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widely variable, but ranged from low to medium. Apertures of the joints were <br />moderately open to tight with slightly rough to rough surfaces and were <br />moderately to slightly weathered. The second primary joint set exhibited a strike <br />ranging from 270 degrees to 275 degrees with dips ranging close to 90 degrees. <br />This joint set had similar properties to primary joint set 1— poor to very poor RQD, <br />moderately spaced joints, low to medium persistence, moderately open to tight <br />joint apertures, and slightly rough to rough rock surfaces, and moderate to slight <br />weathering. Foliations exhibited a strike ranging from 180 degrees to 230 degrees <br />with dips ranging from 55 degrees to 75 degrees. The spacing between of the <br />foliation varied, but was typically moderate to close. The persistence of the <br />foliation was also widely variable, but ranged from medium to high. Apertures of <br />the foliation were very moderately open to tight with slightly rough to rough <br />surfaces and were moderately to slightly weathered. <br />Small blocks may form in this area due to the orientation of the highwall and joint sets of the <br />rock. In addition, due to the fractured nature of the rock and highwall weathering, raveling of <br />small to medium sized rocks can also be expected. These rocks resulting from block <br />formation and raveling are anticipated to be limited in size, and should be retained on the <br />bench below the highwall and only cause local operational delays. <br />Sta. 3 +20 to 4 +60 consisted of primarily of granitic and biotitic gneiss with <br />localized pegmatite intrusions. Rocks observed within the highwall typically <br />exhibited medium high to high compressive strength (estimated) and poor quality <br />RQD. The trend of the highwall was 355 (north 5 degrees west). Two primary joint <br />sets were evident. The first set exhibited a strike ranging from 0 degrees to 180 <br />degrees with dips ranging from 75 to 85 degrees. The spacing between of these <br />joints varied, but was typically close to moderate. The persistence of the joints was <br />also widely variable, but ranged from low to medium. Apertures of the joints were <br />open to moderately open with slightly rough to rough surfaces and were highly to <br />moderately weathered. The second primary joint set exhibited a strike ranging <br />from 75 degrees to 275 degrees with dips ranging from 80 degrees to 90 degrees. <br />This joint set had similar properties to primary joint set 1— poor quality RQD, <br />moderately spaced joints, low to medium persistence, open to moderately open <br />joint apertures, and slightly rough to rough rock surfaces, and high to moderate <br />weathering. Foliations exhibited a strike ranging from 195 degrees to 350 degrees <br />with dips ranging from 10 degrees to 70 degrees. The spacing between of the <br />foliation varied, but was typically close to moderate. The persistence of the <br />foliation was also widely variable, but ranged from medium to high. Apertures of <br />the foliation were very open to tight with slightly rough to rough surfaces and were <br />highly to moderately weathered. <br />Small blocks may form in this area due to the orientation of the highwall and joint sets of the <br />rock. In addition, due to the fractured nature of the rock and highwall weathering, raveling of <br />GEI Consultants, Inc. 17 January 2014 <br />2013 Morrison Quarry Annual Report <br />