report on exploration by mega uranium ltd. on the ... · greenwich lake 4244236 2008-nov-28...

REPORT ON EXPLORATION

BY MEGA URANIUM LTD.

ON THE GREENWICH LAKE PROPERTY,

GREENWICH LAKE AREA,

NTS MAP SHEET 52A/15

NORTHWESTERN, ONTARIO

THUNDER BAY MINING DIVISION

Tony Gilman, M.Sc., P.Eng., Mega Uranium Ltd. April, 2010

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TABLE OF CONTENTS Page Table of Contents ……………………………………………………….. i List of Figures …………………………………………………………... ii List of Tables …………………………………………………………… ii List of Plates ……………………………………………………………. ii List of Maps …………………………………………………………….. ii Summary ………………………………………………………………... 1 1.0 Introduction …………………………………………………………….. 3 2.0 Property Description and Location …………………………………….. 3 3.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography 6 4.0 Geological Setting ……………………………………………………. 7 4.1 Regional Geology and Exploration Potential ………………….. 7 4.2 Property Geology ……………………………………………… 10 5.0 Previous Work ………………………………………………………… 14 5.1 Exploration Prior to East West/Mega …………………………. 14 5.2 Exploration by East West/Mega Previously

for Uranium ………………………………………..……….. 14 6.0 2009 and 2010 EXPLORATION - MEGA URANIUM LTD……… 16 6.1 Prospecting Program Summer 2009 ………………….…….. 16 6.2 Diamond Drill Program Winter 2010 ………………………… 19 6.2.1 Diamond Drill Core Sampling and QA/QC…………… 19 6.2.2 2010 Greenwich Lake Diamond Drill Program Results.. 19 7.0 Conclusions and Recommendations.…………………………………. 22 8.0 References ………………………………………………………………. 24 Appendix A: Certificates of Qualifications Appendix B: Certificates of Assay Appendix C: Prospecting Database Appendix D: Drill Logs and Drill Sections

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LIST OF FIGURES Page 1. Location of the Greenwich Lake Property …………………………….. 4 2. Claims Comprising the Greenwich Lake Property ……………………… 4 3. Regional Geology of the Lake Superior Area …………………………. 8 4. Regional Geology of the Greenwich Lake Area ………………….…… 9 5. Regional Geology of Mid-Continental North America ……………… 11 6. Geology of the Greenwich Lake Property …………………………… 12 7. Drill Holes on the Greenwich Lake Property ……………………….… 13 8. 2009 Prospecting Program – Magnetic Anomalies Traversed and Sample Locations……………………………………………………………. 17 9. 2009 Prospecting Program – Sample Locations and Results…………. 18 10. 2010 Diamond Drillng Program – Drill Hole Locations…………. .. 23 LIST OF TABLES Page 1. Claims Comprising the Greenwich Lake Property.…………………… 6 2. 2010 Greenwich Lake Diamond Drill Hole Locations ……………….. 20 LIST OF MAPS (in pocket) 1. Claims Comprising the Greenwich Lake Property 2. Location of Waypoints and Samples on the Greenwich Lake Property 3. 2010 Diamond Drill Program – Drill Hole Locations

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SUMMARY The Greenwich Lake property is owned 100% by Mega Uranium Ltd. The property was previously held 50% by Mega Uranium Ltd. and 50% by East West Resources Inc. (now Rainy Mountain Royalty Corp.) but East West Resources transferred its 50% share to Mega Uranium Ltd. in 2008. The property is located in 1:50,000 NTS sheet 52A/15 in the Greenwich Lake area of northwest Ontario, 55 km northeast of the city of Thunder Bay. The property is located in the Thunder Bay mining division and consists of 16 claims for a total of 141 claim units covering a surface area of 2256 ha. The Greenwich Lake property occurs in the Superior province of the Canadian shield and is underlain by migmatites, granites, and orthogneisses of the Quetico Subprovince. Rocks of the Quetico Subprovince are cut by later Mesoproterozoic Keweenawan mafic intrusions which are considered prospective for Ni, Cu, PGE mineralization. Such Keweenawan mafic to ultramafic intrusions host the nearby (4 km west) Thunder Bay North Deposit currently held and being explored by Magma Metals Ltd. In 2006 through 2008 Mega Uranium and East West Resources (now Rainy Mountain Royalty Corp.) carried out a radiometiric, VLF-EM, & magnetic airborne survey, trenching, and prospecting to evaluate the Greenwich Lake property’s uranium potential. It was concluded that most of the radiometric anomalies on the property were due to pegmatite dikes with radioactivity somewhat higher than background. After completing a final uranium-focused prospecting program in 2008, Mega concluded that the uranium potential of the Greenwich Lake property was not worth pursuing. The recent discovery by Magma Metals Ltd. of a high grade Ni, Cu, PGE deposit, the Thunder Bay North deposit, has turned this area into an emerging Ni, Cu, PGE camp. Given the Greenwich Lake property’s proximity to the Thunder Bay North deposit (4 km to the west) a magnetic, and AeroTEM electromagnetic survey was flown by Aero Quest Ltd. in April, 2009. This survey was flown in an east-west flight direction as opposed to the previous survey which was flown in a north-south orientation. The east-west flight orientation allowed for a better evaluation of the property’s potential to host north to northwest trending, sinuous magnetic highs similar to the magnetic signatures associated with the Thunder Bay North deposit. The Greenwich Lake property was found to host several north to northwest trending magnetic features, which have been the focus of 2009/2010 work completed on the property. In August, 2009 a prospecting program was completed to follow up magnetic anomalies identified from the April, 2009 geophysical survey. The program focused on explaining any north to northwest trending magnetic anomalies, (magnetic highs and extreme magnetic lows) and extensive lake shore prospecting along the shores of Greenwich Lake. This program resulted in the collection of 28 samples of mafic intrusive rocks which returned Pt+Pd+Au values in 12 samples that ranged from 3 ppb to 143 ppb. The mineralization discovered during the prospecting program, while weak, pointed to the possibility of compositionally prospective rocks on the property. The results of this prospecting program coupled with un-tested, co-incident magnetic and EM anomalies

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beneath Greenwich Lake led to the decision to complete a diamond drill program on the property in February, 2010. In February and March of 2010 eight (8) diamond drill holes for a total of 1803 m were completed on the Greenwich Lake property. These drill holes were designed to test a series of sinuous approximately north-south to northwest-southeast trending magnetic highs, any co-incident EM anomalies, and nearby compositionally prospective grab samples collected during the 2009 prospecting program. Drilling in DDH GL-10-8 intersected 140 m of weak anomalous (above background relative to 248 samples of mafic material assayed on the property) Pt, Pd, and Au mineralization in a chlorite and hematite altered gabbro associated with a “bulls-eye” magnetic anomaly on the western portion of the property. Assay results from 31 samples (note the gabbro was sampled every 5 m) of the altered gabbro returned Pt+Pd+Au values ranging from 10 to 129 ppb. In addition to the positive results encountered in GL-10-8 two of our key targets below Greenwich Lake, defined by a co-incident, sinuous, electromagnetic (EM) and magnetic anomalies remain untested due to above-average winter temperatures in northern Ontario this past winter which cut the drill program short 3-4 weeks. After completing the initial drill program on the Greenwich Lake drill property, it is recommended that further work be completed to: 1.) adequately access the anomalous mineralization in GL-10-8 and GL-10-3, and 2.) thoroughly test the targets below Greenwich Lake.

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1.0 INTRODUCTION Mega Uranium Ltd. (Mega) owns 100% of the Greenwich Lake property in the Greenwich Lake area northwest Ontario (Fig. 1). The property was originally staked by East West Resources Corporation (now Rainy Mountain Royalty Corp.; Rainy Mountain) and explored by Rainy Mountain and later Mega for its perceived uranium potential. Exploration was not successful, but potentially economic Pt-Pd-Cu-Ni mineralization was encountered during recent exploration by Magma Metals Limited on a property immediately west of the Greenwich Lake property. A review of the geology, geophysics and regional structure of the Greenwich Lake property by Mega in April, 2009 suggested that this property might have the potential for Ni, Cu, PGE mineralization as well. This report describes work conducted in 2009 and early 2010 by Mega on the Greenwich Lake property. This work was conducted to evaluate the property’s Ni, Cu, PGE potential. The work described in this report includes prospecting completed in the fall of 2009 and diamond drilling completed in the winter of 2010. The 1983 North American Datum (NAD83) co-ordinate system is used in this report. The Greenwich Lake property is in Universal Transverse Mercator (UTM) Zone 16N. Assessment reports cited in the references are available on the website of the Ontario Ministry of Northern Development and Mines (www.geologyontario.mndm.gov.on.ca). The AFRI (Assessment File Research Imaging) number is provided wherever possible for each assessment report. All monetary figures quoted in this report are in Canadian dollars. 2.0 PROPERTY DESCRIPTION AND LOCATION The Greenwich Lake property consists of 16 claims totaling 141 claim units in the Greenwich Lake area in the Thunder Bay Mining division (Fig. 2; Table 1; Map 1). The claims are registered 100% to Mega (Table 1). The property was previously held 50% by Mega Uranium Ltd. and 50% by East West Resources Inc. (now Rainy Mountain Royalty Corp.) but Rainy Mountain transferred its 50% share to Mega Uranium Ltd. in 2008. The property is 2256 ha in surface area and is centered at approximately 0363000E, 5407000N (NAD 83 Datum, UTM Zone 16N) or 88º52’W/48º48’N (latitude/longitude) in National Topographic System (NTS) 1:50,000 map sheet 52A/15. The Greenwich Lake property consists of unpatented, unsurveyed claims, for which the mineral rights are 100% owned by Mega. The mineral rights give Mega the right to explore for ore on the claims, subject to a 400' surface rights reservation around all lakes and rivers, and a 300' surface reservation around major roads (this may be waived by the Crown). Unpatented claims require work expenditures of at least $400 per 16 hectare claim unit in the first two years, and $400 per year thereafter (by the anniversary of their recording date); all claims are in good standing at the time of writing (Table 1). There are no known mineral reserves on the property, and no environmental liabilities occurring to Mega.

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330000 340000 350000

Lake Superior

360000 370000 380000

Figure 1: Location of The Greenwich Lake Property NAD 83, UTM Zone 16N

a 2 4 8 12 16 __ -=:i-..:::::i. ___ i::::==::::i ___ Kilom eters

Legend

_ GREENWICH CLAIMS

5

360000 361000 362000 363000 364000

360000 361000 362000 363000 364000

Figure 2: Claims Comprising the Greenwich Lake Property

365000

4244233

365000

366000

u o o o

, ~

1 1.5 2 Kilometersl

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Table 1: Claims Comprising the Greenwich Lake Property

Township/Area Claim Number

Recording Date

Claim Due Date

Registered Ownership

Claim Units Area (ha)

GREENWICH LAKE 3014745 2004-Nov-09 9-Nov-10 100 % 4 64 GREENWICH LAKE 3014754 2004-Nov-09 9-Nov-10 100 % 8 128 GREENWICH LAKE 4207834 2005-Jun-06 6-Jun-11 100 % 2 32 GREENWICH LAKE 4211690 2006-May-03 3-May-10 100 % 10 160 GREENWICH LAKE 4211691 2006-May-03 3-May-10 100 % 4 64 GREENWICH LAKE 4211692 2006-May-03 3-May-10 100 % 16 256 GREENWICH LAKE 4211693 2006-May-03 3-May-11 100 % 8 128 GREENWICH LAKE 4211694 2006-May-03 3-May-12 100 % 2 32 GREENWICH LAKE 4211695 2006-May-03 3-May-14 100 % 1 16 GREENWICH LAKE 4244231 2008-Nov-28 28-Nov-10 100 % 16 256 GREENWICH LAKE 4244232 2008-Nov-28 28-Nov-11 100 % 16 256 GREENWICH LAKE 4244233 2008-Nov-28 28-Nov-11 100 % 16 256 GREENWICH LAKE 4244234 2008-Nov-28 28-Nov-11 100 % 16 256 GREENWICH LAKE 4244235 2008-Nov-28 28-Nov-15 100 % 3 48 GREENWICH LAKE 4244236 2008-Nov-28 28-Nov-11 100 % 16 256 GREENWICH LAKE 4244237 2008-Nov-28 28-Nov-11 100 % 3 48 Total 141 2256 3.0 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY The Greenwich Lake property is accessible via two main routes; 1.) Escape Lake road off of Highway 527 will provide access to the western portion of the property, and 2.) The Greenwich Lake road accessible off of Ouimet Canyon Provincial Park road will provide access to the eastern portion of the property (Fig. 1). Off of either Escape Lake road or Greenwich Lake road a series of narrow logging roads provide access into the property. At the southern end of Greenwich Lake a small walking/ATV trail provides access to Greenwich Lake itself. Most of the property can be accessed via a small boat or canoe on Greenwich Lake. The property is 55 km northeast of Thunder Bay, a city with a long history of mining and home to personnel with the skills to work in the mining industry. Water is abundant in the region, and the property contains gravel roads which could be upgraded to all-weather status if necessary. Suitable locations for constructing mineral processing facilities are abundant on the property. The climate of the project area is continental in nature, with cold winters (-10 to -35C) and warm summers (+10 to +35C). Seasonal variations affect exploration to but the climate would not significantly hamper any mining operations.

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The topography on the property varies from gently rolling hills with low lying swamps, bogs, and ponds to steep escarpments along the edge of Greenwich Lake. Elevation varies from 415 to 505 m above sea level. Approximately half of the property is underlain by the 10 km long, up to 850 m wide Greenwich Lake. In addition to Greenwich Lake several smaller lakes, ponds, and swamps occur on the property (Fig. 2; Map 1). However, the majority of the property is dominated by jack pine, aspen, and birch forest. Parts of the property have been logged recently and much of the present forest is second growth. The bulk of the property is covered by a thin till overburden at higher elevations and glacio-lacustrine sediments, and boulders along the shores of Greenwich Lake. The outcrop density on the property is highly variable with some locations being entirely sediment covered and others being nearly 100% outcrop. Overall the outcrop density of the entire property is approximately 15-30%. 4.0 GEOLOGICAL SETTING 4.1 Regional Geology and Exploration Potential The Greenwich Lake property is proximal to the Nipigon Plate, which defines an aulacogen (failed rift) off the main Mid-continent Rift (Franklin, 1982; Drost, 2001). The Mid-continent Rift is roughly coincident with Lake Superior and with the southern margin of the Archean Superior Province (Fig. 3). The Superior Province in this region is subdivided into the Abitibi, Wawa, Quetico, Wabigoon and English River subprovinces (Fig. 3). The Abitibi, Wawa and Wabigoon subprovinces are typical granite-greenstone subprovinces, whereas the Quetico and English River subprovinces are composed mainly of (metamorphosed) sediments, granites, and migmatites (Thurston, 1991). The Nipigon Plate/aulacogen is younger and cross-cuts all the geological subprovinces mentioned above. The basin (Sibley Basin) associated with this rift served as a locus for sedimentation at approximately 1340 Ma, and was reactivated as a locus for magmatism at approximately 1100 Ma, during the main (Keweenawan) igneous events associated with the Mid-continent Rift.

The 1340 Ma Sibley Group, dominated by conglomerates, red bed sandstones, and calcareous sandstones is preserved within the aulacogen (Fig. 4). This may be due to early movement along the rift-bounding fault system (Franklin et al., 1980) or sagging of Middle Proterozoic crust in this region (Cheadle, 1986). The group is interpreted to have been deposited in an alluvial-playa lake to evaporative environment (Cheadle, 1986). Sibley Group sediments outcrop extensively in the southern part of the aulacogen (Fig. 4), but have also been intersected in drill holes in the northern part, where they are covered by Nipigon sills (East West Resource Corporation web site). The 1100 Ma Keweenawan Supergroup was deposited within the Mid-continent Rift (Sutcliffe, 1991). The lower part of the supergroup is dominated by subaerially extruded basalts, with lesser rhyolites (Green, 1977; Sutcliffe, 1991), and the upper part is comprised mainly of sandstone, shale and conglomerate. Mafic magmas such as the Duluth Complex, the Logan Sills and the Nipigon Sills form the bulk of the Keweenawan intrusive magmatism. The aulacogen served as the locus for intrusion of Nipigon sills (and associated Keweenawan mafic intrusive) during the Mesoproterozoic (Fig. 4).

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Figure 4: Regional Geology of the Greenwich Lake Area 300000 320000

Proterozoic

~ Nipigon Sills

5440000 ~ Sibley Group

Archean

5420000

5400000

5380000 J:i,i"::f.~,<.>./.:>

340000 360000

Modified After Ontario Geological Survey 199

300000 320000 340000 360000

380000 400000 420000

+

o 10 20 Kilometers

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5420000

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5380000

9

\ \

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o

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Great Lakes Tectonic Zone

200 I

km I

urray Fau System

Abitibi Subprovince

Grenville Province

Figure 3: Regional geology of Lake Superior Area, modified after Thurston (1991). NP: Nipigon Plate; red dot is the location of the Greenwich Lake property.

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The Sibley Basin is considered prospective for uranium deposits based on it tectonic similarities with the Athabasca Basin, and the presence of numerous uranium showings within and adjacent to the Sibley Basin (Scott, 1987). The basin underwent a staking rush for uranium in 2006 (www.bentonresources.ca, 2010). The Greenwich Lake property is approximately 6 km west of the nearest mapped occurrence of Sibley Group sediments (Fig. 4). Given the Greenwich Lake property’s proximity to a portion of the Mid-continent Rift, the property may have potential for magmatic metal (Keweenanwan intrusive related) deposits. The mafic to ultra-mafic magmatism that accompanies such large scale intra-crustal continental rifting events is responsible for the majority of the world’s Ni-Cu-PGE deposits. Notably the world’s largest Ni-Cu-PGE deposit, Noril’sk, in Siberia, is found within such an intra-crustal rifting site known as the Siberian traps (Eckstrand and Hulbert, 2007). Figure 5 shows the location of the Greenwich Lake property in relation to the major Ni-Cu-PGE deposits in the Mid-continent Rift. There are five major deposits shown on this figure: 1.) North American Palladium’s Inc., Lac De Iles Mine (currently placed on care and maintenance); 2.) Marathon PGM Corp., Marathon Deposit; 3.) Duluth Metals Inc., Duluth Deposit; 4.) Kennecott Minerals Inc., Eagle deposit; and 5.) Magma Metal’s Inc., recently discovered Thunder Bay North deposit. The Thunder Bay North deposit is adjacent (4 km to the west) to the Greenwich Lake property. Recent press releases by Magma Metals Inc. (www.magmametals.com.au, 2010) report 44.65 m grading at 5.50 g/t Pt, 4.75 g/t Pd, 1.2% Cu, and 0.49% Ni, including 2.6 m grading 52.77 g/t Pt, 41.54 Pd, 11.6% Cu, and 3.29% Ni. 4.2 Property Geology A large area including the Greenwich Lake property was mapped by Carter (Fig. 6; 1979 adapted), who determined the property to be underlain by east-trending migmatites derived from sediments (wackes), in contact with variably metamorphosed and migmatized Archean monozonites to granite. These rocks form part of the Quetico Subprovince (Fig. 3), and are intruded by north to northwest-trending diabase dikes, possibly associated with the Keweenawan age Nipigon sills as discussed above. Historically the main feature of economic interest on the property was the Christianson showing, which occurs within the north-northwest trending Christianson Fault (Fig. 7). The fault contains fault breccia, including clasts of Sibley Group sediments, along with abundant radioactive pyrite (Scott, 1987). However, the focus on the property has switched to Ni, Cu, PGE potential associated with geophysical signatures that suggest the property may host north to northwest trending Keweenawan mafic to ultramafic intrusive.

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,-________ --, Mid-Continent Rift Simplified Geology CANADA

WdegN

North Ameri can Palladium Lac des lies Mine [email protected] Pd(Open Pit) 14mt@5 .3gA Pd(Undeground)

Magma Metals In c. Thunder Bay North Deposit

Duluth Metals Duluth Deposit 449Mt @O.6% Cu, 0 .2% Ni & 0 .6 gA Pt+Pd+Au

45degN

U.S.A

200 km

~degW

Marath on PGM Corp. Marath on Deposit 81 [email protected] gl1: Pt+Pd+Au & 0.3% Cu

Greenwich Lake Property

Kennecott - Eag le Deposit 3.6 Mt @ 3.8% Ni, 3 .0% Cu & 1.6 glt Pt+Pd+Au

......-::...--. "~---,---------' H "-'-- ' '-''',

D Sediments

II Volca nics

............. Major Faults

Figure 5: Regional Geology of Mid-Continental North America displaying Major PGE, Ni-Cu deposits and generalized Geology. Figure adapted from Magma Metals Inc.

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, ------------- , ----------- -----, ---

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Legend

- _ Inle<p'eted Fautt.

- - - - InICfp'eted Corrtaol.

C:=J Greerl'Mch Uioke Propeny

~ Diabase Dike

362000 363000 364000 365000 366000 367000

Figure 6 : Geology of Greenwich Lake Property Geology digitized from Ontario Geological Survey Preliminary Map P.2249, Geology Greenwich Lake Area.

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Figure 7: Historical Drill Holes on the Greenwich Lake Property 358000 360000 362000

• Drill Hole

\ Christianson Fault

5412000 ''T-\------~m~

" .. ·· r ); 5408000 + + ~

Uvinex ~~/ Ho I es '-ll-.l- -.Io

5406000 + +

5404000 +

5402000 + +

Drill Hole Locations from MNDM Database

+

358000 360000 362000

364000 366000

+~

+ 1 o

364000 366000

368000

Property Boundary

+ 1 2 Kilometers

368000

5412000

5410000

5408000

5406000

5404000

(

5402000

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5.0 PREVIOUS WORK 5.1 Exploration Prior to East West/Mega In 1921 T.L. Tanton discovered a vein described as containing quartz, marcasite and galena near the western shore of the southwestern part of Greenwich Lake. In 1949 T. Christianson discovered radioactivity in this vein, which subsequently became known as the Christianson Fault (Carter, 1983). In 1954, Pan Canadian Development Co. Limited drilled 16 holes totaling 402 m on the Christianson Fault (Ager, 1954). Best results were 3’ of 0.5% U3O8 and 3.25’ of 0.8% U3O8. Univex Exploration and Development Corporation flew a radiometric survey over much of the present Greenwich Lake property in 1969 (Oja, 1969). They drilled holes G-1 to G-14, G-36 to G-41 G-57 to G-60 and P-1 to P-6 in 1969 and 1970 for a total of 1290 m (Chisolm and Oja, 1970; Oja, 1970). These holes are mainly drilled in the north-central part of the present property (Fig. 7), and are not well documented. Consolidated Monarch Metals Limited drilled holes 75-1 to 75-6 on the Christianson Fault in 1975 for a total of 405 m (Heshka, 1975a; b). No anomalous uranium was encountered. In 1976, Rio Tinto investigated a block of ground that comprises the southern third of the present Greenwich Lake property (Benkis, 1977). They were most interested in the potential of pegmatite dikes that they mapped, and that intrude both the felsic intrusives and the migmatized sediments on the property. They mapped the property, conducted a scintillometer survey, blasted 14 trenches and drilled holes RTG1 to RTG3 for a total of 506 m. Anomalous but not economic uranium values were encountered during drilling (Benkis, 1976a; b). In 1978, Greenwich Lake Exploration Ltd drilled 21 holes totaling 1227 m in the southern part of the Greenwich Lake property, and excavated 31 trenches (Christianson and Fairbairn, 1978a; b). This work is not well documented. They commissioned a TURAM and an IP survey in 1979 (Webster, 1979). In 1982, Greenwich Lake Exploration Ltd drilled hole 82-1 near the Christianson Fault, but ran out of funding before the fault could be intersected (Fairbairn, 1982).

5.2 Exploration by East West/Mega Previously for Uranium East West and Mega originally acquired the Greenwich Lake property because of its perceived uranium potential. An Athabasca Basin model was favored-the property had three major attributes: i) its proximity to the presently exposed Sibley Basin; ii) the recorded occurrence of Sibley Group clasts in the Christianson Fault, suggesting that the basin covered the property prior to recent erosion; and iii) the structurally controlled Christianson showing.

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East West/Mega commissioned Terraquest Ltd to fly a magnetic/VLF-EM/radiometric survey over the entire property (Barrie, 2007; property was larger than the present property). The survey was completed on 100 m spaced, north-south flight lines in November, 2006. The magnetic data is dominated by east-northeast trending linear anomalies which have been interpreted as corresponding to the east-northeast striking migmatites, granites, and orthogneisses of the Quetico Subprovince The radiometric data showed a number of discrete total count radiometric anomalies. East West/Mega excavated eight trenches in 2007 to test total count radiometric anomalies and magnetic highs (East West was the operator). Nothing of significance was found in the trenches. Mega took over owner-ship of the Greenwich Lake property in 2008. In addition to compiling recent work on the property, Mega reprocessed the geophysical data to produce an eU/eTh (Equivalent Uranium/Equivalent Thorium) map. The eU/eTh ratios are commonly considered to reflect the amount of hydrothermal uranium present in any one area. It was apparent that the neither the 2007 trenching nor the historical drilling had sufficiently tested the eU/eTh anomalies. The decision was thus made to field check several eU/eTh anomalies. One day was spent examining eU/eTh anomalies in the field in the southern part of the property. A selection of anomalies of variable strength was visited. The rock type encountered in the field varied from migmatite (apparent melted sediment) to granitoid. The background radiometric readings were on the order of 200 counts per second (cps). Pegmatite dikes with readings up to 3,000 cps were present locally. Other eU/eTh anomalies are also associated with zones of above background radioactivity, justifying the use of this processing technique as an exploration tool. However, the eU/eTh anomalies were found to be caused by pegmatite/coarse-grained granitoids with levels of activity that were not economically significant. Two samples were taken-sample GR487 from the pegmatite dike with the highest reading encountered (waypoint 386), and sample GR488 from the Christianson showing (waypoint 387). Sample GR487 returned a U value of 12.5 ppm, and sample GR488 had a U value of 7.6 ppm (Appendix B). In view of these disappointing assay values and the general lack of extensive zones of significant radioactivity, Mega has concluded that the uranium potential of the Greenwich Lake property is not worth pursuing. 5.3 Property Evaluation by Mega for Ni-CU, PGE Potential The recent discovery by Magma Metals Ltd. of a high grade Ni, Cu, PGE deposit, the Thunder Bay North deposit (TBN), has turned this area into an emerging Ni, Cu, PGE camp. Given the Greenwich Lake property’s proximity to the Thunder Bay North deposit (4 km to the west) a magnetic, and AeroTEM electromagnetic survey was contracted to Aero Quest Ltd. in April, 2009. This survey was flown in an east-west flight direction as opposed to the previous survey by Terraquest which was flown in a north-south orientation. The east-west flight orientation allowed for a better evaluation of the

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property’s potential to host north to northwest trending, sinuous magnetic highs and magnetic lows similar to the magnetic signatures associated with the Thunder Bay North deposit. The Greenwich Lake property was found to host several similar north to northwest trending magnetic features. These magnetic anomalies have been the focus of 2009/2010 work completed on the property. 6.0 2009 and 2010 EXPLORATION - MEGA URANIUM LTD. 6.1 Prospecting Program Summer 2009 In August, 2009 a prospecting program was completed to follow up magnetic anomalies identified from the April, 2009 geophysical survey. The program focused on explaining any north to northwest trending magnetic anomalies, (magnetic highs and extreme magnetic lows) and extensive lake shore prospecting along the shores of Greenwich Lake. The prospecting program was designed to traverse across any significant linear to sinuous magnetic anomalies identified from the 2009 geophysical survey. Additionally, all of the lake shore that falls within Mega’s claims along Greenwich Lake was prospected. The prospecting was carried out by one team of two; a geologist, and a prospector. The program was designed to traverse the anomalies by each person 100 m a part in at least one location. Figure 8 shows the GPS tracks associated with all traverses completed as part of this prospecting program and sample locations. In the vicinity of each anomaly any mafic material encountered either as a boulder or an outcrop was sampled. If no mafic material was encountered the anomaly was attempted to be explained by the outcrops in the vicinity of the anomaly. There were two main explanations for the magnetic anomalies prospected as part of this program; 1.) mafic material was encountered and was magnetic relative to the surrounding country rock, or 2.) the country rock (i.e the Quetico schist or the monozonites) contained fine grained magnetite in certain horizons making it magnetic relative to other rocks around it. Generally it was discovered that the north to northwesterly trending magnetic anomalies were associated with fine grained to coarse grained, black to green, non-foliated mafic intrusive units and the dominantly east west magnetic anomalies were stratagraphic anomalies related to the trend of the regional geology in the area. A database of all way points visited (Map 2), and samples taken along with descriptions are located in Appendix C. As a result of this prospecting program 27 samples of mafic material were collected on the property. The locations of these samples and the results of any anomalous Ni, Cu, PGE’s are shown on Figure 9 and Map 2. For the purposes of this program Pt+Pd+Au mineralization above 30 ppb was considered anomalous while Cu and Ni values greater than 200 ppm were considered anomalous. Of the 27 samples of mafic material taken on the property, 6 samples contained anomalous Pt+Pd+Au mineralization, 3 samples contained anomalous Ni, and 6 samples contained anomalous Cu. The analytical results are included in Appendix B, and a sample database can be found in Appendix C. The

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"""" """"

•

j

"5000 "7000

Legend

• 2009 Boulder Samples

• 2009 O utcrop S3mples

Daily_Tracks

-- Greenwich Lake Access Roads

c::J Green\o\lich Lake Property

c::::::::J Lakes 0.5

Figure 8 • 2009 Prospecting Program - Magnetic Anomalies Tra versed and Sample Locations. TMI Magnetics as Background Image. NAD 83, UTM Zone 16N

18

,

Legend

Cu_Above_200ypm

• Ni_Above_200....wm

• F't_Pd_Au_Above_30ypb

• 2009 Boulder Samples

• 2009 Outcrop Samples ....• Daily_Tracks

-- Greenwich Lake Access Roads c:::J Gr~nwich Lake Property

c::=J Lakes o 0.5

Figure 9 - 2009 Prospecting Program - Sample Locations and Results. TMI Magnetics as Background Image. NAD83. UTM Zone 16N

19

results of this prospecting program were used along with the magnetic signatures, and EM anomalies to in targeting the diamond drill holes outlined below. 6.2 Diamond Drilling Program Winter 2010 In 2010 Mega Uranium conducted a diamond drill program including 1803 m of diamond drilling on the Greenwich Lake property. Drill logs and sections are presented in Appendix D. Collar locations and drill traces are shown on Figure 10 and Map 3. These drill holes were designed to test a series of sinuous approximately north to northwest trending magnetic highs and magnetic lows. Below is a summary of each of the holes drilled as part of the 2010 Greenwich Lake drill program. 6.2.1 Diamond Drill Core Sampling and QA/QC All samples were split and a sample tag was left in the core box at the beginning of the sample interval. All core boxes were labeled with embossed metal tags and stored at the Mega’s Thunder Bay facility at 855 Field Street. All Assay results and laboratory certificates are included in Appendix B. All samples assayed were sent to Activation Laboratories in Thunder Bay, Ontario and analyzed using their 1C-exploration Fire Assay-ICP/MS method for Au, Pt, and Pd. This method has a lower detection limit for Au of 2 ppb, and a lower detection limit for Pt and Pd of 1 ppb. Additionally, all of the samples were analyzed using the Activation Laboratories package 1F2 near total digestion ICP/OES which assay’s for 36 elements. Approximately every 5th sample was also analyzed for whole rock geochemistry to measure all major oxides using XRF. Quality Control/Quality Assurance (QA/QC) samples were inserted into each batch of core samples sent for analysis. One pulverized CANMET standard (UMT-1) was inserted into each lab batch every 30th sample. Additionally, duplicate samples (quarter section of core) were taken every 30th sample. 6.2.2 2010 Greenwich Lake Diamond Drill Program Results The drill holes (Fig. 10, Map2, Table 2) were designed to test a series of sinuous approximately north to northwest trending magnetic highs and magnetic lows, along with any co-incident EM anomalies, and nearby compositionally prospective grab samples collected during the 2009 prospecting program.

20

Table 2: 2010 Greenwich Lake Diamond Drill Holes

DDH No. UTM Zone 16N,

NAD 83 Azimuth Dip Depth (m) Start Date End Date

Easting Northing

GL-10-1 0364350 5404769

Vertical N/A 189 Feb. 20,

2010 Mar. 4, 2010

GL-10-2 0364064 5409513

070 -50 259 Feb. 27,

2010 Mar. 4, 2010

GL-10-3 0364205 5409325

070 -50 219 Mar. 04,

2010 Mar. 07,

2010

GL-10-4 0362924 5408767

067 -50 251 Mar. 04,

2010 Mar. 16,

2010

GL-10-5 0363374 5409302

270 -50 250 Mar. 07,

2010 Mar. 11,

2010

GL-10-6 0361745 5404876

060 -50 225 Mar. 17,

2010 Mar. 20,

2010

GL-10-7 0363832 5404687

255 -50 201 Mar. 18,

2010 Mar. 24,

2010

GL-10-8 0362153 5406622

315 -50 209 Mar. 21,

2010 Mar. 23,

2010

Total 1803 Diamond drill hole GL-10-1 was drilled to test a weak EM conductor and coincident moderate “tear-drop” shaped magnetic bulge along linear magnetic trend, at bend in magnetic and EM anomaly trend below Greenwich Lake (Fig 10, Map 3). The 2010 drilling failed to encounter any mafic intrusive associated with this anomaly. Due to site conditions (ice quality, and deep sediment at the bottom of the lake) this drill hole was forced to be drilled ~ 25 m from the peak UTM of the mag anomaly associated with this anomaly. Given the width (~25 m to 70 m) of Magma Metals TBN deposit one vertical drill hole could easily miss any mineralized mafic intrusive associated with this anomaly. Due to spring like conditions in early March in northern Ontario this year only one drill hole was completed on this target. Diamond drill hole GL-10-2 and GL-10-3 were drilled to test the northerly continuation of the weak to moderate magnetic trend, along the eastern of the two magnetic trends that bifurcate near GL-10-1 (Fig 10, Map 3). Additionally, there are three proximal outcrop samples and 1 boulder sample with 8.5 – 10.5% MgO, 200 – 500 ppm Cr2O3, 125 – 200 ppm Ni, 106 – 300 ppm Cu and up to 140 ppb Pt+Pd+Au suggesting compositionally prospective rocks with indications of Cu & PGE mineralization. The 2010 drilling encountered ~40 m of magnetic, medium grained, non-foliated gabbro in each hole. GL-

21

10-3 encountered (139.75 m to 142.75 m) 3 m of weakly anomalous Pt, Pd, and Au mineralization (above background relative to 248 samples of mafic material assayed on the property). GL-10-4 was drilled to test the northern continuation of a weak to moderate linear magnetic anomaly trend associated with GL-10-6 (Fig. 10, Map 3). Three outcrop rock samples close to the target area contain up to 13.7% MgO, 1500 ppm Cr2O3, 160 ppm Ni, 245 ppm Cu and 22 ppb Pt+Pd+Au , suggesting compositionally prospective rocks with indications of Cu & PGE mineralization. The 2010 drilling encountered ~6 m of magnetic, fine grained, non-foliated, green to dark grey chlorite altered, mafic intrusive with disseminated sulphides at the top of the hole. Assay results, and visual comparison indicate that the mafic intrusive unit encountered at GL-10-4 is very similar to the mafic intrusive encountered at GL-10-6 and GL-10-7 and is likely the northern continuation of a chlorite altered diabase dyke encountered in GL-10-7. Diamond drill hole GL-10-5 was drilled to test the north to northwesterly trending sinuous weak to moderate magnetic anomaly that starts south of GL-10-5 beneath Greenwich Lake (Fig. 10, Map 3). Additionally it contains three outcrop rock samples close to the target area containing up to 12.6% MgO, 200 ppm Cr2O3, 125 ppm Ni, 205 ppm Cu, suggesting compositionally prospective rocks with weak indications of Cu & PGE mineralization. The 2010 drilling encountered ~10 m of magnetic, hematite altered, medium grained, non-foliated gabbro. Assay results indicate a non-mineralized, high (>10%) MgO rock with no Ni, Cu-PGE mineralization. GL-10-6 tested the moderate to high northwesterly magnetic trend, and what appeared to be fresh, fine grained mafic rocks nearby in outcrop. Outcrop sampling results in the area are variable, but one sample contains 9.5% MgO, 600 ppm Cr2O3 , 295 ppm Ni and 53 ppm Cu. The 2010 drilling encountered ~12 m of magnetic, fine grained, non-foliated, green to dark grey sulphide-rich mafic intrusive rock. Petrographic analysis showed that this unit is a fine grained, chlorite altered diabase. Furthermore, assay values from this hole returned results with low MgO (~6%), low Cr2O3 (<100 ppm), and no Pt, Pd, or Au mineralization. Diamond drill hole GL-10-7 was drilled to test the north-northeast trending weak to moderate magnetic high, adjacent to a historical diamond drill hole (75-2) by Consolidated Monarch Minerals Ltd. that was logged as possibly containing peridotite. The 2010 drilling encountered ~11 m of magnetic, fine grained, non-foliated, green to dark grey chlorite altered, mafic intrusive with disseminated sulphides throughout. Assay results, proximal prospecting sample results, and visual comparison indicate that the mafic intrusive unit encountered in GL-10-7 is very similar to the mafic intrusive encountered in GL-10-6 and is thus likely a chlorite altered diabase dyke. GL-10-8 was drilled to test the strong magnetic “bull’s eye” associated with one outcrop rock sample assayed at 12.7% MgO, 1100 ppm Cr2O3 , 269 ppm Ni, 221 ppm Cu and 29 ppb Pt+Pd+Au possibly indicating a compositionally prospective rock type with indications of Ni, Cu, PGE mineralization. The 2010 drilling encountered 140 m of

22

magnetic, homogenous, medium grained, non-foliated, green/gray with red, chlorite and hematite altered gabbro. Assay results from 31 samples (note the gabbro was sampled every 5 m throughout the 140m section) of the altered gabbro returned weakly mineralized values of Pt+Pd+Au. These values ranged from 10 to 129 ppb (each sample was over 1 m) with the average of Pt+Pd+Au of all 31 samples being 56 ppb (Appendix B). 7.0 CONCLUSIONS AND RECOMMENDATIONS In August, 2009 a prospecting program was completed on the Greenwich Lake property to evaluate the property’s potential to host an economic deposit of Ni, Cu, PGEs. This program resulted in the collection of 28 samples of mafic intrusive rocks which returned elevated Pt+Pd+Au values in 12 samples that ranged from 3 ppb to 143 ppb. The mineralization discovered during the prospecting program, while weak, pointed to the possibility of compositionally prospective rocks on the property. Theses encouraging results coupled with un-tested, co-incident magnetic and EM anomalies beneath Greenwich Lake led to the decision to complete a diamond drill program on the property in the winter of 2010. In February and March of 2010 eight (8) diamond drill holes for a total of 1803 m were drilled on the Greenwich Lake property. These drill holes were designed to test a series of sinuous approximately north to northwest trending magnetic highs, any co-incident EM anomalies, in addition to any nearby compositionally prospective grab samples. Drilling in GL-10-8 intersected 140 m of weak anomalous (above background relative to 248 samples of mafic material assayed on the property) Pt, Pd, and Au mineralization in a chlorite and hematite altered gabbro. This gabbro is associated with a “bull’s-eye” magnetic anomaly on the western portion of the property. Assay results from 31 samples (the gabbro was sampled every 5 m from 0 to 140 m) of the altered gabbro returned Pt+Pd+Au values ranging from 10 to 129 ppb. In addition to the positive results encountered in GL-10-8 two of our key targets below Greenwich Lake, defined by a co-incident, sinuous, electromagnetic (EM) and magnetic anomalies remain untested due to above-average winter temperatures in northern Ontario this past winter. After completing the initial drill program on the Greenwich Lake drill property, it is recommended that further work be completed to: • Adequately access the anomalous mineralization in GL-10-8 and GL-10-3. This work should include a look at regional Pt, Pd, Au values in lower Keweenawan mafic intrusive rocks and possibly more drilling.

• Thoroughly test the targets below Greenwich Lake with further drilling in winter 2011.

23

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24

8.0 REFERENCES Barrie, C. 2007. High Resolution Magnetic, XDS VLF-EM & Radiometric Airborne

Survey, Greenwich Project, Thunder Bay, Ontario. East West Resource Corporation/Mega Uranium Ltd. Internal Report Submitted for Assessment, 37 p.

Benkis, R.A. 1976a. Drill Log, Holes RTG-1. Assessment Report, Rio Tinto Canadian

Exploration Ltd. (AFRI File No. 52A15SW0012), 11 p. Benkis, R.A. 1976b. Drill Logs, Holes RTG-2 and RTG-3. Assessment Report, Rio

Tinto Canadian Exploration Ltd. (AFRI File No. 52A15SW0010), 30 p. Benkis, R.A. 1977. N.T.S. 52-A-15 MW Option, Greenwich Lake Area, Ontario:

Geological Report. Assessment Report, Rio Tinto Canadian Exploration Ltd. (AFRI File No. 52A15SW0008), 25 p.

Carter, M.W., 1979, Greenwich Lake Area, District of Thunder Bay. Ontario Geological

Survey, Preliminary Map P.2249, scale 1:15,840. Carter, M.W. 1983. Geology of the Greenwich Area, District of Thunder Bay. Ontario

Geological Survey Open File Report 5427, 49 p. Cheadle, B.A. 1986. Alluvial-playa sedimentation in the lower Keweenawan Sibley

Group, Thunder Bay District, Ontario. Canadian Journal of Earth Sciences, v.23, pp. 527-542.

Chisolm, L. And Oja, R.V. 1970a. Drill Logs. Assessment Report, Univex Exploration

and Development Corporation (AFRI File No. 52A15SW0016), 13 p. Chisolm, L. And Oja, R.V. 1970b. Drill Logs. Assessment Report, Univex Exploration

and Development Corporation (AFRI File No. 52A15SW0014), 12 p. Christianson, D.E. and Fairbairn, D. 1978a. Drilling and Trenching. Assessment

Report, Greenwich Lake Exploration Ltd. (AFRI File No. 52A15SW0007), 16 p. Christianson, D.E. and Fairbairn, D. 1978b. Drill Logs. Assessment Report, Greenwich

Lake Exploration Ltd. (AFRI File No. 52A15SW0011), 31 p. Drost, A. 2001. Synopsis of geology, metallogeny and mineral potential, Nipigon Basin

signature site. Internal Ontario Geological Survey Memorandum, 3 p. Eckstrand, O.R., and Hulbert, L.J., 2007, Magmatic Nickel-Copper-Platinum Group

Element Deposits, in Goodfellow, W.D., ed., Mineral Deposits of Canada: Geological Association of Canada, Mineral Deposits Division, Special Publication No. 5, p. 205-222.

25

Fairbairn, D. 1982. Drill Log, Hole 82-1. Assessment Report, Greenwich Lake

Exploration Ltd. (AFRI File No. 52A15SW0006), 3 p. Franklin, J.M. 1982. The Sibley Group. In Proterozoic geology of the northern Lake

Superior Area. Geological Association of Canada Field Trip Guidebook, Trip 4, pp. 32-41.

Franklin, J.M., McIlwaine, W.H., Poulsen, K.H. and Wanless, R.K. 1980. Stratigraphy

and depositional setting of the Sibley Group, Thunder Bay district, Ontario, Canada. Canadian Journal of Earth Sciences, v.1, pp. 633-651.

Green, J.C. 1977. Keweenawan plateau volcanism in the Lake Superior region.

Geological Association of Canada Special Paper 16, pp. 407-422. Heshka, W. 1975a. Drill Logs, Holes 75-1 to 75-6B. Assessment Report, Consolidated

Monarch Metals Limited (AFRI File No. 52A15SW0013), 25 p. Heshka, W. 1975b. Drill Logs, Holes 75-1 to 75-6B. Assessment Report, Consolidated

Monarch Metals Limited (AFRI File No. 52A15SW0019), 41 p. Oja, R.V. 1969. Report on the Airborne Radiometric Survey, Greenwich Lake Area.

Assessment Report, Univex Exploration and Development Corporation (AFRI File No. 52A15SW0020), 5 p.

Oja, R.V. 1970. Drill Logs. Assessment Report, Univex Exploration and Development

Corporation (AFRI File No. 52A15SW0015), 25 p. Ontario Geological Survey. 1991. Bedrock geology of Ontario, west-central sheet.

Ontario Geological Survey, Map 2542, scale 1:1,000,000. Scott, J.F. 1987. Uranium Occurrences of the Thunder Bay-Nipigon-Marathon Area.

Ontario Geological Survey Open File Report 5634, 150 p. Sutcliffe, R.H. 1991. Proterozoic geology of the Lake Superior area. Ontario Geological

Survey, Special Volume 4, pp.627-658. Thurston, P.C. 1991. Archean geology of Ontario: Introduction. Ontario Geological

Survey, Special Volume 4, pp. 73-78. Webster, B. 1979. Report on TURAM and Induced Polarization Surveys, Greenwich

Lake Grid, Thunder Bay, Ontario. Assessment Report, Greenwich Lake Exploration Ltd. (AFRI File No. 52A15SW0002), 9 p.

APPENDIX A: Certificates of Qualifications

I, Tony Ldo hereby (1) I am (2) I resi (3) I am

Geolo (4) I am

Geolo (5) I hav (6) I am

• AP

• P• A• G

(7) I help

Tony Gil

L Gilman, My certify tha

a Geologist

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a graduate oogical Engin

a graduate oogy (2006).

ve been pract

a member inAssociation o

.Eng rospectors a

Association oGeological So

ped write thi

lman, April 2

M.Sc., P.Eng at:

and Project

061 Fort St.

of the Univeneering (200

of the Pennsy

ticing my pr

n good standof Profession

and Developeof Mineral Eociety of Am

is assessmen

26, 2010

of the City o

t Manager fo

., Victoria, B

rsity of New00).

ylvania State

rofession con

ding of the:nal Engineer

ers AssociatExploration Bmerica (GSA

nt report.

of Victoria, P

or Mega Uran

British Colum

w Brunswick

e University

ntinuously si

rs and Geosc

tion Canada British ColumA)

Province of

nium Ltd.

mbia, Canad

k with a Bach

y with a Mas

ince 2000.

cientists of B

(PDAC) mbia (AMEB

British Colu

da, V8V 5A1

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umbia, Cana

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ence in

ce degree in

mbia (APEG

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GBC),

CER

TIFICA

TE OF A

NA

LYSIS

Innovative Technologies Q

uality Analysis ...

Invoice No.:

Invoice Date:

Date Subm

itted:

Your Reference:

20-Apr-10

25-Mar-10

A10-1323

Mega U

ranium Ltd.

P3 1061 Fort StreetVictoria B

C V8V 3K

5C

anada

Tony Gilm

anA

TTN:

This report may be reproduced w

ithout our consent. If only selected portions of the report are reproduced, permission

must be obtained. If no instructions w

ere given at time of sam

ple submittal regarding excess m

aterial, it will be

discarded within 90 days of this report. O

ur liability is limited solely to the analytical cost of these analyses. Test results

are representative only of material subm

itted for analysis.

AC

TIVATIO

N LA

BO

RA

TOR

IES LTD.

1336 Sandhill D

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+1.905.648.9611 or +1.888.228.5227 FA

X +1.905.648.9613E-M

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A10-1323

Notes:

2 Pulp sam

ples and 43 Rock sam

ples were subm

itted for analysis.

Code 1C

-Exp IC

PO

ES

-Tbay Fire Assay ICP

OE

SC

ode 1F2-Tbay Total Digestion IC

P(TO

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Code 4C

(1-10) Whole R

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Values w

hich exceed the upper limit should be assayed for accurate num

bers.

Sam

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Quality C

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The following analytical packages w

ere requested:

PO N

umber:

Activation Laboratories Ltd. Report: A10-1323 rev 1Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K Mg Mn Mo Na Ni P Pb Sb SAnalyte Symbol

ppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % % ppm ppm % ppm % ppm ppm %Unit Symbol0.3 0.01 3 7 1 2 0.01 0.3 1 1 1 0.01 1 1 0.01 0.01 1 1 0.01 1 0.001 3 5 0.01Detection Limit

TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICPAnalysis Method

0.4 5.23 251 2286183 < 2 5.18 0.4 51 118 246 9.74 26 < 1 1.18 4.26 1310 < 1 2.50 89 0.090 4 < 5 0.03< 3

< 0.3 5.06 289 2286184 < 2 5.05 < 0.3 50 114 180 9.67 26 < 1 1.07 4.16 1140 < 1 2.13 87 0.095 7 < 5 0.02< 3

< 0.3 4.97 345 2286185 < 2 5.19 < 0.3 50 101 281 9.65 25 < 1 1.03 4.19 1170 < 1 2.02 86 0.084 4 < 5 0.03< 3

0.6 3.69 118 1286186 < 2 5.08 0.4 50 68 175 8.83 26 < 1 0.77 3.38 1080 < 1 2.23 75 0.115 < 3 < 5 0.02< 3

0.6 3.87 345 1286187 < 2 5.13 0.4 54 139 216 9.40 26 < 1 1.02 3.88 1150 < 1 1.82 79 0.111 < 3 < 5 0.04< 3

0.3 5.20 259 2286188 < 2 5.48 0.6 45 37 262 9.65 27 < 1 0.92 3.55 1180 < 1 2.32 68 0.086 9 < 5 0.024

< 0.3 5.21 949 2286189 < 2 5.35 0.7 50 68 283 10.1 27 < 1 1.79 3.62 1720 < 1 1.88 75 0.086 5 < 5 0.04< 3

0.4 5.25 806 2286190 < 2 4.54 0.8 48 57 260 9.08 26 < 1 1.92 3.58 1600 < 1 1.98 65 0.077 5 < 5 0.04< 3

0.6 5.66 611 2286191 < 2 3.62 0.4 34 12 149 6.93 30 < 1 2.79 2.86 849 < 1 2.15 24 0.245 3 < 5 0.05< 3

0.5 5.02 394 2286192 < 2 5.86 < 0.3 52 53 247 9.68 28 < 1 1.09 3.55 1340 < 1 1.41 65 0.091 < 3 < 5 0.05< 3

0.5 5.63 378 2286193 < 2 5.23 < 0.3 45 5 373 8.74 27 < 1 1.21 2.97 1220 < 1 2.10 48 0.090 < 3 < 5 0.05< 3

0.5 5.66 435 2286194 < 2 4.53 < 0.3 46 24 340 9.13 27 < 1 1.45 3.41 1350 < 1 2.49 58 0.093 4 < 5 0.05< 3

0.7 1.86 37 < 1286195 < 2 4.37 0.9 77 2150 758 9.20 15 < 1 0.06 12.8 1140 < 1 0.46 1450 0.010 4 < 5 0.18< 3

0.8 3.83 174 1286196 3 4.29 < 0.3 43 26 320 8.11 26 < 1 0.71 2.66 1000 < 1 2.52 49 0.104 3 < 5 0.057

0.7 4.27 315 < 1286197 < 2 5.19 0.5 53 49 333 9.25 26 < 1 0.94 3.28 1200 < 1 2.54 72 0.105 < 3 < 5 0.05< 3

0.5 5.93 552 2286198 < 2 4.95 0.4 47 18 431 9.53 27 < 1 1.66 3.13 1370 < 1 2.53 62 0.077 5 < 5 0.046

0.4 5.61 319 1286199 < 2 6.15 0.7 50 70 310 9.66 27 < 1 0.97 3.91 1240 < 1 2.38 88 0.078 5 < 5 0.04< 3

0.5 5.92 375 1286200 < 2 5.50 0.5 47 40 323 8.95 27 < 1 1.25 3.42 1060 < 1 2.56 74 0.073 5 < 5 0.044

0.5 5.56 347 1286201 < 2 5.73 0.4 53 67 315 9.84 26 < 1 1.11 3.96 1250 < 1 2.26 96 0.077 < 3 < 5 0.04< 3

0.5 5.33 267 1286202 < 2 5.91 0.6 53 141 188 9.75 26 < 1 0.90 4.85 1200 < 1 2.23 112 0.081 < 3 < 5 0.03< 3

0.5 5.35 267 1286203 < 2 5.68 0.5 52 163 157 9.58 26 < 1 0.86 5.10 1240 < 1 2.36 121 0.073 7 < 5 0.02< 3

0.7 5.49 175 2286204 < 2 5.52 < 0.3 41 138 192 8.35 27 < 1 1.04 3.78 916 < 1 2.74 98 0.065 < 3 < 5 0.02< 3

0.3 5.42 382 1286205 < 2 6.16 0.4 56 63 186 10.2 27 < 1 1.09 3.89 1320 < 1 2.04 89 0.072 5 < 5 0.02< 3

< 0.3 5.27 214 2286206 4 5.93 0.4 51 77 157 9.82 26 < 1 0.76 3.91 1120 < 1 2.36 91 0.078 5 < 5 0.02< 3

0.4 3.73 269 < 1286207 < 2 5.62 0.4 60 81 161 9.47 26 < 1 0.74 3.27 1150 < 1 1.94 85 0.097 < 3 < 5 0.02< 3

0.5 4.15 296 1286208 < 2 6.08 < 0.3 52 222 198 8.84 24 < 1 1.12 4.28 1160 < 1 2.10 114 0.068 < 3 < 5 0.03< 3

< 0.3 4.31 460 2286209 < 2 6.53 0.4 57 434 167 9.07 23 < 1 1.31 5.48 1290 < 1 1.56 166 0.089 4 < 5 0.02< 3

0.5 4.32 452 1286210 < 2 6.71 < 0.3 60 382 164 9.22 23 < 1 1.31 5.58 1320 < 1 1.59 171 0.082 5 < 5 0.03< 3

0.4 4.63 484 1286211 < 2 6.54 0.5 55 272 218 9.30 23 < 1 1.74 5.23 1130 < 1 1.39 155 0.071 3 < 5 0.035

< 0.3 4.32 314 1286212 < 2 6.87 < 0.3 57 432 129 9.27 23 < 1 0.94 5.78 1180 < 1 1.64 188 0.092 5 < 5 0.02< 3

0.4 4.36 206 1286213 < 2 6.15 < 0.3 57 421 138 9.07 22 < 1 0.85 5.52 1060 < 1 1.95 172 0.089 < 3 < 5 0.02< 3

0.4 4.63 304 1286214 < 2 6.50 0.4 57 421 157 9.19 24 < 1 0.82 5.50 1200 < 1 1.86 173 0.085 5 < 5 0.024

0.8 1.95 38 < 1286215 < 2 4.45 0.5 77 2040 793 9.42 18 < 1 0.07 13.2 1170 < 1 0.49 1500 0.010 3 < 5 0.18< 3

0.5 3.66 235 < 1286216 < 2 4.54 0.6 55 19 49 9.61 28 < 1 0.66 2.12 1340 < 1 2.19 52 0.159 4 < 5 0.08< 3

0.4 4.20 278 1286217 < 2 5.37 0.5 55 19 51 10.2 30 < 1 0.79 2.53 1330 < 1 2.30 51 0.149 5 < 5 0.043

< 0.3 5.55 302 1286218 < 2 5.56 0.6 53 17 54 10.4 30 < 1 0.94 2.60 1330 < 1 2.34 54 0.130 5 < 5 0.043

< 0.3 5.67 306 1286219 < 2 5.77 0.6 52 15 54 10.6 31 < 1 0.94 2.64 1320 < 1 2.37 53 0.133 5 < 5 0.03< 3

< 0.3 5.68 301 1286220 < 2 5.67 < 0.3 53 17 53 10.4 31 < 1 0.91 2.71 1280 < 1 2.34 56 0.130 4 < 5 0.02< 3

< 0.3 5.68 288 1286221 < 2 5.76 < 0.3 51 15 50 10.3 28 < 1 0.85 2.73 1320 < 1 2.33 57 0.126 3 < 5 0.02< 3

0.4 5.64 286 1286222 < 2 5.58 < 0.3 54 15 48 10.5 33 < 1 0.94 2.80 1300 < 1 2.45 53 0.144 < 3 < 5 0.03< 3

< 0.3 5.49 308 1286223 < 2 5.39 0.5 50 17 52 10.2 31 < 1 1.05 2.50 1290 < 1 2.36 54 0.131 4 < 5 0.03< 3

< 0.3 5.45 295 1286224 < 2 5.38 0.6 50 13 52 10.2 30 < 1 0.95 2.52 1280 < 1 2.34 53 0.126 6 < 5 0.04< 3

0.5 4.05 285 < 1286225 < 2 4.95 0.8 53 14 49 9.81 29 < 1 0.84 2.27 1300 < 1 2.28 47 0.162 4 < 5 0.05< 3

0.5 4.15 279 1286226 < 2 4.91 < 0.3 55 14 53 10.3 30 < 1 0.85 2.59 1360 < 1 2.45 53 0.155 < 3 < 5 0.07< 3

< 0.3 5.61 244 1286227 < 2 5.21 0.6 51 16 55 10.3 30 < 1 0.68 2.88 1370 < 1 2.41 54 0.135 4 < 5 0.07< 3

Page 2 of 10

Activation Laboratories Ltd. Report: A10-1323 rev 1Sc Sr Te Ti Tl U V W Y Zn Zr SiO2 Al2O3 Fe2O3(T) MnO MgO CaO Na2O K2O TiO2 P2O5 Cr2O3 LOI TotalAnalyte Symbol

ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % % % % % % % % % % % % %Unit Symbol4 1 2 0.01 5 10 2 5 1 1 5 0.01 0.01 0.01 0.001 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01Detection Limit

TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRFAnalysis Method

29 241 0.53 < 5286183 < 10 125 < 5 31 94 178 47.45 12.39 13.83 0.172 7.14 6.83 3.24 1.38 3.20 0.30 0.03 2.73 98.697

27 288 0.19 < 5286184 < 10 74 < 5 31 101 862

28 288 0.10 < 5286185 < 10 77 < 5 28 98 247

15 295 1.54 < 5286186 < 10 339 < 5 21 77 28411

18 372 1.23 < 5286187 < 10 292 < 5 24 94 2794

27 537 0.13 < 5286188 < 10 59 < 5 31 102 48 47.64 12.59 13.95 0.163 6.06 7.38 3.07 1.17 3.64 0.30 < 0.01 2.82 98.79< 2

28 795 0.16 < 5286189 < 10 70 < 5 31 109 51< 2

25 772 0.32 < 5286190 < 10 81 < 5 34 101 145< 2

15 564 0.46 < 5286191 < 10 99 < 5 47 72 2898

27 1080 0.44 < 5286192 < 10 113 < 5 33 89 1806

24 978 0.41 < 5286193 < 10 84 < 5 33 81 166 48.00 13.84 12.93 0.167 5.14 7.09 2.80 1.46 4.11 0.33 < 0.01 3.13 99.007

25 426 0.66 < 5286194 < 10 117 < 5 32 86 197< 2

31 70 0.25 < 5286195 < 10 177 < 5 8 68 18< 2

11 305 1.67 < 5286196 < 10 294 < 5 20 73 33520

16 582 1.68 < 5286197 < 10 328 < 5 23 78 28323

26 740 0.09 < 5286198 < 10 39 < 5 30 89 19 47.29 13.87 13.64 0.186 5.34 6.62 3.29 1.98 4.48 0.28 < 0.01 2.05 99.03< 2

30 610 0.25 < 5286199 < 10 76 < 5 29 84 87< 2

26 681 0.33 < 5286200 < 10 78 8 28 82 11217

30 787 0.64 < 5286201 < 10 127 < 5 28 89 171< 2

31 604 0.65 < 5286202 < 10 156 < 5 28 93 18917

32 545 0.67 < 5286203 < 10 161 < 5 27 91 186< 2

28 354 0.64 < 5286204 < 10 157 < 5 31 63 312< 2

30 837 0.18 < 5286205 < 10 80 < 5 27 84 51 46.72 12.83 14.72 0.181 6.63 8.39 2.59 1.32 3.38 0.24 0.01 2.40 99.41< 2

28 542 0.08 < 5286206 < 10 76 < 5 28 85 24< 2

15 656 1.58 < 5286207 < 10 423 < 5 18 77 25216

19 357 1.20 < 5286208 < 10 275 < 5 20 79 280< 2

31 452 0.23 < 5286209 < 10 60 < 5 28 96 1258

32 449 0.41 < 5286210 < 10 86 < 5 29 98 19411

33 347 0.51 < 5286211 < 10 105 < 5 28 74 20014

32 486 0.32 < 5286212 < 10 68 < 5 29 89 140< 2

31 406 0.47 < 5286213 < 10 80 < 5 29 88 166 48.38 10.50 13.30 0.150 9.61 8.51 2.52 1.08 2.49 0.29 0.07 2.35 99.258

31 540 0.20 < 5286214 < 10 62 < 5 27 99 736

32 73 0.26 < 5286215 < 10 180 < 5 9 72 19< 2

10 300 1.49 < 5286216 < 10 296 < 5 23 110 24722

16 333 0.90 < 5286217 < 10 223 < 5 31 119 21614

25 341 0.16 < 5286218 < 10 75 < 5 40 124 48 50.88 13.36 15.04 0.183 4.49 7.46 3.08 1.15 2.89 0.40 < 0.01 0.32 99.25< 2

26 348 0.21 < 5286219 < 10 80 < 5 40 123 68< 2

25 354 0.20 7286220 < 10 77 < 5 39 118 716

25 349 0.20 < 5286221 < 10 74 < 5 38 119 687

25 359 0.75 < 5286222 < 10 167 < 5 40 107 216 50.80 13.41 14.91 0.170 4.71 7.35 3.18 1.15 2.88 0.40 < 0.01 0.75 99.71< 2

24 343 0.15 < 5286223 < 10 75 < 5 39 116 46< 2

24 335 0.14 < 5286224 < 10 102 < 5 39 116 58< 2

13 308 1.50 < 5286225 < 10 301 < 5 28 116 2533

16 329 0.96 < 5286226 < 10 227 < 5 31 115 20113

25 337 0.15 < 5286227 < 10 85 < 5 40 111 42 50.06 13.17 14.71 0.181 4.88 6.86 3.14 0.84 2.85 0.41 < 0.01 2.07 99.17< 2

Page 3 of 10

Activation Laboratories Ltd. Report: A10-1323 rev 1Au Pd PtAnalyte Symbol

ppb ppb ppbUnit Symbol2 5 5Detection Limit

FA-ICP FA-ICP FA-ICPAnalysis Method

11 22286183 36

6 20286184 37

13 17286185 36

5 36286186 56

6 15286187 25

9 23286188 51

11 18286189 40

11 19286190 35

3 5286191 5

9 17286192 35

4 < 5286193 6

7 12286194 21

49 106286195 134

11 11286196 21

12 14286197 34

10 7286198 15

12 21286199 45

11 15286200 34

15 25286201 50

9 25286202 46

8 28286203 54

7 18286204 29

12 42286205 75

4 38286206 39

4 31286207 53

5 13286208 21

10 7286209 16

5 9286210 17

6 10286211 18

2 13286212 18

3 < 5286213 < 5

4 7286214 13

286215

< 2 < 5286216 < 5

< 2 < 5286217 < 5

< 2 5286218 < 5

2 < 5286219 < 5

< 2 < 5286220 < 5

< 2 < 5286221 < 5

< 2 < 5286222 < 5

< 2 < 5286223 < 5

< 2 < 5286224 < 5

< 2 < 5286225 < 5

4 < 5286226 < 5

< 2 < 5286227 < 5

Page 4 of 10

Activation Laboratories Ltd. Report: A10-1323 rev 1Quality Control

Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K Mg Mn Mo Na Ni P Pb Sb SAnalyte Symbolppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % % ppm ppm % ppm % ppm ppm %Unit Symbol

0.3 0.01 3 7 1 2 0.01 0.3 1 1 1 0.01 1 1 0.01 0.01 1 1 0.01 1 0.001 3 5 0.01Detection LimitTD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICPAnalysis Method

31.5 1.70 757 1GXR-1 Meas 1390 0.92 3.3 8 17 1180 23.6 18 4 0.04 0.21 881 15 0.05 43 0.061 733 44 0.2342231.0 3.52 750 1.22GXR-1 Cert 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 0.217 852 18.0 0.0520 41.0 0.0650 730 122 0.257427

99DNC-1 Meas 54 258 97 250 < 5 118DNC-1 Cert 57.0 270.0 100.0 247 0.96

MICA-FE MeasMICA-FE Cert

3.5 5.07 290 2GXR-4 Meas 10 1.11 0.5 15 69 6450 3.10 22 < 1 1.81 1.66 156 314 0.52 37 0.140 48 < 5 1.811054.00 7.20 1640 1.90GXR-4 Cert 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 1.66 155 310 0.564 42.0 0.120 52.0 4.80 1.7798.0

< 0.3 6.27 630 4SDC-1 Meas < 2 1.12 < 0.3 19 61 26 4.71 2.66 0.98 835 < 1 1.53 37 0.055 23 < 5 0.06< 30.0410 8.34 630 3.00SDC-1 Cert 2.60 1.00 0.0800 17.9 64.0 30.0 4.82 2.72 1.02 883 0.250 1.52 38.0 0.0690 25.0 0.540 0.06500.220

0.3 5.76 592 2SCO-1 Meas < 2 2.15 0.4 13 75 28 3.73 2.33 1.64 404 < 1 0.73 29 0.089 28 < 5150.134 7.24 570 1.84SCO-1 Cert 0.370 1.87 0.140 10.5 68.0 28.7 3.59 2.30 1.64 410 1.37 0.670 27.0 0.0900 31.0 2.5012.4

0.5 9.27 > 1000 1GXR-6 Meas < 2 0.18 0.5 16 88 68 5.66 37 < 1 1.84 0.59 1120 1 0.10 28 0.030 98 < 5 < 0.012291.30 17.7 1300 1.40GXR-6 Cert 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 0.609 1010 2.40 0.104 27.0 0.0350 101 3.60 0.0160330

BE-N MeasBE-N CertW-2a MeasW-2a CertOREAS 13P Meas 2690 7.91 2240OREAS 13P Cert 2500 7.58 2260MICA-Mg MeasMICA-Mg CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert286192 Orig286192 Dup

0.7 1.85 38 < 1286195 Orig < 2 4.40 1.1 76 2160 749 9.30 14 < 1 0.07 12.9 1150 < 1 0.46 1420 0.010 5 < 5 0.18< 30.6 1.86 36 < 1286195 Dup < 2 4.33 0.8 78 2130 767 9.10 15 < 1 0.06 12.7 1130 < 1 0.46 1470 0.010 4 < 5 0.17< 3

286202 Orig286202 Dup

0.4 4.32 460 1286209 Orig < 2 6.52 0.4 58 437 168 9.07 23 < 1 1.31 5.41 1290 < 1 1.56 166 0.088 5 < 5 0.02< 3< 0.3 4.31 460 2286209 Dup < 2 6.53 0.4 57 431 165 9.06 23 < 1 1.31 5.54 1290 < 1 1.56 167 0.091 4 < 5 0.02< 3< 0.3 4.32 314 1286212 Orig < 2 6.87 < 0.3 57 432 129 9.27 23 < 1 0.94 5.78 1180 < 1 1.64 188 0.092 5 < 5 0.02< 3

0.4 4.24 309 1286212 Split < 2 6.85 0.4 59 493 135 9.21 23 < 1 0.93 5.75 1180 < 1 1.61 188 0.086 < 3 < 5 0.02< 3286213 Orig286213 Dup286227 Orig286227 Dup

Page 5 of 10


Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K Mg Mn Mo Na Ni P Pb Sb SAnalyte Symbolppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % % ppm ppm % ppm % ppm ppm %Unit Symbol

0.3 0.01 3 7 1 2 0.01 0.3 1 1 1 0.01 1 1 0.01 0.01 1 1 0.01 1 0.001 3 5 0.01Detection LimitTD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICPAnalysis Method

< 0.3 < 0.01 < 7 < 1Method Blank Method Blank

< 2 < 0.01 < 0.3 < 1 7 1 < 0.01 < 1 < 1 < 0.01 < 0.01 14 < 1 < 0.01 < 1 < 0.001 < 3 < 5 < 0.01< 3

< 0.3 0.02 < 7 < 1Method Blank Method Blank

< 2 0.02 < 0.3 < 1 6 < 1 0.03 < 1 < 1 < 0.01 < 0.01 6 < 1 < 0.01 2 < 0.001 < 3 < 5 < 0.01< 3

Method Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

Page 6 of 10


Sc Sr Te Ti Tl U V W Y Zn Zr SiO2 Al2O3 Fe2O3(T) MnO MgO CaO Na2O K2O TiO2 P2O5 Cr2O3 LOI TotalAnalyte Symbolppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % % % % % % % % % % % % %Unit Symbol

4 1 2 0.01 5 10 2 5 1 1 5 0.01 0.01 0.01 0.001 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01Detection LimitTD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRFAnalysis Method

< 4 294 < 5GXR-1 Meas 30 90 159 26 749 35181.58 275 0.390GXR-1 Cert 34.9 80.0 164 32.0 760 38.013.0

32 131DNC-1 Meas 144 23 54 53 46.70 18.46 9.97 0.151 10.14 11.19 1.98 0.23 0.49 0.08 31 144.0DNC-1 Cert 148.0 18.0 70.0 38 47.15 18.34 9.97 0.150 10.13 11.49 1.890 0.234 0.480 0.070

MICA-FE Meas 34.35 19.35 25.68 0.349 4.76 0.43 0.49 8.71 2.51 0.40 0.02MICA-FE Cert 34.4 19.5 25.6 0.350 4.55 0.430 0.300 8.75 2.50 0.450 0.01

8 214 < 5GXR-4 Meas < 10 93 36 20 71 67< 27.70 221 3.20GXR-4 Cert 6.20 87.0 30.8 14.0 73.0 1860.970

16 169 0.08SDC-1 Meas 31 < 5 48 100 3517.0 183 0.606SDC-1 Cert 102 0.800 40.0 103 290

13 168 0.31SCO-1 Meas 129 < 5 30 100 14910.8 174 0.380SCO-1 Cert 131 1.40 26.0 103 160

26 37 < 5GXR-6 Meas < 10 120 < 5 19 134 98327.6 35.0 2.20GXR-6 Cert 1.54 186 1.90 14.0 118 1100.0180

BE-N Meas 38.11 10.01 0.201 13.16 13.75 3.23 1.39 2.67 1.05 0.05BE-N Cert 38.2 10.1 0.200 13.1 13.9 3.18 1.39 2.61 1.05 0.0500W-2a Meas 52.42 15.28 10.82 0.174 6.41 10.73 2.27 0.63 1.08 0.13 0.01W-2a Cert 52.4 15.4 10.7 0.163 6.37 10.9 2.14 0.626 1.06 0.130 0.01OREAS 13P MeasOREAS 13P CertMICA-Mg Meas 37.99 15.15 9.31 0.254 20.30 0.01 0.21 9.96 1.64 0.01 0.01MICA-Mg Cert 38.30 15.20 9.46 0.26 20.40 0.08 0.12 10.00 1.63 0.01 0.01CDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert286192 Orig286192 Dup

31 70 0.25 < 5286195 Orig < 10 179 < 5 9 66 18< 231 70 0.25 < 5286195 Dup < 10 176 < 5 8 70 18< 2

286202 Orig286202 Dup

31 453 0.30 < 5286209 Orig < 10 70 < 5 29 95 1751331 451 0.16 < 5286209 Dup < 10 50 < 5 28 97 76332 486 0.32 < 5286212 Orig < 10 68 < 5 29 89 140< 232 482 0.46 < 5286212 Split < 10 97 < 5 29 97 200< 2

286213 Orig286213 Dup286227 Orig286227 Dup

Page 7 of 10


Sc Sr Te Ti Tl U V W Y Zn Zr SiO2 Al2O3 Fe2O3(T) MnO MgO CaO Na2O K2O TiO2 P2O5 Cr2O3 LOI TotalAnalyte Symbolppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % % % % % % % % % % % % %Unit Symbol

4 1 2 0.01 5 10 2 5 1 1 5 0.01 0.01 0.01 0.001 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01Detection LimitTD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRFAnalysis Method

< 4 < 1 < 0.01 < 5Method Blank Method Blank

< 10 < 2 < 5 < 1 < 1 < 5< 2

< 4 2 < 0.01 < 5Method Blank Method Blank

< 10 < 2 < 5 < 1 < 1 < 5< 2

Method Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

< 0.01 < 0.01 < 0.01 < 0.001 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01 -0.01 < 0.01

Method Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

Page 8 of 10


Au Pd PtAnalyte Symbolppb ppb ppbUnit Symbol

2 5 5Detection LimitFA-ICP FA-ICP FA-ICPAnalysis Method

GXR-1 MeasGXR-1 CertDNC-1 MeasDNC-1 CertMICA-FE MeasMICA-FE CertGXR-4 MeasGXR-4 CertSDC-1 MeasSDC-1 CertSCO-1 MeasSCO-1 CertGXR-6 MeasGXR-6 CertBE-N MeasBE-N CertW-2a MeasW-2a CertOREAS 13P MeasOREAS 13P CertMICA-Mg MeasMICA-Mg Cert

363 458CDN-PGMS-15 Meas 99 410.000 428.000CDN-PGMS-15 Cert 98.000










10 17286192 Orig 359 16286192 Dup 34

286195 Orig286195 Dup

8 24286202 Orig 4610 25286202 Dup 46

286209 Orig286209 Dup

2 13286212 Orig 184 10286212 Split 174 7286213 Orig 174 9286213 Dup 15

< 2 < 5286227 Orig < 5< 2 < 5286227 Dup < 5

Page 9 of 10


Au Pd PtAnalyte Symbolppb ppb ppbUnit Symbol

2 5 5Detection LimitFA-ICP FA-ICP FA-ICPAnalysis Method

Method Blank Method BlankMethod Blank Method Blank

< 2 < 5Method Blank Method Blank

< 5


< 5


< 5

Method Blank Method Blank


< 5


< 5


< 5


< 5


< 5


< 5


< 5


< 5


< 5

Page 10 of 10

CER

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uality Analysis ...

Invoice No.:

Invoice Date:

Date Subm

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Your Reference:

25-Mar-10

22-Mar-10

A10-1235

Mega U

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Activation Laboratories Ltd. Report: A10-1235Au Pd Pt Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K Mg Mn Mo Na Ni PAnalyte Symbol

ppb ppb ppb ppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % % ppm ppm % ppm %Unit Symbol2 5 5 0.3 0.01 3 7 1 2 0.01 0.3 1 1 1 0.01 1 1 0.01 0.01 1 1 0.01 1 0.001Detection Limit

FA-ICP FA-ICP FA-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICPAnalysis Method

6 < 5 < 0.3 6.23286147 < 3 229 1 < 2 3.24 < 0.3 44 275 131 6.08 21 < 1 1.20 7.27 779 < 1 1.65 106 0.026< 5

6 < 5 < 0.3 5.84286148 < 3 157 2 < 2 2.79 0.4 42 292 39 6.57 18 < 1 1.50 8.49 759 < 1 0.87 104 0.019< 5

4 < 5 < 0.3 1.30286149 < 3 56 2 < 2 3.13 < 0.3 31 156 11 4.94 12 < 1 0.35 5.45 709 < 1 0.24 66 0.009< 5

15 6 < 0.3 2.66286150 < 3 53 1 < 2 3.45 < 0.3 29 158 16 4.65 12 < 1 0.37 5.53 700 < 1 0.24 61 0.009< 5

4 < 5 < 0.3 5.45286151 < 3 110 < 1 < 2 4.03 < 0.3 38 228 54 5.75 14 < 1 1.03 6.70 775 < 1 1.48 87 0.018< 5

6 5 < 0.3 5.86286152 < 3 278 < 1 < 2 2.13 0.5 45 261 106 6.50 18 < 1 1.15 8.22 681 < 1 1.48 99 0.018< 5

2 < 5 < 0.3 6.05286153 < 3 409 < 1 < 2 2.34 0.4 44 270 99 6.14 20 < 1 1.62 7.28 653 < 1 1.49 101 0.022< 5

3 < 5 < 0.3 5.78286154 < 3 209 < 1 < 2 1.24 0.5 46 298 117 6.93 19 < 1 1.64 8.92 639 < 1 0.87 95 0.021< 5

< 2 < 5 < 0.3 6.13286155 3 229 < 1 < 2 1.39 0.4 45 262 147 6.60 20 1 1.78 9.22 657 < 1 0.89 96 0.022< 5

8 < 5 < 0.3 5.71286156 < 3 194 < 1 < 2 2.66 0.3 43 285 128 6.68 16 < 1 1.75 7.91 717 < 1 0.70 107 0.020< 5

2 < 5 < 0.3 5.94286157 < 3 242 2 < 2 4.17 0.5 46 295 44 6.38 21 < 1 2.19 7.11 906 < 1 0.66 109 0.022< 5

< 2 < 5 0.3 5.35286158 < 3 400 3 < 2 2.23 < 0.3 26 183 6 4.35 18 < 1 1.83 4.31 658 < 1 1.17 63 0.028< 5

< 2 < 5 0.5 2.71286159 < 3 233 < 1 < 2 4.71 0.9 49 14 47 9.13 27 < 1 0.83 1.90 1100 < 1 1.80 44 0.158< 5

< 2 < 5 0.5 2.96286160 < 3 238 < 1 < 2 5.07 0.6 51 16 48 9.45 28 < 1 0.80 2.19 1150 < 1 1.89 45 0.156< 5

< 2 < 5 0.5 4.66286161 < 3 213 < 1 < 2 5.11 < 0.3 49 20 49 9.27 26 < 1 0.76 2.70 1020 < 1 1.97 45 0.156< 5

9 < 5 0.4 5.19286162 < 3 185 1 < 2 5.24 0.6 45 16 48 9.16 31 < 1 0.54 3.05 998 < 1 2.11 48 0.120< 5

< 2 < 5 0.4 5.17286163 < 3 460 1 < 2 5.39 0.9 47 17 49 8.93 28 1 0.94 2.65 1250 < 1 1.70 47 0.120< 5

< 2 7 < 0.3 5.18286164 < 3 521 1 < 2 4.92 0.9 46 17 49 9.51 27 < 1 0.93 2.95 1380 < 1 1.69 46 0.129< 5

49 110 0.8 1.87286165 < 3 33 < 1 < 2 4.37 0.8 72 1730 758 9.49 14 < 1 0.08 14.3 1130 < 1 0.43 1460 0.010139

< 2 < 5 < 0.3 4.93286166 < 3 271 2 < 2 4.66 1.1 53 57 34 12.1 27 < 1 0.71 4.46 1260 < 1 1.05 47 0.150< 5

< 2 < 5 < 0.3 5.06286167 < 3 289 2 < 2 5.82 0.4 52 56 33 12.7 27 < 1 0.95 3.62 1670 < 1 1.31 48 0.155< 5

2 < 5 < 0.3 4.99286168 < 3 278 2 < 2 5.74 0.8 49 57 33 12.2 26 < 1 0.97 3.34 1810 < 1 1.25 44 0.144< 5

< 2 5 0.6 2.32286169 < 3 258 1 < 2 5.25 0.6 64 48 26 11.3 26 < 1 0.88 2.45 1640 < 1 1.06 39 0.194< 5

67 118 0.7 1.11286170 < 3 33 < 1 < 2 4.24 1.3 72 2180 748 9.23 14 < 1 0.07 13.6 1110 < 1 0.42 1450 0.010145

7 < 5 0.4 4.63286171 < 3 271 1 < 2 5.04 1.4 49 63 30 11.1 26 < 1 1.09 3.69 1310 < 1 0.92 46 0.146< 5

< 2 < 5 < 0.3 4.88286172 < 3 371 1 < 2 4.65 0.9 50 73 36 11.6 26 < 1 1.36 3.89 1270 < 1 0.90 57 0.121< 5

< 2 < 5 < 0.3 4.86286173 < 3 257 2 < 2 5.26 0.9 50 63 28 11.8 29 < 1 0.95 3.85 1380 < 1 0.99 49 0.145< 5

< 2 < 5 0.3 5.06286174 < 3 254 1 < 2 5.67 0.4 51 53 32 11.9 26 < 1 0.90 3.45 1670 < 1 1.25 45 0.159< 5

5 < 5 < 0.3 5.00286175 < 3 266 2 < 2 5.72 0.7 47 60 33 12.2 28 < 1 0.85 3.42 1810 < 1 1.23 46 0.159< 5

< 2 < 5 < 0.3 4.86286176 < 3 272 2 < 2 5.67 1.0 47 54 32 11.7 25 < 1 0.94 3.30 1850 < 1 1.23 54 0.156< 5

7 < 5 < 0.3 4.83286177 < 3 257 2 < 2 5.70 0.6 46 61 33 11.7 25 < 1 0.91 3.31 1620 < 1 1.29 46 0.145< 5

2 < 5 < 0.3 4.46286178 < 3 207 2 < 2 5.14 0.5 47 51 30 11.6 26 < 1 0.71 3.76 1230 < 1 0.99 42 0.134< 5

< 2 < 5 < 0.3 1.95286179 < 3 559 2 < 2 0.23 0.4 2 8 2 0.98 19 < 1 3.08 0.34 150 < 1 2.61 < 1 0.022< 5

< 2 < 5 < 0.3 4.61286180 < 3 571 2 < 2 0.48 < 0.3 2 6 2 1.08 20 < 1 1.86 0.40 138 < 1 2.72 < 1 0.024< 5

< 2 < 5 < 0.3 4.94286181 < 3 228 3 < 2 5.72 0.6 48 53 35 11.6 25 < 1 0.79 3.44 1420 < 1 1.35 48 0.142< 5

5 < 5 0.5 6.65286182 < 3 527 4 < 2 0.18 0.5 7 7 40 9.60 30 < 1 3.33 2.51 290 2 0.74 16 0.032< 5

Page 2 of 7

Activation Laboratories Ltd. Report: A10-1235Pb Sb S Sc Sr Te Ti Tl U V W Y Zn Zr SiO2 Al2O3 Fe2O3(T) MnO MgO CaO Na2O K2O TiO2 P2O5Analyte Symbol

ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % % % % % % % % % %Unit Symbol3 5 0.01 4 1 2 0.01 5 10 2 5 1 1 5 0.01 0.01 0.01 0.001 0.01 0.01 0.01 0.01 0.01 0.01Detection Limit

TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRFAnalysis Method

< 3 < 5 36 138286147 < 2 0.37 < 5 < 10 193 < 5 16 39 560.08

3 < 5 38 72286148 < 2 0.31 < 5 < 10 194 < 5 17 52 43 44.64 14.56 9.77 0.105 13.93 3.74 1.26 1.64 0.62 0.050.02

6 < 5 8 40286149 3 0.15 < 5 < 10 123 < 5 4 41 120.14

< 3 < 5 15 40286150 3 0.17 < 5 < 10 108 < 5 11 43 190.10

< 3 < 5 36 97286151 < 2 0.31 < 5 < 10 168 < 5 17 43 39 46.36 13.89 8.67 0.111 11.17 5.71 2.20 1.13 0.59 0.050.05

< 3 < 5 37 128286152 < 2 0.33 < 5 < 10 184 < 5 13 44 380.06

< 3 < 5 37 139286153 < 2 0.39 < 5 < 10 203 < 5 14 39 460.09

< 3 < 5 37 105286154 < 2 0.39 < 5 < 10 202 < 5 14 37 420.09

< 3 < 5 39 109286155 < 2 0.38 < 5 < 10 207 < 5 13 43 440.12

< 3 < 5 37 105286156 < 2 0.36 < 5 < 10 195 < 5 14 44 41 46.04 14.35 9.77 0.101 13.07 3.62 1.05 1.90 0.61 0.050.08

< 3 < 5 38 106286157 5 0.36 < 5 < 10 197 < 5 18 43 430.06

3 < 5 21 82286158 < 2 0.23 < 5 < 10 108 < 5 13 40 960.01

< 3 < 5 9 295286159 12 1.49 < 5 < 10 283 < 5 16 103 1780.03

< 3 < 5 5 305286160 18 1.48 < 5 < 10 286 < 5 18 107 1900.03

< 3 < 5 18 296286161 7 1.41 < 5 < 10 263 < 5 28 99 201 50.29 13.12 14.44 0.151 4.69 7.56 3.03 0.93 2.86 0.410.10

3 < 5 21 306286162 < 2 0.28 < 5 < 10 140 < 5 31 73 1250.14

9 < 5 21 328286163 5 0.24 < 5 < 10 131 < 5 33 97 1000.19

10 < 5 21 331286164 7 0.19 < 5 < 10 116 < 5 32 94 780.17

< 3 < 5 28 73286165 < 2 0.26 < 5 < 10 173 < 5 7 68 150.18

6 < 5 33 146286166 2 0.43 < 5 < 10 115 < 5 47 87 850.35

4 < 5 34 188286167 7 0.26 < 5 < 10 160 < 5 47 126 810.26

3 < 5 33 190286168 6 0.31 < 5 < 10 176 < 5 46 125 100 44.51 12.58 18.75 0.265 5.47 8.20 1.83 1.11 3.68 0.490.18

< 3 < 5 12 167286169 < 2 1.86 < 5 < 10 332 < 5 22 112 2510.43

< 3 < 5 12 70286170 5 0.26 < 5 < 10 168 < 5 7 66 140.18

< 3 < 5 30 181286171 7 0.78 < 5 < 10 225 < 5 39 116 1550.19

3 < 5 32 175286172 24 0.20 < 5 < 10 167 < 5 38 117 870.19

< 3 < 5 32 171286173 21 0.30 < 5 < 10 121 < 5 43 109 49 43.12 12.48 18.61 0.206 6.45 7.66 1.50 1.11 3.72 0.460.37

< 3 < 5 33 192286174 17 0.33 < 5 < 10 105 < 5 47 135 760.27

5 < 5 33 192286175 5 0.28 < 5 < 10 131 < 5 46 125 870.22

3 < 5 32 186286176 20 0.22 < 5 < 10 124 < 5 45 126 78 44.62 12.59 18.50 0.271 5.53 8.15 1.87 1.03 3.64 0.500.12

< 3 < 5 32 177286177 < 2 0.18 < 5 < 10 138 < 5 44 125 640.14

5 < 5 30 140286178 6 0.27 < 5 < 10 159 < 5 42 115 830.31

19 < 5 < 4 110286179 < 2 0.09 < 5 < 10 11 < 5 < 1 41 980.01

21 < 5 < 4 185286180 5 0.08 < 5 < 10 10 < 5 2 37 1040.01

6 < 5 31 170286181 < 2 0.23 < 5 < 10 145 < 5 43 113 970.15

40 < 5 < 4 111286182 < 2 0.10 < 5 80 19 < 5 16 59 1320.57

Page 3 of 7

Activation Laboratories Ltd. Report: A10-1235Cr2O3 LOI TotalAnalyte Symbol

% % %Unit Symbol0.01 0.01Detection Limit

FUS-XRF FUS-XRF FUS-XRFAnalysis Method

286147

0.05 9.57286148 99.93

286149

286150

0.03 9.63286151 99.54

286152

286153

286154

286155

0.04 9.06286156 99.66

286157

286158

286159

286160

< 0.01 1.39286161 98.87

286162

286163

286164

286165

286166

286167

0.01 2.36286168 99.25

286169

286170

286171

286172

0.01 3.84286173 99.17

286174

286175

0.01 2.35286176 99.07

286177

286178

286179

286180

286181

286182

Page 4 of 7

Activation Laboratories Ltd. Report: A10-1235Quality Control

Au Pd Pt Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K Mg Mn Mo Na Ni PAnalyte Symbolppb ppb ppb ppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % % ppm ppm % ppm %Unit Symbol

2 5 5 0.3 0.01 3 7 1 2 0.01 0.3 1 1 1 0.01 1 1 0.01 0.01 1 1 0.01 1 0.001Detection LimitFA-ICP FA-ICP FA-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICPAnalysis Method

31.6 2.15GXR-1 Meas 432 694 1 1400 0.93 3.3 8 11 1180 23.7 17 4 0.05 0.25 868 14 0.05 39 0.06231.0 3.52GXR-1 Cert 427 750 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 0.217 852 18.0 0.0520 41.0 0.0650

< 0.3 7.59DNC-1 Meas 3 93 < 1 < 2 7.91 54 228 99 6.88 18 0.22 6.43 1040 < 1 1.37 252 0.0270.0270 9.69DNC-1 Cert 0.200 114 1.00 0.0200 8.06 54.7 285 96.0 6.94 15.0 0.190 6.06 1150 0.700 1.39 247 0.0370


3.4 3.52GXR-4 Meas 102 418 2 4 1.00 0.6 13 65 6450 2.83 21 < 1 2.15 1.48 142 315 0.46 39 0.1304.00 7.20GXR-4 Cert 98.0 1640 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 1.66 155 310 0.564 42.0 0.120

< 0.3 6.70SDC-1 Meas < 3 630 4 < 2 1.18 < 0.3 18 67 31 5.00 2.98 1.17 900 < 1 1.53 39 0.0620.0410 8.34SDC-1 Cert 0.220 630 3.00 2.60 1.00 0.0800 17.9 64.0 30.0 4.82 2.72 1.02 883 0.250 1.52 38.0 0.0690

< 0.3 5.98SCO-1 Meas 16 549 2 < 2 2.10 < 0.3 12 67 30 3.76 2.33 1.82 404 < 1 0.67 29 0.0930.134 7.24SCO-1 Cert 12.4 570 1.84 0.370 1.87 0.140 10.5 68.0 28.7 3.59 2.30 1.64 410 1.37 0.670 27.0 0.0900

0.5 10.1GXR-6 Meas 280 > 1000 1 < 2 0.18 < 0.3 14 86 70 5.68 33 < 1 1.80 0.67 1100 3 0.09 27 0.0381.30 17.7GXR-6 Cert 330 1300 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 0.609 1010 2.40 0.104 27.0 0.0350

BE-N MeasBE-N CertW-2a MeasW-2a CertOREAS 13P Meas 2530 7.58 2160OREAS 13P Cert 2500 7.58 2260OREAS 14P Meas 708 9850 33.9 > 10000OREAS 14P Cert 750 9970 37.2 21000DTS-2b MeasDTS-2b Cert



< 0.3 5.47286151 Orig < 3 111 < 1 < 2 4.04 < 0.3 37 244 54 5.77 14 < 1 1.04 6.75 787 < 1 1.49 89 0.019< 0.3 5.44286151 Dup < 3 109 < 1 < 2 4.02 0.6 38 212 54 5.72 15 < 1 1.02 6.66 763 < 1 1.47 85 0.018

3 < 5286156 Orig < 513 < 5286156 Dup < 5

0.8 1.87286165 Orig < 3 33 < 1 < 2 4.36 1.0 72 1690 761 9.48 14 < 1 0.08 14.3 1130 < 1 0.43 1470 0.0100.8 1.87286165 Dup < 3 34 < 1 < 2 4.38 0.7 72 1760 755 9.50 13 < 1 0.08 14.4 1140 < 1 0.43 1460 0.010

< 2 < 5286166 Orig < 5< 2 < 5286166 Dup < 561 118286170 Orig 14373 118286170 Dup 147

< 2 < 5 < 0.3 4.86286176 Orig < 3 272 2 < 2 5.67 1.0 47 54 32 11.7 25 < 1 0.94 3.30 1850 < 1 1.23 54 0.156< 5< 2 < 5 0.3 5.20286176 Split < 3 291 2 < 2 5.89 0.7 50 58 34 12.4 29 < 1 0.99 3.49 1900 < 1 1.32 48 0.165< 5

7 < 5286177 Orig < 58 < 5286177 Dup < 5

< 0.3 4.51286178 Orig < 3 211 2 < 2 5.18 0.6 48 50 29 11.6 26 < 1 0.72 3.79 1240 < 1 1.01 43 0.136< 0.3 4.41286178 Dup < 3 204 2 < 2 5.09 0.4 47 52 30 11.5 25 < 1 0.70 3.74 1220 < 1 0.98 42 0.132< 0.3 < 0.01Method Blank Method

Blank< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 9 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 16 < 1 < 0.01 < 1 < 0.001

< 0.3 < 0.01Method Blank Method Blank

< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 5 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 12 < 1 < 0.01 < 1 < 0.001


< 5


< 5


< 5


Page 5 of 7


Pb Sb S Sc Sr Te Ti Tl U V W Y Zn Zr SiO2 Al2O3 Fe2O3(T) MnO MgO CaO Na2O K2O TiO2 P2O5Analyte Symbolppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % % % % % % % % % %Unit Symbol

3 5 0.01 4 1 2 0.01 5 10 2 5 1 1 5 0.01 0.01 0.01 0.001 0.01 0.01 0.01 0.01 0.01 0.01Detection LimitTD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP TD-ICP FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRF FUS-XRFAnalysis Method

735 19 < 4 297GXR-1 Meas 18 < 5 30 87 154 35 750 340.25730 122 1.58 275GXR-1 Cert 13.0 0.390 34.9 80.0 164 32.0 760 38.00.257

4 < 5 29 136DNC-1 Meas 0.29 < 5 < 10 142 < 5 20 53 43 46.91 18.44 10.03 0.149 10.22 11.26 1.98 0.24 0.49 0.080.056.30 0.960 31.0 145DNC-1 Cert 0.287 0.0260 0.100 148 0.200 18.0 66.0 41.0 47.0 18.3 9.93 0.149 10.1 11.3 1.87 0.234 0.480 0.09000.0390

MICA-FE Meas 34.33 19.36 25.67 0.350 4.80 0.44 0.51 8.75 2.54 0.40MICA-FE Cert 34.4 19.5 25.6 0.350 4.55 0.430 0.300 8.75 2.50 0.450

47 < 5 5 189GXR-4 Meas < 2 < 5 < 10 86 41 11 67 531.7852.0 4.80 7.70 221GXR-4 Cert 0.970 3.20 6.20 87.0 30.8 14.0 73.0 1861.77

25 < 5 16 188SDC-1 Meas 0.10 36 < 5 44 104 450.0625.0 0.540 17.0 183SDC-1 Cert 0.606 102 0.800 40.0 103 2900.0650

27 < 5 12 176SCO-1 Meas 0.39 138 < 5 26 100 14231.0 2.50 10.8 174SCO-1 Cert 0.380 131 1.40 26.0 103 160100 < 5 28 40GXR-6 Meas < 2 < 5 < 10 149 < 5 17 131 1080.01101 3.60 27.6 35.0GXR-6 Cert 0.0180 2.20 1.54 186 1.90 14.0 118 1100.0160

BE-N Meas 38.18 10.00 0.200 13.14 13.81 3.21 1.39 2.69 1.05BE-N Cert 38.2 10.1 0.200 13.1 13.9 3.18 1.39 2.61 1.05W-2a Meas 52.18 15.43 10.91 0.169 6.42 10.85 2.28 0.63 1.09 0.13W-2a Cert 52.4 15.4 10.7 0.163 6.37 10.9 2.14 0.626 1.06 0.130OREAS 13P MeasOREAS 13P CertOREAS 14P MeasOREAS 14P CertDTS-2b Meas 38.92 0.47 49.14 0.12DTS-2b Cert 39.4 0.450 49.4 0.120CDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert

< 3 < 5 36 98286151 Orig < 2 0.33 < 5 < 10 181 < 5 17 43 400.05< 3 < 5 36 95286151 Dup < 2 0.29 < 5 < 10 156 < 5 17 42 380.05

286156 Orig286156 Dup

< 3 < 5 28 73286165 Orig < 2 0.26 < 5 < 10 172 < 5 7 68 150.18< 3 < 5 28 73286165 Dup < 2 0.26 < 5 < 10 173 < 5 7 68 150.18

286166 Orig286166 Dup286170 Orig286170 Dup

3 < 5 32 186286176 Orig 20 0.22 < 5 < 10 124 < 5 45 126 78 44.62 12.59 18.50 0.271 5.53 8.15 1.87 1.03 3.64 0.500.12< 3 < 5 35 198286176 Split 24 0.63 < 5 < 10 199 < 5 49 135 153 44.67 12.53 18.47 0.271 5.52 8.16 1.85 1.03 3.65 0.500.13

286177 Orig286177 Dup

6 < 5 30 142286178 Orig 2 0.22 5 < 10 164 < 5 42 112 750.304 < 5 30 139286178 Dup 9 0.32 < 5 < 10 153 < 5 41 118 920.31

< 3 < 5 < 4 < 1Method Blank Method Blank

< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01

Method Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

< 0.01 < 0.01 < 0.01 < 0.001 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01

Page 6 of 7


Cr2O3 LOI TotalAnalyte Symbol% % %Unit Symbol

0.01 0.01Detection LimitFUS-XRF FUS-XRF FUS-XRFAnalysis Method

GXR-1 MeasGXR-1 Cert

0.04DNC-1 Meas 0.04DNC-1 Cert

0.01MICA-FE Meas 0.01MICA-FE Cert

GXR-4 MeasGXR-4 CertSDC-1 MeasSDC-1 CertSCO-1 MeasSCO-1 CertGXR-6 MeasGXR-6 Cert

0.05BE-N Meas0.0500BE-N Cert

0.02W-2a Meas 0.01W-2a Cert

OREAS 13P MeasOREAS 13P CertOREAS 14P MeasOREAS 14P Cert

2.24DTS-2b Meas 2.27DTS-2b Cert

CDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert286151 Orig286151 Dup286156 Orig286156 Dup286165 Orig286165 Dup286166 Orig286166 Dup286170 Orig286170 Dup

0.01 2.35286176 Orig 99.070.01 2.35286176 Split 99.01

286177 Orig286177 Dup286178 Orig286178 DupMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

< 0.01 -0.01Method Blank Method Blank

< 0.01

Page 7 of 7

CER

TIFICA

TE OF A

NA

LYSIS


uality Analysis ...

Invoice No.:

Invoice Date:

Date Subm

itted:

Your Reference:

24-Mar-10

11-Mar-10

A10-1089

Mega U

ranium Ltd.


C V8V 3K

5C

anada

Tony Gilm

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TTN:






aterial, it will be




itted for analysis.

AC

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1336 Sandhill D

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ntario Canada L9G

4V5 TELEP

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+1.905.648.9611 or +1.888.228.5227 FA

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A10-1089

Notes:

3 Pulp sam

ples and 79 Rock sam

ples were subm

itted for analysis.

Code 1C

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PO

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P(TO

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Code 4C

(11+) Whole R

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RF

Values w


bers.

Quality C

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ere requested:

PO N

umber:




5 7 < 0.3 6.07286065 < 3 631 2 < 2 5.12 0.4 44 339 20 6.50 19 < 1 1.92 5.90 951 < 1 0.98 108 0.0196

3 < 5 < 0.3 5.50286066 < 3 535 1 < 2 4.29 < 0.3 46 232 25 6.87 19 < 1 2.44 7.39 1070 < 1 0.57 105 0.020< 5

6 < 5 < 0.3 5.74286067 < 3 412 2 < 2 6.21 1.2 44 238 17 7.50 21 < 1 2.24 5.32 1300 < 1 0.79 104 0.019< 5

< 2 < 5 0.3 5.84286068 < 3 751 < 1 < 2 3.78 0.8 44 219 49 7.15 19 < 1 2.03 7.04 964 < 1 0.99 104 0.021< 5

5 11 0.3 6.06286069 < 3 > 1000 < 1 < 2 4.99 < 0.3 44 309 135 6.79 20 < 1 1.35 6.38 1020 < 1 1.36 108 0.021< 5

6 < 5 < 0.3 6.27286070 < 3 771 < 1 < 2 4.62 0.7 42 309 128 6.01 23 < 1 1.44 5.17 957 < 1 1.76 102 0.036< 5

4 < 5 0.7 6.16286071 < 3 554 2 < 2 2.15 < 0.3 22 232 97 4.95 24 < 1 2.93 1.97 802 < 1 1.36 77 0.070< 5

3 < 5 0.6 6.16286072 < 3 464 2 < 2 1.97 < 0.3 23 234 55 4.62 26 < 1 1.83 2.25 634 < 1 2.34 78 0.060< 5

< 2 < 5 0.6 8.42286073 < 3 532 1 < 2 1.97 < 0.3 22 231 55 4.70 25 < 1 2.06 2.32 721 < 1 2.46 79 0.071< 5

< 2 < 5 0.6 6.28286074 < 3 547 2 < 2 1.86 < 0.3 21 224 69 4.68 23 < 1 1.88 2.13 736 < 1 2.25 79 0.060< 5

49 104286075 130

< 2 < 5 0.5 6.21286076 < 3 536 2 < 2 1.94 < 0.3 24 251 79 4.56 24 < 1 2.44 2.25 677 < 1 1.96 83 0.063< 5

3 6 0.5 6.89286077 < 3 564 2 < 2 1.79 < 0.3 27 221 53 5.27 30 < 1 2.50 2.67 789 < 1 2.09 98 0.077< 5

< 2 < 5 0.5 6.77286078 < 3 569 2 < 2 1.29 < 0.3 19 163 33 4.09 27 < 1 2.46 2.22 535 2 2.82 68 0.177< 5

< 2 < 5 0.5 6.81286079 < 3 449 2 < 2 1.21 < 0.3 22 180 33 4.56 28 < 1 1.90 2.34 553 < 1 2.78 88 0.087< 5

< 2 < 5 0.4 6.51286080 < 3 636 2 < 2 1.63 < 0.3 22 227 69 4.73 25 < 1 2.90 2.25 685 < 1 2.18 87 0.074< 5

< 2 < 5 0.7 6.46286081 < 3 627 2 < 2 1.42 < 0.3 20 185 65 4.26 25 < 1 2.52 2.13 619 1 2.44 76 0.080< 5

< 2 < 5 0.5 6.28286082 < 3 447 2 < 2 1.54 0.3 23 217 65 4.56 24 < 1 2.00 2.38 614 < 1 2.33 85 0.068< 5

< 2 5 0.4 6.44286083 4 402 2 < 2 1.48 < 0.3 23 216 44 4.61 24 < 1 1.72 2.66 589 < 1 2.48 90 0.071< 5

< 2 < 5 0.4 4.07286084 < 3 277 2 < 2 0.75 < 0.3 17 190 25 3.69 23 < 1 1.27 1.99 484 2 2.67 71 0.062< 5

2 < 5 0.5 4.85286085 < 3 470 1 < 2 1.42 < 0.3 22 226 66 4.46 26 < 1 2.08 1.96 686 < 1 2.28 76 0.077< 5

2 6 0.5 5.29286086 < 3 465 2 < 2 3.53 < 0.3 26 223 88 4.90 24 < 1 2.26 2.36 815 < 1 1.66 73 0.141< 5

4 < 5 0.6 6.32286087 < 3 369 2 < 2 1.33 < 0.3 23 206 93 4.52 26 < 1 1.49 2.21 542 < 1 2.82 76 0.069< 5

< 2 < 5 0.5 6.46286088 < 3 264 1 < 2 1.72 < 0.3 38 235 42 4.65 25 < 1 1.01 2.41 494 < 1 2.94 97 0.067< 5

< 2 < 5 0.5 6.66286089 < 3 232 2 < 2 1.70 < 0.3 23 198 55 4.41 24 < 1 0.93 2.42 515 < 1 3.03 83 0.068< 5

< 2 < 5 0.5 6.46286090 < 3 222 2 < 2 1.68 < 0.3 21 197 53 4.17 24 < 1 0.89 2.33 493 < 1 2.93 82 0.068< 5

< 2 < 5 0.4 6.48286091 < 3 204 2 < 2 1.71 < 0.3 22 207 37 4.25 27 < 1 0.74 2.30 440 < 1 3.47 78 0.066< 5

3 < 5 0.4 6.44286092 < 3 213 2 < 2 1.53 < 0.3 23 201 51 4.41 25 < 1 0.84 2.46 510 < 1 2.98 85 0.067< 5

< 2 < 5 0.5 6.84286093 < 3 108 2 < 2 1.62 < 0.3 26 206 33 4.66 28 < 1 0.50 2.87 505 < 1 4.04 95 0.083< 5

< 2 < 5 < 0.3 5.26286094 < 3 347 < 1 < 2 3.85 < 0.3 25 216 70 4.47 23 4 1.44 2.81 701 < 1 2.60 73 0.040< 5

< 2 < 5 < 0.3 5.61286095 < 3 106 < 1 < 2 7.82 < 0.3 46 343 111 7.19 20 < 1 0.55 5.27 1280 < 1 1.28 104 0.019< 5

< 2 < 5 < 0.3 6.28286096 < 3 106 < 1 < 2 7.88 < 0.3 44 300 103 7.62 21 < 1 0.68 5.61 1240 < 1 1.44 100 0.020< 5

< 2 < 5 < 0.3 6.45286097 < 3 108 < 1 < 2 7.41 1.2 43 311 115 7.47 20 < 1 0.92 5.37 1330 < 1 2.08 93 0.022< 5

< 2 < 5 < 0.3 6.46286098 < 3 149 < 1 < 2 7.50 0.8 47 337 117 7.36 20 < 1 1.18 5.11 1260 < 1 2.00 97 0.022< 5

4 < 5 0.3 6.58286099 < 3 188 < 1 < 2 8.08 < 0.3 44 286 125 7.23 20 < 1 1.30 5.08 1330 < 1 1.26 104 0.019< 5

2 < 5 0.4 6.40286100 < 3 182 < 1 < 2 8.25 0.3 45 252 140 7.02 20 < 1 1.31 5.02 1330 < 1 1.27 100 0.018< 5

5 9 < 0.3 6.27286101 < 3 162 < 1 < 2 8.08 0.4 44 410 186 6.54 19 < 1 1.10 5.78 1190 < 1 1.23 174 0.01611

15 31 0.3 6.47286102 < 3 155 < 1 < 2 8.68 1.0 46 440 370 6.57 20 < 1 0.98 5.87 1170 < 1 1.18 274 0.01631

4 6 0.3 6.54286103 < 3 147 < 1 < 2 8.35 0.7 45 451 167 6.43 20 < 1 1.08 5.64 1150 < 1 1.39 158 0.0167

8 12 < 0.3 6.34286104 < 3 155 < 1 < 2 8.44 0.3 44 533 221 6.71 19 < 1 1.01 5.58 1160 < 1 1.33 187 0.01612

55 102286105 135

3 < 5 0.3 6.34286106 < 3 170 < 1 < 2 7.76 0.5 39 284 97 6.72 21 < 1 1.16 4.58 1190 < 1 1.54 89 0.018< 5

< 2 < 5 < 0.3 6.39286107 < 3 142 < 1 < 2 8.10 < 0.3 41 299 102 6.93 19 < 1 1.19 4.85 1240 < 1 1.35 100 0.018< 5

< 2 < 5 0.3 6.64286108 5 132 < 1 < 2 8.15 < 0.3 45 311 111 7.04 20 < 1 1.19 4.90 1250 < 1 1.31 100 0.020< 5

< 2 < 5 < 0.3 6.52286109 < 3 124 < 1 < 2 8.22 0.4 42 303 98 6.82 19 < 1 1.06 4.67 1240 < 1 1.85 93 0.019< 5

< 2 < 5 0.3 6.72286110 < 3 161 < 1 < 2 7.78 1.3 42 232 98 6.88 20 < 1 1.35 4.65 1270 < 1 1.65 86 0.020< 5

< 2 < 5 < 0.3 6.74286111 14 155 < 1 < 2 7.96 0.3 41 240 104 6.96 20 3 1.36 4.68 1290 < 1 1.55 90 0.019< 5

4 < 5 0.3 6.57286112 < 3 123 < 1 < 2 7.57 1.0 44 250 104 7.22 20 < 1 1.05 5.02 1320 < 1 1.81 94 0.020< 5

3 < 5 0.3 6.46286113 < 3 145 < 1 < 2 8.05 0.4 47 256 144 8.07 21 < 1 0.98 5.17 1460 < 1 1.31 109 0.024< 5

4 < 5 0.4 6.38286114 < 3 130 < 1 < 2 8.01 0.4 46 268 103 7.56 20 < 1 1.07 5.14 1340 < 1 1.41 100 0.022< 5

2 < 5 0.4 6.47286115 < 3 118 < 1 < 2 7.74 0.9 45 249 110 7.49 20 < 1 1.10 5.17 1360 < 1 1.43 103 0.020< 5

2 < 5 < 0.3 4.69286116 < 3 111 < 1 < 2 6.73 0.4 44 327 101 6.76 18 < 1 0.91 4.59 1330 < 1 1.39 104 0.018< 5

Page 2 of 13




4 < 5 0.3 6.06286117 < 3 108 < 1 < 2 6.06 0.5 44 350 94 6.98 18 < 1 0.87 5.90 1330 < 1 1.87 106 0.022< 5

< 2 < 5 < 0.3 6.18286118 < 3 121 < 1 < 2 7.64 < 0.3 46 347 105 7.40 20 < 1 1.01 5.30 1370 < 1 1.31 113 0.021< 5

< 2 < 5 < 0.3 6.37286119 < 3 128 < 1 < 2 8.10 0.4 48 267 110 7.72 20 < 1 0.94 5.34 1400 < 1 1.28 113 0.021< 5

< 2 < 5 < 0.3 6.31286120 < 3 129 < 1 < 2 8.08 1.0 50 268 114 7.70 20 < 1 0.95 5.30 1390 < 1 1.24 117 0.022< 5

< 2 < 5 < 0.3 6.32286121 < 3 131 < 1 < 2 8.05 0.5 47 264 109 7.70 20 < 1 0.89 5.32 1350 < 1 1.24 112 0.022< 5

< 2 < 5 0.3 6.33286122 < 3 126 < 1 < 2 8.20 0.5 49 295 122 7.86 20 < 1 0.85 5.56 1380 < 1 1.33 120 0.022< 5

6 7 < 0.3 6.07286123 < 3 123 < 1 < 2 7.94 0.7 49 301 111 7.87 20 < 1 0.87 5.76 1380 < 1 1.21 127 0.021< 5

< 2 < 5 < 0.3 6.16286124 < 3 97 < 1 < 2 6.96 0.4 46 242 93 7.08 20 < 1 0.76 5.24 1130 < 1 2.19 104 0.020< 5

< 2 6 < 0.3 6.36286125 < 3 150 < 1 < 2 7.89 0.4 49 227 104 7.66 21 < 1 1.16 4.96 1310 < 1 1.45 93 0.023< 5

< 2 < 5 < 0.3 4.27286126 < 3 126 < 1 < 2 7.09 0.8 44 280 105 7.11 19 < 1 1.00 4.27 1280 < 1 1.27 94 0.019< 5

< 2 < 5 < 0.3 4.89286127 < 3 125 < 1 < 2 7.63 1.1 42 299 92 6.50 19 < 1 1.15 4.54 1220 < 1 1.49 91 0.016< 5

2 < 5 0.4 6.09286128 10 133 < 1 < 2 7.71 0.6 43 321 102 6.98 20 3 1.26 4.79 1240 < 1 1.35 95 0.021< 5

3 < 5 < 0.3 6.11286129 < 3 144 < 1 < 2 7.56 0.5 44 307 101 6.47 18 < 1 1.23 4.69 1240 < 1 1.65 93 0.019< 5

< 2 < 5 10.9 6.04286130 < 3 121 < 1 < 2 7.54 < 0.3 42 279 103 6.53 19 < 1 1.21 5.02 1200 < 1 1.66 98 0.018< 5

< 2 < 5 0.3 6.28286131 < 3 190 < 1 < 2 7.86 0.4 41 298 106 6.80 18 < 1 1.42 5.04 1230 < 1 1.21 108 0.019< 5

< 2 < 5 < 0.3 6.27286132 < 3 140 < 1 < 2 7.78 < 0.3 44 276 99 7.18 18 < 1 1.28 4.94 1270 < 1 1.67 96 0.021< 5

< 2 < 5 < 0.3 6.40286133 < 3 137 < 1 < 2 7.86 1.1 44 236 114 7.35 20 < 1 1.13 5.08 1340 < 1 1.88 88 0.030< 5

4 < 5 0.3 6.21286134 < 3 139 < 1 < 2 7.60 < 0.3 45 297 119 7.46 20 < 1 1.17 5.09 1350 < 1 1.78 96 0.021< 5

58 102286135 147

3 < 5 0.3 6.17286136 < 3 173 < 1 < 2 7.41 0.6 47 293 124 7.31 19 < 1 1.23 4.97 1360 < 1 1.70 90 0.020< 5

2 < 5 0.4 4.07286137 < 3 49 < 1 < 2 6.75 < 0.3 43 381 80 6.18 19 < 1 0.15 4.33 1040 < 1 1.99 104 0.019< 5

4 < 5 < 0.3 6.15286138 < 3 145 < 1 < 2 7.27 0.9 43 338 111 7.26 22 < 1 1.28 5.14 1360 < 1 1.76 95 0.020< 5

2 < 5 < 0.3 6.21286139 < 3 157 < 1 < 2 7.76 0.6 45 297 111 7.44 20 < 1 1.05 5.27 1380 < 1 1.36 95 0.021< 5

< 2 < 5 0.4 6.39286140 < 3 162 < 1 < 2 7.77 0.5 47 291 111 7.59 20 < 1 1.07 5.35 1420 < 1 1.38 99 0.021< 5

2 < 5 < 0.3 6.65286141 < 3 242 < 1 < 2 7.10 1.2 44 310 113 7.14 20 < 1 1.02 5.86 1460 < 1 1.52 103 0.022< 5

< 2 < 5 0.3 6.63286142 < 3 141 < 1 < 2 7.63 0.6 46 296 111 7.28 20 < 1 0.84 5.68 1350 < 1 1.38 103 0.021< 5

3 < 5 < 0.3 6.22286143 < 3 127 < 1 < 2 5.04 0.6 45 361 110 6.81 19 < 1 0.63 6.27 1210 < 1 2.14 103 0.020< 5

3 < 5 < 0.3 6.18286144 < 3 103 < 1 < 2 6.70 0.5 45 347 106 6.98 18 < 1 0.47 5.71 1220 < 1 1.59 105 0.020< 5

< 2 < 5 0.4 6.67286145 < 3 216 1 < 2 5.26 < 0.3 38 316 87 6.06 21 < 1 0.74 3.93 920 < 1 2.41 102 0.041< 5

2 < 5 0.5 3.02286146 < 3 262 1 < 2 1.19 < 0.3 24 198 53 4.58 24 < 1 0.73 1.58 595 1 2.92 90 0.067< 5

Page 3 of 13




< 3 < 5 40 131286065 < 2 0.22 < 5 10 128 < 5 13 48 33 45.27 14.76 9.19 0.124 10.00 7.29 1.32 2.19 0.60 0.050.08

4 < 5 37 97286066 8 0.37 7 < 10 179 < 5 11 63 470.02

< 3 < 5 37 84286067 16 0.36 < 5 10 187 < 5 13 59 470.04

< 3 < 5 40 192286068 4 0.39 < 5 < 10 206 < 5 13 63 490.04

< 3 < 5 40 206286069 < 2 0.39 < 5 < 10 203 < 5 13 51 500.07

18 < 5 34 196286070 < 2 0.37 < 5 < 10 175 < 5 13 50 88 52.17 14.50 8.08 0.118 8.45 6.24 2.31 1.61 0.56 0.090.10

13 < 5 15 371286071 2 0.38 < 5 < 10 111 < 5 16 106 1890.43

14 < 5 15 415286072 < 2 0.38 < 5 < 10 115 < 5 14 64 1790.31

17 < 5 22 434286073 < 2 0.40 < 5 < 10 112 < 5 22 75 1860.34

12 < 5 15 370286074 < 2 0.38 < 5 < 10 114 < 5 14 79 1740.32

286075

9 < 5 15 365286076 < 2 0.40 < 5 < 10 119 < 5 14 64 1920.36

7 < 5 18 280286077 3 0.38 < 5 < 10 126 < 5 18 71 1940.26

13 < 5 13 252286078 5 0.33 < 5 < 10 91 < 5 30 46 2060.20

9 < 5 15 261286079 < 2 0.31 < 5 < 10 94 < 5 19 58 1970.22

16 < 5 15 325286080 < 2 0.30 < 5 < 10 89 < 5 16 83 167 62.55 15.26 6.63 0.085 3.68 2.06 2.89 3.24 0.59 0.180.26

16 < 5 13 316286081 < 2 0.27 9 < 10 80 < 5 21 67 2870.23

11 < 5 14 304286082 < 2 0.32 < 5 < 10 90 < 5 14 64 1520.25

9 < 5 15 291286083 3 0.34 < 5 < 10 99 < 5 14 63 1630.25

6 < 5 8 180286084 3 0.34 < 5 < 10 96 < 5 6 51 1650.14

8 < 5 11 295286085 < 2 0.38 < 5 < 10 110 < 5 11 68 161 63.39 14.95 6.75 0.090 3.64 2.04 3.09 2.63 0.59 0.190.29

12 < 5 13 321286086 < 2 0.33 < 5 < 10 121 < 5 19 79 1720.53

5 < 5 14 252286087 < 2 0.38 6 < 10 106 < 5 15 60 2120.43

15 < 5 14 335286088 < 2 0.38 < 5 < 10 110 < 5 16 54 1860.46

4 < 5 14 360286089 < 2 0.36 < 5 < 10 104 < 5 15 57 1840.24

8 < 5 14 351286090 < 2 0.34 < 5 < 10 100 < 5 15 55 1660.24

5 < 5 14 297286091 < 2 0.28 < 5 < 10 82 < 5 16 50 1590.26

< 3 < 5 15 278286092 8 0.31 < 5 < 10 93 < 5 15 58 1550.27

< 3 < 5 16 217286093 < 2 0.32 < 5 < 10 95 < 5 16 52 1570.24

6 < 5 14 179286094 5 0.29 < 5 10 122 < 5 9 42 950.10

4 < 5 33 161286095 < 2 0.37 < 5 < 10 198 < 5 11 54 48 49.13 14.67 10.22 0.169 9.34 11.34 1.67 0.67 0.61 0.060.10

< 3 < 5 41 164286096 4 0.37 10 < 10 201 < 5 12 55 470.10

3 < 5 43 212286097 4 0.42 < 5 < 10 211 < 5 13 46 540.12

< 3 < 5 42 203286098 6 0.41 < 5 < 10 213 < 5 13 52 520.12

< 3 < 5 42 220286099 7 0.37 < 5 < 10 201 < 5 12 65 480.11

< 3 < 5 41 222286100 3 0.36 < 5 < 10 199 < 5 11 57 44 48.93 14.97 9.76 0.168 8.41 11.57 1.61 1.46 0.56 0.050.10

4 < 5 40 202286101 < 2 0.31 < 5 < 10 180 < 5 10 53 410.09

4 < 5 42 209286102 2 0.31 < 5 < 10 184 < 5 10 50 400.16

< 3 < 5 41 209286103 < 2 0.31 < 5 < 10 183 < 5 10 48 410.11

3 < 5 39 227286104 3 0.32 < 5 < 10 181 < 5 10 51 400.12

286105

< 3 < 5 38 239286106 < 2 0.28 < 5 10 151 < 5 11 50 380.10

< 3 < 5 39 231286107 < 2 0.34 5 < 10 182 < 5 12 55 440.10

< 3 < 5 40 227286108 < 2 0.37 < 5 < 10 194 < 5 12 59 480.09

< 3 < 5 39 230286109 2 0.37 < 5 < 10 192 < 5 12 54 480.09

< 3 < 5 40 240286110 < 2 0.38 < 5 < 10 195 < 5 12 56 49 48.77 15.45 9.75 0.164 7.86 11.04 2.09 1.54 0.60 0.050.10

< 3 < 5 39 251286111 12 0.37 6 10 193 < 5 12 56 470.10

5 < 5 40 222286112 < 2 0.39 < 5 < 10 200 < 5 12 60 520.10

4 < 5 43 208286113 7 0.44 < 5 < 10 218 < 5 14 66 590.12

< 3 < 5 41 221286114 < 2 0.41 < 5 < 10 209 < 5 14 52 550.10

3 < 5 40 214286115 7 0.40 < 5 < 10 204 < 5 12 56 50 48.57 14.78 10.39 0.172 8.67 10.87 1.83 1.33 0.63 0.050.10

4 < 5 25 207286116 2 0.37 < 5 10 189 < 5 9 71 440.09

Page 4 of 13




4 < 5 40 280286117 < 2 0.39 < 5 < 10 189 < 5 12 76 500.09

< 3 < 5 40 201286118 3 0.37 < 5 < 10 195 < 5 13 62 500.10

< 3 < 5 42 195286119 < 2 0.41 < 5 < 10 207 < 5 13 65 530.10

< 3 < 5 41 197286120 4 0.41 < 5 < 10 207 < 5 13 66 540.10

< 3 < 5 41 193286121 < 2 0.41 < 5 < 10 207 < 5 13 61 530.10

< 3 < 5 42 187286122 < 2 0.42 < 5 10 213 < 5 13 62 550.11

< 3 < 5 43 183286123 < 2 0.40 < 5 < 10 206 < 5 13 61 510.10

< 3 < 5 38 169286124 < 2 0.39 < 5 < 10 196 < 5 13 52 570.09

< 3 < 5 42 215286125 6 0.42 < 5 10 207 < 5 14 55 57 48.80 14.95 10.58 0.164 8.37 11.01 1.88 1.29 0.67 0.060.10

< 3 < 5 22 195286126 7 0.38 7 < 10 205 < 5 8 52 440.10

< 3 < 5 26 206286127 < 2 0.33 7 < 10 192 < 5 8 51 380.09

< 3 < 5 39 209286128 < 2 0.37 < 5 < 10 193 < 5 12 53 470.10

< 3 < 5 38 208286129 < 2 0.35 < 5 < 10 182 < 5 11 53 440.09

< 3 < 5 39 204286130 6 0.35 < 5 < 10 186 < 5 11 48 43 48.97 14.56 9.53 0.164 8.88 11.04 2.19 1.44 0.57 0.050.10

< 3 < 5 41 218286131 < 2 0.35 < 5 < 10 188 < 5 11 59 450.10

< 3 < 5 42 226286132 4 0.36 < 5 < 10 196 < 5 12 52 470.11

< 3 < 5 43 224286133 < 2 0.41 6 10 215 < 5 14 53 520.12

< 3 < 5 42 215286134 3 0.39 < 5 < 10 210 < 5 12 54 490.11

286135

3 < 5 42 218286136 3 0.39 < 5 < 10 208 < 5 12 56 490.11

4 < 5 20 432286137 < 2 0.33 7 < 10 186 < 5 8 49 400.12

< 3 < 5 41 208286138 < 2 0.28 5 < 10 162 < 5 12 53 390.11

< 3 < 5 42 181286139 < 2 0.40 7 < 10 210 < 5 13 57 510.11

< 3 < 5 43 182286140 < 2 0.40 < 5 < 10 213 < 5 13 59 52 49.02 14.42 10.45 0.177 8.91 10.78 1.73 1.19 0.62 0.050.10

< 3 < 5 43 223286141 < 2 0.42 < 5 < 10 215 < 5 14 53 540.11

< 3 < 5 43 179286142 8 0.40 < 5 10 212 < 5 13 58 510.12

< 3 < 5 41 205286143 < 2 0.39 < 5 < 10 200 < 5 12 55 490.12

6 < 5 39 185286144 8 0.36 < 5 < 10 190 < 5 11 54 450.10

7 < 5 30 219286145 < 2 0.29 6 10 145 < 5 14 49 87 53.81 15.52 8.82 0.119 6.59 7.52 3.12 0.88 0.62 0.110.17

7 < 5 4 228286146 4 0.37 < 5 < 10 122 < 5 6 52 1770.20

Page 5 of 13




0.05 8.76286065 99.60

286066

286067

286068

286069

0.04 4.50286070 98.67

286071

286072

286073

286074

286075

286076

286077

286078

286079

0.03 2.23286080 99.42

286081

286082

286083

286084

0.03 2.11286085 99.50

286086

286087

286088

286089

286090

286091

286092

286093

286094

0.05 1.95286095 99.88

286096

286097

286098

286099

0.05 2.16286100 99.70

286101

286102

286103

286104

286105

286106

286107

286108

286109

0.04 2.36286110 99.72

286111

286112

286113

286114

0.04 2.32286115 99.65

286116

Page 6 of 13




286117

286118

286119

286120

286121

286122

286123

286124

0.04 2.02286125 99.84

286126

286127

286128

286129

0.04 2.71286130 100.1

286131

286132

286133

286134

286135

286136

286137

286138

286139

0.05 2.22286140 99.62

286141

286142

286143

286144

0.04 2.40286145 99.55

286146

Page 7 of 13




31.6 2.16GXR-1 Meas 442 735 1 1380 0.91 3.3 8 16 1240 23.9 13 4 0.04 0.23 871 15 0.05 43 0.06231.0 3.52GXR-1 Cert 427 750 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 0.217 852 18.0 0.0520 41.0 0.0650

< 0.3 7.98DNC-1 Meas < 3 101 < 1 < 2 7.98 56 201 105 7.31 19 0.20 5.98 1120 < 1 1.52 250 0.0270.0270 9.69DNC-1 Cert 0.200 114 1.00 0.0200 8.06 54.7 285 96.0 6.94 15.0 0.190 6.06 1150 0.700 1.39 247 0.0370


3.3 5.91GXR-4 Meas 96 544 2 14 1.04 < 0.3 12 67 6390 2.85 23 < 1 2.08 1.70 151 314 0.48 36 0.1324.00 7.20GXR-4 Cert 98.0 1640 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 1.66 155 310 0.564 42.0 0.12017.1 10.3GXR-2 Meas 16 > 1000 2 < 2 0.92 4.0 8 43 79 1.74 38 2 1.32 0.80 949 1 0.54 19 0.05917.0 16.5GXR-2 Cert 25.0 2240 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 0.850 1010 2.10 0.556 21.0 0.105

< 0.3 6.66SDC-1 Meas < 3 630 4 < 2 1.11 < 0.3 17 67 31 4.69 2.73 1.02 890 < 1 1.55 36 0.0560.0410 8.34SDC-1 Cert 0.220 630 3.00 2.60 1.00 0.0800 17.9 64.0 30.0 4.82 2.72 1.02 883 0.250 1.52 38.0 0.0690

0.3 6.04SCO-1 Meas < 3 566 2 < 2 1.94 0.4 11 77 29 3.55 2.35 1.60 394 < 1 0.68 28 0.0860.134 7.24SCO-1 Cert 12.4 570 1.84 0.370 1.87 0.140 10.5 68.0 28.7 3.59 2.30 1.64 410 1.37 0.670 27.0 0.0900

0.5 10.5GXR-6 Meas 268 > 1000 1 < 2 0.18 1.0 16 95 70 5.40 38 < 1 1.87 0.59 1080 < 1 0.09 25 0.0361.30 17.7GXR-6 Cert 330 1300 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 0.609 1010 2.40 0.104 27.0 0.0350

FK-N MeasFK-N CertBE-N MeasBE-N CertOREAS 13P Meas 2510 7.11 2020OREAS 13P Cert 2500 7.58 2260SGR-1b MeasSGR-1b Cert






0.3 5.84286068 Orig < 3 756 < 1 < 2 3.78 0.9 44 212 49 7.21 19 < 1 2.04 7.05 964 < 1 0.99 104 0.0210.3 5.83286068 Dup < 3 746 < 1 < 2 3.79 0.8 44 227 48 7.10 19 < 1 2.03 7.03 963 < 1 0.98 103 0.021

< 2 9286074 Orig < 53 < 5286074 Dup < 5

< 2 < 5286084 Orig < 53 < 5286084 Dup < 5

0.5 6.44286090 Orig < 3 222 2 < 2 1.68 < 0.3 21 198 52 4.14 25 < 1 0.89 2.34 494 < 1 2.92 82 0.0680.5 6.48286090 Dup < 3 222 2 < 2 1.68 < 0.3 21 195 53 4.20 24 < 1 0.89 2.33 493 < 1 2.95 82 0.068

< 2 < 5 < 0.3 5.26286094 Orig < 3 347 < 1 < 2 3.85 < 0.3 25 216 70 4.47 23 4 1.44 2.81 701 < 1 2.60 73 0.040< 58 < 5 < 0.3 4.82286094 Split < 3 339 < 1 < 2 3.82 < 0.3 24 216 65 4.35 22 < 1 1.39 2.82 672 < 1 2.51 71 0.038< 5

< 2 < 5286095 Orig < 52 < 5286095 Dup < 56 < 5286109 Orig < 5

< 2 < 5286109 Dup < 54 < 5 0.4 6.38286114 Orig < 3 130 < 1 < 2 8.01 0.4 46 268 103 7.56 20 < 1 1.07 5.14 1340 < 1 1.41 100 0.022< 5

< 2 7 < 0.3 6.22286114 Split < 3 125 < 1 < 2 7.73 1.1 42 267 104 7.19 20 < 1 1.02 4.94 1290 < 1 1.36 97 0.02160.3 6.11286118 Orig < 3 119 < 1 < 2 7.55 < 0.3 47 373 104 7.33 20 < 1 1.00 5.24 1380 < 1 1.30 112 0.021

< 0.3 6.25286118 Dup < 3 122 < 1 < 2 7.73 0.6 46 321 106 7.47 20 < 1 1.02 5.36 1370 < 1 1.33 115 0.021< 2 < 5286119 Orig < 5< 2 < 5286119 Dup < 5< 2 < 5 < 0.3 6.16286124 Orig < 3 97 < 1 < 2 6.96 0.4 46 242 93 7.08 20 < 1 0.76 5.24 1130 < 1 2.19 104 0.020< 5

3 6 < 0.3 6.22286124 Split < 3 96 < 1 < 2 6.95 < 0.3 44 245 94 6.97 20 < 1 0.76 5.22 1130 < 1 2.20 103 0.020< 5< 2 < 5286130 Orig < 5

Page 8 of 13




< 2 < 5286130 Dup < 50.4 6.15286132 Orig < 3 140 < 1 < 2 7.77 0.9 46 272 98 7.18 19 < 1 1.28 4.94 1270 < 1 1.63 96 0.021

< 0.3 6.40286132 Dup < 3 140 < 1 < 2 7.79 < 0.3 41 281 101 7.17 18 < 1 1.27 4.95 1280 < 1 1.70 96 0.0203 < 5286144 Orig < 52 < 5286144 Dup < 5


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 9 1 < 0.01 < 1 < 1 < 0.01 < 0.01 23 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 5 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 5 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 6 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 5 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 6 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 11 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 7 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 11 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 11 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 9 < 1 < 0.01 < 1 < 0.001


< 5


< 5


< 5


< 5


< 5


Page 9 of 13




770 21 < 4 294GXR-1 Meas 18 < 5 40 87 158 31 753 370.26730 122 1.58 275GXR-1 Cert 13.0 0.390 34.9 80.0 164 32.0 760 38.00.257

4 < 5 30 138DNC-1 Meas 0.31 < 5 < 10 148 < 5 17 57 500.066.30 0.960 31.0 145DNC-1 Cert 0.287 0.0260 0.100 148 0.200 18.0 66.0 41.00.0390


39 < 5 8 214GXR-4 Meas < 2 < 5 < 10 84 37 16 68 621.7752.0 4.80 7.70 221GXR-4 Cert 0.970 3.20 6.20 87.0 30.8 14.0 73.0 1861.77657 14 6 149GXR-2 Meas < 2 < 5 < 10 46 < 5 17 525 1800.03690 49.0 6.88 160GXR-2 Cert 0.690 1.03 2.90 52.0 1.90 17.0 530 2690.031322 < 5 15 177SDC-1 Meas 0.11 34 < 5 37 102 370.06

25.0 0.540 17.0 183SDC-1 Cert 0.606 102 0.800 40.0 103 2900.065024 < 5 12 166SCO-1 Meas 0.38 134 < 5 22 100 152

31.0 2.50 10.8 174SCO-1 Cert 0.380 131 1.40 26.0 103 16094 < 5 28 39GXR-6 Meas < 2 7 < 10 123 < 5 14 130 1010.02

101 3.60 27.6 35.0GXR-6 Cert 0.0180 2.20 1.54 186 1.90 14.0 118 1100.0160FK-N Meas 64.75 18.75 0.10 0.006 0.04 0.07 2.49 12.64 < 0.01 0.02FK-N Cert 65.0 18.6 0.0900 0.00500 0.0100 0.110 2.58 12.8 0.0200 0.0240BE-N Meas 38.08 9.99 0.191 13.18 13.99 3.17 1.36 2.67 1.03BE-N Cert 38.2 10.1 0.200 13.1 13.9 3.18 1.39 2.61 1.05OREAS 13P MeasOREAS 13P CertSGR-1b Meas 28.69 6.81 3.06 4.51 8.57 3.11 1.57 0.25 0.28SGR-1b Cert 28.24 6.52 3.03 4.44 8.38 2.99 1.66 0.253 0.328CDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert

< 3 < 5 40 191286068 Orig 5 0.39 < 5 < 10 204 < 5 13 63 490.045 < 5 40 193286068 Dup 3 0.39 < 5 < 10 207 < 5 13 63 490.04

286074 Orig286074 Dup286084 Orig286084 Dup

7 < 5 14 352286090 Orig < 2 0.34 < 5 < 10 100 < 5 15 54 1600.249 < 5 14 350286090 Dup 2 0.34 < 5 10 101 < 5 15 56 1730.246 < 5 14 179286094 Orig 5 0.29 < 5 10 122 < 5 9 42 950.107 < 5 13 169286094 Split < 2 0.28 < 5 10 119 < 5 8 43 910.10

286095 Orig286095 Dup286109 Orig286109 Dup

< 3 < 5 41 221286114 Orig < 2 0.41 < 5 < 10 209 < 5 14 52 550.104 < 5 39 211286114 Split < 2 0.30 < 5 < 10 154 < 5 13 50 420.10

< 3 < 5 39 199286118 Orig 2 0.39 < 5 10 197 < 5 12 61 500.105 < 5 41 203286118 Dup 3 0.35 < 5 < 10 192 < 5 13 64 510.10

286119 Orig286119 Dup

< 3 < 5 38 169286124 Orig < 2 0.39 < 5 < 10 196 < 5 13 52 570.094 < 5 37 168286124 Split < 2 0.38 < 5 < 10 197 < 5 13 51 570.10

286130 Orig

Page 10 of 13




286130 Dup< 3 < 5 42 224286132 Orig 4 0.39 < 5 < 10 207 < 5 13 51 490.11< 3 < 5 42 227286132 Dup 4 0.34 < 5 < 10 185 < 5 12 53 450.11

286144 Orig286144 Dup


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01

Method Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

< 0.01 < 0.01 < 0.01 < 0.001 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01

Page 11 of 13




GXR-1 MeasGXR-1 CertDNC-1 MeasDNC-1 Cert


GXR-4 MeasGXR-4 CertGXR-2 MeasGXR-2 CertSDC-1 MeasSDC-1 CertSCO-1 MeasSCO-1 CertGXR-6 MeasGXR-6 CertFK-N MeasFK-N Cert


OREAS 13P MeasOREAS 13P CertSGR-1b MeasSGR-1b CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert286068 Orig286068 Dup286074 Orig286074 Dup286084 Orig286084 Dup286090 Orig286090 Dup286094 Orig286094 Split286095 Orig286095 Dup286109 Orig286109 Dup286114 Orig286114 Split286118 Orig286118 Dup286119 Orig286119 Dup286124 Orig286124 Split286130 Orig

Page 12 of 13




286130 Dup286132 Orig286132 Dup286144 Orig286144 DupMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank


< 0.01

Page 13 of 13

CER

TIFICA

TE OF A

NA

LYSIS


uality Analysis ...

Invoice No.:

Invoice Date:

Date Subm

itted:

Your Reference:

25-Mar-10

09-Mar-10

A10-1039

Mega U

ranium Ltd.


C V8V 3K

5C

anada

Tony Gilm

anA

TTN:






aterial, it will be




itted for analysis.

AC

TIVATIO

N LA

BO

RA

TOR

IES LTD.

1336 Sandhill D

rive, Ancaster, O

ntario Canada L9G

4V5 TELEP

HO

NE

+1.905.648.9611 or +1.888.228.5227 FA

X +1.905.648.9613E-M

AIL ancaster@

actlabsint.com A

CTLA

BS G

RO

UP W

EB

SITE

http://ww

w.actlabsint.com

Em

manuel E

seme , P

h.D.

CER

TIFIED B

Y :

RE

PO

RT

A10-1039

Notes:

64 Rock sam

ples were subm

itted for analysis.

Code 1C

-Exp IC

PO

ES


OE

SC


P(TO

TAL)

Code 4C

(11+) Whole R

ock Analysis-X

RF

Values w


bers.

Quality C

ontrol


ere requested:

PO N

umber:




3 < 5 < 0.3 6.12286001 < 3 171 1 < 2 4.64 1.3 46 343 120 6.96 20 < 1 0.70 6.89 935 < 1 1.38 109 0.021< 5

4 < 5 < 0.3 5.92286002 < 3 181 < 1 < 2 4.06 < 0.3 42 291 107 6.91 19 < 1 0.87 6.83 929 < 1 1.40 97 0.020< 5

< 2 < 5 < 0.3 5.75286003 < 3 313 < 1 < 2 3.92 < 0.3 43 303 110 7.15 19 < 1 1.03 7.07 996 1 1.50 94 0.020< 5

4 < 5 < 0.3 3.34286004 < 3 275 < 1 < 2 4.13 0.8 40 351 107 5.53 17 < 1 0.98 4.69 1010 < 1 1.51 92 0.014< 5

< 2 < 5 0.3 4.62286005 < 3 207 < 1 < 2 5.50 0.7 43 335 113 6.90 19 < 1 1.26 5.38 1190 < 1 1.82 94 0.022< 5

< 2 < 5 0.3 6.04286006 < 3 238 < 1 < 2 5.03 < 0.3 41 254 108 7.14 23 < 1 1.01 6.43 1090 < 1 1.96 92 0.018< 5

< 2 < 5 < 0.3 6.68286007 < 3 194 < 1 < 2 6.34 1.0 43 273 123 6.98 19 < 1 1.43 6.14 1170 < 1 1.41 104 0.019< 5

4 < 5 < 0.3 6.57286008 < 3 385 < 1 < 2 5.49 0.5 42 286 103 6.73 18 < 1 1.31 6.63 1010 < 1 1.46 107 0.017< 5

< 2 < 5 < 0.3 6.43286009 < 3 243 < 1 < 2 6.04 1.2 44 284 106 6.56 19 < 1 1.30 6.35 1100 < 1 1.71 108 0.018< 5

< 2 < 5 < 0.3 6.29286010 < 3 186 < 1 < 2 6.21 0.4 43 293 120 6.44 19 < 1 1.27 6.39 1060 < 1 1.37 115 0.018< 5

< 2 < 5 < 0.3 6.23286011 < 3 213 < 1 < 2 5.60 0.6 46 318 111 6.70 20 < 1 1.13 6.70 1080 < 1 1.48 108 0.017< 5

< 2 < 5 < 0.3 5.89286012 < 3 189 < 1 < 2 5.14 0.8 42 313 99 6.82 20 < 1 1.23 6.82 1070 < 1 1.39 98 0.018< 5

7 < 5 < 0.3 6.18286013 < 3 143 < 1 < 2 5.66 0.4 42 296 108 6.84 20 < 1 1.11 6.33 1100 < 1 1.77 100 0.019< 5

< 2 < 5 < 0.3 4.39286014 < 3 169 < 1 < 2 5.80 0.9 42 349 102 5.93 19 < 1 1.16 4.88 1100 < 1 1.12 99 0.018< 5

49 107286015 142

< 2 < 5 < 0.3 5.73286016 < 3 222 < 1 < 2 5.93 < 0.3 42 352 98 6.80 20 < 1 1.18 5.89 1200 < 1 1.59 102 0.019< 5

< 2 < 5 0.3 6.31286017 < 3 195 < 1 < 2 6.13 < 0.3 45 313 113 7.08 20 < 1 1.22 5.67 1260 < 1 1.37 97 0.020< 5

< 2 < 5 0.3 6.48286018 < 3 226 < 1 < 2 7.06 0.4 47 270 147 7.64 21 < 1 1.21 5.66 1400 < 1 1.34 115 0.022< 5

< 2 < 5 < 0.3 6.45286019 < 3 262 < 1 < 2 7.00 0.6 46 280 118 7.38 20 < 1 1.44 5.54 1330 < 1 1.27 110 0.022< 5

< 2 < 5 < 0.3 6.29286020 < 3 251 < 1 < 2 6.64 1.1 45 270 108 7.29 20 < 1 1.31 5.79 1320 < 1 1.32 110 0.021< 5

2 < 5 < 0.3 6.43286021 < 3 213 < 1 < 2 6.16 0.8 44 275 98 6.41 19 < 1 1.36 6.16 1180 < 1 1.61 110 0.014< 5

2 < 5 < 0.3 6.44286022 < 3 112 < 1 < 2 4.52 < 0.3 28 284 67 3.84 20 < 1 0.67 5.23 668 < 1 3.06 112 0.010< 5

< 2 < 5 0.4 6.09286023 < 3 63 < 1 < 2 2.77 < 0.3 17 222 43 2.31 18 < 1 0.12 3.56 357 < 1 4.76 63 0.013< 5

< 2 8 0.3 6.59286024 < 3 166 < 1 < 2 5.80 0.9 38 303 80 5.29 20 < 1 1.24 5.57 967 < 1 2.14 100 0.010< 5

< 2 < 5 < 0.3 6.42286025 < 3 176 < 1 < 2 6.30 0.6 43 294 92 6.85 20 < 1 1.20 5.59 1280 < 1 1.68 96 0.020< 5

2 < 5 0.3 4.41286026 < 3 166 < 1 < 2 5.61 < 0.3 39 309 85 6.33 20 1 1.08 4.88 1190 < 1 1.54 89 0.018< 5

< 2 < 5 < 0.3 4.85286027 < 3 181 < 1 < 2 5.69 < 0.3 40 288 95 6.48 19 < 1 1.21 4.84 1240 < 1 1.59 83 0.019< 5

2 < 5 < 0.3 6.62286028 < 3 195 < 1 < 2 6.22 1.0 45 252 99 6.94 19 < 1 1.33 5.90 1240 < 1 1.70 97 0.019< 5

< 2 < 5 0.3 6.17286029 < 3 192 < 1 < 2 6.61 < 0.3 45 243 115 7.38 20 < 1 1.40 5.92 1340 < 1 1.29 95 0.021< 5

< 2 < 5 0.3 6.29286030 < 3 200 < 1 < 2 6.32 1.1 46 237 104 7.37 20 < 1 1.43 5.74 1340 < 1 1.34 96 0.023< 5

< 2 < 5 < 0.3 6.62286031 3 213 < 1 < 2 6.16 < 0.3 45 271 111 6.77 20 < 1 1.61 6.28 1220 < 1 1.22 104 0.019< 5

< 2 5 < 0.3 6.84286032 < 3 221 < 1 < 2 6.02 0.8 43 236 117 6.71 20 < 1 1.60 5.78 1250 < 1 1.44 91 0.019< 5

< 2 < 5 < 0.3 6.34286033 < 3 219 < 1 < 2 6.07 0.4 45 288 105 7.15 21 < 1 1.39 5.73 1290 < 1 1.43 88 0.020< 5

< 2 < 5 < 0.3 6.24286034 < 3 234 < 1 < 2 5.20 0.8 45 256 108 7.09 20 < 1 1.37 5.75 1330 < 1 1.58 82 0.021< 5

< 2 < 5 < 0.3 4.36286035 < 3 173 < 1 < 2 4.92 < 0.3 40 339 111 6.60 19 < 1 1.05 5.40 1200 < 1 1.51 92 0.019< 5

< 2 < 5 < 0.3 5.07286036 < 3 146 < 1 < 2 4.81 0.6 45 330 109 7.15 20 < 1 0.86 6.27 1110 < 1 1.38 95 0.020< 5

3 5 < 0.3 5.82286037 < 3 124 < 1 < 2 6.11 0.4 43 225 107 6.70 19 < 1 0.62 5.88 1100 < 1 1.30 98 0.019< 5

< 2 < 5 0.3 6.46286038 < 3 95 < 1 < 2 8.17 1.1 49 275 117 7.31 20 < 1 0.36 5.47 1190 < 1 1.25 113 0.021< 5

< 2 < 5 0.6 6.46286039 < 3 286 2 < 2 0.98 < 0.3 19 159 67 4.38 30 < 1 1.27 1.80 455 4 3.32 62 0.027< 5

< 2 < 5 0.5 6.50286040 < 3 373 2 < 2 1.17 < 0.3 18 156 26 4.02 25 < 1 2.53 2.09 622 1 2.27 59 0.059< 5

4 < 5 0.5 6.28286041 < 3 330 4 < 2 2.94 < 0.3 19 137 52 4.13 25 < 1 2.60 2.20 745 < 1 1.45 64 0.130< 5

3 < 5 0.4 5.91286042 < 3 385 1 < 2 1.94 < 0.3 17 122 30 3.83 23 < 1 1.82 1.25 530 1 2.41 49 0.048< 5

< 2 < 5 0.5 7.10286043 < 3 504 1 < 2 1.10 1.1 29 197 11 9.57 29 3 3.27 2.26 844 < 1 2.39 87 0.066< 5

< 2 < 5 0.3 2.71286044 < 3 380 1 < 2 0.96 0.9 23 158 41 7.73 25 < 1 2.00 1.44 724 < 1 1.99 67 0.056< 5

62 104286045 128

4 < 5 0.4 8.28286046 < 3 416 1 < 2 1.63 0.4 20 148 55 5.98 25 < 1 1.88 1.69 697 1 2.03 56 0.061< 5

< 2 < 5 0.4 5.24286047 < 3 280 1 < 2 0.21 0.5 13 145 17 3.27 23 < 1 1.45 1.65 414 < 1 2.49 50 0.046< 5

< 2 < 5 0.4 5.50286048 < 3 75 2 < 2 0.44 < 0.3 19 173 5 4.27 24 < 1 0.62 2.24 581 3 2.85 70 0.075< 5

< 2 < 5 < 0.3 6.42286049 < 3 172 2 < 2 0.31 < 0.3 17 147 6 3.68 27 < 1 1.44 2.11 569 < 1 2.98 58 0.071< 5

< 2 < 5 0.5 6.90286050 < 3 435 2 < 2 1.22 < 0.3 18 170 40 3.77 24 < 1 2.17 2.20 560 < 1 2.36 60 0.069< 5

< 2 < 5 0.4 6.26286051 < 3 251 3 < 2 0.69 < 0.3 13 108 22 2.87 24 < 1 1.81 1.66 483 < 1 2.82 39 0.051< 5

4 < 5 0.3 6.54286052 < 3 341 2 < 2 0.96 < 0.3 18 131 32 3.70 24 < 1 1.83 1.86 570 < 1 2.54 59 0.067< 5

Page 2 of 13




< 2 < 5 0.3 5.87286053 < 3 559 2 < 2 0.78 < 0.3 11 62 18 2.53 22 < 1 2.35 1.27 406 1 2.30 31 0.036< 5

4 < 5 0.3 5.92286054 < 3 619 3 < 2 0.60 < 0.3 17 134 27 3.32 23 < 1 1.61 1.88 570 < 1 2.25 57 0.058< 5

< 2 < 5 0.4 3.64286055 5 537 2 < 2 0.84 < 0.3 17 167 32 3.24 25 3 1.84 1.86 627 < 1 2.25 59 0.057< 5

< 2 < 5 0.4 7.95286056 < 3 692 2 < 2 1.71 < 0.3 17 191 38 3.84 23 < 1 1.85 2.20 751 < 1 2.00 56 0.063< 5

< 2 < 5 0.4 6.07286057 < 3 638 2 < 2 1.29 < 0.3 19 155 50 3.51 25 < 1 1.51 1.85 661 < 1 2.57 66 0.064< 5

< 2 < 5 0.4 6.24286058 < 3 505 2 < 2 0.91 < 0.3 15 133 66 3.39 25 < 1 1.89 1.61 561 < 1 2.80 49 0.051< 5

< 2 < 5 0.4 6.66286059 < 3 521 3 < 2 0.56 < 0.3 17 132 31 3.97 30 < 1 2.16 2.00 646 8 3.08 69 0.045< 5

< 2 < 5 0.4 6.58286060 < 3 447 3 < 2 0.56 < 0.3 17 145 23 4.10 30 < 1 1.89 2.12 676 2 2.86 73 0.047< 5

3 < 5 0.4 6.20286061 < 3 281 2 < 2 0.52 < 0.3 19 158 20 4.24 28 1 1.54 1.86 628 3 3.09 65 0.062< 5

< 2 < 5 < 0.3 6.20286062 < 3 311 3 < 2 0.56 < 0.3 17 127 22 3.68 28 < 1 2.35 1.78 595 < 1 2.65 63 0.054< 5

< 2 < 5 < 0.3 6.31286063 < 3 435 3 < 2 0.86 0.3 17 147 21 4.01 25 < 1 2.16 1.89 762 1 2.37 47 0.059< 5

7 < 5 0.3 6.70286064 < 3 582 3 < 2 1.33 0.4 20 165 31 4.46 26 < 1 2.35 2.46 920 < 1 2.36 63 0.071< 5

Page 3 of 13




7 < 5 40 136286001 < 2 0.39 < 5 < 10 201 < 5 13 64 50 47.25 14.41 9.72 0.123 11.69 6.32 1.80 0.80 0.61 0.050.09

< 3 < 5 39 166286002 < 2 0.35 < 5 < 10 184 < 5 12 54 450.11

< 3 < 5 39 181286003 7 0.39 < 5 < 10 197 < 5 12 55 480.15

4 < 5 19 226286004 < 2 0.32 < 5 10 185 < 5 5 53 330.09

3 < 5 26 340286005 < 2 0.38 < 5 < 10 208 < 5 10 55 46 48.61 14.65 9.93 0.160 9.89 7.84 2.52 1.73 0.63 0.060.10

4 < 5 38 296286006 < 2 0.35 < 5 < 10 192 < 5 12 60 440.09

< 3 < 5 41 213286007 8 0.35 < 5 < 10 195 < 5 12 49 450.10

< 3 < 5 39 188286008 9 0.34 < 5 < 10 187 < 5 11 46 430.09

< 3 < 5 38 200286009 < 2 0.34 < 5 < 10 187 < 5 11 48 420.09

< 3 < 5 40 194286010 < 2 0.34 5 < 10 190 < 5 11 47 42 47.92 14.97 9.06 0.144 10.86 8.66 1.84 1.47 0.54 0.040.09

< 3 < 5 39 174286011 < 2 0.34 < 5 10 189 < 5 11 49 410.09

4 < 5 36 161286012 < 2 0.33 < 5 < 10 178 < 5 10 53 410.08

< 3 < 5 36 165286013 6 0.35 < 5 < 10 185 < 5 11 54 440.09

< 3 < 5 24 185286014 < 2 0.33 < 5 < 10 184 < 5 7 47 380.09

286015

4 < 5 35 237286016 < 2 0.38 5 10 196 < 5 11 51 47 48.24 14.76 9.67 0.160 10.33 8.39 2.12 1.44 0.60 0.050.09

< 3 < 5 39 211286017 < 2 0.37 6 < 10 190 < 5 12 49 480.10

< 3 < 5 41 201286018 < 2 0.41 6 < 10 209 < 5 13 57 540.12

< 3 < 5 40 216286019 5 0.40 < 5 < 10 206 < 5 13 53 530.11

< 3 < 5 41 207286020 < 2 0.39 < 5 < 10 201 < 5 12 53 51 48.68 14.52 10.26 0.176 9.89 9.22 1.72 1.51 0.62 0.060.11

< 3 < 5 39 208286021 < 2 0.30 6 < 10 183 < 5 9 49 400.08

< 3 < 5 26 176286022 3 0.16 5 10 88 < 5 5 45 530.04

< 3 < 5 17 102286023 < 2 0.14 < 5 10 50 < 5 6 26 790.05

< 3 < 5 33 216286024 < 2 0.22 7 10 140 < 5 7 45 360.06

< 3 < 5 39 206286025 4 0.39 < 5 < 10 199 < 5 12 51 50 48.66 15.02 9.84 0.175 9.71 8.88 2.20 1.45 0.63 0.050.10

< 3 < 5 25 219286026 16 0.35 < 5 < 10 187 < 5 8 49 420.09

< 3 < 5 24 241286027 5 0.35 < 5 < 10 187 < 5 9 51 440.08

< 3 < 5 40 230286028 < 2 0.36 < 5 < 10 189 < 5 12 52 470.09

< 3 < 5 39 187286029 < 2 0.39 < 5 < 10 204 < 5 12 57 500.10

5 < 5 41 192286030 2 0.41 < 5 < 10 205 < 5 13 56 530.11

< 3 < 5 40 199286031 6 0.36 < 5 < 10 194 < 5 12 55 46 47.65 15.29 9.41 0.161 10.87 8.54 1.57 1.81 0.56 0.050.10

< 3 < 5 39 222286032 5 0.35 < 5 < 10 192 < 5 12 48 460.10

< 3 < 5 41 212286033 < 2 0.39 < 5 < 10 205 < 5 12 48 480.10

< 3 < 5 39 262286034 < 2 0.40 5 < 10 205 < 5 13 62 500.10

< 3 < 5 27 207286035 11 0.35 < 5 10 190 < 5 9 51 41 48.29 14.62 9.95 0.168 10.61 7.45 2.25 1.42 0.61 0.050.10

< 3 < 5 32 175286036 < 2 0.39 6 < 10 203 < 5 10 55 460.10

< 3 < 5 38 155286037 < 2 0.37 < 5 < 10 193 < 5 12 49 470.10

15 < 5 41 145286038 6 0.38 < 5 < 10 204 < 5 12 52 490.11

8 < 5 14 258286039 6 0.38 < 5 < 10 105 < 5 9 59 1830.21

13 < 5 13 255286040 < 2 0.30 < 5 < 10 83 < 5 12 91 172 65.20 14.97 5.77 0.082 3.48 1.49 3.04 2.96 0.55 0.140.12

6 < 5 13 387286041 3 0.31 < 5 < 10 98 < 5 17 77 1500.17

10 < 5 11 388286042 < 2 0.32 < 5 < 10 86 < 5 11 64 1730.16

14 < 5 21 202286043 < 2 0.37 < 5 < 10 142 < 5 15 87 1520.07

15 < 5 6 142286044 4 0.33 < 5 < 10 113 < 5 5 71 1190.18

286045

10 < 5 20 240286046 6 0.33 < 5 < 10 98 < 5 18 62 1410.28

6 < 5 12 54286047 < 2 0.31 < 5 < 10 76 < 5 8 31 138 69.68 12.52 4.89 0.054 2.87 0.27 3.54 2.31 0.49 0.110.13

4 < 5 15 56286048 < 2 0.38 < 5 < 10 101 < 5 10 42 1560.19

< 3 < 5 11 143286049 4 0.31 < 5 < 10 84 < 5 10 42 1350.12

53 < 5 11 321286050 7 0.32 < 5 < 10 88 < 5 9 44 1350.18

14 < 5 8 176286051 < 2 0.23 < 5 < 10 59 < 5 8 33 1240.11

11 < 5 11 237286052 2 0.26 < 5 < 10 78 < 5 9 41 119 62.54 16.53 5.65 0.080 3.32 1.28 3.78 2.29 0.54 0.170.20

Page 4 of 13




17 < 5 8 168286053 < 2 0.20 < 5 < 10 58 < 5 8 27 1450.10

23 < 5 10 202286054 < 2 0.28 < 5 < 10 85 < 5 7 35 1170.16

38 < 5 4 204286055 4 0.28 < 5 < 10 87 < 5 4 37 1130.12

47 < 5 15 207286056 7 0.29 < 5 < 10 80 < 5 11 42 1290.21

71 < 5 12 251286057 < 2 0.30 < 5 < 10 92 < 5 10 49 127 62.43 15.77 5.51 0.091 3.34 1.81 3.76 2.46 0.50 0.160.23

22 < 5 9 284286058 < 2 0.23 6 < 10 69 < 5 8 28 1090.24

10 < 5 12 274286059 < 2 0.26 < 5 < 10 89 < 5 8 32 1450.11

9 < 5 13 259286060 < 2 0.23 < 5 < 10 83 < 5 9 32 1290.13

5 < 5 11 183286061 4 0.31 < 5 < 10 91 < 5 8 30 1460.27

8 < 5 11 168286062 < 2 0.22 < 5 < 10 75 < 5 9 35 115 62.46 16.42 5.38 0.080 3.04 0.75 3.83 2.81 0.47 0.130.17

6 < 5 10 169286063 6 0.28 < 5 < 10 83 < 5 8 39 1220.25

8 < 5 12 179286064 2 0.29 < 5 < 10 92 < 5 11 52 1350.21

Page 5 of 13




0.05 7.21286001 100.0

286002

286003

286004

0.04 3.99286005 100.1

286006

286007

286008

286009

0.06 4.18286010 99.74

286011

286012

286013

286014

286015

0.05 3.92286016 99.73

286017

286018

286019

0.05 2.99286020 99.70

286021

286022

286023

286024

0.04 3.32286025 99.97

286026

286027

286028

286029

286030

0.05 4.09286031 100.1

286032

286033

286034

0.05 4.53286035 100.00

286036

286037

286038

286039

0.01 2.17286040 99.86

286041

286042

286043

286044

286045

286046

0.02 2.51286047 99.27

286048

286049

286050

286051

0.02 3.16286052 99.36

Page 6 of 13




286053

286054

286055

286056

0.02 3.78286057 99.63

286058

286059

286060

286061

0.01 3.35286062 98.71

286063

286064

Page 7 of 13




31.6 2.16GXR-1 Meas 442 735 1 1380 0.91 3.3 8 16 1240 23.9 13 4 0.04 0.23 871 15 0.05 43 0.06231.0 3.52GXR-1 Cert 427 750 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 0.217 852 18.0 0.0520 41.0 0.0650

NIST 694 MeasNIST 694 Cert

< 0.3 7.98DNC-1 Meas < 3 101 < 1 < 2 7.98 56 201 105 7.31 19 0.20 5.98 1120 < 1 1.52 250 0.0270.0270 9.69DNC-1 Cert 0.200 114 1.00 0.0200 8.06 54.7 285 96.0 6.94 15.0 0.190 6.06 1150 0.700 1.39 247 0.0370


3.3 5.91GXR-4 Meas 96 544 2 14 1.04 < 0.3 12 67 6390 2.85 23 < 1 2.08 1.70 151 314 0.48 36 0.1324.00 7.20GXR-4 Cert 98.0 1640 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 1.66 155 310 0.564 42.0 0.12017.1 10.3GXR-2 Meas 16 > 1000 2 < 2 0.92 4.0 8 43 79 1.74 38 2 1.32 0.80 949 1 0.54 19 0.05917.0 16.5GXR-2 Cert 25.0 2240 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 0.850 1010 2.10 0.556 21.0 0.105

AN-G MeasAN-G Cert

< 0.3 6.66SDC-1 Meas < 3 630 4 < 2 1.11 < 0.3 17 67 31 4.69 2.73 1.02 890 < 1 1.55 36 0.0560.0410 8.34SDC-1 Cert 0.220 630 3.00 2.60 1.00 0.0800 17.9 64.0 30.0 4.82 2.72 1.02 883 0.250 1.52 38.0 0.0690

0.3 6.04SCO-1 Meas < 3 566 2 < 2 1.94 0.4 11 77 29 3.55 2.35 1.60 394 < 1 0.68 28 0.0860.134 7.24SCO-1 Cert 12.4 570 1.84 0.370 1.87 0.140 10.5 68.0 28.7 3.59 2.30 1.64 410 1.37 0.670 27.0 0.0900

0.5 10.5GXR-6 Meas 268 > 1000 1 < 2 0.18 1.0 16 95 70 5.40 38 < 1 1.87 0.59 1080 < 1 0.09 25 0.0361.30 17.7GXR-6 Cert 330 1300 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 0.609 1010 2.40 0.104 27.0 0.0350

BE-N MeasBE-N CertBX-N MeasBX-N CertUB-N MeasUB-N CertW-2a MeasW-2a CertOREAS 13P Meas 2510 7.11 2020OREAS 13P Cert 2500 7.58 2260NIST 696 MeasNIST 696 Cert





4 < 5286010 Orig < 5< 2 < 5286010 Dup < 5

< 0.3 6.21286013 Orig < 3 142 < 1 < 2 5.60 0.3 41 307 110 6.79 19 < 1 1.10 6.25 1080 < 1 1.78 99 0.019< 0.3 6.15286013 Dup < 3 144 < 1 < 2 5.72 0.5 42 286 106 6.89 20 < 1 1.11 6.40 1120 < 1 1.75 101 0.019

< 2 5286020 Orig < 52 < 5286020 Dup < 5

< 0.3 6.49286028 Orig < 3 189 < 1 < 2 6.09 0.7 44 240 97 6.77 18 < 1 1.29 5.76 1220 < 1 1.66 95 0.018< 0.3 6.75286028 Dup < 3 201 < 1 < 2 6.35 1.3 46 264 102 7.11 21 < 1 1.37 6.04 1270 < 1 1.75 99 0.020

< 2 < 5 0.3 6.29286030 Orig < 3 200 < 1 < 2 6.32 1.1 46 237 104 7.37 20 < 1 1.43 5.74 1340 < 1 1.34 96 0.023< 5< 2 < 5 < 0.3 5.16286030 Split < 3 182 < 1 < 2 5.87 0.6 45 297 100 6.76 19 < 1 1.24 5.17 1280 < 1 1.25 89 0.021< 5< 2 5286031 Orig < 5< 2 < 5286031 Dup < 5

4 < 5286046 Orig < 55 < 5286046 Dup < 5

< 2 < 5 0.5 6.90286050 Orig < 3 435 2 < 2 1.22 < 0.3 18 170 40 3.77 24 < 1 2.17 2.20 560 < 1 2.36 60 0.069< 5< 2 < 5 0.4 8.58286050 Split < 3 439 2 < 2 1.39 < 0.3 17 179 39 3.93 25 < 1 2.02 2.31 572 < 1 2.31 58 0.072< 5

0.4 6.83286050 Orig < 3 430 2 < 2 1.21 < 0.3 18 171 39 3.73 25 < 1 2.14 2.18 555 < 1 2.33 59 0.068

Page 8 of 13




0.5 6.98286050 Dup < 3 440 2 < 2 1.23 < 0.3 19 170 40 3.82 23 < 1 2.20 2.22 565 < 1 2.39 61 0.069< 2 < 5286050 Split < 5< 2 < 5286055 Orig < 5< 2 < 5286055 Dup < 5< 2 < 5 0.4 6.58286060 Orig < 3 447 3 < 2 0.56 < 0.3 17 145 23 4.10 30 < 1 1.89 2.12 676 2 2.86 73 0.047< 5< 2 < 5 0.4 6.93286060 Split < 3 456 3 < 2 0.57 < 0.3 19 141 23 4.21 29 < 1 1.80 2.14 679 4 2.91 75 0.049< 5

0.3 6.82286064 Orig < 3 583 3 < 2 1.35 0.4 20 163 31 4.50 27 < 1 2.34 2.47 929 < 1 2.37 64 0.0720.4 6.58286064 Dup < 3 581 3 < 2 1.32 0.5 20 167 30 4.42 26 < 1 2.37 2.45 910 < 1 2.35 63 0.069


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 9 1 < 0.01 < 1 < 1 < 0.01 < 0.01 23 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 5 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 5 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 6 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 5 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 6 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 11 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 7 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 11 < 1 < 0.01 < 1 < 0.001


< 3 < 7 < 1 < 2 < 0.01 < 0.3 < 1 11 < 1 < 0.01 < 1 < 1 < 0.01 < 0.01 9 < 1 < 0.01 < 1 < 0.001



< 5


< 5


< 5


< 5


< 5

Page 9 of 13




770 21 < 4 294GXR-1 Meas 18 < 5 40 87 158 31 753 370.26730 122 1.58 275GXR-1 Cert 13.0 0.390 34.9 80.0 164 32.0 760 38.00.257

NIST 694 Meas 11.54 1.95 0.78 0.014 0.41 43.65 0.98 0.52 0.14 30.37NIST 694 Cert 11.2 1.80 0.790 0.0116 0.330 43.6 0.860 0.510 0.110 30.2

4 < 5 30 138DNC-1 Meas 0.31 < 5 < 10 148 < 5 17 57 500.066.30 0.960 31.0 145DNC-1 Cert 0.287 0.0260 0.100 148 0.200 18.0 66.0 41.00.0390


39 < 5 8 214GXR-4 Meas < 2 < 5 < 10 84 37 16 68 621.7752.0 4.80 7.70 221GXR-4 Cert 0.970 3.20 6.20 87.0 30.8 14.0 73.0 1861.77657 14 6 149GXR-2 Meas < 2 < 5 < 10 46 < 5 17 525 1800.03690 49.0 6.88 160GXR-2 Cert 0.690 1.03 2.90 52.0 1.90 17.0 530 2690.0313

AN-G Meas 46.30 29.93 3.32 0.047 1.90 15.93 1.71 0.16 0.23 0.02AN-G Cert 46.30 29.8 3.36 0.040 1.79 15.90 1.63 0.13 0.22 0.01

22 < 5 15 177SDC-1 Meas 0.11 34 < 5 37 102 370.0625.0 0.540 17.0 183SDC-1 Cert 0.606 102 0.800 40.0 103 2900.0650

24 < 5 12 166SCO-1 Meas 0.38 134 < 5 22 100 15231.0 2.50 10.8 174SCO-1 Cert 0.380 131 1.40 26.0 103 160

94 < 5 28 39GXR-6 Meas < 2 7 < 10 123 < 5 14 130 1010.02101 3.60 27.6 35.0GXR-6 Cert 0.0180 2.20 1.54 186 1.90 14.0 118 1100.0160

BE-N Meas 38.27 10.03 0.203 13.16 13.90 3.21 1.40 2.72 1.06BE-N Cert 38.2 10.1 0.200 13.1 13.9 3.18 1.39 2.61 1.05BX-N Meas 7.62 54.04 23.50 0.039 0.26 0.16 0.04 0.07 2.38 0.13BX-N Cert 7.40 54.21 23.17 0.050 0.11 0.17 0.04 0.05 2.37 0.13UB-N Meas 39.68 2.89 8.34 0.125 35.53 1.22 0.17 0.03 0.10 0.01UB-N Cert 39.4 2.90 8.34 0.120 35.2 1.20 0.100 0.0200 0.110 0.0400W-2a Meas 52.18 15.43 10.91 0.169 6.42 10.85 2.28 0.63 1.09 0.13W-2a Cert 52.4 15.4 10.7 0.163 6.37 10.9 2.14 0.626 1.06 0.130OREAS 13P MeasOREAS 13P CertNIST 696 Meas 3.95 54.36 8.82 0.006 0.18 0.02 0.02 2.70 0.05NIST 696 Cert 3.79 54.5 8.70 0.00400 0.0120 0.0180 0.00900 2.64 0.0500CDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert286010 Orig286010 Dup

< 3 < 5 36 163286013 Orig 3 0.34 < 5 < 10 184 < 5 11 52 440.09< 3 < 5 37 167286013 Dup 10 0.35 < 5 10 186 7 11 55 450.09

286020 Orig286020 Dup

4 < 5 39 221286028 Orig 7 0.33 6 10 175 < 5 11 50 450.09< 3 < 5 41 239286028 Dup < 2 0.39 < 5 < 10 202 < 5 12 54 490.09

5 < 5 41 192286030 Orig 2 0.41 < 5 < 10 205 < 5 13 56 530.114 < 5 30 178286030 Split < 2 0.38 < 5 < 10 195 < 5 9 51 460.09

286031 Orig286031 Dup286046 Orig286046 Dup

53 < 5 11 321286050 Orig 7 0.32 < 5 < 10 88 < 5 9 44 1350.1857 < 5 15 349286050 Split < 2 0.33 6 < 10 88 < 5 12 42 1440.2056 < 5 11 316286050 Orig 9 0.31 < 5 < 10 88 < 5 9 44 1330.18

Page 10 of 13




50 < 5 11 326286050 Dup 5 0.32 < 5 < 10 89 < 5 9 45 1370.19286050 Split286055 Orig286055 Dup

9 < 5 13 259286060 Orig < 2 0.23 < 5 < 10 83 < 5 9 32 1290.13< 3 < 5 14 266286060 Split < 2 0.34 < 5 < 10 105 < 5 9 32 1660.15

9 < 5 12 180286064 Orig 2 0.35 < 5 < 10 104 < 5 11 51 1480.227 < 5 12 178286064 Dup 3 0.24 7 < 10 80 < 5 11 52 1210.21


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 2 < 0.01 < 5 < 10 < 2 < 5 < 1 < 1 < 5< 0.01


< 0.01 < 0.01 < 0.01 < 0.001 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01 < 0.01

Method Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

Page 11 of 13




GXR-1 MeasGXR-1 Cert

0.12NIST 694 Meas 0.10NIST 694 Cert

DNC-1 MeasDNC-1 Cert


GXR-4 MeasGXR-4 CertGXR-2 MeasGXR-2 Cert

0.01AN-G Meas 0.01AN-G Cert

SDC-1 MeasSDC-1 CertSCO-1 MeasSCO-1 CertGXR-6 MeasGXR-6 Cert


BX-N MeasBX-N Cert

0.34UB-N Meas 0.34UB-N Cert

0.02W-2a Meas 0.01W-2a Cert

OREAS 13P MeasOREAS 13P CertNIST 696 MeasNIST 696 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-15 MeasCDN-PGMS-15 CertCDN-PGMS-17 MeasCDN-PGMS-17 Cert286010 Orig286010 Dup286013 Orig286013 Dup286020 Orig286020 Dup286028 Orig286028 Dup286030 Orig286030 Split286031 Orig286031 Dup286046 Orig286046 Dup286050 Orig286050 Split286050 Orig

Page 12 of 13




286050 Dup286050 Split286055 Orig286055 Dup286060 Orig286060 Split286064 Orig286064 DupMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank


< 0.01

Method Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method BlankMethod Blank Method Blank

Page 13 of 13

Greenwich Lake 2009Prospecting DatabaseNAD83 UTM Z16N

ID WayPt x y Date Blrd or OC Sample # Magnetic Notes

STN‐1 S1 364153 5404607 Aug. 26, 2009 OC n/a nPegmatite to Migmatite with alternating dark biotite/feldspar rich layers and light medium grained pegmatite viens. OGS mapping correct at stn.

STN‐2 S2 364142 5404675 Aug. 26, 2009 OC n/a y

Black to grey; weathers rusty to grey; magnetite bearing; fine to medium grained; feldspar, hornblende, biotite; diorite (?). Strike in the area 050 deg. steeply dipping.

STN‐3 S3 364160 5404888 Aug. 26, 2009 OC n/a n

Black to green/grey; med. To coarse grained biotite/hornblende; mafic unit cut by late pegmitite veins within pink monzonite (granatoid) host rock. The mafic unit is concordant with main body.

STN‐4 S4 363901 5405222 Aug. 26, 2009 OC n/a nGreen to blue grey; fine grained; intermediate dyke cross cutting pink monzonite and trending north.

STN‐5 S5 364384 5405238 Aug. 27, 2009 OC n/a n

Confirming OGS mapping on small island at southern end of Greenwich Lake. Mapped as Unit 2 (pegmatite, migmatite, and meta‐seds.) ‐ correct. The eastern shore of this island has numerous mafic to intermediate (diorite to monzonite) with abundant hornblende, magnetite, pyroxene, and feldspar with minor olivine (?).

STN‐6 S6 364376 5405430 Aug. 27, 2009 BLDR n/a weakGreen to blue/black; med. Grained; hornblende, pyroxene, olivine, with minor magnetite; well rounded; gabbro boulder with a fresh look.

99026 99026 364154 5404881 Aug. 27, 2009 OC 99026 y

Black to green/black; medium grained; pyroxene, hornblende, biotite & dssm pyrite (1‐2%); gabbro intrusion (1.5 m by 5 m trending into lake). The outcrop is cut by a later pegmatite dyke.

99027 99027 364376 5405231 Aug. 27, 2009 BLDR 99027 y

Black to dark grey; fine to medium grained; magnetite, hornblende, pyroxene, with numerous green tinged translucent minerals (Olivine); minor dssm. Pyrite/chalco pyrite; Gabbro boulder.

STN‐7 S7 361858 5404697 Aug. 28, 2009 OCNarrow (~10 cm) N‐S trending mafic intrusion within granitoids cut by later quartz veins. Minor sulphides observed (less than 0.5 %).

99028 99028 361852 5404695 Aug. 28, 2009 OC 99028 n Black to blue/grey; fine grained ; mafic intrusion cross cutting granitoid.

STN‐8 S8 361855 5404702 Aug. 28, 2009 BLDR n/a nSmaller section of mafic material at north end of EWR 2007 trench. Similar to STN‐7.

STN‐9 S9 361870 5404713 Aug. 28, 2009 n/a n/a

RAINING HARD: Immediately E of EWR Trench 1 the ground drops off into a low area and is swampy (ressively weathered zone). This area is co‐incident with Tr2C (i.e the waypt that is the center of the magnetic anomaly associated with traverse).

STN‐10 S10 361857 5404740 Aug. 28, 2009 OC ? RAINING HARD: More mafic intrusions. Will go back and sample when rain stops.

99029 99029 361719 5404922 Aug. 29, 2009 BLDR 99029 nGreen; fine to medium grained; euhedral pyroxene in fine grained olivine matrix; mafic intrusive. BOULDER is angular to Sub‐Angular

99030 99030 361703 5405031 Aug. 29, 2009 Sub‐Crop/OC 99030 Moderately

Dark green; fine grained; sulphide rich (with some semi‐massive sulphide zones in hand sample); primarily pyroxene and olivine; ultramafic intrusive. Sample is from Subcrop with outcrop right beside sample.



STN‐11 S11 361685 5405057 Aug. 29, 2009 OC ModeratelyDark green to dark grey; very fine grained; mafic intrusive. The mafic unit cross cuts a pegmatite dyke in the area.

Tr3C Tr3C 362041 5404489 Aug. 30, 2009 BLDR n Heavily forested area.Tr4C Tr4C 362242 5404301 Aug. 30, 2009 n/a n Low lying recessively weathered swampy area.

Tr5C Tr5C 362379 5404083 Aug. 30, 2009 n/a n Low lying recessively weathered swampy area. Found Diabase sub‐crop near by.

99031 99031 362383 5404087 Aug. 30, 2009 Sub‐Crop/OC 99031 y

Black to blue/grey; very fine grained; pyroxene, olivine, magnetite, with 3‐5% sulphides dssm. Throughout and in blebs; mafic intrusion; diabase(?); the sulphides are magnetic indicating phyrotite.

Tr6C Tr6C 362540 5403783 Aug. 30, 2009 Sub‐Crop/OC weaklyBlack to blue/grey; very fine grained; pyroxene, olivine, magnetite, with trace sulphides; diabase(?).

Tr100C Tr100C 362719 5403460 Aug. 30, 2009 OC n Migmatites on high ground with nothing to easily explain the mag anomaly.

Tr13C Tr13C 363896 5403258 Aug. 31, 2009 n/a n Heavily wooded area; no oc or boulders near by. Anomaly not explained

Tr12C Tr12C 363916 5403704 Aug. 31, 2009 n/a n Heavily wooded area; no oc or boulders near by. Anomaly not explainedTr11C Tr11C 363867 5403945 Aug. 31, 2009 n/a n Heavily wooded area; no oc, fine grained mafic boulders near by. STN 12 S12 363850 5403934 Aug. 31, 2009 BLDR y Black to grey; fine grained well rounded mafic boulder.

Tr10C Tr10C 363891 5404219 Aug. 31, 2009 n/a n Heavily wooded area; no oc or boulders near by. Anomaly not explained

STN 13 S13 363708 5404776 Sept. 1, 2009 OC Y

Dark black; very fine grained; mafic intrusion in prominent N‐S trending topographic lineament; sub‐crop to outcrop; pyroxene, magnetite, trace dssm. Sulphides.

Tr9c Tr9C 363811 5404432 Sept. 1, 2009 n/a n Very prominent N‐S trending low lying swamp/stream.

Tr8C Tr8C 363720 5404790 Sept. 1, 2009 OC n

High ridge to west of Christianson fault. Several angular fine grained mafic boulders with no sulphides. Anomaly explained by near by magnetic intrusive (STN 13 & Sample 99032).

99032 99032 363712 5405033 Sept. 1, 2009 OC/Sub‐crop 99032 YBlack; weathers rusty; very fine grained; magnetic; pyroxene, magnetite, with trace dssm. Sulphides; mafic intrusive.

Tr7C Tr7C 363719 5405033 Sept. 1, 2009 OC N Migmatites co‐incident with EWR trench. Anomaly not easily explained.

STN 14 S14 361714 5405036 Sept. 2, 2009 OC Y

Dark green to black; fine grained; very fresh; olivine, pyroxene, magnetite; mafic intrusion trending N‐S ~ 1 m wide. Very close to sample 99030 with semi‐massive sulphides.

99033 99033 361785 5404876 Sept. 2, 2009 BLDR 99033 YBlack to grey/blue; fine grained; milky plag., pyroxene, magnetite; moderately to highly magnetic with dssm. Very fine grained sulphides.

99034 99034 361807 5404856 Sept. 2, 2009 OC 99034 YBlack to grey; fine grained; plagioclase laths (black fibrous) occasionally twinned, pyroxene, magnetite; mafic intrusive; blebs and dssm. Sulphides (2‐4%).



Tr23C Tr23C 364760 5411305 Sept. 3, 2009 OC YPink to cream; coarse grained; monozonite with large (1‐3 m) xenoliths of altered magnetic mafic dykes. Anomaly explained by these magnetic dykes.

Tr24C Tr24C 364917 5409939 Sept. 3, 2009 OC Y

Black fine grained and white medium to coarse grained alternating layers of quartzofeldpathic and schistose material (migmatite). The melanocratic zones of the migmatite are slightly magnetic explaining the near by small anomaly.

Tr21C Tr21C 364714 5409569 Sept. 3, 2009 OC n Fine grained melanocratic zone within migmatitie.Tr20C Tr20C 364409 5409451 Sept. 3, 2009 n/a n On edge of hill no outcrop. Low lying area 25 m west of point.

99035 99035 364336 5409439 Sept. 3, 2009 BLDR 99035 YAngular boulder 25 cm squared; fine grained mafic, olivine (?), magnetite, plagioclase, trace dssm. Cpy‐py, black to blue/green.

Tr22C Tr22C 364140 5409287 Sept. 3, 2009 BLDR NLow lying area with boulder of pegmatite, and gneiss. 50 m NW of Tr22C is a medium grained gabbro outcrop that is magnetic.

99036 99036 364120 5409308 Sept. 3, 2009 OC 99036 YMedium grained gabro outcrop; 4 m by 4m exposed, lightly magnetic; minor dssm. Sulphides throughout.

Tr16C Tr16C 363980 5409530 Sept. 3, 2009 n/a Prominent low lying N‐W trending lineament.

99037 99037 364069 5409540 Sept. 3, 2009 OC/Sub‐crop 99037 Y Fine grained mafic, light blue color, slightly magnetic, minor dssm. Sulphides.

99038 99038 364134 5409545 Sept. 3, 2009 BLDR 99038 YFine to medium grained; mafic, rusty weathered, minor dssm. Very fine grained Cpy, olivine, magnetite, feldspar. Sub‐rounded.

Tr17C Tr17C 364252 5409575 Sept. 3, 2009 BLDR N Co‐incident with creek. Pegmatite boulders.Tr18C Tr18C 365369 5409571 Sept. 3, 2009 BLDR N Low lying area.Tr19C Tr19C 364696 5409690 Sept. 3, 2009 BLDR N Low lying area.

Tr14C Tr14C 361942 5406671 Sept. 4, 2009 OC Y

Main anomaly is co‐incident with low ling swampy area adjacent to EWR trench from 2007. The trench is dominantly pink; med to coarse grained quartz monzonite to pegmatite. On the eastern edge of trench is a small (10 m long NE direction by 1 m wide) mafic intrusive that is magnetic. Sample 099040 is from this location.

STN 15 S15 361942 5406639 Sept. 4, 2009 OC YBlack to greenish; fine to medium grained; OUTCROP; MAGNETIC; pyroxene, milky to pink feldspar; trace very fine grained dssm. Sulphides; mafic intrusive.

99040 99040 361938 5406664 Sept. 4, 2009 OC 99040 Y

Black to greenish; FRESH; fine to medium grained; OUTCROP; MAGNETIC; pyroxene, milky to pink feldspar; trace very fine grained dssm. Sulphides; mafic intrusive.

STN 17 S17 361984 5406700 Sept. 4, 2009 OC YBlack to greenish; fine to medium grained; OUTCROP; MAGNETIC; pyroxene, milky to pink feldspar; trace very fine grained dssm. Sulphides; mafic intrusive.

Tr27C Tr27C 362514 5406782 Sept. 4, 2009 n/a NWooded area; adjacent to pegmatite; non‐magnetic; anomaly not easily explained.

Tr26C Tr26C 361995 5407006 Sept. 4, 2009 n/a NHigh knob of migmatite; several coarse grained altered magnetic mafic well rounded boulders.



LSE1 LSE1 364636 540592 Sept. 5, 2009 n/a N

The easter shore of Greenwich Lake at along license 3014745 is dominantly migmatite and granite boulders and out crop. The mafic boulders in the area are 1.) fine grained blue to black/green with a lot of milky plagioclase, or 2.) coarse grained hornblende rich, highly magnetic, with rusty to green plag.

99040 99040 364494 5404723 Sept. 5, 2009 OC 99040 YBlack to Greenwich; coarse grained; well rounded OUTCROP; highly magnetic; w hornblende, white to greenish plag., pyroxene, dssm. Cpy and py; Gabbro.

99041 99041 364627 5405138 Sept. 5, 2009 BLDR 99041 YGreen to dark grey; possibly chlorite altered; fine grained; plag., hornblende or pyroxene; trace dssm. very fine grained sulphides. ANGULAR BOULDER

Tr25C Tr25C 362594 5408964 Sept. 6, 2009 OC Y

Large E‐W trending mag anomaly parallel to regional trend in northeast corner of property. Anomaly explained by large volume (3‐5%) of fine grained magnetite within coarse grained; plag. + alkali feldspar, magnetite, biotite, monozonite (pegmatite).

99043 99043 362962 5409007 Sept. 6, 2009 OC 99043 YGrayish blue; very fine grained; OUTCROP; mafic intrusive with cpy, py blebs and dssm. Throughout.

99044 99044 363035 5408810 Sept. 6, 2009 OC 99044 Y

Green to dark grey; med. To coarse grained; pyroxene, hornblende, olivine(?), trace dssm sulphides; moderately magnetic, cut by qtz. pegmatite vein; slightly altered; OUTCROP.

99045 99045 363033 5408748 Sept. 6, 2009 OC 99045 Y

Green to black; coarse grained; hornblende, pyroxene, magnetite, biotite; gabbroic intrusive; trace dssm sulphides. Very similar to sample 99044 above. Cut by qtz. pegmatite veins.

Tr31C Tr31C 362983 5408778 Sept. 6, 2009 OC Y

Anomaly not easily explained TR31C is in a wooded area with migmatite outcrop near by. On the shore of Greenwich Lake near TR31C two mafic intrusives were found.

Tr33C Tr33C 363573 5409603 Sept. 7, 2009 OC weakly

Anomaly co‐incident with a pink; coarse grained; quartz monozonite; the monozonite is weakly magnetic. This may explain the weak mag anomaly in the area.

99046 99046 363260 5409564 Sept. 7, 2009 OC 99046 NGreen to grey; very fine grained; OUTCROP; mafic intrusive; trace very fine grained dssm. sulphides; non‐magnetic.

99047 99047 363247 5409369 Sept. 7, 2009 OC 99047 N Fine grained; mafic; non‐magnetic, minor dssm. Sulphides; green.

99048 99048 363290 5409247 Sept. 7, 2009 BLDR 99048 weaklyGreen to blue/grey; medium grained; BOULDER; well rounded; mafic intrusive; pyroxene, olivine, magnetite, 3‐5% dssm. Sulphides.

99049 99049 363146 5407164 Sept. 8, 2009 OC 99049 YBlack; very fine grained; mafic intrusive in low lying N‐S trending topographic lineament; on edge of monozonite outcrop; magnetic; trace dssm sulphides.

Tr28C Tr28C 363134 5407277 Sept. 8, 2009 n/a N

Co‐incident with low lying topographic depression (swamp); within 50 m of 99049; area contains several fine to medium grained; green; sub‐angular; magnetic boulders.



Tr50C Tr50C 363452 5407190 Sept. 8, 2009 n/a weaklyAlternating biotite rich and quartzofelspathic rich layers (migmatite) cut by several coarse grained weakly magnetic pegmatites.

Tr30C Tr30C 363261 5406787 Sept. 8, 2009 OC weakly White; coarse grained; plag. + alkali feldspar; pegmatites; weakly magnetic.

Tr29C Tr29C 363836 5404992 Sept. 8, 2009 OC weaklyBlack to dark grey; very fine grained; highly magnetic; OUTCROP(?)/Sub‐crop; very angular; mafic intrusive; dssm sulphides; may explain anomaly Tr29C

99050 99050 363413 5405647 Sept. 8, 2009 OC 99050 magneticBlack to dark grey; very fine grained; highly magnetic; OUTCROP(?)/Sub‐crop; very angular; mafic intrusive; dssm sulphides; may explain anomaly Tr29C

Tr15C Tr15C 362765 5404899 Sept. 9, 2009 BLDR YGrey to black; very fine grained; fresh; mafic intrusive; BOULDER; possible sb‐crop(?); very angular; highly magnetic; trace dssm sulphides.

99051 99051 362770 5404908 Sept. 9, 2009 BLDR 99051 YGrey to black; very fine grained; fresh; mafic intrusive; BOULDER; possible sb‐crop(?); very angular; highly magnetic; trace dssm sulphides.

Tr34C Tr34C 362232 5404813 Sept. 9, 2009 OC YPink to cream; medium grained; qtz. monozonite; weakly to moderately magnetic.

Tr35C Tr35C 362294 5404904 Sept. 9, 2009 OC YPink to cream; medium grained; qtz. monozonite; weakly to moderately magnetic.

99052 99052 361852 5404741 Sept. 9, 2009 OC Y

Black to steely grey; fine to medium grained; very fresh; magnetic; pyroxene, plagioclase, olivine, magnetite, hornblende; mafic intrusive; gabbro (?); dssm. and blebs. Of sulphides throughout.

Tr32C Tr32C 366162 5410226 slept. 10, 2009 OC Y Pink; medium grained; monozonite; weakly to moderately magnetic.

99039 99039 364142 5409537 Sept. 3, 2009 BLDR 99039 YMedium grained gabbro, weathered surface, magnetic, plag. Rich, hornblende, olivine (?), pyroxene, magnetite, minor dssm cpy and py, angular block.

99042 99042 364627 5405138 Sept. 4, 2009 BLDR 99042 YGreen to Dark grey; fine grained; plag., hornblende, pyroxene, possible olivine; minor to trace dssm. Sulphides; mafic intrusive.

Location:

Footage Degrees

Collar -9060 m Notes:

100 m150 m Claim No.: NTS Map:

200 m 3014745

From To0.0 30.0

30.0 66.5

66.5 105.6

105.6 117.5

117.5 120.0

120.0 138.2

138.20 150.20

150.20 169.80

MEGA URANIUM LTD. - SUMMARY LOG

51A/15

Location Map

Date Logged: Logged By:Drill Company:

Date Started:

Core Storage: 533 Field St. Thunder Bay, Ontario

Total Depth:

Migmatite

Medium Grained Foliated Mafic Intrusive; biotite rich.

Medium Grained Foliated Mafic Intrusive; biotite rich.

Quartz Monzonite

Pink Pegmatite

Water

February 20, 2010

Summary Diamond Drill Log Description

March 1, - March 7, 2010Date Completed:

March 6, 2010

Tony Gilman

Meterage

189 m 426 m

Collar Elevation:

LAKE HOLE - First attempt was cased down to 54 m and they lost the hole. Second Attempt 17 m NW was succesful.Rugged Aviation/Drilling Inc.

5404769 North0364350 EastDip of Drill Hole

Zone 16NNAD 83

Overburden

Quartz Monzonite

Project: GREENWICH LAKE

Size: BTW core

Azimuth:

N/AHole No.: GL-10-1

169.80 177.30

177.30 189.00

Quartz Monzonite

Migmatite

MEGA URANIUM LTD. - GEOLOGICAL LOGProject: GREENWICH LAKE Easting: 0364350Logged By: T. Gilman Northing: 5404769Date: February 20 - March 4, 2010 Datum & Projection: NAD 83, UTM Zone 16 N

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Comments0 30 30 WATER30 66.5 36.5 OB OVER BURDEN

66.5 92.3 25.8 QMZ Pink mg/cg sr 1

QUARTZ MONZONITE to GRANITE; Pink with grey black, medium to coarse grained; non-foliated/massive; weakly to moderately magnetic; with magnetite stringers; from 86.25 to 86.90 m fine grained pink Quartz Monzonite to granite; pervasive, weak, sericite alteration throughout.

92.3 92.5 0.2 DBf Black fg ct 15FINE GRAINED MAFIC NTRUSIVE; Black to grey; fine grained; cut by pink pegmatite dyke.

92.5 105.55 13.05 QMZ Pink mg/cg sr 2

QUARTZ MONZONITE to GRANITE; Pink with grey black, medium to coarse grained; non-foliated/massive; weakly to moderately magnetic; with magnetite stringers and veins; pervasive, weak to moderate, sericite alteration throughout.

105.55 108.58 3.03 DBf Black fg ct 55FINE GRAINED MAFIC INTRUSIVE to intermediate intrusive; Black to grey; fine to medium grained; upper contact 55 deg TCA; cut by pink, coarse grained pegmatite dykes (i.e @ 108 m)

108.58 117.52 8.94 PPEG Pink cg sharp 0 sr 1

PINK PEGMATITE to QUATRTZ MONZONITE; coasre grained to pegmatitic; non-foliated; weakly magnetic; pervasive, weak, sericite alteration; lower contact 45 deg TCA.

HOLE NO.: GL-10-1


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HOLE NO.: GL-10-1

117.52 120 2.48 DBm Black to grey fg dssm. py .05

FINE GRAINED FOLITED MAFIC INTRUSIVE to intermediate intrusive; Black to grey; fine to medium grained; cut by coarse grained pegmatite dykes; minor to trace amounts of dssm. Pyrite.

120 130 10 QMZ Pink mg/cg sr 2

QUARTZ MONZONITE to GRANITE; Pink with grey black, medium to coarse grained; non-foliated/massive; non- magnetic; ; pervasive, weak to moderate, sericite alteration throughout.

130 130.45 0.45 DBm Black to grey fg dssm. py .05

FINE GRAINED FOLIATED MAFIC INTRUSIVE to intermediate intrusive; Black to grey; fine to medium grained; cut by coarse grained pegmatite dykes; minor to trace amounts of dssm. Pyrite.

130.45 138.15 7.7 QMZ Pink/green mg/cg sr 3

QUARTZ MONZONITE to GRANITE; Pink with green, medium to coarse grained; non-foliated/massive; non- magnetic; pervasive, moderate, sericite alteration throughout.

138.15 150.2 12.05 DBm Black to grey fg dssm. py .05

MEDIUM GRAINED FOLIATED MAFIC INTRUSIVE to intermediate intrusive; Black to grey; fine to medium grained; minor to trace amounts of dssm. Pyrite; cut by numerous 5-25 cm, pink to white, pegmatite dykes (i.e @ 140 m and 148 m); Moderate, pervasive, chlorite and epidote alteration; moderately well fliated; primarily plagioclase in a biotite and muscovite ground mass.


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HOLE NO.: GL-10-1

150.2 169.8 19.6 MIGBlack and

White

fg to cg dssm. py 1

MIGMATITE; Alternating white (coarse grained pegmatitic) and black layers (fine grained); moderately to well foliated; foliation @ 45 TCA; mafic layers dominated by plagioclase, and biotite.

169.8 177.3 7.5 QMZ Pink cg ep 2QUARTZ MONZONITE to GRANITE; Pink, coasre grained; non-foliated; non-magnetic; intense epidote alteration of feldspars at contact with overlying Migmatite; weakly to non-magnetic.

177.3 189 11.7 MIGBlack and

White

fg to cg dssm. py 1

MIGMATITE; Alternating white (coarse grained pegmatitic) and black layers (fine grained); moderately to well foliated; foliation @ 45 TCA; mafic layers dominated by plagioclase, and biotite.

MEGA URANIUM LTD. - SAMPLE RECORDProject: GREENWICH LAKELogged By: Tony GilmanDate: February 20 - March 6, 2010

SAMPLE DETAILSSample Depth Depth Sample Rock Lab Lab Lab Sample Lab

QA/QCNumber From To Interval Code Package Package Package Type Batch

1 2 2286047 105.50 106.50 1.00 DBf 1C Exploration 1F-2 4C COMP A10-1039286048 106.50 107.65 1.15 DBf 1C Exploration 1F-2 COMP A10-1039286049 117.50 118.50 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286050 118.50 119.50 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286051 119.50 120.50 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286052 138.20 139.20 1.00 DBf 1C Exploration 1F-2 4C COMP A10-1039286053 139.20 140.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286054 140.20 141.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286055 141.20 142.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286056 142.20 143.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286057 143.20 144.20 1.00 DBf 1C Exploration 1F-2 4C COMP A10-1039286058 144.20 145.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286059 145.20 146.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286060 146.20 147.20 1.00 1C Exploration 1F-2 COMP A10-1039 DUPLICATE286061 146.20 147.20 1.00 1C Exploration 1F-2 COMP A10-1039286062 147.20 148.20 1.00 DBf 1C Exploration 1F-2 4C COMP A10-1039286063 148.20 149.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039286064 149.20 150.20 1.00 DBf 1C Exploration 1F-2 COMP A10-1039

HOLE NO.: GL-10-1

MEGA URANIUM LTD. - GEOTECH LOGProject: GREENWICH LAKELogged By: Mike McNeillDate: March 3 - 8, 2010

From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)66.45 69 2.55 83.6% 1.73 56.7%69 72 3 100.0% 2.53 84.3%72 75 3 100.0% 2.3 76.7%75 78 3 100.0% 2.37 79.0%78 81 3 100.0% 2.16 72.0%81 84 2.92 97.3% 2.59 86.3%84 87 3 100.0% 2.73 91.0%87 90 3 100.0% 2.6 86.7%90 93 3 100.0% 2.01 67.0%93 96 3 100.0% 2.52 84.0%96 99 2.9 96.7% 2.67 89.0%99 102 3 100.0% 2.38 79.3%102 105 3 100.0% 2.93 97.7%105 108 2.83 94.3% 2.58 86.0%108 111 2.94 98.0% 2.54 84.7%111 114 2.97 99.0% 2.45 81.7%114 117 2.96 98.7% 2.42 80.7%117 120 2.88 96.0% 1.75 58.3%120 123 3 100.0% 2.55 85.0%123 126 3 100.0% 2.71 90.3%126 129 2.93 97.7% 2.62 87.3%129 132 2.93 97.7% 2.39 79.7%132 135 3 100.0% 2.47 82.3%135 138 2.99 99.7% 2.54 84.7%138 141 2.7 90.0% 1.75 58.3%141 144 2.95 98.3% 2.44 81.3%144 147 3 100.0% 2.5 83.3%147 150 3 100.0% 2.9 96.7%150 153 3 100.0% 2.78 92.7%153 156 2.82 94.0% 2.66 88.7%156 159 2.9 96.7% 2.9 96.7%159 162 3 100.0% 2.29 76.3%162 165 3 100.0% 2.33 77.7%165 168 2.79 93.0% 2.45 81.7%168 171 2.98 99.3% 2.47 82.3%171 174 2.82 94.0% 2.8 93.3%174 177 2.93 97.7% 2.68 89.3%177 180 2.98 99.3% 2.2 73.3%180 183 3 100.0% 2.13 71.0%183 186 3 100.0% 2.53 84.3%

HOLE NO.: GL-10-1

Meterage Recovery RQD

MEGA URANIUM LTD. - GEOTECH LOGProject: GREENWICH LAKELogged By: Mike McNeillDate: March 3 - 8, 2010

From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)

HOLE NO.: GL-10-1


186 189 3 100.0% 2.31 77.0%EOH EOH EOH EOH EOH EOH

MEGA URANIUM LTD. - DH GeophysicsProject: GREENWICH LAKELogged By: Mike McNeillDate: March 3 - 8, 2010Mag Sus: KT-9, Core Diamater Set to: 4.00

Meter Mag Susc. CPS (>500) Comments66 0.047

68 0.055

70 0.032

72 0.183

74 0.046

76 0.033

78 0.045

80 0.06

82 0.045

84 0.049

86 0.025

88 0.055

90 0.093

92 0.276

94 0.053

96 0.049

98 0.04

100 0.049

102 0.036

104 0.015

106 0.263

108 0.053

110 0.025

112 0.008

114 0.097

116 0.065

118 0.058

120 0.075

122 0.113

124 0.021

126 0.015

128 0.026

130 0.172

132 0.018

134 0.097

136 0.02

138 0.03

140 0.018

142 0.084

144 0.162

146 0.117

HOLE NO.: GL-10-1

MEGA URANIUM LTD. - DH GeophysicsProject: GREENWICH LAKELogged By: Mike McNeillDate: March 3 - 8, 2010Mag Sus: KT-9, Core Diamater Set to: 4.00

Meter Mag Susc. CPS (>500) Comments

HOLE NO.: GL-10-1

148 0.042

150 0.212

152 0.026

154 0.251

156 0.156

158 0.074

160 0.032

162 0.103

164 0.162

166 0.016

168 0.157

170 0.035

172 0.069

174 0.048

176 0.169

178 0.114

180 0.044

182 0.172

184 0.011

186 0.008

188 0.034

EOH EOH EOH EOH

0.0

50.0

100.0

150.0

0 64Magnetic Susceptibility

DDH NO.: GL-10-1

LithologyFine Grained Mafic Intrusive

Foliated Mafic Intrusive

Gabbro

Migmatite

Overburden

Pink Pegmatite

Quartz Monzonite

Water

White Pegmatite

EASTING: 0364350

NORTHING: 5404769

ELEVATION: 426 m

AZIMUTH: Vertical Hole

DIP: -90

E.O.H: 189 m

MEGA URANIUM LTD.Drafted By: TLG, APRIL 2010

GREENWICH LAKE PROPERTY

Location:

Footage Degrees

Collar -5060 m n/a Notes:

100 m n/a150 m n/a Claim No.: NTS Map:

200 m n/a 4244232

From To0.0 1.9

1.9 37.5

37.5 73.2

73.2 95.6

95.6 128.8

128.80 188.50

188.50 199.60


51A/15

Location Map


Date Started:


MIGMATITEAlternating quartzofeldspathic and melanocratic layers, with short aletered mafic intrusive sections

MIGMATITEAlternating quartzofeldspathic and melanocratic layers

QUARTZ MONZONITE

PINK PEGMATITE to COARSE GRAINED GRANITE

OVER BURDEN

EOH

Cobra Drilling

February 27, 2010


February 28 - March 4, 2010Date Completed:

March 4, 2010

Tony Gilman

Meterage

Hole No.: GL-10-2 259.23 m 434 m

Collar Elevation:

Pink


Zone 16NNAD 83

Medium grained; green to dark grey; with minor dssm. Pyrite and calcopyrite.

QUARTZ MONZONITE

GABBRO


Size: NQ core

Azimuth:

250

199.60 222.80

222.80 231.30

231.30 259.23

259.23 EOH

GRANITIC GNIESS

PINK PEGMATITE to COARSE GRAINED GRANITE

MEDIUM GRAINED MAFIC INTRUSIVE


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Comments0 1.95 1.95 OB OVER BURDEN

1.95 26.1 24.2 QMZ Pink cg grad

QUARTZ MONZONITE to GRANITE; Pink to grey/blue, coarse grained to pegmatitic; highly fractured; non-foliated/massive; plagioclase, and quartz phenocrysts up to 2 cm. Breccia Zone from 18.3 to 18.7 m.

26.1 37.5 11.4 QMZ Pink mg hm (?)

QUARTZ MONZONITE to GRANITE; Pink to brick red, medium grained to pegmatitic; highly fractured; non-foliated/massive; quartz eyes (~1-3 mm). Numerous healed qtz. veins.

37.5 57.78 20.3 GAB Green/dark grey mg sharp 65 Py dssm .5 sr, chl 1

GABBRO; Green to dark grey; medium grained with a fine grained chilled margin at the contact with the overlying monzonite; highly fractured and faulted @ ~38 m to 41 m; non-foliated; Plagioclase, Pyroxene, and Olivine (?) make up the dominant mineralogy. Sercite and Chlorite alteration is weak but pervasive throughout; minor (less than 0.5%) pyrite.

57.78 58.31 0.53 QMZ Pink mg/fg grad

QUARTZ MONZONITE to GRANITE; Pink to grey/green; medium to fine grained; non-foliated/massive; possible xenolith within mafic intrusive.

58.31 73.2 14.9 GAB Green/dark grey mg grad Py,

Cpy dssm .5

GABBRO; Green to dark grey; medium grained; non-foliated; Plagioclase, Pyroxene, and Olivine (?) make up the dominant mineralogy. Sercite and Chlorite alteration is weak but pervasive throughout; minor dssm. (less than 0.5%) pyrite; moderately magnetic.

73.2 79.18 5.98 PPEG Pink cg sharp 85PINK PEGMATITE to GRANITE; Pink to pinkish grey; coarse grained; non-foliated/massive; minor sercite alteration; lower contact 84 deg TCA.

79.18 80.71 1.53 DBf Grey to black fg sharp 70

FINE GRAINED MAFIC INTRUSIVE; Black to grey; fine grained; 10 cm section of Pink Pegmatite at 80 m; minor sercite alteration. No sulphides.

80.71 95.65 14.9 PPEG Pink cg grad 45PINK PEGMATITE to GRANITE; Pink to pinkish grey; coarse grained; non-foliated/massive; minor sercite alteration; lower contact 45 deg TCA.

95.65 113.88 18.2 MIGWhite and

Blackfg/cg grad 45 sr 1

MIGMATITE; Alternating black and white to pink; fine (melanocratic layers) to coarse (leucocratic layers) grained; well foliated; foliation at 45 deg TCA; minor pervasive, weak, sercite alteration; dominant mafic mineral is biotite; lower contact 45 deg TCA.

113.88 114.4 0.52 DBf Black fg sharp 35 Py dssm .5FINE GRAINED MAFIC INTRUSIVE; Black; fine grained; lower contact 45 deg TCA; non-foliated.

114.4 128.85 14.5 MIGWhite and

Blackfg/cg sharp 45 sr 1

MIGMATITE; Alternating black and white to pink; fine (melanocratic layers) to coarse (leucocratic layers) grained; well foliated; foliation at 45 deg TCA; minor pervasive, weak, sercite alteration; dominant mafic mineral is biotite; lower contact 35 deg TCA.

128.85 136.27 7.42 QMZ Pink mg/cg grad 35 Py .5 sr 1

QUARTZ MONZONITE to GRANITE; Pink to grey, medium to coarse grained ; moderately foliated to massive; foliation 45 deg TCA; plagioclase, and quartz phenocrysts up to 1 cm.

136.72 136.9 0.18 DBf Black fg sharp 50 Py .5FINE GRAINED MAFIC INTRUSIVE; Black; fine grained; lower contact 50 deg TCA; non-foliated; minor dssm. Pyrite.

HOLE NO.: GL-10-2

Page 1 of 2


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HOLE NO.: GL-10-2

136.9 170.6 33.7 QMZ Pink mg/cg sharp 50 sr 1

QUARTZ MONZONITE to GRANITE; Pink to grey, medium to coarse grained to pegmatitic; moderately to well foliated; foliation 45 deg TCA; plagioclase, and quartz phenocrysts up to 1 cm; Contains well foliated fine grained biotite rich zones (i.e 146.7 m).

170.6 171.4 0.8 DBm Black mg sharp 45 Py .5

MEDIUM GRAINED MAFIC INTRUSIVE; Black to steely gray; medium grained; biotite rich; likely melancocratic section of migmatite; moderately to well foliated.

171.4 188.5 17.1 MIGWhite and

Blackmg/fg grad Py

MIGMATITE; Alternating black and white to pink; fine (melanocratic layers) to coarse (leucocratic layers) grained; moderately to well foliated; foliation at 45 deg TCA; dominant mafic mineral is biotite; lower contact 35 deg TCA.

188.5 190.2 1.7 PPEG Pink cg sharp 35PINK PEGMATITE to GRANITE; Pink to pinkish grey; coarse grained; weakly foliated; minor sercite alteration; lower contact 50 deg TCA.

190.2 199.6 9.4 DBm Black mg sharp 50

MEDIUM GRAINED MAFIC INTRUSIVE; Black to steely gray; medium grained; biotite rich; likely melancocratic section of migmatite; moderately to well foliated; commonly cut by 10 - 50 cm white and pink pegmatite section (i.e @ 193.15 and 194, and 194.4 m); weak to non-magnetic.

199.6 222.8 23.2 QMZ Black mg/fg sr 1

GRANITIC GNIESS to QUARTZ MONZONITE; Alternating black and white to pink; fine (melanocratic layers) to coarse (leucocratic layers) grained alonmg with well foliated pink granite to quartz monzonite; moderately to well foliated; foliation at 45 deg TCA; dominant mafic mineral is biotite; lower contact 35 deg TCA.

222.8 231.3 8.5 DBm Black mg sharp 55

MEDIUM GRAINED MAFIC INTRUSIVE; Black to green/gray; medium grained; biotite rich; likely melancocratic section of migmatite; moderately to well foliated; weak to non-magnetic; commonly cut by 5 - 80 cm, pink to white pegmatite veins, lower contact parallel to foliation at 45 deg TCA.

231.3 242 10.7 PPEG Pink cg sharp 45

PINK PEGMATITE to GRANITE; Pink to pinkish grey; coarse grained; weakly foliated; minor sercite alteration; pegmatite commonly cut by black to green biotite rich, mod. to well foliated mafic sections (i.e @ 236.5 m).

242 254.6 12.6 DBm Black mg irr

MEDIUM GRAINED MAFIC INTRUSIVE; Black to green/gray; medium grained; biotite rich; magnatite visible at ~246 m; likely melancocratic section of migmatite; moderately to well foliated; moderate to stronly magnetic; commonly cut by 5 - 80 cm, pink to white pegmatite veins (i.e @ 245.2 m) often ~ paralle TCA; lower contact irregular.

254.6 259.23 4.63 PPEG

PINK PEGMATITE to GRANITE; Pink to pinkish grey; coarse grained; weakly foliated to non-foliated; minor sercite alteration; pegmatite commonly cut by black to green biotite rich, mod. to well foliated mafic sections (i.e @ EOH).

EOH End of Hole @ 259.23 m

Page 2 of 2

MEGA URANIUM LTD. - SAMPLE RECORDProject: GREENWICH LAKELogged By: T. GilmanDate: February 27 - March 4, 2010



1 2 2286001 37.50 38.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286002 38.50 39.50 1.00 GAB 1C Exploration 1F-2 A10-1039286003 39.50 40.50 1.00 GAB 1C Exploration 1F-2 A10-1039286004 40.50 41.50 1.00 GAB 1C Exploration 1F-2 A10-1039286005 41.50 42.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286006 42.50 43.50 1.00 GAB 1C Exploration 1F-2 A10-1039286007 43.50 44.50 1.00 GAB 1C Exploration 1F-2 A10-1039286008 44.50 45.50 1.00 GAB 1C Exploration 1F-2 A10-1039286009 45.50 46.50 1.00 GAB 1C Exploration 1F-2 A10-1039286010 46.50 47.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286011 47.50 48.50 1.00 GAB 1C Exploration 1F-2 A10-1039286012 48.50 49.50 1.00 GAB 1C Exploration 1F-2 A10-1039286013 49.50 50.50 1.00 GAB 1C Exploration 1F-2 A10-1039286014 50.50 51.50 1.00 GAB 1C Exploration 1F-2 A10-1039286015 STANDARD 1C Exploration 1F-2 A10-1039 STANDARD286016 51.50 52.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286017 52.50 53.50 1.00 GAB 1C Exploration 1F-2 A10-1039286018 53.50 54.50 1.00 GAB 1C Exploration 1F-2 A10-1039286019 54.50 55.50 1.00 GAB 1C Exploration 1F-2 A10-1039286020 55.50 56.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286021 56.50 57.50 1.00 GAB 1C Exploration 1F-2 A10-1039286022 57.50 58.50 1.00 GAB/QMZ 1C Exploration 1F-2 A10-1039286023 58.50 59.50 1.00 QMZ 1C Exploration 1F-2 A10-1039286024 59.50 60.50 1.00 GAB 1C Exploration 1F-2 A10-1039286025 60.50 61.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286026 61.50 62.50 1.00 GAB 1C Exploration 1F-2 A10-1039286027 62.50 63.50 1.00 GAB 1C Exploration 1F-2 A10-1039286028 63.50 64.50 1.00 GAB 1C Exploration 1F-2 A10-1039286029 64.50 65.50 1.00 GAB 1C Exploration 1F-2 A10-1039286030 64.50 65.50 1.00 DUPLICATE 1C Exploration 1F-2 A10-1039 DUPLICATE286031 65.50 66.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286032 66.50 67.50 1.00 GAB 1C Exploration 1F-2 A10-1039286033 67.50 68.50 1.00 GAB 1C Exploration 1F-2 A10-1039286034 68.50 69.50 1.00 GAB 1C Exploration 1F-2 A10-1039286035 69.50 70.50 1.00 GAB 1C Exploration 1F-2 4C A10-1039286036 70.50 71.50 1.00 GAB 1C Exploration 1F-2 A10-1039286037 71.50 72.50 1.00 GAB 1C Exploration 1F-2 A10-1039286038 72.50 73.20 0.70 GAB 1C Exploration 1F-2 A10-1039286039 79.20 80.70 1.50 GAB 1C Exploration 1F-2 A10-1039286040 113.88 114.40 0.52 DBf 1C Exploration 1F-2 4C A10-1039286041 136.72 136.9 0.18 DBf 1C Exploration 1F-2 A10-1039286042 197.00 198.00 1.00 DBm 1C Exploration 1F-2 A10-1039286043 228.00 229.00 1.00 DBm 1C Exploration 1F-2 A10-1039286044 229.00 230.00 1.00 DBm 1C Exploration 1F-2 A10-1039286045 A10-1039 STANDARD286046 230.00 231.00 1.00 DBm 1C Exploration 1F-2 A10-1039

HOLE NO.: GL-10-2

MEGA URANIUM LTD. - GEOTECH LOGProject: GREENWICH LAKELogged By: Mike McNeillDate: February 27 - March 04, 2010

From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)1.95 5 3.05 100.0% 0.0%5 8 3 100.0% 2.48 82.7%8 11 3 100.0% 1.87 62.3%11 14 3 100.0% 1.28 42.7%14 17 3 100.0% 2.45 81.7%17 20 3 100.0% 1.41 47.0%20 23 3 100.0% 1.89 63.0%23 26 3 100.0% 2.07 69.0%26 29 3 100.0% 2.09 69.7%29 32 3 100.0% 1 33.3%32 35 3 100.0% 1.32 44.0%35 38 3 100.0% 1.67 55.7%38 41 3 100.0% 0.4 13.3%41 44 3 100.0% 1.25 41.7%44 47 3 100.0% 1.57 52.3%47 50 3 100.0% 1.24 41.3%50 53 3 100.0% 1.25 41.7%53 56 3 100.0% 1.68 56.0%56 59 3 100.0% 2.14 71.3%59 62 3 100.0% 1.83 61.0%62 65 3 100.0% 1.09 36.3%65 68 3 100.0% 1.83 61.0%68 71 3 100.0% 1.64 54.7%71 74 3 100.0% 1.89 63.0%74 77 3 100.0% 2.93 97.7%77 80 3 100.0% 2.89 96.3%80 83 2.9 96.7% 2.38 79.3%83 86 3 100.0% 2.69 89.7%86 89 3 100.0% 2.64 88.0%89 92 3 100.0% 2.8 93.3%92 95 2.92 97.3% 2.55 85.0%95 98 3 100.0% 2.9 96.7%98 101 2.97 99.0% 3 100.0%101 104 3 100.0% 2.78 92.7%104 107 2.92 97.3% 2.92 97.3%107 110 3 100.0% 2.48 82.7%110 113 3 100.0% 2.66 88.7%113 116 3 100.0% 2.56 85.3%116 119 3 100.0% 2.66 88.7%119 122 3 100.0% 2.65 88.3%

HOLE NO.: GL-10-2




HOLE NO.: GL-10-2


122 125 3 100.0% 2.57 85.7%125 128 3 100.0% 2.6 86.7%128 131 3 100.0% 2.8 93.3%131 134 3 100.0% 2.25 75.0%134 137 3 100.0% 2.78 92.7%137 140 3 100.0% 2.63 87.7%140 143 3 100.0% 2.36 78.7%143 146 3 100.0% 2.9 96.7%146 149 2.95 98.3% 2.89 96.3%149 152 3 100.0% 2.99 99.7%152 155 2.96 98.7% 2.64 88.0%155 158 3 100.0% 2.92 97.3%158 161 3 100.0% 2.97 99.0%161 164 3 100.0% 2.68 89.3%164 167 3 100.0% 2.83 94.3%167 170 3 100.0% 3 100.0%170 173 3 100.0% 2.44 81.3%173 176 2.96 98.7% 2.23 74.3%176 179 2.87 95.7% 2.51 83.7%179 182 2.89 96.3% 2.68 89.3%182 185 3 100.0% 2.57 85.7%185 188 3 100.0% 2.78 92.7%188 191 3 100.0% 2.63 87.7%191 194 3 100.0% 2.6 86.7%194 197 3 100.0% 2.54 84.7%197 200 3 100.0% 2.91 97.0%200 203 3 100.0% 3 100.0%203 206 3 100.0% 2.79 93.0%206 209 2.92 97.3% 2.86 95.3%209 212 3 100.0% 2.92 97.3%212 215 3 100.0% 2.92 97.3%215 218 2.96 98.7% 2.89 96.3%218 221 2.96 98.7% 2.74 91.3%221 224 3 100.0% 2.86 95.3%224 227 3 100.0% 2.83 94.3%227 230 2.98 99.3% 2.69 89.7%230 233 3 100.0% 3 100.0%233 236 3 100.0% 2.69 89.7%236 239 3 100.0% 2.94 98.0%239 242 3 100.0% 2.92 97.3%



HOLE NO.: GL-10-2


242 245 3 100.0% 2.53 84.3%245 248 3 100.0% 2.84 94.7%248 251 2.96 98.7% 2.6 86.7%251 254 3 100.0% 2.51 83.7%254 257 3 100.0% 2.87 95.7%257 259.23 2.2 73.3% 1.92 64.0%EOH EOH EOH EOH EOH EOH

MEGA URANIUM LTD. - DH GeophysicsProject: GREENWICH LAKELogged By: Mike McNeillDate: February 27 - March 04, 2010Mag Sus: KT-9, Core Diamater Set to: 4.00

Meter Mag Susc. CPS (>500) Comments1

2 0.05

3 0.032

4 0.034

5 0.076

6 0.06

7 0.03

8 0.032

9 0.043

10 0.054

11 0.048

12 0.031

13 0.053

14 0.036

15 0.158

16 0.03

17 0.029

18 0.028

19 0.168

20 0.155

21 0.025

22 0.217

23 0.262

24 0.174

25 0.016

26 0.053

27 0.073

28 0.033

29 0.051

30 0.028

31 0.029

32 0.163

33 0.058

34 0.055

35 0.196

36 0.193

37 0.309 Contact between Granite and Mafic Intrusive38 9.231

39 0.528

40 0.443

41 2.403

HOLE NO.: GL-10-2



HOLE NO.: GL-10-2

42 0.969

43 0.652

44 1.531

45 0.362

46 4.84

47 0.487

48 0.334

49 0.324

50 1.214

51 3.601

52 3.95

53 7.125

54 0.912

55 9.878

56 4.224

57 0.257

58 0.189

59 0.033 Granite mafic contact60 1.327 Mafic61 2.514

62 2.067

63 0.777

64 5.858

65 6.562

66 4.756

67 6.693

68 10.2

69 0.356

70 0.457

71 6.655

72 2.315

73 0.036 Mafic74 0.201 Granite75 0.209

76 0.494

77 0.204

78 0.289

79 0.207

80 0.507

81 0.271

82 0.182



HOLE NO.: GL-10-2

83 0.025

84 0.328

85 0.269

86 0.22

87 0.254

88 0.045

89 0.154

90 0.017

91 0.041

92 0.046

93 0.216

94 0.038

95 0.202

96 0.035

97 0.16

98 0.04

99 0.293

100 0.01

101 0.036

102 0.017

103 0.236

104 0.215

105 0.028

106 0.178

107 0.093

108 0.166

109 0.012

110 0.019

111 0.063

112 0.213

113 0.076

114 0.044

115 0.012

116 0.022

117 0.194

118 0.172

119 0.205

120 0.052

121 0.21

122 0.025

123 0.036



HOLE NO.: GL-10-2

124 0.101

125 0.067

126 0.007

127 0.018

128 0.031

129 0.038

130 0.015

131 0.011

132 0.004

133 0.012

134 0.02

135 0.01

136 0.35

137 0.339

138 0.169

139 0.039

140 0.058

141 0.039

142 0.241

143 0.034

144 0.172

145 0.023

146 0.018

147 0.047

148 0.059

149 0.023

150 0.099

151 0.044

152 0.064

153 0.079

154 0.04

155 0.204

156 0.167

157 0.092

158 0.034

159 0.024

160 0.017

161 0.069

162 0.231

163 0.077

164 0.334



HOLE NO.: GL-10-2

165 0.304

166 0.078

167 0.166

168 0.047

169 0.032

170 0.008

171 0.008

172 0.038

173 0.013

174 0.061

175 0.027

176 0.024

177 0.012

178 0.149

179 0.03

180 0.035

181 0.041

182 0.035

183 0.022

184 -0.01

185 0.043

186 0.008

187 0.013

188 0.001

189 0.254

190 0.185

191 0.064

192 0.04

193 0.07

194 0.24

195 0.203

196 0.05

197 0.071

198 0.102

199 0.01

200 0.181

201 0.019

202 0.24

203 0.035

204 0.195

205 0.08



HOLE NO.: GL-10-2

206 0.018

207 0.019

208 0.01

209 0.01

210 0.135

211 0.068

212 0.036

213 0.006

214 0.008

215 0.032

216 0.029

217 0.041

218 0.021

219 0.026

220 0.03

221 0.024

222 0.018

223 0.08

224 0.079

225 0.073

226 0.071

227 6.111

228 40.88 Migmatite (magnetite associated)229 26.72 Migmatite (magnetite associated)230 57.15 Migmatite (magnetite associated)231 0.349

232 0.342

233 0.019

234 0.052

235 0.289

236 0.239

237 0.017

238 0.027

239 0.022

240 0.051

241 0.052

242 0.31

243 0.55

244 0.44

245 0.26

246 0.642



HOLE NO.: GL-10-2

247 0.351

248 0.33

249 0.128

250 0.859

251 0.012

252 0.095

253 0.172

254 0.032

255 0.016

256 0.017

257 0.008

258 0.036

259 0.173

EOH EOH

EASTING: 0364064

NORTHING: 5409513

ELEVATION: 434 m

AZIMUTH: 250

DIP: -50

E.O.H: 259.23 m



0.0

50.0

100.0

150.0

200.0

250.0

0 to 64

Magnetic Susceptibility

LithologyFine Grained Mafic IntrusiveFoliated Mafic IntrusiveGabbroMigmatiteOverburdenPink PegmatiteQuartz MonzoniteWaterWhite Pegmatite

GL-10-2

070250

Location:

Footage Degrees



200 m n/a 4244232

From To0.0 2.7

2.7 49.1

49.1 59.1

59.1 106.5

106.5 113.9

113.9 134.8

134.80 180.30

180 30 219 00


51A/15

Location Map


Date Started:


Mi tit

Fresh; non-foliated; strongly magnetic; not cut by pegmatites.

Medium Grained Mafic Intrusive

Gabbro

Migmatite

Migmatite

Overburden

EOH

Cobra Drilling

March 4, 2010


March 4 - March 7, 2010Date Completed:

March 7, 2010

Tony Gilman

Meterage

Hole No.: GL-10-3 219 m 446 m

Collar Elevation:


Zone 16NNAD 83

Dominantly Migmatite and White Pegmatite

Fine Grained Mafic Intrusive


Size: NQ core

Azimuth:

260

180.30 219.00

219.00 EOH

Migmatite

MEGA URANIUM LTD. - GEOLOGICAL LOGProject: GREENWICH LAKE Easting: 0364205Logged By: T. Gilman Northing: 5409325Date: March 4 - March 7, 2010 Datum & Projection: NAD 83, UTM Zone 16 N

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2.65 3.7 1.05 MIG Black fg/mg sharp 35

MIGMATITE; Black to steely gray; fine to medium grained; moderately to well foliated melanocratic section of migmatite; dominant mineralogy is biotite and hornblende.

3.7 4.75 1.05 WPEG White cgWHITE PEGMATITE; White to grey, coarse grained; non-foliated.


whitefg/mg sharp 35

MIGMATITE; Black to steely gray; fne to medium grained; moderately to well foliated; foliation at 30 deg TCA; melanocratic section (from 4.75 m to 24 m); changing to alternating melanocratic and leucocratic zones after 24 m; cut by numerouswhite, coasre grained pegmatite veins (i.e 12.2 m and 15.9 m); moderately magnetic with some visible magnetite; dominant mineralogy of melanocratic sections is biotite and hornblende.

36 39.05 3.05 WPEG White cgWHITE PEGMATITE; White to grey, coarse grained; non-foliated.

39.05 49.1 10.1 MIGBlack and

Whitefg/mg sharp 45

MIGMATITE; Black to steely gray with alternating white leucocratic layers; medium to fine grained; moderately to well foliated; foliation at 30 deg TCA; moderately magnetic with some visible magnetite; dominant mineralogy of melanocratic sections is biotite and hornblende.

49.1 59.1 10 DBf Green/Grey fg/mg shapr 55 chl 2

FINE GRAINED MAFIC INTRUSIVE; Green to dark grey; fine grained; non-foliated; moderate, pervasive, chlorite alteration throughout. Major fault zone from 56.2 m to 59.2 m)

59.1 74.75 15.7 MIGBlack and

Whitefg/mg

MIGMATITE; Black to steely gray with alternating white leucocratic layers; medium to fine grained; moderately to well foliated; foliation at 30 deg TCA; weak to non-magnetic; dominant mineralogy of melanocratic sections is biotite and hornblende; commonly cut by coarse grained, white pegmatite dykes.

74.75 75.9 1.15 DBf Black fg/mg sharp 90 py dssm .5FINE GRAINED MAFIC INTRUSIVE; Black to dark grey; fine grained; non-foliated.

75.9 98.75 22.9 MIGBlack and

Whitefg/mg

MIGMATITE; Black to steely gray with alternating white leucocratic layers; medium to fine grained with coarse grained pegmatite sections; moderately to well foliated; foliation at 30 deg TCA; weak to non-magnetic; dominant mineralogy of melanocratic sections is biotite and hornblende; commonly cut by coarse grained, white pegmatite dykes.

98.75 101.3 2.55 DBm Black fg/mg sharp 55 py dssm 1

MEDIUM GRAINED MAFIC INTRUSIVE; Black; fine to medium grained; non-foliated; contains up to 1% dssm pyrite throughout; dominant mineralogy is hornblende and biotite.

101.3 102.55 1.25 WPEG White cg sharp 40WHITE PEGMATITE; White to grey, coarse grained; non-foliated.


MEDIUM GRAINED MAFIC INTRUSIVE; Black; fine to medium grained; non-foliated; contains up to 1% dssm pyrite throughout; dominant mineralogy is hornblende and biotite.

103.8 106.45 2.65 WPEG White cg sharp 40WHITE PEGMATITE; White to grey, coarse grained; non-foliated.

HOLE NO.: GL-10-3

Page 1 of 2


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Comments

HOLE NO.: GL-10-3


MEDIUM GRAINED MAFIC INTRUSIVE; Black; fine to medium grained; weakly foliated; contains up to 1% dssm pyrite throughout; dominant mineralogy is hornblende and biotite; cut by pegmatite veins (i.e @ 108 to 108.4 m)

113.9 126.75 12.9 MIGBlack and

Whitefg/mg

MIGMATITE; Black to steely gray with alternating white leucocratic layers; melanocraitc section contain up to 1-2 % dssm and vein pyrite; medium to fine grained with coarse grained pegmatite sections; moderately to well foliated; foliation at 30 deg TCA; weak to non-magnetic; dominant mineralogy of melanocratic sections is biotite and hornblende; commonly cut by coarse grained, white pegmatite dykes.

126.8 134.8 8 DBm Black fg/mg sharp 55 py dssm 1

MEDIUM GRAINED MAFIC INTRUSIVE; Black; fine to medium grained; non-foliated; contains up to 1% dssm pyrite throughout; dominant mineralogy is plagioclase and pyroxene (fresh); changes gradiationally into under lying gabbro.

134.8 180.25 45.5 GAB Grey to Green mg grad py dssm 1

GABBRO; Green to grey; medium grained; non-foliated; chlorite+/- sericite+/-epidote alteration pervasive througout; contains up to 1 % dssm pytire and minor calcopyrite; dominant mineralogy is plagioclase and pyroxene;moderately to strongly magnetic; lower contact shows chilled margin.


whitemg/cg sharp 45

MIGMATITE; Black and white alternating; medium grained (melanosomes) to coasre grained (leucosomes); moderatley to well foliated; foliation @ 35 deg TCA; dominant mafic minerals in melanosomes are hornblende and biotite.

EOH 219

Page 2 of 2

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MEGA URANIUM LTD. - SAMPLE RECORDProject: GREENWICH LAKELogged By: T. GilmanDate: March 4 - March 7, 2010



1 2 2286065 49.10 50.10 1.00 DBf 1 C Exploration 1 F-2 4 C COMP A10-1089286066 50.10 51.10 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286067 51.10 52.10 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286068 56.25 57.25 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286069 57.25 58.25 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286070 58.25 59.10 0.85 DBf 1 C Exploration 1 F-2 4 C COMP A10-1089286071 74.75 75.90 1.15 DBf 1 C Exploration 1 F-2 COMP A10-1089286072 98.75 99.75 1.00 DBm 1 C Exploration 1 F-2 COMP A10-1089286073 99.75 100.75 1.00 DBm 1 C Exploration 1 F-2 COMP A10-1089286074 100.75 101.30 0.55 DBm 1 C Exploration 1 F-2 COMP A10-1089286075 1 C Exploration A10-1089 Standard286076 102.60 103.75 1.15 DBm 1 C Exploration 1 F-2 COMP A10-1089286077 106.50 107.50 1.00 1 C Exploration 1 F-2 A10-1089286078 107.50 108.50 1.00 DBm 1 C Exploration 1 F-2 COMP A10-1089286079 108.50 109.50 1.00 DBm 1 C Exploration 1 F-2 COMP A10-1089286080 109.50 110.50 1.00 DBm 1 C Exploration 1 F-2 4 C COMP A10-1089286081 110.50 111.50 1.00 DBm 1 C Exploration 1 F-2 COMP A10-1089286082 111.50 112.50 1.00 DBm 1 C Exploration 1 F-2 COMP A10-1089286083 112.50 113.50 1.00 DBm 1 C Exploration 1 F-2 COMP A10-1089286084 113.50 114.00 0.50 DBm 1 C Exploration 1 F-2 COMP A10-1089286085 117.00 118.00 1.00 MIG 1 C Exploration 1 F-2 4 C COMP A10-1089286086 118.00 119.00 1.00 MIG 1 C Exploration 1 F-2 COMP A10-1089286087 125.70 126.10 0.40 MIG 1 C Exploration 1 F-2 COMP A10-1089286088 126.75 127.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286089 127.75 128.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286090 127.75 128.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089 Duplicate286091 128.75 129.75 1.00 DBf 1 C Exploration 1 F-2 A10-1089286092 129.75 130.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286093 130.75 131.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286094 131.75 132.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286095 132.75 133.75 1.00 DBf 1 C Exploration 1 F-2 4 C COMP A10-1089286096 133.75 134.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286097 134.75 135.75 1.00 DBf 1 C Exploration 1 F-2 COMP A10-1089286098 135.75 136.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286099 136.75 137.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286100 137.75 138.75 1.00 GAB 1 C Exploration 1 F-2 4 C COMP A10-1089286101 138.75 139.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286102 139.75 140.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286103 140.75 141.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286104 141.75 142.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286105 UMT-1 1 C Exploration A10-1089 Standard286106 142.75 143.75 1.00 GAB 1 C Exploration 1 F-2 A10-1089286107 143.75 144.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286108 144.75 145.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286109 145.75 146.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286110 146.75 147.75 1.00 GAB 1 C Exploration 1 F-2 4 C COMP A10-1089286111 147.75 148.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286112 148.75 149.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286113 149.75 150.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286114 150.75 151.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286115 151.75 152.75 1.00 GAB 1 C Exploration 1 F-2 4 C COMP A10-1089

HOLE NO.: GL-10-3

of 2




1 2 2

HOLE NO.: GL-10-3

286116 152.75 153.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286117 153.75 154.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286118 154.75 155.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286119 155.75 156.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286120 155.75 156.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089 Duplicate286121 156.75 157.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286122 157.75 158.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286123 158.75 159.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286124 159.75 160.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286125 160.75 161.75 1.00 GAB 1 C Exploration 1 F-2 4 C COMP A10-1089286126 161.75 162.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286127 162.75 163.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286128 163.75 164.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286129 164.75 165.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286130 165.75 166.75 1.00 GAB 1 C Exploration 1 F-2 4 C COMP A10-1089286131 166.75 167.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286132 167.75 168.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286133 168.75 169.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286134 169.75 170.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286135 UMT-1 1 C Exploration A10-1089 Standard286136 170.75 171.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286137 171.75 172.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286138 172.75 173.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286139 173.75 174.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286140 174.75 175.75 1.00 GAB 1 C Exploration 1 F-2 4 C COMP A10-1089286141 175.75 176.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286142 176.75 177.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286143 177.75 178.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286144 178.75 179.75 1.00 GAB 1 C Exploration 1 F-2 COMP A10-1089286145 179.75 180.75 1.00 GAB 1 C Exploration 1 F-2 4 C COMP A10-1089286146 180.75 182.00 1.25 GAB 1 C Exploration 1 F-2 COMP A10-1089

MEGA URANIUM LTD. - GEOTECH LOGProject: GREENWICH LAKELogged By: Mike McNeillDate: March 05 - March 07, 2010

From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)5 8 3 98.4% 2.95 96.7%8 11 2.95 98.3% 2.75 91.7%11 14 3 100.0% 2.69 89.7%14 17 3 100.0% 2.7 90.0%17 20 2.98 99.3% 2.92 97.3%20 23 2.9 96.7% 2.31 77.0%23 26 2.98 99.3% 2.66 88.7%26 29 3 100.0% 2.98 99.3%29 32 2.91 97.0% 2.42 80.7%32 35 2.95 98.3% 2.6 86.7%35 38 3 100.0% 2.29 76.3%38 41 2.92 97.3% 2.66 88.7%41 44 2.97 99.0% 2.25 75.0%44 47 2.92 97.3% 2.35 78.3%47 50 2.79 93.0% 1.76 58.7%50 53 3 100.0% 1.47 49.0%53 56 2.53 84.3% 0.24 8.0%56 59 2.7 90.0% 2.08 69.3%59 62 2.56 85.3% 0.92 30.7%62 65 2.96 98.7% 2.7 90.0%65 68 3 100.0% 2.62 87.3%68 71 3 100.0% 2.44 81.3%71 74 3 100.0% 2.53 84.3%74 77 3 100.0% 2.95 98.3%77 80 3 100.0% 2.92 97.3%80 83 2.9 96.7% 2.49 83.0%83 86 3 100.0% 2.69 89.7%86 89 3 100.0% 2.85 95.0%89 92 3 100.0% 1.94 64.7%92 95 2.95 98.3% 2.07 69.0%95 98 3 100.0% 2.9 96.7%98 101 3 100.0% 2.55 85.0%101 104 3 100.0% 2.75 91.7%104 107 3 100.0% 1.5 50.0%107 110 3 100.0% 2.28 76.0%110 113 3 100.0% 2.5 83.3%113 116 3 100.0% 2.39 79.7%116 119 3 100.0% 2.29 76.3%119 122 3 100.0% 2.64 88.0%122 125 3 100.0% 2.45 81.7%

HOLE NO.: GL-10-3




HOLE NO.: GL-10-3


125 128 2.92 97.3% 2.82 94.0%128 131 3 100.0% 1.84 61.3%131 134 2.86 95.3% 1.53 51.0%134 137 3 100.0% 2.54 84.7%137 140 3 100.0% 2.62 87.3%140 143 3 100.0% 2.35 78.3%143 146 3 100.0% 2.78 92.7%146 149 2.9 96.7% 0.0%149 152 3 100.0% 2.4 80.0%152 155 3 100.0% 1.94 64.7%155 158 3 100.0% 2.62 87.3%158 161 2.94 98.0% 2.86 95.3%161 164 3 100.0% 2.7 90.0%164 167 3 100.0% 2.9 96.7%167 170 3 100.0% 2.87 95.7%170 173 3 100.0% 2.97 99.0%173 176 2.94 98.0% 2.63 87.7%176 179 3 100.0% 1.41 47.0%179 182 3 100.0% 2.43 81.0%182 185 3 100.0% 2.73 91.0%185 188 2.89 96.3% 2.71 90.3%188 191 2.96 98.7% 2.06 68.7%191 194 3 100.0% 1.58 52.7%194 197 3 100.0% 1.9 63.3%197 200 3 100.0% 2.52 84.0%200 203 3 100.0% 2.42 80.7%203 206 3 100.0% 2.28 76.0%206 209 3 100.0% 2.42 80.7%209 212 2.9 96.7% 2.7 90.0%212 215 2.92 97.3% 2.55 85.0%215 218 3 100.0% 2.67 89.0%218 219 1 100.0% 0.64 64.0%EOH EOH EOH EOH EOH EOH

MEGA URANIUM LTD. - DH GeophysicsProject: GREENWICH LAKELogged By: Mike McNeillDate: March 05 - March 7, 2010Mag Sus: KT-9, Core Diamater Set to: 4.00


4 0.094

6 0.105

8 0.264

10 4.978

12 0.034

14 0.2

16 0.197

18 0.21

20 0.137

22 0.217

24 0.024

26 0.036

28 0.309

30 0.125

32 0.072

34 0.285

36 0.079

38 0.157

40 0.085

42 0.165

44 0.053

46 0.246

48 0.123

50 0.284

52 0.497

54 0.063

56 0.265

58 0.359

60 0.056

62 0.048

64 0.243

66 0.246

68 0.052

70 0.084

72 0.198

74 0.093

76 0.209

78 0.118

80 0.216

82 0.077

HOLE NO.: GL-10-3

84 0.109

86 0.262

88 0.067

90 0.189

92 0.107

94 0.024

96 0.142

98 0.205

100 0.226

102 0.036

104 0.034

106 0.091

108 0.209

110 0.224

112 0.276

114 0.053

116 0.2

118 0.194

120 0.07

122 0.098

124 0.325

126 0.045

128 0.222

130 0.22

132 0.308

134 7.257 Change from fine grained mafic intrusive to Gabbro (Start High)136 6.722

138 5.786

140 9.658

142 4.976

144 7.903

146 0.557

148 0.85

150 9.503

152 6.424

154 0.691

156 9.966

158 10.65

160 3.542

162 5.974

164 2.621

166 0.408

168 0.682

170 3.189 End High Magnetism172 0.344

174 0.78

176 0.461

178 0.303

180 0.517

182 0.285

184 0.267

186 0.271

188 0.262

190 0.392

192 0.243

194 0.373

196 0.229

198 0.196

200 0.202

202 0.187

204 0.092

206 0.194

208 0.184

210 0.188

212 0.091

214 0.19

216 0.206

218 0.223

EOH EOH

EASTING: 0364205

NORTHING: 5409325

ELEVATION: 446 m

AZIMUTH: 260

DIP: -50

E.O.H: 219 m



GL-10-3

080260

0.0

50.0

100.0

150.0

200.0

0 to 64




Gabbro

Migmatite

Overburden

Pink Pegmatite

Quartz Monzonite

Water

White Pegmatite

Location:

Footage Degrees



200 m n/a 4244234

From To0.0 1.5

1.5 5.2

5.2 111.5

111.5 120.9

120.9 136.6

136.6 146.0

146.00 188.00

188.00 203.00


Zone 16N

NAD 83

FINE GRAINED MAFIC INTRUSIVE

MIGMATITE and PEGMATITE


Size: BTW core

Azimuth:

067

EOH

Rugged Aviation/Drilling

March 10, 2010


March 11 - March 18, 2010Date Completed:

3/16/2010

Tony Gilman, Stefan Kruse

Meterage

Hole No.: GL-10-4 251 m 439 m

Collar Elevation:

Brecciated PINK PEGMATITE



WHITE PEGMATITE

QUARTZ MONZONITE

OVERBURDEN


51A/15

Location Map


Date Started:


203.00 204.85

204.85 251.00 Brecciated PINK PEGMATITE, MIGMATITE and QUARTZ MONZONITE

Brec

FINE GRAINED MAFIC INTRUSIVE

MEGA URANIUM LTD. - GEOLOGICAL LOGProject: GREENWICH LAKE Easting: 0362924Logged By: T. Gilman, S. Kruse Northing: 5408767Date: March 10 - March 16, 2010 Datum & Projection: NAD 83, UTM Zone 16 N

From To

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Alte

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n

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ity

Comments0 1.5 1.5 OB OVERBURDEN

1.5 5.15 3.65 DBf Black fg sharp 75 py, cpy dssm 1

FINE GRAINED MAFIC INTRUSIVE; Black to blue gray; fine grained; non-foliated; moderately to highly magnetic; moderate, pervasive chl alteration throughout; v. fine grained cpy and py dssm. Throughout (.1 - .5%); dominant mineralogy is plagioclase with minor pyroxene, and pyrite.

5.15 111.5 106 MIGBlack and

whitefg/cg

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine- to medium-grained melanosomes with coarse grained white to pink; non-foliated pegmatite; non-magnetic.

111.5 120.9 9.4 QMZ Pink mg grad 80 hem,ser 1QUARTZ MONZONITE to GRANITE; Pink; medium grained; non-foliated; non-magnetic; weak, pervasive, sercite alteration of feldspars throughout.

120.9 136.6 15.7 MIGBlack and

whitefg/cg sharp 5 cpy,

py vein .25

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse grained white to pink; non-foliated pegmatite; non-magnetic. Trace cpy in calcite veins ~ 85 deg TCA. Trace py in qyartz segregations oriented 5-10 deg TCA.

136.6 146 9.4 WPEG White/pink cg grad 5 epi? 1

PEGMATITE. Pinkish-white coarse-grained muscovite, biotite, K-spar, plag, quartz pegmamtite. Plag has moderated green epidote/clay(?) alteration.

146 188 42 MIGBlack and

whitefg sharp 45

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse grained white to pink; non-foliated pegmatite; non-magnetic. Plag in pegmatite has local green epidote/clay(?) alteration.

188 203 15 PPEGPink and

blackbx grad hem,chl,

ser,epi 3

PINK PEGMATITE, possibly a coarse-grained equivalent of the QUARTZ MONZONITE to GRANITE unit; Unit becomes progressivly more brecciated down-hole. Feldspars are pervasivley hemitized. Matrix is chloritic, with local gouge zones developed. Patchy sericite and epidote alteration. Coarse-grained books of muscovite locally.

203 204.85 1.85 DBf Black fg sharp 60 py bleb .5

FINE GRAINED MAFIC INTRUSIVE; Black to blue gray; fine grained; non-foliated; moderately to highly magnetic; very fresh/unaltered; py throughout in 1- 2 mm circluar blebs. Also py in calcite-chlorite veinlets; dominant mineralogy is acicular plagioclase and pyroxene. Well defined chill margins.

203 225.25 22.3 PPEGPink and

blackbx grad hem,chl,

ser,epi 4

PINK PEGMATITE, possibly a coarse-grained equivalent of the QUARTZ MONZONITE to GRANITE unit; Unit becomes progressivly more brecciaed down-hole. Feldspars are pervasivly hemitized. Matrix is chloritic, with local gouge zones developed. Patchy sericite and epidote alteration. Coarse-grained books of muscovite locally.

225.3 229.8 4.55 MIG Black/red mg grad 45 py dssm .75 hem,chl,

ser,epi 4

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse-grained white to pink; non-foliated pegmatite; non-magnetic. Unit is overprinted by large-scale breccia zone and associated hematite, chlorite, sericite and epidote alteration. .75-1% disseminated pyrite.

229.8 251 21.2 QMZPink and

blackbx grad py dssm .25 hem,chl,

ser,epi 4

QUARTZ MONZONITE to GRANITE unit; Unit becomes progressivley more brecciated and altered down-hole. Varies from fine- to coarse- grained; locally pegmatiic. Feldspars are pervasivley hemitized. Matrix is chloritic, with local gouge zones developed. Patchy sericite and epidote alteration. Coarse-grained books of muscovite locally. 10 cm clast of fine grained mafic unit at 237.8. Trace disseminated pyrite in fine-grained intervals.

HOLE NO.: GL-10-4

Page 1 of 1

MEGA URANIUM LTD. - SAMPLE RECORDProject: GREENWICH LAKELogged By: T. Gilman, S. KruseDate: March 10 - March 18, 2010



1 2 2286159 1.50 2.50 1.00 DBf 1 C Exploration 1 F-2 A10-1235286160 2.50 3.50 1.00 DBf 1 C Exploration 1 F-2 A10-1235286161 3.50 4.50 1.00 DBf 1 C Exploration 1 F-2 4 C A10-1235286162 4.50 5.15 0.65 DBf 1 C Exploration 1 F-2 A10-1235286163 203.00 204.00 1.00 DBf 1 C Exploration 1 F-2 A10-1235286164 204.00 204.85 0.85 DBf 1 C Exploration 1 F-2 A10-1235286165 1 C Exploration 1 F-2 A10-1235 Standard

HOLE NO.: GL-10-4

MEGA URANIUM LTD. - GEOTECH LOGProject: GREENWICH LAKELogged By: RJ MalloryDate: March 10 - March 17, 2010

From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)1.5 3 1.5 100.0% 1.2 40.0%3 6 2.65 88.3% 1.66 55.3%6 9 2.85 95.0% 2.33 77.7%9 12 2.94 98.0% 2.44 81.3%12 15 3 100.0% 2.6 86.7%15 18 3 100.0% 2.88 96.0%18 21 2.9 96.7% 2.6 86.7%21 24 3 100.0% 2.75 91.7%24 27 3 100.0% 2.78 92.7%27 30 3 100.0% 2.6 86.7%30 33 3 100.0% 2.38 79.3%33 36 3 100.0% 2.66 88.7%36 39 3 100.0% 2.7 90.0%39 42 3 100.0% 2.06 68.7%42 45 3 100.0% 2.91 97.0%45 48 3 100.0% 2.22 74.0%48 51 2.9 96.7% 2.78 92.7%51 54 3 100.0% 2.65 88.3%54 57 3 100.0% 2.68 89.3%57 60 3 100.0% 2.69 89.7%60 63 3 100.0% 2.56 85.3%63 66 3 100.0% 2.71 90.3%66 69 3 100.0% 2.31 77.0%69 72 3 100.0% 2.17 72.3%72 75 3 100.0% 2.64 88.0%75 78 3 100.0% 2.64 88.0%78 81 3 100.0% 2.36 78.7%81 84 3 100.0% 2.87 95.7%84 87 2.86 95.3% 2.42 80.7%87 90 2.9 96.7% 2.58 86.0%90 93 3 100.0% 2.87 95.7%93 96 3 100.0% 2.24 74.7%96 99 3 100.0% 2.49 83.0%99 102 3 100.0% 2.73 91.0%102 105 3 100.0% 2.26 75.3%105 108 2.9 96.7% 2.46 82.0%108 111 3 100.0% 2.82 94.0%111 114 3 100.0% 2.44 81.3%114 117 2.91 97.0% 2.47 82.3%117 120 2.62 87.3% 1.27 42.3%

HOLE NO.: GL-10-4




HOLE NO.: GL-10-4


120 123 2.84 94.7% 2.32 77.3%123 126 2.96 98.7% 2.76 92.0%126 129 2.85 95.0% 2.01 67.0%129 132 2.94 98.0% 2.28 76.0%132 135 3 100.0% 2.52 84.0%135 138 2.94 98.0% 2.28 76.0%138 141 2.71 90.3% 2.17 72.3%141 144 3 100.0% 2.3 76.7%144 147 2.97 99.0% 2.29 76.3%147 150 3 100.0% 1.88 62.7%150 153 2.83 94.3% 2.6 86.7%153 156 2.95 98.3% 2.45 81.7%156 159 3 100.0% 2.08 69.3%159 162 2.79 93.0% 2.15 71.7%162 165 2.93 97.7% 2.43 81.0%165 168 2.8 93.3% 1.55 51.7%168 171 2.82 94.0% 1.22 40.7%171 174 2.97 99.0% 2.71 90.3%174 177 3 100.0% 2.52 84.0%177 180 2.93 97.7% 2.68 89.3%180 183 2.85 95.0% 2.22 74.0%183 186 3 100.0% 1.6 53.3%186 189 3 100.0% 2.44 81.3%189 192 2.9 96.7% 2.2 73.3%192 195 2.73 91.0% 2 66.7%195 198 3 100.0% 2.65 88.3%198 201 2.96 98.7% 2.7 90.0%201 204 2.99 99.7% 2.01 67.0%204 207 2.88 96.0% 1.98 66.0%207 210 2.7 90.0% 1.72 57.3%210 213 3 100.0% 2.71 90.3%213 216 3 100.0% 2.65 88.3%216 219 3 100.0% 2.91 97.0%219 222 3 100.0% 2.58 86.0%222 225 3 100.0% 1.94 64.7%225 228 2.9 96.7% 2.4 80.0%228 231 3 100.0% 2.36 78.7%231 234 3 100.0% 2.44 81.3%234 237 2.96 98.7% 2.7 90.0%



HOLE NO.: GL-10-4


237 240 3 100.0% 2.21 73.7%240 243 3 100.0% 2.47 82.3%243 246 2.64 88.0% 1.32 44.0%246 249 2.92 97.3% 2.1 70.0%249 251 1.96 98.0% 1.5 75.0%251 EOH

MEGA URANIUM LTD. - DH GeophysicsProject: GREENWICH LAKELogged By: RJ MalloryDate: March 10 - March 17, 2010Mag Sus: KT-9, Core Diamater Set to: 4.00

Meter Mag Susc. CPS (>500) Comments2 14.06 Fine Grained Mafic Intrusive4 16.73 Fine Grained Mafic Intrusive6 0.033 Pegmatite/Migmatite8 0.05510 0.13212 0.01814 0.06716 0.02118 0.03320 0.02722 0.15824 0.02726 0.06928 0.16330 0.08332 0.02334 0.35736 0.3938 0.38440 0.20342 0.07444 0.07646 0.0448 0.10850 0.04152 0.28254 0.06456 0.13258 0.0760 0.17162 0.11264 0.2266 0.09868 0.25170 0.19872 0.20374 0.44376 0.178 0.34780 0.01982 0.10184 -0.1286 0.036

HOLE NO.: GL-10-4



HOLE NO.: GL-10-4

88 0.27190 0.02792 -0.02194 0.32496 0.20298 0.203

100 0.038102 0.152104 0.204106 0.031108 0.16110 0.029112 0.02114 0.02116 0.048118 0.027120 0.022122 0.008124 0.117126 0.186128 0.27130 0.053132 0.145134 0.296136 0.078138 0.002140 0.015142 0.14144 0.021146 0.08148 0.123150 0.085152 0.009154 0.19156 0.091158 0.021160 0.133162 0.022164 0.017166 0.009168 0.017170 0.015172 0.035



HOLE NO.: GL-10-4

174 0.006176 0.096178 0.019180 0.045182 0.022184 0.038186 0.078188 0.028190 0.007192 0.026194 0.088196 0.449198 0.057200 0.106202 0.043204 5.986206 0.021208 0.02210 0.01212 0.088214 0.02216 0.108218 0.134220 0.189222 0.138224 0.002226 0.121228 0.183230 0.062232 0.015234 0.028236 0.217238 0.061240 0.008242 0.035244 0.142246 0.101248 0.111250 0.016 EOH 251 m

EASTING: 0362924

NORTHING: 5408767

ELEVATION: 439 m

AZIMUTH: 067

DIP: -50

E.O.H: 251 m



GL-10-4

067247

0.0

50.0

100.0

150.0

200.0

250.0

0 to 64

Magnetic Susce

ptibility



Gabbro

Migmatite

OverburdenPink Pegmatite

Quartz Monzonite

Water

White Pegmatite

Location:

Footage Degrees



200 m n/a 4244232

From To0.0 3.6

3.6 49.4

49.4 124.3

124.3 135.3

135.3 250.0

250.0


51A/15

Location Map


Date Started:


Migmatite and Pink to White Pegmatite

EOH

Gabbro

Overburden

EOH

Cobra Drilling

March 7, 2010


March 8 - March Date Completed:

March 11, 2010

Tony Gilman

Meterage

Hole No.: GL-10-5 250 m 441 m

Collar Elevation:


Zone 16NNAD 83

Migmatite

Migmatite and Pink to White Pegmatite


Size: NQ core

Azimuth:

270


From To

Leng

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Roc

k C

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Col

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Con

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Ang

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CA

Sul

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Text

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Alte

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n

Alte

ratio

n In

tens

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3.64 49.4 45.8 MIG Black fg/mg sharp 35MIGMATITE; Black to steely gray; fne to coarse grained; well foliated; foliation at 30 deg TCA; cut by numerous white, coasre grained pegmatite veins; dominant mineralogy of melanocratic sections is biotite, plagioclase, and hornblende.

49.4 58.4 9 PPEG Pink cgPINK PEGMATITE; Pink to grey, coarse grained; non-foliated; non-magnetic; weak, pervasive, sericite replacement of feldspars.

58.4 108.4 50 MIGBlack and

Whitefg/cg sharp 90

MIGMATITE; Black alternating with white to pink; fine grained melanosomes dominated by biotite and hornblende with medium to coarse grained lecosomes of white to pink pegmatite; moderatley to well foliated; dominatly weakly magnetic, containing one section @ 62 - 63 m of magnetite stringers; lower contact 90 deg TCA.

108.4 115.26 6.86 PPEG Pink cg gradPINK PEGMATITE; Pink to grey, coarse grained; non-foliated; non-magnetic; weak, pervasive, sericite replacement of feldspars.

115.26 124.3 9.04 MIGBlack and

Whitefg/cg

MIGMATITE; Black alternating with white to pink; fine grained melanosomes dominated by biotite and hornblende with medium to coarse grained lecosomes of white to pink pegmatite; moderatley to well foliated; weakly magnetic.

124.3 135.3 11 GAB Black to Green mg sharp 60 py dssm 5

GABBRO; Black to green; medium grained; non-foliated; commonly cut by 1-3 mm wide hematized, quartz veins @ 45 to 90 deg TCA; weakly magnetic; contains 3-5% dssm pyrite; dominant minerology is plagioclase and pyroxene; lower contact in fault contact @ 90 deg TCA; lower contact strongly hematized.

135.3 186 50.7 PPEG Pink cg fault 90PINK PEGMATITE; Pink to grey, coarse grained; non-foliated; non-magnetic; weak, pervasive, sericite replacement of feldspars.

186 250 64 MIGBlack and

Whitefg/cg

MIGMATITE; Black alternating with white to pink; fine grained melanosomes dominated by biotite and hornblende with medium to coarse grained lecosomes of white to pink pegmatite; moderatley to well foliated; weakly magnetic.

HOLE NO.: GL-10-5

Page 1 of 1




1 2 3286147 124.30 125.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286148 125.30 126.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286149 126.30 127.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286150 126.30 127.30 1C Exploration 1 F-2 Comp A10-1235 DUPLICATE

286151 127.30 128.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286152 128.30 129.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286153 129.30 130.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286154 130.30 131.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286155 131.30 132.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286156 132.30 133.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286157 133.30 134.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235286158 134.30 135.30 1.00 GAB 1C Exploration 1 F-2 Comp A10-1235

HOLE NO.: GL-10-5


From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)3.64 5 1.36 44.6% 1.04 34.1%5 8 2.9 96.7% 1.47 49.0%8 11 3 100.0% 2.78 92.7%11 14 2.96 98.7% 2.66 88.7%14 17 3 100.0% 2.24 74.7%17 20 3 100.0% 2.3 76.7%20 23 3 100.0% 2.72 90.7%23 26 3 100.0% 2.52 84.0%26 29 2.97 99.0% 2.42 80.7%29 32 3 100.0% 2.95 98.3%32 35 3 100.0% 2.91 97.0%35 38 3 100.0% 2.8 93.3%38 41 3 100.0% 2.35 78.3%41 44 3 100.0% 2.54 84.7%44 47 3 100.0% 2.79 93.0%47 50 3 100.0% 2.94 98.0%50 53 3 100.0% 2.67 89.0%53 56 3 100.0% 2.65 88.3%56 59 2.93 97.7% 2.73 91.0%59 62 2.93 97.7% 2.7 90.0%62 65 2.9 96.7% 2.63 87.7%65 68 3 100.0% 2.77 92.3%68 71 3 100.0% 2.49 83.0%71 74 2.97 99.0% 2.51 83.7%74 77 3 100.0% 2.51 83.7%77 80 3 100.0% 2.7 90.0%80 83 2.95 98.3% 2.88 96.0%83 86 3 100.0% 2.94 98.0%86 89 3 100.0% 2.84 94.7%89 92 3 100.0% 2.7 90.0%92 95 2.92 97.3% 2.77 92.3%95 98 3 100.0% 2.72 90.7%98 101 3 100.0% 2.77 92.3%101 104 2.96 98.7% 2.76 92.0%104 107 3 100.0% 2.72 90.7%107 110 2.95 98.3% 2.47 82.3%110 113 3 100.0% 2.59 86.3%113 116 2.99 99.7% 2.66 88.7%116 119 2.95 98.3% 2.55 85.0%119 122 3 100.0% 2.31 77.0%

HOLE NO.: GL-10-5




HOLE NO.: GL-10-5


122 125 3 100.0% 2.82 94.0%125 128 3 100.0% 2.52 84.0%128 131 2.9 96.7% 2.67 89.0%131 134 3 100.0% 2.32 77.3%134 137 2.92 97.3% 1.88 62.7%137 140 2.99 99.7% 1.96 65.3%140 143 3 100.0% 2.55 85.0%143 146 2.86 95.3% 2.31 77.0%146 149 2.92 97.3% 2.42 80.7%149 152 3 100.0% 2.85 95.0%152 155 2.96 98.7% 2.51 83.7%155 158 3 100.0% 2.94 98.0%158 161 2.92 97.3% 2.76 92.0%161 164 2.88 96.0% 2.47 82.3%164 167 3 100.0% 2.4 80.0%167 170 3 100.0% 2.03 67.7%170 173 2.93 97.7% 2.31 77.0%173 176 2.94 98.0% 2.29 76.3%176 179 2.85 95.0% 1.85 61.7%179 182 2.88 96.0% 2.2 73.3%182 185 3 100.0% 2.51 83.7%185 188 2.99 99.7% 1.91 63.7%188 191 3 100.0% 2.65 88.3%191 194 2.92 97.3% 2.51 83.7%194 197 2.94 98.0% 2.49 83.0%197 200 3 100.0% 2.7 90.0%200 203 3 100.0% 2.71 90.3%203 205 2.99 99.7% 2.66 88.7%205 208 2.91 97.0% 2.18 72.7%208 211 3 100.0% 2.3 76.7%211 214 2.97 99.0% 2.52 84.0%214 217 2.79 93.0% 2.64 88.0%217 220 2.94 98.0% 2.75 91.7%220 223 3 100.0% 2.44 81.3%223 226 3 100.0% 2.61 87.0%226 229 2.94 98.0% 2.43 81.0%229 232 2.98 99.3% 2.56 85.3%232 235 3 100.0% 2.8 93.3%235 238 3 100.0% 2.76 92.0%



HOLE NO.: GL-10-5


238 241 3 100.0% 2.15 71.7%241 244 2.93 97.7% 2.63 87.7%244 247 3 100.0% 2.71 90.3%247 250 3 100.0% 3 100.0%250 EOH



6 0.235

8 0.391

10 0.047

12 0.036

14 0.041

16 0.081

18 0.047

20 0.055

22 0.096

24 0.12

26 0.17

28 0.166

30 0.317

32 0.121

34 0.165

36 0.36

38 0.233

40 0.026

42 0.02

44 0.341

46 0.053

48 0.146

50 0.041

52 0.036

54 0.081

56 0.074

58 0.05

60 0.931

62 63.57 Magnetie rich section64 0.052

66 0.035

68 0.034

70 0.153

72 0.088

74 0.103

76 0.091

78 0.224

80 0.02

82 0.02

84 0.01

86 0.098

88 0.208

HOLE NO.: GL-10-5



HOLE NO.: GL-10-5

90 0.1

92 0.048

94 0.033

96 0.068

98 0.057

100 0.024

102 0.117

104 0.209

106 0.023

108 0.133

110 0.044

112 0.016

114 0.005

116 0.175

118 0.186

120 0.019

122 0.109

124 0.141

126 0.021

128 0.23

130 0.335

132 0.223

134 0.148

136 0.028

138 0.048

140 0.02

142

144 0.51

146 0.48

148 0.402

150 0.245

152 0.432

154 0.77

156 0.3

158 0.006

160 0.002

162 2.121

164 0.061

166 0.132

168 0.183

170 0.005

172 0.028

174 0.024



HOLE NO.: GL-10-5

176 0.205

178 0.028

180 0.37

182 0.055

184 0.046

186 0.028

188 0.015

190 0.376

192 0.255

194 0.7

196 0.063

198 0.089

200 0.143

202 0.398

204 0.111

206 0.179

208 0.012

210 0.109

212 0.062

214 0.067

216 0.481

218 0.1

220 0.031

222 0.089

224 0.145

226 0.101

228 0.117

230 0.128

232 0.05

234 0.093

236 0.105

238 0.843

240 0.107

242 0.064

244 0.44

246 0.095

248 0.019

250 0.01

EASTING: 0363374

NORTHING: 5409302

ELEVATION: 441 m

AZIMUTH: 270

DIP: -50

E.O.H: 250 m



GL-10-5

090270

0.0

50.0

100.0

150.0

200.0

250.0

0 to 64


LithologyFine Grained Mafic IntrusiveFoliated Mafic IntrusiveGabbroMigmatiteOverburdenPink PegmatiteQuartz MonzoniteWaterWhite Pegmatite

Location:

Footage Degrees



200 m 4211693

From To0 72.3

72.3 83.3683.36 83.8483.84 85.0885.08 122.46

122.46 123.9123.9 225.0EOH

Gabbro - 3-4% py and cpy


LAND HOLE

Zone 16N

NAD 83

Granitic Orthogneiss

Quartz Monzonite

Quartz Monzonite


Size: NQ core

Azimuth:

060

EOH

Cobra Drilling

March 17, 2010


March 18 - 20thDate Completed:

March 20, 2010

Stefan Kruse

Meterage

Hole No.: GL-10-6 225 m 508 m

Collar Elevation:

Gabbro - 3-4% py and cpy

Quartz Monzonite

Quartz Monzonite


51A/15

Location Map


Date Started:


MEGA URANIUM LTD. - GEOLOGICAL LOGProject: GREENWICH LAKE Easting: 0361745Logged By: S. Kruse Northing: 5404876Date: March 17 - March 20, 2010 Datum & Projection: NAD 83, UTM Zone 16 N

From To

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%

Alte

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Alte

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n In

tens

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Comments

0.00 72.30 72.3 QMZ Pink mg py vnlt .25

QUARTZ MONZONITE - biotite, magnetite Quartz Monzonite. Generally medium grained, but contains some melanocratic fine grained intervals and locally coarse-grain/pegmatitic intervals as well. Contains ~1-2% magnetite. Sparse 0.5-2 cm wide grey quartz veins contain trace pyrite.

72.30 83.36 11.06 GAB Black fg sharp 29 py,cpy bleb 3

GABBRO - Fine-grained mafic intrusive rock with chilled margins. Slightly porphyritic texture with 1-4mm pyroxenes in a maritx of possible fine-grained chlorite altered plagioclase. Strongly magnetic. Pyrite is disseminated in 1-15mm blebs and in discontinous veinlets Some pyrite blebs contain trace cpy. Late factures contain calcite and chlorite infill.

83.36 83.84 0.48 QMZ Pink mg sharp 70 QUARTZ MONZONITE - biotite, magnetite Quartz Monzonite. Generally medium grained, Contains ~1-2% magnetite.

83.84 85.08 1.24 GAB Black fg broken n/A py,cpy bleb 3

GABBRO- Fine-grained mafic intrusive rock with chilled margins. Slightly porphyritic texture with 1-4mm pyroxenes in a maritx of possible fine-grained chlorite altered plagioclase. Strongly magnetic. Pyrite is disseminated in 1-15mm blebs and in discontinous veinlets Some pyrite blebs contain trace cpy. Late factures contain calcite and chlorite infill.

85.08 122.46 37.38 QMZ Pink mg sharp 46 py vnlt .25


122.46 123.90 1.44 QMZ Black mg grad 45 py, cpy bleb 5 hem 2GRANTIC GNEISS - Hrnb, K-spar, Pl, Qrtz orthogneiss. Locally brecciated. Up to 5% pyrite in irregular belbs in quartz veins and breccia zones. Boiling textures and .5% Cpy in quartz vein at 123.8 m. Patchy brick-red hematite staing of feldspars

123.90 225.00 101.1 QMZ Pink mg sharp 46 py vnlt .25


EOH

HOLE NO.: GL-10-6

Page 1 of 1

MEGA URANIUM LTD. - SAMPLE RECORDProject: GREENWICH LAKELogged By: S. KruseDate: March 17 - 20th



1 2 3286166 72.30 73.00 0.70 PER 1 C Exploration 1 F-2 A10-1235286167 73.00 74.00 1.00 PER 1 C Exploration 1 F-2 A10-1235286168 74.00 75.00 1.00 PER 1 C Exploration 1 F-2 4C A10-1235286169 75.00 76.00 1.00 PER 1 C Exploration 1 F-2 A10-1235286170 0.00 1 C Exploration 1 F-2 A10-1235 Standard286171 76.00 77.00 1.00 PER 1 C Exploration 1 F-2 A10-1235286172 77.00 78.00 1.00 PER 1 C Exploration 1 F-2 A10-1235286173 78.00 79.00 1.00 PER 1 C Exploration 1 F-2 4C A10-1235286174 79.00 80.00 1.00 PER 1 C Exploration 1 F-2 A10-1235286175 80.00 81.00 1.00 PER 1 C Exploration 1 F-2 A10-1235286176 81.00 82.00 1.00 PER 1 C Exploration 1 F-2 4C A10-1235286177 82.00 83.00 1.00 PER 1 C Exploration 1 F-2 A10-1235286178 83.00 83.36 0.36 PER 1 C Exploration 1 F-2 A10-1235286179 83.36 83.84 0.48 QMZ 1 C Exploration 1 F-2 A10-1235286180 83.36 83.84 0.48 QMZ 1 C Exploration 1 F-2 A10-1235 Dup286181 83.84 85.08 1.24 PER 1 C Exploration 1 F-2 A10-1235286182 122.46 123.9 1.44 GG 1 C Exploration 1 F-2 A10-1235

HOLE NO.: GL-10-6


From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)1 2 1 100.0% 0.9 90.0%2 5 3 100.0% 2.6 86.7%5 8 3 100.0% 2.95 98.3%8 11 3 100.0% 2.85 95.0%11 14 3 100.0% 3 100.0%14 17 3 100.0% 2.84 94.7%17 20 3 100.0% 2.75 91.7%20 23 3 100.0% 1.9 63.3%23 26 2.92 97.3% 2.18 72.7%26 29 3 100.0% 2.88 96.0%29 32 2.94 98.0% 2.55 85.0%32 35 3 100.0% 2.72 90.7%35 38 3 100.0% 2.5 83.3%38 41 3 100.0% 2.59 86.3%41 44 2.98 99.3% 2.65 88.3%44 47 3 100.0% 2.98 99.3%47 50 2.95 98.3% 2.81 93.7%50 53 3 100.0% 3 100.0%53 56 3 100.0% 2.75 91.7%56 59 3 100.0% 2.77 92.3%59 62 3 100.0% 2.86 95.3%62 65 2.92 97.3% 2.4 80.0%65 68 2.69 89.7% 2.07 69.0%68 71 2.85 95.0% 1.35 45.0%71 74 3 100.0% 2.42 80.7%74 77 2.96 98.7% 2.73 91.0%77 80 3 100.0% 2.95 98.3%80 83 2.92 97.3% 2.71 90.3%83 86 2.9 96.7% 2.25 75.0%86 89 2.93 97.7% 2.46 82.0%89 92 3 100.0% 2.64 88.0%92 95 2.55 85.0% 2.03 67.7%95 98 2.78 92.7% 2.04 68.0%98 101 3 100.0% 2.77 92.3%101 104 3 100.0% 2.86 95.3%104 107 2.98 99.3% 2.85 95.0%107 110 3 100.0% 2.8 93.3%110 113 3 100.0% 2.67 89.0%113 116 3 100.0% 2.47 82.3%116 119 3 100.0% 2.69 89.7%

HOLE NO.: GL-10-6




HOLE NO.: GL-10-6


119 122 3 100.0% 2.57 85.7%122 125 2.89 96.3% 2.14 71.3%125 128 3 100.0% 2.54 84.7%128 131 3 100.0% 2.88 96.0%131 134 2.98 99.3% 2.38 79.3%134 137 3 100.0% 2.85 95.0%137 140 3 100.0% 2.67 89.0%140 143 2.98 99.3% 2.78 92.7%143 146 2.91 97.0% 2.71 90.3%146 149 3 100.0% 2.76 92.0%149 152 2.87 95.7% 2.43 81.0%152 155 3 100.0% 2.7 90.0%155 158 3 100.0% 2.78 92.7%158 161 2.94 98.0% 2.71 90.3%161 164 2.97 99.0% 2.97 99.0%164 167 3 100.0% 2.85 95.0%167 170 3 100.0% 2.84 94.7%170 173 2.91 97.0% 2.78 92.7%173 176 3 100.0% 2.79 93.0%176 179 2.97 99.0% 2.8 93.3%179 182 2.93 97.7% 2.93 97.7%182 185 3 100.0% 2.82 94.0%185 188 2.98 99.3% 2.74 91.3%188 191 3 100.0% 2.95 98.3%191 194 2.98 99.3% 2.89 96.3%194 197 3 100.0% 2.9 96.7%197 200 3 100.0% 2.97 99.0%200 203 2.87 95.7% 2.68 89.3%203 206 3 100.0% 2.22 74.0%206 209 3 100.0% 2.59 86.3%209 212 3 100.0% 2.12 70.7%212 215 3 100.0% 2.78 92.7%215 218 2.85 95.0% 2.39 79.7%218 221 2.88 96.0% 1.8 60.0%221 224 3 100.0% 2.47 247.0%224 225 1 100.0% 1 100.0%EOH EOH EOH EOH EOH EOH


Meter Mag Susc. CPS (>500) Comments2 2.2294 1.329

6 1.572

8 5.513

10 6.313

12 3.563

14 1.704

16 0.769

18 3.712

20 3.44

22 7.053

24 2.042

26 0.893

28 0.054

30 4.617

32 6.63

34 2.354

36 6.193

38 3.108

40 3.33

42 1.396

44 3.116

46 3.307

48 2.793

50 2.643

52 3.305

54 3.043

56 1.634

58 2.441

60 0.048

62 2.263

64 0.027

66 0.047

68 0.014

70 0.053

72 8.888

74 55.63

76 4.227

78 10.3

80 35.86

HOLE NO.: GL-10-6



HOLE NO.: GL-10-6

82 23.24

84 38.63

86 0.015

88 0.033

90 0.014

92 0.018

94 0.003

96 0.033

98 0.023

100 0.045

102 0.669

104 0.072

106 0.169

108 0.025

110 0.036

112 0.03

114 0.019

116 0.01

118 0.025

120 0.016

122 0.028

124 0.038

126 0.026

128 0.026

130 0.016

132 0.005

134 0.039

136 0.083

138 0.045

140 0.669

142 3.387

144 2.087

146 0.017

148 2.885

150 0.1

152 0.069

154 1.119

156 0.767

158 1.539

160 2.275



HOLE NO.: GL-10-6

162 3.348

164 1.994

166 1.185

168 1.817

170 3.117

172 3.137

174 3.093

176 2.101

178 4.215

180 2.95

182 0.549

184 1.19

186 1.124

188 0.107

190 4.674

192 6.697

194 4.822

196 2.631

198 0.033

200 2.243

202 0.062

204 0.038

206 0.022

208 0.05

210 0.272

212 0.549

214 0.809

216 0.143

218 0.024

220 0.113

222 0.507

224 0.043

EOH EOH

EASTING: 0361745

NORTHING: 5404876

ELEVATION: 508 m

AZIMUTH: 060

DIP: -50

E.O.H: 225 m



GL-10-6

060240

0.0

50.0

100.0

150.0

200.0

0 to 64

Magnetic Susce

ptibility



Gabbro

Migmatite

Overburden

Pink Pegmatite

Quartz Monzonite

Water

White Pegmatite

Location:

Footage Degrees



200 m 4207834

From To0 2.2

2.2 39.439.4 46.37

46.37 50.6750.67 51.551.5 65.73

65.73 66.5666.56 120.05

120.05 121.1121.1 122.81

122.81 134.6134.6 168.49

168.49 201201

51A/15

Location Map

Fine Grained Mafic Intrusive



Date Started:

EOH

Quartz MonzoniteMafic Biotite Gniess

Quartz MonzoniteMigmatite and Pegmatite

Migmatite and Pegmatite

Quartz Monzonite

Overburden




Quartz Monzonite

Quartz Monzonite

March 18, 2010


March 19 - March 23rdDate Completed:

March 24, 2010

Stefan Kruse & Tony Gilman

Meterage


LAND HOLE

Zone 16N

NAD 83EOH

Rugged Drilling

Hole No.: GL-10-7 201 m 434 m

Collar Elevation:

5404687 NorthProject: GREENWICH LAKE

Size: BTW core

Azimuth:

255

0363832 EastDip of Drill Hole

MEGA URANIUM LTD. - GEOLOGICAL LOGProject: GREENWICH LAKE Easting: 0363832Logged By: S. Kruse/T. Gilman Northing: 5404687Date: March 18 - March 24, 2010 Datum & Projection: NAD 83, UTM Zone 16 N

From To

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Comments

0.00 2.20 Overburden

2.20 39.40 37.2 MIGWhite and

Blackcg grad 20 py dssm .25 clay, epi 1

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse grained white to pink; non-foliated pegmatite; non-magnetic. Plag in pegmatite has local green epidote/clay(?) alteration. Trace 0.5-1 mm grains of pyrite. Contains mafic, biotite rich, foliated sections.

39.40 46.37 6.97 QMZ Pink mg grad 20 clay,ser 1QUARTZ MONZONITE - biotite, magnetite Quartz Monzonite. Generally medium grained, and weakly banded. Local sericte/clay alteration of feldspars.

46.37 50.67 4.3 MIGWhite and

Blackcg grad 20 py dssm .25 clay, epi 1

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse grained white to pink; non-foliated pegmatite; non-magnetic. Plag in pegmatite has local green epidote/clay(?) alteration. Trace 0.5-1 mm grains of pyrite.

50.67 51.50 0.83 QMZ Pink mg grad 20 clay,ser 1 QUARTZ MONZONITE - biotite, magnetite Quartz Monzonite. Generally medium grained, and weakly banded. Local sericte/clay alteration of feldspars.

51.50 65.73 14.2 MIG Grey black mg sharp 45 py dssm .25 clay, epi 1

MIGMATITE and PEGMATITE with foliated medium grained mafic sections; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse grained white to pink; non-foliated pegmatite; non-magnetic. Plag in pegmatite has local green epidote/clay(?) alteration. Trace 0.5-1 mm grains of pyrite. Interval from 56.6-59.5 is locally brecciated and contains brick-red hematite alteration. Anomalous radiation up to 420 CPS recorded within breccia zone.

65.73 66.56 0.83 QMZ Pink mg grad 30 clay,ser 1 QUARTZ MONZONITE - biotite, magnetite Quartz Monzonite. Generally medium grained, and weakly banded. Local sericte/clay alteration of feldspars.

66.56 120.05 53.5 MIG Grey black mg sharp 30 py dssm .25 clay, epi 1

MIGMATITE with PEGMATITE with MAFIC BIOTITE GNIESS; Biotite Gniess - Medium to fine grained biotite, quartz plagioclase gneiss. Grey to black and relatively homogenous. Trace disseminated pyrite. Weak clay/epidote alteration of feldspars. Interdigitated with 5-10 cm intervals of QMZ and MIG. Migmatite and Pegmatite; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse-grained white to pink; non-foliated pegmatite; non-magnetic. Plag in pegmatite has local green epidote/clay(?) alteration. Trace 0.5-1 mm grains of pyrite.

120.05 121.10 1.05 QMZ Pink mg grad 30 py dssm .25 hem 2QUARTZ MONZONITE - biotite, magnetite Quartz Monzonite. Generally medium grained, and weakly banded. Hematite alteration of plagioclase. Local sericte/clay alteration of feldspars.

121.10 122.10 1 DBm Grey black mg irreg py frac .25 clay, epi 1 MAFIC BIOTITE GNIESS. Medium to fine grained biotite, quartz plagioclase

gneiss. Grey to black and relatively homogenous. Subtle folding in banded layers. Trace pyrite on fractures. Weak clay/epidote alteration of feldspars.

122.81 134.60 11.8 DBf Black fg sharp 25FINE GRAINED MAFIC INTRUSIVE (DIABASE) - Black to dark grey/green; fine grained mafic intrusive; non-foliated; lower contact with 60 deg TCA and shows brick red hematite alteration, moderate, pervasive chlorite alteration of feldspars; strongly magnetic; trace py.

134.60 168.49 33.9QMZ Pink cg sharp 60 py dssm tr hm 2

QUARTZ MONZONITE - Pink to brick red; coarse grained to pegmatitic; non-foliated; locally contains sercite alteration of feldspar; lower 4 m moderatley to well foliated; lower contact gradational.

168.49 201.00 32.5 MIGWhite and

Black

fg to cg irreg

MIGMATITE and PEGMATITE; Black and white to pink; alternating moderately to well foliated fine to medium grained melanosomes with coarse-grained white to pink; non-foliated pegmatite leucosomes; non-magnetic. Plag in pegmatite has local green epidote and sercite/clay(?) alteration.

HOLE NO.: GL-10-7

Page 1 of 1

MEGA URANIUM LTD. - SAMPLE RECORDProject: GREENWICH LAKELogged By: S. KruseDate: March 18 - March 24, 2010



1 2 3286216 122.70 124.00 1.30 Dbf 1 C Exploration 1 F-2 A10-1323286217 124.00 125.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286218 125.00 126.00 1.00 Dbf 1 C Exploration 1 F-2 4C A10-1323286219 126.00 127.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286220 127.00 128.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286221 128.00 129.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286222 129.00 130.00 1.00 Dbf 1 C Exploration 1 F-2 4C A10-1323286223 130.00 131.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286224 131.00 132.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286225 132.00 133.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286226 133.00 134.00 1.00 Dbf 1 C Exploration 1 F-2 A10-1323286227 134.00 134.45 0.45 Dbf 1 C Exploration 1 F-2 4C A10-1323

HOLE NO.: GL-10-7

MEGA URANIUM LTD. - GEOTECH LOGProject: GREENWICH LAKELogged By: Mike McNeill/RJ MalloryDate: March 20 - March 24, 2010

From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)2.2 3 0.8 80.0% 0.57 57.0%3 6 3 100.0% 2.56 85.3%6 9 2.2 73.3% 2.05 68.3%9 12 2.98 99.3% 2.6 86.7%12 15 3 100.0% 2.86 95.3%15 18 2.62 87.3% 2.43 81.0%18 21 3 100.0% 2.78 92.7%21 24 3 100.0% 2.81 93.7%24 27 3 100.0% 1.43 47.7%27 30 3 100.0% 2.97 99.0%30 33 3 100.0% 2.67 89.0%33 36 2.96 98.7% 2.38 79.3%36 39 3 100.0% 2.8 93.3%39 42 3 100.0% 2.74 91.3%42 45 3 100.0% 2.88 96.0%45 48 3 100.0% 2.76 92.0%48 51 2.94 98.0% 2.73 91.0%51 54 2.93 97.7% 2.68 89.3%54 57 3 100.0% 1.4 46.7%57 60 3 100.0% 2.38 79.3%60 63 2.95 98.3% 2.17 72.3%63 66 3 100.0% 2.96 98.7%66 69 3 100.0% 2.34 78.0%69 72 2.94 98.0% 2.28 76.0%72 75 3 100.0% 2.47 82.3%75 78 2.82 94.0% 2.51 83.7%78 81 3 100.0% 2.23 74.3%81 84 2.98 99.3% 2.73 91.0%84 87 3 100.0% 2.13 71.0%87 90 2.98 99.3% 2.72 90.7%90 93 3 100.0% 2.55 85.0%93 96 2.99 99.7% 2.77 92.3%96 99 2.85 95.0% 2.24 74.7%99 102 2.3 76.7% 1.1 36.7%102 105 2.98 99.3% 2.86 95.3%105 108 2.98 99.3% 2.38 79.3%108 111 3 100.0% 2.83 94.3%111 114 2.96 98.7% 2.34 78.0%114 117 3 100.0% 2.01 67.0%117 120 2.99 99.7% 2.27 75.7%

HOLE NO.: GL-10-7


MEGA URANIUM LTD. - GEOTECH LOGProject: GREENWICH LAKELogged By: Mike McNeill/RJ MalloryDate: March 20 - March 24, 2010


HOLE NO.: GL-10-7


120 123 2.9 96.7% 2.45 81.7%123 126 2.97 99.0% 2.68 89.3%126 129 2.95 98.3% 2.7 90.0%129 132 2.9 96.7% 2.14 71.3%132 135 3 100.0% 1.95 65.0%135 138 2.95 98.3% 2.43 81.0%138 141 3 100.0% 2.53 84.3%141 144 2.87 95.7% 2.65 88.3%144 147 3 100.0% 2.57 85.7%147 150 3 100.0% 2.4 80.0%150 153 2.95 98.3% 2.4 80.0%153 156 2.8 93.3% 2.52 84.0%156 159 2.9 96.7% 2.49 83.0%159 162 2.97 99.0% 2.77 92.3%162 165 2.92 97.3% 2 66.7%165 168 3 100.0% 2.35 78.3%168 171 2.92 97.3% 2.46 82.0%171 174 3 100.0% 2.84 94.7%174 177 2.94 98.0% 2.64 88.0%177 180 3 100.0% 2.89 96.3%180 183 3 100.0% 2.84 94.7%183 186 3 100.0% 2.7 90.0%186 189 3 100.0% 2.55 85.0%189 192 3 100.0% 2.91 97.0%192 195 2.98 99.3% 2.73 91.0%195 198 3 100.0% 2.8 93.3%198 201 3 100.0% 2.65 88.3%EOH EOH EOH EOH EOH EOH

MEGA URANIUM LTD. - DH GeophysicsProject: GREENWICH LAKELogged By: Mike McNeill/RJ MalloryDate: March 20 - March 24, 2010Mag Sus: KT-9, Core Diamater Set to: 4.00


6 0.007

8 0.031

10 0.064

12 0.008

14 0.022

16 0.034

18 0.033

20 0.008

22 0.021

24 0.028

26 0.054

28 0.019

30 0.013

32 0.154

34 0.033

36 0.02

38 0.034

40 0.035

42 0.038

44 0.021

46 0.024

48 0.052

50 0.032

52 0.217

54 0.083

56 0.097

58 0.078

60 0.058

62 0.114

64 0.123

66 0.052

68 0.154

70 0.099

72 2.443

74 0.09

76 0.083

78 0.024

80 0.131

82 0.009

HOLE NO.: GL-10-7

84 0.261

86 0.211

88 0.183

90 0.194

92 0.013

94 0.228

96 0.24

98 0.085

100 0.104

102 0.004

104 0.037

106 0.156

108 0.013

110 0.065

112 0.036

114 0.077

116 0.054

118 0.03

120 0.038

122 0.04

124 12.96

126 14.28

128 12.99

130 14.28

132 14.84

134 24.9

136 0.048

138 0.096

140 0.111

142 0.047

144 0.372

146 0.1

148 0.051

150 0.059

152 0.536

154 0.693

156 0.13

158 0.212

160 0.078

162 0.067

164 0.063

166 0.062

168 0.057

170 0.09

172 0.055

174 0.012

176 0.088

178 0.012

180 0.153

182 0.169

184 0.088

186 0.001

188 0.056

190 0.135

192 0.907

194 0.216

196 0.02

198 0.001

200 0.025

EOH EOH

EASTING: 0363832

NORTHING: 5404687

ELEVATION: 434 m

AZIMUTH: 255

DIP: -50

E.O.H: 201m



GL-10-7

075255

0.0

50.0

100.0

150.0

200.0

0 to 64


GL-10-7


Foliated Mafic IntrusiveGabbro

MigmatiteOverburden

Pink PegmatiteQuartz Monzonite

Water

White Pegmatite

Location:

Footage Degrees



200 m 4211690

From To0 39.71

144.75 168.8

168.8 182.48

182.48 196.35

196.35 209


LAND HOLE

Zone 16N

NAD 83

QUARTZ MONZONITE

MIGMATITE


Size: NQ core

Azimuth:

315

Total Depth:

Cobra Drilling

March 21, 2010


March 22 - March 24thDate Completed:

March 23, 2010

Stefan Kruse

Meterage

Hole No.: GL-10-8 209 m 472 m

Collar Elevation:

MIGMATITE

QUARTZ MONZONITE

GABBRO - medium grained, epidote/chlorite/hematite alteration


51A/15

Location Map


Date Started:


MEGA URANIUM LTD. - GEOLOGICAL LOGProject: GREENWICH LAKE Easting: 0362153Logged By: S. Kruse Northing: 5406622Date: March 21 - March 23, 2010 Datum & Projection: NAD 83, UTM Zone 16 N

From To

Leng

th

Roc

k C

ode

Col

our

Text

ure

Con

tact

Angl

e TC

A

Sulp

hide

Typ

e

Text

ure

Sulp

hide

%

Alte

ratio

n

Alte

ratio

n In

tens

ity

Comments

0 144.75 145 GAB green-black mg 45 py dsmm .25 hem,epi,

chl 3

GABBRO - 2-4 mm tabular plagioclase crystals in a mafic (pyroxene rich) groundmass. Significant replacement of plag with epidote+-hematite and replacement of groundmass with epidote+chlorite. 1-2% magnetite. Trace disseminated very fine-grained py. 33.90-35.0 m heavily altered (hematite and epidote) interval surrounding a qtz+cal vein.

144.75 168.8 24.1 QMZ red cg 65 hem 3QUARTZ MONZONITE - Course-grained quartz monozonite. Hematite alteration is strongest proximal to overlying Gabbro contact, decreasing in intensity down hole. Trace py on late fractures.

168.8 182.48 13.7 MIGblack and

whitecg sheare

d 80 py frac .25 epi,chl

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse-grained white to pink; non-foliated pegmatite; non-magnetic. Commonly contains both biotite and muscovite. Plag in pegmatite has local green epidote/clay(?) alteration. Trace py on fractures.

182.48 196.35 13.9 QMZ red cg sharp 85 hem 3 QUARTZ MONZONITE - Course-grained quartz monozonite. Patchy hematite alteration.

196.35 209 12.7 MIGblack and

whitecg

MIGMATITE and PEGMATITE; Black and white to pink; alternating well foliated fine to medium grained melanosomes with coarse-grained white to pink; non-foliated pegmatite; non-magnetic. Commonly contains both biotite and muscovite. Plag in pegmatite has local green sercite and epidote/clay(?) alteration. Trace py on fractures.

HOLE NO.: GL-10-8

Page 1 of 1

MEGA URANIUM LTD. - SAMPLE RECORDProject: GREENWICH LAKELogged By: S. Kruse & T. GilmanDate: March 21 - March 23, 2010



1 2 2286183 2.00 3.00 1.00 GAB 1 C Exploration 1 F-2 4C comp A10-1323286184 7.00 8.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286185 12.00 13.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286186 17.00 18.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286187 22.00 23.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286188 27.00 28.00 1.00 GAB 1 C Exploration 1 F-2 4C comp A10-1323286189 32.00 33.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286190 33.00 34.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286191 34.00 35.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286192 37.00 38.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286193 42.00 43.00 1.00 GAB 1 C Exploration 1 F-2 4C comp A10-1323286194 47.00 48.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286195 UMT-1 A10-1323 Standard286196 52.00 53.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286197 57.00 58.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286198 62.00 63.00 1.00 GAB 1 C Exploration 1 F-2 4C comp A10-1323286199 67.00 68.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286200 72.00 73.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286201 77.00 78.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286202 82.00 83.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286203 87.00 88.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286204 92.00 93.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286205 97.00 98.00 1.00 GAB 1 C Exploration 1 F-2 4C comp A10-1323286206 102.00 103.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286207 107.00 108.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286208 112.00 113.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286209 123.00 124.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286210 123.00 124.00 1.00 GAB 1 C Exploration 1 F-2 A10-1323 Dup286211 128.00 129.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286212 133.00 134.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286213 138.00 139.00 1.00 GAB 1 C Exploration 1 F-2 4C comp A10-1323286214 143.00 144.00 1.00 GAB 1 C Exploration 1 F-2 comp A10-1323286215 UMT-1 A10-1323 Standard

HOLE NO.: GL-10-8


From (m) To (m) Length (m) Percentage (%) Length (m) Percentage (%)0 2 1.6 160.0% 1.32 132.0%2 5 2.97 99.0% 2.75 91.7%5 8 3 100.0% 2.8 93.3%8 11 3 100.0% 2.39 79.7%11 14 3 100.0% 2.96 2.0%14 17 3 100.0% 2.9 98.7%17 20 2.96 98.7% 2.63 87.7%20 23 2.95 98.3% 2.6 86.7%23 26 2.96 98.7% 2.77 92.3%26 29 2.98 99.3% 2.89 96.3%29 32 2.99 99.7% 2.86 95.3%32 35 3 100.0% 2.74 91.3%35 38 2.98 99.3% 2.67 89.0%38 41 3 100.0% 2.86 95.3%41 44 2.99 99.7% 2.83 94.3%44 47 2.91 97.0% 2.69 89.7%47 50 3 100.0% 2.9 96.7%50 53 2.95 98.3% 2.8 93.3%53 56 2.9 96.7% 2.7 90.0%56 59 3 100.0% 2.83 94.3%59 62 2.97 99.0% 2.97 99.0%62 65 2.98 99.3% 2.98 99.3%65 68 3 100.0% 2.86 95.3%68 71 3 100.0% 3 100.0%71 74 2.96 98.7% 2.77 92.3%74 77 2.97 99.0% 2.81 93.7%77 80 2.99 99.7% 2.85 95.0%80 83 2.93 97.7% 2.67 89.0%83 86 2.94 98.0% 2.34 78.0%86 89 2.93 97.7% 2.42 80.7%89 92 3 100.0% 2.92 97.3%92 95 2.96 98.7% 2.89 96.3%95 98 2.92 97.3% 2.76 92.0%98 101 3 100.0% 2.87 95.7%101 104 2.91 97.0% 2.76 92.0%104 107 2.98 99.3% 2.91 97.0%107 110 3 100.0% 2.93 97.7%110 113 3 100.0% 2.94 98.0%113 116 3 100.0% 2.68 89.3%116 119 3 100.0% 2.94 98.0%

HOLE NO.: GL-10-8




HOLE NO.: GL-10-8


119 122 3 100.0% 2.91 97.0%122 125 2.94 98.0% 2.91 97.0%125 128 3 100.0% 2.91 97.0%128 131 3 100.0% 2.83 94.3%131 134 2.94 98.0% 2.48 82.7%134 137 3 100.0% 2.85 95.0%137 140 3 100.0% 2.92 97.3%140 143 3 100.0% 3 100.0%143 146 3 100.0% 2.95 98.3%146 149 2.92 97.3% 2.92 97.3%149 152 2.98 99.3% 2.77 92.3%152 155 2.97 99.0% 2.28 76.0%155 158 2.94 98.0% 2.81 93.7%158 161 2.83 94.3% 2.13 71.0%161 164 3 100.0% 2.64 88.0%164 167 2.97 99.0% 2.73 91.0%167 170 3 100.0% 2.4 80.0%170 173 2.9 96.7% 2.31 77.0%173 176 3 100.0% 2.76 92.0%176 179 2.97 99.0% 2.43 81.0%179 182 3 100.0% 2.84 94.7%182 185 2.92 97.3% 2.83 94.3%185 188 3 100.0% 3 100.0%188 191 2.97 99.0% 2.87 95.7%191 194 3 100.0% 2.93 97.7%194 197 2.95 98.3% 2.89 96.3%197 200 3 100.0% 2.81 93.7%200 203 3 100.0% 2.45 81.7%203 206 2.97 99.0% 2.48 82.7%206 209 3 100.0% 2.75 91.7%EOH EOH EOH EOH EOH EOH



6 38.52

8 30.11

10 39.46

12 36.37

14 34.74

16 45.56

18 31.98

20 29.77

22 18.4

24 19.02

26 27.4

28 35.6

30 9.635

32 31.53

34 0.935

36 26.28

38 28.88

40 18.89

42 17.9

44 14.58

46 18.08

48 20.25

50 23.45

52 20.08

54 25.31

56 34.47

58 30.1

60 18.5

62 24.13

64 17.92

66 15.29

68 35.31

70 29.89

72 29.44

74 17.6

76 33.03

78 17.18

80 14.71

HOLE NO.: GL-10-8



HOLE NO.: GL-10-8

82 35.15

84 20.03

86 18.64

88 43.89

90 28.04

92 38.96

94 42.68

96 34

98 40.12

100 39.69

102 42.89

104 56.95

106 39.93

108 35.17

110 14.69

112 6.113

114 35.54

116 37.45

118 21.98

120 13.16

122 35.35

124 20.42

126 5.086

128 17.87

130 21.19

132 16.93

134 22.94

136 16.98

138 16.85

140 19.59

142 22.39

144 7.99

146 14.59

148 0.02

150 0.003

152 0.006

154 0.003

156 0.009

158 0.005

160 0.044



HOLE NO.: GL-10-8

162 0.024

164 0.044

166 0.019

168 0.033

170 0.026

172 0.068

174 0.043

176 0.002

178 0.046

180 0.091

182 0.217

184 0.047

186 0.015

188 0.051

190 0.004

192 0.01

194 0.029

196 0.044

198 0.024

200 0.004

202 0.023

204 0.047

206 0.058

208 0.167

EOH EOH

EASTING: 0362153

NORTHING: 5406622

ELEVATION: 472 m

AZIMUTH: 315

DIP: -50

E.O.H: 209 m



GL-10-8

135315

0.0

50.0

100.0

150.0

200.0

5 to 75Pt

5 to 42Pd

2 to 15Au

0 to 64

Magnetic Susc.

GL-10-8

GL-10-7

GL-10-6

GL-10-5

GL-10-4

GL-10-3

GL-10-2

GL-10-1

361000

361000

362000

362000

363000

363000

364000

364000

365000

365000

366000

366000

367000

367000

5402

000

5402

000

5404

000

5404

000

5406

000

5406

000

5408

000

5408

000

5410

000

5410

000

±

0 1 20.5Kilometers

1:20,000

Legend

Final_GL-10_DDH_Collars

FINAL_DDH_Trace_GL-2010

Greenwich Lake Access Roads

Greenwich Lake Property Claims

Lakes and Ponds

Map 3: 2010 Diamond Drill Program - Drill Hole Locations , NAD 83, UTM Zone 16

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# # #

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###

99038

9903999035

LSE8

LSE7

LSE6

LSE5

LSE5

LSE4

LSE3

LSE2

LSE1

Tr9ETr9C

Tr9W

Tr8ETr8C

Tr8W

Tr7ETr7C

Tr7W

Tr6E

Tr6C

Tr6W

Tr5E

Tr5C

Tr5W

Tr4E

Tr4C

Tr4W

Tr3E

Tr3C

Tr3W

Tr2ETr2CTr2W

Tr1E

Tr1C

Tr1WTr35ETr35C

Tr35WTr34C

Tr34S

Tr33E

Tr33C

Tr33W

Tr32E

Tr32CTr32W

Tr31W

Tr31C

Tr31E

Tr30WTr30E

Tr29W

Tr29CTr29E

Tr28N

Tr28S

Tr27ETr27C

Tr27W

Tr26E

Tr26C

Tr26W

Tr25E

Tr25C

Tr25W

Tr24C

Tr23C

Tr22ETr22CTr22W

Tr21ETr21C

Tr21W

Tr20E

Tr20CTr20W

Tr19ETr19CTr19W

Tr18E

Tr18CTr17E

Tr17C

Tr17WTr16E

Tr16CTr16W

Tr15E

Tr15C

Tr15W

Tr14ETr14CTr14W

Tr13E

Tr13C

Tr13W

Tr12ETr12C

Tr12W

Tr11ETr11C

Tr11W

Tr10ETr10C

Tr10W

Tr28C

99052

99050

99049

99047

99046

9904599044

99043

99036

99034

99032

99031

99030

99028

99026

99051

99048

99042

99041

99040

99037

99033

99029

99027

361000

361000

362000

362000

363000

363000

364000

364000

365000

365000

366000

366000

367000

367000

5402

000

5402

000

5404

000

5404

000

5406

000

5406

000

5408

000

5408

000

5410

000

5410

000

±

0 1 20.5Kilometers

1:20,000

Legend

# Waypoints Visited

Cu_Above_200_ppm

Ni_Above_200_ppm

Pt_Pd_Au_Above_30_ppb

2009 Boulder Samples

2009 Outcrop Samples

Greenwich Lake Access Roads

Greenwich Lake Property Claims

Lakes and Ponds

2009 AeroTEM Magnetic SurveyRGB

Red: Band_1

Green: Band_2

Blue: Band_3

Map 2: 2009 Prospecting Program - Sample Locations and Results, NAD 83, UTM Zone 16

Mag High

Mag Low

4244234

4211692

4244233

4244231

4244232

4244236

4211690

4211693

3014754

4211691

3014745

4244235

42116944207834

4244237

4211695

360000

360000

361000

361000

362000

362000

363000

363000

364000

364000

365000

365000

366000

366000

5402

000

5402

000

5404

000

5404

000

5406

000

5406

000

5408

000

5408

000

5410

000

5410

000

0 1 20.5Kilometers

1:20,000

LegendGreenwich Lake Property Claims

Contour

Streams and Rivers

Lakes and Ponds

Map 1: Claims Comprising the Greenwich Lake Property, NAD 83, UTM Zone 16

report on exploration by mega uranium ltd. on the ... · greenwich lake 4244236 2008-nov-28...

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