Laserfiche WebLink
0 , PROJECT: Morrison South Quarry LOG OF BORING 2007 PI1-2 <br /> Exploration <br /> GE1 Consultants <br /> PROJECT NO. SHEET 1 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 a) 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 /> 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 <br /> locally fine micro banding.Basic mineralogy of predominantly quartz, <br /> rose quartz,feldspars,and other high silica minerals,interstratified with <br /> thin(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 locally very strong breaking <br /> 5 1 10.0 3.0 NA 30 NA preferentially along micro dark gneiss-o-banding/disturbed <br /> metamorphosed laminations.The core is also slightly weathered with <br /> superficial partially oxidized Iron staining(earthy yellow)on fractures. <br /> The core is persistently fractured by sub horizontal,45 degree and sub <br /> vertical sets,slightly rough locally smooth,the fractures have some clay <br /> filling from 0-Y. <br /> = I <br /> Note-Presumed 0'was bedrock and so even loss of core <br /> 10 = Coarse medium vertically micro to meso gneiss-o-banding,increased <br /> percentage of silica than above. <br /> Quartz vain,localized iron pyrites and clay on vain walls <br /> Coarse medium,locally fine medium,distorted micro to meso <br /> = gneiss-o-banding with occasional coarse(1/2 In)porphyroblasts of o <br /> quartz. <br /> = I <br /> 15 2 10.0 2.6 NA 26 NA = <br /> - I <br /> = I <br /> - I <br /> 20 = <br /> Strongly stratified dark thin(lmm)bands of weak accessory minerals I <br /> within high pink and colorless silica thicker bands(5mm).Core is strong <br /> = locally very strong breaking preferentially along darker thin bands.Core <br /> remains slightly weathered with Iron staining on slightly rough fracture <br /> 3 5.0 4.0 NA 80 NA _ surfaces.The reduction in core loss suggests a reduction in facture <br /> density. <br /> - I <br /> Box <br /> 25 1 _ <br /> Box �'" Very strongly stratified dark thin(lmm)bands of weak accessory <br /> 2 _- minerals within higher silica and accessory mineral silica thicker bands <br /> (5mm).The lithology is contains occasional thick(1")fine coarse <br /> crystalline bands.Core is very strong locally strong fresh with <br /> 4 5.0 6.5 NA 130 NA = occasional localized slightly weathered(Iron staining on slightly rough <br /> _ fracture surfaces)fractures from 25-27.5'.There is significant reduction <br /> in facture density. <br /> N <br /> 30 " <br /> Pink pegmatite vain-very high silica minerals,very coarse well <br /> interlocked crystals.Core is strong,fresh with a random orientation of <br /> 5 3.5 2.5 NA 71 NA fracturing. <br /> I <br /> Box <br /> 2 -_-" Very strongly stratified dark thin(lmm)bands of weak accessory <br /> Box minerals within higher silica and accessory mineral silica thicker bands <br /> 35 3 (5mm).The lithology contains occasional thick(1")fine coarse <br /> crystalline bands.Core is strong locally very strong fresh with <br /> occasional localized slightly weathered(Iron staining on slightly rough <br /> 6 12.0 10.3 - NA 86 NA fracture surfaces).An isolated 8'pegmatite vain is present and exhibits <br /> the same characteristics as above. <br /> 40 <br />