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PERMFILE134266
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PERMFILE134266
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Last modified
8/24/2016 10:34:58 PM
Creation date
11/26/2007 2:04:30 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
EXHIBIT 70 REFUSE PILE EXPANSION
Media Type
D
Archive
No
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REFUSE PILE EXPANSION <br /> <br />~~ <br /> <br />to obtain suitable samples for direct shear and <br />triaxial testing. <br />Two permanent 2-inch diameter slotted Schedule 40 <br />PVC piezometers were installed in borings LRP-1 <br />and LRP-4 during the October, 1995, drilling <br />program. The other borings were sealed and <br />abandoned in accordance with exploration Notice of <br />Intent to Explore (NOi) No. X-95-212-04. The <br />piezometer borings were placed on the approximate <br />border of the proposed RPE foundation footprint. <br />The piezometers were installed in order to obtain <br />groundwater elevations and water quality <br />information prior to and during construction of the <br />proposed RPE. Both piezometers were installed as <br />per the requirements of the NOI X-95-212-04. The <br />slotted screen section of each piezometer was <br />established as close to the bedrock surface as <br />possible. The piezometer borings were backfilled <br />with Ottawa course grained sand to within ten feet <br />of the natural surface. A seven foot concrete plug <br />(to stop surface water infiltration into the boring) <br />was placed from three feet to ten feet below surface. <br />The remaining portion of the piezometer borings <br />were filled with auger cuttings and soil. The logs of <br />the piezometer installations can be found in <br />Appendix F of this report. <br />5.2 Laboratory Testing <br />The laboratory testing program conducted on the <br />soil samples retrieved from the drilling investigation <br />included gradation tests, moisture content <br />determination, Atterberg limits, and triaxial shear <br />testing. The laboratory testing was conducted by <br />Garco Testing Laboratories of Salt Lake City, Utah, <br />and Colorado State University's soil laboratory. All <br />testing utilized the appropriate ASTM procedures. <br />The Shelby tube soil samples tested for triaxial <br />shear strengths values consisted of predominantly <br />gravely-sandy soils. Due to the very granular nature <br />of [he gravely soils in the proposed RPE area, only <br />two Shelbv tubes could be obtained. The results of <br />the triaxial shear testing are found in Appendix G. <br />The gradations, moisture contents and Atterberg <br />limits of [he soils can be found in Appendix G. <br />5.3 Geology <br />5.3.1 Introduction <br />This section presents the results of the geologic <br />engineering mapping of the proposed RPE site. The <br />purpose of the geologic engineering mapping was to <br />evaluate the presence of geologic and hydrologic <br />features that may impact the development of the <br />proposed RPE. The proposed RPE will be used by <br />MCC for consvucting a fill of coal refuse generated <br />by future coal mining operations. As part of this <br />geologic engineering mapping, HLA: <br />• conducted a field evaluation of landslide and <br />landslide prone areas within the proposed <br />limits of the RPE; and <br />• examined and evaluated all hydrologic <br />features and associated Flows within and <br />outside the proposed limits of the RPE. <br />5.3.2 Background <br />The following section is a brief discussion of site <br />location and previous site investigations. <br />5.3.2.1 Location/Site Description <br />The West Elk Mine (WEM) site is located two miles <br />east of the town of Somerset, Colorado, to the south <br />of the North Fork of the Gunnison River, and <br />approximately six miles west of Paonia Reservoir. <br />The WEM is an active underground coal mining <br />operation. <br />The proposed site for the development of the RPE is <br />currently an undeveloped section of land owned by <br />MCC. The site is located on the lower portion of an <br />area referred to as the West Flatiron and is bordered <br />by Highway 133 on the north, Sylvester Gulch on the <br />west, and an unnamed gulch between Sylvester Gulch <br />and Box Canyon on the east. The site is generally <br />vegetated with Gambel oak, spruce, and aspen trees. <br />Historical development of this area is limited to an <br />old jeep trail through [he central portion of the site, <br />and an abandoned cistern and stock watering tank <br />on the east Flank of Sylvester Gulch. <br />5.3.2.2 Site Investigation <br />Harding Lawson Associates <br />4 <br />
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