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APPCOR12542
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APPCOR12542
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Entry Properties
Last modified
8/24/2016 6:32:57 PM
Creation date
11/19/2007 2:31:46 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981034
IBM Index Class Name
Application Correspondence
Doc Date
11/8/1982
Doc Name
GRAND MESA CHIS
From
MLR
To
DAN MATHEWS
Media Type
D
Archive
No
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<br />-- <br />~< <br />y~ , <br />~~ <br />~" . <br /> -' <br />• <br />STATE OF COIA RADO girN ~•d'A. Gnv ¢,vn <br />DEPARTMENT OF NATURAL RESOURCES III III III III IIII III <br />D. Monte Pascoe, Executive Director <br />999 <br />ML~VED LAND RECLAi17A'TION <br />423 Centennial Building. 1313 Sherman Street <br />Denver. Colorado 80203 Tel. (303) F6G-3567 <br />David C. Shelton <br />Director <br />DATE: November 3, 1982 <br />TD: Dan Pla thews <br />/[~n <br />FROM: David Craig .. 1--i <br />RE: Grand Mesa CNIS <br />Grand Mesa Coal Company <br />Red Canyon Mines <br />Cumulative Hydrologic Impact Statement - (CNIS) <br />The only other mine in the vicinity of the Grand Pfesa operation which <br />could cumulatively impact ground-water resources is the Quinn Tomahawk <br />Mine. It is located about two miles to the west. The incised valley <br />of 47ard Creek separates the two mines. Both operafi:ons mine coal from <br />the same sequence of strata. The Tomahawk 7•fine will have both surface <br />and underground mining operations. The Grand Mesa 14ine is solely an <br />underground operation. For more detail regarding the proposed mininy <br />plans the reader is directed to the description of operations portion of <br />this document and of the Quinn 4bmaha~ok Ffine findings document (published <br />by the Division on April 9, 1932). Also discussed in the findings <br />documents are the statements of probable hydrologic consequences of each <br />individual mining operation. <br />The coal being mined at both operations is situated in the lower portion <br />of the [dilliams Fozk Formation; whose strata consist of interbedded <br />standstones, siltstones, shales, and coals. Most of these strata are <br />laterally discontinuous. The only continuous strata are the coal seams <br />and the underlying Rollins Sandstone. The coal seams outcrop neaz~ the <br />mines and generally dip to the north beneath Grand Afesa, continuing deep <br />beneath the Piceance Basin. Because of their limited aquifer potential <br />and great depth, the strata to be disturbed by the proposed mininy <br />operations are not used extensively for water supplies. Only a few <br />stock-watering ~oells have been completed in the potentially affected <br />s tra to . <br />
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