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K1L D UFF RMR Aggregates, Inc. <br /> U N ❑ E R G R O U N ❑ Rock Failure Analyses and Stabilization Report <br /> E NGIN E E R I N G,INC. Mid Continent Limestone Ouarry <br /> Figure 3 (provided by Lewicki & Associates)with corresponding site numbers, detailed below from <br /> south to north: <br /> • Site 2: 39.57167; -107.322920, approx. elev. 7,170 ft. <br /> o Structure measurement (dip/dip direction): 34°;185. <br /> 0 15 ft thick upper/lower limestone beds. <br /> o Laterally continuous bed surface. No significant aperture or adverse interbed. <br /> o Pairs with comparable surface looking west across drainage. <br /> • Site 3: 39.57190; -107.32288, approx. elev. 7,200ft. <br /> o Upper limestone layer measured 10 ft thick. <br /> o Laterally continuous bed surface without significant aperture or interbed. <br /> • Site 4: 39.57211; -107.32257, approx. elev 7,290 ft. <br /> o Daylight of laterally continuous bedding plane. Upper limestone beds have pinched out <br /> at this line of latitude. <br /> • Site 1: 39.57250; -107.32250, approx. elev. 7,370 ft. <br /> o Structure measurement (dip/dip direc): 28°;183. <br /> o Laterally continuous joint surface (>10 meters), wavy, covered in thin talus. <br /> o Pairs with comparable surface looking west across drainage. <br /> Photos of the site locations are provided in Appendix F. Talus cover and the waviness of the bed <br /> surface limited the ability for high confidence structural measurements at some sites. <br /> The spatial intent of the slope configuration models discussed in section 6 should be to extend north <br /> to where the upper limestone layers pinch out above the current mining activities. The bedrock <br /> bedding slope, which is the boundary between the massive limestone below and the adverse <br /> limestone units above, was observed as very laterally continuous but could undulate locally creating a <br /> slight change in dip direction.To meet the established minimum FOS for the slope, using a bench <br /> slope geometry of 1.4H:1V or greater that leaves varying thicknesses of the upper limestone layers in <br /> place will likely require the use of mechanical stabilization. This is considered a lesser option for long- <br /> term stability and safety, but is considered below on an as needed basis. <br /> 8. MINE STABILIZATION <br /> A summary of the mine operation plan recommendations, from a geotechnical perspective, is <br /> provided here to inform a full mine operation plan provided by RMRA under separate cover. The <br /> overall intent is to achieve longterm slope stability by eliminating the potential for headwall failure <br /> along the upper limestone beds. The mine plan works under the assumption the upper unit planar <br /> slide failure mode , dipping to the south along the laterally continuous bedding plane, will only <br /> release in that direction. The mine plan is a phased and stepped approach working from the <br /> southwest corner of the headwall to the northeast with the intent to eliminate the possibility of <br /> permanent or temporary condition of the upper limestone in the cutslope wall. <br /> It is the opinion of WE that the upper limestone layer should be removed completely from the <br /> highwall to minimize the risk of another release. This can be performed via multiple mining methods. <br /> Page 13 <br /> 535 16th STREET,SUITE 620 1 DENVER,CO 80202 1 (303)732-3692 1 WWW.KILDUFFUNDERGROUND.COM <br />