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PERMFILE112237
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PERMFILE112237
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Last modified
8/24/2016 10:08:38 PM
Creation date
11/24/2007 9:19:51 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981071
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
PR2 RULE 2.05 Operation and Reclamation Plans
Media Type
D
Archive
No
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In reference to Areas 9 and 10, and 31, no repair is required for the Swale <br />• and Swale-like feature in these areas. Water Engineering and Technology <br />Inc. has prepared a report (see Appendix II) which demonstrates that these <br />areas comply with the backfilling and regrading requirements of the <br />regulations. <br />A section of the report in Appendix II utilizes hypsometric analysis to <br />show that three AOC requirements leave been met at the CYCC operation. As <br />part of this analysis, the mine areas were initially combined to form a <br />drainage basin. However, the combined mine areas consisting of Areas 31,7, <br />51 and 41 can be divided into five watersheds (i.e. first-order basins). <br />Analysis on a basin scale is justified by the contention by many that a <br />drainage basin is the smallest fundamental hydrologic or geometric unit. <br />For instance, Gregory and Walling (1973, preface) state that the drainage <br />basin, "... is visualized increasingly as the fundamental unit of study in <br />fluvial geomorphology...". Ritter (1978, p. 169) describes basins as, <br />" excellent fundamental units of geomorphic systems." Charley et <br />al. (1987, p. 3i6) point out that the drainage basin,"... has been <br />recognized as a viable process-response unit since the beginning of the last <br />century." It is concluded then, that comparison of mine areas smaller than <br />a first order basin is inappropriate because it is a comparison of only a <br />portion of the basic geomorphic system unit. <br />The five watersheds are approximately the size of first-order basins and <br />they extend from the lowermost portions of the mine adjacent to South Foidel <br />Creek to the top cf the mine. Approximate drainage divides were drawn <br />• between adjacent watersheds that remain fixed on both existing and approved <br />topographic maps so that the same area is measured for both conditions. <br />Contour interval for the analysis is 50 feet except in the area of the Swale <br />where contour interval is 25 feet. Hypsometric curves for existing and <br />approved topography within the five watersheds (Figs. 1 through 5) are <br />similar indicating, as did the analysis presented in our report, that spoil <br />material has not been significantly re-arranged by mining. Figure 6 shows <br />the relative locations of mine areas, stream channels, and watershed areas. <br />in addition, portions of the Swale in Areas 9 and 10 have been topsoiled and <br />revegetated. It tiould not be prudent to disturb these revegetated areas <br />when no benefit would be gained by such an action. Likewise, for the <br />Swale-like feature in Nrea 31, the entire area iias been topsoiled and <br />revegetated. Disturbing this area to eliminate a Swale-like feature is not <br />warranted. <br />It should be noted that the 4later Engineering and Technology report included <br />procedures that thie Wyoming Department of Environmental Quality (DEQ) has <br />proposed for determining pre- and post-mining surface configurations. A <br />copy of the DEQ memorandum is contained in Appendix III. <br />In addition, the postmining land use is for both rangeland and wildlife. <br />The creation of topographic diversity, i.e. swales, certainly benefit the <br />utilization of the reclaimed areas by wildlife. <br />~. - 53 - Revised 04/11/88 <br />
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