EXPLORATION 1996 SETTING NET LAKE

53C13SE2001 2.18319 SETTING NET LAKE 010

WOLFDEN RESOURCES LIMITED

EXPLORATION 1996at

SETTING NET LAKE

HAR -P iGF"

53C13SE2001 2.18319 SETTING NET LAKE Q 10C

TABLE of CONTENTS

PAGE INTRODUCTION l

PROPERTY l

LOCATION 8c ACCESS 2

GENERAL GEOLOGY 2

HISTORY 4

PRESENT PROGRAMME

HISTORY 5

LINECUTTING 8

MAGNETIC SURVEY 8

GEOLOGY 11

MINERALISATION 16

CONCLUSIONS 19

RECOMMENDATIONS 20

APPENDIX ISAMPLES NUMBERS b ASSAY RESULTS

MAPS and DRAWINGS

LOCATION MAPS "A", "B" AND "C"

GEOLOGY (O.G.S.) 1/250,000

LEGEND FOR ABOVE

LONGITUDINAL SECTIONSVALUES (96Cu.) WRSN.001 FEET 96 WZ WRSN.002 FEET 9fc EZ WRSN.003

GEOLOGY (1:2,500)

MAG. SURVEY

WRSN.004

-POSTINGS (1:5,000)-CONTOURS (1:5,000)-COLOUR (1:5,000)

before P. l

after P.2

after P. 17

in pockets at rear

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SETTING NET CREEK G-1878WOLFDEN RESOURCES LIMITED

Location Mao 'B'

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, WOLFDEN RESOURCES LIMITED!

mr v Setting Net Lake ii.;k.- . CC^li

94000'Location Map 'C'

5 93 ooo'6 92=30-

INTRODUCTION

This report provides a summary of exploration for gold and base metals at the Setting Net

Lake, N.W. Ont. holdings of Wolfden Resources Inc., Thunder Bay, Ont.. The work was

conducted under supervision by the author on behalf of Wolfden Res. and T fe H Resources of

Toronto, Ont. which provided funds for this work under a joint venture agreement with Wolfden.

The activities described were performed with the knowledge and approval of E.S. Downie (Pres.,

Wolfden) and J.A. Pollock (Pres., Jonpol).

PROPERTY

The property consists of 15 contiguous claims comprising nominally 201 units and 3216

Ha.. From the claim map it is calculated that the area covered is 3434 Ha..

CLAIM UNITS (nominal) AREA

1215044 16 2561215045 16 2561215046 16 2561215047 15 2321215152 9 1411215229 16 2401215230 16 3021215231 16 3201215232 16 2761215233 6 1161215234 16 3021215235 16 3201215236 16 2461215237 2 301215238 9 141

15 201 3434

These may be found on M.N.R. Map No. G. 1879: Setting Net Lake Area

LOCATION AND ACCESS

The claims lie immediately east and north of Setting Net Lake astride a northwest-

southeast line extending from 52 0 45'N., 93 0 31'W. to about 52 0 50'N., 93 0 37'W.: principally

within the SE/4 of the claim map (G. 1879) area. The north shore of the southern end of Setting

Net Lake is about 190km. north and slightly east of Red Lake, Ont..

Access in summer is from Red Lake by float-equipped aircraft, a distance of 190km.. In

a normal year this is true of ski-equipped aircraft in winter. This winter, we are told, a winter-

road will be made between Red Lake and North Spirit Lake, and extended to the Deer Lake I.R.,

and Sandy Lake the latter passing close to the Flanagan R. hydro-dam (to be refurbished) at

Northwind Lake; it will most likely follow the old route to Flanagan River dam and Big Sandy

Lake which means crossing the Setting Net Lake property or possibly a new route 2-3km. south

of Setting Net. This winter should permit driving to or close to the property, which will

substantially reduce the cost of a drill programme.

GENERAL GEOLOGY

The rocks at Setting Net Lake are part of an elongate volcano-sedimentary belt extending

l lONOURABLE LEO DERNIER..\lmislcr of Ndiiirtil ResourcesW. Q- MACN'EE. Dcpiilv Minislrr nf Niiliini) Ilijsourrrs

G. A. li'Wtt. Kxi.riilivi: Director. Division of Mines E. C. I've. Dircrlor. (inoioy/cnl lirunc/i

Admins Map 2178 fe Stull Lake—Sandy Lake Sheet

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^ SETTING NET LAKE AREA

GEOLOGY

OGS MAP No.2262 Scale 1 l 2 50,000 JIT- -V,"S- ^ ', , -

^-îJ'-' ^* ' 1.^,'

CKN07.0ICQUA

swamp. lakfi and stream sediments

n.KiMocKNrrji.nri.il ( ill ai'd outwash (sand and gravel)

PKKCAMUKIANAUCIIKAN

l ] Late Malic Intrusive Rocksl la Unsuljdividedl 'b Biolile-rich lamprophyre

1 le Ampl-ibole phenocrysl bearing Inmprophyrg

l Id Polasslum leldspar-megacryslic lamprophyre11s Follalsd

VlintlfilvG COH1ACT

BAT LAKE STOCK, MIRROR BAY STOCK

late F elsic 1 0 Intermediate Intrusive Rocks

lOb Mei).i.-ijsiii; biotite gianilolOc D iolile grnniielOd Blolile -hornblende g ranodiorite, lonalile10g Pegmatoid and/or aplitic d ikes10li LayerndlOn Mi*cd conlacl zonetns ("ciliatedIQw EpidclclOz Ampl'ibolilized and/or epidotized volcanic

xonoMhs

JACKFISH LAKE--WEI LER l AKE PLUTON, VICKERS LAKE

PLUTON. BRETZ LAKE STOCK

Late Felsic to Inlcitnedlale Inliuslve Rocks

9b Medium groined b iolile and biotile-hornblendagranite to granodiorite

9c Polassiunvleldspar-megactystic granite logranodiorite

9d QunHz monzonite

91 Monzoriilc, monzodiorite, diorite

9rj Grani'e. p ngnialotd and/or a plitic d ikes9j Polass'uni-leldspa'-rnegactyslic monzonile lo

gr,-|nil3

9in Fclsilo9n M ined corilocl zone. Intrusive breccia

Esox Lake Melascdlments

8b fvluds'one. sillslone, shale, argillileBc Sond-.lone (unsubdivided)8d l c'dsjnlliic wacke8c Lithic wackoQl folds jalhic n rcnita. quadz aionileOtJ l. ill lie a run! lo81' CongorneraleOj RfecciaBk Mudslono. nrgilhle or sillslone with line-

gtaincd sandstone inierbtjds

Brn Thinly liiminalnd lo thinly bedded(*3 lo 100 Mini)

Bn Med'im lo nxlrcmc'y thicldy bedded(100 mm to >D m)

8p Graded hoddintj 8q S cour channels, l lnme s kuclures. load casls,

ball and pillow slruclures

8r C.-ilc.'iieous 8s CliluMid si;hisl *, chlniile-scricile schisl * ,

phylMe. s l^lo. h ighly loHated *. crenu'aied8t Fpiriiqinous

Bu Small-scale folds

8z Arnpl tbolilized {amphibole, game) or staurolile

porphyroblast!

Early Mplamorpliosed Felsic To Intermediate

Intrusive flocks 1 7,1 UnsinHividcd ?b On.iriz p'jfphyy7c F cUJr;p:ir porphyry

?d Ouarlz-lclUspar porphyry7t? fclsil?71 M.'ilic phenoctysts7s Ouarlz-se'icile schist

Mrl.irnniphoscci Malic Intrusive Rocks'

Gil O.lllliro

Gr: Mi'U|;iMiio

6d l fMir-[,n,il)l)ro6r H orn|ii''nd(! or a clinolile gabbio61 OuiiHz g.ihb'OGc) M-vnclublnr-lic n-^'brnOh f'l:i()ioLl:r;'.' phyrictribhio 1

G| Op 1 '!' 1 ;. gloinOKicrystic. oikocrysllc or

p'jiikiluN;trlic gabbro 6n Slmn-jly lolintod, chlorite sericite schisl -

Gr Aiiipl'iljjiiii?i i f], locatly with pervasive

fpiilnn/.ittnn or fpiifolrj Irndutfl Nil

I Mptanioiphjscd Ullramallc Intrusive Rocks'

5a PyiOM-nilo 5b f'r.'Mdolilo 5c Mclririjihhio 5t) r.l"p1-i"i •'.I'.iMiictf Ifixlu'O Hn 11-;l d rluicd ni;i[)iir'lilc disscminalcd

51 Smnil r,t:;\\c toldc. crenulaled

55 Uiic [hlyriiy r.cli'sl. chlorile schist, dolomiteschiol. :il;uriilo"l nu.Tilz veins

5y Cnrhon.'ilo-tich bicrcia

Inlrnvolcanic Mcltascdltnents-^ ^ ;1 Un3utnlivKl(?d

4 b Cli'fM^C l'';iiig]M'Misclicr1•Id S.niKl-.lt.iK-

lil M;iinl,' ihitily l;nntn;iled lo Ihinly bedded

(•c3 lo U10 nun)•1| M;iuil/ umliuin t irxMed lo cxlremely Ihickly

•In f-' niir 111.11111*;!-;, tlnnto slruclures, ball and

•Iq Mudn;iii:ly to highly loldcd. crenulaled,

Ay l l umhlrrnl'!. biolite, g arnel or slaurolila

____ pn.pliyrnl.lrr.K

- 3 ! lnlfrtnc(!l;il- In l fhlr Melnvolcanlc Rocks'

3b Prt:di iniiijMlly lull a'ld/nr Cfysl.il lull

3c l j tt;(|[.iiiiit;inlly lap-Hi lull and/or lapillistone

3d ricdciiiininlly lull breccia and/or pyroctaslic

3n lull l M "t f in inl(rrc;il;ilod wilh lull and/or lapilli

lull31 CJ'I irl/ |)lii!iK)r.iy:-,ls 3(] F'l.inuM l,i'-,r pluinocrysls

3s

3.v ;\T

ci'Hiiil" otlii'jl", cliloulo r.cricilc scliisl'. iiiii|ihiliMlu r,chi5l ". liiilily lolialed '. gneissic

MiiHc In lul' Miii'ill.iln MiM.lvnlcniilC llockj'

- ;1 ll.nilMli idnl21) Cilljv.i-il Hum2c M.I ,:,.;f ilini! In Medium T.niii'-tJ) How

2(J G il 'h tjid [Mii'diuin lo coarse giaiiiL'd) How *

?c Aui(^',i:.lir biccci.1 (liynloclnslile. How breccia.pillu.vl'i.'UMl

PH SrM'i .I'.il hi .itilvdi.il pl.iniofl.lf.0

2k 2n) 2M

M.ili.. |.lirnwiy'.lri hlri : .i. i iMinlull "y-,l;il lit!!, lapilli lulllull It'1" (l.i. pyioukislic tupcci.TAi icn .'ir pl.jr}iocl.Tse plienocrysls

(J lo 7 linn)On.iillr.yi".{.lili, i ir - 1 I tisl rl . cMn'iln r.oiir.ilQ schisl -. highlylnli.iliil". (inni'.'.k:Lpiilrli.-i'dAni[il ib;jlili7i'(), t(Kr\lly vvilh poivnsive

ppiifo i?;i!K)'t or ppidole liaclure lill

c Rocks

Hi d floIr; Mie.',, vi- (I'm: lo m"diijin grained} Mow

Id L'., il i 1 1' on l (i in;- In lin lo co;iist? (joined) How *

|p Aiiijcnl.ilijid.il MowII /\u!nf.t;rlic birccta ( hyaloclaslile, How breccia,

lg

Hi

||Ik

fi )f|rfifl:r;f.' phyric How ' (up to 3 cm subhedral

lo iiiilii-iJt.il pl;itjioi:lasB)

Omul/ -yrs

f cr.,1,'1 ilikni

\r. ( 'him ii" r- 1 hi 1 . l ''. rhliiiitp R(!ficilo schist *.

;i'ii|iln!i!jlL' schist, highly lolialcd. gneissic

lw t[mlili,-i'i(

Iz Ampl.ihrjlilijf'd, locjilly willi pervasive

(.'|iidnli;riliori nf npi'Jfilf? fracture Ml


from North Spirit Lake through Favourable Lake and on into Manitoba. This defines the

southern edge of the Sachigo sub-Province (or Gods Lake Block) of the Archean Superior

Province, and butts directly on the Berens River Block; this boundary partially marked by the

Bear Head Fault.

The rocks consist of mafic volcanics, lesser felsic volcanics, and their associated

intrusives, and quartz-poor to arkosic graywacke, plus conglomerate and minor quantities of

other sediments.

Mafics are primarily pillowed flows with minor pyroclastic units and form the bulk

(about 27a) of the sequence. Metamorphic grade varies from greenschist to amphibolite facies.

Felsics are relatively minor (^109fr) and sediments somewhat more than 1096. The balance

consists of diorite to gabbroic intrusives that are probably synvolcanic, plus

peridotite/pyroxenite/hybrid gabbro that may be synvolcanic and, in the work area, a biotitic

quartz diorite.

Two major, complex batholiths (granitic to dioritic) are found in the general area; the

more southerly is directly west of the claims: this is the Setting Net Lake Batholith which

consists largely of biotite quartz diorite to granodiorite, and lesser hornblende-biotite quartz

granodiorite.

This is a much simplified picture and a more detailed description can be found on ODM

3

Preliminary Maps P. 538 and P. 756 as well as in GR. 113; all are attributed to L.D. Ayres 1968-

1974.

HISTORY

According to L.D. Ayres, exploration in the belt began around 1927, and has been

ongoing since, although somewhat sporadic during the last two decades.

The principal occurrence is the Berens River Mine which lies but a few km. north of the

north end of Wolfden Res. holdings. From 1939 to 1948 more than V2 million tons were mined

and milled: this returned just under 0.3 oz. Au/ton and some lOoz. of silver plus minor quantities

of lead and zinc (*:0.759fc combined).

During the 60s Golsil explored the mine area and by 1968 had apparently defined a

reserve of 600,000 tons grading 0.18 oz Au., 7.8 oz Ag. wilh 2Vo Pb. and 3*7o Zn..

Other exploration in the area has exposed numerous showings of sulphides with

chalcopyrite, pyrrhotite, pyrite, ± sphalerite, ±galena (infrequently) and often very minor

molybdenite. Gold occurs with sulphides usually associated with quartz veins some of which

contain arsenopyrite; but it also occurs in "barren" quartz veins.

On the Wolfden holdings are found several showings of base metals and gold which have

been explored at various times by Senet Copper Mines, Getty, Newconex, Kega Gold Mines as

well as prospectors such as K. Koleff.

PRESENT PROGRAMME

HISTORY

E. S. Downie in the course of researching assessment files in Red Lake in late winter,

1996 came across leased claims held by Senet Copper Mines which were about to become

Crown Land once more. Senet Copper Mines held land covering two copper showings: i). The

McCloskey Showing in cherty sulphide I.F. and ii). to the northeast, the Main Copper or Senet

Showing in "felsic" volcanics. Near the east edge of this lease is the Yonge Showing of Kega

Gold Mines - gold with pyrite and chalcopyrite in a quartz vein within biotite quartz diorite and

parallel to its contact with the mafic volcanics. These were staked for Wolfden.

In addition, to the east of the showing, were two other gold/quartz vein occurrences on

the north edge of the main quartz diorite outcrops. These too were staked for Wolfden, as was a

swath of other available lands covering any favourable geology between the Senet/Yonge

Showings and Berens River Mines. Included in this acquisition, to the north of the Main Copper

Showing are the Springer Showing and the Watts-Durham Showing.

The Yonge Showing was drilled in 1944-45 by Kega Gold Mines; 20 drill holes in a very

small area - ^400 feet strike length) on outcrop: no casing or holes were found. The total

footage is 3660 from hand-written logs; the logs for holes 10 and 12 are missing, and not

included in this total.

No sample numbers or intervals are given, and the only evidence that gold was found

comes from clippings from the Northern Miner. The initial five holes defined a zone 300 feet in

length with all holes claimed to have intersected values - from O.lloz across 10 feet and 0.13oz.

across 25 feet to 0.34 oz. across 7 feet.

Later drilling reportedly encountered wonderful intersections such as 0.94oz. Au. and

10.14oz. Ag. across 2.5 feet and 3.94oz. Au. and 2.6oz. Ag, across 1.67 feet. Supposedly the

Watts (Watts-Durham) showing was to be drilled in 1946, but no further information is available.

In the 50s Senet drilled at least 23 drill holes on the Main Copper Showing for a footage

in excess of 9000. From the surface showings there appear to be two zones with reasonable

values: 1.996 Cu. across 8 feet (The West Zone or WZ) and 2.5596 Cu. across 18 feet (the East

Zone or EZ). Since the holes were not surveyed, it is difficult to come to a comfortable

evaluation of this work— one can but assume that all of the holes are dead straight, and this is

supported in part by the presence of minor flattening as portrayed in the available sections. The

drilling supports the presence of two zones containing reasonable copper values. The zones

appear to dip very steeply west at surface, and to roll over to steeply east at depth. This may be

6

an effect of the lack of hole surveying: where holes flatten (at depth), they usually diverge

laterally too, the net effect of this is to move intercepts closer to the hole collar - westward at

depth in this instance: this would partially compensate for the (apparent?) roll from steep west to

steep east.

On longitudinal sections, the surface expression is about 500 feet in length, but for most

of this distance extends to a depth of less than 100 feet. At 23N. (Senet Grid - about 8N. on

Wolf den Grid) the W. Z. is as much as 200 feet wide with a richer core about 100 feet in width,

to a depth of 400 feet vertically, and it is open to depth. This is true of copper values over

narrower widths at 24N., as well as for a width x 96 Cu. calculation at 23N. to 24N..

The E. Z. shows stronger copper values closer to 24N., but on a width x 9b basis it

apparently plunges northward from -lOOfeet at 23N. to -300 feet at 24N. (see accompanying

longitudinal sections).

Senet drilled another 10-12 holes on various other showings, not including the Yonge

Showing or the Contact Veins east of it.

Kega drilled holes on the latter, but across the veins, and parallel to the contacts, the

contact zones of the quartz diorite are untested, as at the Yonge Showing, a somewhat

unexpected omission.

Various geophysical surveys have been carried out - magnetic, electro'magnetic and an

early I.P.. The anomalies are moderate/weak to very weak and, except as seen at the Main

Copper Showing, seem not to correlate well with known mineralisation.

PRESENT PROGRAMME

LINE-CUTTING

The grid (Loc. Map B) is across the McCloskey, Main Copper, Yonge and Contact

Showings; it consists of a 2.5km. base-line about 1km. from the east shore of the south part of

Setting Net Lake, and roughly parallel to it at about Azimuth 327 0 -328 0 . Cross lines are turned

off at 90 0 at intervals of 100m..Lines 0-15N. extend westward to the lakeshore and Lines 16N. -

19N. to 5W., Lines 0-19N. are cut to 12E.; Lines 20N.-25N. are cut to 5W. and IE.. All lines are

marked by pickets erected at intervals of 25m.. The grid consists of 53.7km. of lines.

The contractor was Vytyl Exploration Services of Thunder Bay, and the work

complement varied from 4-8 men, decreasing towards the end of the work, which was completed

on 26th July.

MAGNETIC SURVEY

The ground magnetic survey covered the entire grid, but due to a scale error, the

magnetometer apparently failed to record some values or refused to give them up while the data

was being dumped into a computer.

8

The work was carried out by Vytyl Exploration Services, of Thunder Bay between the

20th and 30th of July, 1996; the operators were E.S. Downie, B. MacKay, and N. Laporte, all

from Thunder Bay.

Instrumentation consisted of two GEM GSM-19, continuous reading, proton

magnetometers - one as survey instrument and one as base-station set up at L.5N., 8+OOW..

These units read the total field to a claimed accuracy of ±0.01nT., but it is unrealistic to expect

much better than ±lnT. under typical field conditions, and under noisy magnetic conditions even

that accuracy probably cannot be achieved: all readings are reduced to the nearest unit.

The data from survey unit and base-station are dumped into a computer, transferred to

diskette, and forwarded to the Pro-Tech Drafting of La Ronge, Sask. for processing including

correction for diurnal variation. Pro-Tech provides the final maps to the clients specifications -

contours with/without colours, stacked profiles or other presentation. In this instance the data is

provided as black and while contour maps, and colour/conlour niiips having colour interval of

ZOOnT., and a map scale of 1:5,000. For colour maps, a vertical bar scale illustrates the

colour/value correlation. Postings are supplied on a separate plan at the same scale as other

presentations.

The background for the grid area is about 59,OOOnT, or somewhat less. The 200nT.

contour interval does not define some of the more subtle magnetic features, but provides fine

definition of the more important ones.

9

The most obvious feature is the large, strong anomaly in the west part of the grid. This

defines a moderately altered fine to medium grained peridotite. Where the contact of this unit

can be established from outcrop, it would appear to be defined by the 58,800nT contour - with

minor variance. This approximate magnetic value was used to interpret the contact where

outcrop is sparse or lacking. This anomaly is commonly ^,OOOnT. over background, and peaks

at M.OOOnT. at 9N., 8+50E..

Another prominent feature is a partially discontinuous linear anomaly running from 25N.,

7+OOE. To 7N., 2+75W.. This essentially defines the "felsic" unit of Ayres; the reasons for the

anomaly's discontinuity will be discussed in the section of geology. It varies in intensity from

essentially OnT. to 1700nT. above background.

An irregular anomaly just west of the south end of the previous anomaly appears to

define somewhat irregular magnetite mineralisation in mafic volcanics. This attains a peak of

^.OOOnT. over background.

The final noteworthy anomaly is arcuate (concave eastward) and extends from 15N.,

6+OOW. through 9N., 8+50W. to 0., 6+OOW.. This defines a single, magnetite-rich mafic unit. It

peaks at :^500nT. over background.

10

GEOLOGY

There are seven elements to the geological picture,

i). a western sequence of mafic volcanics in the north part of the grid and from the base-line

to the lake, south of 16N..

ii). an eastern sequence of mafic volcanics in the eastern 200m. or so of the grid,

iii). a major biotite quartz diorite intrusion in the southern part of the grid,

iv). a major peridotite body in the east half of the grid between the Q.D. and the eastern mafic

volcanics,

v). a narrow band of silicified, mineralised volcanics trending north-north-westerly across

the centre of the grid and described by Ayres as "felsic",

vi). a mafic intrusive (?) within the western mafic volcanics.

vii). a small (area) zone of argillite, chert, sulphides and magnetite within the western mafic

volcanics.

i). The western mafic volcanics are generally fine grained, massive rocks in the

western part of the unit with local amphibolite, or hornblendite phases-possibly

metamorphic, although the general grade is greenschist rather than amphibole.

These are massive to pillowed with only minor, local breccia or

agglomerate.

11

Eastward, towards the base-line, there are more pillows and pillow

breccias with minor agglomerate and fine, magnetic zones that rust prominently

and may best be described simply as iron formation. These may in part be

altered/mineralsized by the Q.D. to the east (?).

The magnetite phases are generally narrow and discontinuous. The most

prominent magnetite content observed is between 3 and 6W. (max. width) on lies

5-10N. with a spike of magnetite rich volcanics tapering away at about 4+50W.

on L12N.: from the magnetics it appears to die completely on L.13N..

The other zone is the arcuate anomaly noted in the section, MAGNETIC

SURVEY. The anomaly to the south of L6N. is not as prominent as to the north:

magnetite is observed to be as prominent in the one area as in the other.

At the very N.W. of the grid the volcanics frequently grade into

hornblendite.

ii). The eastern mafic volcanic sequence consists of thin flows interbedded

with more voluminous agglomerate. There is little flattening of the fragments, but

a distinct aligning parallel to the schistosity/foliation. Carbonate and minor

quartz-carbonate veining is prominent, and carbonate is locally quite enriched,

giving the rock a bleached look. This is presumably what shows on P.M.756 as

12

felsic pyro'elastics of which none was found in this area.

iii). The biotite quartz diorite is generally medium grained, flesh coloured and

contains lS-25% quartz and S-15% biotite. It is as much as, or more than 1200m.

wide at the south end of the grid and lies predominantly east of the base-line. It

narrows northward to about 700m. in width at 9N. and then narrows sharply to

150-200m. at UN. and tapers to nothing at 20N., 4E..

iv). The peridotite is a fresh-looking, fine to medium grained, hard, gray to

greenish gray, very magnetic to but moderately magnetic unit. Serpentinisation is

variable but never reaches a content that permits the rock to be scratch easily. The

outcrop rarely weathers to the "typical" orange-brown.

This unit attains a maximum thickness of almost 700m. in the north

eastern quadrant of the grid. It narrows sharply at ION. and tapers to nothing just

south of LIN., 9+50E..

v). Ayre's "felsic" unit is the first area of major conflict. This is not felsic

volcanic. The unit is quite variable along its length on the grid varying from quite

felsic to quite mafic.

Where the rock is felsic around 20N., it is obviously felsic. It is also quite

13

magnetic. When looked at under a powerful (20x) hand lens this fine grained

rock does not differ noticeably from the Q.D.. From 18N. or 19N. southward the

rock is "intermediate" to quite mafic by L/14N. Even the intermediate phase is

seen to be a felted mafic that has been silicified. Further south-from 12N. to 8N..

- the "felsic" parts probably represent a f.g. Q.D. sill and the "intermediate"

volcanic represents silicified mafics. This is particularly obvious at the trench on

the Main Copper Showing.

The discontinuity in the magnetics may also provide a clue- the less felsic,

less siliceous, the rock is, the less magnetic. I believe that the magnetite in the

"felsics" is the sole remnant of the mafic volcanic that is all but totally re'sorbed

by invading Q.D..

Also, in support, the mineralisation at the Main Copper Showing, consists

of chalcopyrite and pyrrhotite with local veins of magnetite and even minor

grunerite: pyrite and sphalerite are so negigible in content as to pass virtually

unnoticed. Since cobalt and nickel are barely, or are not anomalous, this unit will

have to stand as mafic on copper content alone - a VMS - style deposit this is not.

vi). A medium grained, dark green, massive unit with occasional, peripheral

basaltic or gabbroic (^20*?fc feldspar) phases. This is mapped by Ayres as

predominantly serpentinised peritotite and minor pyroxenite. It is, in fact,

14

predominantly pyroxenite with minor hybrid gabbro (^2096 feldspar).

The Pyroxenite is a felt-like mass of prismatic crystals, locally elongate

enough to be hornblende - the texture is hornfelsic and that may be the best term,

as this rock at 8W. on Lines UN. and 12N. is apparently part of the strong

arcuate, magnetic mafic volcanic, but the rock is felted, medium - grained and

massive as seen in outcrop.

The unit extends from 6W., 6N. northward to 8W., 12N. hooks around UN. and 12N. as

far east as 4W. and tapers southward to 4+50W. at 9N.. It resembles an extracted molar in

which the eastern root is stunted.

vii). This unit almost has no business in being. It is a modest unit of short

strike length consisting of chert, silicified argillite, and argillite or very fine, mafic

volcanic debris. Mineralisation consist of pyrrhotite, magnetite, pyrite and

chalcopyrite in decreasing order of abundance: cherty I.F.. This is host to the

McCLoskey Showing on L5N. just west of 5+00W..

Geology is presented on a map of scale 1:2,500.

15

MINERALISATION

The McCloskey Showing and the Main Copper Showing have been partially described

under HISTORY, and under GEOLOGY.

The McCloskey is trenched immediately north of L.5.N., parallel to the line just west of

5W.. Casing at the west end of the trench indicates a drill hole directly under it. The

mineralisation is stong in the trench, but is quite light 15-20m. north and was not found to the

south.

The trench was sampled by M. Kremko across 21m. (Samples 25758-771 inclus.). From

this it is found that the most easterly - and least impressive sample - gives 1.196 Cu and 72 g.

Ag./T.., otherwise there are anomalous Cu. values, but none in Ag. - or Au.. Co never exceeds

246 p.p.m. and Ni. 810 p.p.m..

The Main Copper Showing is impressive where stripped, an outcrop 20m. or more in

diameter just north of L.8.W., and west of 2W.. There is minor evidence of the zone to the north

and south, but it is minor. M. Kremko sampled this zone across more than 10m. (25786-793

inclus.).. All Cu. values exceed Q.5% and the best is 2.69fc. Au. and Ag. are weakly anomalous,

and Co. and Ni. are barely anomalous. This body will survive solely on its copper content, and

that must show enrichment and volume at depth - but that may be, and the longitudinal sections

16

indicate this possibility. It is recommended that a deepish hole - to -175m. vertically be drilled

50m. north of the showing and west of it.

D. Ho of Freewest took six (6) samples (6DHO53R-57R) in this trench with similar

results. Samples 49R-52R N. and S. of the trench returned substantially poorer values.

Longitudinal sections have been constructed from available data. The simple values

(96Cu.) for east and west zones on WRSN.OOl, and a width x value (feet96Cu.) section for each

zone (EZ: WRSN.002 and WZ: WRSN.003). The latter show the WZ to be nearly vertical and

possibly opening up at depth; the EZ plunges northward (grid) and appears to be uniform in

width to depth.

The Yonge Showing occurs near the base-line and sub'parallel to it between 7 and 8 N..

This consists of a mineralised (chalcopyrite and pyrite) quartz vein in biotitic quartz diorite. It is

sub'parallel to the contact of Q.D. and mafic volcanics which occurs about 40m. west of the

trenches. Some Kega Gold Mines drill holes mention fragments of mafics, but did not drill into

the main body of the volcanics.

M. Kremko sampled the various expsoures (Samples 25772-780 inclus., and 782-785

inclus..) from S. to N.: some had low values, some modest but four exceeded 0.25 oz. Au/T

including a high of 0.468 oz. Au.. All samples are anomalous in Cu. and Ag. with two exceeding

Z.5% Cu. and giving about 8 oz. Ag./T.

17

24. N. jfioZiZf: tt-H- W. N.0.8S/Z X.

i f-0/9

o-zs/s1 ttlL

o


Setting Net Lake Property

Longitudinal Section

/oo 2 00 M ain Copper Showing; /eet. from Senet Copper Mines drilling

ve'f-t..

24. N.Wain.Cu.

. yV. Ô.N. /&.K

o.as/3 x./ l j \ >^.0 Ia-ss" x y '7 l '

' V. 8"?/o

7

d. d. h. mt'erse.c.t/ort: U/.

A e.

l l \ \\ \ ^\\ \a \

\

WEST ZONE

/oo

-Sc.ct.Le. : feet.

Aof/f. 4nd Ve f t..

./O




Main Copper Showing

from Senet Copper Mines drilling

. 002.

X. d-d. h.

t -83/4 t~*

/.e.

./Y.O. x A \ "~

l W?* \ 22 \ \'±0 \ }

\ '-*7/.

J l'•"/* x j i '

''•20/3 f / l 0/' t /H*

' 7 7 '' / /x/

4y f

U/. zone

E.EAST ZONE

10 O

/tor*/f. And Ve f t..

J^

r

/6./Y

* c?-38y'13.

HIL O

-- 330"




Main Copper Showing

from Senet Copper Mines drilling

OV/Gt. :/o/

D. Ho took samples 6DHO20R-33R inclus.; one of these, 21 R, gave 8oz. Au./T and 30R

and 32R give 0.678 oz. and 0.927 oz. respectively. I suspect that Mr. Ho "grabbed" for "best" .

E.S. Downie took samples at the Yonge Showing, including several in wall rock: KEGA -

Q.P., KEGA- WR, and K-WR-1 to 6 inclus. all of these return substantial values in gold - as high

as 1.318 oz./T..

These are interesting as it is not known if Kega Gold Mines sampled the weakly pyritised

Q.D. noted in the drill logs, and at a distance from quartz veins. It is this fact, in conjunction

with the obtained (Wolfden) and reported (Kega) values, that demands a new drill programme:

probably 4 holes drilled at 25m. intervals from E. of the showing into the mafic volcanics. All

mineralisation, even lacking quartz vein association should be sampled.

Mr. Ho's samples (6DHO34R-46R) for theContact Showings east of the base line along

the N. margin of the Q.D. are generally poor in gold; 35R, 20cm. of quartz vein with py. and cpy.

gives 0.335 oz. Au/T., 44R gives 0.058.

The author also sampled The Contact Showings (Samples 25810-822) and the results

verify those of Mr. Ho - mostly negligible gold values to sparse, weak values are achieved.

The author also sampled many modest mineralised areas occurring in the western mafic

volcanic suite where it lies east of the "felsics" and west of the north end of the main quartz

18

diorite body. The results are unspectacular. A chalcopyrite occurrence just west of the base-line

at 10+75N., and sampled for "representation" rather than "best" gives values around G.5% Cu.

and from 0.6 to 1.2 oz. Ag./T. However, it is worth noting that there is more minerlisation in this

"wedge" of volcanics from 6N. to UN., than in all the rest of the mafics on the grid. The

mineralisation has some bond with the Q.D. and the entire mafic/Q.D. contact southward may be

of interest.

CONCLUSIONS

The McCloskey Showing shows neither the extent nor the values to justify additional

investigation.

The Main Copper Showing is somewhat light in values, and of limited extent. At depth

fclOOm.) according to sections from assessment files and constructed longitudinal section, the

zone opens up, and it is noted that values increase. Neither is wildly impressive, but the potential

must be investigated. One drill hole is warranted 50-55m. north of L.8N. and some 75-80m.

back (west) from the zone to be drilled at -60 0.

Due to the uncertainty of the location with depth, contingency funding for a second hole

is necessary should the first intersect the zone at a depth considered to be too shallow, or if the

first diverges too much laterally.

19

The Yonge Showing returns handsome values at surface, and did so from drill results

only known from NORTHERN MINER clippings. It is not known if sulphide mineralisation

(reported in drill logs) in Q.D. removed from any quartz veins was sampled. The Q.D.,

particularly in proximity to the mafic volcanics, may have more potential than any other area on

the property including The Yonge vein itself.

It is felt that the Contact Showings are, at best, poor. The Yonge Showing is in a similar

location with respect to the contact the Q.D.; a hole under the most easterly showing, drilled

northeasterly to the Q.D./peridotite contact is justified.

RECOMMENDATIONS

i). A drill hole to intersect the Main Copper Showing at a depth of 150m.: i.e. 50m.

N. and 75m. W. (GRID) of the exposure 180m.

ii). Contingency drill hole for this showing. 200m.

iii). Four drill holes to test The Yonge Showing and adjacent Q.D./Mafic Volcanic

contact - all at 0+30E. and 7.N., 7+33N., 7+66N. and 8.N. drilling grid W.

500m.

iv). Drill hole at about 7+35E., 7+70N. drilled N.E. (GRID) to test E. Contact Vein

120m.

v). A max-min hlem survey using 125-150m. long cable on Lines 4N. to 12N. from

20

6W. to 4E. To test the Main Copper Showing and the Q.D./Mafic Volcanic

Contact. 9km.

TOTAL 1,000m.

Further recommendations concerning these, the better showings, must follow this initial

evaluation, as must consideration given to expanded investigation on lesser targets elsewhere on

the property.

Respeq

lain F. Downie, P. Eng (Ont.)..

21

APPENDIX I

McCLOSKEY SHOWING 5+03N., West of 5+OOW (approx)

Sample No.

2575825759257602576125762257632576425765257662576725768257692577025771

Gold Silver Copper Cobalt Nickelppb (oz/T)

^^1718149^7^9141713

g./T (oz/T)

•ci2211

*d*cl.ci•ci2222

ppm (9fc) 96427242897274881688441829

11201052832760

ppm.386524623581152404754546051146141

Ppm162139578573149307104546810689250272463482

22

THE MAIN COPPER SHOWING 8+1 ON., west of 2+00W. (approx)

Sample No.

2578625787257882578925790257912579225793

THE MAIN

Sample No.

6DHO49R6DHO50R6DHO51R6DHO52R6DHO53R6DHO54R6DHO55R6DHO56R6DHO57R

Goldppb (oz/T)

21212676525967

228153

COPPER SHOWING

Goldppb (oz/T)

1818254112337

20117937

Silverg.7T (oz/T)

920131515163220

plus showings

Silverg./T (oz/T)

778

282721225525

Copperppm ( W*)

5752Ô5 (1.3)75209120MO5 (1.03)

(1.05)(2.6)

5264

N. and S. at

Copperppm (9fc)

Cobaltppm.

56655256661555335

±25m.

Cobaltppm.

THE YONGE SHOWING

Sample No.

577257735774577557765777577857795780

Goldppb (oz/T)

584975(0.145)4829742(0.284)16503(0.468)4543947(0.115)6378311(0.242)

Silverg./T (oz/T)

Copperppm ( W*)

Cobaltppm.

Nickel Ppm

58576749841048627

Nickel Ppm

Nickel Ppm

23

57825783578457856DHO20R6DHO21R6DHO22R6DH023R6DHO24R6DHO25R6DHO26R6DHO27R6DHO28R6DHO29R6DHO30R6DHO31R6DHO32R6DHO33RK-Q1K-Q2K-WR-1K-WR-2K-WR-3K-WR-4K-WR-5K-WR-6KEGA - VW

-CONT-4.8-N.Cu-QV-QP-WR

2412247710927(0.319)23561389 15

^8.0) 608^19)815 123974(0.116) 162450 142667 781748 41173 526 3

11.113(0.324) 712^20.5)23232(0.678) 1011523 5931788(0.927) 160^5)177 4

8697(0.254) 1324490(0.131) 1311354(0.331) 1445199(1.318) 541311 3627781 (0.810) 33513 13778 135691(0.166)3533(0.103)6311112(0.324)13023046 (0.672)6570(0.192)

THE CONTACT ZONE (Showings: E on Lines

Sample No.

6DHO34R6DHO35R6DHO36R6DH037R6DHO38R

Gold Silverppb (oz/T) g.7T (oz/T)738 611470(0.335) 15175 54828 1023 4

:^05 (2.46)2644153629846680296016562844

7 A 8 N.)

Copperppm Cfa)

Cobalt ppm.

Nickel Ppm

24

6DHO39R 93 26DHO40R 111 26DHO41R 121 986DHO42R 294 46DHO43R 218 76DHO44R 1974 26DHO45R 316 36DHO46R 7 l6DHO47R 1037 86DHO48R 89 525810 325 122 (~4) 137225811 181 ^ 525812 14 3 14025813 13 2 8925814 441 4 69625815 9 2 11025816 1576 4 42225817 295 17 41725818 236 15 74425819 31 7 56025820 4013(0.117) 12 125625821 233 16 20425822 199 22 100

CORE SAMPLES (Main Copper Zone - not "ore") -Hole No.'s unknown

Sample No. Gold Silver Copper Cobalt Nickel ppb (oz/T) g.7T (oz/T) ppm (96) ppm. Ppm

25751 63 5 81125752 18 3 132

-25753 22 7 250825754 396 39 :^05 (2.29)25755 31 2 44025756 7 2 10025757 8 2 167

25

MISCELLANOUS

Sample No.

258012580225803258042580525806258072580825809258232582425825258262582725828258292583025831258322583325834

Goldppb (oz/T)2591613142355^^3882466^^6171016285050

Silverg.lT (oz/T)681057141112343222.223193724

Copperppm (92924596820485584558443681741723423061220277238210308190422420846246400

Location

7N., 2+52W.. 8+50N., 1+85W.

8+95N., 1+75W. ION., 1+25W.. 10+55N., 0+70W.tt M

21N., 3+20E.. 8+75N., 2+75W.. 10+40N., 1+20W, 10+90N., 1+25W. 11N..O+80W..tt 99

11N..O+75W.. 11N..O+70W.. UN., 0+45W.tt 99

10+70N., 0+03W.,

26

18319ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.

1070 LITHIUM DRIVE, UNIT 2 THUNDER BAY, ONTARIO P7B 6G3

PHONE (807) 623-6448 ) 623-6820^(807)

WOLFDEN RESOURCES Aug 7, 1996

Job# 9641039

SAMPLE # Accurassay Customer

123456789

1011 Check12131415161718192021 Check2223242526272829

2575125752257532575425755257562575725758257592576025760257612576225763257642576525766257672576825769257692577025771257722577325774257752577625777

Goldppb

631822

3963178

c5c5c5<51718149

^57

<59

147

171358

4975482

974216053

454

GoldOz/t

0.002cO.OOlcO.OOl0.012

cO.OOlcO.OOl<0.001cO.OOlcO.OOl<0.001<0.001<0.001cO.OOl*0.001<0.001cO.OOlcO.OOlcO.OOlcO.OOlcO.OOlcO.OOlcO.OOlcO. 0010.002 0.145*0.014 k0.2840.4680.013

Certified By:


RECEIVEDJUS) 8 H 1-

GEOSCIENCE ASSESSMENT OFFJCC

ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.

S.M.L 1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3

PHONE (807) 623-6448FAX (807) 623-6820Page 2

WOLFDEN RESOURCES Aug 7, 1996

Job* 9641039

SAMPLE #Accurassay Customer

3031 Check32333435363738394041 Check42434445464748495051 Check5253545556575859

257782577825779257802578225783257842578525786257872578825788257892579025791257922579325801258022580325804258042580525806258072580825809258102581125812

Goldppb

39474230637

831124122477

109272356 2121267299525967

2281532591613141323554.5^38

32518114

GoldOz/t

0.1150.1230.0190.2420.0700.072 .0.319 r0.069 t 0.0060.0040.0020.0030.0020.0020.0020.0070.0040.008

cO.OOlcO.OOlcO.OOlcO.OOlcO.OOl0.002

cO.OOlcO.OOl0.0010.0090.005

cO.OOl

Certified By:


M , 1070 LITHIUM DRIVE, UNIT 2 . L. ^ THUNDER BAY, ONTARIO P7B 6G3

PHONE (807) 623-6448 FAX (807) 623-6820Page 3

WOLPDEN RESOURCES Aug 7, 1996

Job* 9641039

SAMPLE # Gold GoldAccurassay Customer ppb Oz/t

60 25813 13 cO.OOl61 Check 25813 11 *:0.00162 25814 441 0.013" l63 25815 9 cO.OOl64 25816 1576 0.04665 25817 295 0.00966 25818 236 0.00767 25819 31 *:0.001 '{68 25820 4013 0.117 /J69 25821 233 0.007 ^70 25822 199 0.006 ^71 Check 25822 113 0.00372 25823 8 ^.00173 25824 246 0.00^74 25825 6 -cO.OOl75 25826 <5 -cO.OOl76 25827 <5 <0.00177 25828 6 *:0.00178 25829 17 *:0.00179 25830 10 -cO.OOl80 25831 16 -cO.OOl81 Check 25831 22 <0.00182 25832 28 <0.00183 25833 50 0.00184 25834 50 0.001

Certified By:


S.M.L. 1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3

PHONE (807) 623-6448. FAX (807) 623-6820

WOLPDEN RESOURCES INC. 4283 LOCH LOMOND RD. THUNDER BAY, ONTARIO PTC 4Z2

Aug 7, 1996

Job* 9641039

SAMPLE f Accuraasay Customer

123456789

1011121314151617181920212223242526272829

25751

123456789

101112131415161718192021222324252627

Copperppm

811132

2508s.10, 000

44010016796

427242897274881688441829

11201052832760266

s-10,00013722088

:.10,00016726480275

Silverppm

537

39222

*:1^2211

*:1*:1-ci^22222

728

7323410452

Certified By:J


S -, , 1070 LITHIUM DRIVE, UNIT 2 fSj , L . THUNDER BAY, ONTARIO P7B 6G3

PHONE (807) 623-6448 FAX (807) 623-6820

Page 2

WOLFDKN RESOURCES INC. Aug 7, 1996

4283 LOCH LOMOND RD.THUNDER BAY, ONTARIO Job* 9641039

P7C 4Z2

SAMPLE # Copper Silver Accuraasay Customer ppm

30 28 3232 32

31 25782 2272 2132 25783 2528 1733 25784 :*10,000 25034 25785 2012 30

35 25786 5752 9

36 25787 :*10,000 2037 25788 7520 1338 25789 9120 15

39 25790 s-10,000 1540 25791 :.10,000 16

41 25792 :*10,000 32

42 25793 5264 20

43 25801 924 6

44 25802 5968 8

45 25803 2048 10

46 25804 5584 5

47 25805 5584 7

48 25806 4368 1449 25807 174 l

50 25808 172 l

51 25809 34 l

52 25810 1372 12253 25811 5 ci54 25812 140 3

55 25813 89 2

56 25814 696 4

57 25815 110 2

58 25816 422 4

59 25817 419 17

Certified By:


S.M.L . 1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3

PHONE (807) 623-6448, FAX (807) 623-6820Page 3

WOLFDKN RESOURCES INC. 4283 LOCH LOMOND RD. THUNDER BAY, ONTARIO P7C 4Z2

Aug 7 , 1996

Job* 9641039

SAMPLE ft Accurassay Customer

6061626364656667686970717273747576

2581825819258202582125822258232582425825258262582725828258292583025831258322583325834

Copper ppm

744560

125620410023061

220277238210308190422

420846246400

Silver

157

1216222

343222223

193724

Certified By:

Ontario Ministry ofNorthern Developmentand Mines

Declaration of Assessment Work Performed on Mining LandMining Act, Subnotion 65(2) and 66(3), R.S.O. 1990

Transaction Number (office use)

Assessment Files Research Imaging

of subsections 65(2) and 66(3) of the Mining Act. Under section 8 of the ) review the assessment work and correspond with the mining land holder, j Recorder, Ministry of Northern Development and Mines, 6th Floor,


Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary)Name

Address y 'y of 2 /^

//^cj^JÊff" xTName

\Jou*J HAddress

c?^ ^^'tcct^^9i

'^^ - ^ A,,- */Vcr Se- c/'Xrc ^~5 jf f^C -

A /0,~-.~* X?X7A

-5 ^1 S* l x-s. / -~S -o

/ot.Lor^

) ^xLjt^^C- /ters

er Q*)7- s^2 x/ l y 7*

Cflent Number

Telephone Number

#o 7 . y ?Fax Number

#0? - /7.Client Numbery 7^"^Telephone Number //y/ ô' 7

1S - C 7 ^.3

? - /777

' T 0

-/(? S '7Fax Number

2. Type of work performed: Check ( s ) and report on only ONE of the following groups for this declaration.

|T7i Geotechnical: prospecting, surveys, r— i Physical: drilling, stripping, f— i Rehabilitation Ifcl assays and work under section 18 (regs) l—1 trenching and associated assays *— '

Work Type ^ lAie

#

Dates Work e Performed FrorT

cutrtMC, y MAC* ^ u(2.vxe.--j Geoi-ocxV ;

pCiOCv

10/07.9(0 To O *S &J J(o /Dty | Month | Y*w Oiy | Month Yaw

Global Positioning System Data (H available) Township/Area

M or G-Plan NumberC7 - 1879

Office Use

Commodity

Total $ Value of , Work Claimed y-^.frrij

NTS Reference

Mining Division VB * P. iAô- ^-/^CCj

Resident Geologist^Tl T/ yDistrict ^J h fJzjL^

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)

Name ^

Address -.^ . —— ~—. , r—^

oloSS (YloOMOê- p lace. /huna^^ iSuJName ' 7

Address

Name

Address

Telephone Number

Fax NumberSol - -5-77 - /977

Telephone Number

Fax Number

Tetophc

FaxNu

4. Certification by Recorded Holder or Agent

me Number

-bO CCD VE D iv m •••B ^t^r mmmm B V •••i TTT^

MAR - S 1998 ,o^GEOSCIENCE ASSESSMENT

nccipc

1, /CCA-Vq/O J) Ot^ ^j f (^ , do hereby certify that 1 have personal knowlerine nf the facts set(Print Name)

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during

or after its completion arjd^to thefS^t of my knowledge, the annexed report is true.

Signature

Agent's Address ~?

IS /^

Telephone Number

Date~JA

8ax Number

7

5. Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form.

Mining Claim Number. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

TB 7827

1234567

1234568

ka l 2 l S O "4 4

KO- l 1 1 S C H S"

Ut 1 2 1 S C 4 C

K*C iiiSo.V-?

"t ) z i s f S 2.KELUKZ33

*

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

lwlU

l t,

(^9 '

C

Column Totals

Value of work performed on this claim or other mining land.

S26, 825

0

S 8, 892

i" O OO1

^L ^9

#73. /Ten4 9 iCOC

* 4, Soo

M M ^, ooo

Value of work applied to this claim.

N/A

S24,000

34,000

*4? tyorf"ty@P i Q6O

"jCJi . ©OO

* C, 660

* 3,^,00

K- 1, 400

——— i —————

Value of work assigned to other mining claims.

S24,000

0

0

fegcjz&zr* 7oo -^* "~}GO '

f^fe^tfffiQ* fee

s ^~^

* 1^00

Bank. Vr,'ue of work to. be distributed at a future date.

S2,825

0

S4,892

^

^^

^^

fi ij^&oott

*? u f (y-)^^-^

* |gr00.0tl. td

(Print Full Name)

subsection 7 (1) of the Assessment Workx

the claim where the work wayoone/

, do hereby certify that the above work credits are eligible under

Signature of Recorded Ho

ition 6/96 for assignment to contiguous claims or for application to

Date

6. Instructions for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check ( ^ ) in the boxes below to show how

you wish to prioritize the deletion of credits:^3^ 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.

D 2. Credits are to be cut back starting with the claims listed last, working backwards; or

D 3. Credits are to be cut back equally over all claims listed in this declaration; or

4. Credits are to be cut back as prioritized on the attached

Note: If you have not indicated how your credits are to be deleted, credits v followed by option number 2 if necessary.

ippendixjDr as follows (describe):

RECEIVED, MAR - 9 1998^

GEOSCIENCE ASSESSMENT) III uu uul UacFrf Ifiîii ihe-Bank first,

For Office Use OnlyReceived Stamp Deemed Approved Date Date Notification Sent

0241 (02/96)

Date Approved Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

Ontario Ministry ofNorthern Developmentand Mine*

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal Information collected on this form Is obtained under the authority of subsection 6(1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act. the Information Is a public record. This Information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed lo the Chief Mining Recorder, Ministry of Northern Development and Mines, 6th Floor, 933 Ramsey Lake Road. Sudbury, Ontario. P3E 685.

r -

Work Type

L i *J &C-V-4 T r i /o ex

MA-CV Stiffv&yG ec CD a f 5*T

Units of WorkDepending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

S3 . 7 ^

5~3 , 7 /or-,

o?/ tfki/S

Associated Costs (e.g. supplies, mobilization and demobilization).

/?s*.^s

/*7v6 y tie sn 0& - y^^.s/r?66 V Avwo - '/&MS.

/

Transportation Costs

Food and Lodging Coats

RECEIVEDMAR -1 1998P|p|iM

Cost Per Unit

•&33S

t 90^t/GC,

f

To al Value of Assessment Work GEOSCIENCE ASSESSMENT

OFFIQF

Total Cost

t -z i/r^êf r y /ox.

4. # ,3,r-9 j (,oo ~

3-70 -"-2/y/o-^

M J fi* -t*1 f

fft-,99*-2*-

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 10046 of the above Total Value of Assessment Work.2. If work Is filed after two years and up to five years after performance, tt can only be claimed at 50*ft of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0 .50 Total S value of worked claimed.

Note:- Work older than 5 years Is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

If t*JA*J iOCuo*J'tr , do hereby certify, that the amounts shown are as accurate as may(please print full name)

reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on

the accompanying Declaration of Work form as

to make this certification.(recorded holder, agent'or sial* company position with signing authority)

| am authorized

Signature Dale

Ministry ofNorthern Developmentand Mines

Ministers du DeVeloppement du Nord et des Mines Ontario

JulyS, 1998

Ewan DownieWOLFDEN RESOURCES INC.4283 LOCH LOMOND ROADTHUNDER BAY, ONTARIOP7C-4Z2

Dear Sir or Madam:

Subject: Transaction Number(s):

Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (888)415-9846 Fax: (705) 670-5881

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Submission Number: 2 .18319

StatusW9820.00027 Approval After Notice

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact Steve Beneteau by e-mail at [email protected] or by telephone at (705) 670-5855.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 12526

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.18319

Date Correspondence Sent: July 08, 1998 AssessonSteve Beneteau

First Claim Number1215044

Township(s) l Area(s)SETTING NET LAKE

StatusApproval After Notice

Approval Date

July 08, 1998

Transaction NumberW9820.00027

Section:14 Geophysical MAG 12 Geological GEOL

The material submitted in response to the 45 Day Notice dated June 02, 1998, has corrected all deficiencies associated with this submission. Accordingly, assessment work credit has been approved as outlined on the Report of Work form that accompanied this submission.

Correspondence to:Resident Geologist Red Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):Ewan DownieWOLFDEN RESOURCES INC.THUNDER BAY, ONTARIO

JOHN A. POLLOCK WILLOWDALE, ONTARIO

Page: 1Correspondence ID: 12526

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DWQ.-WRSN.005

WOLFDEN RESOURCES INC. T and H RESOURCES LIMITED

GROUND MAGNETIC SURVEY - POSTINGS SETTING NET LAKE

INSTRUMENT: GSM 19 MAGNETOMETER DATE; JULY 1996BASE STATION CORRECTED

DRAWN BY: PRO-TECH DRAFTING SERVICES - LARONGE SASK

VYTYL EXPLORATION SERVICES

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DWQ.-WRSN.006

WOLFDEN RESOURCES INC. T and H RESOURCES LIMITED

GROUND MAGNETIC SURVEY -CONTOURS SETTING NET LAKE

INSTRUMENT: GSM 19 MAGNETOMETER DATE: JULY 1996BASE STATION CORRECTED

DRAWN BY: PRO-TECH DRAFTING SERVICES - LARONGE SASK.

VY7YL EXPLORATION SERVICES

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Geology Map

RED LAKE MINING DIST., ONT..

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EXPLORATION 1996 SETTING NET LAKE

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