, Upper Dry Fork, Sylvester Gulch and Gribble Gulch are ephemeral <br /> streams. Minnesota Reservoir controls much of the flow in the lower Dry Fork of <br /> Minnesota Creek, and Beaver Reservoir controls the flow in the East Fork of Minnesota <br /> Creek. Lone Pine Gulch has no evidence of recent flow; therefore, no gaging station has <br /> been constructed. Even when all of the six gaged watersheds were found to be flowing, <br /> Lone Pine Gulch showcd no flow or evidence of flow. <br /> There are three different types of springs within the permit area including alluvial, colluvial, <br /> and bedrock springs. At least 69 springs have been identified within the permit area. <br /> Available data indicate that approximately 65 percent originate from alluvium and/or <br /> colluvium, and 35 percent have bedrock formation as their source. The flow rates of these <br /> springs are highly seasonal with peak flows occurring during wet weather conditions. <br /> Reservoirs and stock ponds also occur within or near the permit area. Minnesota Reservoir, <br /> on the Dry Fork of Minnesota Creek, is centrally located within the coal lease area. Beaver <br /> Reservoir on the East Fork of Minnesota Creek is located near the southwestern boundary of <br /> the coal lease area. <br /> In addition to the storage reservoirs in the area of the West Elk Mine, a total of 74 stock <br /> water impoundments have been identified in or adjacent to the permit area. Map 37 of the <br /> permit document shows the locations of the known stock water ponds. These ponds <br /> generally do not represent adjudicated water rights or perennial flows. Within the Gunnison <br /> National Forest, the ponds are managed for seasonal use by the U.S. Forest Service. <br /> Wetlands have also been identified within the permit area. Based upon inspection of <br /> conventional and infra-red aerial photographs and reconnaissance-level field investigation, <br /> there are estimated to be 2 to 3 acres of wetlands (as defined by the U.S. Army Corps of <br /> Engineers) in the Apache Rocks permit revision area. Most of the wetlands are found in <br /> drainage channels, although there are small, isolated wetlands on the hillsides where springs <br /> and seeps occasionally emerge as a result of landslides/sumps. <br /> Climatological Information - Rules 2.4.8 <br /> Information regarding climate characteristics can be found in Section 2.04.3 and 2.04.8 of <br /> West Elk's permit application. <br /> The mine site lies within the North Fork valley near Somerset, Colorado. At the mine site <br /> the valley is narrow and steep sided and follows a general east-west orientation. <br /> Considerable topographic variation across the mine site, and west central Colorado in <br /> general, results in marked fluctuation in seasonal and average precipitation and temperature <br /> values for the entire area. <br /> The mountains of the Continental Divide provide an effective barrier to the movement of <br /> moisture-laden air that reaches the eastern slope of the Rocky Mountains from the Gulf of <br /> Mexico. Under this influence, two basic types of climate, semi-arid and undifferentiated <br /> highlands, are characteristic of the general area where the mine is situated. Temperatures <br /> 11 <br />
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