OPAP FINAL SUBMISSION KENOGAMING TOWNSHIP PROPERTY

Transcription

1 42A04NW KENOGAMING ^ * J. i er OPAP FINAL SUBMISSION KENOGAMING TOWNSHIP PROPERTY J SALO JANUARY 199

2 OPAP 9721 INDEX 1. General Location Map 2. Township Location Map. Location 4. Access. Access Map 6. Previous history 7. Regional Geology S. Property Geology g.project 10. East Side of Akweska Lake 11. West Side of Akweska Lake 12. Magnetometer Survey 1. Drill Log 14. Drill Section 1. Assays 16. Daily Logs and Expenses 17. OPAP forms 16. Sample and Traverses Map 42A04NW KENOGAMING 010C

3 .Map KENORA LAKE OF WOODS "V. \LAKE Property location j^juj TERRACE M ^'S Q X too ZOO SCALEi:tOOOO FIGUREI

4 wfc^.s^ rv '.~. r 1 r fs^^^rf^/f fe^ Fig. 2 Township and Property Location Map Kenogaming

5 LOCATION The ^encgaming Township Property consists of 7 unpatented mining claims. Tney are located in K,enogaming Township (claim map (29), MNR Administrative District of Timmins, Porcupine Mining Division and the jurisdiction of the Sudbury Lands Title Offices, The longitude and latitude are 61 4', 46 11' and cover a large portion of Akeweskwa Lake. Claim Number Unit: O

6 ACCESS The Kenogaming Township Property is located in Kenogaming Township approximately 4 km southwest of Timmins. Access is via highway 101, km west of Timmins past Opishing Lake to Kenogaming Road then S km south on the road. A series of secondary cottage roads and trails provide good weather access to the property. As claims are on Akweska Lake a float plane can also be used.

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8 PREVIOUS HISTORY Although several companies have worked in the Kenogaming Area, only one has actually performed work on the claim block. That being Texas Gulf Inc. in They put in place three drill holes (which may or may not be) on the property. The three ho es totaled 69 feet of!ex drilling. They are located on old claim number P.2711, which is the northwesterly boundary of ths property. No casings or signs of drilling have been found. The drill logs report disseminated pyrite, choicopyrite and magnetite but do not report the assays. The files in the Timmins resident geologists office show that files T9S (Falconbridge Ltd.), T1 (Texas Gulf Inc.), T2726 (Morin Prop.) and T27 (Norunda Mines Ltd.) have performed work around the claim blocks but not directly on them. ODM Report 9997 "The Geology of the KukatushSeweli Lake Area, District of Sudbury" by V.G. Milne, details Kenogaming Township, but again very little on the property itself. As part of an OPAP grant, Mr. E. Mord did a VLFEM16 survey on the easterly part of the claims. In 1996 l performed line cutting and a magnetometer survey over the original 1 unit claim, with some grab sample assays.

9 REGIONAL GEOLOGY The property lies within the eastern part of the Swayze Greenstone Belt, located in the Superior Province of the Canadian Shield. The Belt is of Archean and forms a lenticular eastwest trending Tectonic stratigraphic sequence composed predominantly of greenschist facies metavolcanics, subvolcanics and m eta sedimentary rocks with coeval ultramfic and flesic intrusions. The Belt is bounded to the north and south t?y Archeangneissic and medisedimentary rocks. An explanation of the General Geology of the Swayze Greenstone belt from OGS Report 297 Precambrian Geology 'Northern Swayze Greenstone Belt' by J.A.Ayer, is enclosed and explains the lithological units for the area.

10 General Geology The northern Swayze greenstone belt (NSGB) is locat ed within the western Abitibi Subprovince of the Superior Province. The Abitibi Subprovince is a Neoarchean granitoidgreenstone terrane that devel oped between 2.8 and 2.6 Ga (Jackson and Fyon 1991). The NSGB is bounded by the Kapuskasing Structural Zone to the west, the Nat River granitoid complex to the north, and the Kenogamissi batholith to the east. A narrow septum of metavolcanic and metasedimentary rocks wrapping around the northern margin of the Kenogamissi batholith provides continu ity of the supracrustal rocks with those of the Abitibi greenstone belt to the east. Although largely separated from rocks of the Abitibi greenstone belt (AGE) by the Kenogamissi batholith, the 2 greenstone belts are con sidered to be roughly equivalent in age, based on the general similarity of lithological assemblage types and the limited UPb zircon ages determined to date in the Swayze greenstone belt (Jackson and Fyon 1991; Heather and van Breemen 1994). With the exception of Proterozoic diabase dikes, all bedrock in the study area is Archean. The oldest rocks appear to be the paragneiss and amphibole gneiss units of the Kapuskasing Structural Zone, located west of the Ivanhoe Lake cataclastic zone. They are pan of a sedi mentaryvolcanic succession that was intruded by the Shawmere anorthosite complex, which predates 276 Ma (Percival and Krogh 198). Both the Shawmere anorthosite and the gneissic units are intruded by grani toid gneiss. Rock units and structures generally trend northeast, and dip moderately to the northwest. East of the Kapuskasing Structural Zone, the rocks of the Swayze greenstone belt and associated intrusions are younger in age, typical of the southern Abitibi Subprovince (Jackson and Fyon 1991). Within the supracrustal sequences, the rock units and structural fea tures generally trend easterly with steep dips. Supracrustal rocks have been metamorphosed to green schist facies, with the exception of areas in close proximity to the granide intrusions which are of amphibolite facies. All the Archean rocks have been metamorphosed to some extent and for the sake of brevity, the prefix "meta" will be assumed in the rock nomenclature used throughout this report. The chronological order and stratigraphy of the area is as yet poorly understood, as there are only precise iso topic age determinations on a few of the intrusions in the NSGB. A program of UPb geochronological investiga tion is in progress which should soon provide more age data (Heather and van Breemen 1994) and thus a better framework for the stratigraphy. Jackson and Fyon (1991) subdivided the supracrustal rocks within the map area into assemblages (see Figure 2): 1) MuskegoReeves assemblage (MRA) 2) Horwood assemblage (HWA) ) Hanrahan assemblage (HNA) l l Granitic

11 NORTHERN SW,WZE GREENSTONE BELT Jackson et al. (1994) define supracrustal assemblages as regional map units that contain rocks sharing some, but not all, of the following properties: lithic attributes, geochemistry, facies association, geophysical signature, structural style and age. The units contained within an assemblage need not be stratigraphically related, and an assemblage may either be in fault or depositional contact with other assemblages. The MRA is confined to the northern part of the belt and is composed of tholeiitic mafic volcanic rocks with lesser components of komatiitic ultramafic volcanic rocks, calcalkalic intermediate and felsic volcanic units, and clastic and chemical sedimentary units. The HWA extends south of the synoptic area into the central part of the Swayze greenstone belt. It consists predominantly of tholeiitic mafic volcanic rocks, with minor intercalations of finegrained clastic and chemical sedimentary rocks, calcalkalic felsic pyroclastic rocks and komatiitic ultramafic flows. The HNA is confined to the southeastern part of the N'SGB and consists predominantly of calcalkalic intermediate and felsic volcanic rocks that have been intruded by extensive ultramafic and gabbroic sills. A lat erally extensive, but relatively thin, unit of iron formation caps the HNA and delineates much of the boundary between the HNA and the MRA. Table l is a presentation of the main rock units within the synoptic area. These units are discussed in more detail below. ARCHEAN Ultramafic Metavolcanic Rocks Previous mapping in the synoptic area took place prior to the general recognition of the existence of ultramafic extrusive rocks and thus all ultramafic rocks were classi fied as intrusions (e.g., Prest 191; Milne 1972; Breaks 1978). However, current mapping has shown many of these ultramafic units to be of extrusive origin. The close spatial relationship of the komatiite flows (unit l, Map 2627, back pocket) with massive, mediumgrained cumulatetextured serpentinite bodies of more enigmatic origin (unit 7, Map 2627, back pocket) suggests a eogenetic rela tionship which is not as yet fully understood. Komatiitic ultramafic flows (unit l. Map 2627, back pocket) represent an estimated ' rc of the MRA, IVo of the HWA and were not observed within the HNA. A number of these units in the MRA are laterally extensive. The most extensive unit occurs in Penhorwood and eastern Keith townships, with dimensions of about 1 km (length) by up to l km (width). In central Keith Township, a number of lenticular units l to 2 km!ong appear to lie along the same stratigraphic horizon, suggesting the lenticular morphology might represent basinal areas of komatiite accumulation separated by areas of higher paleorelief without komatiite deposition. This observation is supported by the common Table 1. Lithologic units for the northern Swayze greenstone belt. ' PHANEROZOIC CENOZOIC QUATERNARY PLEISTOCENE AND RECENT Glacial, glaciofluvial, lacustrine and fluvial deposits PRECAMBRIAN PROTEROZOIC Mafic Intrusive Rocks Diabase dikes Unconformity ARCHEAN Alkalic Mafic Intrusive Rocks Lamprophyre dikes Late Felsic to Mafic Plutonic Intrusive Rocks Granodiorite, quartz monzodiorite, granite, tonalite, quartz diorite, gabbro, clinopyroxenite, pegmatite, porphyry, felsite Early Felsic to Mafic Plutonic Intrusive Rocks Tonalite, quartz diorite, granodiorite, quartz monzodiorite, granite, diorite, gabbro, porphyry, felsite Metamorphosed Mafic Intrusive Rocks Gabbro, melagabbro. leucogabbro, diorite, anorthosite, anorthosite gabbro Metamorphosed Ultramafic Cumulate Rocks Dunite, peridotite, pyroxenite Chemical Metasedimentary Rocks Magnetite iron formation, siderite iron formation, sulphide iron formation, graphitic mudstone, chert Clastic Metasedimentary Rocks Sandstone, siltstone, mudstone, conglomerate, tuffaceous wacke, paragneiss Felsic Metavolcanic Rocks Tuff, lapilli tuff, tuff breccia, massive flow, brecciated flow Intermediate Metavolcanic Rocks Tuff, lapilli tuff, tuff breccia, pillowed flow, massive flow, amygdaloidal flow, brecciated flow Mafic Metavolcanic Rocks Massive flow, pillowed flow, variolitic flow, amygdaloidal flow, brecciated flow, plagioclasephyric flow, pyroxenespinifextextured flow, tuff, lapilli tuff, tuff breccia Ultramafic Metavolcanic Rocks Massive flow, spinifextextured flow, polyhedraljointed flow, brecciated flow

12 PROPERTY GEOLOGY Geology map 221 Penhorwood and kenogaming Townships show the property divided into three main geological areas. The central part being granite. The west side of the property is felsic to intermediate volcanics with feisic tuffs. This is divided with a central band of early mafic intrusive rocks with actinc'.itic hornblendic amphibolite. There are several outcrops throughout the area. The west side of trie property is also show as felsic to intermediate voicasnics. The geology map also shows two nickel showings, one on the western claim and one on the eastern claim. ODM preliminary map P 46, Kenogaming Township, also shows the nickel showing. The eastern claim block has encompassed an area which shows to have a 4 onductor airborne anomaly. OGS Report 297 Precambrian Geolcgy'Northern Swayze Greenstone Belt' by J. A. Ayer Has a description of the Akweskwa Lake showing just south westerly claim.

13 OCS REPORT 297 copper and zinc were not reported. Detailed surface exam ination of the occurrence reported in Thurston et al. (1977) indicates that the iron formation consists of alternating layers of quartz, sulphides, magnetite and amphibole. Locally they contain minor intercalations of what may be finegrained, metamorphosed lithic sandstone. The unit has been intruded by pink, mediumgrained porphyritic granite and bluegrey quartz diorite. NICKEL AND PLATINUM GROUP ELEMENTS Nickel occurrences are closely associated with the cumulatetextured ultramafic rocks, mostly within the Hanrahan assemblage (HNA). The presence of large ultramafic bodies, some of which have documented nickel mineralization, is an indication that there may be good potential for komatiitehosted nickel deposits similar to those found in the Timmins area and the Kambalda area of Australia (Lesher 1989). In addition, locally elevated platinum group ele ment levels in assay results are also of exploration interest. Akweskwa Lake (1) There may be some confusion about the location of this showing in Kenogaming Township, as the area is under lain by numerous ultramafic bodies, a number of which have associated nickel mineralization. A grab sample taken at this location is reported to have assay values of 17o Cu and Q.9% Ni (Milne 1972). In 197, Hanna Mining con ducted a regional survey and sampled ultramafic rocks over much of Kenogaming Township. The highest returned assay value in this immediate area was only Q.0% Ni. Fumerton and Houle (199) report a massive, fine to mediumgrained, highly serpentinized peridotite with about 2"7c disseminated sulphides at the indicated area of mineralization, but could not find any evidence of channel sampling. Grab samples collected by Fumerton and Houle (199) returned values of up to Q.28% Ni and D.1% Cu. Amax Minerals Limited (2) Amax minerals conducted a magnetic and EM survey in 1978 that was followed up by a diamonddrill hole in 1979, in northeastern Kenogaming Township. Drill logs report assay values of up to Q.2% Ni over m within a carbonatized and serpentinized ultramafic unit containing talc and chlorite bands. International Norvalie (1) In 1971, Norvalie Mines Limited optioned the Jonsmith property in eastcentral Kenogaming Township and dia mond drilled a number of holes in this area, east of the occurrence. One of the holes returned a value of Q.26% Ni over m of serpentinized ultramafic rock containing l to 29fc disseminated and fracturefilled pyrrhotite and pyrite. Another hole, located further to the north, intersected an 18 m zone with copper mineralization in a unit identified as a grey banded tuff. The mineralization consists of chal copyrite stringers which returned anomalous values of up to Q.2% Cu. Ireland (14) The Ireland occurrence is located in northern Kenogaming Township. It was discovered by Timmins Nickel Incorporated in 1989 and explored in 1990 by stripping, trenching and diamond drilling. The showing consists of cumulatetextured dunites differentiating into melagabbro, isoclinally interfolded with magnetitechert iron formation and felsic tuffs of the underlying HNA. Mineralization consists of l to 2*2? disseminated sulphides which locally form a poorly developed net texture containing up to 10*^ sulphides. The sulphides consist of pyrrhotite and minor amounts of pentlandite. Late fractures are also mineralized with pentlandite. Grab samples returned assay values of up to Q.94% Ni, Q.10% Cu, 0.27 g/t Pt and 0.2 g/t Pd. Geochemical analyses of the ultramafic rocks in the vicin ity of the mineralization show REE patterns that are dis tinctively different than those of similar, but unmineralized, ultramafic rocks in the same unit to the northeast. The slightly elevated LREE patterns in the rock hosting the mineralization suggest that contamination of the ultra mafic magmas may be the mechanism responsible for localizing the sulphides and platinum group element min eralization (see "Geochemistry"). Mcintyre Johnson (22) The Mcintyre Johnson occurrence lies in poorly exposed, amphibolitefacies mafic metavolcanic rocks in the eastcentral part of Sewell Township. Mcintyre Porcupine Mines Limited carried out geophysical surveys followed by diamond drilling in The mineralization is reported as millerite which occurs in aggregates and along joint surfaces within a differentiated mafic intrusion. Reported assay values are up to Q.2% Ni over 2. m within peridotite. Norduna (27) The Norduna occurrence is located within a cumulatetextured ultramafic body within the HNA, in central Kenogaming Township. There has been considerable exploration work on this occurrence since its discovery in This work has included geophysical surveys, strip ping, trenching and diamond drilling, with the most recent work by Falconbridge Limited. The mineralization con sists of up to 9fc disseminated sulphides in serpentinized ultramafic rocks that are in close proximity to the sheared contact with intermediate fragmental rocks to the south. The best reported intersection was Q.88% Ni and Q.16% Cu over 7.6 m, including a 1. m section with 1.2*6 Ni and Q.24% Cu. 2

14 SALO CLAIM GROUP, KtiMCGAMING TOWNSHIP MAP 221 l Coiojrsd csological Map

15 PROJECT PROPOSAL AND CHANGES The proposal for this CPAP program was to do grass roots prospecting, including plugger work, sampling, assaying, line cutting, magnetometer survey, slit sampling, and aeoloa\cs\ j ' i ~ *.j.j After traversing the claims, not as many outcrops were visible as expected. Those found wers blasted and sampled, some assays were sent from these samples The line cutting and magnetometer sur/ey was also performed on the area of the airborne anomaly. A drill hole of 94' was also put into place to test the mag anomaly. The maps and results are contained herein.

16 : PT ds DAILY LOG Log of Isengoaming Township Property July 1th Line cut LO ^rom O 6+OOE July 17th Line cut BLO 6+QOE to Line &+00E to the north July 19th Line cut line 7E north and 6E north July 20th Line cut line SE north and line E north July 22nd Line cut Line 4E north and E north July 24th Line cut E north and 2E north July 20th Line cut 1E north and O north July 27th Line cut O north and O eouth Aug 14th Line cut!e south and 2E south Aug 16th Line cut 2E south and E south Aug 17th Line cut 4E south and E eouth Aug 19th Line cut E south and 6E south Aug 2rd Line cut 7E south and SE south Aug 24th Line cut &E south and chained all lines JoeAnne and Larry JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and Larry Larry Larry Larry Larry Larry Larry Larry Larry Larry Larry Larry Larry Aug 26th Magnetometer survey Aug 2#th Magnetometer survey Aug 29th mapping magnetometer data JoeAnne JoeAnne JoeAnne Aug 0th traverses on east side Aug 1et traverses on eaet side Sept 2nd traverses on east side Sept 4th traverses on east side ept 6th traverses on west side Sept 7th traverses on west side Sept 9th traverses on west Side Sept 11th travereee on weet side Sept 1th traverses on west side Sept 14th plugger work and blasting Sept 16th plugger work and blasting Sept l&th plugger work and Wasting Sept 20th plugger work and blasting JoeAnne and Larry JoeAnne and Larry JoeAn ne and Larry JoeAnne and Larry JoeAnneand Larry JoeAnne and Larry JoeAnne and Larry JoeAnne and Larry JoeAnne and Larry JoeAnne and Larry JoeAnne and Larry JoeAnne and Larry JoeAnne and Larry 69IZ S9S OIDNt)1d SZ:6T NOW 8 6 t' l d S

17 69 T 2 90: Ft ds Sept 21st plugger work and blasting Sept 2rd plugger work and blasting Sept 2th plugger work and blasting JoeAnne and tarry JoeAnne and Larry JoeAnne and Larry Sept 27th sampling Sept 29th sampling Sept 1st sampling Get 2nd sampling Oct 4th sampling Oct 6th sampling Oct 7th sampling Oct 27th mapping samples JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne and JoeAnne Larry Larry Larry Larry Larry Larry Larry Dec 7th mobilization of drill Dec 6th mobilization of supplies Dec 9th drilling overburden Dec 10th drilling Dsc 11th drilling Dec 12th drilling Dec 1th drilling Dec 14th demobilization of supplies Dec 1th demobilization of drill Larry and Larry and Larry and Larry and Larry and Larry and Larry and Larry and Larry and Denis Denis Denis Denis Denis Denis Denis Denis Denis Dec 17th logging core Harold Dec 18th splitting core Dec 19th splitilng core Dec 20th samples taken to Swastika Eero Eero JoeAnne Jan drill sections and report JoeAnne Jan 24 making copies of report and maps JoeAnne 69 T Z 92 0 i. oidnw~id NOW

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23 EAST SIDE OF ASKWEKWA LAKE For the period of July 1th to August 24th, a line grid was put in place.on claim The lines total.4 km at 10O meter spacings with 2 meter stations. A magnetometer survey was done on this grid on August 26th and 26th. Traverses were done over claim O and claim 1219O71 over a period of nine days. Although the geology maps shows an outcrop on the east side of , it could not be found. Only one outcrop was found during these traverses. It is located between L1E and L2E and +0N. It appears to be an altered volcanic with visible arseno pyrite. After blasting sample 7769 was sent for multi element assays, (see Intertek Testing report for results). After completing the west side of the lake, it was determined that not enough outcrop existed on the property an a drill hole was put into place on Line tooe at 1+2N to test the anomaly found during the mag survey. See drill section for results.

24 WEST SIPE OF AKWESKA LAKE The west side of Akweskwa Lake was also traversed using the 1996 line grid. A total of 16 km was covered, on claims 12O9S1 and A 'total of fourteen outcrops were located. Due to the terrain in some places it was difficult to tell if it was one of two outcrops. The outcrops were blasted and sampled, some sent for assays. On claim some old working were found. This Included an old drill site and some trenching. The trenches were also blasted and of all the outcrop looked the most promising for nickel. The following is a description of the outcrops. ( map for locations and numbers) 771L0W2H0N fine grained, weakly foliated (amphibolite, mafic metavolcanic) chloritic. 772 L11W +60 moderatestrongly talccarb, altered Intermediate metavolcanic (pyroclastic*) surface rind of rusty umoxite iron carbonate 77 L10W1+OON finer grained version of sample 7766, this rock appears to be somewhat more altered than sample some very minor rusty spots noted Fe/Fe carb. 774 L&+2W 4+2 Quartz eyed gabbro Assayed for Au Pt Pd Cu Ni se Intertek Testing report for results

25 77 L7+7W +0 rhyolite, gabbro with rust folded and striking SO degreed EW dipping 90 degrees Assayed for multielements see Intertek Testing report for reults. 776 L6+0W +0 Sheared gabbro old drill hole Assayed for Au Pt Pd Cu Ni see Intertek Report for results. 777 L6+OW 6+0 calcite in altered volcanics, mineralized gabbro striking EW dip of 90 degrees Assayed for multi elements see Intertek Testing report for results. 776 L6+0W 6+0 pinkish quartz veining in granitized gabbro visible arseno pyrite Assayed for Au Pt Pd Cu Ni see Intertek Testing report for results. 779 L6+OW 6+OS mineralized gabbro Assayed for multi elements see Intertek Testing report for results. 776O L7+0W 9+27 quartz phorphry Assayed for Au Pt Pd Cu Ni see Intertek Testing report for results L6+20W 9+27 altered metavolcanics Assayed for multi elements see Intertek Testing report for results. NOTE #776#7761 are from the area of the old trenches. 7762HOW 1+0N maficintermediate weakly foliated amphibolite minor rusting noted on some surfaces (amphibolized mafic metavolcanic)

26 776 L11W 1+2N moderatewell foliated, mediumcoarse grained talc altered intermediate feldspar porphyry with some brown rusting L10W 2+00 N gabbro diabase (possibly glomero porphyritic diabase) 776 L12W 4+OON intermediate feldspar porphyry same as L12WU2N weakly foliated medium to coarse grained feldspar porphyry with abundant 2007a evaedral white grey feldspar phenocrysts set within a visibly chloriticsericitic altered ground mass (general fairly fresh looking) 7767 L12W 6+2N weakly foliated maficintermediate metavolcanic (pyroclastic) trace pyrite 776g.L4W 2+20 granite

27 MAGNETOMETER SURVEY Discussion This magnetometer survey shows activity in the north east quarter of the survey area and that the remaining area is relatively flat. Using a McPhar Proton Magnetometer, the grid was trasversed in loops, checking back with a base station located at LO L4E. The diurinal drift was accounted for based on time durations and number of readings. Line E seems to be the center of the 4 channel air born anomaly. The map was drafted using 000 gammas as the O point and everything was either above or below (below indicated by Q),

28 PRILL LOG ~4 7"

29 ivy I Northern ueveiopment Dtveioppement du Nord nmi.. fnrnnp an \Vj and Mines et des Mines Drilling lorage 8 LI omano Log diamant Drilling Company Compagnia de lorage Diamond Journal de Complete this form and CoHai Elevation Elevation du collier Date Hole Started Data Completed Date Logged Data da commencement du foraga Data d'achevement Data d'inscription au journal Exploration Co.. Owner or Optionee Compagnie d'axploration, proprietaire ou titulaire d'option Dale Submitted Data da depot Bearmg of hort trom true North/Position du forage 9*1 (oppofl au nofd vrai Logged by,,. Inscrit par ^/pou Total Footage Dip ol Hole at ' Avancement total du Inclinatson du forage au """"24 *" "^ Collar/collier FlJPi L**L^ * Submitted by (Signatu ) FtJPi rdepose par (signature ) ' : FI /Pi o related sketch In duplicate. Fill in on every page Hole No ^ Page No. Remplir en deux exemplalret li Remplir ces cases a W "rafle " a9" n presente formule et le croquls annex* chaque page r J \/ ^)/ l Address/Location where core stored Adrasse/endroit od la carone esl siockee Map Reference No. N4 de reference sur la carte Claim No. N0 de concession miniere Location (Twp. Lot, Con. or Lat. and Long.) Emplacement (canton, lot, concession, ou latitude et longitude) fro /t M21N/ Property Name Nom de la propriety d Footage/Avancement From/De O.oi To/A ~:~i ' Rock Type Type de roche.j^'klc, Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometric, texture mineraux, transformation, etc.) "v^et^ci^'a.^.s^r^t^ ^.TO'D^f^,',.^ ' ^ : FI /Pi PwnvNlltu* You Sampt* No Fwugtt'UvvM/ N* d'tcnvttiuon duprortpacuur MwmwU d* I'lclunLllofl (m DMdil From/D* To/A SnpK Login Assays I/Analyses mineralurgiques ^,,1K ^C/ii/nil Hiri 'K. 7 'o 77'"70 11'" i 07 J* 1 *\r^~em:t?p l/jtt r\y O' 1 ten:!/' ' : f./ \Ji?L'' ^'V I'o'v;. 'jltfuiilafit ftr^.ve. r 'f f..^ V^iiF ^ :^.. ^ ir.. C ' ' Tn\Jt '7D /'. /CT.ni;!.tA'V'r^, hvuv.'i i /i"".v,'^p if 1 v"'!i 't ^, TCcn ; ip^ /.'J.r^iOi? ro''1"^, '^/Lr' 1 ' ^; '"t 1 ^/' ]J.' 'V/1 1: n ^; ll'j^ UV'ILLO :X irr' ^','t.ona^x 'I 1"" ''/Li.^ "" ' 'ferj^. 1.1 i j j.! T ^, i ' '. ;'., i; ' i..,. ' j ^ ;N j. f' ^ (o.'k trfk ATI '^)hi'"'. ; F / VVOit /'J'S^'J' K', :..'i.';. ~..^ /vo i.'r,t(~^.y\, ; ' ') ' ; ri' ;.. ' /"i, ' ^ 4; ffi j... ^f^cl'^c.^^ pf'...: \ ^i /C*N! x* foo 'jv^lm'.:' "1'^ r!") pi x r: o,'/ rt'., 7 i.r rt L. HOJTXTl'JAjL }Jifx gfcoiri 'k:if,'/ CTT.0,",., irr,^ 'Pjr'tofr", " orlr^t'. ^.N ^.. ^^,. ;'.. V^ 7. Tiir ^i^e O'j m\ in) t fi.'t.v " 7 ''.,. PACJC cii2t/ K'lA'r ' ^ ' L'l: i'tt 1 lv'.' ^' ^i 1. v/rr^uia 4o l/"' /t l r/.'."/.r. "' ' ' i." ;. " 1 '^ P?"* "I. ^^ "777 77/V 777^ f 777 /^P( ^2J ^^ ^^^ ts 777 * U 47 0 /^!4 40 A Ay 47 &G /7 fe ~ ^ i. ' * For features such as foliation, bedding, schistosity, measured from the long axis of the core. Examples de caracteristiques : foliation, schistosity, stratification. L'angle est mesure par rapport i I'axe longitudinal de la carotte. t Additional credit available. See Assessment Work Regulation. t Des credits supplementaires son! offerts. Consulter les reglements relatits aux Iravaux devaluation. Nota : Dans cette formule, iorsqu'll designe des personnas, le masculin est utilise au sens nautra.

30 ' Complete this form md IWI Northern Development Developpement du Nord nriii:nn foraae au related sketch in duplicate. Vi; and Mine, e, des Mines ^'"'"9 ^ RempHr en deux exemp,.,.. l. """"lu "*a presente lormule et le croquls annexe brilling Company Cornpagnie da forage Collar Elevation Elevation du collier Beanng of hola from trua Total Footage Dip of Hole at North/Position du foraga Avancement total du Inclinaison du forage au a Address/Location where cora stored Adressa/endroit ou la carotta est stockae par rapport au nord vrai forage Collar/CMIwr Data Hole Sianed foraga Data Completed Data d'achevement Data Logged Logged by Data d'inacription au Inscrit par. " journal FI./PJ * Exploration Co.. Owner or Optionee Compagnie d'exploralion. proprietaire ou titulaira d'option Data Submitted Submitted by (Signature),,pl Fl./Pll Fill in on every page Hole NO. Page No. Remplircescasesa k For"e "' "^'"' chaque page r /B Map Reference No. Claim No. N* da reference sur la carte N* de concession miniere Location (Twp. Lot, Con. or Lat. and Long.) Emplacement (canton, lot, concession, ou latitude et longitude) Property Name Nom de la proprieta Footage/Avancement From/De To/A Rock Type Type de roche Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometric, texture, mineraux, transformation, etc.) ^ \ C**..' r l ^'^ f i ' TT O ' ' ' / ' " f " r ' ' '" ' ~ *i ' ' : i ^ r j r ~ *i '. t~ \. '. ; " r ~ ~:,;.' M,.1' : c "i ^ '. ' ^'' ~ r.'r.'~" : ' t: ; ''.i r.^ : 'T.; "? r.fi ' ^.: K" i', y 7 fvvpo TKpt:^itT7.i'N rrc 'DC''Oi. "."'; e.,; r :f^' r,;i r^'.'e1^,7 'ro rf'c '.TjCes. r'.i'i^ ~~') ' f"c c. M fiiurp LO iru M^v^'Ni? re :' c.'ce'}^ ^"^ H'i'^'t^. ^! ^0(^4 91 TT ruv. (Z',' ^A.'^'^S *JfeQ.VJrl^;. ^i'7 TTiyPv ^rj,0'^' 'c inito^t MifiPo / t;. ATV ^ ')'f.j,,'t'. (",,y,i,..^^ ^v'r' 4 tt, fr' ^'c rri/r^c rt'.j'.tlt^ tc.; ": ' ^'" ".''' '..) ; t'. 1.' I 1 ''.. ' ^D, C)'c"ri! L FIVPI.~ K"i *r^ p~ Your SMTlpM No. N* d'tehanhllon du prmpfcttur S*mp** Footagt/NrvMu d* pr* l*vwn*ni dt I'tchantiHon (w Dwdst From/Da To/A Sonpl* Ungft Longuwr d* I'MwiMlon Assays t /Analyses mineralurgiques VJ, fhu: V.rrr'^L '^ :r r ' ijl'e.tt f ;V'.P 'c "~T ^ :.v.i,;.,' i \i ''.^o " ' ' ; t'x t 1 ".."r r,. L.'iiTt;.tS^. }'2'^ 'tcyv,: /i'no^c.r'.,!. 1 (Y.^v ;. ^c MoS"./ros: L'jL.0^: A'r"rc. : ).)^ f, Cf' ' '' ')r \'..' ^..... ; j.j.. ^ "'^O )/ ' 'i') ''J '. xlrr'".' ^L. "r'c ^o' " 'i''') V' N; ^ ''^'^l t'.'r^':o "^ O'lr. ^ /C,C.Ji.'l ; C.l ^ "' :''" '",1 " r 1 ' B'pi. n ViT vfol^u) S ^k *s*\jx ^* ^ ) ^ ^ ^ ' '. ' f*l l ~\ "^ y ^Lc ( y ~ ',\ 'Ci f" "*..j i^. ^. C"^ i~ ' f i~f\^ C? i *^^ ~ N (' ' v ' S'lrT1 J (~ J J " j "Tl (f *" r" V l "^ j ^^^ V^ 1 ' ' *" S" 7; L'.VrCll^^ J'tr'r ' V ~, \ ^ 1 V "i: '". L'.\ V, i For features such as foliation, bedding, schistosity, measured from the long axis of the core. Examples de caracteristiques : foliation, schistosity, stratification. L'angle est mesure par rapport a I'axe longitudinal de la carotte. t Additional credit available. See Assessment Work Regulation. t Des credits supplementaires son! offerts. Consulter les r6glements relatifs aux travaux devaluation. Nota : Dana catta formula, loraqu'il daaigna das peraonnaa, le maaculin eat utiliae au una naulra.

31 Ministry of Ministere du Diamond Journal de Complete this form and Northern Development Developpement du Nord fjr ng forage au related sketch In duplicate. Fill In on every page and Mines et des Mines H dlamant Remplir en deux exemplaire* la Remplir ces cases A Ontario uog presente tormule et le croquia annexe chaque page Drilling Company Compagnia de forage Collar Elevation Elevation du collier Data Hole Started Data Completed Dale Logged Data de commencement du forage Dale d'acnavement Date description au journal Exploration Co.. Owner or Optionee Compagnia d'exploratlon. praprietaire ou litulalre d'optkm Date Submitted Dale de depot Bearing ut hole from inn Total Footage Dip of Hole at 0 Nonh/Position du forage Avancement total du Inclinaison du forage au Adresse/endroit ou la carotte est stockee par rapport au nord vrai forage Collar/cotlier Logged by " Inscrit par FUPi 0 Submitted by (Signature) ~,,D, Hole No. ^ Forage n* r Page No. Page n0 Map Reference No. Claim No. N* de reference sur la carte N9 de concession mmiere Location (Twp. Lot, Con. or Lat and Long.) Emplacement (canton, lot, concession, ou latitude et longitude) FUPI Property Name Norn de la propriete Footage/Avancement From/Da To/A Rock Type Type de roche Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometric, texture, mineraux, transformation, etc.) ' T. :~? '. ' ' :. ' " ;. T'^O'jyCi *^ Tr'. X:. r.v.iciro':. ' ^ i'.o'.'jv'../'. \ ' ).~r "; oft^c T'~' ] "i"^'"^ti)v\t,, fv..:yxot^ ;.;... 'ir'i'l.c.'l,/''?.1 " V' f ^ p,!,'./ i 'ftf,,'' ^ :zt. s w fr&p:,' \ rr'o'j'/aiv'o ^ '.tcp^o" ri T Srti/W'r.a! 'J T; A.IV^ "frt fc if. Of C. f V1 ZV V MS u c 'J's P^P. r ' ' Tot : i )T v 1 4. va 0 v\! "f '*; Of S1 L V f 1 ^L l" uiid^, i'jcec.'.': ^'/q :oipt cruus..vfev^' 'o /Of?i.x C 'J' f.^c'k. ilstr'i'.oi j.t /. '^ee/.'v.,? 1 '; ^'.,'": ~ ; ' ': "'. T^t f'.'j. rc Ft./Pi Plm* FNkm AnfflAAVi ON 11 ;.~. FwMgiT'Un*** ItNdiManMM (*~ Your Sampto No. Svnplt FoptugMNtvHu M pr* UvwntxH da l'*cri*nwton (an oitds) aurxospw.u From/0* TOA Longueur df I'fchantillM) Assays f/ Analyses mineralurgiques ^. Z'^^V' r " A i *','t O J ^ t. ' ', ; ' " 'j 'i.'ii; ~y ' ; '!,^y^c.'^~. /^"^ ; ' " t 'iii ' ^ic ^,'fc.ps ^ v ^'!^ /'''^c'c^ ALO /..o'' r,h^ '^r; T' '.. /^v ^i^.rvr HA/^. p s J f ^ ^^ M 'ii? ' ' "* f A i P 1 V C* ^ ) / ^, \J t ^ l O U t. ^ ' l' ". *' ^ ' "t V. jl t "t. ^' ', " " ^ * *1 s. \ f''~" ^ "^. x f * f~~ *. ^ i i ^^? i **x^ J ' r' ' *C f i ' ^1 A^V^~, 'i.x ' ~ ' i '..rfr'.osr.'mcc.u/ ^fi.y* r?.^ ;[^ Fl' r/, rhee^ ^CAL. vet^'.'.irj*rtos OV^I ''pp.rj;'^ ruin s H 0 &U.OT 'X ^^oomd 'Op ""^ cr^e ikttrlt V '(2pfS^tr'T O?1 For features such as foliation, bedding, schistosity, measured from the long axis of the core. Exemples de caracteristiques : foliation, schistosity, stratification. L'angle est mesure par rapport a Taxa longitudinal de la carotte. ^ ^ tt4l ^ k^n. *^ y ^ ^ t Additional credit available. See Assessment Work Regulation. t Des credits supplemental son! otferts. Consulter les reglements relatifs aux travaux devaluation. Nota : Dans cette formule, lorsqu'll dasigna des personnes. le masculin ast utilise au sens neutre.

32 Ministry of Ministere du Diamond Journal d6 Complete thl* form and Northern Development Developpement du Nord nrillinn foratje i U related sketch In duplicate. Fill in on every page Hole No. Page No. and Mines et des Mines UMIHIIIJ a Forage n* Page n* Rempllr en deux exemplaire* la Remplir ces cases a ^ Ontario Log diaman presente formula et le croquls annexe chaque page r Drilling Company Campagna de forage Collar Elevation Elevation du collier Date Hole Started Date Completed Date Logged Dale de commencement du forage Date d'achavement Dale description au journal Exploration Co.. Owner or Optionee Compagnie d'axploratkm, proprielaire ou titulaire d'option Date Submitted Date de depot Baarino of hole Irom true Total Footage Dip of Hole at 0 Nonh/Posttion du loraga Avancament total du Inclinaison du forage au par rapport au nord vrai forage Logged by Inscrit par Submitted by (Signature) Collar/collier FUPi Fl,PI FL/Pi j ' 0 Address/Location where core stored Adresse/endroit oil la carotte est stockee Map Reference No. N0 de reference sur la carte Claim No. N* de concession miniere Location (Twp. Lot, Con. or Lat. and Long.) Emplacement (canton, lot, concession, ou latitude et longitude) Property Name Nom de la propriety Footage/Avancement From/De To/A Hock Type Type de roche Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometric, texture, mineraux. transformation, etc.) FtVPi Cd*Sp*omtn Your Sample No. N* d'khamiikw du prospkttur Svnpit FooU9tf NivMu M pr* Ffom/Di To/A SvnpkLirani LonguMr o* l'*ch*iijjon Assays t/ Analyses mineralurgiques.. '..16;. r :?^? "O ' ^.' y.) ri :r. f.l r'v ;f^'., C~)^t ^ t,.1 ' ( i. ^ 'JJ'T^ ::V':. 0 ^S7 )." dttfccr^ti^ f.('.vtt.'.. ^A/'VO /I'ra'n::^ ^ fecvurrvb ^'.T'prric^o "V^ p^it Jr.tRi.e re.'' c/.vee^d. A;^ ^,;' ". v t..'s )':)(^ lr r\i; T~XJ.TV" ' ^''^"/ibb MM ^o \'2.Q t~ ^ "fc&m D ^T f '^D* l^t^t "t. T') "J/"* ~ Co * ^. 't N 'A i?'v t. ^ ^C'P piici*^.'^ *L^ ^ N! 'Til.i^^' jp'j"i ^ ^ CTT7 1)N^ ;y7'j t'\',' 0 ^^'.70^', i^.^ ; : '^ " '^.r^jd 9~ /^ )^\cptttv T'J) \'tf?^, 1 T O'.' o "Tt LC tutct:4\^ 1 0)74. w.. L'.T^.r,.^' /^ov. ''.^.' A/v/.j rtt. ro^ll ^ufo'2.r ir:trr;'";/'^ /./^:VI^L v.'e':. i^'^"' Cio'''?A^:D jr ^TV.' ^rtr'i.0 ' " 1 ' " ^t,^c*.'~* "'t',* 9^ A 'T7 '.? *. O j.) '"1' ' ~ '^.'1.' \ t ")O'^ ^''' "r: ^ ' ' '. V ": ^ ' ' '' '.". ^' :;^.: O^;:M /M"^i^ '^''; ^ r ; r ; ; \ ^ j^(i ^ t " ' ;. o' ^ :, f " : ^ ' 2t ' '. ~ i ' c.'^ ' ^ ' *: ii"'is. ^tc1, "S A Vcrt'.' :TCO^'^. I I '^''' ' "r! y,': ec.tio^ ^o^rr.oot&jl.v/ rv2ok.) tpfov 11** i*rr" ^' *For features such as foliation, bedding, schistosity, measured from the long axis of the core. Examples de caracteristiques : foliation, schistosity stratification. L'angle est mesuri par rapport a I'axe longitudinal de la carotte. i p 10 * f.okvn 7^77 77^ ^*^^ '77SC 77 ^ f 77^2 77^ )Ms /: 77^ 77?6 itn //Q f'~fcl ^ J^ 17 IT* w /zy ID (/f, X? 7 y^9 /2? f?0 r^ ^ m /fy X#4 /^7 Pit T x.^9 /7/ ^* "? ivcui ^ ^. D 1::' ~) ~'' rt,. Nl07 ;r). t Additional credit available. See Assessment Work Regulation. t Des credits supplemental sonl offerts. Consulter les reglements relatifs aux travaux d'evalualion. Nota : Dans cene formula, lorsqu'il deaigne daa parsonnas, la masculin ast utilisa au sans neutra.

33 Ministry of Ministere du Diamond Journal de Complete this form and Northern Development Developpement du Nord Drilling forage U r*l"*d *l"tch In duplicate. Fill in on every page and Mines et des Mines a diamant Remplir en deux exemplalres la Hemplir ces cases a k 0 nlano LO9 presente formule et le croquia annexe chaque page r Dhlling Company Collar Elevation Searing ol Mole horn true Total Footage Dip ol Hole at " Compagni* d* lorag* Elevation du collier North/Position du forage Avancement total du Inclinaison du (orage au par rapport au nord vrai forage Address/Location where core stored Adresse/endroit ou la carone est stocfcee Map Reference No. N* de reference sur la carte Hole No. Forage n" Page No. Page na Claim No. N" de concession miniere CoUsr/collw Dal* Hoi* Started Date Completed Date Logged Logged by " Data d* commanconwu du forag* Date d'achevement Date description au Inscrit par journal FI /p, Exploration Co., Owner or Option** Coimpagni* d'txptoration, proprietor* ou titulair* d'option Oat* Submitted Submitted by (Signature),,p, 0 Location (Twp. Lot, Con. or ut. and Long.) Emplacement (canton, tot, concession, ou latitude et longitude) Ft/PI 0 Property Name Nom de la propriete Footage/Avancement From/De To/A Rock Type Type de roche X to.)'*;? r^ip^ y? l ' Tr"f JC.TI ON'^x.. ;iiv~^o /\'*v 1^0 "0 i.ou^st ^IN^ yr~ Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur. granulometric, texture, mineraux, transformation, etc.) c.'v ' ' cri, '^ 'v/tgp'. r.v.nv^tl ro r'.'. ^..('. :f.,^^:^ ^(.^ "ji:'.'a'fc'" ^f"1 TU^L jllte^vo^ ^1 ao ion a ' ' I&: ^ r...' ' 1) viic,... 'c^j! :e FI./PI '.^'^ '. 'W "'. TUis ''Sivi omc C*T Trx't C.S'&C'JrO T^fV' M^!fTili.L ^ Vi ' ' i M^\)c i s* DLLS 9 "j M t. pr" *i;^ P;tJt 'ci..'\ c."vc ^ C*. " "Hifc ^LT^sUK 1 AT'.N/fj AJ^&'fiSU} t^i^ct? ^.^ /' /o PC" TT t. r i, livito.:^^ TCL.L /.Ut Ei.^j.0. ' ^ "^ '" ~ v^ P ^ ; ' ^/ '.. ' I'W F^f;if*ed LO^.^lA^i 'frot ',ft i C,TO~) ')VT f^t r 'AT* f Cv' ^"^ '0~CSf, T^ '^ ^" : OC' l C! '..'^',.f : r ''rt" 'ih",tc. r; TUc i'.i;r^^' ;' V'D.' ( r von '. oj^''' z\'^''"" ^';.r.'r:") BlCtlly 0^ TC.U tae^ttt'..!. tilfmim TlfC 61^0^ rtk; ^v Hfcs seoj rnc'.rtfv,,njrilitd ^v~ For features such as foliation, bedding, schistosity, measured from the long axis of the core. Examples de caracteristiques : foliation, schistosity, stratification. L'angle est mesur* par rapport l I'axa longitudinal de la carotte. Plan* F**jw* AngNrAnqM OM pmml "i? Vf?.' i.' ' * FgaupT'LjnpjM ^, ^" Your Sampto No, dupro9pm*ur 7/Jfe 77?7 77^ 7/W 779D 7~fl/ 77^7 77^ ^r^ 22^21 ^^^ C70T ^C'VxD?ns'^ 'X f.r;:(ci"\ ' r',;..r:' fjiro: ICM' CO 'rodift t''t f '.;.^' i.'^'c n( 'v:.' '.. r.1 / ^lo1"^'" ;','Jt^ceTXM^! ;.(i Ni!fr2iii., Oy,:ee ^ ': prr' t^'ro.':.t^ c.^o^r'' : i ii" " Te n/^.1^^:'; X..OT ~';. t'., t''..^ O,. "' ; u, 7.1/^1.^;s. 1^ 77*26 Tfik 77^7 7/9^ f(9t) itteafc? Sanpt* FooiagdifiwMU d* prt From/Da )Cj j jcf^ 7^ /Q~7 f ^}f\f ^i\*rj ^?o /^x 07 C9 AH dl A\to ^ ^A 6 ro/a '/q q j96 /tj /9Q AGf 6 S)/*^ **it'^) 0~7 ) ^.^9 ^K/ 4) 1 /t? ^ Cj.^ ^ asfr S*mpl* Ltngtti Longueur M I'lchantiUon.2. J Q 2. a * ^ ^ c? Assays t/analyses mineralurgiques t Additional credit available. See Assessment Work Regulation. t Des credits supplementaires son) offerts. Consuller les reglemenls relatifs aux travaux devaluation. Nota : Dans can* formula, lorsqu'il design* des personnel, l* masculin *st ulilisa au Mnt rautra.

34 Ministry of Ministere du Diamond Journal Qe Complete this form and Northern Development Developpemem du Nord... (nronn )U related sketch In duplicate. Fill in on every page and Mines et des Mines Drilling forage, Rernpllr en deux exemplaires la Rempiir ces cases 4 ^ ontano Log diaman present* formule et le croquls annexe chaque page r Drilling Company Compagni* d* loraga Collar Elevation Elevation du collier Data HoK Started Dal* Completed Date Logged Gat* d* commencement du forage Data d'achevemenl Date description au journal Exploration Co., Owner or Optionee Compagni* ^'exploration, propnelair* ou titulair* d'opllon Dal* Submitted Date de depot Bearing of hole from true Total Footage Dip of Hole at * North/Position du forage Avancement total du Inclinaison du forage au par rapport au nord vrai forage. Coilv/colliar Logged by * Insert! par Ft./Pi o Submitted by (Signature) Fl m. Address/Location where core stored Adrasse/endroit ou la carotte est stockee Map Reference No. N0 de reference sur la cane Hole No. Page No. Forage n0 Page n* Claim No. N" de concession miniere Location (Twp. Lot, Con. or Ut. and Long.) Emplacement (canton, lot, concession, ou latitude et longitude) Ft /Pi a Property Name Nom de la prophet* Footage/Avancement From/De To/A iot vba 00 Rock Type Type de roche i PiSS' 9 ^ow.tofc 7.,^.^ J^maz/Aoi/irpc ^jfoa^ifo 7 M^T^VO^NJlZ. Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometric, texture, mineraux, transformation, etc.) igpeoinj^rsd pc ' /T\T'^ TA'r p'^ /.l/ 1 ),':;c fe?cku 'cmpl^ctd ' OM'i rfc.": ''rr ' ')^'''i Srit^t^P f. "Vcoj.^ ''Ke, AL!vtix err io 0TDi. ^^/ ' : O* " J~~ t~ Co'.itL '/\)~f^fc /j'~!'^j.c i ' S ' ' '"v.j n"' r ' ' *^ i ' ^ "* ' ' f~~ *j. ^ ^, 2x?4 or ff NJf\/ ^in'oji O'^. CJ'.r^, FI /Pi rco^'i'.'l :,C', :"^' IO/ B/ '.' 'LO)^, ^ '..'! ;c J /. r 'CO,.';oUxC SrC" 'feeer J" ^0.''!:^. 'fr..^. "... (.v ' ilo:. ' ; f,, ;.^fi. i.t rv.:^..^ /' c^s. '.^n'l. 1 t'm^ '.NTOt'./^L i'.cn ';0'^)f..' v c: M::M 0^ 's.^r^cp :^..^' :.T^ r,..r..;l ^^1' ue ^ "^ '"" i"* u l' c^r/'' i * ' ' ** * ' ^ "^ ^ * ' " ' ' ' T v '"^ l ' /' * '* ^ 'C* ' 'T ^ ' ~ r y r " i t j \f \ ^ ^X.^ i v V', 7 ' ^,"11.^^ ' r V^." v ^o^r^.es 'M^nj'MTO "Lt'L hfc s /, ^ [.! c ^O Vl L 1; ' V( /i '/Tti^ td, ^O^fei^VVtii, i rf o? ;:J1 C^'/ iev'i'or^d, G^ ^ffl^^to Px M^CK; 'p JJf ' '/^'.''j. 1 \CjC4^!j\j^i?.0 S.\"^O ' "r 1.^'.,^ U^/r 6^e/ cex/^m."7* 1 '.\h"c ^csril r^fi^nt^tj:. C*lcM(NliquiM utnm ConSptoMn IMaMM Jfc76 CT1 kcyffi Your Sampta No, N* d'tetwhiuon du prttpkuur o^ ^b9 ^I0f76 ^71 ^07J2 d&yft M14 wyfc ( Xx *i ^fissw SiO^gD ^0"?/ Ai^a. ^0^ ^10 ^ oia^ From/ D* y{ y( o ^I ^/ ^4 Q1 'MO SA'Z SAk ^SL *^?*.itft A(PLI flk'i Z7D ~7?y A~fa 27H TO* ^j?a "? dg 4 4L? 4^ o^6 i^ss" Ak( AM Zk7 JCfo Z7 Q*~7/ t\ / L# ZTd 2^( * SimpK Lmrh Longueur n I'ichanliuan Samp** Footag.VNfv.Mu (M pf* JO*fr*""c ^^ i O ^ s*.. Assays t 'Analyses mineralurgiques 0204 (oyai) *For features such as foliation, bedding, schistosity, measured from the long axis of the core. t Additional credit available. See Assessment Work Regulation. Exemples de caracterlstlques : foliation, schistosity, stratification. L'angle est mesure par rapport a I'axe longitudinal de la carotte. t DBS credits supplememalres son) offerts. Consulter las reglements relatifs aux travaux devaluation. Nota : Dans cene formule, lorsqu'll designe des peraonnes, le masculin est utilise au sens neutre.

35 Ministry of Ministers du Diamond Journal de Complete this form and evoluppomonl du Nuiu1 Drilling forage au related sketch In duplicate. Fill in on every page Hole No. ^ Page No. \2/ and Mines e t des Mines dlamant Rempllr en deux exemplalrea la Remplir ces cases a k Foraao "' f*^"' Ontario a presents formula at le croqula annexe chaque page r i rilling Company Compagnia da forage Data Hole Started Data de commencement du forage Data Completed Data d'achevemenl Exploration Co., Owner or Optionee Compagnie d'exploration. proprielalre ou titulaira d'opton Footage/Avancement From/De To/A "SyO ^ ) ~ 0 Rock Type Type de roche!j!jpa*iat'c l^tm^v't.. Collar Elevation Elevation du collier Date Logged Date d'inscnption au journal Data Submitted Data de depot Beanng of hole from true Total Footage Dip of Hole al e Nonrt/Position du forage Avancement total du Inclinatson du forage au par rapport au nord vrai forage Logged by Intent par Submined by (Signature) Collar/coilisr Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometry, texture, mineraux, transformation, etc.) ' ' ''' i.e.1,c'^l~ PW 'f.*j. J 1."' "i * ~M [.'^.T' ^' ' F ox: '.'fi r^cv"'^ 1 /.' " C'. " ^ t. f. ''D '^L'ilnlCA' (^ 7o'Tti±± ^^ '' i V.e/'.OfcJi. ~Ht.r* /i' : f I':',^ v'i.fcieo^ i ^ v '. ":,j. i LliL't'f't ' ~.'^.'*'1 Jf ' ~) 1'^, rs )"~ Vu." I'UtO:, fjfit A r r Vs* j^w ^f'.rv T7 G : /ij. e oo* 1 ' ^ r ^(L CTCI v/,^ : c^j ' ii ^ ^ ' u ' ' '\ ;. r not anvf!it,'(x, /i f t t:'.'^fa'^c 1^fc ; r..jr"i ^.o ^T; C fe^ ' "tt~r C^r L^it Lv/i '"j'' 'Vt.^? r!f\:j!'. C,1/' 'tr,jfjr.ijt..'';7.'fe ::v..'.. '. /.C^i.'^ ' ^ fvvy' o 'r v'tkt'.; ''"' ilitl "."J u''' v 1 :, \^'.':.S ; P*'. 'W' r '^ \'av ^ '.^,rrv'e^' ^rf...'r;.:o St "' Mj^r, Hrt6'Ni's:. T")',Vfr^ : '^^ Ni!^L c r:," T :. v^f' L.'^. "I't. ' 1(V' y i ^ T 1. fcf" *~ i 1 ' ^' '^" ; ". ^.r* tu it'..^: 'fvro'i^'j i ".! : ' i or r t M')i'LS ' '^ r UcO.^ ; ^ r T(?.t(,Tot6S l "^ "P,l t fix. raw (OMii.por features such as foliation, bedding, schistosity, measured from the long axis of the core.. t Additional credit available. See Assessment WorK Regulation. Exemples de caracteristiques : foliation, schistosity stratification. L'angle est mesure par rapport a I'axe longitudinal de la carotte. t Des credits supplementaires sont offerts. Consulter les reglements relatlfs aux travaux devaluation. Nota : Dans cetta formula, lorsqu'il designe daa peraonnes. la maaculin est utilisa au sana neutre. FI /Pi pt,pi FIVPi Ft /Pi 0 Address/Location where core stored Adresseyendroit ou la carotte est stockee '^CCr' 1. i lv '.r^ls ' '^C',' '.r'.t'v iyp;\"a'"i v 'r. 'ZilF. Tt Li fci'vcf f'*' 'j' ' v'''j f' L.VAUM P. T"v^ ( s^c.it.^ ofsj,/ljtp O rr/er 1 j)g^ Jto?!'?'? T&40C Ycxt; Sampto No. N* d'tchanlihon du prmpkuur C^7 H0.S*! ^6So /JC V / jj;vl2 'l, O.' ^09 ^S^f{^r lolfc ^ v is1^ ^ 4 ; Map Reference No. N9 de reference sur la carte Claim No, N" de concession miniere Location (Twp. Lot, Con. or Lat. and Long.) Emplacement (canton, lot, concession, ou latitude el longitude) Property Name Nom de la propriete Svn tt FooU9*Nn*au di pr4. Mvtffltffl (M rtchanlihon (an Dwlsl To/A FronVOe 9?( ^ X7 ^ (fi f) tf^ /C7) 'Ti Ctt^~. (f\ 1 ~J &Q7 e^c/v ^^ C1 ( ^ ^? ^ (7l u^7 T O Q f9j as f\1 d^l &.S. fa 1 c Jci^ /6 SuipkLangin Longueur d* I'lcWiUUi ^ J 2 a ^ ^/0^ ^/ 4 Assays t/ Analyses mineralurgiques ^ ^ ^ S' l \

36 Ministry ol Ministere du Complete this form end IVy l Northern Development Developpement du Nord Drj Jing forage U related sketch In duplicate. Fill In on every page ViiX and Mines et des Mines M Hlamant Rempllr en deux exemplairea la Hemplir ces cases a k O"""0 Lo9 aiamam pr.j,nte formule et lecroqule annexe chaque page T Drilling Company Compagnla da torage Collar Elevation Elevation du collier Data Hole Stafled Date Completed Date Logged Data de commencement du forage Date d'achevement Date d inscription au journal Exploration Co.. Owner or Optionee Compagnie d'expkxation, proprietaire ou titulaira d'optkxi Footage/Avancement From/De To/A ;6! ' b" :. W.1 Rock Type Type de roche STSEMetn crc?v.'po:.lc^t; ~. f9k li'.uvl.'zsn'. V. 'k'./lr.vvv /jsrpomk ^ 0 blt'nfv Data Submitted Data da depot Bearing of hole from true Total Footage Dip of Hole at " North/Position du forage Avancement total du tnclinaison du forage au par rapport au nord vrai forage CoHv/coilitr Logged by " Inscrit par Ft./Pi 0 Submitted by (Signature) Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometric, texture, mineraux, transformation, etc.) ^^s^ y^^'^ ]\. i, 'r j 'C, \)'i'^ ' ): :, /,v ; n' ft TiNt. '( C^/fc ^ vi?'i:^^^r^d ^.i.jji't ^.'Jcf.C.no; TTt''^. ")T r"'mc P 1'^:?^ vi.'jgi*^: v ' v^^' "i ^ r ' ^ 't ) ' [^ D ' v i ; f IjlMV 'T' i!j*. ^' r ' v ^j&'t; r'ufcr')rr't f f i r ". ' y/: e v )f f " ^ x ' " L) ' T rt ^ " rrr ' /c.. t'^,ij//.o cc^ ',r^/, fi^^' j/' ^ r~)li::\ 'C'^:^, ' ' V ^Mc*^ AX ' ^ 1 L. ' ^1 i i^1 r^l^^ ^ 1 '^^' ^^. r. ^ ^ f"' ^ ^, 1! l h 'i.,jvt '.'c. v" l 'i ^~ p.,ni FUPI FI./PI ci.'/ 'Vil.l, ro'1/lt'lv. ao" "A. c ^ ^'/y:t\ M'^.L1.' '''Si ;j. " ' ^ i /i' ir 9 ' *! ~. '.^' CLL'.I 'p,,"' JL^'' J O ' 'i'! ^S. :v^t')0" oi "i C'f'j"'''i." r.'c '' ~VMO: r;i.'"" ^c; ': ' 1::: '^rr..:.! :..I',D j ^r^no^r: ''OrCD r^o'}'?i ;?)T. ' ^' ~ ~''S.'^ "'If '7^, y '', ; FC U0~ ' 1"'" Oox'~ :^ ; 7.1 e *"i? ^ "' * /'l r ' i : x,.. ^T 7 V " ' ' V r^t f.irrin/^u/i^i':.?^"7 "^C0.f^; L ov'c^'/ f'mt f,'f tlt/^l^t: f^cj'v'e ID Ci^C'r'f./tT'^ c 10.' 'C. t!;.is"f;at70^1 ^f MtTAvlOi',.;/ n: tc O'Ki'D f'^itt M^rPD. For features such as foliation, bedding, schistosity, measured from the long axis of the core. Exemples de caracteristiques : foliation, schistosity, stratification. L'angle esl mesure par rapport a I'axe longitudinal de la carolte. Address/Location where core stored Adresse/endroit oil la carotte est stockee PUn* FMtwrl,'.,x:i Feottgi r/longuw t pwm on ctram prmmm ^^ 6 fe St/ ttk&q 6M to^' ( ^8^ ^8^ j ^^7 rf ihq(gf :6ft(f).faffiiO ; ^22^ s^: (.^ f f*/ /^^ &Z/I bfaftg ' km t t i feffi/ty (l foffi/l Map Reference No. N" de reference sur la cane Hole No. Forage n" Page No. Page n' a Claim No. N0 de concession miniere Location (Twp. Lot. Con. or Lat. and Long.) Emplacement (canton, lot, concession, ou latitude at longitude) Property Name Norn de la prapriett You SampM No. Siwnpt* FoouoaVNivejau di p/tv Mvwntffl (M I'tcnvtilkm (m txedti From/Off Ml ^ 2^7 *? /' /7 J? ^L,' j^^ ^^ ^^ 72 7^\ 7^ ^0 L^W^'V \Z"7 91 TiMk 4k ^ 6 ~J ^L ^ ^ fr9 27 ^7 7Z ^ ^ "2 fjfj '^^^ *~) ~4*^^fLf 27 9/?4 SampULmgth LongiMurd* I'fcnanwion (f m A Z Assays T /Analyses mineralurgiques t Additional credit available See Assessment Work Regulation. t Des credits supplementaires sont otferts. Consulter les reglements relatifs aux travaux devaluation. Nola : Dana cane lormuli, lorsqu'll designe des peraonnes. la masculin ait utilise au sem nautra.