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PERMFILE51657
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PERMFILE51657
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Last modified
8/24/2016 10:55:41 PM
Creation date
11/20/2007 3:00:40 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981008A
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
NH1 TAB 6 GEOLOGIC INFORMATION
Media Type
D
Archive
Yes
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• III. SITE SPECIFIC GEOLOGY <br />A. INTRODUCTION. For a pericd of n;ore than 23 years, Peabody <br />Coal Company has gathered and 'analyzed detailed information on <br />the geology of the mine plan area. This information ir~cludes a <br />program of high density exploration drilling, geologic mapping, <br />topographic mapping, aerial photography, field investigations <br />and ground water quantity and quality data. A comprehensive <br />description and analysis of this information will provide <br />background information for ground water and surface water <br />hydrology, soils and revegetation sections covered later in the <br />permit, <br />B. RECORDS OF DRILL HOLES. Appendices 6-1 and 7-4 contain <br />numerous lithologic and geophysical drill logs for the permit <br />area which show and describe the lithologic characteristics and <br />thickness for each coal seam and associated strata. The <br />• location and elevation of these drilling sites are provided in <br />Tables 6-2 through 6-4. The locations of these drill holes are <br />shown on Exhibits 6-3, 6-3.A and/or 7-2. <br />2.04.6(1} <br />(a)(i)(ii) C. STRUCTURE. The mine site is located a few miles north <br />of the axis of the structurally simple Nucla Syncline. <br />Structure contours drawn as the top of the Lower Dakota <br />(#2) coal seam indicate that the coal dips 1° to 2° southwest <br />and strike N. 25° W to N. 45° :J (see Exhibit 6-3). Minor <br />local variations in the attitude of these coals occur due <br />to spuriously trending small folds and peneconteinporaneous <br />depositional features. These slight undulations are best <br />seen in the highwalis and mind floors of active and <br />abandoned mine pits in the northwest pur•t of the permit <br />area. The outcrop patterns and configuration of <br />overburden thicknesses are determined by a combination of <br />• topography and geologic structure. Overburden isopach contours <br />are shown in Exhibit 6-3. Tfrree geologic cross sections, <br />6-9 Revised 11/O1/II6 <br />
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