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_GENERAL DOCUMENTS - C1981017 (262)
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_GENERAL DOCUMENTS - C1981017 (262)
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Last modified
11/2/2020 11:08:18 AM
Creation date
6/21/2012 10:47:08 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981017
IBM Index Class Name
GENERAL DOCUMENTS
Doc Name
Bid Documents (IMP) Backfilling and Grading Plan for Preparation Plant Area
Permit Index Doc Type
General Correspondence
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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-32- <br /> Surface Water <br /> The major river of this study area is the Roaring Fork River. The <br /> Roaring Fork joins with the Colorado River at the town of Glenwood <br /> Springs. For the purpose of this CHIS, the mouth of the roaring Fork <br /> will serve as the cumulative surface water impact reference point. All <br /> mines considered in this CHIS are tributary to the Roaring Fork. Please <br /> refer to Figure No. 1 for locations of all affected drainages, and Tables <br /> 2 and 3 for surface water quantity and quality characteristics. <br /> The Coal Basin Mines affects the Coal Creek Drainage. This stream joins <br /> the Crystal River at the town of Redstone. The Snowmass operation is <br /> located within Thompson Creek' s drainage basin just north of Coal 'Basin. <br /> Thompson Creek joins the Crystal River 11 miles downstream from Redstone. <br /> The Crystal River flows toward the town of Carbondale, where it joins <br /> with the Roaring Fork River. One-half mile downstream of this confluence <br /> is the Snowmass Coal Company loadout facility. <br /> Five miles downstream of the confluence of the Roaring Fork and the <br /> Crystal Rivers, is the confluence with Fourmile Creek. The Sunlight Nine <br /> is located on Fourmile Creek, 7.2 miles above this confluence. The <br /> Roaring Fork gaging station (the point defining the study watershed) is <br /> located 4.2 miles downstream of the Fourmile Creek confluence with the <br /> Roaring Fork River at Glenwood Springs, Colorado. <br /> Streams in the region cross t'ie outcrops of the Lower Mesaverde Group <br /> ( Iles and Lower Williams Fork Formation) at right angles to the strike of <br /> rock strata. This seems to indicate that these stream valleys have <br /> formed in zones of weakness such as fault and fracture systems, since <br /> these strata are relatively resistant to erosion. Other tributaries flow <br /> through strike valleys formed in less resistant shale units. <br /> Table 2 displays the flow characteristics of the streams affected by coal <br /> mining operations which are considered in the general area. <br /> The Crystal and Roaring Fork Rivers are similar in quality. Total <br /> suspended solids are less than 50 milligrams per liter for much of the <br /> year. Total dissolved solids are 200-500 milligrams per liter (mg/1 ) . <br /> Nith a pH slightly above neutral , heavy metals and trace elements in <br /> solution are low. All of these are indicators of good water quality. <br /> The Coal Creek Basin includes a 26.6 square mile watershed and consists <br /> of eight tributary streams. The Coal 3asin Hines affect six 3f these <br /> tributaries and a i0 square mile 'watershed area. Sediment loads ,iithin <br /> :his basin are naturally sign. This is due to the steep terrain and I <br /> large volumes or runoff generated primarily :�y snowmelt. eater quality <br /> is ,00d with total dissolved solids concentration less than 500 mg/l . <br />
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