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2005-04-08_GENERAL DOCUMENTS - C1980007
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2005-04-08_GENERAL DOCUMENTS - C1980007
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Last modified
5/26/2020 4:04:33 PM
Creation date
11/23/2007 7:57:07 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
General Documents
Doc Date
4/8/2005
Doc Name
Proposed Decision & Findings of Compliance for PR11
From
West Flatiron Lease
Permit Index Doc Type
Findings
Media Type
D
Archive
No
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The West Elk mining operation is adjacent to Sylvester Gulch, Lone Pine <br />Gulch, and Gribble Gulch, which are ephemeral streams that flow <br />directly to the North Fork. No flow has been observed in Lone Pine <br />Gulch for a period of several years. Sylvester Gulch has a drainage area <br />of 4.25 square miles. The hydrologic yield of Sylvester Gulch is low <br />compared to the other watersheds in the West Elk life-of--mine area. This <br />is due to the fact that it drains an area which is lower in elevation and has <br />gentler slopes. To the south most of the West Elk Mine underlies the <br />Minnesota Creek drainage. <br />The Minnesota Creek basin is a significant drainage system occurring in <br />the southern part of the five-year permit area, and within the life-of--mine <br />coal lease boundary. Minnesota Creek and its tributaries drain the <br />southern portion of the coal lease area. These tributaries include Horse <br />Creek, South Prong, Lick Creek, Dry Fork, and East Fork. Minnesota <br />Creek enters the North Fork of the Gunnison near Paonia. <br />The Minnesota Creek drainage extends approximately 53.5 squaze miles <br />as shown in Figure 3 of this document. The West Elk life-of--mine area is <br />drained by five tributaries to Minnesota Creek. These tributaries include <br />East Fork, Horse Creek, South Prong, Lick Creek, and Dry Fork. <br />Characteristics of the drainages are given in Table 3 of this document. <br />Lick Creek and Dry Fork average slopes are generally steeper and the <br />watersheds aze at higher elevations than those tributary to the North Fork. <br />Based upon streamflows measured in water yeaz 1978, the water yields <br />from these drainages are nearly an order of magnitude greater than that <br />from Sylvester Gulch. <br />The evaluation of flow within the Minnesota Creek drainage can only be <br />considered an approximation due to infiltration and seepage losses, <br />seasonal vaziations in precipitation and potential evaporation and <br />sampling difficulties. Nevertheless, approximately 1,000 acre-feet is <br />annually transferred from the Little Gunnison Creek to the Dry Fork of <br />Minnesota Creek, and the average annual flow of the East Fork of <br />Minnesota Creek is approximately 19,920 acre-feet. Irrigation ditches <br />annually remove about 20,000 acre-feet from Minnesota Creek. <br />Two reservoirs are located within the Minnesota Creek drainage. <br />Minnesota Reservoir is located on the Dry Fork. It has a decreed <br />capacity of 1,285 acre-feet, but the actual capacity may be closer to 500 <br />acre-feet. Beaver Reservoir is located on the East Fork of Minnesota <br />Creek and has an absolute decreed capacity of 1,620 acre-feet and a <br />conditional decree of 522 acre- feet. Both reservoirs store water for <br />irrigation purposes and aze filled during spring runoff. They are usually <br />drained by late August or early September. <br />49 <br />
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