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Strike Dip Joint Designation Remarks <br /> N33W 35NE J-f Foliation (Primary) <br /> N58W 74NE J-1 Secondary <br /> N54E 75SE J-2 Secondary <br /> N38W_ _ _ 77SW _J-3 _ Secondary <br /> N54e 76NW J-4 Secondary <br /> N27W 41SW 1-5 Tertiary <br /> N20E 40NW J-6 Tertiary <br /> Stability evaluations for proposed highwall slopes were preformed using the average joint orientations <br /> listed above. There were based mainly on the primary foliation and secondary steeply dipping joints, <br /> but also considered the tertiary daylighting joint sets. Because the tertiary joint sets are not very <br /> common or persistent,the two sets were averaged into one westerly dipping orientation for the <br /> analyses. Also because of the lack of occurrence and persistence of these tertiary features,they are <br /> considered to be relevant only to individual highwall,and not overall slope,stability. <br /> The stereonet analysis and summary included in Attachment D shows potential; sliding plane and wedge <br /> failures. These all assume continuous,through-going joint features,which is a conservative assumption <br /> for this rock mass. Analysis shows potential slope failures if the slope were steepened to 1:4 from <br /> originally proposed 1:2 configuration, but acceptable slope conditions for a quarry development if <br /> steepened to 1:3 as Elk Creek is presently proposing(12 ft benches by 35 ft highwalls= 1:2.9). <br /> For slope failures to occur, planar or wedge failures must first be kinematically(geometrically) possible <br /> or admissible. In addition,for given possible planar or wedge failures mode,the material strength <br /> properties of the rock must be low enough for these failures to be mechani9cally possible or admissible. <br /> Such analyses were run for all kinematically admissible planes and wedges for both weathered and <br /> unweathered rock using internal friction angles of 30 degrees and 40 degrees, respectively. <br /> For the proposed 1:3 slopes, our analyses indicate that sliding failure is kinematically admissible only on <br /> the averaged westerly dipping joint set, but that this is mechanically admissible only in the upper <br /> weathered rock. Toppling failure is not kinematically admissible for any of the six joint sets analyzed. Of <br /> five wedge failures modes identified in the analyses,three are kinematically and mechanically <br /> admissible in the upper weathered rock, but not in the general rock mass. Two of the wedges might <br /> require spot bolting, but limited individual wedge failure in final highwalls is usually considered <br /> acceptable in quarry operations. As an example, DMG permitting for the Morrison Quarry in a similar <br /> rock mass assumed up to 15 to 20 percent such failures to be acceptable. The upper weathered rock <br /> should be laid back to 1:1 for long term stability. <br /> Part of the slope stability analyses included interpretation of rock mass classification and therefore, <br /> strength properties. Summaries of estimated rock mass properties based on rock mass classification <br />