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2.14493 ANGLESEA 010
ASSESSMENT WORK DURING 1991 ON
H. DOWHALUK KILLER CREEK CLAIM GROUP
ANGLESEA TOWNSHIP, L&A Co.,ONTARIO
Covering Dates:
April l, 1991to
December 20, 1991
by Harry Dowhaluk, B.A.,F.G.A.C.
December 20, 1991
- r4/
HARRY DOWHALUK
/:A'-3xv7 h/;;m^N*AHY|^i;0 II
\ -p'1 * ''. .* *''--^viv^-^i'^ 'W&i^. ij'v\fe^i^
31CMSW8081 2 .H493 ANGLESEA 010C
CONTENTS
MAPi ANGLESEA TOWNSHIP VOLCANIC BELT a
INTPODUCTION . . . . . . . . . . . . . . . . . . . . . . , . . . l
PROPERTY, LOCATION, ACCESS............ l
TOPOGRAPHY. . . . . . . . . . . . . . . . . . . . . . . . . . . . 2HISTORY AND PREVIOUS WORK . . . . . . . . . . . . 2
PLEISTOCENE GLACIATION . . . . . . . . , , . . . . . kTAELE OF FORMATIONS . . . . . . . . . . . . . . . . . . 5
GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
A1 203 - (FeO * Fe20;j*Ti0 2 ) - MgO Plot.. ?STRUCTURAL GEOLOGY . . . . . . . . . . . . . . . . . . . 8ASSESSMENT WORK . . . . . . . . . . . . . . . . . , . . . . 8
SUMMARY OF STRIPPING . . . . . . . . . . . . . . . . . 9
THE GS ZONE . . . . . . . . . . . . . . . . . . . . . . . . . . 11
THE E- 12 SHEAR ZONE . . . . . . . . . . . . . . . . . . 13
SOME MAGNETIC ANOMALIES . . . . . . . , . . . . 13
CROSS ZONE . . . . . . . . . . . . . . . . . . . . . . . . . . 14
EAST BOUNDARY ZONE . . . . . . . . . . . . . . . . . . 14
E- 16 ZONE . , . . . . . . . . . . . . . . . . . . . . . . . . 14
CONCLUSIONS Se RECOMMENDATIONS . . . . . . . 16
REFERENCES . . . . . . . . . . . . . . . . . . . . . . . . . . 18
CERTIFICATE . . . . , . . . . . . . . . . . . . . . . . . . 19
MAP #ls INDEX MAP, KILLER CREEK CLAIMSScale j l in. - 200 ft (in pocket
MAP 2A: GS Zone, Sample Plan MAP 2Bi GS zone, Stripping Plan MAP 3 : E- 12 Zone Se Gold in HumusMAP 4 : E- 16 Zone, Geology, Sampling
in pocket MAP 5, Log Pile Zone, Geology, in pocketMAP 6, East Boundary Zone j Geology MAP 7, Cross Zone? Geology MAP 8, Lines 6-S, 9-S. Geology MAP 9, Mag Anomalies} N.W. Corner ASSAY REPORTS
HARRY DOWHALUK
-1-
INTRODUCTION
This report covers the assessment wor.k done on twelve unpatented mining claims situated in the northwest quadrant of Anglesea Township in the county of Lennox and Addington, Ontario during the year of 1991. Work consisted mainly of stripping and detailed mapping, sampling, some gepchemistry and minor line cutting. This program of work was aimed at evaluating the magnetic and VLF electromagnetic anomalies obtained in the previous year and also to pick out some diamond drill targets. The work was carried out under the Ontario Prospectors Assistance Program (Grant No. OPG91-034, OPAP Registration No. OP91-20?).
PROPERTY. LOCATION. ACCESS
The twelve claims were recorded on September 15, 1989 and comprise 600 acres, more or less.The claims are held 100# by the writer, Harry Dowhaluk, whose address is Box 118, Tamworth, Ontario, KOK 3GO. The claims are in Anglesea Township which is subdivided and is in lennox and Addington County. These claims are further described as follows:Concession XIII Si lots 28,27,26. 25, claims 1104437, -38, -39,-40 Concession XII Ni lots 28,27,26, 25, claims 1104441, -42, -43,-44 Concession XII Si lots 28,27,26, 25, claims 1104445, -46, -47,-48
There is easy access to the claims by vehicle. The claims lie astride the Cloyne-Gilmour access road. This road goes west from the north end of the village of Cloyne on Highwqy 4l, skirts the south shore of Skootamata lake, crosses Killer Creek in two places, crosses our claim group and proceeds westwards accross Grimsthorpe Township and on to Gilmour near Highway 62. There are four old logging roads on the property to provide additional access.
The NTS 1:50,000 topographic map that covers the area is numbered 31 C/14, Mazinaw Lake. The MNR map M-43, Anglesea Township, shows the subdivisions and claims. The Ontario Geological Survey has recently released the Open File Map 132 , "Geology of the Mazinaw Lake Area (31 C/14". This publication mainly concerns the southwest part of the area which includes the property area.
HARRY DOWHALUK
-2-
TOPOGRAPHY
The claim block is roughly 1,000 feet above sea level (330 meters). The terrain is hummocky with relief generally less than 100 feet.. There are numerous beaver ponds, large and small, often filled with standing dead trees (shlekos). The Killer Creek drains the whole area; it is a slow meandering stream in the north part of the claim block where it cuts through a large beaver meadow, but has a series of rapids, cascades and fast water in the lower end. It enters a large marshy pond at the east end from which it continues easterly to spill into Skootamata Lake.
The area has been extensively logged over the years. Where some of the larger trees are left, the forest floor is cleanj but most of the forest has an upper story of sporadic "la'rge trees'; and a very brushy understory. The mixed forest consists of balsam fir, white pine, hemlock, white cedar, white spruce, sugar maple, white birch, aspen poplar, basswood, black ash and the occasional beech. Significant underbrush consists of speckled alder (wet places), hazelnut, moose maple, and mountain holly (in ash swamps). Prickly raspberry and thimbleberry canes thrive on ground disturbed by logging machines.
At present, the claim-block has no permanent inhabitants; however, there are two small hunting camps. There were no logging operations in 1990 or 1991.
The climate is humid continental with cool summers and cold winters. Snow covers the ground for about four months of the year.
HISTORY AND PREVIOUS WORK
The claims are in the Eastern Ontario Gold Belt. Over half of the production in this belt has come from one mine - the Cordoba in the Marmora area, which, from 1897 to 19^0 mined 119,813 tons of ore presumably grading 0.16 oz/t gold which was valued at $i^50,826. The Addington Mine (Golden Fleece) in nearby Kaladar Township, the Ore Chimney in nearby Barrie Township and the Gilmour Mine in Grimsthorpe Township are all well known gold properties in the general area of the claim block. Quartz stringers and veins carry the gold in these properties.
HARRY DOWHALUK
-3-
In 198?, United Reef Petroleums Limited staked tweny claims which - form a block on the north side of the subject twelve claims to follow up an occurence of gold from which a grab sample returned a value of 0.19 oz/t gold. A grid was cut and magnetic and VLFelectromagnetic surveyswere carried out on the twenty claims under
of thv direction,, Wayne Johnson, geologist. This work was followed upwith some backhoe trenching.
At about this time, some claims were staked on the east part of the subject claims as part of an investigation of building stone potential of the Killer Creek Gabbro. These claims were abandoned.
In 1989, the writer carried out the Killer Creek Project under a grant from OPAP. This involved reconnaissance mapping-prospecting (with some geochem) in a swath along the Cloyne-Gilmour access road from the mouth of Killer Creek at the west end of Scootamata Lake westwards to the Partridge Creek bridge in Grimsthorpe Township. This work indicated large zones of fine disseminated pyrite j also, a small flat-lying quartz vein four inches wide yielded an assay of 0.6?4 oz/t gold. The twelve claims were staked in late summer and recorded on Septeber 15i 1989* These claims are known as the Killer Creek claims.
In the following year, 1990* the writer carried out 16.7 miles of line cutting at 300-foot intervals, a VLF electromagnetic and magnetometer surveys, as well as geological mapping on a scale of i inch to 200 feet.This was carried out under an OPAP grant.
During the summer of 1990, the southwest quadrant of the Mazinaw Lake area (31 C/14) was mapped by R, M. Easton of the Geological Survey of Ontario. The twelve claims are covered by this mapping. (Open File map 132). Easton shows the Partridge Creek Shear Zone which crosses the claims and coincides with the strongest":anomaly on the.property, namely, E-16.
During 1991, the writer did hand stripping on some nine areas the details of which are shown on smaller larger-scaled maps. An index map on a scale of one inch to 200 f eeti shows theJ location of the detailed maps.
HARRY DOWHALUK
PIEISTOCENE GLACIATION
Gravelly till of Pleistocene age-covers the entire property. Since both the direction of glaciation and the strike of formations are south, there is a tendency to north-south cragsand-tail drumlin oid ridges.The drift cover is shallow for the most part and the terrain is hummocky. The till is to a large extent lodgement till - the lowermost layer deposited at the base of the glacier. Consequently, the till tends to reflect the nature of the underlying rock. There is one large erratic of dolomitic marble on the east side of the GS zone.
The till contains abundant clasts of basalt up to one foot or more in length. Oxidation of the basalt clasts in the top three feet gives the till a bright red-brown colour.
Digging small holes in-'.theiiiir.airihthelyiciri^ty' of an&roaiiee^tsr. provides clues to explain the anomaly, e.g., some disseminated pyrite and pyrrhotite grains in basalt clasts on a small magnetic ':-. anomaly appear to account for the slightly higher mag values.
Marshy areas where large low mag readings are extensive could be underlain by clay.
HARRY DOWHALUK
-5-
)TABLE OF FORMATIONS
QUATERNARY
PLEISTOCENE and RECNT
Glacial drift, gravel, sand, clay, swamp depoits, soil.
PRECAMBRIAN
PROTEROZOIC
ACID INTRUSIVE ROCKS
Feldspar Porphyry (FP) Dikes
MAFIC INTRUSIVE ROCKS (Killer Creek Gabbro)Gabbro (Gb)Anorthositic Gabbro (Gba)Melanogabbro (Gb)
CLASTIC METASEDIMENTS
Arkose (Ark)Hornblende biotite schist (HB sch)Graywacke (Gwke)Feldspathic wacke (FW)Quartz wacke (QW)
MAFIC METAVOLCANICS (Tudor Volcanics) 1.3 b.y.Basalt (tholeiite) (Vb)
Massive (Vm), Schistose (VbsTuff (Vbt)
GEOLOGY
The claim block is in the Grenville Structural Province. The western two-thirds of the property consists of basaltic metavolcanics of the Tudor Formation which have been dated at 1,3 b.y. The eastern third of the property is underlain by rather coarse-
grained anorthositic gabbro (The Killer Creek Gabbro).The ODK map No. 2053, Madoc area, shows the Tudor volcanics
to be horseshoe-shaped in Anglesea Township. The belt comes into the southeast corner of Anglesea Township and continues northward through Cloyne, then arches westwards on the north side of Skootamata Lake to continue southerly along the Anglesea-Grimsthorpe!'boundary.
The basalt is black in colour, fine-grained, massive to schistose and has been metamorphosed to fine-grained hornblende and white plagioclase} the latter mineral shows a marked tendency to segregate
HARRY DOWHALUK 1p 1^9, GAG Spec Paper #16
-6-
as small clots or grains but some of these may be distorted amygdules. A whole rock analysis of one sample shows the basalt to be tholeiitic. The prevailing schistocity is north to northeast. Shearing on the surface often gives rise to rows of weathering pits, or pot-holes,which are up to two inches deep. The rock f:weathers dark green.
The gabbro is typically -coarse-grained., ofL medium colour and the plagioclase is conspicuously. snow-\vhite.~Sills 6f^gabbro "are intercalated with the volcanics in some places.
Two whole rock analyses were made of the two main rock types. :/. ^' : - i ; '"'"' ; #WRA-1'- ' WRA-2
L-15-S, 9-W L-21-S, 20E
Basalt Gabbro
Sl0 2 ^7.08 ft 50.02
A1 203 13.65 20.49
Fe203 15.51 7.88
5.200.1210.423.550.560.83
0.18
A phase of the volcanics that generally carries some fine, disseminated pyrite (1-350 shows rusty weathering on outcrops. The rock is massive, fine-medium grained, black to greenish black with fine, wispy intergranular plagioclase. It weathers dark green. In spots it grades into graywacke and hornblende biotite schist. It seems to be atuff made up of dust and ash-sized particles. Calcite probably filled the spaces between the ash particles to be replaced later by feldspar. Such rocks are most abundant in the E-16 zone (part of the Partridge Creek Shear Zone). This rock is associated with volcanogenic sediments which are interbedded and range from graywacke to feldspathic and quartz wackes.
Feldspar porphyry weathers pinkish gray and occurs as dikes up fifteen feet wide and strjjc.e. N 7QO *.
FeOMgOMnOGaoNa20K20Ti0 2P 20 2
-
7.990.23
10.622.090.201.59
0.20
w '
ff J w s Q
- v
d "ti'Q
-L-
-8-
EPUCTUPAI. GEOLOGY
The schistocity of both basalt and gabbro strike north to north- northeast. The Partridge Creek Shear Zone is apparently conformable with the schistocity in general j it coincides with the E-16 conductor axis. The zone is probably 400 feet wide.
There are several ponds along a small creek that flows west to east in a pronounced valley. Some of the stripping shown on Map 5 revealed three small quartz veins up to one inch wide which are parallel to this east-west presumed fault. A small fault is associated with one of these veinlets; it shows that the north side has moved east relative to the south side.
On the GS zone, which strikes N 150E, small drag folds are Z-shaped showing that the shearing movement pushed the west side northward relative to the east side.
ASSESSMENT WORK
Two short base lines were cut. The GS zone base line is shown on maps 2, 2a, and is 1200 feet long in the direction N 15 E. The base line 8+43 E is -' shown on map 5t is 330 feet long in the direction S 20'0E; it starts at 8+43 E on L-18-S.
Total line-cutting 1,530 ft. (446 m)The stripping . is listed on the following pages. Altogether,
the total stripping was:Stripping 3,194 sq feet (297 sq m)
The location of the stripping is shown on the accompanying maps.Some geochemistry was carried out at the GS zone. The nine maps
show the work done t stripping, geochem work, geological observations, and sampling. These will be discossed individually.
HARRY DOWHALUK
SUMMARY OF STRIPPING
-9-
ZONE MAP NO. DIMENSIONS LOCATION CLAIM NO.
V, J ' 1
J 1L- 15-S 1
D 1
GS 2b
GS -2b
GS 2b
GS 2b
GS 2b
GS 2b
GS 2b GS v. 2b
GS
GS
GS
GS
GS
D
DL-11
M
E-
E-
E-
E-
E-
E-
E-
E-
E-
-
2b
2b
2b
2b
2b
1
1
15-s l1
1
12 312 312 312 312 312 314 314 3
14 33
E- 6 3
2x4 3x12 2x22x3 2x4
2x3
2x2 2x2 2x3
2x2 2x32x3 2x1
5x8
2x32x122x22x22x4
2x3
2x22x32x3
2X 92x9
2x122x102x102x102x82x11
3x182x32x2
8 26
4
6 86 4 4 6 4 66 2
406
244686466
1818242020201622
5412
4
sq
sq
sq
sq sq
sq
sq
sq
sq
sq
sq
sq sq
sq
sq
sq
sq
sq
sq
sq
sq
sq
sq
sq
sqsqsq
sq
sq
sq
sq
sq
sq
sq
ft
ft
ft
ft ft
ft
ft
ft
ft
ft
ft
ft ft.
ft.
ft.
ft.
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
ft
25+50 s,L-15 S,
L-15 S , L- 15-S,
i&S B. L.
GS B. L.
GS S.L.
GS B. L.
GS B. L.
GS B. L.
GS GS
G.
GS
GS
GS
GSL-
11
"
M
(i
B. L, B. L.
S.BL.
B. L.
B. L.
B. L.
B. L.
15-s,,
Ir-6-S,
L-
L-L-
15-s15-s,15 s,
L15-S,Ir-
L-L-
L-
18-S,15-s,15-S,
15-s,L-21-S
L-6-S,
30 W. 1104445 22 W. 24 W
28 W
, 7+50 N 1104441
, 6+70 N , 5+00 N " , 5+40 N , 4+30 N , 1+50 N 11044450+50 N0+50 N0-N
.0+30 sf 1+40 S
, 2+12 S
. 22+40 S
28W
28W24W22W
24+50 W7+50 w.14+00 W14+20 W15+00 w15+00 w14+40 W9+50 W9+50 w10-W
14 W
i 11
it iMHn
1104445M
II
II
II
11044421104446
. "M
II
II
II
It
II
11
13 W 1104442
HARRY DOWHALUK
-10-
AZONE MAP NO. DIMENSIONS
0 E-6
; E-6E-6E-6
0 E-6E-6
Aw
Ae
Q----
--
E BndryA E Bndry
E-16E-16
E-16
E-16E-16E-16
E-16E-16
W E-16E-16E-16
LOg pile^P log pile
ti
ti
li
^^^B "
ii
3333339977777
777
664
44
444444445555555
3x6 18 sq ft2x6 12 sq ft2x6 12 sq ft2x6 12 sq ft2x2 4 sq ft3x12 36 sq ft2x4 8 sq ft2x2 4 sq ft2x2 4 sq ft2x3 6 sq ft19x10 190 sq ft8x6 48 sq ft
12x40 480 sq ft 2x3 24 sq ft2x6 12 sq ft2x8 16 sq ft
26x4 104 sq ft22x6 132 sq ft20x3 60 sq ft2x2 4 sq ft4x6 24 sq ft 3x8 24 sq ft 2x3 6 sq ft4x8 32 sq ft2x12 24 sq ft3x6 18 sq ft5x5 25 sq ft15x20 300 sq ft
5x6 30 sq ft3x10 30 sq ft
2x3 6 sq ft5x15 75 sq ft6x6 36 sq ft
4xl4 56 sq ft2x4 8 sq ft6x7 42 sq ft1x6 6 sq ft
LOCATION
L-6-s, 13 Wi. ti i Hii iiiiii H
L-15-N,23-W
L-17-N, 18-W
L-15-S, , 3-W
L-15-S , 3-WL-15-S , 3-wL-15-S , 2=50 W
L-15-S , 2+25 W L-15-# , 2-w
L-15-s, 1+50 wL-15-s 1+00 W
L-12-S, 25+50 EL-12-S, 25+75'E ;B. L. 4-W, 21+00 SL-21-S,6f60 W
L-21-S, 4+50 W L-21-S, 5-W
L-21-S, 1+80 W
L-21-S, 0+00
L-21-S, 1+30 E
B. L. 4W, 22+20 S
E. L. 4W, 23-SL- 24- S, 3-1- 20- W
L- 24- s, 2+15 W
B. I. 8+43 E, 0+60-Si,
,,
, 1+40 SII M
, 2-SM "'
Claim No.
1104442"" i' I"
1104437"
1104446H"
11044V-
H""
1.104444'"
1104446"
11
1104447 i11
1104446"
1104447"
itii -""H"
HARRY DOWHALUK
-11-
SOKE
Log Pile
MAP NO.
5 5. 5
DIMENSIONS
10x12
1x6
2x410x122x26x187x5
5 x3 6x2
12x205x26x10
12068
2204
108
3515
i 12240
1060
sqsqsqsqsqsqsqsq sqsqsqsq
ftftftftftftftftftftftft
LOCATIONBL. 8+43
" i
i8-E'
8-E,8-E,
8-E,
9- E
9+15 E,9+30 E,
CLAIM NO.E, 2-S i:
, 2+30 S
2+40 S
2+40 S
2+55 s2* ?0- S2+80- S2* 90- S
2* 70- S2+70- S2* 70- S2+70 S
L 044*1it"M
II
II
II
II
II
II
It
II
55
3tl94 sq ft s 29? sq meters
THE GS ZONE (THE GABBRO SCHIST ZONE)
A small outcrop at 19+50 W on L-15-S on claimll04445 was re- examined beause of its altered appearance.The rock is a gabbro schist which is sometimes called flaser gabbro. This is a cataclastic rock in which are preserved lenses of undeformed rock separated by streaks of finely crystalline, foliated material or aggregates of parallel scales (mica). Acentral zone carries thin lenses of quartz from paper thin up to four inches wide at the north end.
The GS Zone (See maps 2a, 2B) strikes N 15OE and dips 800 to the east.It is exposed in numerous outcrops for a distance of 400 feetj it is at least 26 feet wide. The zone could not be traced north of the access road. Neither the magnetometer nor the electro magnetic surveys showed any anomalies over this zone.
No significant values in gold were obtained in the samples takeni
Boulder w 3-in vein of qtz
5-in vein in gzbbro schist
l-in qtr in gb sch, grab
Sugary qtz vn in gb sch, grab
l-in qtz stringers, grab
#11495
#11489
jpll490
#11491
#11492
1+33 N
1-N
0+23 S
1+38 S
1+80 S
Nil oz/t Au/0.2 ft.-2 ppb Au/ 0.5 ft.
-2 ppb Au, -l ppb Pd
-0.01 oz/t Au
-0.01 oz/t Au
#11493 1+94 S Up to l-in qtz, grab -0.01 oz/t Au
HARRY DOWHALUK
-12-
One sample taken for palladium was negative. A geoscan (#G-1) showed:( at 0-N)
Zn 20 ppmCo
GrCuMnMoNi
6 ppm455768-212
PPbSbSnTiV
320 ppm6
25-10
820
110 Digested in aqua regia
Two pieces of float quartz were found on or rear the GS Zone in th? vicinity of the access road, gne piece at 3+50 N on the GS base line is in the ditch and was probably moved by road construction. This piece of glassy, white quartz measures 12"x7"x6". The other piece of float quartz was found about 200 feet to the southeast} it had rusty cracks and measured 9"x9"x?". The float quartz carried no values of significance, namelyi#11W Grab -0.01 oz/t Au In ditch
#11488 " - 2 ppb Au
The presence of this quartz float allows for speculation on the existence of a quartz vein near the GS Zone, perhaps in an east-west direction. To check this possibility, 28 humus samples for gold were taken on L-12-S starting at 10-W and ending at 18-W, and also on I-15-S from 21-W to 8-W.
The humus sampling (see Map #3) was quite negative. There is one value of 5 PP^ and four values of 3 ppb. If a quartz vein does exist in the area sampled, it probably does not carry any significant gold. .-''
In the sampling, the black, decomposed humus layer at the base of the A horizon was used which is about four inches below the surface. In the lab (Swastika Laboratories Ltd), the sample was macerated, ashed, screened through 80 mesh, then subjected to fire assay with atomic absorption finish.
An attempt to trace the zone northeasterly across the access road, over the higher ground and across the swampy area, E-l, E-6, F-8 on map #3. was unsuccessful. A search was also made to the south- west but no signs of the shear zone were found (Map #1).
HARRY DOWHALUK
-13-
'he E-12 SHEAF ZONE
This anomaly reflects a strong shear zone which consists of greenstone schisi/Unlike the GS Zone, this shear zone is well defined by; the VLP electromagnetic survey. The zone extends for some 2,100 feet(650m), strike N150E and dips about 80OE which is conformable to the formations.It contains two small magnetic anomalies, 'O' and 'K*.
It is well exposed in several outcrops just to the southwest of 13-W on L-15-S and 15-W on L-18-S. The zone also crosses the flat-lying gold-bearing quartz vein in the gravel pit and continues northeastward to L-6-S. The magnetic anomaly 'M'occurs in the zone.
The flat-lying four-inch-wide quartz vein (The Gravel Pit Vein), was discovered and sampled in 1989 by the writer; the sampling yielded the following results from grabs of the quartz rocki 0.674, 0.113, 0.024, 0.00?, 0.002, nil, and nil oz/t gold. This vein lies in the west side of the shear zone.It is possible that there could fee a^setctffssoeji veins. The 'M 1 magnetic anomaly is weak but it is associated with the E-12 conductor zone and the Gravel Pit Vein.
There is no significant mineraliztion apart from the vein. At 7-W on L-6-S, a few scattered grains of pyrite and arsenopyrite were noted. Du L-18-S si SO-iW-rS, a thin streak of spotted schist appears to contain small garnet porphyroblasts.
SOME MAGNETIC ANOMALIES :
On anomaly D at the west boundary on L-15-S (maps #1, 2B) ( pome sparse, disseminated pyrite and pyrrhotite were found. Onr grain of chalcopyrite was seen. Although of no consequence, it still shows more sulphides than is usual in most outcrops.
In the J anomaly (Map #1)located in the southwest corner of the property, much float basalt was present but no sulphides. Possibly some fine disseminated magnetite was present.
AW (map 9)on L-15-N on the east side of the road, reads 1,495 gammas. A large number of large gabbro boulders was noted at this location.
e (map 9) is on L-17-N and 18-W and reads 1,255 gammas. A hole was dug which contained clasts of of basalt, feldspar porphyry, and gabbro but nothing that was magnetic. The source of magnetic force was probably lower down.
HARRY DOWHALUK
-:4 -14-
CROSS ZONE (Map #7')
Some outcrops of volcanic flows were stripped here which is on the west side of of the E-16 zone. Apart from a half-inch quartz vein, no other quartz veins parallel to the east-west valley (on the south side) were turned up. Weathering pits are abundant in this area.
Similar volcanics were stripped on L-6-S and I-9-S between 13-E and 12-E.
EAST BOUNDARY ZONE (Map #6}The gabbro is coarse-grained and sheared (striking N 200E)
in the vicinity of26-E on L-12-S. The west outcrop is a dark gabbro and contains a three-inch syenite dike that parallels the schistocity but dips 850 to the west. The east outcrop is extremely dark-colouredwith very sparse plagioclase! it can be called a melanogabbro. The E-16 ZONE ( map #4 )
The E-16 Zone appears to be the most significant feature on the property. It appears to coincide with R.M. Easton's Partridge Creek Shear Zone. It crosses the entire property from south to north and is about 400 feet wide j it carries from l to 3^ dissem inated pyrite.
The tuff horizon, which is the main constituent of this zone, marks a change from volcanic flows to tuff falls which allowed for the development of volcanogenic sediments. Winnowing of the tuffaceous material continued through stages of wackes until quartz wacke was the end result. This natural panning action was effective enough to show up in a grab sample of quartz wacke to yield 60 ppb of gold at 4+50 W on L-24-S.
A generalized cross section from west to east would give some thing as follows:
Volcanic flows Basalt tuff 220 ft. Arkose 30 ft. Basalt tuff ?0 ft.Anorthositic
gabbro 30 ft.Quartz wacke 30 ft.Greenstone
schist 30 ft400 ft.
-15-
The E-16 area was sampled in many places mostly for gold and forpalladium. A grab sample of a one-inch quartz vein in basalt tuff gave:.
#1149? L-l8-S 2-W ? ppb gold
In the L-21-S section four geoscans were takem *
Co
GrCuMnMoNiP
PbTiWZnFe
#1149920+00-S4- W Vt
16 ppm
7242
220-2
20760
311,500-10
24
Z.0%
#1149620+60-S 3* 85- WVt
17 ppm1766120-2
3064018
930-1010
2.4#
#1149822+00-G4-W Vt
24 ppm100150
250-2
141,100
36660-10
243.4 fo
#8176122+60- S5-w
Qtz Vn
1 ppm3634852
17848
22-10
31.2 f.
*I.C.A.P. Plasma scan, Aqua-regia digestion.In the above first three tuff samples, titanium, phosphorous
and manganese are quite higfc; they seem to be associated with bas altic rocks. Copper may be slightly elevated. The other sample, (#81761) is from a one to three-inch vein striking east and dipping 15 to the south which occurs in a n arkose outcrop on the edge of the pond.The wider part of the vein is smoky to large extent with some material a very dark brown-black. A peculiar 'chatoyant 1 luster is associated with the smoky quartz and brilliant blue and golden yellow reflectios could be seen with the aid of a strong hand lens. Oddly enough, the reflections disappeared after the quartz was kept indoors for some three weeks; the brilliant yellow colour fading to a dull grayish tan.The geoscan did not show any anomalous copper to account for the blue and yellow reflections. A grab sample from the quartz vein showed: (81761)
Au 17 ppb Ctt 47 ppm
-16-
A grab sample from the arkose outcrop containing the small rflat-lying vein (# 8l?62) showed i
Au 17 ppb Cu 28 ppm
Some sampling was done on the basalt tuffwhich carries fine, disseminated( l to 3 #) pyrite. See Map 4. Grab samples.
20-S, 4-W#81759
#11499
##11496
#8175?
20-S, 4-W
20+90 S, 4-W
21+65 S, 3+20 W
Aut Nil
Pd: -5 ppb
Au: Nil Pd: -5 ppb
Au: nil Pdt -5 ppb Au: 4 ppb Pd: -l ppb Pt: -l ppb Au: Nil Pd: -5 ppb Pt: -l ppb
Au: -2 ppb Pd: -l ppb Pt: -l ppb
Also, in the anorthositic gabbro: #8l?60 21+70 S, 4-W Au: Nil
Pd: -5
#81756 22+05 S, 3+85 W
-#81758 22-S, 4+33-W
and in quartz wacke:
#81763 24- S, 4+50- W Au: 60 ppb
CONCLUSIONS AND PECOMMENDATIONS
Work to date suggests that there are two main types of mineraliz- ationof. .interest in the area - quartz veins with gold, pyrite, arseno pyrite, and sphalerite (the O 'Bonnell vein in southeast Anglesea and the Gravel Pit vein on the property) and disseminated sulphide zones such as occurs on the E-16 zone which has potential for gold and base metals.
There is an east- west valley which may be a 'break' for the emplace ment of veins along, or off, this structure.
The E- 16 zone is a very large structure some 400 feet wide and most of it is under ponds, swamps and overburden} there is a variety of rock types and phases. This zone needs to be checked with diamond
HARRY DOWHALUK
-17-
.drilling.At this stage, some diamond drilling is recommended mostly on the
E-16 Zone. The following holes are recommended for an initial 1,000 feet. ( 305 mh
South end of E-16 zone
E-16 Zone and E-W valley
E-16 Zone, north of access road
Collar at 5-W on L-;DDH #1, -450 , S?0'0W, 61 m.
DDH 2, -450 ., N?00S, 61 m. Collar at 2-W, L-18-S
DDH 3 -450 , ,N 450W 46 m. Collar at 5-N, 8+50 E:
DDH 4 -450 , DDH 5 -450 ,
Collar at 10-W, 1?-NDDH 6, -450 , S ?00W 45 m.
N'?00E
S ?00W46 m 46 m
E-l2 shear zone, Gravel PitVein
At the Gravel Pit Vein, there are quartz pieces lying around in the south and west walls of the pit; There could b* another vein nearby. Some digging with a backhoe is needed .to have a look at this'material.
Ideally, this work should be done in the early spring. Such a program would cost j
Diamond drilling, 1,000 ft @ $l8/ft(305 m @
Backhoe stripping, 12 hrsHelper, l day
Transportation, 2,100 km @0.30 Personnel, geologist: 20 days @ Assaying
Miscellaneous Contingency 10 . f*
$18,000
840150630
6-, 000 3,000
500 2.880
^32,000
Respectfully submitted,
Harry Dowhaluk, B.A., F.G.A,C.
December 20, 1991
HARRY DOWHALUK
-18-
REFERENCES
Condie. K.C.,Moore,J.M., 'Geochemistry of Proterozoic Volcanic Rocks from the Grenville province, Eastern Ontario 1 in Baragar, M.R,A., Coleman,L.C., Hall,J.M., Volcanic Regimes in Canada. Geological Assoc of Canada, Spec Paper #16,1977.
Dowhaluk, H.,'The Killer Creek Project 1 Anglesea Twsp, I&A Co.,Ontario. OPAP, Jan.15, 1990.
Dowhaluk,H., 'Report on Killer Creek Claims. Geologic, VLF-EM,and Magnetometer Surveys, Anglesea Twsp, L&A C6.,~Ontario.v*-: Nov. 23, 1990.OPAP.
Easton,R.M., 'Geology of the Mazinaw Lake Area (31 C/14 1 , OGS, Open File Map 132, Scale 1150,000.
Hewitt, D.?;; Geological Notes for Maps ftos2053 and 2054. 'Madoc-Gananoque Areat Geol. Circular 12. ODM. 1964.
Hopkins, Percy E., Ontario Gold Deposits, Vol XXX, Part 2, ODM, 1921.
Johnson, Wayne, 'Magnetic and VLF-EM surveys, Killer Group, Anglesea Twsp, Southern Ontario Mining Division, for United Reef Petroleums LtdJ Resident Geologists Files, Tweed, May 1987.
Lumbers, S.B,, "Preliminary Report on the Relationship of Mineral Deposits, to Intrusive Rocks and Metamorphism in part of the Grenville Province of Southeastern Ontario 1 ,P.r. 1964-4, ODM.
Meen, V.B., Geology of the Grimsthorpe-Barrie Area.Vol II, Part IV, 19^2, ODM.
Moore, T.M., Morton R.L., Marble Lake Area.Report 238, OGS, 1986
HARRY DOWHALUK
-19-
CERTIFICATE
I, Harry Dowhaluk, of the village of Tamworth in the county of Lennox and Addington, do hereby declare j(1) That I am a consulting geologist and reside in the village
of Tamworth, Ontario.(2) That I am a graduate of the University of Western Ontario
with a degree of B.A. (15165)* I have been engaged in geol- logical and related engineering work (mine surveying, diamond drill supervion, geophysical work) for some 39 years
which includes 9 years underground, 5 years of Cordilleran geology, and 5 years -outside of Canada in^.the USA and Mexico. I have t"2en"a fellow of the Geological Association
. of Canada since 1970.(3) That I have a 100?5 interest in the property described in
this report.That I aasre personally carried out all of the work described in this report.
Harry Dowhaluk, B.A., F.G.A.C. December 20, 1991
HARRY DOWHALUK
No u r*
3/v OZ Z l -
-Vt i
l O 444 A
t P 30 10 f t-
/t* m.
ltt*io t
ScAt/a.-
.H-
Cd.
P j //o
8 'W 4WKI
i bil '-fa/* :
'r-9
**H'l A 1, *#* ^A v n
-o t? .
Established 1928
Swastika LaboratoriesA Division of Assayers Corporation Ltd.
Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company:Project:Ann:
H. DOWHALUK
1W-3163-SG1
Date: JUN-26-91 Copy l. P.O.BOX 118JAMWORTH, ONT. KOK 300
We hereby certify the following Geochemical Analysis of 28 HUMUS samples submitted JUN-19-91 by H. DOWHALUK. DECEIVED JOL 3 1991SampleNumberH-30H-31H- 32H-33 H- 34H- 35H- 36H-37H-38H-39H-40H-41H- 42H-43H-44H-45H-46H-47H-48H-49
H- 50H-51H- 52 H-53H-54H-55H-56H-57
AuppbNil 'Nil
5Nil NilNil
3NilNil 1Nil 1
Nil\Nil \Nil 1NilNilNil JNil 7Nil v
3 yNilNilNil NilNilNilNilNil J
\ lb~VJ
1 -T
)5~-uJj /bv
{7-iJTo )j
!i
t 9 \Af *^^~ ^** * 9 r
f fn " Is^r
' " 7 IT- Wi ^ *^r
'3-w
Jl " lv1 w^ K/
Certified by.
P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244, FAX (705)642-3300
H. DOWHALUK
1V-3165-R01
SWASTIKA LABORATORIESP.O. BOX 10, SWASTIKA, ONTARIO
PHONE *: (705) - 642 - 3244 FAX *l (705) - 642 - 3300
I.C.A.P. PLASMA SCANAqua-Ragia Digestion
REPORT MO. : M922Z
Page Ho. : l of lFile No. : JN26MAData : Jim-26-1991
SAMPLE #
0-1
Al
pp*B ,B|
PP"Vl; PPi
Be li*!!
ppmfeppn
ea nidi co mm cu ipcf K pig* Eppi ppnffli'pl pp"il;*lf * iUM
Mn N.
l i.l;:':;:i;*:: : : : 5 < lQMi.8?
A .5 gn s t 95 CThi* neth
T8L/91
e i* digested with 2 ml of 3:1 HCL/HN03"i" ""d diluted to 10 ml with DI H2O
i partial for many oxide material*
ppnp|[| * ||:PP| PIISlSjBj IsSISf
i pp*tii
RECEIVED JUL * ttdl.,BIONED l
in zn
H. DOWHAUK
1W-3164-R01
SWASTIKA LABORATORIESP.O. BOX 10, SWASTIKA, ONTARIO
PHONE *: (705) - 642 - 3244 FAX fi (705) - 642 - 3300
I.C.A.P. WHOLE ROCK ANALYSISLithium MetaBorate Fusion
REPORT Mo. t M9223Page No. : l of l
File No. : JL02RA
Date : JUL-02-1991
SAMPLE Al203tl|F.!lii
WRA-1
WRA-2
1141168vai".!;.X. . ' ""/;.'1;.: ".W;
Cao|||fi|||l P205
illlHl * ISJtlMlCIi
2.09|||||
T8L/91
SIGNED t
HARRY DOWHALUKSWASTIKA LABORATORIES
P.O. BOX 10. SWASTIKA. ONTARIO
PHONE #: (705) - 642 - 3244 FAX #: (705) - 642 - 3300
I.C.A.P. PLASMA SCANAqua-Regia Digestion
REPORT Ho. : M9452
Page No. i l of l
File No. l AU07MA
Date l AUO-08-1991
SAMPLE t;vXX;r~Xv^v;
Al |i:A|3 B If 18 Be Hill Ca Mill Co BSa Cu Sill K till! Mn
11496
A .5 ym *J^ke i f digeEted with 2 ml of 3:1 HCL/HNO3 at 95 C f^VJ "In and diluted to 10 ml with DI H20 Thia nethoois partial for many oxide materials
T8L/91
In
10J
RECEIVED AUG 2 O 1323SION
ft S
H. DOWHALUK
1W-3856-R01
SWASTIKA LABORATORIESP.O. BOX 10, SWASTIKA. ONTARIO
PHONE #1 (70S) - 642 - 3244 FAX *l (705) - 642 - 3300
I.C.A.P. PLASMA SCANAqua-Reji* Digeatlon
REPORT HO. : M9715
Page No. : l of l
File No. : SB11HZ
Date : SEP-13-1991
RECEIVED SEP 2 6
SAMPLE
11498
11499 < < lo
A .5 gm aai^^ is digested with 2 ml of 3:1 HCL/HN03 •t 95 C 'o^B "I" a"** diluted to 10 ml with DI H20 Thl* •ethod^R partial for many oxide materials
TSL/91
H. DOWKALUK CO,
1W-3909-R01
SWASTIKA LABORATORIESP.O. BOX 10, SWASTIKA, ONTARIO
PHONE #: (70S) - 642 - 3244 FAX #1 (705) - 642 - 3300
I.C.A.P. PLASMA SCANAqua-Regla Digestion
REPORT MO. : M9794Pag* No. i l of l
Fil* No. l 8E20MA
Date-, ,.- ae
RECEIVED OCTl SEP-23-1991
k 1990
SAMPLE #
61761
pi PP-BPI* * mm*:;^^^ K**m*tz pl'M*^
A .5 ga a at 95 C This ne
i laiuaW
ithod^R
la digested with 2 nl of 3:1 HCL/HNO3 Bin and diluted to 10 nl with DI H2O partial for many oxide materials
TfiL/91
S"
pparfiipl ppipiii M Wfa.vteq jifpps-s?
< skin < lOBlll
SIGNED :
Swastika LaboratoriesA Division of Assayers Corporation Ltd.
Assaying-Consulting-Representation Biucn SEP 1 ^
Geochemical Analysis Certificate 1W-3909-RG1Company: H. DOWHALUK Date: SEP-16-91 Project: Copy l. P.O.BOX 118, TAMWORTH, ONT. KOR 300 Ann:
We hereby certify the following Geochemical Analysis of 6 ROCK samples submitted SEP-09-91 by H. DOWHALUK^
vyv. ^"jL. .
Sample Au At'check' Cu Pd ICP MULT Number ppb i ppb ppm ppb8175^""'^!!""""""*"" ^5
81760 Nil - *? ^81761 17 v ,^ 4781762 17 ' 2881763 65 5581764"""""""""""""^!!"""""""""""""""""^"
Certified by i J C\\ ^/u CT^A^w
P.O. Box 10, Swastika, Ontario POK1TO Telephone (705)642-3244, FAX (705)642-3300
Swastika LaboratoriesA Division of Assayers Corporation Ltd.
Established 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate 1W-3856-RG1
Company: H. DOWHALUK Date: SEP-04-91 Project: Copy 1. P.O.BOX 118, TAMWORTH, ONT. KOK 300 Ann:
We hereby certify the following Geochemical Analysis of 3 ROCK samples submitted SEP-03-91 by H. DOWHALUK.
Sanple Au Pd ICP MJLT Nurrfoer ppb ppb ppmn497~" """"""" 7 '"""" ""
11498 Nil K311499 Nil ^
Certified by
P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244, FAX (705)642-3300
\Ministry of Ontario Geological Survey i iinriow
iern Development Geoscience Laboratories Toronto. Ontario aim Mines
0""ctono. 0128-0218-91
OntarioM7A 1W4T*t*phoo* 1-419-895-1337
Mr. H Dowhaluk P.O Box 118 Tamworth ONT KOK 3GO
ni 0''^ r/ 1 o—." r- 1 c lo:;,-. CLO z L
02:10— -at'
Sample
#81756 #81757 #81758
Au (Ppb)
<2 4
<2
Pd (PPb)
^ <l <l
Pt (ppb)
<l <l <l
This completes the analytical work for samples entered in your name on Sep 09,1991.
Please refer to certificate 0218-91 if you have any questions.Fees Received: Coupo,
Peter C. Lightfoot Acting Chief
91/10/03
Swastika LaboratoriesA Division of Assayers Corporation Ltd.
Established 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate 1W-3527-RG1
Company: HARRY DOWHALUK Date: JUL-31-91 Project: Copy 1. BOX 118, TAMWORTH, ONT KOK3QO Ann:
We hereby certify the following Geochemical Analysis of 2 ROCK samplessubmittedJUL-25-91 by. ftpfc&VED AU0 O B 122i
Sample Au TCP Number ppb Mil t i 11495"" - -----------------^ --"--~-~~--~-"-"-~-"-'-"-~------~-~-~-~-~-
11496 Nil
Certified by_
P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244. FAX (705)642-3300
Ministry of Ontario Geological Survey l linri(X NMiern Development Geoscience Laboratories Toronto, amrMines
ajowtonoe 0128-0114-91Laboratories p .Report F9*l
OntarioTttophon*: 1 -416-988-1337
Mr. H DowhalukP.O Box 118TamworthONT KOK 3GO
G LOGS G LO'" p G S
Sample Au (oz/ton)
11491114921149311494
<0.01 <0.01
This completes the analytical work for samples entered in your name on Jun 21,1991.
Please refer to certificate 0114-91 if you have any questions.
Peter C. Lightfoo Acting Chief
Fees Received: Coupon
91/07/05
Except by ipecla! permission, reproduction of then results must Include any qualifying remarks made by this ministry wtth reference to any sample.
Mjatetryof Ontario Geological Survey Nflparn Development Geoscience Laboratories Tocomo.onurtoanoMlnes
OntarioM7A1W4T*tephonc 1 - 416 - 866.1337
Laboratories Report
0128-0103-91
Mr. H Dowhaluk P.O Box 118 Tamworth ONT KOR 3GO
GLOGS GLOGS GLOGS GLOGSG LOGS c,LOGS CLOGS G LOGSG LUGS O l O3erK*P H.OGSG LOGS GlOGS (HOGS G LOGS G.OGS GLOGS GLCGS GLOGS
RECEIVEDY
Sample Au (PPb)
Pd (PPb)
RECEIVED JlIH 1 ^iijft114881148911490
<2 ^ <2 <l
This completes the analytical work for samples entered in your name on May 27,1991.
Please refer to certificate 0103-91 if you have any questions. Fees Received: Coupons
Lightfoot Adting Chief
91/06/10
XVIII
XVII
33 32 31Grimsthorpe \
LokS
30 29 28 27 26 25 24 23 22 211
XVI
XV
XIV h
xii L--
XIr- en
XIII (so" ~ M " (so
x
ntario3ici4sweeei 8.14493 ANGLESEA 900
Ministry ofNorthern Developmentand Mines
Ministeredu Mining Lands Branch Developpement du Nord Geosciene Approvals Sectionet des Mines 1 59 Cedar Street
4th Floor SUDBURY,Ontario P3E 6A5
Toll Free: Telephone: Fax:
1-800-465-3880 (705) 670-7264 (705) 670-7262
Mining RecorderMinistry of Northern Development Our File: 2.14493and Mines Your File: W9290. 0000710 Wellesley Street East1st FloorToronto, OntarioM4Y 1G2
March 19, 1992
Dear Sir:
SUBJECT: APPROVAL OF ASSESSMENT WORK SUBMITTED ON MINING CLAIMS SO 1104437 ET AL. , ANGLESEA TWP.,
The assessment work credit for Report of Work W9290-00007 has been approved as of March 18, 1992. The distribution of "Assessment Work Done" has been reorganized on the enclosed amended Assessment Work Credit Form. This reflects the work claimed having been restricted exclusively to claim SO 1104446, as indicated on the detailed plans submitted with the Report of Work.
Please indicate this approval on your records.
Yours sincerely,
Ron C. GashinskiSenior Manager, Mining Lands BranchMines and Minerals Division
DT/jl Enclosures:
cc: .....Assessment Files Office Toronto, Ontario
Resident Geologist Tweed, Ontario
ASSESSMENT WORK CREDIT FORM
FILE NO. : 2. 14493
WORK REPORT NO. : W9290. 00007
DATE: MARCH 19, 1992
RECORDED HOLDER: Harry Dowhaluk
CLIENT No. : 126944
TOWNSHIP/AREA: Anglesea Township
CLAIM No.
VALUE OF ASSESSMENTWORK DONE
DONE ON THIS CLAIM
SOsososososososososososo
110443711044381104439110444011044411104442110444311044441104445110444611044471104448
0.0.0.0.0.0.0.0.0.
609.0.0.
000000000000000000370000
VALUE APPLIED TO THIS CLAIM
50. 7850. 7850. 7850. 7850. 7850. 7850. 7850. 7850. 7850. 7850. 7850. 78
VALUE ASSIGNED FROM THIS CLAIM
0. 000. 000. 000. 000. 000. 000. 000. 000. 00
558. 590.000. 00
12 claims 6609. 37 S609. 37 6558. 59
CREDITS RESERVED
0.000. 000. 000. 000. 000. 000. 000. 000. 000. 000. 000.00
0. 00
Noniiorn Development and Mines
Ontario
Personal Infor Ihle collection e Sudbury, Ontario,
OJ tVUl U CondUCled l linsaction Number
After Recording ClaimMining Act
collecled on this form Is oblalned under the authority of the Mining Act. This Information will be used lor correspondence. Questions about ' be directed to the Provincial Manager, Mining Lands. Ministry of Northern Development and Mines. Fourth Floor, 159 Cedar Street,
P3E 6A5, telephone (705) 670-7264.
MiningInstructions: - Please type or print and submit In duplicate. ^-. '
- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining 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.
Recorded Holders)
Address
Mining Division
Dates Performed
Township/AreaOAJ T- K o 13
• c- S
Client No.
Telephone No,4/3-377-
M or a Plan No. 'W-
From: To:
Work Performed (Check One Work Group Only)
V
Work C ip
Oeotec' i Survey
Physics k, Include . ling
Rehabilitation
Other Authorized Work
Assays
Assignment from Reserve
R j- c*. F- i \ d^n——————————————— MAR 1 Q 190? ————————————————————
MINING LANDS BRANCH
*^ **t- i \ t*. , /*t4.vvft^c Att , d*, (p.C0fG*l*\5 vJ^**/* tfoc (f
7
Total Assf' )nt Work Claimed on the Attached Statement of CostsNote: The M,nister 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.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address
nl*.
(attach s schedule If necessary)
Certification of Beneficial Interest ' See Note No. 1 on reverse sideRecorded Holder or Agent (Signature)
l 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 by the current recorded holder. ^^^^
Date
j) f C. 2
Certification of Work Reportl certify itir. ea personal knowledge ol the facts set forth In this Work report, having performed the work or witnessed same during and/or after Its completion 6"d annexed report Is true. ^^^
Name and Address ol Person Certifying
o w HCertified By (Signature)
For Office Use OnlyTotal Value Cr. Recorded Dole Recorded
RECEIVEDOoemod Apptov Dele
JAN 2 '5 1 992Dolil Notice lor Amendments Sent
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D C
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In th
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Exam
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No/them Development Mines
Ontario
ht'puu ut tivuiK Conducted After Recording Claim
Mining Act
transaction Number
. ooooS
Personal InfqAflon collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this coilectloPPtould be directed lo the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 160 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264. " "*
Instructions: - Please type or print and submit In duplicate,- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining
Recorder.- A separate copy of this form must be completed for each Work Group.
7 ' Technical reports and maps must accompany this form In duplicate, y - A sketch, showing the claims the work Is assigned to, must accompany this form.
Recorded Holders)
Address
Client No.
BMining Division
T 4 AiTelephone No.
"Bates Work •Performed
Township/ Area M or d Plan No.
From: t\ /t To:Work Performed (Check One Work Group Only)
y
^
Work Group
Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other AuthorizedWork
Assays
Assignment from Reserve
Type
fAf^ro^RL ^TR.\P? M^GI| riW?uoO. ( SrtmpcnJQ.
AA Jjj/, 1 A i ,- T fl j 0 0 1 X /* f - t .A A n f* A A if1 ' ' ' ' I'T'llvVf — - , . , ~- .
Total Assessment Work Claimed on the Attached Statement of CostsNote: 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.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name
///Q A 4-7 J)^rt A^ o^
'
Address
73
(attach a schedule If necessary)
^X i i^ -f /l /-i o) t) A. TH , o xJ T' /C&K3 ^oOWAKIUGEOtoGICATsURVEY
GIS- ASSESSMENT FILES
MAR 1 0 iqq?
REChlVEDCertification of Beneficial Interest * See Note No. 1 on reverse side
Recorded Holder or Agent (Signature)l certify that at the lime the work was performed, (he claims covered in this work report were recorded In the current holder's name or held under a beneficial Interest by the current recorded holder. ^^^
Date
Certification of Work Reportl certify that l have a personal knowledge ol the facts set forth In this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report Is true. ____________ ___________-________
Name and Address o! Person CertifyingK -
Telepone No. Date Certllled By (Signature)
For Office Use OnlyTotal Value Cr. Recorded Dale Recorded Ree 'WBW&rtffONTARIO MINING DIVISION
RECEIVED
Dile Notice (or Amendments SentJAN 2 3 1992
AM
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1
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IV. DAILY REPORTS (Summarize work activity in Section I)
Day Project Area x ,\ Date K.LUE* CA&t ?f-*JM& C*
1234567891011121314151617181920212223242526272829303132333435363738394041
TT- f
/
Work Performed
.cro 56- tfO
.oro
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Attach additional sheets as required.
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Effingham Twp.(M.87)
33 32 31 30 29 28 27 26 25 24 23 22 21 20 l 9 l 8 ;; 17 ' 6 5 14 13 12 10
Abinger Twp. (M.4I)
XVIIIGrimsthorpe
Lake
•~ V-'"- l 0^ I I
Skootamatto(Loon Lake)
!OOAc. lOO Ac. l 11-
O 109(762 IO9I759 1091750 109(75809176! M***
1091760 109(757 1091756 IOOAe
Deerock
33 32 '31 30 '29^*^27 2628
Elzevir Twp.(M.89)
25 24 23 22 21 20 19 18' 17 16 15 14 13rf
Kaladar Twp.(M.108)
r
THE TOWNSHIP^wr r— -* yfl ACTi P "l o- *-r^^f i i B ^Tt -m- O^Bf w E ""^^^9 -J*-
ANGLESEACOUNTY OF
LENNOX aADDINGTON
SOUTHERN ONTARIOMINING DIVISION
SCALE'l-INCH-40 CHAINS
DISPOSITION OF CROWN LANDS
PATENT, SURFACE AND MINING RIGHTS ,.__ 0 " , SORFACt RIGHTS ONLY..,.____. ® " , MINING RIGHTS ONLY ________. O
LEASE, SURFACE AND MINING RIGHTS___ B " , SURFACE RIGHTS ONLY__...,__. H " , MINING RIGHTS ONLY ________ B
LICENCE OF OCCUPATION_____________ YROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYS
POWER ^INESMARSH OR MUSKEGMINES X*CANCELLED C.
TRAILS ,~-
JMPJES. This Map Is Not To Be UsedFOR SURVEY PURPOSES.
Lo! And Concession Lines Shown Heieon Are Projected From The Best Informations Available, Hut Their True Position Is Not Guaranteed. For Official Survey Purposes Consult The Original Survey P'ans And Field Notes Of Records In The Ministry of N atural R esources.
400 surface rights reservation along Ihe shores of ali loke^ and rivers
®
SAND and G RAVEL
Gravel , Filt. 140242
MNR Gravel Reserve No. 202 Gravel File 3534
150905
Quarry Permit
RESERVES
(J) Reserved l or Public use , File I449OO
DATE O F ISSUE
FIB l ?, 1992
SOUTHERN ONTARIO DIVISION
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN CO.MPILED 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 WENT AND MINES. FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON
PLAN NO.-M.43ONTARIO
MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH
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^ E-l 6 ZOIUEANGLFS-A TOWNSHIP
LENNOX ADDINGTON .COUNTY ONTARIO
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