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Bench 7220 <br />Foliation spacing ranges from approximately 4 inches to more than 2 feet, and <br />foliation apertures were tight to moderately open and slightly rough to rough. The <br />primary joint set strike ranges from 20 to 40 degrees and generally dips from 80 to 85 <br />degrees northwest. A second primary joint set is evident in this area and exhibits a <br />strike of 310 to 355 degrees with dips ranging from 55 to 75 degrees southwest. The <br />spacing of the primary joint sets varied widely, but averaged approximately 18 <br />inches. Joint apertures were tight to moderately open with slightly rough to rough <br />faces. <br />Adversely dipping foliation is present within this scanline primarily between approximate <br />stations 2 +45 and 2 +70. Special care should be taken to avoid small scale slide and raveling that <br />could occur in this area. <br />• Stations 3 +45 through 4 +75 were unmappable due to nearly complete rubble and <br />debris coverage. The condition of the highwall is unknown in this section. <br />Due to the maximum height of the highwalls on bench 7450 and adjacent to the upper haul road, <br />special care should be taken to avoid raveling from high on the highwall that could potentially <br />extend 25 feet or more from the highwall toe, possibly extending onto Bench 7220. A berm at <br />the base of the highwall will tend to restrict the range of the raveling rock. <br />Figures 6 and 7 are a photo documentary of the features observed in the upper haul road <br />highwall. <br />The Bench 7220 scanline is approximately 410 feet long and is currently unmappable due to <br />nearly complete debris and rubble coverage. The approximate orientation of the highwall is 340 <br />degrees (north 20 degrees west). The condition of the highwall is unknown in this section. <br />Due to the height of the highwalls above bench 7220, special care should be taken to avoid <br />raveling from high on the highwalls that could potentially extend 25 feet or more from the <br />highwall toe, possibly extending onto bench 7220. A berm at the base of the highwall will tend <br />to restrict the range of the raveling rock. <br />Figure 8 is a photo documentary of the features observed in Bench 7250. <br />Bench 6700 <br />The Bench 6700 scanline is approximately 300 feet long and was separated into 3 discrete <br />sections. The approximate orientation of the highwall is 0 degrees (north). A nearly vertical <br />granitic pegmatite was observed at approximate station 0 +40. This scanline is in addition to the <br />scanline conducted at this elevation for the 2011 Annual Report. <br />• Stations 0 +00 through 0 +40 consisted of highly fractured granitic gneiss. The <br />foliation strike varies in this area due to minor folding and ranges from 320 to 350 <br />6 <br />Morrison Quarry Annual Report 2012 <br />P \23514 \133- 23514- 13002\Dehverables\Dehv -01 -2012 Annual Report\Annual Report 20 12 Geolech doc <br />January 2013 <br />