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GENERAL32613
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Last modified
8/24/2016 7:55:04 PM
Creation date
11/23/2007 7:21:31 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981025
IBM Index Class Name
General Documents
Doc Date
7/14/1983
Doc Name
PROPOSED DECISION AND FINDINGS OF COMPLIANCE
Permit Index Doc Type
FINDINGS
Media Type
D
Archive
No
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• <br />-16- <br />Mid-Continent will be undermining the headwaters of Muddy Creek, a <br />tributary of the North Fork of the Gunnison. The underground workings at <br />that point will be over 2,000 feet below the ground surface. There is no <br />surface disturbance in this watershed and subsidence effects are <br />projected to be minimal, therefore, this portion of the Coal Basin mining <br />operation will not be considered in the cumulative hydrologic impact <br />assessment (See Coal Basin Mines Permit Application). The other two <br />mines are entirely within the Roaring fork drainage basin. <br />All three mining operations in the general area are underground <br />operations. The life-of-mine areas of these mines are plotted on Figure <br />3. In addition, the coal seams to be mined, the area of surface <br />disturbance, the area to be undermined during the first 5-year permit <br />period and the area to be undermined during the life-of-mine are <br />tabulated 1n Table 1. Thts assessment is divided into the three major <br />subsections: Description of the Hydrologic Environment, Probable <br />Hydrologic Consequences of Mining and Cumulative Hydrologic Impact <br />Assessment. <br />Description of the Hydrologic Environment , <br />The first part of this assessment describes the hydrology of the Roaring <br />Fork River Drainage Basin. Thts includes a regional description of <br />1) topography, 2) preclpitatlon and runoff, 3) geology, 4) ground water, <br />and 5) surface water. <br />Topography <br />The topography of the Crystal-Roaring Fork Drainage Basin consists of <br />broad flood plains and terraces to the lowland river valleys flanked by <br />steep walled canyons and broad park areas along the tributary streams. <br />The topography is strongly controlled by the erosional resistance of the <br />sedimentary rock strata along the Grand Hogback. Resistant sandstone <br />strata form steep sloped water gaps along stream channels, and form <br />prominent ridges and cliffs. Erosive shale strata form the broad river <br />valleys and tntra-mountain parks. <br />The tributaries that flow within the affected area of the mines have <br />steep relief and steep stream gradients. Fourmlle Creek varies 1n <br />elevation from 10,361 feet at Bald Mountain to 7,831 feet at the Sunllyht <br />Mine to 5,950 feet at the Roaring Fork River. Thompson Creek varies from <br />10,927 feet at Twin Peaks to 7,500 feet at the North Thompson Creek Mines <br />to 6,350 feet at the Crystal River. Coal Creek varies from 11,852 feet <br />at Huntsman Ridge to 8,000 feet at the surface facilities of the Coal ,~~ <br />Basin Mines to 7,165 feet at the confluence with the Crystal River. <br />Preclpitatlon and Runoff <br />Mean annual precipitation varies with elevation and slope attitude, that <br />1s preclpitatlon is orographically controlled. The mean annual <br />precipitation at Glenwood Springs (lowest end of the Roaring Fork <br />watershed) 1s 16 inches per year; at the Sunlight Mine, it is about 18 <br />inches; dt Basdlt, Colorado, tt 1s 15 inches; at the Coal Basin Mines, 1t <br />1s 26.A inches; and, at the upper elevations along Huntsman Ridge, the <br />mean annual preclpitatlon is in excess of AO inches. <br />
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