52GMSE1122 52GMSE0058B1 VALORA LAKE 010

P.G. LACOMBE 6 ASSOCIES

Geological Report

Ideal Bay Explorations Limited

Sturgeon Lake, Ontario

By: Pierre G. Lacombe, Eng.,P.G. Lacombe 6 Associates, Consulting Engineers. July 16, 1971.

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P. G.LACOM-S

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P.G. LACOMBE f. ASSOCIES

Geological Report

Ideal Bay Explorations Limited

Sturgeon Lake, Ontario

Introduction;

Ideal Bay Explorations Limited has acquired 20 claims totalling approximately 800 acres on the south shore of Beidehman Bay, Sturgeon Lake, Ontario.

A line system has been cut on the property and was used to complete a Radem VLF electro magnetic survey on the property in October 1970 and March 1971. This survey located 11 conductors striking east-west and varying in length from 300 to 4000 feet.

These conductors were later verified by means of a magnetometer survey which showed 4 of them to be conjugated to magnetic anomalies. Taking into con sideration the particular conditions existing in the area, geophysicists are agreed that the absence of magnetic anomalie with an electromagnetic conductor does not preclude the conductor from being caused by the underlying presence of sulphides in this environment.

The extent of the electromagnetic conductors is such as to warrant a diamond drilling program to further investigate the cause of the electromagnetic anomalies. Prior to effecting this program it has been recommended to proceed with a geological survey as a base to determine the extent of the program recommended, the actual site and attitude of the drill holes planned. Such a survey was effected between July 4th and lith, 1971, the results of which are given in the present report.

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P. G. LACOM82 St ASSOCIES

Geological F.-j r oy t

Ide P. l 3r.y Explorations Unite

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Ideal Bay Sxplorsticr.s Limited ha'-; acquired 20 claias totalling apprc-:-:l;..atily oOO t-cree on the south shore oi' B^idolr.on Bay, Sturgeon L&ko, Ontario.

A line aysten has c c or. cut en the pro perty and was used to coupleto a Hadsn VL? slootro r.arnetic survey on the property ir. October 1570 cjr.d Itarch 1971. This survey located 11 conductors striking east-west and varying in length iron 300 -co 4000 feet.

These conductors v/sre later verified by r.eans of a zagnetoseter survey \vhich showed 4 of then: to be conjugated to magnetic ancnalios. taking into consideration -she particular conditions existing in the area, geophysicisto are agroed that the absence of aagnatic 'anosalie v;ith an electro magnetic conductor does not preclude the conductor fron being caused by the underlying presence of sulphides in this-'.environment.

The extent of the electro magnetic con ductors is such as^to warrant a diamond drilling program to further^lnvestigate the cause of: tho electro magnetic -aiiOEalie s. Prior to effecting , this program itvflas'i'been raooraended to;proceed . With, a f eolo^a^feyey. aa fiTbaae^toLdetai^aino

cite and atti'&ade^i^tthe'drill holes' planned.' Such a survey was "effected between July 4th .and

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Property;

The property consists of 20 claims staked under licences Nos. 243453 to 243472 inclusive.

They are located immediately south of Deidelman Bay at Sturgeon Lake and extend over the west shore of Cluster Lake. The property lies approximately 45 miles north and east of Ignace, on the Trans Canada Highway, about 2 miles due west of the mill site of Mattabi Mines Limited, presently under construction.

It is easily reached by good gravel road leading to Mattabi Mines and it is also crossed by the power line and the projected railroad going into Mattabi Mines. Several bush roads have been cut across the property in a north-south direction creating good access to any claims for future drilling purposes.

Topography;

The claims are generally low lying and the areas bordering streams, ponds and lakes are either swamps or low ground. Such areas have been indicated on the geological map by the conventional swamp sign.

Areas left in blank are generally flat and covered with a mixed small growth of trees, mainly spruce and poplars with the odd birch patch. This ground is generally covered by overburden exhibiting a few boulders and the depth of overburden appears to be such as to prevent any conclusion as to the under lying formation. Such areas have been left blank on the map.

Overburden and boulder hills have been indicated on the map. These are hillocks rising 20 to 75 feet above the surrounding flatter landscape. They are made up of very abundant and generally very large boulders which can at times be mistaken for outcrops. The amount of boulders present give the impression that they well may be representative of the underlying formation, although the general shape and distribution of these hillocks is suggestive of morainic deposits.

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Property;

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She property consists cf 20 claims stalred raider licences HOD. 243453 to 242472 inclusive.

2hey are l coated immediately south of Boidclnan Bay at S'-ur^ctt lake- ar.c o::ter.d OY. r the west chore o. Cluster Lake. Dho pro-port/ lies approximately 45 nilas ::crth a::d cast of Zjr.'.is, on the 2rar.s Canada Highway, c. b on t 2 cilos clu-i v/cist of the sill sit a of Llattabi Alines lisitoi, presently under contraction.

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ci.t acrcae tho i-rcpcrty iii a I'ior^h-jouth di. creating good ecce drilling purpocej.reating good eccess to any cl-ir:o for future

rjhe claims are senerclly lev; lyinj and tho r.r^as borderinj s"rea^3, ponds and lake-c ara

. either cv/arps or lov/ ground. Such areas havu been indicated en the geological nap by the conventional sv.-ar.p sign.

Areas left in blan'jc arc generally flat ar.d covered with a ni:ced s^all growth of trees, mainly spruce and poplars with the odd birch patch. 2his ground is generally covered by over burden exhibiting few boulders and the depth of overburden appears to be such as to prevent any conclusion as to the underlying formation. Such areas have been left blank on the nap.

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Overburden and boulder hills have been indicated on the nap. ffhese" are hillocks rising 20 to 75 feet above the surrounding flater land scape. They are aado up of ver; abundant and ,

^generally very large^bottlders^whiclf^c&n^ " J 'be mistaken for outcrops, i'he anount of boulders present givo the impression" that they well may be representative of thO;underlying formation, v.; although the general sfcap6 end distribution :;of T? ; these hillocxcs is suggestive of norainic-'".deposits";

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Topography: (Cont'd)

Definite moraines made up of large boulders lying in elongated strips without any interstitial gravel or sand have been observed in numerous locations on the edge of the hills.

Where the ground appears to be underlain by solid rock formation within shallow depth, it is covered by a sparce growth of spruce without the usual mixture of deciduous trees. Ground elevation rises sharply to 100 feet or more in the north-eastern part of the property on claims 243456 and 243459, where granitic and dioritic formations outcrop.

The claims are intersected by the gravel road leading from highway 593 to the Mattabi Mine mill site. A railroad spur line is being brought to the mill site along with a power line and both of these will be crossing the property. A number of access roads and slashes have been cut across the claims to reach these railroad and power lines so that access to most parts of the property will be made very easy. The slashing in progress has been indicated on the geological plan but could be considerably changed and added to in the coming weeks.

Water is within easy reach almost anywhere, which factor would facilitate an eventual drilling program.

Outcrops are quite scarce on the property except over the northern granitic formations. One must be very careful not to confuse large boulders with formations in place since huge blocks first mistaken for outcrops have been later observed to be isolated boulders. This absence of rock exposures render very difficult the correlation between the various outcrops mapped and locating with precision any contacts between formations is presently impossible. It is surmised that a close study of the boulder hills may provide useful information regarding the underlying formations and such a study is recommended.

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Topography; (Conv'cl)

Dafinito noraine-s jrado up z- lc^r^s bculdic-i ly.iig in elongated strips without say interstitial ^^r.vel or sand have beer, observed in r.unircuo looa'-ic/.s or. the edge of the hills.

by solid rock f oration v.'it-hin chill-T..- deyi. : ; it is covered by a spar c o rrcv/th ci" sprue,, ri-sh :-ivc ^he- usual mixture of deciduous -crc^s. ~ C-r-yaria ol:.va-:ion risss sharply to 100 fost cr nora ir. the r.or-.h- eastern part of the property cr. cis i".:. 2-!-34 i,; ;" c-r.d S-.-3459, where granitic and dioritii fcrc:a-wic.'.a cut- crop.

2he clair.s are inter .re- road leadir.^ frcr. r.ill cite.to tho :cill oite along with a - over Lin i a:-:.- of these v/ill be crofoir. :3 thu- j-i-oper^: of access roads and slashes h^-.'-j tv ;r. cat ac the clair.2 to r-saeh these railriai -:d pov.-cr so that access to r.ost parts ci" th3 property bo nade very easy. 5?ha"slashir..j in " -cjrsss been indicated on the seolosicr.l pi.-: cut cov. be considerably changed and added -o in the c weeks.

y/illi. a 3 Id

Vi'atcr is v/ithin easy reach aluost any- v/here, v/hich factor would facilitate aii eventual drilling program.

Outcrops are quite scarce ex the property except over the northern granitic ferretions. *Cne must be very careful not -co confuse largo boulders v/ith foriAations in place since huge blocks first nistakcn for outcrops have beer, later observed to be isolated boulderc. tfhis aboonce of rock ex- pooures render very difficult the correlation bctv/een the various outcrops napped and locating with precision any contacts betv/ecn foruations is presently inpossible. It is surmised that a close study of the"boulder hills cay provide useful information regarding the underlying formations and such a study is recommended.

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TABLE OF FORMATIONS

Cenozoic

Pleistocene and Recent

Sand, gravel, clay.

Unconformity

Precambrian

Archean

Felsic Igneous and Metamorphic Rocks

5a Biotite- and (or) hornblende-

quartz-feldspar gneiss, granite

gneiss, hybrid granite gneiss.

5b Granite, granodiorite, quartz

monzonite, quartz diorite.

Metavolcanics

Mafic Metavolcanics

la Massive lava, pillow lava, tuff,

and derived schists.

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Pleistocene and Hecent

Sand, gravel, clay.

Unconformity

Precambrian

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Archean

Felsic I^cous -uid I.:^ta.-or:3lvic lioclca

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quar^a-rdcieiDar ^r.cios, granite

gneiss, hybrid granite gneiss.

5b Granite, e:.-ancdiorit3, cuartz

aonsonito, quarts diorite.

: 'otavolcenics

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la I-Iassive lava, pillov/ lava, tuff,

and derived schists.

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Geology;

The area has been little mapped geologically. The Department of Mines has published a map in the Geological Compilation series, at 4 miles to the inch. There is also an uncoloured preliminary map published by the Ontario Department of Mines on the Savant - Caribou Lakes Area and the Minnitaki - Sturgeon Lakes Area at 2 miles to the inch. All this is very broad mapping.

Essentially, all underlying formations are Archean Pre-Cambrian and can be divided into Felsic Igneous and Metavolcanics.

The Felsic Igneous occupy mainly the northern part of the property, although outcrops of granitic rocks have been observed in the south-east corner and along the center of the vast border. These two occurrences may or may not be connected under the rather heavy overburden.

The metavolcanics occur along or south of the northern baseline as large boulders without certainty as to their being in place. In the southern part of the claims, andesites have been mapped, definitely in place confirming that the area between the granitic outcrop is likely occupied by basic formations.

Structure:**

These formations are part of a tightly folded synclinal basin with a slight dip to the north. Dips are nowhere evident on the property and the andesite is very massive without any certain sign of attitude.

In the norther part of the claims, in a transition zone between granite and more basic formations, a small occurrence of schist strikes N65E with a vertical dip.

Rock Types;

As seen on the accompanying map, formations vary from granitic (or more acid) in the north-east to gradually more mafic as one moves either west or south, except for the granite occurrences in the south- east corner.

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The granite (where indicated by the symbol Gr.) is a defintie, fine to medium grained granite made up of orthoclase, quartz and minor biotite or hornblends. Along the west border, just south of the powerline slash, the same granite is very markedly gneissic.

On the northern claims, a s o ne moves west from the main granite occurrences, plagioclase content appear to increase significantly and the rock may be better described as quartz monzonite, with the quartz being very crystalline and almost amethyst in colour.

When moving south from the granite, the plagio clase content increases and the formation becomes quartz- diorite. In one spot, a acid schist was found between the granite and the diorite.

The dioritic rocks vary over a whole scale from quartz-monzonite to diorite, dacite and andesite. An andesite schist mineralized with pyrite was found in the south-west corner, but definitely no an outcrop.

Petrographic identification and description of each of these formations has been asked and will be reported on separately.

EM Correlation;

A Radem VLF survey has been completed over the full extent of the property. It has outlined 11 con ductors, marked A to J, varying in lenflth from 300 to 4,000 feet.

Conductor A is 4000 feet long and extends across the two ponds in the north-west corner of the claims. It lies on line with some old showings west of the property boundary where copper, zinc, silver and gold have been found. It is also close to the transition zone between the granite and the monzonite or other plagioclase rocks.

Conductor B is 1600 feet long and is also the site of a magnetic anomaly. It is difficult to appraise since it lies mostly under the road leading to Mattabi Mines. It is also in the transition zone and therefrom it is deemed to have significance. Conductor C may be a faulted offshoot of B, as tentatively indicated on the map.

DUPLICAiixCQPYQUALrirp&Rl TO FOLLOW

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1 The granite ( where indicated by ^he Symbol Gr.) is a definite, fine to medium grained .jraiiitsratvJe up of orthoclase, quarta and minor bicTito or hornblende. Along the west border, juat south ci' the power line slash, the sase granite 3 s vary nar!:sdly gneissic.

On the northern clairio, as one novas w i st Jroa the main granite occurrences, plagioclase content appear to increase si^iific^itly a:-;d t' ^ roc'.: .-ay be better described aa ouai'tii :jci;sc::ito. :,:.",h tliO cuarta

; very crystalline and aL-'-ost cr:ethyst in colour.

: content increases end the formation beco:-D3 cu ...-ts-dioi'ito. Ir. one cyo" , a acid schist was found betweoii* the granite and tl;o diorite,

The dioritic roc'-cs vary over r. v/hola cc-2.1e ^rc: cuar't^-cionsoni^s to diorite, dacite :o:u ai^da^ivov .'~. a:;deoite achist rii::3ralized-x;ith pyrita \;a^ iO.-:ci in the couth-v/ost cornc;r v bat ddiinitcly nc\; an cutcrop.

retrographic- identification ar.d v'^ocription of each of these forr;a"icns has been aalccd and v;ill be reported on separately.

Sorrel at i en:

A Hade-: YL? survey has been completed ever the full extent of t2;e props^-ty. It has outlined 11 con ductors, marked A to J, varying in length f r on 300 to 4,000 feet.

Conductor A is 4000 feet lcn^ and extends across tlie two ponds in the aorvh-v/est corner of the claims. It lies on line with o osie old, showings we st of the pro perty boundary wliere copper, sine, silver and gold have

.

een found. It is also close to the transition zono betv.-een the granite and the monzonite or other plagioclase roots.

Conductor 3 is 1600 feat Ion.? and io also tha a magnetic anonaly. It is difficult to appraise

since it lies nostly under the road leading to Uattabi :.:ines. It is also in the -transition zone and thsrefroa is deeffid to have eignif icance* Conduotor O may "oe a faul ted off shoot* of B, as tentatively^indicated on the fjnap. -- . ' ' " -- '

Conductors D and F appear to reflect swamp conditions but conductor E, overlying an elongated hill covered with large boulders is definitely not caused by conductive swamp and must be investigated. The same remark apply to conductor J where, further more, a float containing heavily pyritized schist has been found. This float was much too small and altered to have travelled any distance.

Conductor H is 3,000 feet long and, although running across low ground, its location is offset to the north by 300 to 400 feet from the actual stream and its general course suggests a cause separate from conductive swamp bottom. Its presence close to andesite outcrops and near a possible granite contact, in the east end of claim no. 243468. would locate it in a contact zone between volcanics and acid formations, Its eastern end is very close to conductor J where no reference to low ground can be made.

Conclusions;

The Sturgeon Lake property of Ideal Bay Explor ations Limited straddles two contact zones between granites or granitic formations to metavolcanics of the andesite type.

This contact zone is not a sharply defined contact between true granites and tru volcanics but a transition zone where various rock types are seen to evolve from orthoclase granite and gneissic orthoclase granites to quartz monzonites and quartz diorites to diorite and dacite .

The southern part of the property is definitely underlain by metavolcanics of the andesite type.

The presence of long EM conductors in these contact zones is significant, especially where these are connected with magnetic anomalies or where they are not reflection of conductivity in wet ground.

The length and location of long conductors in the northwest and southern part is such that they could be dissociated from water streams, and, hence, should be investigated by drilling. It should be noted that in the Sturgeon Lake area, disseminated copper-zinc sul phides are not necessarily accompanied by magnetic anomalies and that conductor A, 4,000 feet long, on strike with mineralized showings to the west, in an acid to basic transition zone, should be drilled, along with conductors B, E and H. D IIPl IPATE COPY

POOR QUALITY ORIGINAL TO FOLLOW

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Conductors D ?r.d P appear to reflac'- 2.v;?jnp conditions but conductor D j cvcrlyin^ an olcr.^atid hill covered with lar^e boullava is dofir.itely r.ot caused by conductive sv/aup er.d nu-;t b i: invc-s :i;;^1;od. 2he sane renarlc apply to c or. C. not or J viu.-ro ? ;.;uv-hor- nore, a float containing hoc.vily pyritiacd schist has been found. 2his float v;as such too snail ar.;. altered to have travelled any distance.

Conductor :i :..- ^,COO C:.^ lc::^ C-nd, alt-iOu^h running across lc\7 ^.-jr.t., its lcc;.^io:. is o^fsjt to thj north by 300 to -:-OC/ foot .ron the actual 3trec-xi ar.a its general ccu^ao su.,-:^oi-;o a causo oipara^G f r era conductive sv/anp boitc—* It j presence close vo ar.dssito outcrops and near s. possible granite contact; in the. ea:;t end of clain no. 243vo8* r;^uld locate it in a contact cone between volca:-.ico cr.d acid fcr^i:Riccio. It.-' easterr: end is very closo- to conductor J v/hsro no ref erence to lev; ground can bo

riv

rations Limited ^tiT-ddloj t-.ro contact zor.cs -jtv/oc:-. granites or granitic f ornations to ^otavolcai.ics of tho andesite type.

K:is con-;a.c-c; zone is r.o-i a sl-iai'v.,./ c', joined contact "betv/een ~rr,i sraiii'bos crd tru.3 volcaulcs but a 'ircaaaiticn z o~~,-2 v.-hero variouo roolz typss ai-2 seen to ovolvo froa orthoclase granite and gneissic crthoclaso granites to quarts zonaonites and uardiorite and dacite.

rts dioritcs to

southern part of the property ic definitely underlain by etavolcar.ico cf the andesite type.

2he presence of long ZJ conductors L:I those contact zones ic sisnificcnt, especially whei-j theoe are connected with magnetic su.oraalies or where thoy are not reflection of conductivity in vret ground.

The length and location of lcn^ conductors in the northwest and southern part is eueh that they could ba dissociated from v/atcr streans, and, her.ee, should be investigated by drilling. It should bs noted that in the Sturseaon Lato area, disseminated copper-zino sul phides are not necessarily acconpanied by Eiagaetio azio- nalies and that conductor A, 4,000 feet long, ion strike with nineralised showings to the vest, in an acid to basic transition sone, should bo drilled, along \vith conductors 3, 2 and H. " !

Reconunendations;

1. To complete a close study of large boulder formations on boulder and overburden hills as a possible reflection of the underlying formations.

2. To have full identification of each rocktyps effected by a petrograph expert in the Sturgeon Lake formation identification.

3. To proceed to diamond drilling of conductors A, B, E and H immediately upon completion of above reconuneddations.

Cost Estimate:

Study of boulders

Rock Type Identification

- *

500.00

Total: 500.00

Respectfully submitted,

Pierre G. Lacombe, Eng. P.G. Lacombe 6 Associates Consulting Engineers

PGL:id July 1971

DUPLICATE COPYPOOR QUAUHY'ORIGINAL

TO FOLLOW

-3 fei3 S-

^;4:::^ "'-"/^ 'W.

20oamendatione:

1. 2o ccmplote a closs study of J.Z?Q± "boulder t oraationa on boulder cr.d ovcivurc.cn hi?.ls as a porslblo raflootion of tho u^derlyiag for&ations;

2. So h^/a full i^cntifica-iic.^ of caci. roo^: typs effected cy a pcti'02rap;i c;ro.,^-l; i:i -H-.

f crsatica -d3* 2o procaed to diancnd dL*il".ir.f; cf conduct ora

A abovo rocornendaticns.

, , S sad E lasicdiatcly upon cozipletloa of

Cost Estir.ato:

Study of bouldors

Hock 2ypa Identificatica 3 pGO*00

$ 500.00

Hospectfully subuittod,

July 1971.

Pierrs G* Xaoonbe, Eng. P.G.Laconbo A Aasooiatea Consulting Engine eva

t* umtor* tufted* Pierre 4;. I-ACQJM**, f*. A.,

M.A.C,g hereby tat* that j

1. t w tt M in in* engineer UfcrGill 1*541 and a MP0*V*r in qrood *tarxJir^9 of the Corporation of to q i ft** r* of Quebec, of the As&ociat irrn of ',V*olo^i*t3 of Cto^l*?*' *f*fJ rp-^istcr*yd wit the Asftociatioti of rro{***ion*l Engi eer* of Ontario;

f. l have no i nterest, *rtx*tt*?r D irect or ir,- direct, i ti t *^ prop**rt icf o r tecuritiea of Ideal Way Explorations L imited, I ,Ao not iftteni to ac-'|ui^c f w h i nterest nor rio I

to

). 7**** prp*ent report is basevJ CTJ a

4th ,~n*l lith 1971 ,*rwl ot. .* st (*J/ 1-o-t available

July

f ail l y subaitted.

July

G.

, 1971

QUPLICATE COPY30RQUAUm)R!GINAL

TO FOLLOW

Certificate;-

I, ur.dci'jicr.ii t l-o— G. I^

A.G.Q. hereby cta^ -;h^":

1. I an a riini.^ ll^inccr C^C-ill 195-; -.d r. ncraber in ^ccd e"c^-in- ^ xlio Cr.-;^.-u"ic.-. of ii:-i::cc^j 01' C-eoe;., c^ t ".-.s .iicoc-aticri of Gcclcei^- of ^u.c;bco o-'.cl rc^is-JOi-ou v/ith "he Associaticci of Prci'c^sicr.al lr.si.'. :ors of Ontario;

2. T have no ir.-:croo-:, -.:-;^;;.c.- di:-cc" c.? i;i- ciroct, in -iho prc~wr':i:..:- o^ ocouri^-3s of rdeal I.-.;- Ix-.iloiv.?---:. Ii.v.itc-i:, - cc no-; intend ;;o c.cru^ra i,uch ^.-.-j'-i-ost nor vi o I expect to rocuivc a,:y;

2. IT'/.c ::roc:-nt rcr-or'- i c c:.::cofi'octod in -;he fi

vine lith 1S71 c-: i en ;. best availably infcr-uc-tion

;l on c. ~oclo^iCv botv/vscn July

cf --l

July loth 1571.

r. G.0. laccr-bc,

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'PI:RRE GILI^S LACOMBEl."-.-. i'.?t.7 -. t ^ H•T-o:! o? r.-:T-r,s'ONAL

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SPECIAL PROVISION

ASSESSMENT WORK DETAILS

IUMK5 AND ADDRESSES

CkUf Line Cutter o/Contractor DleoQYore Mineral SuTveya. fawn, Ont*f. Hyman

Party Chief

ConsultantP.G.Lacoabe 4 Associates, Box 68, Belocil, Quo.

COVERING DATES

UM

* Field a*d Office

INSTRUMENT DATA

Uafce, Model and Type

Scale Constant or Sensitivity ————-—^.——--———---——... Of frovfV* copy o/ inj/n/Mraf ^*'a /'o* M***(actiirer's brocburr

Total Noaibcr of Station* Vithin Claim Cioup

Number of Miln of Line cut Within Cliiea Cioup .. .. mllftfl ____ .

ASSESSMENT WORK CREDITS REQUESTED

Geological Survey -l—20—4D*y* per Claim

Geophysical Survey ————— D*ya fer Claim

MINING CLAIMS TRAVERSED

D-4TE

PA-243453 to 243472 incl. ; i J l At f ' '. 4

form i* rrquirrd for r** - h lyjte of

e * .t

m iron - am MOHTOOT:

AREA CODE—TELEPHONE — 965-6918

r -M jmi 2.636

DEPARTMENT C^ MlNfcJWAND NDUIHI. "N1 AM AIMS

March 20, 1972

.11 \ tu 'Mr. W. A, ftichan, Mining Recorder, Court House, Sioux Lookout, Ontario.

Dear Sir:Re: Mining Claims Pa. 243453 et al,

S.W. part of Sturgeon Lake, File 2.636

The Geological assessment work credits as listed with my Notice of Intent dated March l, 1972 have been approved as of the datij above. Please inform the recorded holder and so indicate, on your records.

Yours very truly,

OJ/mw

Fred W. MatthewsSupervisor

Projects Section

cc: Anthony Canlsso,9th floor, 366 Bay Street, Toronto, Ontario.

cc: Mr. Pierre G. Lacombe, P. Eng., Box 68, Beloeil, P,Q.

cc: Resident Geologist, ^^ Kenora, Ontario.

SEE ACCOMPANYING MAP(S) IDENTIFIED AS

LOCATED IN THE MAP

CHANNEL IN THEFOLLOWING SEQUENCE

(X)

LEGEND

H/-^* t r i * - * **TL**

"**5*F!f *irl.:.'^lK14iBTT

IDEAL BAY EXPLORATIONS LTD.

O ISO O OIC JVL *fe

BY: P. C.

5SG145EII22 52G14SEC050B1 VALORA LAKE 200