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highwall. A secondary joint set is evident in this area and exhibits a strike of <br />265 to 270 degrees with dips of 80 to 90 degrees southeast. The spacing of <br />joint sets one and two varied widely, but averaged approximately 36 inches. <br />Joint apertures were tight to moderately open with slightly rough faces. Small <br />blocks may form in this area due to the orientation of the highwall and jointsets <br />of the rock. These blocks are anticipated to be limited in size, and should be <br />retained on the bench below the highwall. <br />Stations 4+75 through 5+75 consisted of moderately to highly fractured granitic <br />gneiss. The foliation strike in this area varies due to minor folding and ranges <br />from 305 to 340 degrees with dips of 15 to 40 degrees southwest into the face. <br />Foliation spacing averages approximately 4 inches and foliation apertures were <br />closed and smooth. The primary joint set strike ranges from 160 to 180 degrees <br />and generally dips from 45 to 80 degrees northeast out of the highwall. The <br />secondary joint set strike ranges from 250 to 270 degrees and generally dips 60 <br />to 85 degrees southeast. The spacing from joint set one averaged <br />approximately 36 inches. The spacing on joint set 2 varied widely, but <br />averaged approximately 8 inches. The apertures of both joint sets were <br />generally closed to moderately open and slightly rough. Due to the moderately <br />to highly fractured nature of the rock, raveling is to be expected in this area. <br />Raveling from this zone should be retained on the bench below the highwall <br />and is anticipated to cause only local operational delays. <br />Figure 6 is a photo documentary of the features observed in Bench 6880. <br />The only mining that occurred in 2009 on Bench 6820 removed the highwall observed last <br />year between 2008 scanline stations 0+00 and 2+50. The removed area provides access for <br />a haul road, and there is no highwall remaining at this location, therefore no scanline was <br />conducted on this bench. Figure 7 shows the current conditions at this location. <br />The Bench 6760 scanline was approximately 1360 feet long and was separated into 5 <br />discrete sections. The approximate orientation of the highwall observed is approximately <br />east-west for stations 0+00 through 2+15 and 5+70 through 8+25 and approximately north- <br />south for stations 2+15 through 5+70 and 8+25 through 13+60. The material in the <br />highwall from station 8+25 to 13+60 is material that is in the process of being mined. <br />Stations 0+00 through 0+90 consisted of highly fractured and weathered <br />granitic gneiss. The strike of the foliation varies due to minor folding and <br />ranges from 220 to 245 degrees. Foliation dips range from 20 to 30 degrees <br />southeast. The average spacing of the foliation was approximately 4 inches and <br />the foliation displays slightly rough to rough surfaces with apertures that are <br />generally tight. Due to the highly fractured nature of the rock and inconsistent <br />joint pattern in this area, only one prominent joint set was observable. This <br />joint set strike ranges from 195 to 205 degrees and generally dips from 70 to 80 <br />degrees southeast. The joint set average spacing was 6 inches and exhibited <br />closed, rough faces. <br />-5- <br />Morrison Quarry Annual Report 2009 February 2010 <br />P:\23514\133-23514-10003\Deliverables\Deliv-0l-Annual Report\Annual_Re[rort_2009_Geotech, 1-25-IO.doc