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' Gable, and strikes 260-270°, dips 80-85° to the south, and will continue to be <br />' exposed as the pit deepens (Figure 3). <br />' In the expansion area, Gable (1968) mapped a fault that also trends roughly east <br />to west and may form a structural block that results in distinguishable <br />' discontinuity clusters from the main part of the quarry. This fault was exposed <br />during the 2006 investigation, and is noted by a distinct pegmatite vein that is <br />' surrounded by decomposed weak biotite rich gneiss (Photo 2). The dip of the <br />fault zone is unknown at this time, but it is anticipated that we will obtain more <br />' information on the structural character of this feature as the mining progresses. <br />-6- <br />