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below the highwall. Due to the moderately to highly fractured nature of the rock, raveling is to <br />be expected in this area. Raveling from this zone should be retained on the bench below the <br />highwall and is anticipated to cause only local operational delays. <br />• Stations 14 +95 through 17 +90 consisted of highly to moderately fractured granitic <br />gneiss. The foliation strike varies in this area due to minor folding and ranges from <br />80 to 350 degrees. Foliation dips ranged between 10 and 35 degrees southeast. <br />Foliation spacing ranges approximately from less than 2 inches to approximately 1 <br />foot, and foliation apertures were moderately open to very wide and slightly rough to <br />rough. The primary joint set strike ranges from 250 to 265 degrees and generally dips <br />from 80 to 85 degrees southeast. A second primary joint set is evident in this area <br />and exhibits a strike of 140 to 150 degrees with a dip of 60 to 65 degrees northeast. <br />The spacing of the primary joint sets varied widely, but averaged approximately 6 <br />inches. Joint apertures were moderately open to very wide with slightly rough to <br />rough faces. <br />• A secondary joint set is evident in this area and exhibits an average strike of 125 <br />degrees with an average dip of 25 degrees northeast. The spacing of the secondary <br />joint set varied, but averaged greater than 6 feet. Joint apertures were moderately <br />open with slightly rough to rough faces. <br />• The highwall in this area appears to be nearing the shear zone, as evidenced by the <br />appearance of slightly altered granitic /sillimanitic in the lower portions of the <br />highwall near stations 15 +50 to 16 +50. <br />Small blocks may form in this area due to the orientation of the highwall and jointsets of the <br />rock. These blocks are anticipated to be limited in size, and should be retained on the bench <br />below the highwall. Due to the moderately to highly fractured nature of the rock, raveling is to <br />be expected in this area. Raveling from this zone should be retained on the bench below the <br />highwall and is anticipated to cause only local operational delays. <br />• Stations 17 +90 through 19 +60 consisted of highly to moderately fractured granitic <br />gneiss. The foliation strike varies in this area due to minor folding and ranges from <br />10 to 15 degrees. Foliation dips ranged between 20 and 30 degrees northwest. <br />Foliation spacing ranges approximately from less than 2 inches to approximately 1 <br />foot, and foliation apertures were moderately open to open and slightly rough to <br />rough. The primary joint set strike ranges from 145 to 170 degrees and generally dips <br />from 65 to 80 degrees northeast. A second primary joint set is evident in this area and <br />exhibits a strike of 60 to 75 degrees with a dip of 85 to 90 degrees northwest. The <br />spacing of the primary joint sets varied widely, but averaged approximately 6 inches. <br />Joint apertures were moderately open to open with slightly rough to rough faces. <br />Small blocks may form in this area due to the orientation of the highwall and jointsets of the <br />rock. These blocks are anticipated to be limited in size, and should be retained on the bench <br />below the highwall. Due to the moderately to highly fractured nature of the rock, raveling is to <br />10 <br />Morrison Quarry Annual Report 2012 <br />P \23514 \133- 23514- 13002\Dehverables\Dehv -01 -2012 Annual Report \Annual_Report_2012_Geotech doc <br />January 2013 <br />