PHONE 807-223-rtOSO
CHESTER J. KURYLIW. M.Sc.. CONSULTING GEOI^JGIST
46 INGALL DR. DRYDEN. ONTARIO P*N SB
52C11NE0010 I/V9510-00150 HALKIRK 010
REPORT
onARMSTRONG-KURYLIW NICKEL PROSPECT
HALKIRK IMP. RAINY LAKE AREA OF ONTARIO
DI^IOND DRILLING
Nov 20, 1 995'CHESTER J. KURYLIV/
KENORA - MINING DIV
JAN l O WSAM PM789 10 11 12 1 23456
52C11NE0010 W9510-OC150 HALKIRK
01OC11:33X1
Project Location,'iccess, Property
Regional C-eology
Local Geology
Introduction
Results of Diamond Drilling
Stru ctural Geology
Economic Geology
Con elusions
Recommendations
Certificate
rage
1.
1.
2.
2.
3.
^.
5.
5.
6.
7.
ILLUSTRATIONS;
Cross-Section, D.D.H. 95~3 (Packet in Report)
Claim Kap, D.D.Hoie 95-3 ( Halkirk 4 Farrington Twp.s)
l inch = ^0 Ft.
l in di s ^ mile
Portion of Geologic Tflap RICE BAY l in c h= ^ mile Ttap 22^3, showing D.D.H.95-3
Portion of y.::.R. O.G.3. l" = t- mile GEOPHYSICAL SERIES, Air E-K St Mag. Kap 80^97
Portion of Kap2^3, Geologic Compilation Series
l"- U - miles
LOGS, D.D.Hole 95~3
(a) PROJECT LOCATION
ARKOT Is. NICKEL PROSPECT. Halkirk Twp., Rainy Lake, Ont. Located on Glair. Map G-3808 of Halkirk and Farrington Twps. M.T.S. C-ll, Latitude:^8*^-0'North, Longitude: 93'OV '/test.
(b) LOCATION MAPS:
Claim Kap, Halkirk b Farrington Twps. (scale: l "^ \ Mile) Ont. Geol. Survey Map (Scale: l" *JbQ Kms)
Road Wap Se Geology (Scale: l" = 25 Kms)
(c) ACCESS TO PROJECT SITZ;
There is good access to the Property from Dryden, 151 Kms to the South from Dryden along Hwy. 502 to the junction of Hwy 11, then 5 Kms East along Hwy 11 to Bears Pass, then over
ice by Ski-doo for 5 Kms. to the drill site.
(d) Description of the PropertyThe ARKOT Is. NICKEL PROSPECT Consists of 2 Claim Blocks K-115012? and K-1150128 in Halkirk Twp. Rainy Lake, Ont. These Claim Blocks comprise a total of 30 claim units. These claims are owned by George Armstrong 3 50^* and Chester Kuryliw Q 503. The Claims were staked in June 199^ and are in good standing.
(e) DESCRIPTION OF REGIONAL AND LOCAL GEOLOGY;
REGIONAL GEOLOGY;
The Area is located in the Precambrian Wabigoon sub-province.
This Area Embraces two major East-North-East trending Antiforms.
separated by the Swell Bay steep sided Synclinal trough. In
Cross-Section you have a "K" shaped structure over 6 miles across. The South Antiform is intruded by the Bad Vermillion Lake Gabbro- Anorthosite Complex. The North Antiform (Dome) is intruded by
the Rice 3ay Gabbro Complex. According to ?.R. Harris (G.D."-~.
Geological Report, 19?^) "The Ri c e 3ay yetasediir.ents form a structural Dome, This is the most hi~hly metamorphosed rocks of the Map area." Harris also describes the cor.r-on occurrences of garnets and Staurolite in those rr.etasedimeri's, which i
a high level of thermal metamorphism.
,'i^vul
km
"'
Map 2443 KENORA-FORT FRANCES
Geological Compilation Series
KENORA and RAINY RIVER DISTRICTS
Sonic 1 -.253.440 or l loch lo 4 Miles
6 fl K) 12 M I^S^S*--.'^.L^u-^A
\^, l *
WA
TTE
N
TP
M.2
ss n
jim
ri
'T/W:^-7 * - ..c-V* 'f
' 't "i**M--,' ^f— ——l , 1*" 'j, . -y**r ^ ,'
. - .X---- -,, :t/ ;1 ^:j5K . -.i" .o' 1' :^r ••s~;k?x .',:t-"- ;r^ . .,.*^
^^•o^vfi^u. 2^?^: *** -:* -,X A\ * -' -' * -^ . ^ LyC- \ , "f' *! /^ ' -*" ' *^.. X" ^ /^feafef- E::^^ -^ Vz*^** fV^^ ta i^^^i sxk8-' -: . i
•j -^^^5"?
m&t ^"Y ^ri-^ry?'!'?1'.'? xx "-^T'l"^
w
^y;*.tyj^ • ' ^/r-ff
L
^
^
#11
x
mdpo.int-
x
ARMSTROMC -KURIL CLAIM CROUP
Geology of OM
Rainy Lake Area
District of Rainy River
6' Geological Report 115
•VTMap 2278
P^ RICE BAY
Rainy LakeRAINY RIVER DISTRICT
USA
Scale l: 31.680 or l Inch to Ms .Mile "\.-50 O _________________' Sole l inrt lo W m*i
FM loco o •0000 F*tt
, otopiiiiiiCAi '.to :IICI.IK:JIf MAP j .' - r 'M ATIKOKAN -MINE CENTRE AP.6A l
(WE i T mn PARTI Aliborn* Elociii.nugiioiic Sue.*/ Tuidi iniint l. '•'-•,~
ARMSTRONG-KURYLIW CLAIM OROUP IN KIT -NOMALT
AWSTHONP, ARMOT IS.-SWELL BAY NTCKRL PROSPECTRAINY UK E, ONT, F ECT
METRES
o roo 2000tom- -HUM i*f i 1
South of 3^eeze Hay in the Swell 3ay Synclinal Basin. A c ircular
"agnetic-Kigh Anomalyis outlined or. the O.G.3. Airborne Magnetic and E-:* Survey, 1980. This Xagnetic anomaly was outlined by a detailed ground Magnetic Survey carried over lake ice Feb. 1995 by this writer under Contract to Kr. Armstrong. The Magnetic Anomaly runs E-';/ for a length of nearly l Km. and over a thickness of about 80 K. The Magnetic Anonaly plunges Southwestwards at about 60*. This discrete Magnetic anomaly was interpreted as a magnetic basic to ultrabasic intrusive, within the Swell Bay
metasediments.
Two parallel "formational" Conductors extend for over J Kms from the West where they abut up against the Breeze Bay Magnetic Anomaly
In 1969, Noranda attempted to test the Magnetic Anomaly with drill hole N-88 @ -60*, they encountered 80 feet of water and it was stopped in red mud at a depth of 380 Ft. Drill Hole 1995-3 of this Report, is the first test of both the Conductor
and Magnet!c Anomaly.
INTRODUC'TIC::;
A Ground .Vagnetic Survey was carried out, Jan29-Feb.6 1995.
on Lake ice over the Magnetic-High Anomaly, North of Ar7!ot Is.
A portable S c intrex Kodel r'F-2 pre c ession Magnetometer with a Sensitivity of * l gamma was used in the survey. The combination of deep lake overburden (upto ^00 Ft) and the
high magnetic relief resulted in a relatively uniform, pattern to the ''aanetic anomaly. The pattern of the Magnetic Anomaly indicated a Southwesterly plunge.
A Deep Diamond Drill Hole Number 1995-3 was drilled from a set up located on thr Northeast tip of Araot Is. of 3ainy Lake. The Drill Hole was started Q - 52* with a N-3'-E Bearing targeted to test the Air E-' Conductor and to test the Magnetic-High Anomaly. The Drill Hole was started July 3.1995 and was stopped prematurely July 31,1995 at a depth of 1901 feet. This Drill
Hole essentially flattened very little for the first 1000 feet so that its trend in section did not cross as much ground horizontally as is the normal projection. This resulted in an additional UOO ?t. of Drill hole required to cross the targeted Magneti c Anomaly. Serious Difficulties were also encountered at a depth of 900 Ft. where the Drill hole followed alone; the bedding of Graphite in a Fold Nose, The Graphite walls spall off during drilling and a.use binding of the drill rods which eventually bulged rods at their connections. It is planned to deepen this drill hole when newer stronger drill rods are available.
RESULTS of DIAMOND DRILLING;
The Targets of this Drill Hole were to test the Magnetic-High Anomaly, and along the way to test the Strong Air Survey located 2-M Conductor. As interpreted before the drilling, the E-J'. C onductor was found to be Graphite in Black Sediments- "A Formation
Conductor". The Magnetic-High Anomaly was found to be lenses of magnetite as expected but the magnetite occurs in a thermally metamorphosed metasediment not in a Basic to Ultrabasic intrusive as interpreted. This writer was misled by the"short" lenticular shape of the "agnetic Anomaly set in an extensive trend of the Swell Bay r**etasediments,of uniformly low Magnetic relief, su di an isolated Anomaly was naturally interpreted as a magneti c intrusive, especially in a Geologic environment of numerous large Gabbroic- intrusions. The lenses of magnetite ri di sediment (up to 70?' magnetite) are l-*v feet thick and o c oar over a- intersection of 27^ feet in lengthwith l5:5-20f5 of that length being lenses of magnetite. The "agnetite lenses cannot be classified as the usual cherty banded magnetite Iron Formation, It is magnetite that o cc urs within what were most likely Pelitic sediments originally, but the magnetite lenses, in this writers opinion were con osntrated by a thermal mobilization of magnetite from iron rich sediments and iron sulphides.
There is ample evidence of increasing thermal metamorphism northwards in the drill core, the diagnostic marker minerals of thermal metamorphism have been recorded in the core, these an Biotite - Cordierite - Amphibole *Almandine*:.'agne t ite.
The oore from this Drill Hole is stored at the Kenora c ore library, and forms a very valuable source material for in depth studies of the Swell Bay Sediments and Structural Geology. Thin Section Work and Rock element analyses related to logging in infinite detail,would be valuable to Dept. of Mines and Resources in the area and to Exnlorationists.
STRUCTURAL GEOLOGY;
The core logging of this Drill Hole 1995-3 reveals that the Swell Bay formation are Sediments largely of pelitic composition with some siltstone that exhibits fine c rossbedding structures. An ex csllent "Horizon Marker" was also intersected at 900 Ft. which consists of beds of Black sediments,Sericitic Schists and a distinctive "Limestone bed"-with blebs of apple green Fucshite. This Black Sediment-Graphite horizon has been traced for several Kilometers westwards. There are variable gradually changing bedding angles to the core axis some of which were recorded during logsrinfr, this information together with the duplication of the Bla de Sediment- "Limestone Bed" series in a mirror imaare confirms the presence of a series of folds. (NotetThe angle of Bedding to core axis has two complimentary angle directions possible,) This detail of logged information together with the known regional structural geology leads this writer to postulate that: ...,. "The sediments along Swell Bav of Rainy Lake forr. a Synclinorial Basin. " . . .. between the Rice Bay Dome to the North and the Seine Bay-Bad /ermillion Lake Antiform to the South. Some of this information may prove valuable in assessing the Structural relationships in the discovery and tracing of mineral occurrences on the South side of Swell Bay. A postulated s dierr.atic fold pattern is indicated on the vertical cross-se c tion of D.Drill Hole 95-3 included in this report.
SG C?! Oy 1C GEOLOGY;
The iv'agne tic -High Anomaly was found to consist of a series
of magnetite-rich lenses in a mass of limited strike length in the metasediment s. Some narrow sections of Amphibole-Gamet carry a few percent of pyrrhotite and trace spe des of chalcopyrite Several of those sections were sampled and assayed and returned low but possibly significant? Copper values Geochemically. The Black Sediment-Graphite se ction traced by the Air E-K conductor near the depth of 900 Ft. carried Geochemically low values in Zn. and Cu. in the barren sulphides.
Near the bottom of the Drill hole near 1900 Ft. a Gabbro
intrusive? was entered,its North contact has some chance of being mineralized with Cu-Ni. ? If the caving at 900 Ft allows? this drill hole will be deepened several hundred feet.
CONCLUSIONS;
This Drill Hole 95~3 succeeded in testing the Air E-?/!
C onductor, which was discovered to be Black Sediments with Graphite, as previously interpretedthis is a Foraational Conductor. The lenticular to "circular" magnetic-High anomaly was expected to be a Basic to ultrabasic intrusion within the Swell Bay metasedimer.ts. This Magnetic Anomaly was found to be a series of lenses rich in magnetite, each lense appears to be of limited extent, but the mass effect produces a strong magneti c anomaly. It is this writers
interpretation that the concentrations of magnetite resulted from high thermal metamorphic effects.The Gabbro intrusion at the bottom of the drill hole presents some possibility that the North contact of this Southerly
dipping intrusion may be mineralized with Cu.-Ni.
Mov 30, 1995 C.J. Kuryl
33COMMZNDATIONS:
Deepen Drill Hole 1995-31 an additional 300 Ft. from a depth of 1.901.0 - 2,201.0 Ft.
Estimated Costs;
Drilling Contract, @ $l8.00 per Ft.
Engineering Contract @ $3.25 per Ft.
G.S.T. on $6,375
Allowance for assaying
TOTAL,
$5,^K)0.oo
975-00
1*6.25
178.75
37,000.00
Nov. 30, 1995 C. J. Kuryliw
CERTIFICATE
I, Chester J. Kuryliw of 4-6 Ingall Drive, Dryden, Ontario, do hereby certify that:
(1) I am a Professional Engineer and I am currently employed as a Consulting Geologist for several raining companies.
(2) I air. a graduate of:The University of Manitoba B.Se. Degree, 19^9 The University of Manitoba M.Se. Degree, 1966
(3) I am a registered Engineer of the Association of Professional Engineers of Ontario and also Manitoba. I ara a fellow of the Geologic Association of Canada, also a member of the Canadian Institute of Mining and Metallurgy.
(i) I have practiced my profession for over 4.5 years, most of thoseyears at gold mines, during which time l often planned, supervised and directed underground exploration, development and production.
(5) V-y Report is based upon my supervision of the Drilling program. My logging and Sampling of the core and my plotting of the results on the included sections and plan.
Nov. 30, 1995- Chester J. .c. P.Eng.
GEOLOGYDIAMOND uRILL RECORD
B-Q Core sizeStored at Kenora MN R ARMSTRONG PROPERTYare Warehouse HALKIRK TWP. FORT FRAHCIS. OHT. HOLENO 95-3 SHEETNO l
CLAIM BLOCK 1150128, ARMOT Is. RAINY LAKE ' SHEET NO.
ijvrnuDK .. 0t5Q.S....... DATUM .^6aringi -N-3.'-E - .Mxi^^r^G-.. STAHTKD . jZulyDIP i @ 200'-49', @400'-49', @600'-50',
DKPAKTUIIK ...2+00..^..........™.......___ @ 8QH V-49i-'-*-^——_________ COMI'I.KTEI) lilV.
KI.KVATION ...LAKE. *-0,0 Pt,(bllar -52*, 1000' -49*,
nil- .1.200'. .-46*: , .14.00' .-44'.. ... 1600'-40'. @ 1800' -33*'.
lll.TIMATK DKITH 1901.0 Ft...
IIKI-IM n:r. i
0-66.0-65.0
65.0-66.5
66.5-76.7
?6.?-?8, 5
78.5-316.9
316.9-320.0
320.0-365.7
KOIIMATION FOIIMAIION
CasingSKDIMISNT - This is a finely bedded rock with laminations distinguished hy riark-pr
slightly carbonaceous laminae. This Sediment. IR hrnwnlnh er^o\r n nmnoooHalmost mmplwt.oly nf biotite. This h1nt.it.ir oedimont is tho ond
product of medium grade metamorphism where the original serHnient uingmost likely a shaley arpil 1 ite-f reywnnVe that wag T^ + omorph^s^d
—————————— through tho — (hloritic. phage to tho Biotitl-o— ead produot t---Th" bcddinf forms Rn Rnpls of 40* to tho drill ooro axio (dip-Vepti c al(This sediment will be termed the Rainy Lake Swell Bay Formation)
OAB13RO - A greenish medium grained rock with an altered texture, a sill intrusion,
SEDIMENT - As above.
HABBRO - Sill, as above.
SEDIMENT - Dark brownish-grey, finely bedded as above, bedding @ 40' to c/axis.barren, irregular Quartz, glassy @ 182.8-184.2, @242.2-243.0.
flabbro- Sill, greenish, medium altered texture.
SEDIMENT - Dark brownish, alternating fine bedding with unbedded/^e c tfons /l
.i.rii MY Kenora Soil fc Drilling SICNKI)m?^^ P.EHO.
LATITUDE ....
DKI'AHTUIM-: ..
KLEVATION ....
DIAMOND L .ILL RECORDARMSTRONG PROPERTYHALKIRK TWP. FORT FRANCIS, OUT.
ARMOT Is.
DATUM . .. .... .. . ___ ...,....... . . . . . . .
GEOLOGYHOLE NO. SHEET NO.
STAIITKI) ....
COMI'LKTEI)
1)11' ....... ULTIMATK DKITH
OKi'i H n:t:i
365.7 - 368.
368.4-532.0
532.0-535.5
535.5-5^7.4
5^7.^-553.5
553.5-624.0
624.0-625.4
625.4-630.0
KIKMAIKIN KOIIMATION
( f GABBRO- Greenish, medium grained, altered texture, a sill intrusion.
SEDIMENT- Dark brownish-grey biotitic sediment. f inelv bedded at variable intervals,Stronerlv contorted bedding at 407.0-40Q.O represpnts t.hp ax-^ai tram n-ra fold, where there is a marked change in the interse ction of the vbedding with the core axis. @ 380'.40' to c/axis. @ 3Q4 1 . 60* tn o/axis,^428' r 20* to c/axis. @ 441. 0-460. O f 10*- 9 ^' tn ^/avia,
SEDIMENT- Greenish -brown, some amphibole-chlorite with biotite in the sedimentSome grey quartz stringersand irregular quartz, minor pyrrhotite in quart
SEDIMENT- Dark brownish grey, biotitic, Bedding® 10'-15* to (/axis. (dip 60*-N)
SEDIMENT- Greenish -brown, some amphibole-chlorite with the biotite, grey Qtz. strs.
SEDIMENT- Dark brownish grey, biotitic with fine bedding at variable intervals.t* 576' 20* to c/a, @ 592' 40* toc/a, @ 596' 35* to c/a.
GABBRO- Sill, greenish, med grained altered texture.
SEDIMENT- Dark brownish grey, finely bedded. ? /? j S fl
nun i.i:u MV Kenora Soil tt Drilling SIC.NKII fIJJpSTEK J. KUlfYLIW. M.Sc..
DIAMOND L .ILL RECORDARMSTRONG PROPERTYHALKIRK T'.VP. FORT FRANCIS. O NT.
ARMOT Is.
GEOLOGYHOLE NO. 95-3
SHEET NO.
i.ATHunii . . . .......... . . .. ,. ..
DEI'AHTUIIK ............. ....... .. -.
ELEVATION . ...... . ..... . ,.
. . . DATUM ... . ... ....... .
HKAIilNC
............ 1)11' . ... ....... .... .-.
...................... - STAItTKI)
rOMI'I.KTRIl
.. .. ..... .......... ULTIMATE DF.ITM .
HKCiM ti;r.i
630.0-630.6
630.6-749.0
KIMMATION HWMATION
GABBRO- Sill intrusion, greenish, med. grained texture.
SKDIMKNT-Dark brownish grey, highly biotitic, finely bedded at variable intervals,Bedding @ 645' is 45* to c/a, 0 6?6' 65* to (/a, @ 685' 60* to c/a,0 696' 40* to (/a, @ ?24* 50* to c/a, @ 7M '-742' contorted to 90* to c/t
Notei At 682. 0-685.0, A finely developed cross-bedding dearly identifiablein fine silty sediment. The cross-bedding consists of a fine siltysediment, banded A 35' to the core axis caught between beds of finermud-silt each 5mm to 10mm thick and 4cm to 5 c m apart. The mud-silttrue beds are -a* 65* to the core axis. The resultant cross bedding-was lain at its repose ancle of 30* . This particular sprtlmpnt \ R n ffluvial-deltaic ort ?in. deposited from a relatively p-mitlp rlvor mirr^nt..
*si ,/ /J1)1111 .1.1:11 iiv Kenora Soil A Drilling W. M.Se.. I'.ENO.
rip.oMMiirr
DIAMOND L .ILL RECORDARMSTRONG PROPERTY GEOLOGYHALKIRK HOLE NO. 95 ~ 3
SHEET NO.
LATH UDIC
ELEVATION
DATUM --.-..
BEAMING —,...
1)11' .......
STAKTEIJ ...
COMPLETED
tll/riMATK DKITII .
nmn n:i:i
f...
749.0-750.7
750.7-824.0
824.0-831.0
831.0-844.2
844.2-846.5846 *i-84Q 7** ' *~ w ^s ' r' " 1
849.7-854.4854.4-856.4856.4-856.9
KIHMMION FOIIMATION
I
GABBRO- Sill intrusion, greenisn, mea grainea texture.
SEDIMENT -Brownish grey, biotiti c , bedding ft? 50' to ya.
GABBRO -
SEDIMEN't1
Sill intrusion, greenish, med. gr. texture.
-Dark brownish grey biotiti c sediment tKAlNY LAKi'J SWISLL BAI ^EDlMh-iNi- FuttMAT
RAINY LAKE. SWELL BAY. BLACK SEDIMENT FACIES GROUP (844.2-931.0)SEDIMENT -
-BLACK-SED
SEDIMENT -
Sericite s (hist, 5?o quartz stringers, 7# pyrite along bedding @ 35" "to c/a
TMKN'i1 - JMghly mrbonaceous. partly piraphiti c . contorted bedding,y^ Q+7, - /prh s-hrs along bedding. V/o pvrite.Sericite schist, 10?S Qtz-carb along bedding, 7# pyrite.
DYKE- Altered, da c itic composition, fine grained,SEDIMENT - Sericite schist, 10 "/* Q tz-carb, 7^ pyrite. ^ rf j^/ j/
ON)
IMIII.I.U) iiv. Kenora Soil b Drilling cllJfe" J - KU .IW. M. Se.. I'.ENO. nr.ciixKiirr
DIAMOND D. .LL RECORDARMSTRONG PROPERTYHALKIRK TWP. FORT FRANCIS. OUT.
ARMOT Is.
GEOLOGYHOLE NO.
95-3SHEET NO.
KI.EVATION ..
DATUM -....
HKAIUN(5 M.
1)11' .-.-...
STAItTKI) ________..
COMI'I.BTEI) _______.
lll/l'IMATK DKITII .
HKi'in m:i856.9-857.5857.5-860.3
B60.3-862.4862.4-887.0
887.0-902.0
002.0-014. S014. t;-o?i .n0?1 .0-02^.0
o?9,n-rnt -nmi .n-o/n.n
9^3.0-9^8.0
KHIMATION FUIIMATION
SILTSTONE- Sericitic in part, light grey, fine grained.LIMKHTONH- A chemical percipitate? , carbonate with blebs of apple frreen Fucnhit.P,
y/o d isseminated pyrite. (Notei A very similar carbpnatp with nnitti/- pu istructures was mapped underground at the Cbehpnnur Mine \ n the Rod Lakearea, interbedded with a similar Black sediment facies. Rxnppt. that ntthe Mine the Sediment Facies was interbedded with PninwpH vni^^i /,flows, in this drill hole thp Farips 1 Q Into^hoHHo/i with SodimnntarvFormations.)
SEDIMENT- Sericite schist facies, 10# dissem pyrite.BLACK SEDIMENT- Finely bedded, strongly contorted, highly oarbona oaous, partly
graphitic, 5#-10# qtz-carb along bedding, 5^-10'^ pyrite.(iRAPHiri-;- Stressed .Fault-sheared Bla * Sediment, resulted in a flaky-blocky
graphitic schist. This is a very strong E -M CONDUCTOR.
.3TLTSTONK- Sericitic in part, litfht ^rev, fine prainedI.TMR^TONR- An AhnvP f with Funshite.
n^APIHIM-:- r.raphltp schist. a fa\ilt-shear stressed Blade Sp.d, 1 *yA Pyrit.R.n 0 Hrtinr fi lil' t n mrp ayl* A qtrnn/r F-IV rONnilCTO,?
RT.AHir S5RDTMKNT- 1 ^ rtlnspm Py . RprMlnp ga U ^ ' t.n n/a
SKHTMRMT - T^pnwnicih t.n frrppn-prpy in sprt.ions ^Swpl 1 Bay Fnrmat.inn) Rpdri'^r ii ^n ' tn r/;BLACK SKDIMISNT- intermixed black sed. and brown biotitic Sed. Hsds ^ ^* to ^ /n
^ S s/ /)
ihite
Dim .i.i:u nv Kenora Soil Se Drilling SKIN KMM.Se.. P.ENO.
DIAMOND L.JLL RECORDARMSTRONG PROPERTYHALKIRK T WP. FORT FRANCIS. OUT.
GEOLOGY
LATITUDE .
DEPAHTUKE
ELEVA'I ION
ARMOT I s.
DATUM . .......___...
HEAHINIS ————————.
DIP .........
HOLENO.95-3 SHEET NO.
STAMTED ...._______....
COMPLETED ______ ..._l._....
ULTIMATE DEITII .
m:rin 11:1:19^8.0-993.0
993.0-99^.0
99^.0-1129.0
1129.0-1131.
1131.3-1143.1
1143.1-1143.
1143.8-1^6.1
HHIMATKIN HWMATION
SEDIMENT- Dark brown-grey biotiti c sed. Finely bedded with a few widely spacedthin beds of black carbonaceous sed. Bedding @ 947' is 50* to c/a® 957- ky to c/a, @ 977' 35* to c/a, @1005' 32* to c/a.
GABBRO- Dark greenish, roed grained altered texture.
SEDIMENT- Dark brown-grey biotitic sed. finely bedded at variable intervals.Bedding @ 1005' is 32* to core/axis, @ 10lV ^0* to (/a. @ 10UT 30*to c@1077* 25* to (/a, @ 1114' 20* to c/a.
GABBRO- Altered greenish sill intrusion
SEDIMENT- Brownish grey, biotitic, finely bedded at variable intervals. Bedding@ 113^' 10* to c/a, @ 1178' 40* to (/a. @ n44* 2*5* to t/a.
Gabbro- Altered greenish sill intrusion
SEDIMENT- pineiy bedded, brownish grey biotitic, slightly more greyish than thesediments in the first 800 feet of this hole whi di may indicate thatthis portion has an originally higher silt to clay ratio than previously,Bedding is contorted @1203", @ 1210' 40* to c/a,^ 'ft , S //'
a
.1.1:11 MY Konora Soil A Drilling SIC.NKI)CITE . M .SC-.. P.
DIAMOND L JLL RECORDARMSTRONG PROPERTYHALKIRK T WP. FORT FRANCIS. OUT.
AKMOl1 Is.
GEOLOGYMOLE NO.
J~ JSHEET NO.
I.ATITUDIC ..
DEi'Aicruiti:
KI.KVATION .
DATUM ..........
HKAMINO __..
1)11' ........ .
STAHTICU . ._..........
C'OMPLETEI) _______.
UI/riMATK DKITII
HKi'in rr.t.i
12T6. 0-1219. 6
1239.6-1403.0
1 403.0-1406. f
KIMIMMION rOHMATION
Lamprophyre Dyke- Highly biotitic, follows bedding
SEDIMENT- Greyish brown, finely bedded in parts, originally a greater nilt to clayratio as compared to the first 800 feet of this drill hole. Bedding©1244* 40* to c/a, @1251' 35* to (/a, @1257' 40* to c/a.@!28l' 50* to c/a, ©1290' 50.* to c/a, @l299' 60* to c/a,@ 1306' 65* to c/a, @1309' 60* to c/a, ©1313' 55* to c/a,@1333' 50* to c/a, (o) 1339' 30* to c/a, @ 1345' 35' to c/a,a*l350' 40* to c/a, ©1355' 45* to c/a, Q 1 372' 50* to c/a,# 13R5 1 45* to c/a, © l4ll' 50* to c/a, 0
HOTKi Without benefit of thin section identification! this sediment studiedwith the aid of a hand lens, is tentatively identified as a cordieritehornfels sediment, whiteish-grey knots of cordierite? comprise upto l O'/o o f the rock, The knots average2-3 mm thi de and .4-6 mm long,elongated along the bedding. The presence of c ordierite indi cntesthe sediment was subjected to thermal metamorphism, of intermediateintensity. Heavier cordierite was logged at 1378 Ft. and 1397 Ft.
GA13BKO SILL-DYKh' Greenish, highly altered, med grained granular texture.
s/f s S ftniiii.i.KD in
LATITUDE .
i)i:i'Ait ruiti:
ELEVATION .
DIAMOND DKILL RECORDARMSTRONG PROPERTYHALKIRK TWP. FORT FRANCIS. OUT.
ARMOT Is.
DATUM .......___..,....................
HEAHING ______________..____.
DM' ....., .. ....
GEOLOGYHOLE NO. 95-3 SHEET NO. 8
STAHTEI) -.
COMPLETED ______________.
ULTIMATE DKITH .
m.rin ti:i i
1406.8-1476.0
1476.0-1601.0
l60l .0-1603.6
1603.6-1608. 5
1608. 5-161 1.5
1611.5-1622.5
HHIMATION FOMMATION
SEDIMENTS- Swell Bay Formation, Brownish, Finely laminated, brownish biotiticalteration. The laminated bedding is partly crenulated due to foldingand/or shear stresses, cordierite knots @ 1454 Ft. Beddingi?l4ll'50' to n/a, ^l4l7'45*to (/a, @l430'45'to c/a, ^1443' 55' to c/a,(Ln451' 50 'to c/a,
SEDIMENTSr Swell Bay Formation, urownish-urey , Diotitic, lineiy laminated, narrowSections of this sediment have been altered fcy thermal metamorphismto an amphibole- pale pink garnet sediment, The amphibole rich sectionscarry minor pyrrhotite and traces of chalcopyrite, (Some Magnesiummetasomatifim may also have occurred) 1486.5-1487.2 a gabbro Sill-Dyke.Bedding Anglest *Pl454 f 60*to c/a, @lW 70*to c/a, @l485 ( 63'to c/a,y"l506 70 'to c/a, @1538' 70* to c/a, @1564 ( 73 'to (/a, 91591' 80 'tor/a,^1630- 70 'to c/a, ei 645* 70* to c/a, @i665' 65* to t/a,
Lamprophyre dyke- Brownish, minette type.
SEDIMENT- Swell Bay Formation, brownish, finely banded. as above
SEDIMENT- MAGNETITE HI C H SECTIONS in usual biotitic brownish bedded sediment.
firey Feldspar Porphyry Dykei Intruded along bedding @ 75*^0^, L6# Feld. Phenon
Kenora Soil ft Drilling mm i.en IIY -.________________li. SIC.MKM.. P.E.O.
Dl-l'AltTUIIi:
KI.EVATION .
DIAMOND D.xiLL RECORDARMSTRONG PROPERTYHALKIRK T '.YP. FORT FRANCIS, OUT.
ARMOT Is.
DATUM .. ........___.....,...................
HKAKINU ______________—____.
DM 1 ........ .. ..... ...........
GEOLOGYHOLE NO. 95-3 SHEET NO. 9
KTAHTKI) ...
COMI'LKTEI) _______.
ULTIMATE DEITII .
w.riii H;KI
1622. 5-1651. c
1651.0-1653.'
1653.7-1675.
KHIM.MION rOIIMATION
SEDIMENT .MAGNEI'ITE-KI 01 SECTIONS, interbedded with brownish, biotitic, Swell BaySedimentary Formation, Bedding Angles @ 1663 '65 "to c/a,
Groy Feldspar Porphyry Dykei 15?i Feld. Phonos, up to ^ mm. uiam.
i SUDIYRNT i Swell Bay Formation, brownish, Deeming ® 6 5 degrees to core axis.a few narrow greenish amphiDoiitic sections, rrom i66U.u-i6ny.ua magnetite-rich section (70'# magnetite;.
l675.5-l680.5 Feldspar Porphyry Dykei Intruded along bedding, Some slight shear deformation
1680.5-1750.
1750.0-1.^51 .
along the bedding affected the porphyry resulting in an elo .gationof phenocrysts parallel to the bedding of wallrock Sediments.
) SEDIMIiMTi Swell Bay Formation, Greyish, fine siltstone intorlayered with 1-3 footsections richly mineralized with magnetite, a few greenish amphiboliticnarrow sections that arry minor pyrrhotite , traces of chalcopyrite andfine pale pink garnets.
5 Gabbro sill-Dyket Dark greenish, partly sheared, partly talcose.
S?/?// J
mm .1.1:11 iiv .Kenora Soil A Drilling fell J. KUKYI.IW, M.Sc..CONBUKTINCl OroMXllST
DIAMOND DhlLL RECORDARMSTRONG PROPERTYHALKIRK TWP. FORT FRANCIS. OUT.
AHMOT. Is.
GEOLOGYHOLE NO. 95-3 SHEET NO. 1 0
LATITUDE ..
DEI'AMTUME ...——
ELEVATION ........
DATUM ...... ....
BEAMING --.^
DM 1
STAMTIJI) ..
COMPLETED
ULTIMATE DKITII
OKI'1 II IKKI
1751.5-1882.0
1882.0-1892.0
1892.0-1901 .0
jA^/^A^^ A ;V /^,
^ 7 x: ^
KHIMAIION FOIIMAIION
SEDIMENT i Swell Bay Formation, A few magnetite-rich sections of 1-2 footA few narrow amphibole-rich sections that carry minor pyrrhoti
width.t e
with tra c es of chalcopyrite and some fine pale pink Garnets.Bedding Anglesi ^175^' 45'to C/a, 01769' 30* to c/a, ^1775' 35 'to c/a,13*1788' 40*to (/a, S*l807* contorted along the core.
SEDIMENT? Strongly amphibolized, dack greenish, somewhat massive, fine grainedbasaltic composition, @ 1 992.0 Ft. an amphibole-quartz rich contact@ 80* to the core axis ''contains a few pale pink Garnets up to 3 mm Diam.
GABBRO INTRUSIVEi Dark greenish, fine to medium grained, 1 mm Diam. grain texture.This Gabbro differs from(the several narrow highly altered gabbroSill-Dykes intruded into the Swell Bay Sediments) by its relativelyfresh looking equigranular texture. This Gabbro does have some biotiticalteration. 1901.0 Ft. End of Mole a q f)0 ,NOT Ei Persistent caving of Graphitic drill hole wallrock/oiusedof the drill rods,' drill joint bulging and jamming of the wirelcore barrel, an additional 200' to 300' will be drilled as soon
bindingineas new
yrtA/As/ s tronger rods are available.^- NOT Ei The targeted Air IS -M C onductor was found to be graphiteq/ i n sections from 846.5-948.0 Ft.
found.
t? NOT l 1.' i Tho targeted Strong Magnetic Anomaly was intersected ^1608.5-1882.0 Ft.
LATITUDE .
DEI'AHTUKE
ELEVATION .
DIAMOND jRILL RECORDARMSTRONG PROPERTY
HALKIRK T'.VK FORT FRANCIS, OUT.
ARMOT Is
DATUM ™......_____.....__...,.....__.
BEAMING __..______—..-..———..
DU' ......-—..-..-.-..-......-.___.
HOLE NO. 95-3 SHEET NO. t -3/i.Vl 1
STARTED .-...........__...
COMPLETED __..... ....^-............
ULTIMATE DEI'TU ..........
44-3 . Q-'i-'^t' . o
U^5 . '•f-UUo . 0
456. 5-460.0
^P.T-'^.ft
647. 5-650.5
650.5-653.5
RUU.3-RU9.7
fi^q.9-8^.^
054.4-857.5
857.5-860.3
860.3-863.0
KOKMATIIIN
(1.0 Ft.) 40"i Qtz. wallrock heavily biotiticJ'/o Pyrrhotite blebs.
(3.6 Ft.) Q0-;i f.lassv Quartz, chloritic wallrockI'/o P o. trace pyrite.
(3.5 Ft.) 30?S Glassy Utz. along beddin/r in part.Minor pyrrhotite.
(^.^ F t..} 1 f}':'a L)t.7. St.rs In a hin-H+.ln RpH.
1 '\'a Py , t "^ lj n , Rpprlf n-f sphal prl t.p .(3.0 Ft.) 20# Qtz, along core, Biotitic sed.
V/o P o. Trace Py.(3.0 Ft.) 25*;S Qtz. Strs in a biotitic Sed. along
bedding, minor po,py.(5.4 Ft.) Sericite schist, Black Sed, ty Q tz.
v?5 Pyrite.(4.7 Ft.) Sericite schist sed. 10?S Qtz. Strs.
along bedding, ?'# Pyrite.(3.1 Ft.) Siltstone, some sericite schist
•j'A Pyrite.(2.8 Ft.) Carbonate sediment with Fucshite
5'/^ Pv. minor Po.(2.7 Ft.) vJtz-Sericite-Schist Sed. 7# Pv.
Au PPD
3
3
Nil
Nil
Nil
Nil
Nil
Nil
Nil
Nil
Nil
Ag P FM
0.2
^
PPM
on
95
/7s,
Ni PIM
^ /S
Zn PIM
-04 ——
32
.
Sunple Hunter
25066
25067
2506ft
25069
25070
25071
250''2
25073
25074
250^5
?^6
Dllll.l.l'.l) IIV SUiNKItR J jJOmYMW. M.Si:., P.KNC.Cimaill.TINU UEOIXM1I8T
LATITUDE
DIAMOND JRILL RECORDARMSTRONG PROPERTY
HALKIRK T',VP. FORT FRANCIS. OUT.
ARMOT Is. RAINY LAKE DATUM —..-..______.___.__-.__....
SAMPLINGHOLE NO. 95-3 SHEET NO. 2-SAMP.
DEI'AHTUKE ..
ELEVATION .
HKAHING
1)11* .--.
STAHTED
COMPLETED
ULTIMATE DEITM .......
IIKI'I'II KHIM
863.0-867.5
876.0-87^. 5890.0-894.0
914.^-921 .0921 .0-927.0927.0-931.01483.9-1486.31497.2-1499.8
1 529.7-1532.0
1718.0-1720.4
1723.2-1724.7
1805.8-1807.5
KOIIMATInN
(4.5 Ft.) Black Sed. tO^J Qtz-Carb. 10# Pyrite.(1.5 Ft.) Hla c k Sed. 15# dissem. Py.(4.0 Pt.) Graphitic, 10# (Jtz. 5"/' Py.(6.5 Ft.) Ckrbonate Sed. Pucshite, 5"^ Py, 2# Po.(6.0 Ft.) Graphitic, 5/0 Po.(4.0 Ft.) Sericite schist, 7# Py. Specks Sphal.(2.4 Ft.) Amphibolitic, 596 Po, Rarnets, yf* Q -Carb(2.6 Ft.) Amphibolitic, garnets, minor Qtz-Carb,
5'tf Po, Speck Chai co.(2.3 Ft.) Two narrow amphibolitic sec 'n, garnets
5?" Po. in bands, traces Chalco.(2.4 Ft.) Amphibolized Sed. garnets, 2 ",'o streaks
Py A Po. spe cXs Chalco.(1.5 Ft.) Strongly amphibolized Sed. with
(1.7 Ft.) Highly contorted amphibolized Sed.lO'1'. Py. Po. spe des Chalco.
Au PPBNilNilNilNilNilMil
AUPFM
0.10.20.20.20.31.2
^
Cu PRvl
92120158176
83101
140
40
64
67 T
r rf S
Ni PIM
7566
60
45
46
106
/
Zn PFM
31270
200361
/A .
Swrple Hunter
?S07725078
25079
250RO250812508225083250fi'(
25085
25086
25087
2S088
1)1(11.1.KI) IIV SI(iNKI)iXv7M.Sc.,
oroixxjisrr
Established 1928
Swastika LaboratoriesA Division of TSL/Aonayrr* Inc.
Assaying - Consulting - Representation
geochemical Analysis CertificateG. ARMSTRONG
5W-3255-RG1
; AUG-18-95Project: Armot Is. Aim: G. Armscrong/C. Kuryliw
We hereby certify the following submitted AUG- 10-95 by .
Sample Nun* e r2506625067250682506925070250712507225073250742507525076250772507825079250802508125082250832508425085250862508725088
Geochemical Analysis
Au PPB
33
NilNilNilNilNilNilNilNilNilNilNilNilNilNilNil
.--..
Au Check PPB
.--.-.
Nil----
Nil.--...--..
of 23 Core
Ag PIM
-.---,
0.20.2
.-.
0.10.20.20.20.31.2
.
.-.-
samples
Cu PIM
.- :-
98-.
9573
---.-
9212015817683
1011424064
673
Ni PIM
.----.-----.---.-
7566604546
106
ZnPFM
---
91--
3263
---.-
31270200361
.
.-.-
Certified by-
P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244 FAX (705)642-3300
SOUTH RANGE
NORTH RANGE f
lSOUTH RANGE
i l'P !d~K — TTT f"i.
1^939154 9Z7S65 J927S
——— J IT —— IK ——— +K""9J9I98 9Z7S67 1927966 l927S('
l {Breeze/Bay II5005I
594 P
05951s in50127 -EJJ__
LINE GRID & DRILLI^g AREA
(7
INE GRIDDRILLING.50 26 ARMSTRONG Q0#rtl ^ KUrtYLItf io2 ^OWNERSHIP
HALKIRKFARRINGTONCLAIM MAP
GEORGE ARMSTRONG HOLDING
'zsiQfl NTS C-llMinistry ol Natural Resources
SCALE:O 900 1000 1000
ARMSTRONG KURYLIW 5 OWNERSHIP
Ministry ofNorthern Developmentand Mines
Ontario
Report of Work Conducted After Recording Claim
Mining Act
Transaction Number
fi* j
^pnoneJ information collected on this form is obtained under the authority of the Mr Ms collection should be directed to the Provincial Manager, Mining Lands, Mini Sudbury, Ontario. P3E 6A5, telephone (705) 670-7264.
nstnictions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for req
Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.
52CHNE001Q W9510-00150 HALKIRK 900
Recorded Holders) (l) (JrtiST:i.t J. ."..U.tYLIii ^0/uuJ George Armstrong 50?*
Address (l) 46 INGALL iJr. DxYDEi. , Oi.J1 . P8l. 3B"7(2) ^07 /ictoria Ave. Fort Francis, Ont.
lining DivisionKENOrtA
DatesSted From: July 3, 1995
Township/AreaHALKIRK
Client No. I 3*^0 J 3A r\ O f-LQ-Q. Jtf?4^4^T*^^^^^^^' i "s f 9
Telephone No. BO 7 223 6080807 2^4 5957
M or G Plan No.G-3808
To: I.ov 30, 1995
Work Performed (Check One Work Group Only)Work Group
Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other Authorized Work
Assays
Assignment from Reserve
Type
UlAl^uNB D^ILLII.Lr CGnl'.iA (T Drill Hole Engineering Contract, Core Assaying.
fotal Assessment Work Claimed on the Attached Statement of Costs
tote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
^•rsons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address
Kenora Soil ft Drilling; Box 109. Kenora, Ont. P9*: 3X1
C. J. KURYLIW, Cons. Geologi :t 46 Ingall Dr. Dryden, Ont. F8N 3B"7
Swastika Labs, Assaying Box 10, Swastika, Ont. POK 1TO
(attach a schedule if necessary)
^truncation of Beneficial Interest * See Note No. 1 on reverse sidel certify that at the time the worK was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest toy the current recorded holder.
Date
Dec 7, 1995Recorded
Oerttflcation of Work Reportl certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after
t|to completion and annexed report is true.and Address of Person Certifying
CHESTER J. KU3YLIW 46 Ingall Dr. Dryden, Ont. P8N JQyteonna NoData HartifioH Rw lKjnnatifi\ ^ 7^
SO'7 223 6080Date
Dec. 7, 1995
^or Office Use OnlyTotal Value Cr. Recorded
**
ftf^l1^"
Date Recorded
/)2* . /l^ t iffDeHmed Approval Aate
Minino/ftacprder /-^ .-^^
Date Approved
AfAit- li.Date* Notice for Amendments Sent ' X
J4& ——
R^eeived Stamp
4*1(03*1)
fo
-x]
O
CD
s'3
rf
S3
H
S
ito S-
li li* m
^ ^
1j
1
V '
cis/l
•fc
^ r^
~^
V*4^
^^
.
i
•- -
l-* -K-vji
r* Xro- -o. oO U30 0. o
*-
——— v vr —
M
1
.
M
h.
t ,\1
O
;
D
i-' •is~.-V\
ro ^-o ^i-* iX*: J1 COO r-** O
- —— *
SJ1sfi.fi551!'B 3 * X 1
3-2 ji
Btf3I&S
i
l
gfiai
^
1H
i
f
V
r™
~.
k
M"bo
"V
'^
cV.
N
-
V*feVn ^"^
*l^
'ij
^- O3
ro tt "b r-1O i-*
- oroCO
^w. vx"\
*"^ ?^*
r\jo ""O CO 0 0- o
o
-6-.
UX
00
:
Illfi3 i
1
*
0*
? Q ?3Bs.e.0?*!?| sty*9
Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from i which claims you wish to priorize the deletion of credits. Please mark (^) one of the following: i1. H Credits are to be cut back starting with the claim listed last, working backwards.2. ~ Credits are to be cut back equally over all claims contained in this report of work. ;3. L- Credits are to be cut back as priorized on the attached appendix. J
, ji In the event that you have not specified your choice of priority, option one will be implemented. -'
Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.
Note 2: If work has been performed on patented or leased land, please complete the following:.^.m ....._,-——^T-
I certify thai the recorded holder had a beneficial interest in the patented j or leased land at the time the work was performed.
Ontario
M'nistry ofNorthern Developmentand Mines
Mmistere du Developpement du Nord et des mines
Statement of Costs for Assessment Credit
Etat des couts aux fins du credit devaluation
Mining Act/Loi sur les mines
Transaction No./N 0 de transaction
l
Personal information collected on this form is obtained under the authority of the Mining Act This information will be used to maintain a record and ongoing status of the mining claim(s) Questions about this collection should be directed to the Provincial Manager, Minings Lands. Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street. Sudbury. Ontario P3E 6A5. telephone (705) 670-7264.
Les renseignements personnels contenus dans la presente formula son! recueillis en vertu de la Loi sur les mines et serviront a tenir a jour un registre des concessions minieres Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, ministere du Developpement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/Couts directs
Type DescriptionAmount ; Totals Montan) j Total global
Wages 1 Labour
('entrepreneur •t da I'expert- consell
Salaires
Contractor's and Consultant'sFeesDroits de
Mam-a oeuvreField Supervision Supervision sur le terrain
Type -,- . , r| --~ p.-., 7j—J -L/* . Vx a ^ LJ L-J - \. —
f A \ * "\ * T T * ^
f r} \ ~~t * *
LLI:;Gntra ^tr. C ont
.^35.993
Supplies UsedFoumrture*utilise**
Type
Till
Equipment RentalLocation de materiel
Type
Total Direct Costs Total des couts directs ^2,918
Included in Contr 2. Indirect Costs/Couts indirects ( '''s+imated)* * Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work.Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admissibles en (ant que travaux d'evaluation
Type
Transportation Transport
Food and Lodging Nourriture et hebergementMobilization and Demobilization Mobilisation et demobilisation
Description
Type Hoat
; ."on Tru c k
r'ood
Amount Montan!
V.500.
Sub Total of Indirect Coste Total Darttel des couts indirects
Amount Allowable (not greater than 20H of Direct Costs) Montan! admissible (n'excedant pas 20 H des couts directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and Allowable d'evaluation Indirect costs) (Total de* coot* direct*
•t IndlncU idmluiilM
Totals Total global
i i
32.000 01.300
Si , ooo
5?, 300.
?7, 300.
^2,918
Note: The recorded holder will be required to verify expenditures claimed m this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted
Note : Le titulaire enregistrg sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 jours suivant une demande a cet effet Si la verification n'est pas effectuee. le ministre peut rejeter tout ou une partie des travaux d'evaluation presentes.
Filing Discounts Remises pour depdt
1. Work filed within two years of completion is claimed at 1 000fa of the above Total Value of Assessment Credit.
Les travaux deposes dans les deux ans suivant leur achevement sont rembourses a 100 0A de la valeur totate susmentionnee du credit d'evaluation
2. Work filed three, four or five years after completion is claimed at 50*Vb of the above Total Value of Assessment Credit See calculations below:
Total Value of Assessment Credit Total Assessment Claimed
x 0.50
Les travaux deposes trois. quatre ou cinq ans apres leur achevement sont rembourses a 50 "/b de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.
| Valeur totale du credit d'evaluation Evaluation totale demandeel x 0,50 ~
Certification Verifying Statement of Costs Attestation de I'etat des couts
1 hereby certify::hat the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown eh the accompanying Report of Work form.
rtat as .-•"older cc Afcent(Reco'aed Hotde'. Agent. Position m Company)
o make this certification
J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont etc engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.
l am authorized Et qu'd titre de je suis autorise(titulaire enregistre. represemant. poste occupe dans la compagme)
faire cette attestation.
Date
Do c ",Nota : Dans cette formulex *orsqu'il designe des/ersonnes. le masculin est utilise au sens neutre.
r*'
d
o o
_________NOTES^^^^^^
4OO' surface rights reservation along the shores of all lakes and rivers.
All Islands in Rainy Lake WITHDRAWN FROM STAKING under Sec39 subXc) of Mining Act R5.0. I960.
AREAS WITHDRAWN FROM DISPOSITIONMRO- M ining Rights Only
SRO - Surface Rights OnlyM * S "Mining and Surface R ights
Description Oxter No. Date Dnpositan
42WSOI960) 9/O6/69 &RO. -
5) PUBUC RESERVE 1967 S R.O
43(RSO IflTOt W53/73 6/12/73 SRBWR
RE-OPEMED WWR.IVS4 7/T2/M
43(R9OSm 1*44/73 18/08/79 SRO
WSTE DSPOSAi. W 89/85 28/01/65 SRO
Hte163472
163472
176403
7451 VS
36*80 1988——W 188/81
36IRSO I960) W 27/88 14/O4/86
WD-KE-4O/S1 NWR JULY I/Si SRO
M-tS 188995
OBIKOBA LAKE M.2126 PORTER INLET M.2459
2051
120489 )116146
\I2D48
Grc a? Pot tagej^
;:44276Z (442763^
7TT33S (7T73S4
"/ ~~"
73/399 ( 7314001731001
9l54i 927565 (92736- 731390
SOUTH RANGE1
1150056 Jb
IT50I27a n y
50128
50126 L-JS1178217 BLISS
CD ^~
OJ
Uy
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES. AND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES. FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON
EFFECTIVE DATE
LEGEND
HIGHWAY AND ROUTE No
OTHER ROADS
TRAILS
SURVEYED LINESTOWNSHIPS. BASE LINES, ETC LOTS, MINING CLAIMS. PARCELS, ETC
UNSURVEYED LINESLOT LINESPARCEL BOUNDARYMINING CLAIMS ETC
RAILWAY AND RIGHT OF WAY
UTILITY LINES
NON-PERENNIAL STREAM
FLOODING OR FLOODING RIGHTS
SUBDIVISION
ORIGINAL SHORELINE
MARSH OR MUSKEG
MINES
DISPOSITION OF CROWN LANDS
TYPE OF DOCUMENT
rMTBTT 30HFACE S MINING RIGHTS
SURFACE RIGHTS ONLY
MINING RIGHTS ONLY
LEASE. SURFACE A MINING RIGHTS
SURFACE RIGHTS ONLY
MINING RIGHTS ONLY
LICENCE OF OCCUPATION
CROWN LAND SALE
ORDER-IN-COUNCIL
RESERVATION
CANCELLED
SAND A GRAVEL
SYMBOL
T cs ocO
SCALE : 1 INCHO 3OO lOOO ZOOO
METRESO ZOO 4OO WO MO KM
ACRES HECTARES
TOWNSHIPS
HALKIRK FARRINGTONDISTRICT
RAINY RIVER
MINING DIVISIONKENORA
Ontario
Ministry of Natural ResourcesSurveys and Mapping Branch
Date APRIL 1970
Whitney Block Queer's Perk, Toronto
Ran No.
G-3808
52C11NE001O WM10-OO150 HALKIRK 200
K&E 1-73
nn
G-3839 WATTEN TWP
9609120229
Puiuc NesERve4?(M8CI**0)
RHCftVC
RMIRVE
4NK80IWO)
SCC 96/iO W 54/8Z
1193832IIHV|.Mtt (7,IH7
50062
81183834 183834
NO ROAD ALLOWANCE
DOMESDAY
Volume H-N, Page 85ON THIS MAP
CN COMPILED SOURCES,
ACY IS NOT EED. THOSE
HAS FROM AND QUAR
TO STAKE MIN- SHOULD CON- THE MINING MINISTRY OF
ERN DEVELOP-
K-207
GooseK-216
Green L ^- * NORT MENTomON LAN
INFORMATION STATUS OF THE LEGENDHIGHWAY AND ROUTE No. OTHtR ROADS TRAILSSURVEYED LINES:
TOWNSHIPS. BASE LINES. ETC50128LOTS. MINING CLAIMS. PARCELS. ETC
UNSURVIYEO LINES:LOT LINES
. PARCEL BOUNDARYMINING CLAIMS ETC.
RAILWAY AND RIGHT OF WAY UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RSMRVATIONt 0*tGrNAL4HORCLIN6 ..........,^...MARSH OR MUSKEG C C^^^g* MINES ft TRAVERSE MONUMENT -6V
0-1429 w 0-HW
KduekU I.
7Sei6
DISPOSITION OF CROWN LANDS
TWE Of DOCUMENTPATENT. SURFAdl li MINING RIGHTS
, SURFACE RIGHTS ONLY............... ....... 6," , MINING RIGHTS ONLY ....—.................. Q
LEASf. SUMFACi ft MINING RIGHTS" , SURFACE RIGHT8 ONLY.....,.——.—...—^. H " . MINING RIGHTS ONLY..............—........... B
LICENCE OF OCCUPATION .~—.........—~....~..-. TOROER-IN-COUNCIL .........-.....-.........^....-..... OCRESERVATIONCANCELLEDSAND li GRAVEL
Dinsmore
PROVINCIAL
DEPARTMENT OF LANDS AMD FORJ8TS
FEB - 9 1996KfNORATOWNSHIP
CANADA AND A
STATES
REFERENCESTOPOGRAPHY
LAKES, RIVERS, ETC. FROM FOREST RESOURCES INVENTORY SHEETS No.486-931AND 487- 9)1.
lSURVEYS
NORTH BOUNDARY OF WATTEN TOWNSHIP,PART'OF BASE LINE BY NIVEN, OLS. ista,FIELD NOTE BOOK No. 2436.
ORIGINAL SURVEY OF WATTEN TOWNSHIP BY H. B. PROUDFOOT OLS, 1894, FIELD NOTE BOOK No. 1858.
RESURVEY OF EAST BOUNDARY OF WATTEN TOWNSHIP. BY R.S. KIRKUP OLS. 1948. FIELD NOTE BOOK No. 2707. PLAN No. M-S-18, **
RETRACE WENT OF LINE BETWEEN CONCESSIONS A" ond ISR., LOTS l to 12 , BY H.A SMITH OLS, 1962, FIELD NOTE BOOK No. 2927, PLAN No. W-25-32,
RETRACEMENT OF LINE BETWEEN CONCESSIONS4 ond S, BY H.A. SMITH, OLS. 1964,
FIELD NOTE BOOK No. 2996, PLAN No. L-ll-93,
RETRACEMENT OF NORTH LIMIT OF WATTEN TWR BY H.A SMITH OLS, '961 FIELD NOTE BOOK No. 2935, PLAN No. W-24-43,
RETRACEMENT OF LINE BETWEEN CONCESSIONS5 and 6, BY GEORGE WEGMAN OLS, 1962, FIELD NOTE BOOK No. 2937, f LAN No. L-30-6,
RETRACEMENT OF LINE BETWEEN LOTS 6omJ7, 7 ond 8, 8 and 9, CONCESSION M and LINE BETWEEN CONCESSION H NR. and CONCESSION l, ACROSS LOTS 7 and 8, BY,
OtS, I960, PLAN No. W-16-25, FIELD NOTE BOOK No. 2910,
ISLANDS NUMBERED l to 77 INCLUSIVE BY H.B. PROUDFOOT OLS. 1894, Un original Two plan) FIELD NOTE BOOK No- 1858.
INTERNATIONAL BOUNDARY IN ACCORDANCE WITH THE PROVISIONS OF ARTICLE J OF THE TREATY SIGNED IN WASHINGTON D.C, APRIL II, 1908 AND ARTICLE I OF TREATY SIGNED IN WASHINGTON D.C, FEB. 24, 1925, REFER TO INTERNATIONAL BOUNDARY COMMISSION 1931.
ISLANDS IN RAINY LAKE LETTERED 'Vor'G'BY D.J.GILLON OLS, 1911, PLANS ond FIELD NOTES, DRAWER K-12 (map off le*)
AREAS WITHDRAWN FROM STAKINGS R - SURFACE RIGHTS M R - MINING RIGHTS
jetton____Ordtr No DoH Dlipogition PileNOV 14/62 (R 168472COT 9/t* an "
IKNOV 27/67 (N
MAM ZI/6S (R 2M68
NOV ( 3/62 3 ROMK
RE-OPENED DEC 10/66
ALL ISLANDS IN RAINY LAKE WrTHDRAWN PROM STAKING UNDER SECTION M SUB SEC C OF THE MININ6 ACT
HIGHWAYS— HIGHWAY No. II, 150' R/W-, SEE D.H.O, PLANS, P-3377-10,11,12,15,15 A, 16, |7, IB ond 24,
RAILROADS — CANADIAN NATIONAL RAILWAYS 99'R/w,Ref. No. AA—13539, Nov. 24, 1904, PLAN No. M- 4-6,
TRANSMISSION LINES —H E.PC. TRANSMISSION LINETHROUGH WATTEN TOWNSHIP BY E.H.LOW OLS, 1926,
LO-6627, f.lt-61486, PLAN No. N-17-23,
SYSTEM OF SURVEY
MOTE -LOT AND CONCESSION LINES SHOWN HEREON ARC PROJECTED FROM THE BEST INFORMATION AVAILABLE, HOWEVER, THEIR TRUE POSITION IS NOT GUARANTEED.
FOR OFFICIAL SURVEY PURPOSES CONSULT THE ORIGINAL PLAN AND FIELD NOTES, OF RECORD IN THE DEPARTMENT OF LANDS AND FORESTS, TORONTO.
100
20 O FT
300
400
'//v? B LOCK K- IISOI26
500
a5g 8b)
y
SZCT/QfL A/-32- RAINY
\
RXO MUD
7
f.'
/ /
•ATS*
RED "W O
moIM^MM
St.''"' K fc~--
600
700
800
900
1100
1200
1300
1400
220
Xz ,'-^Vo^Vf 'ti?-.^ .**^ ^i**-' .4-.
XV••^.-•".^Vs
. T"..^
\
.*
/s
•f•\\
^^u
f*'1**
ll
/
l
Xl
\
ARMSTRONG-KURYLIW CLAIMSARMOT IS, HALKIRK TWP. RAINY LAKE,
•MM
LOOKING WESTSCALE:
NOV. I99S. C. J. KURYLIW
