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0 , PROJECT: Morrison South Quarry LOG OF BORING 2007 PH1-2 <br /> Exploration <br /> GE1 Consultants <br /> PROJECT NO. SHEET 3 OF 9 <br /> Location South quarry Date(s) Drilling Bearing <br /> N 1653268.842 E 3083230.031 Drilled 7/11/2007 - 7/11/2007 Contractor Spectrum Exploration (Azimuth) NA <br /> Ground Surface 6941.08 NAVD88 Logged Thomas Clifford/ Drill Rig - Plunge 90 <br /> Elevation(ft) � byAdr Type (Degrees) <br /> Borehole Fluid Depth(ft) Reviewed Core Total 350.0 <br /> and(Date Measured) NA by - Diameter(in) NQ Depth(ft) <br /> CORING (SEE LEGEND) <br /> n n° rn <br /> = MATERIAL CO <br /> oco <br /> m DESCRIPTION <br /> U N i O U) <br /> O � Iq a) N E E . 0_' O tl5 C C J > a) <br /> LLl Z N 0_' 0_ O a) N d O O �O .�. <br /> N O 3 N a) — O 0 O N N_ N_ U <br /> 0 Z 0 0 d J 0 Z J = 0 of rL 0 0 0 <br /> 80 / <br /> 12 4.0 4.0 NA 100 NA <br /> Quartz vain <br /> Shear zone-highly fractured weak core with an abundance of weak <br /> accessory minerals,clearly visible fine crystals of dark and white micas. <br /> 13 4.0 3.5 NA 88 NA Y Well stratified dark thin(lmm)bands of weak accessory minerals within <br /> / higher silica and accessory mineral silica thicker bands(5mm).Core is <br /> Box / strong locally very strong,fresh with occasional localized slightly <br /> 85 7 weathered smooth fractures of predominantly 45 degrees and sub <br /> Box horizontal. <br /> B // Occasional coarse(10mm)quartz crystals zones.Core is very strong <br /> locally strong,predominate sets of slightly rough to smooth 45 degree, <br /> sub vertical and sub horizontal fracturing with iron staining on walls. <br /> / I <br /> I <br /> I <br /> / o <br /> 90 <br /> 14 11.0 9.7 - - - - NA 88 NA N <br /> i <br /> 0 <br /> I <br /> I <br /> / I <br /> / I <br /> 95 Box / <br /> B <br /> Box Core is locally medium coarse,strong often very strong with an increase <br /> s in fracture density.The fractures are slightly rough to smooth with <br /> predominate sets at 45 degrees,sub vertical and sub horizontal.The <br /> fractures have iron staining(earthy yellow)upon the walls.Vertical iron <br /> strained fractures are present however the core remains in tacked and <br /> / does not tend to fail upon this orientation. <br /> Quartz vein at 98.2-98.5 <br /> 100 0 <br /> N <br /> 15 10.0 8.3 - - - NA 83 NA / N <br /> I <br /> / I <br /> I <br /> 105 Box / <br /> s <br /> Box Local coarse zones of high silica minerals(quartz),deduction in fracture <br /> 10 / density however localized zones(1/2')still present.Fractures are <br /> predominantly smooth to slightly rough sub vertical.Core is strong to <br /> very strong,fresh with localized(fracture wall)iron staining). <br /> / <br /> 110 <br /> 16 9.7 10.5 - NA 108 NA / <br /> Box / <br /> io <br /> Box <br /> 115 11 / <br /> Quartz vain at 115.5-115.7 <br /> Core is clearly fractured producing large fragments that are strong and <br /> slightly weathered.The core varies from coarse to fine grain size which <br /> suggests a shift to meta-sediments.Large dark mica(biotite)books <br /> 17 9.3 8.0 NA 86 NA (large porphyroblasts)are present at 122'-123'. <br /> / Fractured zone <br /> 120 <br />