report on the c. v. group baden township
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42A02SE2018 2.20025 BADEN 010
REPORT ON
THE C. V. GROUP
BADEN TOWNSHIP MATACHEWAN AREA, ONTARIO
by
L. J. Cunningham, B.Sc. P. Eng.Mining EngineerDecember 1999
for
Blaine Vallier OPAP #99-505
REPORT ONTHE C.V. GROUP
BADEN TOWNSHIPMatachewan Area, Ontario
A) LOCATION
Southeast Corner of Baden TwpClaim Map No. M0205
Larder Lake Mining DivisionMatachewan AreaN.T.S. No. 42A/2
Longitude 800 , 42'W, Latitude 480 , 02'N
B) LOCATION MAP: Figure l
C) ACCESS
The claims straddle the Montreal River. They are accessible by water
from the Town of Matachewan - the distance being 10 kms. They are also
accessible by all-terrain vehicle via a tractor road which extends from Hwy
566 for 7 kms to an Ontario Hydro control dam located on the C.V. Group.
The exit point for this road is 5 kms north of Matachewan.
D) DESCRIPTION Figure 2
The group consists of 6 contiguous claim groups totalling 37 claim
units which are numbered: LI 213953, L1222565-66, L1222582, L1222689-
90.
E) THIS IS A GOLD PROSPECT
Vein type deposits are the most common in the area - similar to the
Matachewan Consolidated Mine and the Ashley Mine. Both mines were
local past producers.
F) REGIONAL GEOLOGY
The Matachewan camp which includes the C.V. Group is located in
the southwestern Abitibi Greenstone Belt of the Superior Province, 55 kms
west of Kirkland Lake. The volcanic rocks in the camp have been assigned
to the Larder Lake and Kinojevis groups, which are predominantly pillowed
and massic mafic to ultra mafic flows with some pyroclastic units and minor
interflow sedmiment. The volcanic rocks are unconformable overlain by a
narrow belt of sedimentary and alkali volcanic rocks of the Temiskaming
Group, which is spatially coincident with the Larder Lake-Cadillac Break.
All of the large gold deposits of the Abitibi Greenstone Belt occur within a
few kilometres of the Larder Lake-Cadillac Break or the Porcupine-Destor
Break which is approximately parallel and 40 kms to the north. There have
been several periods of intrusive activity in the area of the Larder Lake-
Cadillac Break. The latest intrusives are felsic bodies of syenite which
include the Cairo, Holmes and Dixon stocks in the Matachewan area.
G) PROPERTY GEOLOGY Figures 3, 4, 4A, 5, 6
D. U. Kresz, 1993, OGS Open File #5874, states that the Archean
rocks of Baden Township are metamorphosed volcanic rocks which are
divided into two chemically distinctive groups: a mafic tholeiitic unit and an
intermediate calc-alkalic sequence. They face north and the line separating
the two groups is an east-west line crossing the centre of the property.
Sedimentary horizons 3-30 feet wide of fine-grained wacke, mudstone and
chert occur, conformably within the mafic flows, near the top of the cycle
and are occasionally sheared and carbonatized.
In order to highlight the areas of possible economic potential of the
claim group, the writer has produced a simplified version of the property
geology on Figure 7A.
Intrusive rocks of an early age are very limited in number and size. A
linear dike-like body of diorite to quartz-diorite, with a northeasterly strike
occurs in the northeast corner of the claim group. Kresz indicated an
occurrence of gabbro on the west shore of the Montreal River. A north-south
swarm of Matachewan diabase dikes cross the property.
Early fault and shear zones with an east-west strike cross the property
and according to Kresz these are related to the Larder Lake Break. The locus
for these structures would appear to be in some cases the interflow
sedimentary bands.
The NW/SE Montreal River fault and the North/South faults are,
according to Kresz, late faults.
H) HISTORY
In 1934, visible gold was discovered on present claim L1222690. By
the next year, Woman River Gold Mines had carried out trenching and
drilling of four short holes. The discovery attracted considerable interest and
the following geologists examined the showing:
1. 1934 W.T. Robson, Lakeshore Mines F. Austin, Teck Hughes Mine
2. 1935 G. L. Holbrooke, Sylvanite Gold Mine3. 1938 C.F. Rice, Howey Gold Mines
Robson reported "an irregular quartz vein carrying an exceptionally
large amount of gold." Austin stated that the gold occurred in a northeasterly
striking vein. Holbrooke said that 4 holes were drilled, 3 with negative
results and one returned 1.14 oz over 40 feet. Whether this was core or
sludge was not recorded. Numerous pits and trenches were dug in the region
in an effort to identify other possible gold bearing quartz veins or structures.
In 1973 Melville Mines completed line cutting, mapping and a
magnetometer and vertical EM survey of the property. The site of the
original gold showing was not found. A few short east-west conductors were
defined but no further work was undertaken.
From 1973 to 1996, the Indian Land Caution applied to these claims
and exploration ceased. Kresz reported that he could not locate the site of the
original gold showing.
In 1998 Cunningham and Vallier made five trips to the area of the
Woman River gold find. Pits and trenches are very numerous in an area
estimated to be 1000 feet square. All are collapsed and some are quite deep.
They run north/south and east/west. The source of the gold was not
identified.
I) PROSPECTING TRAVERSES Figure 8
During 1999, five prospecting traverses were made across the claim
group.
Traverse l
The writer and D. Cooper travelled northeasterly from the river across
an outwash plain over two ridges presumably underlain by diabase dikes to
Graveyard Lake, then northwesterly to Baptiste Creek, then south and
westerly along the creek bed to the Montreal River. One outcrop was seen in
the bed of Baptiste Creek, and identified as mafic lapilli tuff.
Traverse 2
From a gravel road (passable to trucks) within the Indian Reserve, the
writer and B. Vallier travelled westerly to Baptiste Creek, then south along
the creek, then returned easterly to the truck. No outcrop was seen. The area
is covered by sand and gravel.
Traverse 3
From the east shore of the Montreal River, the writer and D. Cooper
travelled northeasterly along a badly overgrown and poorly marked old
portage trail in search of pits located in the north central part of the claim
block. Mervin King, an longtime prospector from Matachewan, advised the
writer of the existence of old pits and trenches along the portage and Lovell
(1963, ODM Map 2109) notes copper and sulphide mineralization along the
portage in the same area. Kresz indicates quartz-feldspar porphyry in this
area. Neither the pits, the mineralization nor porphyry were located but
further searching will be carried out in 2000.
Traverse 4
Kresz (1993) reports shearing, carbonate alteration and sediments on
two small islands in Mistinikon Lake immediately west of the CV Claim
Group. Starting on Mistinikon Lake, the write and B. Vallier travelled
easterly to the Montreal River. Locally the west bank of the river is a vertical
cliff over 100 feet high. A wide (± 50 feet) fault can be seen and approached
by boat along the river. No mineralization or alteration are present. The
rocks are massive and uniform, dark grey green in colour. The writer and
Gerhard Meyer, Resident Geologist, who accompanied the writer, conclude
that the rocks are of volcanic origin and possibly are massive fine grained,
ash tuff showing distinct foliation. Similar features were observed by the
writer on flat and limited outcrop on top of the cliff, but otherwise neither
sediments, shearing nor alteration were observed on this traverse.
Traverse 5
From the western boundary of the claim group, the writer and B.
Vallier travelled southeasterly over a prominent ridge (presumable underlain
by diabase) to reach the north edge of a creek flowing, from a small lake,
easterly to the Montreal River. Approximately 1000 feet east of the lake an
old pit was encountered. Limited outcrop and debris from the pit show
massive fine grained dark green rock of mafic origin believed to be ash tuff
exhibiting distinct foliation as observed on Traverse 4 near the river. No
mineralization or alteration were observed. The traverse -easterly along the
north side of the creek - follows low ground to the river and terminates in the
vicinity of a prominent fault which is readily apparent in a cliff face on the
west bank of the Montreal River. Kresz described and photographed this
fault in OGS Open File #5874. It contains a prominent shear, abundant
massive white quartz, and has been sampled by Kresz and many earlier
prospectors (MNDM Assessment files, Kirkland Lake) with negative results.
The return traverse from the Montreal River to Mistinikon Lake did not
encounter outcrop.
J FIELD MAPPING, Figure 9
During 1999, the writer mapped an area measuring 1000 feet x 1000
feet and centered over the mechanically stripped Woman River showing. An
east-west base line and cross lines at 200 feet spacing were established.
Outcrop is not plentiful and the geology is described in detail under
Geology of the stripped area.
This mapping did reveal the following:
1. A 50-foot wide north-south diabase dike occurs approximately
100 feet west of the stripped area;
2. 600 feet west of the Woman River showing and on strike with
an east-west fault (the Woman River Fault) which apparently localized
the gold occurrence, an old trench on the edge of the swamp reveals
the south contact of an northwesterly striking quartz-feldspar prophyry
dike with an exposed width of 3 feet but an unknown true width.
There is no exposed faulting but the writer is of the opinion that the
intrusion is close to the Woman River fault. Old trenches are plentiful
in the area between the diabase and the porphyry dike suggesting that
the Woman River personnel suspected a connection existed between
the gold occurrence and the porphyry dike. Two samples - one of
silicified rock on the exposed south contact of the porphyry and one
from a 2"-6" quartz vein with + \ 07o pyrite, located approximately 100
feet east of the porphyry - returned 87 ppb and 14 ppb gold
respectively.
3. A few scattered rusty patches (pyrite) 2"-4" in diameter were noted on
line l O to the southeast of the showing.
4. Two long, deep trenches, now collapsed to the southwest of and on
strike with the Woman River vein, suggest that the early workers were
seeking an extension to the Woman River Vein. This emphasizes the
writer's belief that the pocket of native gold was found in the NE-SW
striking Woman River vein and was localized at the Woman River
fault.
5. Four, steeply dipping, mafic dikes occur in the stripped area. They
strike north-easterly, average 2-4 feet in width and the maximum
observed length was 25 feet. They are finely and uniformed grained,
dark geen in colour, without chilled edges and have not altered the
intruded rocks. These dikes have a fresh, unaltered appearance. They
are obviously later in age that the alteration event which effected the
flows within the stripped area. They are not diabase dikes. Kresz
states that mafic intrusive rocks, related to the mafic flow rocks,
are scarce in Baden and Argyle Townships (the mapped areas) and are
possibly represented by andesite dikes.
K. DESCRIPTION OF STRIPPED AREA
Kresz states that the Archean rocks of Baden Township are
metamorphosed volcanic rocks, subdivided into 2 chemically distinct groups:
a mafic tholeiitic unit and an intermediate calc-alkalic sequence. The local
area (including the stripped portion) of the Woman River (WR) occurrence
overlies flows of the mafic tholeiitic sequence. According to Kresz they
consist of massive and pillowed varieties. No pillow features were noted by
the writer. The rocks observed were massive, fine-grained but the presence
of a short + 10 foot lense, 2-12 inch wide of graphite with nodular pyrite is
concluded to be interflow sedimentary material. Approximately 50 feet east
of the graphitic horizon, a short ^ 5 feet) layer of distinct well rounded
quartz eyes (l /4 - 1/2 inch in diameter) striking roughly parallel with the
graphitic horizon was observed and it is believed to represent quartz-filled
amygdules, possibly indicating gas cavities in the upper part of a flow. Kresz
recognized variolites in a cliff face on the west short of the Montreal River -
approximately 1200 feet north of the WR occurrence. He states that
variolites are not "unequivocally recognized" in Baden Township and refers
to an island in Mistinikon Lake (which touches the west boundary of the CV
Claim Group) where outcrops show "millimetre size white rounded spots
which maty have been produced by spherulitic growth". Similar features
10
were observed by the writer in a small local area, less than 5 feet in diameter
located immediately east of the WR shaft.
The rocks are most commonly a uniform grey-pale green colour
within the C. V. claims but the rocks within the stripped area have a distinct
"bleached" appearance - the weather surface is a white-grey colour. On a
freshly broken surface the rock shows a whitish vitreous rind up to l /4 inch
thick and below this a typical grey-green colour. They are in the writer's
opinion hydrothermally altered and most intensely in the shaft area. Kresz
notes that "bleached rocks" are most commonly the result of sericitization
and silicification. This latter feature is readily evident within the stripped
area and results in a cherty appearance in the areas adjacent to veins, faults
and fractures. Free quartz in the form of veins, stringers and pods is plentiful
in the area south of the WR fault but rare within the area north of the fault.
A peculiar feature on outcrop surface, particular in the shaft area, are
raised (elevated) ribs of resistant rock following millimetre wide , 10-50 cm
long, fractures containing silicia, epidote and chlorite. There are numerous
and randomly oriented. Associated with these features are similar elevated
irregular patches of 3-5 cms in size. The result is a rock surface with a
highly irregular corrugated surface, abrasive to the hand.
Sericite, if present, was not recognized nor do the rocks exhibit a
brown, rusty colour typical of carbonate alteration which is a common feature
of the Matachewan and Kirkland Lake mining camps. There is little or no
reaction of the rocks to cold dilutes HCL.
11
Structure
The most important structure in the stripped area is a steeply dipping,
E-W zone of fracturing crossing the central part and called the Woman River
Fault (WRF). It consists of a series of shears, 1-8 inches wide, with
branches, splits and crossovers over a width of 10-12 feet. The wider shears
show l -2 inches of gouge and an occasional narrow l -4 inch lense of
discontinuous quartz and occasionally a small amount of pyrite. They are
oxidized, water stained with a dirty brown discolouration and can be traced
for 350 feet across the stripped area. Bands of fine parallel fracturing 1-5
feet wide are located north and south of the WRF and appear parallel to it.
They are not located immediately adjacent to the WRF but occur at intervals
up to 100 feet from the WRF. They show silicification and occasional pods
of quartz.
Kresz considered E-W faulting to be regional, first order structures,
possibly related to the Cadillac-Larder Lake shear system. Late, second order
faults would include the NW-SE Montreal River fault which bisects the CV
property, and the north/south Narrows Lake and Mistinikon Lake faults
which are in the immediate area.
Within the stripped area and largely located south of the WR fault,
there is a great variety of minor faulting consisting of
a. N.E. and N.W. narrow, discontinuous vertical shears;b. Low angle jointing (300-45 0) striking NE and NW;c. Swarms of micro fractures, a millimetre or two in width and
5-10 cms long with random orientation, suggesting micro-brecciation.
12
Prominent steeply dipping, white, barren, quartz veins, striking north,
northeast and northwest, varying from 1-12 inches in width and dying out
within 150 feet of the WRF are believed to occupy tension fractures.
It would appear that the immediate area (mainly south of the WRF)
had been subjected to uplift possibly by a small igneous intrusion (one of
which does occur 500 feet to the west) creating
1. tension fractures now occupied by quartz veins;2. random oriented faults and joints;3. microbrecciation.
Mineralization
Massive coarse pyrite is the most striking mineralization present. It
occurs in spectacular quantities over a limited area between the north end of
the shaft and the WRF. Lesser amounts were noted in and near the WRF on
lines 5+50E and 8+50E. This is a style of pyrite mineralization not
commonly associated with quartz vein gold deposits.
Lesser amounts of massive, fine grained pyrite - mostly in modules -
occurs associated with the graphitic interflow horizon.
Fine grained disseminated pyrite + J-2% was noted (1) in silicified
zones near the Woman River Vein (WRV) in the vicinity of the WRF and
(ii) in a silicified zone near the SE end of the graphitic interflow horizon.
On line 8+50E and approximately 20 feet south of the WRF a pod of
galena 1/2-1 inch wide and 2 inches long was noted in a narrow NW striking
fracture. A sample ran 120 ppb gold.
13
Hematite in botryoidal and crystal form is developed in thin coatings
on flat outcrop in several locations north of the WRF.
Nineteen (19) samples were assayed for gold by Swastika
Laboratories, Swastika, Ontario. Sampling by hammer and moil by the
writer was concentrated on the pyritic and silicified portions of the WRF, the
WRV, coarse pyrite near the shaft and a silicified and pyritic area at the SE
end of the graphitic interflow horizon. Only 6 samples exceed 100 ppb and
returned 120, 111, 144, 158, 326 and 329 ppb respectively. These 6 sample
sites were associated with silicification in and near the WRF. The two
highest values, 326 and 329 ppb, were obtained from the junction of the
WRV and the WRF.
There is no evidence existing today in records or on the ground to
identify the actual site of the spectacular gold occurrence which caused the
excitement in 1934, but it is the writer's opinion based on (i) these few
elevated gold values; and (ii) the geological and physical evidence,
that the splash of free gold was probably located at or near the junction of the
WRF and the WRV.
14
CONCLUSIONS AND RECOMMENDATIONS
The Woman River showing is geologically interesting but the writer
agrees with the early investigations (Austin and Robson, 1934: Holbrooke,
1936; Rice, 1938) that the occurrence offers little economic potential and
further work in not recommended.
It is recommended that the old trenches in the north central part of the
claim group, where chalcopyrite and quartz-feldspar porphyry have been
reported, be located and evaluated.
L. J. Cunnmgham, B.Se. P. Eng
December 1999
Figures1 Location Map2 Claim Map3 Geology Matachewan Area4 Property Geology (OGS Map P3235, Kresz D.U.)4A Geological Legend5 Property Geology: Volcanic facies (OGS OFR #5874 Fig.3)6 Property Geology: Structure fe Alteration (OGS OFR #5874 Fig 12)7 Simplified Property Geology8 Prospecting Traverses9 Geology: 1000' x 1000' Grid; Woman River Area10 Geology: Stripped Area; Woman River Showing
___l_t.C.V. Group, r--*— —
FIGURE l
LOCATION MAPMATACHEWAN AREA
M' -J
INDM - M:ning Claim Map http://www.mndm.gov.or. .ca/win-cgi/cbl msmapcg i.d;
Ontario Ministry of Northern Development and Mines Mines and Minerals Division
Bard Copy Download Ful Map hele Scale image i
fS&^i^^ t. f Jj A11
O 400 800 1000 i l l l
leaoir
ittv^SS^H^^
Back l Main Menu | Mining Lands
^ l OntarioThis site maintained by the Government of Ontario
Comments and feedback to: srevc.bcncteautS'udm.gov.un.ca
© Copyright 1998 Queen's Printer for Ontario - - - —-~—
This information is provided as a public service, but we cannot guarantee that the information is current or accurate. Readers should verify the information before acting on it.
C.V. GROUPBADEN TWP.
CLAIM NO. M.0205
Dated 4/29/99
FIGURE 2
BADEN TWP
MAUDELAKEMINES
lf
AU' h pt*!* 7
ALMA TWP
INDIAN
RESERVE
No. 72
CUNNINGHAM PROPERTY
HOLMES STOCK
HOLMES TWP
(CUNNINGHAM PROPERTY)
DAVIDSON SYENITE STOCK PRODUCED - l MILLION OZ. Au RESERVE - 1.2 MILLION OZ. Au
MATACHEWAN AREAGEOLOGY
LEGEND
DIABASE DIKES OMITTED
5-HURONIAN SEDIMENTS
4-SYENITE INTRUSIVESSTOCKS-CAIRO 4a, DIXON 4b, HOLMES 4c
3a- PORCUPINE Gp SEDIMENT
5- TEMISKAMINQ Gp ALKALI PYROCLASTICS-, SEDIMENTS
2-KINOJEVI8 Qp-MAFIC VOL.
l- LARDER LAKE Op - MAFIC VOL. la-FELSIC VOL. Ib
l 2 3
Km
SCALEFIGURE 3
GEOLOGY C. V. GROUP
from OGS Open File 5874
Map P3235 Geology Argyle and Baden Twps
D.U. Kresz 1993 Scale 1:20,000 Figure 4
ABBREVIATED LEGENDFROM
MAP P 3235OGS OPEN FILE #5874
DU KRESZ 1993
11A DIABASE DIKES
6 INTERMEDIATE TO FELSIC INTRUSIVE ROCKS c - Qtz - Feldspar porphyry
5 INTERMEDIATE INTRUSIVES a - diorite to qtz diorite b - andesite dikes
4 MAFIC INTRUSIVE a - gabbro
3 METASEDIMENTS a - wacke, mudstone b - chert
2 INTERMEDIATE VOLCANICSa - massive h - tuff - breccia b - pillowed m - prophyritic c - breccias s - carbonatized f -tuff-lapilli
l MAFIC VOLCANICS a - massive b - pillowed c - carbonatized
Symbols V-A-- Drill Hole
D Test Pit
Schistosity
Tectonic Lineation
Bedding - Tops
Bedding - Tops Unknown
Geological Contract
Lineament
Shear Zone
Sand, Gravel
Gold Figure 4A
Town of Kirkland Lake
ADMINISTRATION
MEMOTo: Mayor R. Denton, Members of Kirkland Lake Town Council, Department
Heads, Administration Staff, D. Preston, D. HarasymFrom: G. ShaySubject: Time AwayDate: November 27, 1998
Please be advised that I will be away from the office on December 7 and 8, 1998, attending a Year 2000 seminar in Toronto.
During my absence please refer any matters related to my office to Pam Buchanan.
Gary D. Shay,Chief Administrative Officer
GDS/nm
D:\1998\CAO\CORRESP\NOV-98\NOV-27\TIMEAWAY.WPD
on C.V. GROUP
OUTLINED IN Bil
2 Km
j Volcanic racks dominated by flow*
Volcanic rocks dominated by tephra deposit*
Sedimentary horizon*
Volcanic facie* unatrfain due to lock of exposure
/////\ Intrusive Rocks
Proterozoic cover
k* Occurrence of pillow structures(in mafic rocks; In Intermediate rocks)
9 Occurrence of vokanlc-dasflc conglomerate* Occurrence of plagioclase-phyrlc rocks* Occurrence of pyroxene-phyrlc rocks* Occurrence of amygdular rocks* Occurrence of variolitic rocks BADEN TWP.
*f- Synclinal axis
GEOLOGT
Figure 3: Volcanic facies distribution in Argyle and Baden Townships.
0.0.S. OPEN PUB 5874 D. U. Kresz, 1993
FIGURE 5
Stratigraphic Facing
Strike of Tectonic FolIoHon Tectonic Lineation: Inclined, vertical
Shear Zone
Syncline Axis A Au Occurrence
L * 4 4. t j Intrusive Rocks
Fault; spots Indicate down throw side, arrows Indicate horizontal movement
C.V. GROUP
OUTLINED IN BLUE
Lineament Carbonatized Rocks
Green Mica Bearing Rocks Serialized Rocks
Figure 12: Map showing the various structural elements in Argyle and Baden townships as well as locations in which the rocks show obvious hydrothermal alteration.
GEOLOGY BADEN WP. .
O.G.S. OPEN FILE 5874 D. U. Kresz, 1993
FIGURE 6
ral uiQlui
aucu
Qtz-feldspar porphyry
DioriteSediments :SNN^N.
Intermediate VolcanicsMafic VolcanicsGold occurrencesChalcopyrite
C.V. GroupBaden Twp
Simplified GeologyScale 1:20,000
O 0.5 l km f w ~ j
SourceKresz, D.U. 1993 Map P3235
Cunningham, L. 1999 Field Work
Figure 7
Scale 1:20.000 O 05 l km
11 Diabase Dikesa-Matachewan Age
2 INTERMEDIATE VOLCANICS a - massive
l MAFIC VOLCANICS a - massive
C.V.GROUP BADEN TWP
showingPROSPECTING TRAVERSES
L. J. CunninghamDecember 1999
Figure 8
la
CREEK
PUMP SET-UP
PIT ^ 65' LONG /fi
CLAIM POST LINE
14 PPB D QTZ 070 0
SHAFT87 PPB
SMALLWOMAN RIVER VEIN
IRREGULAR QTZ
TR CAVED
TR CAVED
/jLV ^^N \
^ 1vx g ^^^^ v^/cofl\. CAI II T
OLDTRENCHCAVED
T ^?J w y.\) "i "f"
\CLAIM POST
Q 1-1222689D 2-1222690
BASELINE\ rv
io. \v-.tt.t
45-l^
\-30
la
o: ui28Sg
STRIPPED AREA'
^
RIDGE^/^
—————t
V uj
\i
LO:
\cl
ISla
\
RUSTY SPOTS-
la
8
60 STEEL HYDRO TOWER 10
3S
g li'o
COLU Q
< O1- CCu >o
Q. UJ UJI-co
•3UJo: h
4S
5S
Geology 1000' x 1000' Area
centered onWoman River ShowingClaims L1222689-90
Baden Township-OntarioScale l inch-100 feet
0-L—
100i ,
200 feet
L. J. Cunningham, B.Se. P. Eng December 1999
Legend
11 Diabase Dikes a-Matachewan Age
Felsic Intrusive c-Qtz-feldspar porphyry
Mafic Intrusive b-andesite dike
Meta Sediments d-graphitic
Mafic Volcanic Rocks a-massive
Symbols
Swamp
" Tractor Road
k "'^ Stripped Area ^i_ JJL y rr
\ .. i Tr. Trench
D Pit, Shaft
/ ) Outcrop
^, --^' Geological Contact
Fault -f- VERTICAL
Joint
Qtz Vein
Dike
Graphitic Interflow Sediment
FIGURE 9
A/ l
HEMATITE-H BOTRIOYDAL 8. CRYSTAL FORM
MAFIC DIKES5 VERTICAL MAFIC
DIKE 2' WIDEl - 3 WIDE VERTICAL
ROUND QTZ EYES 1/4"-1/2
OLD ( TRENCH /3'-5' DEEP CAVED
-4- ^XHVVKA ^
CL 122269(5 f\WOMAN RIVER FAULT
'T.^r/WevERT.CAL POD GALENASHAFT
W.R. VEIN
DRILL HOLE -S?-- —— QTZ
PODS 1-2 QTZ POD l -2
GEOLOGYSTRIPPED AREA
WOMAN RIVER SHOWING
CLAIMS 1222689-90C.V. GROUP
BADEN TOWNSHIPO________50________100 feet
SCALE: l" " 50'
L.J. CUNNINGHAM, B.Sc. P.Eng. DEC. 1999
LEGE N D
MAFIC DIKE -ANDESITE
SEDIMENTS d - GRAPHITIC
MAFIC VOLCANICS a- MASSIVE
' STRIPPED AREA
V OUTCROPMUCK PILE
WATER
DIKE
QUARTZ VEIN
GRAPHITE HORIZON
TRACTOR ROAD
WOMAN RIVER SHAFT
TRENCH
FAULT
FRACTURE
E"r SWARM OF FRACTURES
X PYRITE
^ SILICIFICATION
H HEMATITE
\ DIRECTION S ANGLE OF DIP
-H VERTICAL
2S FIGURE 10
Ontario Ministry ofNorthern Developmentand Mines
Declaration of Assessment Work Performed on Mining Land
Mining Act, Subsection 65(2) and 66(3), R.S.0.1990
Transaction Number (office use)
LOOOQQ QOQ48Assessment Files Research Imaging
i of subsection 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, he assesment work and correspond with the mining land holder. Questions about this )f Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury,
42A02SE2018 2.20025 BADEN 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 .
L. J. O OClient Number
Address Telephone Number
Utf. P2Nf H}Fax Number -5374Client Number
AddressSI —
—S- 1Telephone Number-~Fax Number
2. Type of work performed: Check (S) and report on only ONE of the following groups for this declaration.
Geotechnical: prospecting, surveys, assays and work under section 18 (regs)
Physical: drilling stripping, trenching and associated assays
Rehabilitation
Work Type Office UseCommodity
Total S Value ofWork Claimed 3C.
Dates Work From Performed l Day
To
( aT)fd NTS Reference
Year
Global Positioning System Data (if available) Township/Area C) A -rv r~ 11 Mining Division
M or G-Plan Number Resident Geologist District 4
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)
L- . vj . v^. c? (v^ ik^ f tj u /v (MAddress ,
Name
Address ,/
Name -
Address S'
Telephone Number~~7 o ^ — t?6 7 ~ S^^ 2.0
Fax Number-74V - 5Ti67 - ^"37^
Telephone Number
Fax Number
Telephone Number
Fax Number
4. Certification by Recorded Holder or Agent l, u . M . C.uMN4fKJ(StfAir*\ ,do hereby certify that l have personal knowledge of the facts set forth in
(Print Name)
this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.
Date C.Agent's Address Telehone Number
0241 (03W7)
RE CE/VED R UKEDIVISION
26 2000 •
RECEIVEDJAN 2 7 ^m
GEOSCIENCE ASSESSMENT OFFICE
rm.
Worn to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining where work was performed, at the time work was performed. A map showing the contiguous link must accompany this
UJooso. noo^sning Claim Number. Or if rk was done on other eligible ining land, show in this lumn the location number dicated on the claim map.
i
)
'
3
3
l
5
TB 7827
1234567
1234568
IZ22.S4 Sl 2.2,2.5 (o^i XZ2 58^l 'L22r(0 clO
Column Totals
Number of Claim Units. For other mining land, list hectares.
16 ha
12
2
-7
83LI
z^
Value of work performed on this claim or other mining land.
526,825
0
5 8,892
V5"o *"c\oo~^?5o-
125*2-
Zo^oZ*
Value of work applied to this claim.
N/A
524,000
5 4,000
2^c?o^2)2 d0 -
\ Zoo-^OO"
K^oo**
Value of work assigned to other mining claims.
524,000
0
0
O
O
o5*400 ^
•54-00*
Bank. Value of work to be distributed at a future date
52,825
0
54,892
#102L
QIOZ^.. , do hereby certify that the above work credits are eligible under
(Print Full Name)ubsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim
'here the work was done.
ignature of Re toOf older or Agent Authoi/LOl''U-^C
in Writing
aDate
Instruction for cutting back credits that are not approved.
5ome of the credits claimed in this declaration may be cut back. Please check (S) in the boxes below to show how you wish to )rioritize the deletion of credits:
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 D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):
tote: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.
:or Office Use Only—————————.^-^—————deceived Stamp
0241 (03/97) RECEIVED LARDER LAKE
MINING DIVISION
JAN 26 2000
Deemed Approved Date
Date Approved
Date Notification Sent
Total Value of Credit Approved
Approved for Recording by Mining Recorder (Signature)
RECEIVEDJAN. 2 7 2000
GEOSCIENCE ASSESSMENT OFFICE
Ontario Ministry ofNorthern Developmentand Mines
Statement of Costs for Assessment Credit
Transaction Number (office use)
rsonal 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 ting Act, this information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. estions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake ad, Sudbury. Ontario, P3E 6B5. -,
Work TypeUnits of work
Depending on the type of work, list the number of hours/day worked, metres of drilling, kilometres of grid line, number of samples, etc.
Associated Costs (e.g. supplies, mobilization and demobilization).
Cost Per Unit of work
Total Cost
4 riz 81loo
V- l 0 00
-'^n Costs
2.QE1
Food and Lodging Costs — 2^JLwc C^. 420
Total Value of Assessment Work
Calculations of Filing Discounts:
1. Work filed within two years of performance is claimed at 1000Xo of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 500Xo of the Total
Value of Assessment Work. If this situation applies to your claims, use the calculation below:
TOTAL VALUE OF ASSESSMENT WORK K 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:
v~l, hereby certify, that the amounts shown are as accurate as may reasonably(please print full name)
be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying
Declaration of Work form as I am authorized to make this certification.(recorded holder, agent, or state company position with signing authority)
/A0212 (03/97)
1RECEIVED
JAN 2 7 2COOGEOSCIENCE ASSESSMENT
OFFICE
OntarioMinistry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines
Geoscience Assessment Office 933 Ramsey Lake Road
March 2, 2000 6th FloorSudbury, Ontario
LEONARD JOSEPH CUNNINGHAM P3E 6B51 MCPHEEAVENUEKIRKLAND LAKE, Ontario Telephone: (888) 415-9845P2N-1M1 Fax: (877)670-1555
Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm
Dear Sir or Madam: Submission Number: 2.20025
Status Subject: Transaction Number(s): W0080.00048 Approval
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 LUCILLE JEROME by e-mail at lucille.jerome@ndm.gov.on.ca or by telephone at (705) 670-5858.
Yours sincerely,
ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section
Correspondence ID: 14634
Copy for: Assessment Library
Work Report Assessment Results
Submission Number: 2.20025
Date Correspondence Sent: March 02, 2000 Assessor:LUCILLE JEROME
Transaction NumberW0080.00048
Section:9 Prospecting PROSP10 Physical PSTRIP 12 Geological GEOL
First Claim Number1222565
Township(s) l Area(s)BADEN
StatusApproval
Approval Date
March 01, 2000
Correspondence to:Resident Geologist Kirkland Lake, ON
Assessment Files Library Sudbury, ON
Recorded Holder(s) and/or Agent(s):LEONARD JOSEPH CUNNINGHAM KIRKLAND LAKE, Ontario
SLAINE WILLIAM VALLIER KIRKLAND LAKE, Ontario
Page: 1Correspondence ID: 14634
fRobertson Twp. M. 310
ShtbaTwpM3(5
g ( , v
S 1222447 lPi l
——-r---! . t 12222 5 1222668
2222
W\
1227003
'2S9
1205575
Powell Twp. M.241
42A02SE2018 2.20025 BADEN 200
CMO CM
D6
THF TOWNSHIP OF
BADENDISTRICT OF
TIMISKAMING
LARDER LAKEMINING DIVISION
SCALE: 1-INCH 40 CHAINS
LEGENDPATENTED LAND CROWN LAND SALE LEASES
LOCATED LAND LICENSE OF OCCUPATION MINING RIGHTS ONLY SUBFACE BIGHTS ONlV ROADSIMPROVED ROADS KING'S HIGHWAYS RAILWAYS POWER LINES MARSH OR MUSKEGMINESCANCELLED PATENTED S.fl.O.
or
c.
NOTES
40Q 1 surf oca rights rtcervation along the chores of oil IcHes and rivers
Ftoodlnq rights la contour tlevalion 870 to Ont, Hydro .L.O. 7601 File : 12290 v.Z
SEC 35 W-LL-C1602/99 ONT MAY 17/99 MSS
Stihini. oc4iofl/R]) M(N'WG a SLJRl-Ar-F RlGMTi, HFOPFW|r:O TO
, SAl.f Ofl ifAbh.WITHDRAWN VJNPFR
&SSE
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCE^. AND ACCURACY IS NOT GUARANTOR THOSE WISHING TO STAKE MIN INfi C[ AIMS SHOULD CON S JIT WITH IHt MININU RFCOflDER. MINISTRY OF NORTHERN OEVfLOP MtNT AND MINES. FOR AD OiriONAL INFORM ATION ON THE STATUS OF THF LANDS SHOWN HERFOfcL
PUN NO M. 20 5
(JNTAKIU
MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH
ARCHIVED APRIL, t (997
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