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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
WRSN.005 in pockets at rearWRSN.006WRSN.007
l [l S—
1' l' l'iiiiliW
'!'!'in
j'i.1 'i .i
WO
LFD
EN
R
ES
OU
RC
ES
LIM
ITE
DLocation M
ap 'A'
_ __ _ _ _\ _ __ _
l _ — — — —
3938'
37 36 35 34' 3332' 31'
SETTING NET CREEK G-1878WOLFDEN RESOURCES LIMITED
Location Mao 'B'
93 0 30'
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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
.'/^D-^J-
x -Jb L—) p-"7 ^r/ 3 se
a.-asb^rv^j t-a\io\!rx*f' L'ate"^:ai3^3!bf™ 0 "
Area of GridnM^XV^-v
'
/-f. v-4 *u - s^'j l "~^ ~ l ra*Ui;^ ,. ''sj?ti' ' ~J^' 86 C*U U-*
WOLFDEN RESOURCES LIMITED
^ SETTING NET LAKE AREA
GEOLOGY
OGS MAP No.2262 Scale 1 l 2 50,000 JIT- -V,"S- ^ ', , -
^-^iJ'-' ^* ' 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
WOLFDEN RESOURCES LIMITED
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
WOLFDEN RESOURCES LIMITED
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. ^O.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
WOLFDEN RESOURCES LIMITED
Setting Net Lake Property
Longitudinal Section
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"
WOLFDEN RESOURCES LIMITED
Setting Net Lake Property
Longitudinal Section
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*)
5752^O5 (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:
53C13SE2001 2.18319 SETTING NET LAKE 020
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:
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
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:
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
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
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
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:
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
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,
53C13SE2001 2.18319 SETTING NET LAKE 900
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^J^Eff" 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/ ^o' 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. iA^o- ^-/^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 (YloOMO^e- 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 Ifi^iii 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^^ef 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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2000N
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800W——i—— 600W ——i—— 400W 200W O 200E 400E 600E 800E IOOOE 1200E
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53C13SE2001 2.18319 SETTING HKT LAKB 210
LIL
2600N
2400N
2200N
2000N
1800N
1600N
1400N
1200N
1000N
800N
600N
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too1:5000
'^...1.00_______200 300
(meters)
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
1200W 1000W
2600N -
2400N -
2200N -
2000N -
1800N -
1600N
1400N
1200N
1000N
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600N
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-2400N
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-1800N
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- MOON
- 1200N
1000N
- 800N
- 600N
- 400N
-200N
100Scale 1:5000
O 100 200 300-
(meters)
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
LEGEND.,-'*\ outcrop or a re.a. &C outcrop
' ^
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Geology Map
RED LAKE MINING DIST., ONT..