diamond drilling rpt

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2-45944

DIAMOND DRILL EXPLORATION PROGRAM 2010

DIAMOND DRILL LOGS NICOL GOLD PROPERTY NORTHSTAR GOLD CORP

NICOL TOWNSHIP - LARDER LAKE MINING DIVISION NTS 41 PINE (41P/10)

A. P. DAVID GAMBLE P.GEO AUGUST 14, 2010

AUG 2 e 'l0'\0

GEOSCIENCE ASSESSMENT OFFICE

• INTRODUCTION LOCATION AND ACCESS MINING CLAIM STATUS PROPERTY GEOLOGY

TABLE OF CONTENTS

DIAMOND DRILL 2010 PROGRAM SAMPLE METHOD AND APPROACH GEOLOGICAL RESULTS FROM 2010 DRILL PROGRAM GEOCHEMICAL RESULTS FROM 2010 DRILL PROGRAM INTERPRETATIONS AND CONCLUSIONS RECOMMENDATIONS AUTHORS CERTIFICATE

LIST OF FIGURES Fig 1 Property Location and Claim Location Maps Fig 2 Property Geology Plan Map Fig 3 Detail Geology Plan Map Showing DDH Locations Fig 4 Location Plan Map Showing DDH Traces Relative To

Claim Boundary 1 :4000 Table 1 Mining Claims List Nicol Gold Property Table 2 Nicol Gold 2010 DDH Collar Location Compilation

Page No 3 3 4 5 6 7 9

11 12 12 13

after page 3 after page 5 after page 6

after page 8 page 4

after page 6

• Plan Map Showing Location of Diamond Drill Hole Traces With Geology Projected Vertically To Surface, scale 1 :4000 with

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Geology Legend Codes Sheet after page 10

Three West-East Vertical Diamond Drill Hole Projection Cross Sections With Accompanying Plan Drill Hole Trace on Line 5274750 mN, Line 5274950mN, and Line 5275050mN (looking East with 50 meter Far/Near Clipping) scale 1 :4000 With Geology Legend Codes Sheet after page 10

APPENDIX SECTION 1 after Page 13 DETAILED DIAMOND DRILL HOLE LOGS N10-01 THROUGH TO N10-07 APPENDIX SECTION 2 DRILL HOLE ORIENTATION SURVEY DATA TABLE APPENDIX SECTION 3 DRILL HOLE SUMMARY GEOLOGY TABLE APPENDIX SECTION 4 DRILL HOLE SUMMARY ASSAY TABLE APPENDIX SECTION 5 ASSAY CERTIFICATES

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INTRODUCTION

Northstar Gold Corp conducted a diamond drill exploration program from April 22 to May 04,2010 on mining claims held in Nicol Township, District of Timiskaming, Larder Lake Mining Division, NTS 41 PINE. The work was conducted on Northstar Gold Corp mining claims with the project identification as the Nicol Gold Property. This project was conducted under the direction, project management, and field supervision by Mr. George Pollock, President of Northstar Gold Corp., 17 Wellington St North, New Liskeard, Ontario, POJ 1PO. Mr. Dave Gamble, P.Geo, of Dave Gamble Geoservices Inc., was contracted to log the diamond drill holes, produce plans and drill sections of the drill holes, and to report on for purpose of this assessment report.

LOCATION AND ACCESS

The Nicol Gold Property centered at Bilsky Lake is located approximately 5.5 km east-southeast of Gowganda, Ontario, and approximately 30 kilometers southwest of Elk Lake, Ontario, see Figure 1 Nicol Gold Property Location Map.

The Nicol Gold Property centered at Bilsky Lake is approximately at 47 degrees 38 minutes North, by 80 degrees 42 minutes West; and by UTM coordinates (NAD 83, Zone 17N) of 522 500 m East, 5 275 000 m North; NTS map sheet 41P/10.

Access to the property is gained via Highway 560 West, traveling west of Elk Lake and continuing west towards Gowganda into Nicol Township. There is a lumber access bush roads that leads southerly onto the Nicol Gold Property from Highway 560 east of Gowganda and south of Miller Lake. Several bush logging roads and ATV trails provide additional access on the property.

The topography of the property consists of low to locally moderate relief with elevations ranging from 350 to 425 meters above sea level. There are prominent gullies and steep rising terrain bordering the small lake and drainage creeks. There are several small lakes on the property known as Jacobs Lake, Bilsky Lake, Bonsall Lake, and Wilson Lake Most of the property is wooded with abundant bedrock exposures .

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• • LEGEND - Land Tenure Freehold Potent Lilenle of O((up.!lon

.-. luri.," & Mining Righi' U,e, Nol Ipecilied 1- -- ---I

~_~~/_~ Mining Claim

- lu,I". Righi, Only Iud", & Mining Righi,

-:- Mining Righi, Only ... lu,foee Righi, Only

1-- ---I

~_ ~z...:~'_! roled Only Mining (iaim

LCOId Te .... Withdrawal. leasehold Pa!.n! Mining Righi' Only Areas Withdrown from Disposition

l.nd Use Per mil ~ lu,I".& Mining Righh

,. luri". Righi' Only Soll~ e 01 Inlormation ~ Order in (ouncil (No! open for sloking)

__ Mining Righl,Only .' . Woler Power Leose Agreflment

50u{{es offaull Information

Omo/io Divisioo of Mirlf1S; Geologiral {ompilo/ion 5erie5 Map 2205 Timmjn5-Kirkloncl LDke Map 2361 Sudbury· Cobalt

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Location Map

Nicol Gold Property Northstar Gold Corp. 17 W.llinglon II., N.· P.O. Box 2529 Hew U,k""d, 1),1 r'o POl I PO Tel (7051647·88]3 · 17051676·6476

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MINING CLAIM STATUS

Northstar Gold Corp property consists of seven (7) mining claims with a total of sixty-seven (67) units that all lie within central Nicol Township, see Figure 1, Nicol Gold Property Location Map showing Claim Location Map Nicol Gold Property, Northstar Gold Corp. This map shows the numbered mining claim blocks, the UTM grid system, and the bush access onto the property.

Also see below the accompanying Table 1: Mining Claims List Nicol Gold Property, that list the recorded mining claims with corresponding units, and recording dates held by Northstar Gold Corp.

Table 1: Mining Claims Nicol Gold Property

Claim Units Lot/Con Description Record Date Number L 4220241 16 Unsubdivided Township June 01 2007 L 4213071 16 " " Aug 242007 L 4213073 16 " " Auq 242007 L 4210722 4 " " Aug 242007 L 4210659 4 " " Sept 172007 L 4210660 3 " " Sept 172007 L 4221735 8 " " Nov 01 2007

TOTALS 53

Also see Fig 4, Plan Map Showing Drill Hole Traces in Relation to Claim Boundaries, Nicol Gold Project, at a scale of 1 :4000 .

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PROPERTY GEOLOGY

The Nicol Gold Property is located in the Abitibi Greenstone Belt (AGB) as part of the Archean volcano sedimentary assemblage of rocks within the Abitibi Subprovince of the Superior Province. The Nicol Gold Property lies in central Nicol see Geology Map 2, as described by Mcllwaine, W. H. 1978: (Geology of the Gowganda Lake - Miller Lake Silver Area, District of Timiskaming; Ontario Geological Survey Report 175, 161 p. accompanied by Maps 2348 and 2349, scale 1:31 680 or 1 inch to Yz mile). The Nicol Gold Property covers an inlier of early Precambrian mafic metavolcanics and metasediments with associated lean iron formation that has been intruded by the Wilson Lake granitic trondhjemite to syenodiorite pluton. Middle Precambrian Proterozoic cover rocks unconformily overlie and flank the inlier and consist of the Cobalt Group sedimentary rocks of the Lorrain Formation polymictic conglomerate, and by late gabbroic intrusive rocks of the Nipissing diabase sills and by the later intrusions of the Matachewan diabase dikes. Two fault structures transect the property; the northeasterly striking Wilson Creek fault segment, and the prominent northwest striking Jacobs Lake fault. Several small gold and copper showings and minor sulphidized magnetite lean iron formation are reported to occur on the property.

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• • LEGEND

PRECAMBRIAN"

LATE PRECAMBRIAN MAFIC INTRUSIVE RQCKSc

DIABASE DIKES

"it OIi~In(> f1Ii!Mse . 110 POff)flYfit,C ol ivine diabase.

10 Diltbase.

NIPISSING DIABASE

9 Unsubdlv lllea. ~ Pylo6ene pabbro. 90 Ampll;!xJllJ p/lobro. Sk Granopflrrf' . 9d Aplite.

INTRUSIVE CONTACT

• FEI....51C INTRUSIVE ROCKS'::

4 Unsuhdi~ ,ded . .ta TrondhJemite. 4b Porphyritic trondhjemite. ok Quarl1 diorite 4d $,enodiorite. 40 Con/llminated l onE' 4/ Pe-Dm./,tc. 4g Fe/dSP<81 IXJIpn'l' '1 .

!NTRUS I'IE C ONT"CT

METAMORPHOSED MAFIC AND ULTRAMAFIC INTRUSIVE

ROCKSc

3a GIID%. Jb S~Iptnlwiled auni((>.

METAVOLCANICS

FELSIC METAVOLCANIC ROCKS'::

1 Unsubdl,>, rdCd. 2. Dacite, f)OfpnYf ilic dlKile. 2b Felsic l u "

HURONIAN SUPERGROUP

COBALT GROUpO l i-- J lIon f ormation .

LORRAIN FORMA liON

8 Un Subdlvldea. S. Mic« eous Sffld s/omJ. 8b Feld sptl/h ic s.tnI15/0n", Be Grey NK /(e. 8d QU4r/IOS(' ~ndslone . plC /O ·

q/Jartt i te. Be F'trruaifl(Jus sands/one 8/ Or /" ocong1o.!neflJ/(>.

GOWGANDA FORMA TION Firslbrook Member

U 1 Ltlminalooa/Q,l!i/e

( olemen Momber

II:] 6 UnsutJ(j,vldcd. 6a Feld~lfl lc g(ey 'li «lce. 6b Fe /(jspIJ lfll(; uncJllofIC .lJ l ko~. 6c C'JIlglomerate. 6d Fef/ uginous $lJMis/OII(J. 6& Rr«citt. 61 AJgdillc ,S"/ slofl(! 6r; Proipqu ltrl lil f.' .

UNCQNI"OI'lMITY

EARLY PRECAMBRIAN (ARCHEAN)

MAFIC INTRUSIVE ROCKSC

DIABASE OOoliES (MATACHEWAN TYPE)

SIt D,.lJiISC . 5b f'oIPhyritie OilJbase

MAFIC TO \NTER.MEOIATE MET AVOLCANIC$C

IU I Unsu txJIYkioo. Ilf &s.iI. anci(>sile r b Ampflibo/i lC. Ie foil illed IItn(J n lbo/lle. 111 Gabbroic f1ows. Ie Am'lfJdaloidtll blJsall. Is;I Pillowed I., .... Ih Pyroclastic l OCI!S . 1; Porphyritic IIIfloosite. II< Schistose rocks. 1m MoIHwimen(/lry fOC~ ! .

·UneonS)ii(Ja!()(j deposils. Cenal oic defj05I ls IN replesen /f!d by the /is;lhfer coIotJrcd par i s oflhe map.

b6edroc~ QroIog'y. Oulcrops and In/erred el l ensions 01 Heh 'IXI< map·unit /l rc shown fc sDCCt ivcly in dre lind l ighl fon~s 0/ the s.m(' colOoJI . Wli lit/:' in p loces formalion Is too nll"(Jw 10 S~ c.oIaur 1Ir,d must represen~ in bllICl< . II shorl biltC A tA r appeiJ/S 1'1 I appropti,/() bfocA.

CRocA typeS in these r,jIOUpS dIe sulxli r ided /i lholog iCiJ""! ttIld tile ord/!1 does not Im ply .~ (f!I;,{lons.fo ; .... ith in the s;lfOUpS.

""",,01_: On."' Miil1Iyri Noilflem~"andMi"" il'JIpl349, lfmimJorI Ntoi lownsfOps,pliJ.1916

o Au Sampl. o Cu Sample

Drill Hoi. 1 Hole Number

It!' Dril~ng Direction

___ ~ __ -J ______ ~~~ __ ~ _______________ 1 Km

Nicol Gold Property Northstar Gold Corp, 11Wel~nglonSI.H.,.P.O. 8ox2529 MnLiskeord,Onlorio POJ1PO 1.: 17051676-6476'17011647·8833

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DIAMOND DRILL 2010 PROGRAM

Northstar Gold Corp completed a diamond drill exploration program in 2010 on the Nicol Gold Property mining claims held in Nicol Township, District of Timiskaming, Larder Lake Mining Division, NTS 41 P/1 O. The objectives of this diamond drill program were to explore the areas where airborne VTEM electromagnetic and magnetic geophysical targets were identified.

A total of 7 diamond drill holes totaling 1,139 meters (3,736.9 feet) of NQ core drilling were completed during the period from April 22, 2010 through to May 04, 2010 utilizing the contract diamond drill company Laframboise Drilling Inc., see Fig 3 Detail Geology Plan Map Showing Drill Hole Locations, and see Table 2 for Nicol Gold 2010 DOH Collar Location Compilation.

The drill program was conducted under the direction and field supervision by Mr. George Pollock, President of Northstar Gold Corp., New Liskeard, Ontario. All target selections, location of drill hole set ups, drill road access routes, monitoring of the diamond drill progress and drill contract supervision, and determination of final depth of holes, were all determined solely by Northstar Gold Corp personnel, Mr. George Pollock.

Mr. Dave Gamble, P.Geo, of Dave Gamble Geoservices Inc., was contracted to provide geological consultation and log the diamond drill holes, produce plans and drill sections of the drill holes, and to report on for purpose of this assessment report.

All diamond drill core when logged and sampled from this drill program have been palletized, covered and secured by steel strapping, moved and stored on a secure farm site of one of the directors of Northstar Gold Corp in New Liskeard, Ontario .

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• • SVPOO

SVS6'.\)

SV~OO

SVSJOO

SVS100

S11SIOOM

SV4900 III 0 C

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t SV4100 -<

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LEGEND

PRECAMBRIANb

LATE PRECAMBRIAN

MAFIC INTRUSIVE ROCKSc

I lot Oliv ine dllJ~S(!.

lID Porpfl'lfl/'c ol,v l/'W! d laDiJSl.'.

10 DiIlNSI?

tI UnsutJOividN. g" Py'o.~r;t! gllbt)fo . 9b AmphIbole gabbrf). 9c Gr/loopllyre. 9d At>/ite.

• FEl.SIC INTRUSIVE ROCKSI:'

4 Unsurxlr'flded. 4, T'OIIdflJem,(e. 40 PorphyritiC trondhjemile . 4C OUllrIL(:/Iofile. 4<J S/enoOIOIde. 4e Conl.mln(J(OO Lon/! 4/ P~1I141'lc. 4g fC!Id~~f POIptlyry.

METAMORPHOSED MAFIC AND ULT~"'MA"'JC INTRUSIVE

I:tOCKSc

3(1 Gllbblo. Jb SIJ(~nllnuea rJunif ...

METAVOLCANICS

f£L.81C MET AVOLCANIC ROCKS(:

2 Unluba .... ItfCO. 2. D«ltt, DOIPfly,;l ic dacile. 20 r~SIC /u".

r ~ J Iron f OlfMIIOfl .

lORRA\N FORMA nON

~ Unsu/XIJllldea. IoAA.FlC TO IHURMEOIA.1E

METAVOLCANICSC &J Mic/lCC'OU$ SdndSfo ne. 8b hldspil/h ic SIlndsfone, 8c Greyw.teol:e. lJd eu"rlzose sanQstone, proto·

qu.trtzi(e . U I Unsub</lviaeo.

'01 Baull . lJfldes l/e . / tJ Am" nitJoJilc .

Be FerruoifJO(J s SIJIldslOf1~ 8( OrlnOCfJng lotTwf.'e .

GOWGANDA FORMATION Firstbrook Member

Coleman Member

IU 6" Un SUiJlii'oded. 61 Feld~lfl lC ()f .tw«" • . 60 hldspal h lc SdndstOnc . • '_O$f'. (iC Conglomerate 6d Feuuginou!; SlIndst~. 6e B'Ke;'. 6/ ArfJ, lhle, $,II~lof)fJ. 6" PU:lloqu6f1Lite .

UNCONFORMITY

EARLY PRECAMBRIAN (ARCHEAN)

MAFIC INTAUSIVE ROCKSc

DIABASE DIKES (MATACHEWAN TYPE)

!,t DI/JDa~. ! b P()I'phyri llC (M b.t-Se.

Ie F'3II(I/e<l amalt/boMc. .a G(lbbfOiC flow s. Ie AmyacJIJIoid41 baS/Jl/. '0 Piltowed ''''II. Ih PyIQCJasl.ic f ocA$. Ii P'otl)hy,itic . ntnsitc. 14 Scfl .slo!W locks. 1m MBla~'menI4/y roells.

' Unconsolida/cc d<>POSlls. CenororC (J~/s ar teDlesen /ed by the haMet colourrd pal l s of Ihe nvp.

bBedr«~ OtOlOgy. Ou/COIOp S M d in ffm ed e.densjons of eM/) rOCII m lJp·ufll/4rC! shown resp«t ively in der and NoM/ones 0/ the .wn\f' co/our. Where ;.""1 pl«es /OIm. ' lon is roo na'(uw 10 show colour . fJd m uSI It"(jleSl!n/e(j in 61« k. (I shOl l bl«k boIr ~(5 In I IJp/lIOPfillc block.

C:Rock 1'11»$ ;n /flese QfOUPS IJre su /xJlvKJed /il holog ica lly 4f1d lite OI(kr ~s not i mP/r M)e '~lJfJonsJti wltllln lhe groups.

SaN<8Solnloooo,,",: OnronoMitlstryoiNotmem08'1f1JOfKTIeIIlandMinas Iiop7319, _IIJdHmTo"""",,, prm,I916

o Au Sompl. o Cu Somple

Drill H.~ 1 Hole Number

,.('OrllingOiredion

Geology Map 2

I Km

Nicol Gold Property Northstar Gold Corp, 17 W.llinglon SI. H.,. P.O. Bax2S19 New lisIteord. Ol1lllrlo pt)J lPO T.I: [70SI 676-i>476'170SI M7,8833

• • • Nic Collar Location Compil 2010

TABLE 2 NICOL PROPERTY 2010 DDH COLLAR LOCATION COMPILATION UTM NAD 83 Zone 17

Hole No Grid E Grid N Elev Az Dip Depth (m) UTM E UTM N Start Finish Size D. Driller Claim # N10-01 N/A N/A 335 232.0 -62.0 278.0 523281 5274788 Apr-22 Apr-25 NO Laframboise L 4210722 N10-02 N/A N/A 380 270.0 -38.0 71.0 522992 5275042 Apr-25 Apr-26 NO Laframboise L 4213073 N10-03 N/A N/A 380 270.0 -45.0 326.0 522992 5275042 Apr-26 Apr-30 NO Laframboise L 4213073 N10-04 N/A N/A 380 235.0 -45.0 140.0 522992 5275042 Apr-30 May-02 NO Laframboise L 4213073 N10-05 N/A N/A 377 225.0 -38.0 50.0 522958 5275054 May-02 May-02 NO Laframboise L 4213073 N10-06 N/A N/A 387 238.0 -50.0 104.0 523056 5274989 May-02 May-03 NO Laframboise L 4213073 N10-07 N/A N/A 355 235.0 -70.0 170.0 523312 5274741 May-03 May-04 NO Laframboise L 4210722

Total 1,139.0

Nic Collar Location Compil 2010

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SAMPLE METHOD AND APPROACH The following procedures were followed for the handling and sampling of all drill core from the Nicol Gold property drilling program for Northstar Gold Corp.

During the exploration diamond drill program all drill core was delivered twice daily by the drilling crews to Laframboise Drilling Inc. secure core logging facility. Once in the logging facility the following procedures were carried out.

All necessary logging equipment, supplies, core racks and core saw were supplied by Dave Gamble Geoservices Inc. 1) All box numbers were verified, the core was measured and meterages and meterage blocks between drill runs were verified, and each core tray was labeled with aluminum tags prior to detail logging, quick summary drill logs were noted when received into the logging facility on a daily basis, and then all core trays were placed in core racks awaiting detailed logging. Four core racks were utilized as active temporary storage racks inside the locked and secure core logging facility. The capacity of the four active core racks was 560 core trays for approximately 2350 meters of core. 2) Careful orientation of drill core and continuous detailed logging including magnetic susceptibility checks on the drill core was conducted on a routine basis. The alignment of the core on a continuous basis in the core boxes was carried out to preserve the measurable fabric and contacts after halving by diamond saw cutting. All geological information, meterage markings, contacts and angle to core axis measurements, etc have been marked with a yellow grease pencil. 3) Delineated and inscribed an actual cut line with red grease pencil for sampling purposes. 4) Establish carefully measured intervals for sampling and mark them directly on the core. 5) Numbered sample tickets with sampled intervals are small poly bagged and are then stapled at the beginning of each sample interval, and recorded on a master sample data sheet. 6) Corresponding sample tear off ticket is placed in poly sample bags. All poly sample bags are new and are also numbered by felt pen with number from the ticket, to assure ticket, bag, and interval are the same for each appropriate sample. 7) The third tear off sample ticket is preserved in the sample ticket book. 8) Sample intervals are carefully cut by a Vancon diamond core saw. One half of the core is preserved in the core box as a permanent archived record, and the corresponding other half core for each respective sample interval is placed in the appropriate numbered sample bag. The poly sample bag is immediately sealed with staples after each cut interval is completed. 9) All sample intervals, in their individual sample bags, are then placed in large farine bags and sealed with poly security cable tie. Each farine bag is labeled with the sample series contents on the outside of the bag with permanent felt marker ink

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10) All drill core and all cut and bagged samples are kept in a locked and secured logging and splitting facility until time of shipping directly to the lab. 11) All sample batches were directly delivered to Swastika Laboratories Ltd, a commercial assaying laboratory for gold and silver assaying. The samples were personally delivered by A. P. David Gamble, P.Geo, consulting geologist for Northstar Gold Corp, All batches of samples are transported by pick up truck and delivered to Swastika Laboratories Ltd in Swastika, Ontario with accompanying sample shipment notice documentation. All samples are received by Swastika Laboratories Ltd personnel and immediately placed within their facility. At no time are samples left unattended outside. 13) All Swastika Laboratories Ltd assay reports and certificates are reported directly to Northstar Gold Corp and copies of all assay reports and certificates are also sent to A. P. David Gamble, P. Geo. consulting geologist. 14) All sample sample pulps for all assayed samples are presently stored with Swastika Laboratories and to be transferred to Northstar Gold Corp at a later date .

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N10-o3I-r ____ .,~N~1~~~~e5~,J- N10-04 N10-o,~V N10-03

$)~ N10-02 .,..~~ 5275000 N

1:4000 o 25 50 75 100 125 150 175

I I I ! ! ! I I

DAVE GAMBLE GEOSERVICES INC NORTHSTAR GOLD CORP.

NICOL GOLD PROJECT 2010 DIAMOND DRILL EXPLORATION PROGRAM, NICOL TOWNSHIP, ONTARIO

PLAN MAP SHOWING LOCATION OF DIAMOND DRILL HOLE

TRACES FIGURE 4

SCALE: 1: 4000 I DATE: AUG 14, 2010 I DAVE GAMBLE P.GEO.

w o o o M N ."

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GEOLOGICAL RESULTS FROM 2010 DRILL PROGRAM

Nicol Gold Project exploration diamond drill program results include the Detailed Diamond Drill Hole Logs N10-01 through to N10-07 see Appendix Section 1 for all detailed drill hole log sheets, and the following Excel dataset spreadsheets Nicol Drill Hole Collars Location Compilation Table see Table 2 in text, Nicol Drill Hole Orientation Survey Data Table see Appendix Section 2 (all holes surveyed by Reflex Easy Shot instrument), Nicol Drill Hole Summary Geology Table see Appendix Section 3, and Nicol Drill Hole Summary Gold Silver Assay Table see Appendix Section 4. All four Nicol data Excel datasets were downloaded into the 3D Datamine and Downhole Explorer software to produce a 3D viewing and to produce the 1 :4000 scale Plan Map and Vertical Cross Sections for this report.

The Drill Hole Plan Map 1 :4000 scale shows the location of the diamond drill hole traces with the coded/color geology projected vertically to surface.

A series of three 1 :4000 scale West - East Vertical DOH Projection Cross Sections were cut for UTM section lines along Lines 5274750 rnN, Line 5274950mN, and Line 5275050 mN that show all the diamond drill holes with coded/color geology, and with the accompanying plan map drill hole surface traces plan, (all sections are all viewed looking east with a 50 meter far and near clipping) .

A plan map was also produced showing the vertically projected to surface traces of all 2010 diamond drill holes with end of hole meterages (EOH) in relationship to mining claim boundaries and surface cut grid. See Fig 4, Plan Map Showing Drill Hole Traces in Relation to Claim Boundaries, Nicol Gold Project, at a scale of 1:4000.

The drill program has revealed that the property in the areas drilled are underlain by a sequence of Archean basalt flows and tuffs with minor intercalated siliceous quartzite horizons that are generally barren of sulphide mineralization. There are however several siliceous quartzite horizons that are mixed with magnetite lean iron formation that has been partially sulphidized to pyrrhotite, pyrite, and rninor chalcopyrite and sphalerite. These narrow intervals were intersected and clearly identified in the drill logs and seen in drill holes N10-01, N10-05, N10-06, N10-07, and weakly seen in N10-03. Some minor feldspar porphyry and aplite dikes also locally cut the sequence. Late diabase dikes probably from the Matachewan swarm also intrude the sequence. The mafic volcanic basalt flows and tuffs exhibit a low amphibolitic metamorphic grade with the development of fine-grained prismatic to acicular needles and crystals of hornblende amphiboles. This amphibolitic metam,orphic grade is most likely a result of a contact metamorphic effect flanking the Wilson Lake granitic pluton as a contact aureole.

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Two holes N10-01 and N10-07 also exhibit Proterozoic cover rocks at the start of each hole as coarse polymictic conglomerate that vary from a hematized oxidized sequence to an unoxidized lower part sequence that probably represents changing conditions from oxidizing to reducing conditions in a sedimentary basin regime. The conglomerate appears to be a sequence of the Lorraine Formation of the Cobalt Sedimentary Group with a contact that overlies the Archean basement with an angular unconformity. Also in these two hole there is a sequence of komatiitic ultramafic basalt flows that are moderately to strongly magnetic and exhibit finely disseminated magnetite. Faulting with narrow well developed muddy fault gouge were also noted in several drill holes generally lack significant alteration .

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PROGRAM NICOL TOWNSHIP ONTARIO

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GEOLOGY/LITHOLOGY CODE OVERBURDEN OVB FAULT ZONE FAZ

INTRUSIVE ROCKS DIABASE DIKE DBDK FELDSPAR PORPHYRY DIKE FPDK APLITE DIKE APDK

PROTEROZOIC SEDIMENTARY ROCKS PROTEROZOIC CONGLOMERATE PCGL

ARCHEAN SEDIMENTARY AND VOLCANIC ROCKS BANDED LEAN IRON FORMATION SULPHIDIZED BIFS QUARTZITE QZT BASALT TUFF BT BASALT FLOW BF KOMA TIITE BASALT FLOW KBF

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1 :4000 o 25 50 75 100 125 150 175 I ! ! I ! ! ! I

NICOL GOLD PROPERTY 2010 DIAMOND DRILL PROGRAM, NICOL TOWNSHIP, ONTARIO

WEST· EAST VERTICAL DIAMOND DRILL HOLE PROJECTION CROSS SECTION WITH ACCOMPANYING DRILL HOLE TRACE ON LINE 5274750 mN (Looking North with 50 meter

far near clipping)

SCALE 1 :4000 DATE: August 14, 2010

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NORTHSTAR GOLD CORP


WEST - EAST VERTICAL DIAMOND DRILL HOLE PROJECTION CROSS SECTION WITH ACCOMPANYING DRILL HOLE TRACE ON LINE 5274950 mN (Looking North with 60 meter

far near cllpplngl

SCALE 1 :4000 DATE: August 14,2010

• • Rl (.oJ o o o m

• N1 0-03.--.~ ___ _

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NORTHSTAR GOLD CORP


WEST - EAST VERTICAL DIAMOND DRILL HOLE PROJECTION CROSS SECTION WITH ACCOMPANYING DRILL HOLE TRACE ON LINE 5275050 mN (Looking North with 50 meter

far near Clipping)

SCALE 1 :4000 DATE: August 14,2010

•

•

•

GEOCHEMICAL ASSAY RESULTS FROM 2010 DRILL PROGRAM

A total 461 sample intervals were core saw cut and submitted to Swastika Laboratories for gold and silver assaying for Nicol Gold Project exploration diamond drill program by Northstar Gold Corp. Also a total of 17 inserted standards were also submitted for control and for QA/QC purposes. A total of 30 sample pulps were also submitted for 30 multi-element ICP-AES analysis with to date 19 with results and 11 samples with pending results. The total meterage of saw cut core samples submitted for assaying from this program was 361 meters. See Appendix 4 - Drill Hole Summary Assay Table, and Appendix 5 - Assay Certificates from Swastika Laboratories Ltd., for a complete listing of all assay results for Northstar Gold Corp's Nicol Property.

The results of the gold assaying were generally disappointing with generally most samples returning low two digit ppb results for gold, several low three digit ppb results for gold, and one sample # 43404 returning 1340 ppb gold over 0.8 meters in N10-03, and another sample # 43481 returning 4230 ppb gold over 0.4 meters in N10-04. The results for the silver assaying were also generally disappointing with most results returning 0.2 ppm, a low number in the 1.0 to 2.8 ppm value range, and one sample # 43481 returning 13.4 ppm silver over 0.8 meters in N10-03.

The sulphidized lean iron formation returned insignificant gold and silver assays . The multi-element ICP-AES analysis for 19 of the sulphidized lean iron formation samples has returned some anomalous values in copper generally ranging from three digit ppm with one sample # 43255 returning up to 3034 ppm Cu in N 1 0-01, and low three digit ppm zinc with one sample #43609 returning up to 2842 ppm Zn in N10-06, and generally low lead ppm values but with one sample # 43602 returning 5735 ppm Pb, Associated with the pyrrhotite and pyrite high iron and sulphur values were reported. Generally the siliceous sulphidized lean magnetite iron formation returned low base and precious metal values that were generally disappointing .

11

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INTERPRETATIONS AND CONCLUSIONS

The purpose of the drill program was to test airborne VTEM electromagnetic and as well some associated magnetic targets. In the area of the diamond drill holes the lithologies encountered were predominantly a sequence of Archean basalt flows and tuffs with intercalated narrow horizons of generally barren siliceous quartzite metasediments. In drill holes N10-01, N10-05, N10-06, N10-07, and weakly seen in N10-03 there were several siliceous quartzite horizons that are mixed with sulphidized magnetite lean iron formation. These intersections appear to have been partially sulphidized with the presence of pyrrhotite, pyrite, and minor chalcopyrite and sphalerite with remnant magnetite fine layers. These narrow intervals that have been intersected clearly identify the cause of the geophysical VTEM and magnetic targets. The geochemical result from the sampling of the drill holes was disappointing with most samples returning generally low insignificant gold and silver assay values. One sample # 43481 did return elevated values of 4230 ppb gold and 13.4 ppm silver over 0.4 meters in N10-04. The gold and silver assaying and the multi-element ICP-AES analysis for 19 samples of the siliceous quartzite with sulphidized magnetite lean iron formation generally returned low insignificant precious metal values. From these samples generally only weak anomalous base metal values with maximum values up to 3034 ppm copper (parts per million), up to 2842 ppm zinc, and up to 5735 ppm lead values being returned . The results of the gold and silver assaying and the ICP-AES analysis were generally disappointing with the conclusion that the siliceous quartzite with sulphidized magnetite lean iron formation where drilled is barren of significant mineralization.

RECOMMENDATIONS It is recommended that further exploration on the Nicol Gold Property be restricted to further surface prospecting in order to possibly identify any targets for future follow up.

Dave Gamble P. Geo Dave Gamble Geoservices Inc August 14, 2010

12

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CERTIFICATE OF AUTHOR

I hereby certify that I, A. P. David Gamble of 378 Grenfell Road, Kenogami Lake, RR #2, Swastika, Ontario, POK 1 TO, hereby certify that:

1. I am a Consulting Geologist, and reside at the above address.

2. I graduated from University of Ottawa with an Honors Bachelor of Science degree in 1973, and also have completed two years of graduate school courses leading towards a M. Sc. degree (geology) at Laurentian University (1974-1976).

3. I am a member in good standing as a registered geoscientist with the Association of Professional Geoscientists of Ontario, APGO Member No 0618. I am also a member of the Geological Association of Canada I am also a member of the Society of Economic Geologists. I am a director of the Northern Prospectors Association and a member of the Ontario Prospectors Association.

4. I have been practicing my profession in Canada for the past +34 years, and have been responsible for exploration programs carried out in the Abitibi Subprovince for +27 years. In this regard the author acquired knowledge of the geology, mineral deposits, exploration potential and exploration activities in the Abitibi Greenstone Belt of Ontario and Quebec .

5. I am a "Qualified Person" as defined in N143-101, and responsible for all portions of this report not subject to disclaimer.

6. I have carried out the diamond drill core logging and related technical work covered in this Diamond Drill Logs Report for Northstar Gold Corp. on the Nicol Gold Exploration Project, Nicol Township, Larder Lake Mining Division.

7. I hold no personal interest in this property and I have no securities or interest in Northstar Gold Corp. during the exploration program or at the time of this report.

A. P. id Gamble, B. Sc., P. Geo. APGO Member 0618 Dated at Kenogami Lake, Grenfell Twp., This 14th day of August, 2010

13

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APPENDIX SECTION 1

NICOL GOLD PROPERTY DETAILED DIAMOND DRill HOLE lOGS

N10-01 THROUGH TO N10-07

• Hole No Elev

Az Dip UTM E UTM N EOH Size Claim #

•

•

SUMMARY COMPILATION TABLE OF DOH LOCATION 2010 (Legend for Abbreviations Utilized)

Diamond Drill Hole Number Elevation of collar at surface in meters, positive numbers are above sea level, and negative numbers are below sea level Azimuth of diamond drill hole at collar Dip inclination of diamond drill hole at collar Universal Transverse Mercator Grid East in meters Universal Transverse Mercator Grid North in meters End of hole and/or meters drilled Core size NQ Mining Claim Number for Diamond Drill Hole Collar Location

• • • DOH No: N 10- 01 __ Sheet _1_of_ 6_ SignedBY~

I DAVE GAMBLE GEOSERVICES INC RR # 2 Site 2, #29, Swastika, Ontario POK no

NORTHSTAR GOLD DRILL RECORD N10 - 01 Project: Northstar Gold Corp Azimuth: 232.0 degrees Started: April 22, 2010 Logged For: Northstar Gold

Corp Property: Nicol Property Dip: - 62.0 degrees Completed: April 25, 2010 Logged By: Dave Gamble Twp/Claim: Nicoll L 4210722 Location:523281mE/5274787mN Core Size: NQ Drilled By: Laframboise Drilling Hole No: N10 - 01 Elevation: 355 m a.s.1. Total Depth: 278.0 m Purpose of Hole: To drill test airborne VTEM electromagnetic and magnetic targets. Remarks: The hole encountered a flat lying sequence of Proterozoic polymictic conglomerate that overlie with an angular unconformity an Archean vOlcano-sedimentary assemblage. Within the Archean assemblage the hole intersected a weak sulphide (pyrrhotite minor chalcopyrite and sphalerite) lean magnetite iron formation in siliceous quartzite within an intercalated sequence of basalt flows, tuffs and barren siliceous quartzite sediments. Metres From: Metres To: Description

0.0 0.0 Bedrock Setup, no casing required. 0.0 46.0 CONGLOMERATE - PROTEROZOIC COBALT SEDIMENTARY GROUP - LORRAIN FORAMTION - / 55 to 60

From 0.0 - 33.0 m a distinctive reddish maroon polymictic conglomerate with a sandy to gritty matrix with maroon hematite cement and coatings to the gritty grains. The matrix is host to a population of conglomerate fragments that consists primarily of dark grey to green siltstone mudstone, greywacke, arkose, pink granite, granodiorite and granite porphyry intrusive clasts and mafic dark green volcanic flow and fine fragmental tuffaceous clasts. The sedimentary clasts are lenticular and have a 5: 1 to 10: 1 long axis to short axis ratio of the lengths to widths. There are volcanic rounded pebbles to small 5 cm boulders, some green gritty sedimentary clasts, occasional quartz pebble to angular clasts, occasional maroon siltstone pebbles and occasional maroon possible fine grained volcanic pebbles. The clasts, pebbles and boulders make up approximately 60 % of the rock while the maroon sandy to gritty hematite matrix makes up 40 % by volume of the rock. The rock is friable with mostly lengths of core rarely exceeding 10 cm in length. A 8 cm quartz boulder occurs at 27.4 m. The flat orientation of the conglomerate pebbles and clasts appears to be at 70 - 75 degrees TCA that represents a very flat layering fabric of 5 - 10 degrees to horizontal i.e. a shallow dipping sequence to flat lying sequence.

From 33.0 - 46.0 m the conglomerate rapidly changes to a green matrix hosting conglomerate with green sedimentary and volcanic pebbles and boulders as above. There are the occasional reddish pink felsic intrusive pebbles and small 5 -10 cm boulders and is one case a large granitic pinkish red boulder 45 cm in size at 43.9 -44.35 m.

• • • DOH No: N 10-01 __ Sheet_2_of_6_ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Description The colour variation in the matrix most likely represents a transition from oxidizing red hematite shallow marine environment to a reducing deeper that shallow marine environment during deposition, i.e. a oxidation to reducing transition due to variation of water depth. The lower contact represents the Proterozoic to Archean unconformity and the contact is sharp at 35 to 60 degrees TCA with a very shallow 5 degrees to horizontal or 0 degrees dip for the Proterozoic conglomerate unit.

46.0 99.5 ARCHEAN: BASALT TO KOMATIITIC BASALT FLOW SEQUENCE 55/50 From 46.0 - 47.6 m a grey bleached section of basalt flow with a calcite veinlet stringer breccia zone at 46.15 -46.55 m with the stringer fabric at 35 - 45 degrees TCA, and a 1 cm muddy fault gouge seam fault zone ( FAZ) at 46.25 m at 35 degrees TCA. Minor pyrite blebs and weak disseminated pyrite occurs associated with the calcite stringers. From 47.6 - 90.85 m, a komatiitic basalt flow, dark green to green black fine grained massive uniform, serpentinized flow is fractured with calcite healed microfractures, is moderate to strongly magnetic from 46.0-90.0 m (4.0 to 10.0 c.g.s. units on a magnetic susceptibility meter checked on 3 m intervals). This part of the flow sequence appears to be a komatiitic basalt flow. There are light green talc stringers and slips locally and dark green serpentine slips and fracture linings throughout. At 72.5 - 77.0 m there is a calcite lined fracture that parallels the core axis and carries weak disseminated pyrite. From 90.85 - 99.5 m, a pyroxene oikocrystic komatiitic basalt flow with 0.5 - 1.0 cm dark green stubby pyroxene crystals as the oikocrysts (oiks) in a medium green groundmass. This interval does not exhibit evidence of spinifex textures, polysutures, or cumulate olivine or relict serpentinized olivine, and this unit may even represent a possible differentiated ultramafic to ultramafic sill. The upper contact is sharp at 55 degrees TCA, and the lower contact is sharp at 50 degrees TCA.

99.5 101.75 BASAL T TUFF 50 / 40 Medium to dark green fine grained with fine laminations imparting a tuffaceous layering at 40 degrees TCA. The interval carries 1 - 3 % disseminated 1 - 3 mm cubes of pyrite throughout from 99.75 - 101.75 m. Sharp upper and lower contacts at 50 degrees with embayments and sharp at 40 degrees TCA.

101.75 110.0 QUARTZITE 40 /45 Medium to pale grey, fine grained (under hand lens and binocular microscope is micro-granular) and contains grey white 1 - 2 mm quartz grains. The unit is massive uniform and unbedded. The rock is brittle and fractured with local calcite and chlorite healed microfractures and with some chlorite lined slips along some fractures. The quartzite also exhibits a weak brown speckled texture that appears as fine incipient biotite or phlogopite.

• • • DOH No: N 10- 01 __ Sheet _3_of_6 _ Signed By: ______ Date: ___ _

Metres From: Metres To: Descri~tion The interval exhibits weak pin prick disseminated pyrite locally. Sharp upper and lower contacts at 40 and 45 degrees TCA.

110.0 110.5 BASALT TUFF 45 / 45 Medium green, fine grained granular with faint laminations at 45 degrees TCA, andesite intercalated tuff. Sharp upper and lower contacts at 45 degrees TCA. A 1 cm fault gouge at 60 degrees TCA at 110.2 m, minor fault zone (FAZ).

110.5 111.55 QUARTZITE 45 / 25 As previously seen at 101.75 -110.0 m, sharp upper and lower contacts at 45 and 25 degrees TCA.

111.55 111.75 BASALT TUFF 25 / 30 As previous, medium green finely laminated intercalated andesite tuff bed with sharp upper and lower contacts at 25 and 30 degrees TCA. The unit carries 1 - 2 % disseminated pyrite.

111.75 115.8 QUARTZITE WITH SULPHIDIZED LEAN MAGNETITE IRON FORMATION 30/45 The sulphide lean iron formation consists of a bedded layered sequence of quartzite, siltstone, quartzite, reworked andesite tuff, and with fine magnetite rich layers 1 - 3 cm near the lower part of the interval. From 111.75 - 115.8 m the interval exhibits disseminated and semi-massive to massive seams of pyrrhotite with minor pyrite and trace splashes and blebs of chalcopyrite, possibly minor sphalerite, red brown patches of garnet, and several layers of magnetite 1 - 3 cm thick from 115.0 - 115.7 m. At 113.25 - 113.75 m a sulphides poor quartzite layer similar to the unit previously seen. The interval exhibits strong primary bedding at 45 degrees TCA at 113.1 m, 55 degrees TCA at 114.1 m, 65 degrees TCA at 114.4 m and 114. 75m, 70 degrees TCA at 114.85 m and at 115.0 m, 55 degrees TCA at 115.35 m and at 115.7 m. The magnetic susceptibility ranges from 0.4 - 1.5 c.g.s. units in the sulphide rich section from 111.75 - 114.75 m, up to a range of 7.0 - 24.0 c.g.s. units in the section with the thin lean magnetite rich 1 - 3 cm beds from 114.75 - 115.8m. Sharp upper and lower contacts at 30 and 45 degrees TCA.

115.8 172.55 BASAL T FLOW SEQUENCE 45 / 40 From 115.8 - 151.85 m is a dark green fine grained massive uniform basalt flow with an overall appearance that this sequence is hornfelsic with amphiboles that probably indicate the lower amphibolitic metamorphic grade. At 123.1 - 123.95 a rubbly possible flew breccia at 40 degrees TCA. The interval is fractured with calcite healed

• • • DOH No: N 10- 01 __ Sheet _4_of_6 _ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Descr~ion m icrofractu res. At 127.5 - 128.3 m several quartz 1 cm stringers with trace pyrite. At 130.25 - 131.25 m quartz stringers and a quartz - epidote red garnet veinlet with trace to 2 % pyrite. At 131.7 m trace splash of chalcopyrite and weak disseminated pyrite, and at 132.6 m and 136.0 m narrow pyrite threadlike stringers. At 146.1 - 146.65 m and at 151.5 - 151.7 m there are two quartz epidote and garnet veins and stringers with trace to 1 % weak disseminated pyrite. The upper and lower contact is sharp at 45 and 60 degrees TeA for the dark green basalt. From 151.85 -162.7 m another basalt flow, medium green, medium grained crystalline with a green mafic and white feldspathic interlocking texture. Sharp internal contacts at 60 and wavy 35 degrees TeA. From 162.7 - 170.1 another basalt flow, medium to dark green coarse grained with 0.5 cm pyroxene and or amphiboles oikocrysts similar to the flow seen at 90.85 - 99.5 m. Sharp upper internal contact wavy at 35 degrees TeA and sharp lower wavy and variable from 30 - 50 degrees TeA. From 170.1 -172.55 medium green, fine grained massive uniform basalt flow with wavy variable 30 - 50 degrees TeA upper contact and sharp planar lower contact at 40 degrees TeA. The basalt flow sequence exhibits sharp upper and lower contacts at 45 and 40 degrees TeA.

172.55 178.7 QUARTZITE 40 / 40 As previously seen at 101.75 - 110.0 m hard dense looking fine grained microgranular with a strong overprinting of incipient biotite or phlogopite that imparts a patchy to massive dirty brown colour. There are still 1 - 2 mm cream white quartz grains throughout. The less biotite altered quartzite is pale to medium grey in colour. Sharp upper and lower contacts at 40 degrees TeA.

178.7 190.0 BASAL T FLOW 40 / 20 Medium to dark green fine grained massive uniform basalt flow that is microfractured with calcite and/or quartz as healed microfractures and as threadlike fracture fillings. From 179.0 - 180.5 m there are several 1 - 3 mm quartz stringers with finely disseminated pyrite 1 - 3%. Sharp upper and lower contacts at 40 and 20 degrees TeA.

190.0 192.8 QUARTZITE 20 /40 As previously seen above at 172.55 -178.7 m, with dirty brown patchy incipient biotite alteration, calcite and quartz healed microfractures, a hard dense looking quartzite with cream white 1 - 3 mm quartz grains. Sharp upper and lower contacts at 20 and 40 degrees TeA.

• • • DOH No: N 10-01 __ Sheet_S_of_6_ Signed By: ______ Date: ___ _

Metres From: Metres To: Description 192.8 213.25 BASAL T FLOW 40 / 60

Dark green fine grained massive uniform basalt flow. There are quartz filled vesicles some rounded, some flattened and misshapen from 0.5 m up to 3 cm x 1 cm in size. At 200.45 - 202.25 m, there are several threadlike calcite quartz stringers with trace pyrite. At 208.45 - 210.25 m there are several quartz veinlets and quartz calcite stringers with trace pyrite. At 212.25 - 213.25 m several quartz stringers with trace pyrite. Sharp upper and lower contacts at 40 and 60 degrees TCA.

213.25 216.15 QUARTZITE 60 / 55 wavy Buff tan, fine grained, siliceous quartzite with 1 - 2 mm clear grey quartz grains or "eyes" locally cut by 1 - 3 mm cream white quartz-calcite stringers, trace specks of pyrite. Sharp upper and lower wavy contacts at 60 and 55 degrees TCA.

216.15 236.25 BASAL T FLOW 55 / 60 As previously seen at 192.8 - 213.25 m medium to dark green, fine grained massive to uniform basalt flow with narrow localized sections of quartz amygdules at 225.0 m. The unit exhibits calcite quartz lined microfractures and also stringer and vein lets. Sharp wavy upper contact at 55 degrees TCA and sharp lower contact at 60 degrees TCA.

236.25 238.75 BASALT TUFF 60/50 Medium to dark green to brown green alternating thin layers with minor 1 - 2 cm cream grey white to dirty brown intercalated quartzite layers at 45 degrees TCA. The dirty brown quartzite and tuff corresponds to fine incipient biotite alteration. Sharp upper and lower contacts at 60 and 50 degrees TCA.

238.75 256.0 QUARTZITE 40 / 25 As previously seen at 172.55 - 178.7 m, massive hard dense siliceous quartzite with dirty brown incipient biotite/ phlogopite alteration throughout the interval and carries trace pyrite. The unit is microfractured with numerous calcite and quartz healed microfractures. Quartz vein lets and stringers occur at 241.0 - 242.0 m, 243.0 - 244.0 m, 246.0 - 248.0 m, and from 254.0 - 256.0 m the interval bleached and appears silicified. Sharp upper and lower contacts at 40 and 25 degrees TCA.

256.0 268.0 BASALT FLOW 25/30 Dark green, fine to medium grained massive uniform basalt flow. From 263.9 - 267.1 m weak disseminated pyrite 1 - 3% locally and trace malachite and chalcopyrite at 266.8 m on a fracture. Sharp upper and lower

• • • DOH No: N 10-01 __ Sheet_6_of_6_ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Description contacts at 25 and 30 degrees TCA.

268.0 271.0 QUARTZITE 30/50 As previously seen at 238.75 - 256.0 m, hard siliceous and dense looking with 1 - 3 mm cream white quartz grains. Sharp upper and lower contacts at 30 and 50 degrees TCA.

271.0 277.8 APLITE DYKE SO/broken A buff tan to grayish-yellowish tan to dirty pink on fresh broken surfaces fine grained aphanitic with micro plagioclase crystal lathes and mafic amphibole needles, and 1 - 3 mm dark green mafic flecks. Sharp upper contact at 50 degrees TCA, broken lower contact.

277.8 278.0 QUARTZITE broken / -EOH As previously seen at 268.0 - 271.0 m broken upper contact, buff grey yellow, siliceous and hard, with 1 - 2 %

disseminated pyrite locally to EOH.

ftf

• • • DOH No: N 10- 02 __ Sheet _1_of_ 2_ SignedBY~

I DAVE GAMBLE GEOSERVICES INC RR # 2 Site 2, #29, Swastika, Ontario POK 1 TO


Corp Property: Nicol Pro~ert~ Dip: - 38.0 degrees Com~eted: A~iI 26, 2010 Logged By: Dave Gamble Twp/Claim: Nicoll L 4213073 Location:522992mE/5275042mN Core Size: NQ Drilled By: Laframboise Drilling Hole No: N10 - 02 Elevation: 380 m a.s.l. Total Depth: 71.0 m Purpose of Hole: To drill test airborne VTEM electromagnetic and magnetic targets.

Remarks: Intersected a series of Archean basalt flows, tuffs, and intercalated barren siliceous quartzite sediments. Metres From: Metres To: Description

0.0 3.0 OVERBURDEN, 3.0 m NW casing left in

3.0 32.5 BASAL T FLOW - / 70 Medium to dark green, fine grained to fine medium grained massive uniform, basalt flow that is fractured and broken from 3.0 m - 9.0 m, with locally poor core recovery. At 9.0 - 9.05 m a fault gouge mud at 55 degrees TCA fault zone a fault (FAZ). From 9.05 - 32.5 m the basalt flow is less fractured. There are calcite with + / -quartz healed microfractures. There are several barren quartz veinlets at 15.6 m (5 cm) at 78.4 - 18.55 m quartz epidote vein at 30 degrees TCA, at 22.15 m a 3 cm veinlet at 35 degrees TCA, at 23.6 m a 5 cm vein at 60 degrees TCA. A 1 cm quartz calcite veinlet at 26.5 m carries weak disseminated pyrite. The basalt flow also exhibits minor trace pyrite locally at 28.5 - 29.1 m 30.1 - 30.5 m. Sharp lower contact at 70 degrees TCA.

32.5 33.0 QUARTZITE 70 / 50 Fine grained, hard, dense, and very siliceous microgranular mottled grey to grey white to tan dirty looking quartzite. The interval is microfractures with quartz healed m icrofractu res. Sharp upper and lower contacts at 70 and 50 degrees TCA. Local minor chlorite lined fractures.

33.0 48.7 BASAL T FLOW 50 / 55 As previous, dark to medium dark green fine grained massive uniform flow. Locally fractured with calcite and/or quartz healed microfractures. Sharp upper and lower contacts at 50 and 55 degrees TCA.


Metres From: Metres To: Description 48.7 60.7 BASALT TUFF WITH MINOR QUARTZITE LAYERS 55/60

Medium green with some lighter green banding or layering at 45 - 50 degrees TCA, fine grained basalt ash tuff. At 48.7 - 48.8 m a series of thin quartz stringers at 55 degrees TCA. Finely disseminated pyrite at 48.8 - 48.9 m, and 49.5 - 49.6 m.

At 49.85 - 50.3 m there are intercalated quartzite narrow bands at 49.85 - 50.05 m and at 50.2 - 50.3 m with the intervening section as basalt tuff. Both disseminated pyrite and stringers of pyrite occur within the quartzite layers are at 50 and 40 degrees TCA respectively.

From 50.3 - 54.0 m the basalt tuff is laminated at 45 - 50 TCA and locally carries blebs and disseminated pyrite at 51.0 m, and at 51.3 - 51.4 m, at 53.0 - 53.1 mat 54.4 - 54.6 m. The basalt tuff alternating medium green to dark green layering is 60 degrees TCA at 58.5 m. Sharp upper and lower contacts at 55 and 60 degrees TCA.

60.7 62.0 QUARTZITE ( or QUARTZ PORPHYRY APLITE DYKE) 60 / 50 Fine grained to aphanitic medium grey groundmass with 1 - 3 mm cream white quartz grains that give it the appearance of a quartz porphyry aplite dyke. Both upper and lower contacts are sharp at 60 and 50 degrees TCA but with no evidence of a chilled margin. The quartz grains do not show any decrease in size next to the contacts so is questionable as a quartz porphyry and is most likely a meta-sediment.

62.0 63.9 BASALT TUFF 50/60 As previous, medium to dark green massive uniform basalt tuff with numerous calcite quartz healed microfractures. Sharp upper and lower contacts at 50 and 60 degrees TCA.

63.9 65.9 QUARTZITE ( or PINK QUARTZ PORPHYRY APLITE DYKE) 60/ wavy 50 Fine grained to aphanitic pink ground mass with 1 - 3 mm light pink to cream white quartz grains or rounded crystals that give it the appearance of a quartz porphyry aplite dyke. There are also 1 - 2 mm clear grey quartz "eyes". There are no chilled margins or grain size variation at the contacts and is most likely a meta-sediment as previous. Sharp upper contact at 60 degrees TCA, and sharp wavy lower contact at 50 degrees TCA.

65.9 71.0 BASALT TUFF EOH As previous, finely laminated and layered medium to dark green layers of basalt tuff with the bedding at 50

degrees TCA to EOH. /12!7 ~/

• • • DDH No: N 10- 03 __ Sheet _1_of_6 _ Date: AL,fr/f'{UVCJ

I DAVE GAMBLE GEOSERVICES INC RR # 2 Site 2, #29, Swastika, Ontario POK 1TO


Corp Property: Nicol Property Dip: - 45.0 degrees Completed: April 30, 2010 Logged By: Dave Gamble Twp/Claim: Nicoll L 4213073 Location:522992mE/5275042mN Core Size: NQ Drilled By: Laframboise Drilling Hole No: N10 - 03 Elevation: 380.0 m a.s.1. Total Depth: 326.0 m Purpose of Hole: To drill test airborne VTEM electromagnetic and magnetic targets. Remarks: Intersected a narrow weak sulphide pyrite lean magnetite iron formation in siliceous quartzite in an intercalated sequence of basalt flows, tuffs and barren siliceous quartzite sediments of Archean age. Metres From: Metres To: Description

0.0 2.5 OVERBURDEN 3.0 m NW casing left in.

2.5 32.25 BASAL T FLOW - / 70 Medium to dark green fine grained to medium fine grained massive uniform basalt flow. The interval from 2.5 -9.0 m is strongly fractured with broken core recovery. The interval exhibits fine threadlike calcite healed microfractures generally throughout. There is local epidote patches and stringers. A minor intercalated basalt tuff bed at 12.85 - 13.6 m at 55 degrees TCA At 20.45 - 20.9 m a quartz vein with wispy to clots of chlorite and trace specks of pyrite, sharp vein contacts at 40 degrees TCA Minor trace specks of pyrite in the enclosing basalt flow near the vein contacts. Massive uniform medium fine grained basalt flow 20.9 - 32.25 m. Sharp lower contact at 70 degrees TCA Local hematite along several fractures.

32.25 32.6 QUARTZITE (GREY) 70 / 70 Fine grained aphanitic, hard, dense, buff tan to medium dirty grey groundmass or matrix with 1 - 3 mm cream white quartz grains that impart a porphyritic type texture. There is no evidence of chilled or fine grained margins at the contacts and appears to be a siliclastic interflow quartzitic sediment, with only a very remote possibility of quartz porphyritic aplite sill. Sharp upper and lower contacts at 70 degrees TCA and conformable to the volcanics.

32.6 50.35 BASAL T FLOW 70 / 70 As previous, medium to dark green, medium fine grained, massive uniform basalt flow. At 34.7 - 35.7 m the flow is cut by a 1 - 2 cm quartz veinlet at low angles to the core axis and parallels the core

• • • DDH No: N 10- 03 __ Sheet _2_of_6 _ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Description axis for most of the interval. At 42.4 - 42.75 m several calcite quartz stringers to narrow 1 - 2 cm vein lets cut the basalt flow at 55 degrees TCA, trace specks of pyrite, at 46.6 - 46.9 m calcite quartz stringers with weak pyrite, at 49.3 - 49.75 m calcite stringers and a 2 cm and a 5 cm quartz vein with 1 - 3% disseminated coarse pyrite. Sharp upper contact at 70 degrees TCA, and sharp partially broken lower contact at 70 degrees TCA.

50.35 64.6 BASALT TUFF 70/60

64.6

67.1

Medium to dark green alternating finely laminated basalt tuff with primary layering bedding at 60 degrees TCA. The interval is cut by calcite plus quartz threadlike and narrow stringers. The interval carries weakly disseminated pyrite locally from 50.35 - 63.0 m. At 55.1 - 55.55 m there is a medium grey intercalated quartzite band with a weak magnetic susceptibility at 55.1 - 55.2 m up to 0.5 c.g.s. units (cm-gm-sec units Scintrex SM-5) and also carries 3 - 5 % disseminated pyrite. The upper contact is sharp at 55 degrees TCA, and the lower contact sharp and wavy at 40 - 50 degrees TCA with no tuffaceous wall rock layers being cut off, thus suggesting as intercalated siliclastic quartzite layer.(This still could also remotely be a conformable to tuffaceous layering small quartz vein.)

Sharp upper and lower contacts at 70 and 60 degrees TCA.

67.1 QUARTZITE (PINK) 60 I broken Fine grained aphanitic, dense, hard pink matrix or ground mass with 1 - 3 mm cream white quartz grains that imparts a weak "porphryitc" texture. There is little to no evidence of a chilled or contact effect at the contacts or em bayed or protruding contact or inclusions to suggest a quartz porphyry aplitic dyke or sill. The upper contact appears conformable to the basalt tuffaceous layering which tends to suggest a sedimentary siliclastic quartzite intercalated bed. The interval also exhibits round 1 - 3 mm quartz grains that certainly imply a granular quartz sandstone to quartzite sedimentary origin. The pink colouration appears to be related to a fine chemical dusting. The interval carries finely disseminated pyrite locally 1 - 2%. Sharp upper contact at 60 degrees TCA, broken lower contact.

90.4 BASALT FLOW broken 115 As previous, medium to dark green fine grained massive uniform flow with numerous calcite + I - quartz, healed microfractures. At 69.4 - 70.6 a narrow section of intercalcated basalt tuff with finely laminated dark green to medium green layering at 60 - 70 degrees TCA. From 70.6 - 90.4 basalt flow as previous. At 75.75 - 76.65 m a narrow interval of quartz calcite stringers with 1 - 3 % finely disseminated pyrite locally and at 77.3 - 78.0 m several quartz

• • • DDH No: N 10- 03 __ Sheet _3_of_6 _ Signed By: ______ Date: ___ _

Metres From: Metres To: Descri~tion

veinlets plus calcite, and from 82.4 - 84.4 m a narrow series of calcite stringers down the core axis forming a weak veinlet breccia with 1 - 3% disseminated pyrite in the calcite stringer/veinlets. From 87.0 - 90.0 m calcite stringers and healed microfractures in dark green fine grained basalt flow with trace specks and splashes of chalcopyrite. At 85.25 m, coarse splashes of chalcopyrite with calcite stringers. Broken upper contact, sharp lower contact at 15 degrees TCA

90.4 99.45 BASAL T TUFF SEQUENCE 15 160 Dark green fine to fine -medium grained granular, massive uniform basalt tuff with 1 - 2 mm dark green mafic grains from 90.4 - 91.9 m. A lower internal contact at 15 degrees TCA. From 91.9 - 93.5 m a dark green finely laminated basalt tuff that grades into a granular tuff as seen at 90.4 -91.9 m. At 93.5 - 94.0 m a fault zone with 1 - 2 cm wide fault gouge black at 5 - 10 degrees TCA and within a grey siliceous quartzite bed, (FAZ). The fault zone also exhibits calcite stringers veinlets and weak trace pyrite. From 94.0 - 99.45 dark green, basalt tuff with 1 - 3 mm granules light brown to creamy beige quartz and I or feldspar grains as a weak sedimentary component to the tuff. There are several narrow bands of arkosic looking intercalated sediment at 96.2 - 96.7 m. At 98.0 - 98.2 m a siliceous aplite dyke light to medium tan with sharp contacts at 55 degrees TCA fine grained aphanitic siliceous ground mass with dark green amphibole crystal needles and plagioclase crystal lathes in a fine grained interlocking mosaic. From 98.2 - 99.45 m dark green basalt tuff as previous. Sharp upper and lower contacts at 15 and 60 degrees TCA.

99.45 104.60 APLITE DYKE 60 I 70 As previously seen at 98.0 - 98.2 m a fine grained aphanitic groundmass, light brown to buff tan hard, siliceous and dense, is pink fine grained on fresh broken surfaces and contains hornblende amphibole crystal needles and interlocking microcrystalline plagioclase lathes. The interval is massive and uniform with a weak fabric at 50 degrees TCA. At 100.75 - 100.9 m a minor inclusion of dark green basalt. There are also several 1 cm darker green basalt inclusions. The interval is cut by the occasional calcite stringer and locally exhibits red hematite along and near microfractures. On dry surfaces the aplite dyke is pink siliceous and exhibits a fine grained crystalline interlocking texture. Sharp upper and lower contacts at 60 and 70 degrees TCA.

104.6 108.45 BASALT TUFF 70/65 Dark green to green black fine grained granular matrix with 1 - 3 mm beige to light brown siliceous grains imparting a gritty texture similar to the sequence at 94.0 - 99.45 m. Local weak layered fabric at 107.7 m at


Metres From: Metres To: Descri~tion 60 degrees TCA. Sharp upper and lower contacts at 70 and 65 degrees TCA.

108.45 133.75 DIABASE DYKE 65 1 50 Dark green fine grained on contact zones and fine to medium grained crystalline in core of the massive uniform diabase dyke. Both upper and lower contacts exhibit fine grained chilled margins intrusive contacts. The upper contact is fine grained from 108.45 - 113.0 m with a gradual increase in crystalline grain size of the plagioclase interlocking crystals to a fine medium grained crystalline texture. From 128.0 - 133.75 m the lower contact gradually also becomes finer grained towards the lower chilled contact. The central part or core of the diabase dyke is massive uniform, fine to medium grained crystalline. The diabase is weakly magnetic with finely disseminated magnetite and with a magnetic susceptibility ranging from 1.1 - 2.5 c.g.s. (magnetic susceptibility units on a Scintrex SM5). Sharp upper and lower contacts at 65 and 50 degrees TCA ..

133.75 137.1 BASALT TUFF 50/40 As previously seen at 104.6 - 108.45 m, a dark green to green black fine grained granular basalt tuff with light coloured siliceous 1 - 3 mm grains that imparts a gritty texture. Sharp upper and lower contacts at 50 and 40 degrees TCA.

137.1 200.4 BASAL T FLOW 40 1 60 Medium to dark green, medium to coarse grained amphibolitized basal flow. The basalt flow exhibits a mottled and patchy looking texture with the coarse recrystallized amphiboles interlocking with cream white to grey white patches of feldspar. There are several narrow intercalated arkosic bands at 138.65 - 138.7 m at 65 degrees TCA, at 139.4 - 139.45 m @ 75 degrees TCA, a narrow quartzite band at 139.65 - 139.7 m at 65 degrees TCA. At 138.85 - 139.25 m there are several narrow bands of strongly magnetic (12.0 c.g.s. magnetic susceptibility) with disseminated magnetite and locally 2 - 4% finely disseminated pyrite in what appears to be a siliceous gritty intercalated gritty tuff to lean iron formation sediment. At 145.4 - 146.15 m calcite stringers with minor pyrite. At 150.9 - 151.4 a narrow interval of basalt tuff at 40 degrees TCA, dark green amphibolitized with fine acicular amphibole needle-like crystals at 30 degrees TCA. At 151.4 - 152.0 m weak disseminated pyrite. At 156.35, an internal flow contact changing from medium to coarse grained basalt flow above to a fine - grained basalt flow below. This flow to flow contact is at 40 degrees TCA. From 156.35 - 200.4 m generally a fine to medium grained amphibolitized basalt flow. At 157.65 - 158.2 m several pyrite stringers, at 159.6 - 160.15 m finely disseminated pyrite 1 - 3%; at 162.55 m a 1 cm calcite veinlet with disseminated chalcopyrite; at 172.7 - 173.5 m 1 - 3% disseminated pyrite; at 177.1 -

• • • DOH No: N 10- 03 __ Sheet _5_of_ 6_ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Description 178.1 m a quartz epidote garnet vein at 5 to 10 degrees TCA, at 185.0 - 185.5 m 2 - 4% finely disseminated pyrite, at 190.6 - 190.7 m a 10 cm calcite veinlet with trace pyrite; at 191.0 - 192.0 m weak disseminated pyrite and at 198.3 - 200.4 m several pyrite threads and stringers pf pyrite at 199.25 - 199.4 m. Sharp upper and lower contacts at 40 and 60 degrees TCA.

200.4 201.3 QUARTZITE 60 / 45 Light to medium grey to grey brown hard and siliceous, micro-fractured quartzite bed with 1 - 2 mm cream white quartz grains and fine brownish to black incipient biotite. The microfractures are healed by quartz, and only trace specks of pyrite are noted. Sharp upper and lower contacts at 60 and 45 degrees TCA.

201.3 237.0 BASALT FLOW 45/70 As previously seen at 156.35 - 200.4 m fine to fine-medium grained amphibolitized dark green basalt flow. At 201.3 - 203.0 m calcite stringers with disseminated pyrite 1 - 2 %, 204.0 - 205.5 m pyrite along fractures and quartz stringers and veinlets with trace pyrite; 211.0 - 212.0 m disseminated pyrite and calcite threads with pyrite 1 - 2%; at 213.4 - 214.4 disseminated 1 - 3% pyrite with calcite stringers at 218.75 - 221.0 m calcite stringers and 1 - 3% disseminated pyrite; at 222.75 - 223.3 m quartz and calcite stringers with 1 - 2 % disseminated pyrite; 230.0 - 235.0 m calcite stringers and disseminated pyrite 1 - 2%. At 235.5 a calcite stringer with minor disseminated magnetite. Sharp upper and lower contacts at 45 and 70 degrees TCA.

237.0 241.6 FELDSPAR PORPHYRY DYKE 70/70 Pale to medium pink fine grained groundmass with 1 - 2 mm cream white and pale pink feldspar crystals euhedral to subhedral imparting a speckled to porphyritic texture. Dark green 1 - 2 mm specks of amphibole also contribute to a porphyritic texture. Sharp chilled upper and lower contacts at 70 degrees TCA. Trace specks of pyrite are noted.

241.6 244.4 BASAL T FLOW 70 / 50 Dark green, fine to fine medium grained basalt flow with an interlocking mosaic of dark green amphiboles and cream white plagioclase. The interval is locally cut by quartz and epidote vein lets at 242.2 m by the occasional calcite stringer and quartz veinlet at 243.4 m. Sharp upper and lower contacts at 70 and 50 degrees TCA.

244.4 246.75 BASAL T TUFF 50/ 50 Dark green to green black with finely laminated amphibolitic to contorted amphibolitic fabric. The interval is cut


Metres From: Metres To: Description by quartz epidote and minor garnet in stringers and veinlets. Sharp upper and lower contacts at 50 degrees TeA.

246.75 257.0 BASAL T FLOW 50/ jagged irregular As previously seen at 241.1 - 244.4 m dark green fine to fine-medium grained amphibole and plagioclase interlocking fabric with fracture filling calcite, epidote threads, and occasional quartz epidote garnet stringer, veinlets and patches from 250.35 - 253.6 m. From 254.65 - 257.0 m the flow exhibits a coarse grained crystalline texture with interlocking dark green black amphiboles with cream white plagioclase. Sharp upper contact at 50 degrees TeA. Sharp lower contact jagged to irregular down the core axis for 40 cm from 257.0 -257.4 m.

257.0 267.9 BASAL T TUFF jagged irregular / 60 As previous dark green, locally laminated to finely layered amphibolitized cut locally by quartz stringer vein lets at 261.2 - 262.7 m, and at 264.75 - 266.2 m. Jagged irregular upper contact, sharp lower contact at 60 degrees TeA.

267.9 321.15 BASAL T FLOW 60 / 50 As previous, dark green to green black amphibolitized basalt flow with amphibole (80%) and interlocking cream white plagioclase (20 %) locally cut by quartz stringers with epidote and minor pink garnet. At 285.2 m a 15 cm quartz vein with garnet and epidote at 35 degrees TeA. From 293.7 - 294.4 m epidote garnet quartz stringer veinlets. At 298.6 - 299.0 m a quartz vein with chlorite trace pyrite at 30 degrees TeA with disseminated 1 - 3% pyrite for 10 cm in the basalt flow wall rocks. At 200.3 - 300.9 m calcite stringers with locally disseminated and coarse splashes of chalcopyrite. At 301.8 - 302.7 m quartz epidote garnet stringers and veinlets cut the basalt flow. From 299.2 - 321.15 the basalt flow is fine grained medium green massive to uniform throughout, and is cut by calcite fracture filled threadlike stringers as healed microfractures. At 312.2 - 312.8 m quartz stringers with epidote stringers and patchy epidote. At 320.0 - 320.1 m a quartz epidote garnet vein barren at 45 degrees TeA. Sharp upper and lower contact at 60 and 50 degrees TeA.

321.15 326.0 BASAL T TUFF 50 I -EOH Medium to dark green finely laminated fine-grained basalt tuff with the layering and foliation fabric at 45 and 55

degrees TeA as dark green to moderate green alternating bands. At 321.15 - 321.6 m there are calcite quartz stringers with local disseminated pyrite (2%), and 1 - 3% disseminated pyrite at 324.75 - 325.55 m. The basalt tuff is cut by the occasio~artz stringer and by calcite stringers to the EOH with occasional ptygmatic folded calcite stringer. /1

r"l

• • • DDH No: N 10- 04 __ Sheet _1_of_ 5_ SlgnedBY~

I DAVE GAMBLE GEOSERVICES INC RR # 2 Site 2, #29, Swastika, Ontario POK HO


Corp Property: Nicol Property Dip: - 45.0 degrees Completed: May 02, 2010 Logged By: Dave Gamble Twp/Claim: Nicoll L 4213073 Location:522992mE/5275042mN Core Size: NQ Drilled By: Laframboise Drilling Hole No: N10 - 04 Elevation: 380.0 m a.s.1. Total Depth: 140.0 m Purpose of Hole: To drill test airborne VTEM electromagnetic and magnetic targets. Remarks: Intersected a series of Archean basalt flows, tuffs, and intercalated barren siliceous quartzite sediments that have been intruded by several narrow feldspar porphyry and aplitic dykes. Metres From: Metres To: Description

0.0 2.5 OVERBURDEN, 6.0 m NW casing left in.

2.5 28.2 BASALT FLOW - / 55 Medium to medium dark green fine to medium fine grained massive uniform basalt flow. From 2.5 -7.0 m the interval is broken with rubbly core recovery. The interval exhibits calcite healed microfractures and some calcite with quartz stringers and vein lets. At 11.5 - 11.65 m a quartz with epidote vein at 30 degrees TCA, at 14.15. -15.15 m several quartz epidote garnet veinlets at 30 degrees TCA. Sharp lower contact at 55 degrees TCA.

28.2 28.75 QUARTZITE 55 / 65 Buff tan to grayish tan, siliceous hard fine grained with 2 - 4 mm cream white quartz granules locally in this quartzite interflow sediment. The interval carries 1 - 3% finely disseminated pyrite and fine threadlike fracture fillings. Sharp upper and lower contacts at 55 and 65 degrees TCA.

28.75 43.65 BASAL T FLOW 65 / 70 As previous, medium green fine grained massive uniform basalt flow. The unit is cut by calcite stringers and healed microfractures. A bull white quartz vein at 36.85 - 37.10 m at 30 /40 degrees TCA is flanked by calcite stringers for approximately 1.0 m on both the up and down hole side of the vein, trace 1 % pyrite occurs locally. At 42.9 - 43.4 m there are 2 cm, 10 cm, and a 5 cm, veinlet of quartz calcite cutting the basalt flow at 30 - 45 degrees TCA. Sharp upper and lower contacts at 65 and 70 degrees TCA.

• • • DOH No: N 10- 04 __ Sheet _2_of_ 5_ Signed By: ______ Date: ___ _

Metres From: Metres To: Description 43.65 55.4 BASALT TUFF 70/65 - 70

Medium to medium light green alteration, tuffaceous layers and foliation fabric at 70 degrees TeA, fine grained locally cut by quartz and calcite stringers and healed microfractures. There are several 2 - 5 cm veinlets of quartz and calcite at 47.75 - 48.25 m, at 51.35 - 51.65 m, and 1 cm stringers at 53.4 - 53.9 m. The interval also carries patchy disseminated pyrite, occasional pyrite calcite stringers, and associated with and near some of the quartz calcite stringers. At 46.85 - 47.0 m a vein and vein lets of reddish brown garnet with minor epidote also occurs with minor pyrite. Form 53.0 - 54.0 m associated with quartz calcite 1 cm vein lets and stringers is 1 - 3% disseminated pyrite. Sharp upper and lower contacts at 70 and 65 - 70 degrees TeA.

55.4 56.6 FELDSPAR PORPHYRY 65 - 70 / 50 - 60 Gray to grayish pink fine grained groundmass with pink feldspar subhedral 1 - 3 mm phenocrysts that imparts a strong porphyritic texture. The contacts exhibit both a slight chilled contact effect and also minor irregularities and undulations. The interval carries weak specks of pyrite. Sharp upper and lower contacts with undulations at 65 - 70 and 50 - 60 degrees TeA respectively.

56.6 59.7 BASALT TUFF 50 - 60/80 Medium to dark green fine grained granular tuffaceous layering at 70 degrees TeA locally at 56.7 m. The interval is cut by fine threadlike calcite healed microfractures and occasional calcite stringer. The interval is massive to uniform, fine granular texture with sharp upper and lower contacts 50 - 60 and 80 degrees TeA.

59.7 61.8 FELDSPAR PORPHYRY 80/30 As previous, pink fine grained ground mass with 1 - 3 mm cream white feldspar phenocrysts, and 1 - 2 mm round quartz "eyes" and a fine granular dark green 1 mm mafic amphibole. The interval exhibits several chlorite lined fractures that carry minor calcite and weak pyrite. Both the upper and lower contacts exhibit scalloped to undulating contacts at 80 and 30 degrees TeA. The lower contact displays protrusions and embayments synonymous with an intrusive type contact. There are also narrow chilled intrusive contacts.

61.8 69.9 BASALT TUFF 30/50 Fine grained, medium green to light green alternating layers at 60 to 55 degrees TeA throughout the basalt tuff interval. This interval exhibits a strong coloured banded layered to bedding fabric, and also a moderate foliation amphibolitic fabric at 55 to 60 degrees TeA. The interval exhibits weak calcite healed microfractures. Sharp upper and lower contacts at 30 and 50 degrees TeA.


Metres From: Metres To: Description 69.9 89.0 BASAL T FLOW 50 / 40 intrusive

Dark green to medium green fine grained at start and becoming coarse grained crystalline with an interlocking texture locally of coarse amphibole hornblende with cream white plagioclase. There is minor locally disseminated pyrite at 70.3 - 75.0 m from trace to 2 % and also at 80.0 - 82.0 m. Sharp upper contact at 50 degrees TCA, and jagged protrusive intrusive lower contact from unit below at approximately 40 degrees TCA.

89.0 89.45 FELDSPAR PORPHYRY 40 intrusive / 40 undulating Medium grey fine grained groundmass with 1 - 5 mm cream white euhedral to subhedral plagioclase feldspar phenocrysts that impart a strong porphyritic texture. Both upper and lower contacts exhibit a 1 - 2 cm fine grained chilled margins that are cream white and aphanitic. The upper contact is jagged but with intrusive injections or protrusions similar to a feathered type contact at 40 degrees TCA and the lower contact is sharp but undulating with local embayments at 40 degrees TCA. Trace specks pyrite.

89.45 109.5 BASAL T FLOW undulating 40 / wavy irregular 60 Dark green, fine to fine-medium grained basalt flow, massive and uniform. The interval is cut by calcite healed microfractures and cut locally cut by calcite epidote and red garnet stringers and veinlets and by the occasional quartz veinlet. At 91.3 - 91.4 m a quartz epidote vein cuts the interval at 50 degrees TCA. There is locally disseminated trace to 2% pyrite at 89.45 - 92.75 m, at 94.3 - 95.5 m with garnet epidote veinlets, at 99.2-103.0 m, and at 107.5 -109.5 m. Sharp upper undulating 40 degrees TCA contact, and lower contact is sharp, irregular scalloped and approximates 60 degrees TCA.

109.5 110.95 APLITE DYKE wavy irregular 60 / wavy 70 Grey to grayish brick red, fine grained groundmass, dense and hard siliceous, with fine grained 1 mm and less white flecks and lathe-like needles of plagioclase feldspar. There are also weakly distributed 1 mm flecks and prismatic dark green amphibole crystals. The interval exhibits 1-3% disseminated pyrite as well some is associated with dark green chlorite lined microfractures. Sharp upper and lower intrusive embayed and wavy contacts at 60 and 70 degrees TCA.

110.95 112.65 BASAL T FLOW wavy 70 / 15 As previous, dark green basalt flow with occasional calcite healed microfractures and stringers, carries 1 - 3% weakly disseminated pyrite, Sharp wavy em bayed upper contact at 70 degrees TCA, sharp planar lower contact at 15 degrees TCA.


Metres From: Metres To: Description 112.65 115.65 APLITE DYKE 15 I 70

As previously seen at 109.5 - 110.95 m grey to grey-brick red fine-grained groundmass with 1 - 3 mm dark green flecks of amphibole, less than 1 mm grey white feldspar specks, and 1 mm needle-like lathes of plagioclase. On a fresh broken surface the colour of the aplite is pale pink siliceous hard dense looking, and is massive and uniform throughout. The interval is cut by calcite stingers and carries 1 - 3% finely disseminated pyrite locally. Sharp upper contact at 15 degrees TCA, sharp lower contact wavy to slightly undulating at 70 degrees TCA.

115.65 117.25 BASALT FLOW 70 wavy/1 0-25 Dark green-black, fine grained massive uniform basalt flow, locally cut by calcite stringers and carries 2 - 4% finely disseminated pyrite. There are several quartz and quartz with epidote vein lets to stringers that cut the interval. Sharp wavy 70 degrees upper contact, and sharp undulating lower contact at 10 - 25 degrees TCA.

117.25 118.0 APLITE DYKE undulating 10 - 25 I 50 As previously seen at 112.65 - 115.65 m, is locally cut by calcite stringers carries 1 - 3% fine disseminated to specks of pyrite. The 1 - 3 mm mafic amphibole flecks and crystals impart a weak porphyritic texture. The interval exhibits 1 - 3% disseminated pyrite. Sharp undulating upper contact at 10 - 25 degrees TCA, and sharp lower contact at 50 degrees TDCA.

118.0 125.0 BASAL T TUFF 50 I 20 Dark green to medium green alternating narrow mm's to cm's layers of fine grained basalt tuff at 55 - 60 degrees TCA. There are minor local layers that are dark green black that consist of amphibole and fine 1 mm garnet porphyroblasts as an amphibolitized basalt tuff. The interval carries finely disseminated pyrite at 118.0 -120.0m, at 122.0 -122.5 m, at 123.65 - 124.65 m. The unit is cut by calcite stringers and occasional calcite veinlet. Sharp upper and sharp wavy lower contacts at 50 and 20 degree TCA respectively.

125.0 132.15 BASAL T FLOW 20 180 As previous, fine to fine-medium grained dark green massive uniform basalt flow. The interval exhibits fine epidote threadlike fracture linings and patchy sausseritized feldspar locally. The interval carries finely disseminated trace - 3% pyrite from 127.0 - 132.15 m, with narrow sections up to 3 - 4% pyrite at 130.4 - 130.7 m. Sharp wavy upper contact at 20 degrees TCA, and sharp planar lower contact at 80 degrees TCA.

• • • DDH No: N 10- 04 __ Sheet _5_of_ 5_ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Description 132.15 132.9 FELDSPAR PORPHYRY 80 I 70

Medium grey to pink fine grained aphanitic matrix or groundmass very hard, siliceous and dense looking with 1 -3 mm cream white chips and broken crystals of feldspar and or quartz that have diffuse to fuzzy anhedral crystal edges and boundaries. The interval exhibits quartz and epidote stringers and fracture linings, and carries only trace specks of pyrite. Sharp upper and lower contacts at 80 and 70 degrees TCA.

132.9 140.0 BASAL T FLOW 70 1-EOH As previous, dark green fine to medium grained massive uniform basalt flow cut by stringers and fracture linings

of epidote and quartz. There are several quartz epidote garnet stringers and veinlets and a 4 cm quartz-epidote-garnet vein at 133.9 m at 40 degrees TCA. There is 1 - 3% locally disseminated pyrite at 132.9 - 136.0 m. The interval is weakly magnetic from 0.3 - 3.9 c.g.s. (magnetic susceptibility units on a Scintrex SM-5 susceptibility meter.) The interval exhibits dark green amphibole crystals in an interlocking texture with cream white plagioclase that has been amphibolitized to the EOH.

ro/

• • • DOH No: N 10- 05 __ Sheet _1_of_3_

I DAVE GAMBLE GEOSERVICES INC

Signed BY;~ Date~~ /t; u/Z'

RR # 2 Site 2, #29, Swastika, Ontario POK no

NORTHSTAR GOLD DRILL RECORD N10 - 05 Project: Northstar Gold Corp Azimuth: 225.0 degrees Started: May 02, 2010 Logged For: Northstar Gold

Corp Property: Nicol Property Dip: - 38.0 degrees Completed: May 02,2010 Logged By: Dave Gamble Twp/Claim: Nicoll L 4213073 Location: 522958m E/5275054mN Core Size: NQ Drilled By: Laframboise Drilling Hole No: N10 - 05 Elevation: 377.0 a.s.l. Total Depth: 50.0 m Purpose of Hole: To drill test airborne VTEM electromagnetic and magnetic targets. Remarks: Intersected a narrow weak sulphide (pyrite with minor chalcopyrite) lean magnetite iron formation in siliceous quartzite within an intercalated sequence of basalt flows, tuffs and barren siliceous quartzite sediments of Archean age. Metres From: Metres To: Description

0.0 2.0 OVERBURDEN, 3.0 m NW caSing left in.

2.0 18.0 BASALT FLOW - / 45 Medium green, fine grained, massive uniform basalt flow with 1 mm and less fine dark green specks. The interval exhibits a weak foliation fabric at 40 degrees TCA. The start of the hole from 2.0 - 6.0 m is locally fractured. From 16.0 - 18.0 m the interval exhibits fine threadlike calcite healed m icrofractu res. Sharp lower contact at 45 degrees TCA.

18.0 22.65 BASALT TUFF 45/65 Medium green, fine grained finely laminated basalt tuff with numerous calcite threadlike stringers from 18.0 -19.65 m with 2 - 4% disseminated pyrite from 18.8 - 19.0 m. The basalt tuff layering is at 45 - 50 degrees TCA and many of the calcite threadlike stringers also conform to that fabric. At 26.5 - 22.65 m there is strong pervasive epidote patch with minor pyrite near and at the lower contact. Sharp upper and lower contacts at 45 and 65 degrees TCA.

22.65 25.0 QUARTZITE WITH SULPHIDIZED LEAN MAGNETITE IRON FORMATION 65/40 Grey white massive, siliceous, hard, quartzite with dirty grey to grey-black thin bands of magnetite and greenish grunerite (?) causing magnetic susceptibility is from 2.7 - 11.0 c.g.s. units (magnetic susceptibility units on a Scintrex SM-5 meter.). The orientation fabric of thin magnetite threads and fine cm seam lets are at 45 degrees TCA. In addition, there are fine threadlike disseminated stringers of pyrite, coarse pyrite patches, and 1-2 cm of


Metres From: Metres To: Description discontinuous pyrite stringers throughout. At 24.3 - 24.4 m there is a semi-massive seam of coarse granular pyrite with remnant black massive magnetite over 1-2 ems. At 24.5 - 25.0 m there are numerous pyrite stringers, trace chalcopyrite, and several patches of reddish brown garnet. Also at the lower contact there is patchy red brown garnet. This quartzite lean magnetite iron formation appears to be partially sulphidized to pyrite, as pyrite appears to replace and also partially replace the magnetite and grunnerite (?). Sharp upper and lower contacts at 65 degrees and 40 degrees TCA.

25.0 34.8 BASAL T TUFF 40 1 50 As previous medium green basalt tuff with alternating lighter green mm to cm scale layering at 45 to 55 degrees TCA. There are several quartz 1 - 3 cm stringer 1 vein lets at 26.5 m and at 28.5 m. There are also calcite stringers and occasional veinlets with fine disseminated pyrite locally. Sharp upper and lower contacts at 40 and 50 degrees TCA.

34.8 35.8 QUARTZITE 50 1 60 Fine grained aphanitic, siliceous hard, dense medium grey quartzite matrix with very fine incipient biotite dusting imparting a dirty grey brown patchy colour, and also containing cream white siliceous 1 - 3 mm quartz and feldspar chips and broken crystal pieces that impart a granular texture. The contacts appear conformable to the enclosing basalt tuff layering at 50 and 60 degrees TCA for the upper and lower contacts respectively. There are no chilled margins and broken crystal faces occur at the contact as part of the contact, and with minor feathering of the tuffaceous basalt with the quartzite at the lower contact. The lower contact also exhibits fine undulating surface with numerous quartz crystal chips right on the contact surface. Sharp upper and lower contacts at 50 and 60 degrees TCA.

35.8 46.0 BASAL T TUFF 601 jagged irregular As previous, medium to light green layered and laminated at 60 degrees TCA, basalt tuff sequence. The interval locally cut by calcite stringers and healed microfractures. There is an increase in calcite stringers and threadlike stringers from 42.75-43.0m, and from 43.4-46.0m, with trace specks of pyrite. Sharp upper contact at 60 degrees TCA, and an irregular jagged lower contact

46.0 48.4 FELDSPAR PORPHYRY jagged irregular 160 Medium pink, fine grained ground mass with 1-3 mm subhedral to anhedral cream white feldspar phenocrysts imparting a porphyritic texture. Upper contact is sharp but jagged irregular, and the lower contact is sharp and


Metres From: Metres To: Description with minor wavy undulations with a 0.5 cm chilled contact at 60 degrees TCA. The interval also carries finely disseminated pyrite and also exhibits pyrite lined fractures locally.

48.4 50.0 BASAL T TUFF 60 1-EOH As previous, basalt tuff locally cut by calcite stringers with trace pyrite and trace speck of chalcopyrite. The

tuffaceous layering is at 60 degrees TCA to the EOH.

#/

• • • DOH No: N 10- 06 __ Sheet _1_of_ 4_

I DAVE GAMBLE GEOSERVICES INC

Signed BY~ Date:h'/~/f{24lo

RR # 2 Site 2, #29, Swastika, Ontario POK HO

NORTHSTAR GOLD DRILL RECORD N10 - 06 Project: Northstar Gold Corp Azimuth: 238.0 degrees Started: May 02, 2010 Logged For: Northstar Gold

Corp Property: Nicol Property Dip: - 50.0 degrees Completed: May 03, 2010 Logged By: Dave Gamble Twp/Claim: Nicoll L 4213073 Location :523056m E/5274989mN Core Size: NQ Drilled By: Laframboise Drilling Hole No: N10 - 06 Elevation: 387.0 m a.s.l. Total Depth: 104.0 m Purpose of Hole: To drill test airborne VTEM electromagnetic and magnetic targets. Remarks: Within an Archean assemblage the hole intersected a weak sulphide (pyrrhotite, pyrite, minor chalcopyrite and sphalerite) lean magnetite iron formation in siliceous quartzite within an intercalated sequence of basalt flows, tuffs and barren siliceous quartzite. Metres From: Metres To: Description

0.0 1.5 OVERBURDEN, 1.5 m NW casing left in.

1.5 25.7 DIABASE DYKE - / 30 Medium grey to greenish grey, medium grained crystalline, massive uniform diabase dyke. The core is fractured with at least on black chloritc line fracture for every 10 cm of core. Typical diabase type texture with an interlocking mosaic amphiboles with plagioclase. The interval exhibits weakly disseminated magnetite grains throughout with magnetic susceptibility readings ranging conSistently from 1.1 - 1.9 c.g.s. units (Scintrex SM-5 Susceptibility meter). From 22.0-25.7m the diabase becomes gradually fine grained towards the lower contact, a broad and gradual chilled margin with a fine grained medium dark grey chilled contact sharp at 30 degrees TCA.

25.7 27.2 QUARTZITE 30 /40 Medium grey, fine grained siliceous hard and dense quartzite with sharp upper and lower contacts at 30 degrees and 40 degrees TCA. There is a weakly granular texture with 1 - 3 mm rounded cream white anhedral quartz grains. There is the occasional speck of pyrite along several healed microfractures.

27.2 55.45 BASAL T FLOW 40 I 40 Medium green, medium grained crystalline with an interlocking mosaic of green amphibole and cream white plagioclase forming a massive uniform basalt flow. There are several patches and stringers of epidote garnet and quartz at 28.6 - 28.9 m, and at 29.2 - 29.75 m. There is a weak sausseritization of the feldspar to epidote as well as threadlike stringers of epidote. There are occasional red hematite lined fractures at 34.0 - 34.6 m.

• • • DDH No: N 10- 06 __ Sheet _2_of_ 4_ Signed By: ______ Date: ___ _

Metres From: Metres To: Description At 39.15 - 39.65 m quartz veinlets and stringers trace with trace speck pyrite. At 42.1 - 42.15 m quartz calcite stringer vein with trace pyrite. At 44.6 m trace specks of chalcopyrite. At 44.5 - 46.1 m calcite stringers with trace - 2% disseminated pyrite. From 48.0 - 55.45 m the basalt flow carries the occasional pyrite threadlike stringer and pyrite along fractures. At 42.15 - 45.5 m the basalt flow exhibits 2 - 4 mm stubby mafic pyroxene crystals. Sharp upper and lower contacts at 40 degrees TeA.

55.45 60.7 QUARTZITE WITH SULPHIDIZED LEAN MAGNETITE IRON FORMATION 40/50 Grey white, massive siliceous, hard quartzite with dirty grey to grey black thin bands or beds of magnetite causing magnetic susceptibilities ranging from a low of 0.1 with no magnetite up to 25.0 to 33.0 c.g.s. units (magnetic susceptibility units on a Scintrex SM-5 meter). The primary layered fabric of the magnetite layers is at 55 - 65 degrees TeA. There are also numerous sulphides stringers and disseminated sulphides resulting narrow intervals of semi-massive sulphides. The sulphides consist of pyrrhotite, pyrite, and chalcopyrite in order of volume abundance. The pyrrhotite in the most common sulphides representing approximately 80 - 85 % of all sulphides followed by 15% pyrite and less than 1 % chalcopyrite. The overall sulphides content for the interval is approximately in the 20 % by volume ranges. There are coarse sulphides stringers to seams at 56.1 m , 56.4 -56.9 m, 57.6 - 57.7 m, 58.8 - 59.0 m, 59.1 - 59.2 m, 59.4 - 59.5 m 59.7 - 59.8 m and at 60.05 m and consist primarily of pyrrhotite with secondary pyrite and trace chalcopyrite. The sulphide stringers and seams appear to be conformable to the magnetite rich bands and also appear to replace the magnetite. This interval is the same as the interval seen in the DOH N 10-01 and N10-05. At 60.45 - 60.55 m there are several stringers and coarse patches of red brown garnet. Sharp upper and lower contacts for this unit at 40 and 50 degrees TeA.

60.7 63.45 BASAL T TUFF 50 I 45 Medium to lighter green alternating bands of basalt tuff with a good layered fabric at 45 degrees TeA. At 61.6 -61.65 m a narrow grey-white quartzite intercalated layer at 45 degrees TeA. At 63.35 - 63.4 m another narrow intercalated quartzite layer at 50 degrees TeA and carrying 15 - 20 % disseminated pyrite. The basalt tuff exhibits isolated stringers of pyrite and weak local disseminated pyrite. Sharp upper and lower contacts at 50 and 45 degrees TeA.

63.45 66.0 QUARTZITE 45 I 50 Fine grained aphanitic, siliceous hard, dense, medium grey quartzite matrix with cream white siliceous 1 - 3 mm quartz and feldspar chips and broken crystals that impart a granular texture. There are also the occasional clear


Metres From: Metres To: Description 1 - 2 mm quartz 'eyes' as round grains. The contacts appear conformable to the enclosing basalt tuff with the upper and lower contacts at 45 and 50 degrees TCA. The interval exhibits quartz healed microfractures and also carries weak disseminated pyrite and the occasional bleb of pyrrhotite.

66.0 74.75 BASALT TUFF SEQUENCE 50/45 As previous medium to light green alternating fine layers and narrow beds of basalt tuff with layering and weak to moderate foliation fabric to 50 degrees TCA from 66.0 - 71.50 m. There are some darker green partially flattened mafic clasts near the top of the interval. The interval exhibits minor stringers of pyrrhotite and pyrite locally at 67.9 m, at 68.45 m, and at 70.9 m, and as well the occasional coarse patch to coarse stringer of pyrrhotite and pyrite at 67.1 m. From 69.5 - 71.5 the interval contains numerous 1 - 3 cm partially flattened darker green lensoidal shaped basalt lapilli with the foliation fabric at 50 degrees TCA. At 71.5 m there is an internal tuff to tuff contact at 60 degrees TCA where from 71.5 - 74.75 m the basalt tuff is a fine grained basalt ash tuff with finely laminated foliation fabric at 50 degrees TCA. This section exhibits calcite healed microfractures and carries trace to 1 % weak pyrite specks. Sharp upper and lower contacts of sequence at 50 and 45 degrees TCA.

74.75 77.0 QUARTZITE 45 I 40 As previously seen at 63.45 - 66.0 m. Near the upper contact at 74.8 m there is a 1 - 3 mm mafic tuff as finely intercalated lamellae layers. This quartzite is siliceous hard aphanitic matrix with 1 - 3 mm cream white fuzzy looking anhedral quartz and feldspar broken crystals to granules. The matrix also exhibits a weak inCipient biotite dusting that imparts a foggy looking light to medium grey brown slight discolouration from the normal grey-white quartzite. Sharp upper and lower contacts at 45 and 40 degrees TCA.

77.0 88.15 BASALT TUFF 40/50 Medium to dark green fine-grained microgranular basalt tuff to basalt ash. Under hand lens and microscope the interval exhibits a very fine grained granular texture, but to the eye it almost appears like a fine grained basalt flow. The interval is cut by calcite healed microfractures and threadlike stringers and also carries weakly disseminated pyrite. Sharp upper and lower contacts at 40 and 50 degrees TCA.

88.15 93.2 QUARTZITE SEQUENCE 50 I 50 From 88.15 - 90.1 m the quartzite is buff beige, granular with 1 - 3 mm rounded siliceous grains and also with dark green occasional 1 - 3 mm mafic rock chip. This interval exhibits 1 - 2 % fine disseminated pyrite and also calcite lined microfractures. The upper and lower contact for this interval is 50 degrees TCA.


Metres From: Metres To: Description From 90.1 - 93.2 m the quartzite is hematized to brick red in colour from 90.1 - 92.0 m with numerous quartz healed microfractures. From 92.0 - 93.2 m the quartzite is pale tan to beige and also has numerous quartz healed microfractures. This section is very siliceous hard, brittle and dense and carries 1 - 3% finely disseminated pyrite. The upper and lower contact of the quartzite sequence is 50 degrees TCA.

93.2 104.0 BASAL T TUFF 50/-EOH As previous seen at 77.0 - 88.15 m, dark green, fine grained, microgranular basalt ash tuff, massive, fine

grained and uniform to EOH. The interval exhibits a weak layering foliation fabric at 50 degrees TCA and carries weak disseminated and specks of trace to 2% pyrite locally as well as several pyrite threadlike stringers associated with calcite stringers to EOH.

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• • • DDH No: N 10-07 __ Sheet_1_of_4 _

DAVE GAMBLE GEOSERVICES INC RR # 2 Site 2, #29, Swastika, Ontario POK 1TO

NORTH STAR GOLD DRILL RECORD N10- 07 Project: Northstar Gold Corp Azimuth: 235.0 degrees Started: May 03, 2010 Logged For: Northstar Gold

Corp Property: Nicol Property Dip: - 71.2 degrees Completed: May 04,2010 Logged By: Dave Gamble Twp/Claim: Nicoll L 4210722 Location:523312mE/5274741mN Core Size: NQ Drilled By: Laframboise Drilling Hole No: N10 - 07 Elevation: 355.0m a.s.1. Total Depth: 170.0 m Purpose of Hole: To drill test airborne VTEM electromagnetic and magnetic targets. Remarks: The hole encountered a flat lying sequence of Proterozoic polymictic conglomerate that overlie with an angular unconformity an Archean vOlcano-sedimentary assemblage. Within the Archean assemblage the hole intersected a weak sulphide (pyrrhotite minor chalcopyrite and sphalerite) lean magnetite iron formation in siliceous quartzite within an intercalated sequence of ultramafic komatiitic basalt flows, tholeiitic basalt flows, tuffs and barren siliceous quartzite sediments. Metres From: Metres To: Description

0.0 5.0 OVERBURDEN, 6.0 m NW casing left in. 5.0 53.9 CONGLOMERATE - PROTEROZOIC COBALT SEDIMENTARY GROUP - LORRAIN FORMATION -/45

From 5.0 - 41.7 m a distinctive reddish maroon polymictic pebble conglomerate with a sandy to gritty matrix with maroon hematite cement and coatings to the gritty sandy grains. This matrix is host to a population of pebbles and fragments that consist primarily of dark grey to green siltstone mudstone, greywacke, arkose, pink granite -granodiorite and granitic porphyry intrusive clasts, and mafic dark green volcanic flow and fine fragmental tuffaceous pebbles. The sedimentary clasts are lenticular and have a 5: 1 to 10: 1 long axis to short axis ration of the lengths to widths. There are volcanic rounded pebbles to small 5 cm boulders and cobbles, some green gritty sedimentary clasts, cream white quartz chips and pebbles to angular clasts, occasional maroon siltstone to mUdstone pebbles and the occasional maroon possible fine grained volcanic flow pebbles. The clasts, pebbles and boulders make up approximately 60% of the rock while the maroon sandy to gritty hematite matrix makes up 40 % by volume of the rock. The rock is friable, easily broken with much of the interval exhibiting a fracture every 10 - 20 cm. At 20.1 - 20.25 a quartz boulder or possible vein, bull white and barren. The flattened orientation of the conglomerate pebble population appears to be consistently at 70 degrees TCA. Several gritty and sandy beds also exhibit a primary layering at 70 degrees TCA as at 7.15 m. This angle to the core axis represents a relative flat lying to very shallow dipping sedimentary sequence at 5-10 degrees TCA. From 44.1 - 53.9 the conglomerate rapidly changes to a predominantly green matrix that hosts many of conglomerate pebbles, boulders and lenticular clasts described above. This colour change appears to represent

• • • DDH No: N 10- 07 __ Sheet _2_of_ 4 _ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Description a transition from shallow marine oxidizing environment to a slightly deeper reducing environment. There are occasional reddish pink felsic intrusive pebbles and boulder clasts from several cms up to 5 to 10 cm in size.

At 25.0 m there is a 2 cm fault gouge fault zone ( FAZ) at 70 degrees TCA. At 34.6 - 34.7 m there is a 10 cm muddy brecciated fault gouge fault zone (FAZ) at 40 degrees TCA.

At 50.75 there is a 5 cm quartzite boulder that is carrying coarse splashes of chalcopyrite. The quartzite with sulphides boulder looks very similar to the sulphidized lean magnetite iron formation seen in the underlying Archean assemblage in other ddh's N 10 - 01, -03, -05, -06, and lower in this hole.

The lower contact is sharp at 45 degrees TCA with a minor small fracture slip.

53.9 122.3 BASALT TO KOMATIITIC BASAL T FLOW SEQUENCE 45 / 35 From 53.,9 - 90.3 m the basalt to peridotitie flow is dark green fine grained massive to uniform, and is fractured with numerous calcite threadlike healed microfractures. There are dark green chlorite to serpentine slips and fracture linings. From 53.9 - 101.1 m the interval is strongly magnetic with magnetite susceptibility ranging from 5.0 - 13.0 c.g.s. units (Scintrex SM - 5 meter), with finely disseminated magnetite throughout. There are also light green serpentine and calcite stringers locally and also vibrant green serpentine to talc stringers with calcite locally at 89.6 - 90.3 m an interval with several 5 cm and one 15 cm vein of light green talc veins with minor calcite.

From 90.3 - 122.3 m the komatiitic basalt changes to a medium to coarse grained crystalline pyroxene oikocrystic komatiitic basalt flow with 0.5 cm stubby dark green pyroxene crystals as the oikocrystic ('oiks') in a medium green ground mass.

At 96.5 - 98.8 m a 'fault zone'. FAZ a rubbly broken core recovery with approximately 40 % material recovered in the zone (i.e. 60 % lost), with some strong slips at 15 to 30 degrees TCA.

The oikocrystic komatiitic basalt flow gradually become less dark green and more leucocratic and from 101.0 -122.3 m is non magnetic with no magnetite present. Form 113.0 - 117.0 the pyroxene 'oiks' gradually become finer grained and eventually disappear. From 117.0 - 118.5 m there is a weak layered fabric at 50 degrees TCA as fine darker green flow banding or possibly intrusive magmatic layering. From 118.5 - 122.3 m the interval is a medium grained tholeiitic type basalt flow that becomes fine grained towards the lower contact.


Metres From: Metres To: Description This flow sequence appears to be a differentiated flow from komatiitic basalt to pyroxene oikocrystic komatiitic basalt to tholeiitc basalt flow sequence with the differentiation becoming more leucocratic uphole or to the southwest. Sharp upper contact at 45 degrees TCA and sharp lower contact at 35 degrees TCA.

122.3 123.3 QUARTZITE 35 / 35 Medium to light grey fine - grained hard siliceous and dense matrix with 1- 3 mm grey white quartz grains. The unit is massive, uniform and unbedded. The rock is brittle fractured with quartz healed microfractures and chlorite, dark green lined fracture slips. The interval carries 1 - 3% pyrite along fractures and locally fine disseminated pin prick pyrite. Sharp upper and lower contacts at 35 degrees TCA.

123.3 124.5 BASAL T TUFF 35/ 35 Dark green, fine grained, finely laminated basalt ash tuff cut by white calcite lined microfractures and thin stringers. The interval carries 1 - 2% finely disseminated pyrite locally. Sharp upper and lower contacts at 35 degrees TCA.

124.5 127.8 QUARTZITE 35 /40 As previously seen at 122.3 - 123.3 m with numerous chlorite lined fracture slips and fine quartz lined microfractures. Disseminated pyrite 1 - 3% occurs along the fractures and as local fine disseminations. Sharp upper and lower contacts at 35 and 40 degrees TCA.

127.8 128.8 BASALT TUFF 40 / 35 As previously seen at 123.3 - 124.5 m dark green fine grained ash tuff cut by calcite stringers and threadlike stringers, carries 1 - 3 % finely disseminated pyrite. Sharp upper and lower contacts at 40 and 35 degrees TCA. At 128.55 m a 1 cm fault gouge seam fault zone (FAZ) at 40 degrees TCA, with calcite stringers locally flanking the fault zone.

128.8 134.6 QUARTZITE 35 / 45 As previously seen above at 124.5 - 127.8 m, fractured with green black chlorite lined fractures with 1 - 3% pyrite, quartz healed microfractures also with pyrite, and also pyrite lined fractures and disseminated pyrite. Sharp upper and lower contacts at 35 degrees and 45 degrees TCA.

• • • DOH No: N 10- 07 __ Sheet _4_of_ 4 _ Signed 8y: ______ Date: ___ _

Metres From: Metres To: Description 134.6 135.7 QUARTZITE SILSTONE WITH SULPHIDIZED LEAN MAGNETIE IRON FORMATION 45/50

Grey quartzite sediment from 134.6 - 135.4 m with semi to massive pyrrhotite blebs at 134.65 - 135.75 m, at 135.880 - 135.85 m at 35 to 45 degrees TCA, thin pyrrhotite filaments conformable to the sedimentary layering at 35 - 46 degrees TCA from 135.85 - 135.3 m. Coarse bands of pyrrhotite from 135.3 - 135.5 m with clots and disseminations of chalcopyrite. There is a minor pyrite component with the pyrrhotite and is generally a 1 - 3 mm cubic crystals as locally disseminated within the fine gained pyrrhotite. From 135.4 - 135.7 m there are siltstone layering and lamellae at 35 - 45 degrees TCA with minor pyrrhotite lamellae and blebs. Sharp upper and lower contacts at 45 and 50 degrees TCA.

135.7 162.5 BASAL T FLOW 50 / 30 - 40 Medium green, fine grained massive uniform basalt flow. From 140.5 - 142.2 the interval is cut by quartz threadlike stringers with calcite and by 0.5 cm stringers, and by a quartz vein at 141.75 -141.85 m at 35 - 40 degrees TCA with associated finely disseminated pyrite near the vein walls with calcite and wispy filaments of sericite. From 145.3 - 146.4 m calcite epidote and quartz stringers and patches with minor red garnet and trace to 1% disseminated pyrite. There are local thin calcite quartz epidote stringers with minor pyrite at 149.6 m, 150.7 m, 151.2 m, 154.2 m, 154.55 m, 155.4 m, 156.15 m with pyrite and trace chalcopyrite, at 158.55 m, and at 158.9 m. Sharp upper and lower contacts at 50 and wavy 30 -40 TCA respectively.

162.5 164.6 BASALT TUFF 30 - 40 / 55 Medium green alternating with brownish green layers of fine grained basalt tuff at 45 degrees TCA. The interval is cut by white calcite stringers and vein lets and locally carries trace to 1 % pyrite specks. Sharp upper wavy contact at 30 - 40 degrees TCA. Sharp lower contact at 55 degrees TCA.

164.6 167.2 QUARTZITE 55 / 45 As previously seen at 128.8 - 134.6 m, medium grey to grey brown, hard siliceous and dense looking matrix with incipient biotite imparting a brownish tinge alteration in contrast to normal buff light grey unaltered patches. The interval is cut by numerous white quartz healed microfractures, and the interval carries finely disseminated 1 -3% pyrite locally. Sharp upper and lower contacts at 55 and 45 degrees TCA.

167.2 170.0 BASAL T TUFF 45 I -EOH As previously seen at 162.5-164.6m with dark green to medium green layering and upper contact at 45 degrees

TCA. The interval is cut by calcite threads and stringers with weak pyrite locally, trace chalcopyrite along a fracture at 169.15 m,~ at 169.95m in a quartz epidote calcite 0.5 m stringer. Fine-grained basalt tuff to EOH.

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APPENDIX SECTION 2

NICOL GOLD PROPERTY DRILL HOLE

ORIENTATION SURVEY DATA TABLE

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SUMMARY TABLE FOR DIAMOND DRILL HOLE ORIENTATION SURVEY DATA (Legend for Abbreviations Utilized)

Hole No I BHID Diamond Drill Hole Identification Number / Bore Hole Identification Number AT or Depth Survey Point Location in meters as core length measurement Dip Dip inclination measurement of hole at survey point + sign means down dip

hole for Datamine BRGorAz Bearing or Azimuth measurement of hole at survey point X Collar Easting Coordinate UTM in meters at collar Y Collar Northing Coordinate UTM in meters at Collar Z Collar Elevation in meters at Collar End Depth End of Hole in meters

Survey Instrument Used - Reflex EZ Shot

DMNicoiCollars2010

BHID X COLLAR YCOLLAR ZCOLLAR ENDDEPTH

• N10-01 523281 5274788 355.0 278 N10-02 522992 5275042 380.0 71 N10-03 522992 5275042 380.0 326 N10-04 522992 5275042 380.0 140 N10-05 522958 5275054 377.0 50 N10-06 523056 5274989 387.0 104 N10-07 523312 5274741 372.0 170

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DMNicSurveys2010

• BHID AT BRG DIP N10-01 0.0 232.0 62.0 N10-01 50.0 232.8 62.6 N10-01 100.0 232.8 62.3 N10-01 150.0 232.8 62.0 N10-01 200.0 233.1 62.0 N10-01 250.0 234.9 60.6 N10-01 278.0 236.4 60.3 N10-02 0.0 270.0 38.0 N10-02 50.0 272.2 39.5 N10-03 0.0 270.0 45.0 N10-03 50.0 272.7 45.7 N10-03 100.0 275.8 45.0 N10-03 150.0 275.9 44.4 N10-03 200.0 276.1 43.5 N10-03 250.0 276.0 43.2 N10-03 300.0 275.9 42.8 N10-04 0.0 235.0 45.0 N10-04 50.0 235.4 45.0 N10-04 100.0 234.4 44.4 N10-04 140.0 232.1 44.0 N10-05 0.0 225.0 38.0 N10-05 50.0 225.6 38.1 N10-06 0.0 238.0 50.0 N10-06 50.0 235.2 50.2

• N10-06 100.0 237.2 49.1 N10-07 0.0 235.0 71.2 N10-07 50.0 236.0 71.1 N10-07 100.0 237.0 71.0 N10-07 150.0 237.8 70.8 N10-07 170.0 238.9 70.8

• Page 1 of 3

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APPENDIX SECTION 3


SUMMARY GEOLOGY TABLE

• BHID FROM TO LITH NLiTH N10-01 0.00 46.00 PCGL N10-01 46.00 46.25 KBF N10-01 46.25 46.26 FAZ N10-01 46.26 99.50 KBF N10-01 99.50 101.75 BT N10-01 101.75 110.00 QZT N10-01 110.00 110.50 BT N10-01 110.50 111.55 QZT N10-01 111.55 111.75 BT N10-01 111.75 115.80 BIFS N10-01 115.80 172.55 BF N10-01 172.55 178.70 QZT N10-01 178.70 190.00 BF N10-01 190.00 192.80 QZT N10-01 192.80 213.25 BF N10-01 213.25 216.15 QZT N10-01 216.15 236.25 BF N10-01 236.25 238.75 BT N10-01 238.75 256.00 QZT N10-01 256.00 268.00 BF N10-01 268.00 271.00 QZT N10-01 271.00 277.80 APDK N10-01 277.80 278.00 QZT N10-02 0.00 3.000VB

• N10-02 3.00 9.00 BF N10-02 9.00 9.05 FAZ N10-02 9.05 32.50 BF N10-02 32.50 33.00 QZT N10-02 33.00 48.70 BF N10-02 48.70 49.85 BT N10-02 49.85 50.30 QZT N10-02 50.30 60.70 BT N10-02 60.70 62.00 QZT N10-02 62.00 63.90 BT N10-02 63.90 65.90 QZT N10-02 65.90 71.00 BT N10-03 0.00 2.500VB N10-03 2.50 32.25 BF N10-03 32.25 32.60 QZT N10-03 32.60 50.35 BF N10-03 50.35 64.60 BT N10-03 64.60 67.10 QZT N10-03 67.10 90.40 BF N10-03 90.40 93.50 BT N10-03 93.50 94.00 FAZ N10-03 94.00 98.00 BT N10-03 98.00 98.20 APDK N10-03 98.20 99.45 BT N10-03 99.45 104.60 APDK • N10-03 104.60 108.45 BT N10-03 108.45 133.75 DBDK

• N10-03 133.75 137.10 BT N10-03 137.10 138.85 BF N10-03 138.85 139.25 BIFS N10-03 139.25 200.40 BF N10-03 200.40 201.30 QZT N10-03 201.30 237.00 BF N10-03 237.00 241.60 FPDK N10-03 241.60 244.40 BF N10-03 244.40 246.75 BT N10-03 246.75 257.00 BF N10-03 257.00 267.90 BT N10-03 267.90 321.15BF N10-03 321.15 326.00 BT N10-04 0.00 2.500VB N10-04 2.50 28.20 BF N10-04 28.20 28.75 QZT N10-04 28.75 43.65 BF N10-04 43.65 55.40 BT N10-04 55.40 56.60 FPDK N10-04 56.60 59.70 BT N10-04 59.70 61.80 FPDK N10-04 61.80 69.90 BT N10-04 69.90 89.00 BF N10-04 89.00 89.45 FPDK N10-04 89.45 109.50 BF

• N10-04 109.50 110.95 APDK N10-04 110.95 112.65 BF N10-04 112.65 115.65 APDK N10-04 115.65 117.25 BF N10-04 117.25 118.00 APDK N10-04 118.00 125.00 BT N10-04 125.00 132.15 BF N10-04 132.15 132.90 FPDK N10-04 132.90 140.00 BF N10-05 0.00 2.000VB N10-05 2.00 18.00 BF N10-05 18.00 22.65 BT N10-05 22.65 25.00 BIFS N10-05 25.00 34.80 BT N10-05 34.80 35.80 QZT N10-05 35.80 46.00 BT N10-05 46.00 48.40 FPDK N10-05 48.40 50.00 BT N10-06 0.00 1.500VB N10-06 1.50 25.70 DBDK N10-06 25.70 27.20 QZT N10-06 27.20 55.45 BF N10-06 55.45 60.70 BIFS N10-06 60.70 63.45 BT N10-06 63.45 66.00 QZT • N10-06 66.00 74.75 BT N10-06 74.75 77.00 QZT

• N10-06 77.00 88.15 BT N10-06 88.15 93.20 QZT N10-06 93.20 104.00 BT N10-07 0.00 5.000VB N10-07 5.00 25.00 PCGL N10-07 25.00 25.02 FAZ N10-07 25.02 34.60 PCGL N10-07 34.60 34.70 FAZ N10-07 34.70 53.90 PCGL N10-07 53.90 96.50 KBF N10-07 96.50 98.80 FAZ N10-07 98.80 122.30 KBF N10-07 122.30 123.30 QZT N10-07 123.30 124.50 BT N10-07 124.50 127.80 QZT N10-07 127.80 128.55 BT N10-07 128.55 128.56 FAZ N10-07 128.56 128.80 BT N10-07 128.80 134.60 QZT N10-07 134.60 135.70 BIFS N10-07 135.70 162.50 BF N10-07 162.50 164.60 BT N10-07 164.60 167.20 QZT N10-07 137.20 170.00 BT

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APPENDIX SECTION 4


SUMMARY ASSAY TABLE

• BHID FROM TO AU AG SAMPLE

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SUMMARY DIAMOND DRILL HOLES ASSAY TABLE fAu-Ag) 2010 (Legend for Abbreviations Utilized)

Bore Hole (Diamond Drill Hole) Identification Number Start of Sample Interval in meters End of Sample Interval in meters Gold Assay in ppb (parts per billion) - 1 ppb equates to trace or not detected in list Silver Assay in ppm (parts per million) Sample Number

• BHID FROM TO AU AG SAMPLE N10-01 46.15 46.55 10 0.2 43233 N10-01 72.50 73.45 10 0.2 43234 N10-01 73.45 74.35 10 0.2 43235 N10-01 74.35 75.00 10 0.5 43236 N10-01 75.00 76.00 10 0.4 43237 N10-01 76.00 77.00 10 0.2 43238 N10-01 99.75 100.75 10 0.2 43239 N10-01 100.75 101.75 10 0.4 43240 N10-01 101.75 102.25 20 0.2 43241 N10-01 102.25 103.00 25 0.2 43242 N10-01 103.00 104.00 20 0.2 43243 N10-01 104.00 105.00 10 0.2 43244 N10-01 105.00 106.00 30 0.2 43245 N10-01 106.00 107.00 30 0.2 43246 N10-01 107.00 108.00 10 0.2 43247 N10-01 108.00 109.00 20 0.2 43248 N10-01 109.00 110.00 35 0.2 43249 N10-01 110.00 110.50 10 0.6 43250 N10-01 110.50 111.00 20 0.2 43251 N10-01 111.00 111.55 20 0.2 43252 N10-01 111.55 111.75 10 0.6 43253 N10-01 111.75 112.25 40 1.6 43254 N10-01 112.25 112.75 40 2.6 43255 N10-01 112.75 113.25 20 1.3 43256

• N10-01 113.25 113.75 10 0.4 43257 N10-01 113.75 114.25 20 1.2 43259 N10-01 114.25 114.75 10 0.8 43260 N10-01 114.75 115.25 10 0.6 43261 N10-01 115.25 115.80 15 0.7 43262 N10-01 115.80 116.50 10 0.2 43263 N10-01 122.50 123.10 10 0.3 43264 N10-01 123.10 123.90 10 0.3 43265 N10-01 127.50 128.30 50 0.3 43266 N10-01 130.25 131.25 10 0.2 43267 N10-01 131.25 132.00 10 0.2 43268 N10-01 132.00 132.85 10 0.3 43269 N10-01 135.75 136.25 10 0.2 43270 N10-01 146.10 146.65 70 0.2 43271 N10-01 151.50 151.70 10 0.2 43272 N10-01 172.55 173.25 10 0.2 43273 N10-01 173.25 174.00 10 0.2 43274 N10-01 174.00 175.00 10 0.2 43275 N10-01 175.00 176.00 10 0.2 43276 N10-01 176.00 177.00 10 0.2 43277 N10-01 177.00 178.00 15 0.2 43278 N10-01 178.00 178.80 10 0.2 43279 N10-01 178.80 179.70 10 0.3 43280 N10-01 179.70 180.50 10 0.2 43281 N10-01 190.00 191.00 10 0.2 43282 • N10-01 191.00 192.00 140 0.2 43284 N10-01 192.00 192.80 40 0.2 43285

• N10-01 200.45 201.45 10 0.2 43286 N10-01 201.45 202.25 10 0.2 43287 N10-01 208.45 209.25 10 0.2 43288 N10-01 209.25 210.25 10 0.2 43289 N10-01 212.25 213.25 10 0.2 43290 N10-01 213.25 214.25 10 0.2 43291 N10-01 214.25 215.25 10 0.3 43292 N10-01 215.25 216.15 10 0.3 43293 N10-01 216.15 217.15 10 0.4 43294 N10-01 217.15 218.00 10 0.3 43295 N10-01 236.25 237.00 10 0.2 43296 N10-01 237.00 238.00 10 0.2 43297 N10-01 238.00 238.75 20 0.5 43298 N10-01 238.75 239.50 20 0.2 43299 N10-01 239.50 240.25 20 0.2 43300 N10-01 240.25 241.00 10 0.2 43301 N10-01 241.00 242.00 20 0.2 43302 N10-01 242.00 243.00 30 0.2 43303 N10-01 243.00 244.00 170 0.2 43304 N10-01 244.00 245.00 10 0.2 43305 N10-01 245.00 246.00 10 0.2 43306 N10-01 246.00 247.00 10 0.2 43307 N10-01 247.00 248.00 10 0.2 43309 N10-01 248.00 249.00 10 0.2 43310 N10-01 249.00 250.00 10 0.2 43311


• N10-03 272.40 274.80 10 0.2 43447 N10-03 278.80 279.10 20 0.2 43448 N10-03 279.55 279.85 10 0.2 43449 N10-03 281.00 281.80 410 0.2 43450 N10-03 283.70 284.40 10 0.2 43451 N10-03 285.20 285.35 20 0.2 43452 N10-03 293.70 294.40 30 0.2 43454 N10-03 298.50 299.10 110 0.2 43455 N10-03 300.30 300.90 170 1.3 43456 N10-03 301.80 302.70 30 0.4 43457 N10-03 307.60 307.90 10 0.6 43458 N10-03 312.20 312.80 40 0.2 43459 N10-03 321.15 321.60 10 0.2 43460 N10-03 324.75 325.55 80 0.6 43461 N10-04 11.30 11.90 10 0.2 43462 N10-04 14.15 15.15 40 0.2 43463 N10-04 28.20 28.75 10 0.2 43464 N10-04 35.80 36.80 10 0.2 43465 1\110-04 36.80 37.20 10 0.2 43466 N10-04 37.20 38.00 10 0.2 43467 N10-04 42.90 43.65 10 0.2 43468 N10-04 43.65 44.50 45 0.2 43469 N10-04 44.50 45.50 10 0.2 43470 N10-04 45.50 46.50 10 0.2 43471 N10-04 46.50 47.00 20 0.2 43472


• N10-05 26.00 27.00 10 0.2 43555 N10-05 27.00 28.00 10 0.2 43556 N10-0S 28.00 29.00 10 0.2 43557 N10-0S 29.00 30.00 10 0.2 435S8 N10-0S 30.00 31.00 10 0.2 43559 N10-0S 31.00 32.00 10 0.2 43560 N10-0S 32.00 33.00 10 0.2 43561 N10-0S 33.00 34.00 10 0.2 43562 N10-0S 34.00 34.80 10 0.2 43563 N10-0S 34.80 35.80 10 0.2 43565 N10-0S 35.80 36.40 10 0.2 43566 N10-0S 36.40 37.00 10 0.2 43S67 N10-05 37.00 38.00 10 0.2 43568 N10-0S 38.00 39.00 10 0.2 43569 N10-0S 39.00 40.00 10 0.2 43S70 N10-0S 40.00 41.00 10 0.3 43571 N10-0S 41.00 42.00 10 0.3 43572 N10-05 42.00 43.00 10 0.2 43573 N10-05 43.00 44.00 10 0.2 43574 N10-05 44.00 45.00 10 0.2 43575 N10-05 45.00 46.00 20 0.2 43576 N10-05 46.00 46.50 10 0.2 43577 N10-05 46.S0 47.00 10 0.2 43578 N10-05 47.00 47.50 10 0.2 43S79 N10-05 47.50 48.00 10 0.2 43580

• N10-05 48.00 48.40 10 0.2 43581 N10-0S 48.40 49.00 10 0.2 43582 N10-05 49.00 50.00 10 0.2 43583 N10-06 26.70 26.45 20 0.2 4358S N10-06 26.45 27.20 20 0.2 43586 N10-06 28.60 28.90 10 0.2 43S87 N10-06 29.20 29.75 10 0.2 43588 N10-06 39.15 39.65 10 0.2 43589 N10-06 42.00 42.40 10 0.2 43590 N10-06 44.25 44.80 10 0.2 43591 N10-06 45.50 46.10 10 0.2 43592 N10-06 48.00 49.00 10 0.2 43593 N10-06 49.00 SO.OO 10 0.2 43594 N10-06 50.00 51.00 10 0.2 43595 N10-06 51.00 52.00 10 0.2 43596 N10-06 52.00 53.00 10 0.5 43597 N10-06 53.00 54.00 10 0.7 43598 N10-06 54.00 55.00 10 0.3 43599 N10-06 55.00 5S.45 10 0.2 43600 N10-06 55.45 56.00 30 1.6 43601 N10-06 56.00 56.50 40 1.6 43602 N10-06 56.50 57.00 30 1.1 43603 N10-06 57.00 57.50 25 0.5 43604 N10-06 57.50 58.00 50 1.2 43605 N10-06 58.00 58.50 10 0.2 43606 • N10-06 58.50 59.00 40 0.6 43607 N10-06 59.00 59.50 90 1.0 43608

• N10-06 59.50 59.80 75 1.3 43609 N10-06 59.80 60.30 30 0.2 43611 N10-06 60.30 60.70 20 0.5 43612 N10-06 60.70 61.50 10 0.2 43613 N10-06 61.50 62.35 10 0.2 43614 N10-06 62.35 63.20 10 0.2 43615 1\110-06 63.20 63.45 20 0.2 43616 N10-06 63.45 64.00 10 0.2 43617 N10-06 64.00 64.50 10 0.2 43618 N10-06 64.50 65.00 10 0.2 43619 N10-06 65.00 65.50 10 0.2 43620 N10-06 65.50 66.00 20 0.3 43621 N10-06 66.00 67.00 10 0.2 43622 N10-06 67.00 68.00 20 0.2 43623 N10-06 68.00 69.00 10 0.2 43624 N10-06 69.00 70.00 10 0.2 43625 N10-06 70.00 71.00 10 0.2 43626 N10-06 71.00 71.50 10 0.2 43627 N10-06 71.50 72.00 10 0.2 43628 N10-06 72.00 73.00 10 0.2 43629 N10-06 73.00 74.00 10 0.2 43630 N10-06 74.00 74.75 10 0.2 43631 N10-06 74.75 75.50 10 0.2 43632 N10-06 75.50 76.25 10 0.2 43633 N10-06 76.25 77.00 10 0.2 43634



• N10-07 135.70 136.20 20 0.5 43689 N10-07 136.20 140.50 10 0.2 43690 N10-07 140.50 141.50 10 0.2 43691 N10-07 141.50 142.20 50 0.3 43693 N10-07 145.30 146.40 10 0.2 43694 N10-07 149.15 149.65 10 0.2 43695 N10-07 150.50 151.25 10 0.2 43696 N10-07 154.20 154.90 10 0.2 43697 N10-07 155.20 155.50 20 0.3 43698 N10-07 156.00 156.25 10 0.2 43699 N10-07 158.50 159.00 10 0.2 43700 N10-07 159.40 159.60 10 0.2 43701 N10-07 162.50 163.20 10 0.2 43702 N10-07 163.20 163.90 10 0.2 43703 N10-07 163.90 164.60 10 0.2 43704 N10-07 164.60 165.50 10 0.2 43705 N10-07 165.50 166.40 10 0.2 43706 N10-07 166.40 167.20 10 0.2 43707 N10-07 168.00 169.00 10 0.2 43708 N10-07 169.00 170.00 10 0.2 43709 N10-07 89.60 90.40 10 0.2 43747

•

• • • Assayers Canada 8282 Sherbrooke St., Vancouver, B.C., V5X 4R6

CAN A D Tel: (604) 327-3436 Fax: (604) 327-3423

Report No

Date

OWl836PJ

Ju\-05-\O

Northstar Gold Corporation Sample type PULP

Project

Attention:

Sample Number

43254 43255

43256 43257

43259

43260

43261 43262

Duplicates: 43254

Standards: Blank

CH-4

NicollAlO-J836 Multi-Element ICP-AES Analysis Aqua Regia Digestion

Ag ppm

AI As Ba Be Bi % ppm ppm ppm ppm

Ca Cd Co Cr Cu % ppm ppm ppm ppm

Fe Hg % ppm

K La % ppm

Mg Mn Mo Na Ni % ppm ppm % ppm

P Pb % ppm

SSbScSrTh % ppm ppm ppm ppm

Ti Tl U V W Zn % ppm ppm ppm ppm ppm p~

1.1

2.1

0.9 <0.2

0.6

1.84

1.65

1.24

0.63 1.16

<5

5 <5

<5

<5

0.3 1.40 <5

<0.2 0.41 <5 <0.2 0.55 <5

20 <0.5

23 <0.5

22 <0.5 29 <0.5

17 <0.5

<5 0.45

<5 0.80

<5 3.69

<5 0.79 <5 1.88

13 133

22 143

11 76

<1 6 8 55

15 <0.5 <5 1.57 6 50 37

18

30 <0.5 <5 5.03 11

15 <0.5 <5 4.49 9

160 811 11.90

34 3034 17.39

21 1169 10.88

3 48 2.18 17 417 11.45

<1 0.08 <10

<1 0.08 <10

<1 0.14 <10

<1 0.11 17

<1 0.08 <10

2.13 477

1.56 423

0.80 939

0.37 311 0.74 560

5 0.01 142

6 0.01 227

2 0.01 116

<2 0.04 4 2 0.02 84

0.049

0.026

0.036

0.015

0.028

17 5.74

17 7.51!

9 4.46 <2 0.38

8 4.96

<S

<S <5

<5

<5

3 4

3 1

2

31 426 9.88 <1 0.09 <10 0.78 504 3 0.02 58 0.035 7 3.69 <5 3 5 508 12.46 1 0.04 <10 0.28 881 <2 0.03

2 503 11.52 <1 0.06 <10 0.34 649 <2 0.03 43 0.054 2 4.55 <5 <1

24 0.053 <2 3.54 <5 <1

0.9 1.83 <5 20 <0.5 <5 0.45 13 131 155 839 12.00 <1 0.08 <10 2.07 464 5 0.01 141 0.049 14 5.71 <5 3

3

4

10

6 7

<5 0.07 <10 < 10 <5 0.06 <10 19

<5 0.06 <10 <10

<5 0.03 <10 <10

<S 0.05 <10 <10

8 <5 0.06 <10 <10 23 <5 0.01 <10 12

18 <5 0.01 <10 11

34 14 2050 48 16 2354

33 15 1191

5 <10 101 33 <10 155

36 <10 161 25 <10 82

21 <10 30

3 <5 0.07 <10 <10 33 14 2013

<0.2 <0.01 <5 <10 <0.5 <S <0.01 <1 <1 <1 <1 <0.01 <1 <0.01 <10 <0.01 <S <2 0.01 <1 <0.001 <2 <0.01 <5 <1 <1 <5 <0.01 <10 <10 <1 <10 <1

1.8 1.73 11 293 0.8 <S 0.59 2 30 107 2092 4.79 <1 1.38 13 1.20 330 2 0.05 53 0.064 15 0.54 <5 7 8 <5 0.19 <10 <10 82 <10 200

A .5 gm sample is digested with 5 ml 3:1 HCIIHN03 at 95°C for 2 hours and diluted to 25m!.

Page 1 of 1 Signed: ----------4..:.........6-·""'· f7L-.!:::.....---

• • • Assayers Canada 8282 Sherbrooke St, Vancouver, B.C, VSX 4R6 Report No OW2106PJ

c A N A D Tel: (604) 327-3436 Fax: (604) 327-3423 Date Aug-05-IO


Project

Attention:

Sample Number

43601

43602

43603

43604 43605

43606

43607

43608 43609

43611

43612

Duplicates. 43601

Starnt.rdSI Blank

CH·4

Nicol Multi-Element ICP-AES Analysis Aqua Regia Digestion

Ag ppm



Fe Hg % ppm

K La % ppm

Mg Mn Mo % ppm ppm

Na Ni % ppm

P Pb % ppm

S Sb Sc Sr Th % ppm ppm ppm ppm

Ti TI U VWZn % ppm ppm ppm ppm ppm pp'

1.4 1.06

2.0 0.10

1.6 0.36

0.5 0.18 1.5 2.06

10 19 <0.5 <5 0.78

5 12 <0.5 <5 0.47

7 13 <0.5 <S 0.74

6 <10 "0.5 <5 0.71 <5 52 <0.5 <5 0.45

0.3 1.03 <5 23 <0.5 <5 0.99

13 <0.5 <5 0.74 17 <0.5 <5 0.62

16 <0.5 <5 0.24 13 <0.5 <5 1.26

1.0 0.20 5 2.0 0.31 7 1.8 0.43 8

0.2 0.81 5

0.4 2.79 <5 20 <0.5 <S 2.46

1.1 1.06 9 19 <0.5 <5 0.78

4

12 18 11

11

23 50 327 6.84 < 1 0.12 < 10 0.46 469

19 2 1287 12.13 <1 0.01 <10 0.12 391 21 7 444 11.03 <1 0.03 <10 0.24 498

5 3 254 5.25 <1 0.01 <10 0.12 331

21 109 374 13.02 <1 0.41 <10 0.95 840

10 56 200 7.62 <1 0.13 <10 0.45 501 9 69 3 480 12.05 <1 0.01 <10 0.12 501

17 26 5 786 16.94 <1 0.01 ,,10 0.23 1096

20 128 4 180 14.25 <1 0.01 <10 0.27 831

6 12 29 133 1.63 <1 0.12 <10 0.40 553

18 0.01

3 0.01 2 0.01

2 0.01

<2 0.01

<2 0.01

<2 0.01

<2 0.01 2 <0.01

<2 0.02

18 0.005 88 2.70

33 0.005 472 5.61 28 0.008 5735 5.24

13 0.005 245 2.23

36 0.010 169 4.79

15 0.007 30 0.007

37 0.014

33 0.006 15 0.018

33 1.97 44 6.57

65 6.86

55 7.85 65 1.67

9 7

14 <1 14

5 <1

18 8

10 4 13 <1

22 <1

18 <1 9 1

1 13 93 168 9.62 <1 0.21 <10 1.51 1341 <2 0.02 41 0.039 17 1.66 11 4

4 23 50 l18 6.72 <1 0.12 <10 0.46 475 17 0.01 18 0.005 91 2.67 9

3 <5 0.05 <10 11 66 <10 157

1 <5 <0.01 <10 24 37 <10 963

3 <5 0.01 <10 21 33 30 2503

2 <5 <0.01 <10 <10 15 20 1666

2 <5 0.10 <10 29 125 12 1193

2 <5 0.04 <10 13

2 <s 0.01 <10 24 2 <5 0.01 <10 42

<5 0.01 <10 33 4 <s 0.04 <10 13

65 <10 386 31 <10 473

50 16 1579 53 34 2842

51 <10 435

9 <5 0.11 <10 19 78 <10 663

2 <S 0.04 <10 11 65 <10 166

<0.2 <0.01 <5 <10 <0.5 <5 <0.01 <1 <1 <1 <I <0.01 <1 <0.01 <10 <0.01 <5 <2 <0.01 <1 <0.001 <2 <0.01 <S <1 <1 <5 <0,01 <10 <10 <1 <10 <1 <

2.1 1.80 16 299 <0.5 "S 0.59 4 29 112 2029 4.66 <1 1.38 14 1.20 342 4 0.05 51 0.066 15 0.55 8 7 8 <S 0.20 <10 <10 89 <10 211

A .5 gm sample is digested with 5 ml 3:1 HCIIHN03 at 95°C for 2 hours and diluted to 25ml.

Signed: ---------~rJ1~~--Page 1 of 1

•

•

•

APPENDIX SECTION 5

NICOL GOLD PROPERTY ASSAY CERTIFICATES FROM SWASTIKA LABORATORIES LTD

FOR ALL CORE INTERVALS SAMPLED FOR DIAMOND DRILL HOLES 2010

Note: - Saw cut core interval samples were assayed primarily for Au, Ag as illus~rated in the list of results for the assayed intervals and within Appendix 4. In }Jddition, a limited number of selected saw cut core sample intervals were also ~§sayed for 30 Element ICP analyses as reported within following assay certificates .

• Swastika Laboratories Ltd

Lstablished J 92X Assaying - Consulting - Representation Page 1 of2

Assay Certificate Certificate Number: 10-1836

Company:

Project:

Attn:

Northstar Gold Corporation Nicol

George Pollock

We hereby certifY the following Assay of 48 core samples submitted 28-May-1 0 by George Pollock

Au Au Chk Au

Sample FA-AAS FA-AAS FA-GRAV Number g/Mt g/Mt g/Mt

43233 < 0.01 43234 < 0.01 43235 < 0.01 43236 0.01 43237 < 0.01

43238 < 0.01 43239 < 0.01

Report Date: 29-Jun-J 0

Au Chk Ag

FA-GRIW AR-AAS g/1~t ppm

0.2 0.2 0.2 0.5 0.4

0.2 0.2

.43240 0.01 0.4 43241 0.02 0.2 43242 0.02 0.03 0.2

43243 0.02 0.2 43244 0.01 0.2 43245 0.03 0.2 43246 0.03 0.2 43247 0.01 0.2

43248 0.02 0.2 43249 0.03 0.04 0.2 43250 < 0.01 0.6 43251 0.02 0.2 43252 0.02 0.2

43253 1 < 0.01 0.6 43254 0.04 1.6 43255 0.04 2.6 43256 0.02 1.3 43257 < 0.01 0.4

• Certified by 1. No Reject Den i s C hartre

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK lTD Telephone (705) 642-3244 Fax (705) 642-3300

Swastika Laboratories Ltd

• Lswl)lish~..J J92~ Assaying - Consulting - Representation Page 2 of2

Assay Certificate

Company:

Project:

Attn:

Northstar Gold Corporation

Nicol

George Pollock

We herehy certify the following Assay of 48 core samples

submitted 28-May-l 0 by George Pollock

Au Au Chk Au

Sample FA-AP.S FA-AAS FA-GRAV

Number g/Mt g/Mt g/Mt

43258 l. 80

43259 0.02

43260 0.01

43261 < 0.01

43262 0.01 0.02

43263 < 0.01

43264 < 0.01

Certificate Number: 10-1836

Report Date: 29-Jun-l0

Au Chk Ag

FA-GRAV AR-AAS

9 /tvlt ppm

l.2 0.8 0.6 0.7

0.2 0.3

.3265 < 0.01 0.3

43266 0.05 0.3

43267 < 0.01 0.2

43268 < 0.01 0.2

43269 < 0.01 0.3

43270 < 0.01 0.2

43271 0.07 0.2

43272 1 < 0.01 0.01 0.2

43273 < 0.01 0.2

43274 < 0.01 0.2

43275 < 0.01 0.2

43276 < 0.01 0.2

43277 < 0.01 0.2

43278 < 0.01 0.02 0.2

43279 < 0.01 0.2

43280 < 0.01 0.3

Blank Value < 0.01

OxF65 0.74

• Cerl (tied by /.' II ;/ ___ . ~~

1. No Reject Denis Chartre

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK no Telephone (705) 642-3244 Fax (705) 642-3300

• • Assaycrs Canada 8282 Sherbrooke St., Vancouver, B.c., V5X 4R6 Report No OWl836PJ

Tel: (604) 327-3436 Fax: (604) 327-3423 Date Jul-05-J 0


Project

Attention:

Sample Number

43254

43255

43256

43257

43259

43260

43261

43262

Duplicates:

43254

Standards:

Blank

CH-4

NicoUAlO-1836 Multi-Element ICP-AES Analysis Aqua Regia Digestion

Ag ppm



Fe Hg % ppm

K La % ppm

Mg Mn Mo Na Ni % ppm ppm % ppm

P Pb % ppm


Ti TI U V W Zn Zr % ppm ppm ppm ppm ppm ppm

1.1

2.1

0.9

<0.2

0.6

1.84

1.65

1.24

0.63

1.16

<5

5 <5

<5

<5

0.3 1.40 <5

<0.2 0.41 <5

<0.2 0.55 <5

20 <0.5

23 <0.5

22 <0.5

29 <0.5

17 <0.5

15 <0.5

30 <0.5

15 <0.5

<5

<5

<5

<5

<5

0.45

0.80

3.69

0.79

l.BB

<5 1.57

<5 5.03

<5 4.49

13 133

22 143

11 76

<1 6 B 55

6

11

9

SO 37

18

160 811 11.90

34 3034 17.39

21 1169 10.88

3 48 2.18

17 417 11.45

<1

<1

<1

<1

<1

0.08 <10

0.08 <10

0.14 <10

0.11 17

0.08 <10

2.13 477

1.56 423

0.80 939

0.37 311

0.74 560

31 426 9.88 < 1 0.09 < 10 0.78 504

5 508 12.46 0.04 <10 0.2B 881

2 503 11.52 <1 0.06 <10 0.34 649

0.9 1.83 <5 20 <0.5 <5 0.45 13 131 155 839 12.00 <1 0.08 <10 2.07 464

<0.2 <0.01

1.8 1.73

<5 <10 <0.5

11 293 0.8

<S <0.01

<5 0.59

<1

2

<1 <1 <1 <0.01

30 107 2092 4.79

<1 <0.01

<1 1.38

<10 <0.01

13 1.20

<5

330

5 0.01 142

6 0.01 227

2 0.01 116

<2 0.04 4

2 0.02 84

0.049

0.026

0.036

0.015

0.028

3 0.02

<2 0.03

<2 0.03

58 0.035

43 0.054

24 0.053

17

17

9

<2

8

5.74

7.58

4.46

0.38

4.96

7 3.69

2 4.55

<2 3.54

<5

<5

<5

<5

<5

3

4

3

1

2

<S 3

<S <1

<S <1

5 0.01 141 0.049 14 5.71 <5 3

<2 0.01

2 0.05

<1 <0.001

53 0.064

<2 <0.01

15 0.54

<5

<5

<1

7

3

4

10

6 7

8

23

18

<5

<5

<5

<5

<5

0.07 <10 <10

0.06 <10 19

0.06 <10 <10

0.03 <10 <10

0.05 <10 <10

<5 0.06 <10 <10

<5 0.01 <10 12

<5 0.01 <10 11

34 14 2050

48 16 2354

33 15 1191

5 <10 107

33 <10 155

36 <10 167

25 <10 82

21 <10 30

22

20

7

17

8

7

6

5

3 <5 0.07 <10 <10 33 14 2013 21

<1

8

<5 <0.01 <10 <10

<5 0.19 <10 <10

<1 <10

82 <10

<1

200

<1

10

A .5 gm sample is digested with 5 ml 3:1 HCIIHN03 at 95°C for 2 hours and diluted to 25m!.

Page 1 011 Signed: --~-------c;;$t---,y&-:..L' #--=----

•

•

•

Swastika Laboratories Ltd Assaying - Consulting - Representation Page 1 01'2


Company:

Project:

Attn:

Northstar Gold Corporation

Nicol

George Pollock

Report Date: 30-Jun-IO

We hereby certifY the following Assay of 48 core samples

submitted 28-May-l 0 by George Pollock

Sample Number

43281 43282 43283 43284 43285

13286 43287 43288 43289 43290

43291 43292 43293 43294 43295

43296 43297 43298 43299 43300

43301 43302

43303 43304 43305

1. No Reject

Au l\u Chk Au Au Chk Ag

FA-AAS FP-,-AAS FJl,-GRAV FA-GRAV AR-AAS

< <

< <

< <

< < < < <

< <

<

9 /t1t

0.01 0.01 8.47 0.14 0.04

0.01 0.01 0.01 0.01 0.01 <

0.01 0.01 0.01 0.01 0.01

0.01 0.01 0.02 0.02 0.01

0.01 0.02 0.03 0.17 0.01

g/Mt g/tlJt g/Mt ppm

0.2 0.2

0.14 0.2 0.2

0.2 0.2 0.2 0.2

0.01 0.2

0.2 0.3 0.3 0.4 0.3

0.2 0.2 0.5 0.2

0.03 0.2

0.2 0.2 0.2 0.2 0.2

Cerlifiedhy ~ J± Denis Chartre



Lslablished 19211 Assaying - Consulting - Representation Page 2 of2

Certificate Number: 10-1837 Assay Certificate

Company:

Project:

Attn:

Northstar Gold Corporation Nicol George Pollock

We herehy certify the following Assay of 48 core samples submitted 28-May-1 0 by George Pollock

Au Au Chk Au

Sample FA-AP,S FA-AAS FA-GRAV Number g/fvJt g/t1Jt g/Mt

43306 0.01 43307 0.01 43308 1. 80 43309 < 0.01 43310 < 0.01 < 0.01

43311 0.01 43312 < 0.01

Report Date: 30-Jun-J 0

Au Chk Ag FA-GRAV AE-AAS

g/Mt ppm

0.2 0.2

0.2 0.2

0.2 0.2

.43313 0.02 0.2 43314 < 0.01 0.2 43315 <

43316 43317 < 43318 < 43319 < 43320 <

43321 < 43322 < 43323 < 43324 < 43325 <

43326 < 43327 < 43328 1

Blank Value < OxF65

• 1. No Reject

0.01

0.02 0.01 0.01 0.01 0.01

0.01 0.01 0.01 0.01 0.01

0.01 0.01 0.01 0.01 0.76

< 0.01

0.03

Cerlijiedby D~ Denis Chartre

0.2

0.2 0.2 0.5 0.2 0.2

0.2 0.2 0.2 0.2 0.2

0.2 0.2 0.2


•

•

•

Swastika Laboratories Ltd Lstabiishcd J 92R Assaying - Consulting - Representation Page 1 of J

Assav Certificate Certificate Number: 10-1912

Company:

Project:

Attn:


George Pollock

We hereby cert!fY the following Assay of24 core samples submitted 31-May-l 0 by George Pollock

Au Au Chk Au Sample FA-AAS FA-AAS FA-GRAV Number g it-it giMt giMt

43329 < 0.01 43330 0.01 43]31 0.02 43332 0.02 43]3] 0.01

43]34 0.01 43335 0.02 43336 < 0.01 43337 0.01 43338 0.02 0.02

43339 < 0.01 43340 o .ll 4]341 < 0.01 43342 0.04 43343 < 0.01

43344 < 0.01 433'~ 5 < 0.01 43346 < 0.01 43347 < 0.01 43348 < 0.01 < 0.01

43349 < 0.01 43350 < 0.01 43351 < 0.01 43352 1. 80 Blank Value 0.01

Report Date: ll-Jun-J 0

Au Chk Ag FA-GRAV AR~AAS

giMt ppm

< 0.2 < 0.2 < 0.2

0.3 < 0.2

< 0.2 0.3 0.3

< 0.2 0.2

0.5 1.1

< 0.2 2.5 0.2

0.7 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2 0.2

< 0.2

Certified by D_~ ~ Denis Chartre

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK lTO Telephone (705) 642-3244 Fax (705) 642-3300


• btabllshcJ J 923 Assaying - Consulting - Representation Page 1 0[2

Certificate Number: 10-2058 Assay Certificate

Company:

Project:

Attn:


George Pollock

We herehy certifY the following Assay of 40 core samples submitted l1-Jun-l 0 by George Pollock

Au Au Chk Au Sample FA-AAS FA-AJl.S FA-GRAV Number g/t/lt g/Mt g/Mt

13353 0.02 43354 0.01 43355 0.02 43356 0.02 43357 < 0.01

43358 < 0.01 43359 0.02

Report Date:

Au Chk Ag FA-GRAV AR-AAS

g/Mt ppm

0.3 < 0.2

< 0.2 < 0.2 < 0.2

< 0.2 < 0.2

.43360 < 0.01 < 0.2 43361 0.02 0.3 43362 < 0.01 < 0.01 0.3

43363 0.02 0.6 43364 < 0.01 0.3 43365 0.02 0.8 43366 0.05 1.4 43367 0.01 0.3

43368 < 0.01 0.3 43369 0.01 0.3 43370 < 0.01 0.4 43371 0.01 0.3 43372 < 0.01 < 0.01 0.5

43373 0.02 0.2 1J337/J < 0.01 < 0.2 0375 0.02 0.3 43376 0.01 . 0.2 <~

43377 < 0.01 < 0.2

• 1. No Reject

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK 1 TO Telephone (705) 642-3244 Fax (705) 642-3300

lS-Jul-l0


• btab!ishc:d 102R Assaying - Consulting - Representation Page 2 of2

Certificate Number: 10-2058 Assav Certificate

Company:

Project:

Attn:


George Pollock

We herehy eerl(fj; the following Assay of 40 core samples

submitted Il-Jun-IO by George Pollock

Au Au Chk Au Sample FA-AAS FA-AAS FA-GRAV Number g/Ht g/Mt g/Ht

43378 1.73 L13379 < 0.01 43380 < 0.01 43381 < 0.01 43382 0.01 0.01

43383 < 0.01 tJ3384 1 0.14 0.13

.43385 0.01 43386 < 0.01 43387 0.02

43388 < 0.01 43389 0.01 43390 < 0.01 43391 0.01 43392 0.02 0.02

Blank Value < 0.01 OxF65 0.80

Report Date: lS-Jul-lO


g/Ht ppm

< 0.2 < 0.2 < 0.2 < 0.2

0.3 5.8

< 0.2 l.0 1.1

0.5 0.5 0.2 1.3 0.3

• 1. No Reject

Cerli/iedhy ~ ~0 Denis Chartre



• }';tahlishd 192X Assaying - Consulting - Representation Page I of2


Company:

Project:

Attn:


We hereby certifj' the following Assay of 40 core samples suhmitted Il-lun-IO by George Pollock

Au Au Chk Au Sample FJl,-AAS FA-JlAS FA-GRAV Number g/Mt 9 /t1t g/~lt

43393 0.01 43394 0.02 43395 0.02 4.3396 0.03 43397 0.01

43398 0.02 43399 0.01

Report Date:

Au Chk Ag FA-GPAV AR-MS

g/Mt ppm

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

0.2 0.2

.43400 0.01 < 0.2 43401 0.02 0.2 43402 1 < 0.01 < 0.01 < 0.2

43 LJ 03 8.62 43404 1. 26 1. 42 0.2 43405 0.02 < 0.2 43406 < 0.01 < 0.2 43407 0.15 < 0.2

43408 0.04 < 0.2 43409 0.01 < 0.2 43410 < 0.01 0.2 43411 0.01 < 0.2 43412 0.01 0.01 0.2

434U 0.01 < 0.2 43414 < 0.01 < 0.2 43415 0.01 < 0.2 LJ3416 0.01 < 0.2 43iJl7 < 0.01 < 0.2

• 1. No Reject

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK lTD Telephone (705) 642-3244 Fax (705) 642-3300

16-lul-IO


hlClbl:shcJ 192~{ Assaying - Consulting - Representation Page2of2


Company:

Project:

Attn:


We hereby certify the following Assay of 40 core samples

submitted 11-.Iun-1O by George Pollock

l".u Au Chk Au

Sample FA-AAS Fl".-AAS FA-GRAV Number g/Mt q /t1t g/Mt

13418 0.21 0.18 43419 0.01 43420 0.01 43421 0.02 43422 0.01

13423 < 0.01 43424 0.02

Report Date: 16-Jul-1O

Au Chk Ag

FA-GRAV A.R-!\A.S

g/Mt ppm

< 0.2

< 0.2

< 0.2

< 0.2

< 0.2

< 0.2

< 0.2

.43425 0.02 < 0.2 43426 0.03 < 0.2 43427 0.02 < 0.2

43428 1. 74

43429 <: 0.01 < 0.2 0430 < 0.01 < 0.2 43431 < 0.01 < 0.2 43432 < 0.01 <: 0.01 < 0.2

Blank Value < 0.01 OxF65 0.82

• 1. No Reject

(\ ' / /) Cer'!iied hy /J~Q./V'---L-:; C~~

Denis Chartre

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK lTO Telephone (70S) 642-3244 Fax (70S) 642-3300


• jstaiJiisilcd J92R Assaying - Consulting - Representation Page I of2


Company:

Project:

Attn:


George Pollock

We hereby certify the following Assay of 29 core samples submitted 11-.1 lln-l 0 by George Pollock

Sample Number

43433 43434 43435 43436 43437

43438 43439

•

43440 43441 1)]442

13443 43444 43445 4.3446 43447

43448 43449 43450 1)]451 43452

43453 43454 0455 43456 43457

1

1

1

1

Au FA-A]\.S

g/Mt

< 0.01

< 0.01 0.02 0.01 0.01

0.02 0.02 0.03 O. en

< 0.01

< 0.01 0.02 0.07 0.01

< 0.01

0.02 0.01 0.31 0.01 0.02

0.03 0.09 0.17 0.03

]\,u Chk Au FA-MS FA-GRAV

g/Mt g/tJ]t

< 0.01

0.51

8.55

0.13

Report Date: 16-Jlll-IO

Ag AR-]\AS

ppm

< 0.2

< 0.2

< 0.2 0.2

< 0.2

< 0.2 0.2

< 0.2 < 0.2 < 0.2

< 0.2 < 0.2 < 0.2

< 0.2

< 0.2

< 0.2 < 0.2 < 0.2

< 0.2 < 0.2

< 0.2 < 0.2

1.3 0.4

• 1. No Reject

(\ , !l ~/ Certified by )~~J-.:, C~k/ ~

Denis Chartre


•

•

•

Swastika Laboratories Ltd Assaying - Consulting - Representation

Assav Certificate

Page 2 of2


Company:

Project:

Attn:


George Pollock

We herehy eert itv the following Assay of 29 core samples

submitted 11-.Iun-l 0 by George Pollock

Au Au Chk Au Ag

Sample Number

[J:;,-AAS FA-J:;AS fA-GRIW AR-AAS

43458 43459 43460 43461 Blank Value

0;·;[65

g/Mt g/Mt g/Mt ppm

0.01 0.04

< 0.01 0.08

< 0.01

0.79

0.6 < 0.2 < 0.2

0.6

Report Date: 16-Jul-l0

C' 'f' I h {') ~ ;'0 j' ;)-" .er/llee y ~\. __ .t/t..~ L.~

1. No Reject Denis Chartre



htab!ished J92X Assaying - Consulting - Representation Page 1 of2


Company:

Project:

Attn:


George Pollock

We hereby cerl(!y the fo1\owing Assay of 40 core samples submitted Il-Jun-IO by George Pollock

Au Au Chk JI,u Sample FA-AI~S FA-JlAS FA-GRAV Number g/Mt g/Mt 9 /t'lt

13462 < 0.01 43463 0.04 43464 < 0.01 43465 < 0.01 43466 < 0.01

43467 < 0.01 43468 0.01

Report Date: 16-Jul-IO

Au Chk Ag FJI,-GRAV AR-AAS

g/Mt ppm

< 0.2 < 0.2

< 0.2 < 0.2

< 0.2

< 0.2 < 0.2

• 43469 0.06 0.03 < 0.2 43470 < 0.01 < 0.2 43471

43472 43473 43474 < 43475 43476

43477 43478 43479 43480 43481

43482 < 43483 < 43484 < 43485 < 43486

•

0.01

0.02 0.02 0.01 0.01 0.02

0.01 0.01 0.02 0.01

0.01 0.01 0.01 0.01 0.01

< 0.2

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2 < 0.2 < 0.2

3.94 4.52 13.4

< 0.2 < 0.2 < 0.2 < 0.2

0.2

(\ , 17 IJ ___ -Cerl(/ied by V'-~~ C~

Denis Chartre



• hUb!ishcd I ')2K Assaying - Consulting - Representation Page 2 of2


Company:

Project:

Attn:


George Pollock


submitted Il-Jun-l 0 by George Pollock

Au Au Chk Au Sample FA-J'.AS Fll.-AAS fA-GRl-\V Number g/tvlt g/lvJt g/Mt

43487 l. 78 43488 0.01 43489 < 0.01 43490 0.02 43491 0.01 0.01

43492 < 0.01 43493 < 0.01

Report Date:

Au Chk 1\g

FA-GRAV AR-AAS g/Mt ppm

< 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2

.43494 0.02 < 0.2 43495 < 0.01 < 0.2 43496 <

43497 43 /198

43499 43500 43501 <

Blank Value < OxF65

•

0.01

0.02 0.01 0.01 0.01 0.01 <

0.01 0.79

<

< < < <

0.01

Certified hy IO~ Denis Chartre

0.2

0.2 0.2 0.2 0.2 0.7


16-Ju\-10


• Assaying - Consulting - Representation Page 1 of2

Assav Certificate

Company:

Project:

Attn:


George Pollock


submitted ll-Jun-1 0 by George Pollock

jl,u Au Chk Au Chk

Sample L~-jlAS Fjl,-T-lAS FA-GRAV Number g/IY:t ]/L'Jt C; /i'1t

43502 < 0.01 43503 0.04 43504 0.04 43505 0.04 43506 0.05

43507 0.04 43508 0.02



Ag AR-AAS

ppm

< 0.2

< 0.2

< 0.2

< 0.2

< 0.2

< 0.2

< 0.2

.43509 0.02 < 0.2

43510 0.04 0.2

43511 0.10 0.09 0.3

43512 8.65 43513 0.02 < 0.2 43514 0.05 < 0.2 43515 0.02 < 0.2 43516 < 0.01 < 0.2

43517 0.02 < 0.2 43518 0.02 < 0.2 43519 0.02 < 0.2 <13520 0.02 < 0.2 43521 0.01 D.01 < 0.2

43522 0.02 0.4 43523 0.02 < 0.2 43524 < 0.01 < 0.2 43525 0.08 0.3 43526 0.02 < 0.2

• Certified by /J '~ to· t '-~~ Denis Chartre



blab!ished 1929 Assaying - Consulting - Representation Page 2 01'2


Company:

Project:

Attn:


George Pollock

We herehy cer/ifji the following Assay of 37 core samples submitted I1-Jun-l 0 by George Pollock

Au Au Chk Au Chk Sample FA-AAS FA-AAS FA-GRAV Number g/Mt g/Mt g/Mt

43527 0.01 43528 < 0.01 43529 0.02 43530 0.02 43531 < 0.01 0.02

43532 < 0.01 43533 < 0.01


Ag AR-AAS

ppm

< 0.2 0.3

< 0.2 < 0.2 < 0.2

< 0.2 < 0.2

• 43534 < 0.01 < 0.2 43535 < 0.01 < 0.2 43536 <

43537 43538 Blank Value < OxF65

•

0.01

1. 74

0.03 0.01 0.80

0.2

< 0.2

Cerlified by )J~ Denis Chartre



Assaying - Consulting - Representation Page 1 of2


Company:

Project:

Attn:


George Pollock

We hereby certifY the following Assay of 46 core samples submitted 14-Jun-l 0 by George Pollock

Au Au Chk Au Sample FA-AAS FA-AAS FA-GRIW Number g/Mt: 9 it'lt g/Mt

43539 .-:: 0.01 < 0.01 43540 < 0.01 43541 < 0.01 43542 < 0.01 43543 < 0.01 < 0.01

43544 < 0.01 43545 < 0.01

Report Date: 16-Jul-IO


g/11t ppm

< 0.2

< 0.2 < 0.2

< 0.2 0.3

< 0.2

< 0.2

• 43546 < 0.01 0.3 43547 0.01 0.6 43548 < 0.01 0.7

43549 0.01 0.3 43550 0.02 2.3 43551 0.02 1.8 43552 1 0.07 2.8 43553 0.02 1.4

43554 < 0.01 < 0.2 43555 0.01 < 0.2 43556 < 0.01 < 0.2 1)3557 < 0.01 < 0.2 43'j58 < 0.01 < 0.01 < 0.2

43559 < 0.01 .; 0.2 43560 < 0.01 < 0.2 43561 .-:: 0.01 < 0.2 43562 < 0.01 < 0.2 43563 .; 0.01 < 0.2

• Certified hy ):)~ 1. No Reject Denis Chartre



• L,lab!ished J 92x Assaying - Consulting - Representation Page 2 of2


Company:

Project:


Attn: George Pollock

We hereby cerlifj; the following Assay of 46 core samples submitted 14-Jun-l0 by George Pollock

Sample Numhpr

43564 43565 43566 43567 43568

43569 43570

•

43571 4357.2 43573

43574 43575 43576 43577 43578

43579 43580 43581 43582 43583

Blank Value OxF65 43584

Au FA-J1.AS

CJmt

< 0.01

< 0.01 <: 0.01

< 0.01

< 0.01 <: 0.01 < 0.01

0.01 <: 0.01

< 0.01 < 0.01

0.02 < 0.01

Au Chk

FA-AAS g/Mt

< 0.01

<: 0.01 < 0.01

< 0.01 0.01

< 0.01 < 0.01 < 0.01

< 0.01 0.79 1.76

Au FA-GRAV

g/['I1t

Au Chk

fA-GRAV g/Mt

8.52

Report Date:

Ag AR-AAS

ppm

< 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2

0.3 0.3 0.2

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2

< 0.2

< 0.2 <: 0.2 < 0.2

• (\ "' Cerl(fied by 0~~

1. No Reject Den i s C hartre


16-Jul-10

•

•

•

,-Swastika Laboratories Ltd

htablishcd J92~ Assaying - Consulting - Representation Page \ of2


Company:

Project:

Attn:


George Pollock

Report Date: 27-Ju\-lO

We hereby certifY the following Assay of 41 core samples

submitted 14-Jun-\O by George Pollock

Au Au Chk Au Au Chk Ag

Sample FA-AAS FA-AAS FA-GRAV FA-GRAV AR-AAS ~~tl:nbGr g/t-1t :1 /~/1t Ij /!'1t ,.. .... //1.1"--

''j / L"~ L i=')prn

43585 0.02 < 0.2 43586 0.02 < 0.2 43587 < 0.01 < 0.2 43588 < 0.01 < 0.2 43589 < 0.01 < 0.2

43590 < 0.01 < 0.2 43591 < 0.01 < 0.2 43592 < 0.01 < 0.2 43593 < 0.01 < 0.2 43594 < 0.01 < 0.01 < 0.2

43595 < 0.01 < 0.2 43596 < 0.01 < 0.2 43597 < 0.01 0.5 43598 0.01 0.7 43599 < 0.01 0.3

43600 < 0.01 < 0.2 43601 0.03 l.6 43602 0.04 l.6 43603 0.03 l.1 43604 0.02 0.03 0.5

43605 0.05 1.2 0606 0.01 < 0.2 43607 0.0,1 0.6 43608 0.09 1.0 43609 0.09 0.06 1.3

, ., ( '. -~ Certl/led by /~ ~ .

Denis Chartre




Certificate Number: 10-2106 Assaf Certificate

Company:

Project:

Attn:


George Pollock

We herehy cerlifjl the following Assay of 41 core samples submitted 14-Jul1-J 0 by George Pollock

Au Au Chk Au Sample FA-pAS FA-AAS FA-GR1W l\Jt...:.rnbcr g/t-lt g/l·'lt 9/ t·1t

43610 8.23 43611 0.03 43612 0.02 43613 <: 0.01 43614 < 0.01

43615 < 0.01 43616 0.02


Au Chk "'.g FA-GRAV AR-AAS

g/f~t ppm

0.2 0.5

< 0.2 < 0.2

< 0.2 < 0.2

.43617 0.01 < 0.2 43618 < 0.01 < 0.2 43619 < 0.01 < 0.2

43620 0.01 < 0.2 43621 0.02 0.3 43622 < 0.01 < 0.2 43623 0.02 < 0.2 43624 0.01 0.01 < 0.2

43625 <: 0.01 < 0.2 Blank Value <: 0.01 OxF65 0.79

• ('cr'ified hy

Denis Chartre


• • Assayers Canada 8282 Sherbrooke St., Vancouver, B.C., V5X 4R6 Report No OW2106P.J

Tel: (604) 327-3436 Fax: (604) 327-3423 Date Aug-05-IO


Project

Attention:

Sample Number

43601

43602

43603

43604

43605

43606

43607

43608

43609

43611

43612

Duplicates:

43601

standards:

Blank

CH-4

Nicol Multi-Element ICP-AES Analysis Aqua Regia Digestion

Ag ppm



Fe Hg % ppm

K La % ppm

Mg Mn Mo % ppm ppm

Na Ni % ppm

P Pb % ppm


Ti TI U V W Zn Zr % ppm ppm ppm ppm ppm ppm

1.4

2.0

1.6

O.S

1.5

1.06

0.10

0.36

0.18

2.06

0.3 1.03

1.0 0.20

2.0 0.31

1.8 0.43

0.2 0.81

10 19 <0.5

5 12 <O.S

7 13 <0.5

6 <10 <0.5

<5 52 <0.5

<5

5

7

8 5

23 <0.5

13 <0.5

17 <0.5

16 <0.5

13 <0.5

<s <5

<5

<S

<5

0.78

0.47

0.74

0.71

0.45

<5 0.99

<5 0.74

<5 0.62

<5 0.24

<5 1.26

4 2:l

12 19

18' 21

11

11 27

10

9 6'1

17 26

20 128

6 12

50 327 6.84

2 1287 12.13

7 444 11.03

254 5.25

109 374 13.02

56 200 7.62

3 480 12.05

5 786 16.94

4 780 14.25

29 133 7.63

<1

<1

<1

<1

<1

<1

<1

<1

<1

<1

0.12 < 10

0.01 <10

0.03 <10

0.01 <10

0.47 <10

0.13 < 10

0.01 <10

0.01 < 10

0.01 <10

0.12 <10

0.46 469

0.12 391

0.24 498

0.12 337

0.95 840

0.45 501

0.12 501

0.23 1096

0.27 831

0.40 553

18

3 2

2

<2

0.01

0.01

0.01

0.01

0.01

<2 0.01

<2 0.01

<2 0.01

2 <0.01

<2 0.02

18

33

28

13 36

15

30

37

33 15

0.005 88

0.005 472

0.008 5735

0.005 245

0.010 169

0.007

0.007

0.014

0.006

0.01l!

33

44

65

55

65

2.70

5.61

5.24

2.23

4.79

1.97

6.57

6.86

7.85

1.67

14

14

18

10

13

22

18

9

0.4 2.79 <5 20 <0.5 <5 2.46 7 13 93 168 9.62 <1 0.21 <10 1.51 1347 <2 0.02 41 0.039 17 1.66 13

1.1 1.06 9 19 <0.5 <5 0.78 4 23 50 318 6.72 <1 0.12 <10 0.46 475 17 0.01 18 O.OOS 91 2.67

<0.2 <0.01 <5 <10 <0.5

2.1 1.80 16 299 <0.5

<5 <0.01 <1 <1 <1 <1 <0.01

<S 0.59 4 29 ll2 2029 4.66

<1 <0.01 <10 <0.01 <5

<1 1.38 14 1.20 342

<2 <0.01

4 0.05

< 1 <0.001 <2 <0.01

51 0.066 15 0.55

9

<5

8

<1

<1

8

4

<1

<1

<1

4

7

<1

2

2

2

2

2

4

<5 0.05 <10

<5 <0.01 <10

<5 0.01 <10

<5 <0.01 <10

<5 0.10 <10

<5

<5

<5

<5

<5

0.04 <10

0.01 <10

0.01 <10

0.01 <10

0.04 <10

11 66 <10 157

24 37 <10 963

21 33 30 2503

<10 15 20 1666

29 125 12 1193

13 24

42

33

13

65 <10 386

31 <10 473

SO 16 1579

53 34 2842

51 <10 435

9 <S 0.11 <10 19 78 <10 663

<1

8

<S 0.04 <10 11 65 <10 166

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

<5 0.20 <10 <10 89 <10 211

3

6

3 6

8

8

4

<1

14

A .5 gm sample is digested with 5 ml 3:1 HCI/HN03 at 95°C for 2 hours and diluted to 25m!.

Signed: _____ ~d6___¥_--Page 1 of 1


hlablishcd J92X Assaying - Consulting - Representation Page I 0[2


Company:

Project:

Attn:


Report Date:

We hereby cert(/j; the following Assay of 41 core samples submitted 14-Jun-l 0 by George Pollock

Au

Sample FA-AAS

Number g/Mt

43626 < 0.01 43627 < 0.01 43628 < 0.01 43629 < 0.01 43630 < 0.01

43631 < 0.01 43632 < 0.01

Au Chk Au Au Chk Ag

FA-AAS FA-GRAV Fl\-CRAV AR-AAS

g/Mt g/Mt g/Mt ppm

< 0.01

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

20-Jul-l0

.43633 < 43634

0.01 0.01

< 0.2

< 0.2 < 0.2 < 0.2

43635

43636 < 43637 < 43638 < 43639 < 43640

43641 43642 < 43643 < 43644 < 43645 <

43646 < 43647 < 436,18 < 43649 < 43650

•

8.55

0.01 0.01 0.01 0.01 0.01

0.02 0.01 0.01 0.01 0.01

0.01 0.01 0.01 0.01 0.05

< 0.01

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

(" 'f' Ih )(1 . . crtl le( Y ... ~'_JL/1/,-J.--o

Denis Chartre



• htdb! ishcd J 92X Assaying - Consulting - Representation Page 2 of2


Company:

Project:


Attn: George Pollock

We hereby certify the tollowing Assay of 41 core samples submitted 14-J un-l 0 by George Pollock

Au Au Chk l:Cu

Sample FA-AAS FA-AAS FA-GRAV Number g/ lVlt 9 /~lt g/Mt

43651 0.07 43652 0.11 t13653 0.08 43654 < 0.01 43655 < 0.01 < 0.01

43656 < 0.01 43657 < 0.01

Report Date:

Au Chk Ag Fi\-GRAV AR-AAS

t]/Mt rpm

< 0.2

< 0.2 < 0.2

< 0.2

< 0.2

< 0.2 < 0.2

.L13658 < 0.01 0.2 43659 < 0.01 < 0.2 43660 1. 81

43661 < 0.01 < 0.2 43662 < 0.01 < 0.2 43663 < 0.01 < 0.2 43664 < 0.01 < 0.2 43665 < 0.01 < 0.01 < 0.2

43666 < 0.01 < 0.2 Blank Value < 0.01 OzF65 0.76

• i,\ Certified hy i-'~v--V'--'L-:7

Denis Chartre


20-Jul-l0


• Assaying - Consulting - Representation Page 1 of2

Assay Certificate

Company:

Project:

Attn:


George Pollock

We hereby cerli/j; the following Assay of 45 core samples submitted 16-Jun-lO by George Pollock

Au p,u Chk Au

Sample FA-AAS FA-pAS FA-GRAV Number 'j/Lv1t g/Mt g/Mt

43667 < 0.01 43668 < 0.01 43669 < 0.01 43670 0.03 43671 < 0.01

43672 < 0.01 43673 < 0.01 < 0.01


Report Date: 29-Jul-10


q/W ppm

0.2 0.2 0.2 0.2 0.2

0.2 0.2

.43674 < 0.01 0.2 43675 0.07 0.2 43676

4]677 < 43678 < 43679 4]680 < 4]681 <

4]682 43683 <:

43684 <:

43685 43686 <

43687 < 43688 4.3689 4]690 < 43691 <

•

0.02

0.01 0.01 0.03 0.01 0.01

0.01 0.01 0.01 0.14 o. ell <

0.01 0.02 0.02 0.01 0.01

0.02 0.4

0.2 0.2 0.2 0.2 0.2

0.2 0.2 0.2 2.1

0.01 0.8

1.5 1.3 0.5 0.2 0.2

Cerlifiedby A~ ~ Denis Chartre




Assal' Certificate Certificate Number: 10-2181

Company:

Project:

Attn:


We herehy eertifj; the following Assay of45 core samples submitted J6-Jun-l 0 by George Pollock

Au Au Chk Au Sample FA-AAS FA-AAS FA-GRAV Number ,]/[vJt q/Mt g/Mt

43692 8.75 43693 0.05 43694 < 0.01 43695 < 0.01 43696 < 0.01 < 0.01

43697 < 0.01 43698 0.02


Au Chk Ag FA-GRAV P-.R-AAS

9 /~/lt ppm

0.3 0.2 0.2 0.2

0.2 0.3

.43699 < 0.01 0.2 43700 0.01 0.2 43701 0.01 0.2

,1]702 < 0.01 0.2 43703 < 0.01 0.2 43704 < 0.01 0.2 0705 < 0.01 0.2 i137 0 6 < 0.01 < 0.01 0.2

43707 < 0.01 0.2 ,13708 0.01 0.2 43709 0.01 0.2 43710 1. 62 '-1]747 <: 0.01 0.2

Blank Value < 0.01 O:.;F65 0.75

• Cl'I"tijil'd by

Denis Charlre


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