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0 , PROJECT: Morrison South Quarry LOG OF BORING 2007 PI1-1 <br /> Exploration <br /> GE1 Consultants <br /> PROJECT NO. SHEET 1 OF 13 <br /> Location South quarry Date(s) Drilling Bearing <br /> N 1653333.973 E 3082634.092 Drilled 7/12/2007 - 7/12/2007 Contractor Spectrum Exploration (Azimuth) NA <br /> Ground Surface 7027.31 NAVD88 Logged Thomas Clifford/ Drill Rig - Plunge 90 <br /> Elevation(ft) � byAdr Type (Degrees) <br /> an Charters <br /> Borehole Fluid Depth(ft) Reviewed Core Total 500.0 <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 W J 0 Z J = 0 of l L 0 0 0 <br /> Box <br /> _ � Low grade gneiss(migmatite)/high grade psammite(low quartz and <br /> - abundant muscovite suggesting highly metamorphosed sediments). <br /> • Stratified pink and very dark brown to black,medium grained with fine <br /> micro banding.Basic mineralogy of predominantly quartz,rose quartz, <br /> feldspars,and other high silica minerals,interstratified with thin(typical <br /> 1/16")dark dull accessory minerals displaying softer mineral <br /> _ characteristics(black micas-biotite).White micas also present <br /> throughout matrix's.The core is strong to very strong breaking <br /> 5 preferentially along micro dark gneiss-o-banding/disturbed <br /> metamorphosed laminations.The core is fresh and persistently fractured <br /> by sub horizontal,45 degree and sub vertical sets,slightly rough locally <br /> 1 13.0 11.7 - NA 90 NA smooth.Thin quartz veins and bands are common throughout along with <br /> an isolated pegmatite vain at 10'(1/2'thick).The pegmatite vain is <br /> predominantly quartz however porphyroblasts of dark mica(biotite)are <br /> --" present(1/3 In in diameter). <br /> 10 <br /> = Pegmatite vain-Mottled pink with occasional colorless white very <br /> Box = coarse crystals,predominantly quartz and feldspars.Veins are strong to <br /> very strong but fail on 45 degree superficially stained(iron)micro <br /> Box fractures. <br /> z Core as above.Material has been removed for testing-but looks <br /> comparable to above.High core loss-probable fracture zone at 14'and <br /> 15 17'. <br /> 2 7.5 6.0 - - - NA 80 NA = <br /> 20 = <br /> Alteration zone-dull dark metallic gray fine crystalline un-stratified <br /> 3 1.5 1.2 NA 80 NA _ moderately weathered zone.There is an abundance of micas both white <br /> and dark(muscovite and biotite)and other weak accessory minerals. <br /> The core is moderately strong but becomes weaker on water. <br /> 4 3.0 1.8 - - - NA 60 NA =' As 13-20.5' <br /> Box <br /> 2 <br /> 25 <br /> eox Box tested,sample and photo comparable to above. <br /> 3 <br /> _ I <br /> _ I <br /> - I <br /> - I <br /> 5 9.0 9.5 NA 106 NA <br /> 30 <br /> _ o <br /> = I <br /> - I <br /> - I <br /> Box = _ <br /> 3 <br /> Box _" As 13-20.5,formation is well horizontally stratified,locally disturbed <br /> 35 a with isolated biotite fine porphyroblasts throughout the core.A <br /> reduction in white mica(muscovite)has been observed.Core is very <br /> strong,fresh with occasional 45 degree slightly rough to smooth iron o <br /> 6 9.5 9.0 NA 95 NA stained(earthy yellow)fractures.Possible fracture zone from 34-35' N <br /> (high core loss). <br /> - J <br /> _ I <br /> _ I <br /> 40 <br />