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52Fe3NE8«17 2 .6246 NAPANEE LAKE 010
GEOLOGY OF THEMANITOU STRAITS PROPERTY
DISTRICT OF KENORA
for
Silver Lake Resources Inc.Suite 4650, P.O. Box 77, TD Bank Tower
Toronto Dominion CentreToronto, Ontario
M5K 1E7
February, 1985
RECEIVED'
JUN 2y 1985
MINING I AMDS SECTION
Harris Lake Area District of Kenora NTS: 52F/3 LORNE BURDEN
SUMMARY
The 161 claim Manitou Straits property is located on the southwestern end of
Lower Manitou Lake. The property is underlain by an Early Precambrian southwesterly trending sequence of metamorphosed mafic to felsic volcanic rocks intruded by mafic sills.
The property is on strike with four gold prospects. The Gaffney deposit, four miles northeast of, and on strike with the Manitou Straits property, has recently undergone an intensive drill programme by a Teck Corporation - Noxe Petroleum Corporation joint venture. Estimates of possible gold reserves prior to recent drilling were as high as 621,000 tons of material grading 0.22 oz gold per ton (Neilson and Bray, 1981).
The Gold Standard North, Sairy Gamp, and Gold Standard South prospects are four, four and one-half, and five miles respectively to the southwest of the property. Each of these prospects were worked near the turn of the century and developed with exploration shafts.
In early 1984, a 400' line grid was established on the property and magnetometer and V.L.F.E.M. surveys were conducted. Several magnetic and V.L.F.E.M. anomalies were outlined. Many of the magnetic anomalies are similar in intensity to the anomaly over the Gaffney gold deposit.
Geological mapping was carried out in conjunction with the geophysical surveys. Several geologically and geophysically promising areas have been identified. Detailed prospecting of these selected areas is recommended for the 1985 field season.
Table of Contents
SUMMARY
INTRODUCTIONLocation and AccessPropertyTopography and Vegetation
EXPLORATION HISTORY AND PREVIOUS WORK
CURRENT EXPLORATION
GEOLOGY
Regional Geology Property Geology Stratigraphy and Lithology Economic Geology
CONCLUSIONS AND RECOMMENDATIONS
COST ESTIMATE
REFERENCES
PERSONAL DECLARATION
52Fe3NEe«17 2.6246 NAPANEE LAKE
Figure 1 Figure 2 Figure 3 Table 1
List of Figures and Tables
LOCATION MAP CLAIM MAPREGIONAL GEOLOGY MAP ROCK SAMPLES
010C
Page
i
I 37
8
10
11
II131415
20
21
22
23
26
1215
Plan 1Plan 2Plan 3Plan 4
List of Plans {map pouch)
Geology Geology Geology Geology
Sheet 1 Sheet 2 Sheet 3 Sheet 4
INTRODUCTION
The Manitou Straits property is underlain by Early Precambrian metavolcanic
rocks and actually straddles a major transition in the volcanic rock chemistry
from tholeiitic to mixed calc alkaline and tholeiitic. This boundary between
oceanic volcanics and an overlying stratovolcano is typically the locus of many
Early Precambrian gold deposits. In the Manitou Lakes area, the Gaffney deposit
occurs at such a contact and numerous other gold occurrences are found in close
proximity to this horizon (Burton & Hodge, 1984).
Magnetic, V.L.F.E.M., and geological surveys were conducted during the 1984
field season. The geophysical surveys were performed in an attempt to outline
zones of geological interest and mineralization. The results of the geological
survey is presented in this report.
Locations and Access
The property is located near the southern end of Lower Manitou Lake
approximately 40 miles south of Dryden, and 40 miles north of Fort Frances,
Ontario (Figure 1). Highway 812 passes approximately 5 miles east of the
property.
Access may be obtained by float or ski equipped aircraft available in both
Dryden and Fort Frances. Boat or snowmobile may also be used to reach the
property from Esox Lake located 20 miles to the south and accessable by logging
roads from Hwy. 812.
Several radio telephones are available at tourist camps and private cabins
around the lake. A barge service is available on the lake for transportation of
heavy equipment, and a seasonal helicopter base is maintained at camp Beaverhead
8 miles northeast of the claim group.
2.
Manitou Straits
Silver Lake Resources Inc. Manitou Straits Property
LOCATION MAPDistrict of Kcnora, Ontario
Figure 1
Property
The 6440 acre, Manitou Straits property was staked for Silver Lake Resources
Inc. during the winter of 1983-1984. The property comprises 161 contiguous
unpatented mining claims which are identified as follows, and illustrated in
Figure 2.
M2469, Napanee Lake Area. District of Kenora
K
Claims
729890729891729892744448744449744450744451744452744453744454744455744456744457744458744459744460744461744462744463744464744465744466744467744468744469744470744471744472744473
Recorded
November 29, 1983
Claims
744474744475744476744477744478744479744480744481744482744483744484744485744486744487744488744489744490744491744492744493744494744495744496744497744498744499744500744501744502744503
Recorded
November 29, 1983
MINING CLAIMS TRAVERSED (cont'd)
K
NUMBER
744504744505744506744507744508744509744516744517744518744519744520744521744530744531744532744533744534744535744544744545744546744547744553744554744555744556744964744965744966744967744968744969744970744971744972744973744974744975744976744977744978744979
Recorded
November 29, 1983
November 29, 1983 February 8, 1984
NUMBER
744980744981744982744983744984744985744986744987744988744989744990744991744992744993744994744995744996744997744998744999745000745001745002745003745004745005745006745007745008745009745010745011745012745013745014745015745016745017745018745019745020745021
Recorded
February 8, 1984
5.
MINING CLAIMS TRAVERSED (cont'd)
NUMBER
745022745023745024745025745026745027745028745029745030745031745032745033745034745035745036745037745038745039
Recorded
February 8, 1984
SILVER LAKE RESOURCES
—-4- —-f—'««&)• I M4W7 IAM
J'**— s-t.. -..,
»«»»!
4-——}- —— .».——t- —KIH43I* J«4Set |/*»6i» .-H4SII
v * f**-i<r* | r^-rs~) ^%«4»
r^.BL^CKI_§ '"« -..—4—
TAKEN FROM M N.R. MAP
MANITOU 8TRAIT8 PROJ
CLAIM MAP !'.
7.
)_ography and Vegetation
Approximately 30 percent of the property is covered by water. The remainder of the property is covered by undulating hills with maximum relief of 70 feet.
Vegetation consists of mature spruce, pine and balsam, with alders and manitoba maple present as undergrowth. Locally, mature cedar swamps can be found in depressed areas.
8.
EXPLORATION HISTORY AND PREVIOUS WORK
The first comprehensive geological mapping of the area was carried out by Thomson (1934) covering both the Upper and Lower Manitou Lakes areas as well as the Manitou Stretch area. More recently, Blackburn (1976, 1982), mapped the Upper and Lower Manitou Lakes area in detail to the north of the Manitou Straits property.
The Manitou Lakes area was the scene of considerable gold prospecting and mining activity from 1895 to 1912, and again in the 1930's (Thomson, 1934). This activity resulted in the discovery of twenty gold occurences in the area. These occurences have been described in detail by Burton and Hodge (1984).
During the 1950's and 1960's, some base metal and iron exploration was carried out in the area. With the discovery of the Mattabi Mine on Sturgeon Lake, approximately 100 miles northeast of the property, exploration in the region was intensified.
Airborne geophysical surveys for base metals were carried out in 1970 by Freeport Canadian Exploration Co. on Lower Manitou Lake to the north of the
Manitou Straits property.
The Canadian Nickel Company held several small claim groups around and included within the bounds of the Manitou Straits property between 1969 to 1972. Three separate locations were tested on the property by diamond drilling. Diamond drill logs, available from the Ministry of Natural Resources, Assessment Office in Toronto, indicate that one drill hole located at the northwest tip of Syndicate Lake intersected mafic volcanics and gabbro with disseminated pyrrhotite and pyrite. A second drill hole southwest of Syndicate Lake intersected fel sic and mafic volcanics containing minor sulphides and carbonate alteration. The third drill hole located immediately south of Calder Lake intersected mafic volcanics and gabbro, also intersected was a zone of 25% disseminated pyrite associated with quartz veining and magnetite. No assay values were published, and gold analyses were probably not performed.
9.
The Gaffney gold deposit, located four miles northwest of the property, was discovered in 1927, and to 1944 was tested by 42 diamond drill holes (Trusler, 1984). The property, dormant since 1944, was acquired in July 1983 by Noxe Petroleum Corporation and Teck Corporation in an 86 claim package. The gold mineralization is associated with pyritic alteration halos surrounding a stockwork of quartz veins at the base of a mafic sill. The mafic sill, rich in magnetite, forms both a strong airborne and ground anomaly. Discussions with the Teck geologist involved with the Gaffney deposit revealed that the magnetic anomaly correlates well with the zone of mineralization.
The Gold Standard North, Sairy Gamp, and Gold Standard South gold prospects occur four, four and one-half, and five miles respectively to the southwest of the Manitou Straits property along the regional geological trend.
10.
CURRENT EXPLORATION
In early 1984, a line grid was established on the Manitou Straits property. A total of 15.91 miles of base and tie lines were cut; perpendicular to this, 95.72 miles of picket lines were cut at 400 foot intervals with pickets every 100
feet.
Magnetometer and V.L.F.E.M. surveys over water covered portions of the property were conducted between February 28 and March 14, 1984 by Norontex Explorations Ltd. of Dryden, Ontario^ Instrument readings were taken at 100 foot intervals on all picket lines.
During the summer of 1984, magnetometer and V.L.F.E.M. surveys were conducted over the remainder of the property by Silver Lake Resources Inc. Instrument readings were taken at 50 foot intervals on all picket lines. In areas with anomalous magnetic values, readings were taken at 25 foot intervals. The above mentioned work was previously summarized in a report by Burden (1985).
In conjunction with the geophysical surveys, geological mapping was conducted along picket lines and shorelines. Outcrop locations were recorded on field work sheets; foliations, textural and compositional variations, alteration and mineralization were noted in the field. The results of these observations are recorded on geological maps in the back pocket of this report.
11.
GEOLOGY
Regional Geology
The Manitou Lakes area is underlain by a northeasterly trending, easterly dipping suite of Early Precambrian metamorphosed volcanic and sedimentary rocks known as the Manitou-Stormy Lakes greenstone belt. This belt joins with an east-west trending sequence in the Dryden area, and in the southwest, the Kakagi Lake - Lake of the Woods metavolcanic belt, and together they form part of the Wabigoon subprovince of the Canadian Shield.
The bedrock consists primarily of thick assemblages of metavolcanic rock with subordinate metasedimentary rock sequences intruded by subvolcanic stocks, sills, and dykes of gabbro, feldspar porphyry, and quartz-feldspar porphyry. Flanking this suite to the west is the large Atikwa batholith, and to the east lies the Irene-Eltrut Lakes batholith (Figure 3).
Blackburn (1982) divides the Manitou Lakes metasedimentary-metavolcanic belt into two segments, separated by the northeasterly trending Manitou Straits fault. The northwesterly segment consists of pillowed and porphyritic mafic flows and intermediate pyroclastics with minor felsic fragments (Burton & Hodge 1984). The southeastern segment is composed of massive and pillowed mafic flows, intermediate pyroclastics and metasedimentary rocks.
Blackburn (1982), indicates that within the northwestern segment of the area, a chemical transition occurs from tholeiitic to mixed tholeiitic and calc-alkaline rocks. This chemical transition in many Canadian greenstone belts is a locus of epithermal activity and favourable for the occurrence of stratabound exhalative gold deposits (Detour Lake) and cross cutting vein deposits (Red Lake) (Trusler 1984).
Granitic ROCKSMetosedimentory RocksMetovolconic Rocks
Fault
Gold OccurrenceAnticlinal AxisSynclinal Axis
Del Norte OptionNOXE TECK
Silver Lake Claims /
Silver Lake Resources Inc. MANITOU STRAITS PROPERTY REGIONAL GEOLOGY MAP
District of Kenora, Ontario
15 KILOMETRES
13.
Burton and Hodge (1984), recognize several horizons of sulphide and carbonate-sericite schists in association with felsic volcanic rocks. The carbonate-sericite schists consist of sheared fine grained rhyolitic tuffs and/or cherts; sulphide-bearing units containing pyrite and pyrrhotite, and minor chalcopyrite, sphalerite, and galena. Burton and Hodge (1984), suggest that because of their proximal relationship to lithological contacts, they probably represent original volcanic exhalite deposits. Burton and Hodge (1984) also indicate that there is a spatial relationship of gold occurences in the Manitou Lakes area to these sulphide/schist/exhalite horizons.
The principal structural feature of the area is the Manitou Straits Fault. This fault trends southwesterly from northeast of Gold Rock on Upper Manitou Lake, through both Upper & Lower Manitou Lakes to connect with an east-west trending fault in the Manitou Stretch area. Several subsidiary parallel to subparallel faults have also been recognized (Blackburn, 1976).
Two major fold structures occur: a major synclinal fold whose axis is presumed to lie along or proximal to the Manitou Straits Fault, and, to the northwest of the Manitou Straits Fault the Manitou Anticline. Trusler (1984)
proposed that the Manitou Straits Fault is actually a highly strained hinge zone to the Manitou Lakes sync! inorium.
Property Geology
During the Early Precambrian a composite mafic to felsic volcanic sequence containing subvolcanic intrusions and minor cherty interflow sediments was
deposited on the Manitou Straits property. Partially coincident with the intrusion of the Atikwa Batholith, to the west, the rocks were folded and regionally metamorphosed. Synchronous to this, shearing occured along the axis of the highly strained Manitou Straits syncl inorium. This zone is highly sericitezed and carbonatized.
14.
tratigraphy and Lithology
The rocks on the property are domlnantly mafic flows. These rocks are fine to medium grained, greyish green to dark green on weathered surfaces and dark green on the fresh surface. Magnetic attraction is generally weak, but locally is very strong. Individual flows are characterized by phenocrysts, amygdules, vesiclues, pillows, or massive textures, and are traceble for hundreds of feet. Within the porphyritic variety, white rounded phenocrysts of feldspar may be up to five inches in diameter. Locally, phenocrysts comprise up to 75% of the rock and are intermeshed. In the vicinity of shear zones, mafic flows are strongly foliated to schistose.
Mafic tuff is dark green to black on the weathered surface and dark green on fresh surfaces. The rock is fine grained with a fissile foliation which readily cleaves. It may also be Icoally magnetic. The rock generally consists of fine ash but this may locally grade into lapilli tuff and/or tuff breccia with fragments being slightly more felsic in composition.
Intermediate to felsic flows are greyish green to buff on the weathered
surface and light green to tan on the fresh surface, aphanatic to fine grained and occasionally porphyritic, massive to weakly foliated, and have no magnetic attraction. Frequently, barren white quartz veins occur in joints in this rock unit.
Felsic pyroclastic rocks include ash, lapilli tuff, and tuff breccia. These
units are frequently intercalated and/or occur as inter-flow units. The ash and lapilli tuffs are grey and light greyish green to buff on weathered and fresh surfaces respectively. Both lapilli and ash are fine grained to aphanatic. Tuff breccia is light greyish tan on weathered surface with fresh surfaces having light green fragments in a slightly darker green matrix. Matrix material and fragments may be aphanatic and/or fine grained. Fragments are usually three
inches to one foot in length, and rarely up to 18 inches.
15.
horizons form two to ten foot thick units at various strati graphic positions on the property. The chert weathers light grey and is light greyish green on fresh surfaces. The rock is aphanatic, thinly laminated to very thinly bedded and unmineral ized, and it breaks with a conchoidal fracture.
Sericite schist underlies a portion of the central and eastern part of the property. This rock is light buff to brown, phyllitic and fissile, locally contains quartz eyes, and lacks magnetic attraction. In many areas the rock contians five to twenty foot wide zones of oxidized quartz-carbonate (ankerite) veining. Mapping across the main 3500 foot wide shear zone which passes through
the property indicates that the sericite schist may be highly altered mafic volcanic rock. Similarly, the quartz sericite schist appears to be the altered product of intermediate to felsic rocks.
Two major metamorphosed gabbro sills and several smaller lenticular metagrabbro bodies intrude the volcanic sequence. The gabbro tends to be massive, medium to fine grained, equi granular, dark green to black on both weathered and fresh surfaces, with subhedral to anhedral black amphibole and dark green plagioclase laths. Locally, the gabbro is strongly magnetic, foliated and may contain blue quartz eyes. In many places the gabbro grades into and locally appears to be intruded by a dioritic phase. The diorite resembles the gabbro, but is much coarser grained, contains lighter coloured feldspars and has no apparent magnetic attraction.
Several small aplite dykes were found on the western end of the property. The rock is very light grey and buff on weathered and fresh surfaces respectivley. Locally, it may exhibit a porphyritic texture. Pherocrysts are
glassy quartz and are generally less than 0.1 inches. Dykes range in width from five to twenty feet.
16.
Geology
A total of 70 rock samples were collected and assayed for gold. The results of these analyses Including sample locations and descriptions are listed in Table 1.
Trace amounts of disseminated pyrite were found in all rocks excepting the cherty interflow rocks and the highly oxidized and sericitized rocks of the main shear zone. Greater amounts of pyrite along with pyrhotite (3-10% total sulphides) were found in a graphitic alteration zone between lines 123+OOW and
124+OOW at 46+OON. Although grab samples assayed from this zone failed to indicate any values better than trace gold, the geophysical surveys indicate that this zone is much larger, and thus warrants additional work.
Table 1
ROCK SAMPLES
Sample # Location
30551 12+OOE 62+25N
30552 23+50E 58+OON
30553 23+50E 58+OON
30554 150+OOW 69+25N30555 150+OOW 69+25N30556 149+50W 59+75N
30557 149+25W 59+75N
30558 32+OOW 28+OON
30559 32+OOW 28+OON
30560 40+OOW 4+OOS
30561 40+OOW 4+OOS
30562 144+OOW 53+50N
30563 136+OOW 14+25N
30564 136+OOW 14+25N
Rock Description Oz. Au/ton
pyritic metovolcanic rock 0.004gossan in metavolcanic rock nilquartz-tourmaline vein nil
gossan in quartz vein nilfelsic tuff nilquartz vein tracefelsic tuff nil
chlorite schist with py tracequartz vein nilquartz vein nil quartz veing with py & malachite tracepyritic mafic tuff trace
chert tracesheared basalt with quartz trace
carbonate veinlets
^65
30566
30567
30568
30569
30570
30571
30572
30573
30574
30575
30576
30577
30578
30579
30580
30581
30582
30583
30584
30585
30586
30587
30588
30589
30590
30591
30592
30593
30594
136+OOW 14+25N
125+OOW 46+OON
125+OOW 46+OON
124+OOW 46+25N
124+OOW 46+25N
120+OOW 24+25N
112+OOW 16+OON
112+OOW 39+50N
112+OOW 42+50N
112+OOW 42+50N
123+OOW 46+OON
123+OOW 46+OON
92+OOW 39+75N
100+OOW 18+50N
100+OOW 22+50N
88+OOW 24+75N
84+OOW 23+OON
33+OOS 48+OOE
31+OOS 45+50E
43+50S 51+50E
96+OOS 5+60W
96+OOS 4+50W
80+OOS 49+50E
80+OOS 49+50E
80+OOS 49+50E
68+OOS 52+OOE
80+OOS 58+OOE
86+OOS 47+50E
90+OOS 45+50E
88+OOS 71+OOE
chemical sediments trace
gossan with graphite & py trace
bleached basalt trace
silicified basalt with py trace
gossan with quartz stringers trace
porphyritic basalt trace
aplite with tr. py trace
gossan with tr. py trace
quartz vein trace
chlorite schist trace
mafic volcanic with graphite trace
and sulphides
mafic volcanic with sulphides trace
lapilli tuff with gossan trace
quartz vein trace
metavolcanic with tr. cpy, py trace
and malachite
mafic tuff with magnetite trace
quartz vein with malachite trace
quartz-carbonate vein trace
quartz sweats with py & magnetite trace
quartz carbonate vein with trace
20% magnetite
carbonate rich sericite schist trace
quartz vein trace
mafic volcanic with py trace
magic volcanic with py trace
mafic volcanic with quartz veins trace
sericite schist trace
carbonate vein trace
pyritic chert trace
quartz breccia trace
pryitic sericite schist trace
'W 30596
30597
30598
30599
30600
30601
30602
30603
80604
30605
30606
30607
30608
30609
A 30610
9 30611
30612
30613
30614
30615
30616
30617
30618
30619
30620
88+OOS 23+25W
88+OOS 23+25W
88+OOS 23+25W
88+OOS 23+25W
136+OOS 15+50E
124+OOS 15+OOE
124+OOS 15+OOE
121+OOS 8+25E
121+OOS 8+25E
63+OOS 76+OOE
113+OOS 97+OOE
113+OOS 97+OOE
133+OOS 61+50E
133+OOS 61+50E
133+OOS 61+50E
77+OOS 35+75W
76+OOS 40+OOW
61+OOS 40+OOW
56+OOS 12+75W60+OOS 16+OOW
60+OOS 16+OOW
60+OOS 16+75W
60+OOS 18+75W
60+OOS 18+75W
64+OOS 35+50W
64+OOS 18+80W
18.
bleached basaltbleached basaltbleached basalt with specularitequartz-carbonate veinquartz veinquartz veinsericite schistgossanbasalt with gossanf el sic tuffrhyolite with py, cpyfeldspar porphyry with pyrhyolite with 15% disseminatedpyriterhyoliterhyolite with quartz-carbonateveinletssericite schistquartz sericite schistfelsic tuff
altered basalt with specularitebasalt with gossan
gossan with 10% sphericulesmafic tuff with 3-10% pyquartz-carbonate veinpyritic gossanbasalt with 20% magnetitequartz sericite schist
0.002tracetracetracetracetracetracetracetracetracetracetracetrace
tracetrace
tracetracetrace
trace0.014
tracetracetrace0.002tracetrace
19.
A grab sample taken from a pyritic and oxidized mafic volcanic rock located on line 60+OOS at 16+OOW assayed 0.014 oz Aii/ton. Malachite stained quartz veins located on line 40+OOW at 4+OOS, and on line 84+OOW at 23+OON failed to indicate any values better than trace gold.
These four areas warrant additional prospecting and exploration.
20.
CONCLUSIONS AND RECOMMENDATIONS
The V.L.F.E.M. and Magnetic surveys revealed dozens of bedrock conductors and magnetically anomalous areas. Geological mapping revealed a zone mineralized with gold on line 60+OOS at 16+OOW.
The strong parallel linear magnetic anomalies located between lines 8+OOW and 128+OOW trending at N75 E are coincident with magnetite rich mafic sills. The Gaffney gold deposit, located four miles northeast of the property is associated with a similar magnetite rich mafic sill. Chances for the occurrence of a similar type of gold mineralization on the Manitou Straits property appear favourable.
The large magnetic anomaly located along the northern boundary of claim K744793 is spatially associated with a V.L.F.E.M. conductor. These anomalies are underlain by intermediate to felsic volcanic rocks and mafic tuff breccias. This anomaly should be explored for Kuroko-type base metals.
Several malachite stained pyrite-bearing quartz veins occur on the property. Malachite is common in many of the vein gold deposits of the Manitou Lakes area. Although only trace gold values were obtained from grab samples, additional prospecting is warranted.
Further geological, V.L.F.E.M., soil geochemical, and magnetic surveys and
prospecting are recommended for the summer of 1985. If warranted, a more detailed and comprehensive exploration programme should follow.
21.
COST ESTIMATES
Phase I
Geological MappingGeochemical SurveyProspectingAssaying (rock samples 300 @ $12/sample)TravelSupervision
Subtotal
6,000.00
18,000.00
3,000.00
3,600.00
3,300.00
3,000.00$36,900.00
Phase II
Drilling 4000' 0 $25.00AssayingLogging
Travel and AccommodationSupervision
Subtotal
TOTAL
$100,000.00
4,000.00
4,000.00
6,000.00
2,000.00
$116,000.00
$152,900.00
22.
REFERENCES
Blackburn, C.E., 1976: Geology of the Lower Manitou/UphiTI Lakes Area, District of Kenora, Geoscience Report 142, Ontario Division of
Mines.
Blackburn, C.E., 1982: Geology of the Manitou Lakes Area, District of Kenora, Report 189, Ontario Geological Survey.
Burden, L.D., 1985: Magnetometer and V.L.F.E.M. Surveys of the Lower ManitouLake Property, District of Kenora, Private report for Del Norte Chrome Corporation.
Burden, L.D., 1985: Magnetometer and V.L.F.E.M. Surveys of the Manitou StraitsProperty, District of Kenora, Private Report for Silver Lake Resources Inc.
Burton, G.B. and Hodge, H.J., 1984: Report on the Manitou Straits Property,Manitou Lakes Area, District of Kenora, Private report for Del Norte Chrome Corporation.
Thomson, J.E., 1934: Geology of the Straw/Manitou Lakes Area, Ontario Department of Mines Annual Report for 1934, Vol 43, pt 4, p 1-28.
Trusler, J.R., 1984: Manitou Straits Project, Kenora Area, Ontario, Private report for Silver Lake Resources Inc.
Geophysical Map, 1160G, Department of Mines and Technical Surveys, Geological Survey of Canada 1962.
23,
:RSONAL DECLARATION
I, LORNE D. BURDEN, of 27 Hollingworth Drive, Scarborough, Ontario,
DO HEREBY CERTIFY THAT:
1. I am a consulting geologist.
2. I have worked in mineral exploration since 1979.
3. I am a graduate of the University of Toronto where I obtained a B.Sc. degree specializing in geological sciences in 1981.
4. I am a member of the Prospectors & Developers Association.
5. This report is based on personal examination of the claim group in conjunction with a review of all available reports, maps and sections concerning the area.
6. I have no interest in the properties or securities of Silver Lake Resources Inc., nor do I expect to receive or acquire any.
DATED THIS 12th day of February, 1985.
LORNE D. BURDEN, B.Sc.
- WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX !87 HAILEYBURY. ONTARIO TEL: (7O5) 672-31O7
POJ 1KO
June 11, 1985
Silver Lake Resources Suite 4650, Box 77 T. D. Bank Tower Toronto Dominion Centre TORONTO, Ontario M5K 1E7
Attention: Mr. Lome Burden
Gentlemen:
As requested, this letter is to confirm that the following invoices, issued to Silver Lake Resources by Bell-White Laboratories Ltd., have been paid in full:
-Invoice #18317, dated April 22, 1985: $4,721.60
-Invoice #17009, dated August 17, 1984: $ 286.00
-Invoice #17283, dated September 18, 1984:$ 484.00
Yours truly,
(Mrs.) P. Lafreniere Secretary
pi
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187 HAILEYBURY. ONTARIO TEL: (7O5) 672-3107
POJ 1KO
Silver Lake Resources,
Suite 4650, P.O. Box 77, Toronto Dominion Bank Tower, Toronto-Dominion Centre, Toronto, Ontario. M5K 1E7
INVOICE N2 17009
ORDER NO.
DATE August 17, 1984
:RTIFICATE NO. DATE DESCRIPTION AMOUNT
29990 Aug.17/84
Charge to: Manitou Straits Project
26 Au, 26 sample preparations
(IfifalfrtfJ \st/ i
sfttLj/r^ •
$ 286.00
HITE ANALYTICAL LABORATORIES LTD,P.O. BOX 187 HAILEYBURY. ONTARIO TEL: (7O5) 672-31O7
POJ 1KO
Silver Lake Resources Inc., Sui t c A650, P. 0. Box 77, Toronto-Dominion Bank Tower, ToronIo-Dominion Centre, Toronto, Ontario. M5K 1 E-l 7
INVOICE NO 17283
ORDER NO.
DATE September 18, 1984
i-'TIFICATE NO
40346
DATE
Sept.18/84
DESCRIPTION
Manitou Straits Project
44 Au @ $8.50 each,44 sample preparations @ $2.50 each
XV
J
AMOUNT
$ 374.00 110.00
$ 484.00
NO. 29990
SAMPLE (S) OF:
SAMPLE (S) FROM:
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-31O7
Certificate of Attalgate
Rock(26)
DATE: A ugust 17, 1984
RECEIVED: A ugust, 1984
Ms. Cynthia Drybrough, Silver Lake Resources
(Re: Manitou Straits Project)
Sample No.
G30551
2
3
4
5
6
7
8
9
G30560
1
2
3
Oz. Gold
0.004
Nil
Nil
Nil
Nil
Trace
Nil
Trace
Nil
Nil
Trace
Trace
Trace
Sample No.
G30564
5
6
7
8
9
G30570
1
2
3
4
5
6
Oz. Gold
Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace
ACCORDANCE WITH LONG.ESTABLISHED NORTH,'ICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATEDRWISE GOLD AND SILVER VALUES REPORTED ONE SHEETS H AVE NOT BEEN ADJUSTED TO COMPEN-
FOR LOSSES AND GAINS INHERENT IN THE FIREASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
PER.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-3107
drrttfirat? nf AnaUj0taNO. 40346 DATE: S eptember 18, 1984
SAMPLE(S) OF: Rock(44) RECEIVED: S eptember, 1984
SAMPLE(S) FROM: Mr. Lome Burden, Silver Lake Resources Inc.
MANITOU STRAITS PROJECT
Samp I e No ,
G3057789
G30580123456789
G3059012345678
Oz. Gold
Trace T race T race T race T race T race T race T race T race T race T race T race T race T race T race T race T race T race 0.002* T race T race T race
Samp I e No ,
G30599 G30600
123456789
G30610123456789
G30620
Oz. Gold
TraceTraceTraceTraceTraceTraceTraceTraceT raceTraceT raceTraceT raceTraceT race0.014TraceTraceTrace0.002*TraceTrace
E s t i ma t ed
ACCORDANCE WITH LONG-ESTABLISHED NORTH:RICAN CUSTOM, UNLESS IT is SPECIFICALLY STATEDlERWISE GOLD AND SILVER VALUES REPORTED ON SE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN- E FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
5aFa3NE8>ai7 2 .6246 NAPANEE LAKE 020
SOIL GEOCHEMISTRY OF SELECTEDPORTIONS OF THE
MANITOU STRAITS PROPERTY DISTRICT OF KENORA
for
Silver Lake Resources Inc.Suite 4650, P.O. Box 77, TD Bank Tower
Toronto Dominion CentreToronto, Ontario
M5K 1E7
2; ,98S
June, 1985 Harris Lake Area District of Kenora NTSi 52F/ LORHE BURDEN
SUMMARY
The 161 claim Manitou Straits property is located on the southwestern end of
Lower Manitou Lake. The property is underlain by an Early Precambrian
southwesterly trending sequence of metamorphosed mafic to felsic volcanic rocks
intruded by mafic sills.
The property is on strike with four gold prospects. The Gaffney deposit,
four miles northeast of, and on strike with the Manitou Straits property, has
recently undergone an intensive drill programme by a Teck Corporation - Noxe
Petroleum Corporation joint venture. Estimates of possible gold reserves prior
to recent drilling were as high as 621,000 tons of material grading 0.22 oz gold
per ton (Neilson and Bray, 1981).
The Gold Standard North, Sairy Gamp, and Gold Standard South prospects are
four, four and one-half, and five miles respectively to the southwest of the
property. Each of these prospects were worked near the turn of the century and
developed with exploration shafts.
In early 1984, a 400' line grid was established on the property;
magnetometer, V.L.F.E.M. and geological surveys were conducted. Several magnetic
and V.L.F.E.M. anomalies were outlined. Many of the magnetic anomalies are
similar in intensity to the anomaly over the Gaffney gold deposit and occur in a
similar geological setting. Also, several other geologically interesting areas
were outlined.
A soil geochemical survey was carried out in conjunction with geological and
geophysical surveys. Several geologically, geochemically and geophysically
promising areas have been identified. Detailed prospecting of these selected
areas is recommended for the 1985 field season.
52F03NE0ei7 2 .8346 NAPANEE LAKE 020C
Table of Contents
SUMMARY
INTRODUCTIONLocation and AccessPropertyTopography and Vegetation
EXPLORATION HISTORY AND PREVIOUS WORK
CURRENT EXPLORATION
REGIONAL GEOLOGY
SOIL GEOCHEMISTRY
CONCLUSIONS AND RECOMMENDATIONS
COST ESTIMATE
REFERENCES
PERSONAL DECLARATION
APPENDIX
Figure 1 Figure 2 Figure 3
Plan 1 Plan 2
List of Figures and Tables
LOCATION MAPCLAIM MAPREGIONAL GEOLOGY MAP
List of Plans (map pouch)
East Sheet Soil Geochemistry; Gold West Sheet Soil Geochemistry; Gold
Page
i
137
8
10
11
14
15
16
17
18
19
26
12
INTRODUCTION
The Manitou Straits property is underlain by Early Precambrian raetavolcanic
rocks and actually straddles a major transition in the volcanic rock chemistry
from tholeiitic to mixed calc alkaline and tholeiitic. This boundary between
oceanic volcanics and an overlying stratovolcano is typically the locus of many
Early Precambrian gold deposits. In the Manitou Lakes area, the Gaffney deposit
occurs at such a contact and numerous other gold occurrences are found in close
proximity to this horizon (Burton & Hodge, 1984).
A geochemical soil survey was conducted during the 1984 field season. This
survey was performed in an attempt to outline zones of mineralization obscured by
overburden. The results of this work are presented in this report.
Locations and Access
The property is located near the southern end of Lower Manitou Lake
approximately 40 miles south of Dryden, and 40 miles north of Fort Frances,
Ontario (Figure 1). Highway 812 passes approximately 5 miles east of the
property.
Access may be obtained by float or ski equipped aircraft available in both
Dryden and Fort Frances. Boat or snowmobile may also be used to reach the
property from Esox Lake located 20 miles to the south and accessable by logging
roads from Hwy. 812.
Several radio telephones are available at tourist camps and private cabins
around the lake. A barge service is available on the lake for transportation of
heavy equipment, and a seasonal helicopter base is maintained at camp Beaverhead
8 miles northeast of the claim group.
Manitou Straits
Silver Lake Resources Inc. Manitou Straits Property
LOCATION MAPDistrict of Kenora, Ontario
Figure 1
Property
The 6440 acre, Manitou Straits property was staked for Silver Lake Resources
Inc. during the winter of 1983-1984. The property comprises 161 contiguous
unpatented mining claims which are identified as follows, and illustrated in
Figure 2.
M2469, Napanee Lake Area, District of Kenora
K
Claims
729890729891729892744448744449744450744451744452744453744454744455744456744457744458744459744460744461744462744463744464744465744466744467744468744469744470744471744472744473
Recorded
November 29, 1983
Claims
744474744475744476744477744478744479744480744481744482744483744484744485744486744487744488744489744490744491744492744493744494744495744496744497744498744499744500744501744502744503
Recorded
November 29, 1983
MINING CLAIMS TRAVERSED ( cont'd)
K
NUMBER
744504744505744506744507744508744509744516744517744518744519744520744521744530744531744532744533744534744535744544744545744546744547744553744554744555744556744964744965744966744967744968744969744970744971744972744973744974744975744976744977744978744979
Recorded
November 29, 1983 K
November 29, 1983 February 8, 1984
NUMBER
744980744981744982744983744984744985744986744987744988744989744990744991744992744993744994744995744996744997744998744999745000745001745002745003745004745005745006745007745008745009745010745011745012745013745014745015745016745017745018745019745020745021
Recorded
February 8, 1984
MINING CLAIMS TRAVERSED ( cont'd)
NUMBER
745022745023745024745025745026745027745028745029745030745031745032745033745034745035745036745037745038745039
Recorded
February 8, 1984
SILVER LAKE RESOURCES
TAKEN FROM M MR. MAP
MANITOU STRAITS PROJ.
CLAIM MAP •'_
Topography and Vegetation
Approximately 30 percent of the property Is covered by water. The remainder
of the property is covered by undulating hills with maximum relief of 70 feet.
Vegetation consists of mature spruce, pine and balsam, with alders and
manitoba maple present as undergrowth. Locally, mature cedar swamps can be found
In depressed areas.
EXPLORATION HISTORY AND PREVIOUS WORK
The first comprehensive geological mapping of the area was carried out by
Thomson (1934) covering both the Upper and Lower Manitou Lakes areas as well as
the Manitou Stretch area. More recently, Blackburn (1976, 1982), mapped the
Upper and Lower Manitou Lakes area in detail to the north of the Manitou Straits
property.
The Manitou Lakes area was the scene of considerable gold prospecting and
mining activity from 1895 to 1912, and again in the 1930's (Thomson, 1934). This
activity resulted in the discovery of twenty gold occurences in the area. These
occurences have been described in detail by Burton and Hodge (1984).
During the 1950's and 1960's, some base metal and iron exploration was
carried out in the area. With the discovery of the Mattabi Mine on Sturgeon
Lake, approximately 100 miles northeast of the property, exploration in the
region was intensified.
Airborne geophysical surveys for base metals were carried out in 1970 by
Freeport Canadian Exploration Co. on Lower Manitou Lake to the north of the
Manitou Straits property.
The Canadian Nickel Company held several small claim groups around and
included within the bounds of the Manitou Straits property between 1969 to 1972.
Three separate locations were tested on the property by diamond drilling.
Diamond drill logs, available from the Ministry of Natural Resources, Assessment
Office in Toronto, indicate that one drill hole located at the northwest tip of
Syndicate Lake intersected mafic volcanics and gabbro with disseminated
pyrrhotite and pyrite. A second drill hole southwest of Syndicate Lake
intersected felsic and mafic volcanics containing minor sulphides and carbonate
alteration. The third drill hole located immediately south of Calder Lake
intersected mafic volcanics and gabbro, also intersected was a zone of 25%
disseminated pyrite associated with quartz veining and magnetite. No assay
values were published, and gold analyses were probably not performed.
The Gaffney gold deposit, located four miles northwest of the property, was
discovered in 1927, and to 1944 was tested by 42 diamond drill holes (Trusler,
1984). The property, dormant since 1944, was acquired in July 1983 by Noxe
Petroleum Corporation and Teck Corporation in an 86 claim package. The gold
mineralization is associated with pyritic alteration halos surrounding a
stockwork of quartz veins at the base of a mafic sill. The mafic sill, rich in
magnetite, forms both a strong airborne and ground anomaly. Discussions with the
Teck geologist involved with the Gaffney deposit revealed that the magnetic
anomaly correlates well with the zone of mineralization.
The Gold Standard North, Sairy Gamp, and Gold Standard South gold prospects
occur four, four and one-half, and five miles respectively to the southwest of
the Manitou Straits property along the regional geological trend.
10
CURRENT EXPLORATION
In early 1984, a line grid was established on the Manitou Straits property.
A total of 15.91 miles of base and tie lines were cut; perpendicular to this,
95.72 miles of picket lines were cut at 400 foot intervals with pickets every 100
feet.
Magnetometer and V.L.F.E.M. surveys over water covered portions of the
property were conducted between February 28 and March 14, 1984 by Norontex
Explorations Ltd. of Dryden, Ontario. Instrument readings were taken at 100 foot
intervals on all picket lines.
During the summer of 1984, magnetometer, V.L.F.E.M. and geological surveys
were conducted over the remainder of the property by Silver Lake Resources Inc.
Instrument readings were taken at 50 foot intervals on all picket lines. In
areas with anomalous magnetic values, readings were taken at 25 foot intervals.
Geological mapping was conducted along picket lines and shorelines, outcrop
locations were recorded on field work sheets; foliations, textural and
compositional variations, alteration and mineralization were noted in the field.
The above mentioned work was previously summarized in two reports by Burden
(1985a, and 1985b).
In conjunction with the geophysical and geological surveys, a soil
geochemical survey was conducted over the Manitou Straits property.
Approximately 3,600 samples were collected of the B horizon, where possible, at
50 foot intervals along each line. Four hundred and fifty-nine of these samples
were selected for analyses. The remaining samples are in storage in Fort
Frances, Ontario.
11
REGIONAL GEOLOGY
The Manitou Lakes area is underlain by a northeasterly trending, easterly
dipping suite of Early Precambrian metamorphosed volcanic and sedimentary rocks
known as the Manitou-Stormy Lakes greenstone belt. This belt joins with an
east-west trending sequence in the Dryden area, and in the southwest, the Kakagi
Lake - Lake of the Woods metavolcanic belt, and together they form part of the
Wabigoon subprovince of the Canadian Shield.
The bedrock consists primarily of thick assemblages of metavolcanic rock
with subordinate metasedimentary rock sequences intruded by subvolcanic stocks,
sills, and dykes of gabbro, feldspar porphyry, and quartz-feldspar porphyry.
Flanking this suite to the west is the large Atikwa batholith, and to the east
lies the Irene-Eltrut Lakes batholith (Figure 3).
Blackburn (1982) divides the Manitou Lakes metasedimentary-metavolcanic belt
into two segments, separated by the northeasterly trending Manitou Straits fault.
The northwesterly segment consists of pillowed and porphyritic mafic flows and
intermediate pyroclastics with minor felsic fragments (Burton & Hodge 1984). The
southeastern segment is composed of massive and pillowed mafic flows,
intermediate pyroclastics and metasedimentary rocks.
Blackburn (1982), indicates that within the northwestern segment of the
area, a chemical transition occurs from tholeiitic to mixed tholeiitic and
calc-alkaline rocks. This chemical transition in many Canadian greenstone belts
is a locus of epithermal activity and favourable for the occurrence of
stratabound exhalative gold deposits (Detour Lake) and cross cutting vein
deposits (Red Lake) (Trusler 1984).
Granitic Rocks
Metosedimentory RocksMetovolconic Rocks
Fault
Gold Occurrence
Anticlinal AxisSynclinal Axis ^A^s\
Del Norte Option ,s *.'
Silver Lake Claims
Silver Lake Resources Inc. MANITOU STRAITS PROPERTY REGIONAL GEOLOGY MAP
District of Kenora, Ontario
13
Burton and Hodge (1984), recognize several horizons of sulphide and
carbonate-sericite schists in association with felsic volcanic rocks. The
carbonate-sericite schists consist of sheared fine grained rhyolitic tuffs and/or
cherts; sulphide-bearing units containing pyrite and pyrrhotite, and minor
chalcopyrite, sphalerite, and galena. Burton and Hodge (1984), suggest that
because of their proximal relationship to lithological contacts, they probably
represent original volcanic exhalite deposits. Burton and Hodge (1984) also
indicate that there is a spatial relationship of gold occurences in the Manitou
Lakes area to these sulphide/schist/exhalite horizons.
The principal structural feature of the area is the Manitou Straits Fault.
This fault trends southwesterly from northeast of Gold Rock on Upper Manitou
Lake, through both Upper & Lower Manitou Lakes to connect with an east-west
trending fault in the Manitou Stretch area. Several subsidiary parallel to
subparallel faults have also been recognized (Blackburn, 1976).
Two major fold structures occur: a major synclinal fold whose axis is
presumed to lie along or proximal to the Manitou Straits Fault, and, to the
northwest of the Manitou Straits Fault the Manitou Anticline. Trusler (1984)
proposed that the Manitou Straits Fault is actually a highly strained hinge zone
to the Manitou Lakes synclinorium.
14
SOIL GEOCHEMISTRY
In conjunction with geological and geophysical surveys, a soil geochemical
survey was conducted over the Manitou Straits property. A total of 3596 samples
were collected of B horizon at 50 foot intervals along each line, where
possible.
Three to ten inches of Organic and A horizon soils were scraped off each
sample location using a grub hoe, and fist size samples of B horizon soil were
placed in numbered paper sample bags. The samples were then dried, and placed in
storage at Fort Frances, Ontario.
After the completion of geological and geophysical surveys, 459 soil samples
were selected over two geologically and geophysically interesting areas. These
samples were sent to Bell-White Laboratories in Haileybury, Ontario for
analysis.
Bell-White screened the samples to -80 mesh, selected 10 gram portions of
this fraction and produced a dore bead. The dore beads were in turn redissolved
into solution with aqua-regia and then tested for gold by atomic absorption.
The analytical results are tabulated in Appendix 1, and presented on Plans 1
and 2.
Using the geometric mean as an estimate of background soil gold values, it
was determined that 4 ppb is background. Truly anomalous values are assumed to
be five times background or 20 ppb.
This simple data massage indicates that there are no truly anomalous soil
samples but there are 12 areas containing possibly anomalous soils which warrant
further investigation.
15
CONCLUSIONS AND RECOMMENDATIONS
The 459 soil samples were chosen to test the response of gold in soils over
selected geophysical anomalies, and geologically favourable areas. Although no
anomalous soils were located, several areas of possibly anomalous soils were
found and these were spatically associated with geophysical anomalies. The best
anomalies, located between lines 80+OOS and 92+OOS at 2+OON and 1+50S are
proximal to magnetic highs within geologically favourable ground, i.e. a wide
shear zone passing through the central portion of the property (Burden, 1985 b).
A second possibly anomalous area located between lines 60+OOS and 64+OOS at
16+OOW is proximal to a surface gold showing. Several more possibly anomalous
values are located along line 124+OOW between 26+OON and 52+OON. These western
possibly anomalous soils are all directly associated with magnetic and V.L.F.E.M.
anomalies.
All possibly anomalous zones warrant stripping and trenching so as to
determine the source of the anomalous gold values. Also, a second batch of soil
samples should be selected over portions of the remaining geophysical anomalies
to further test their association with geochemical anomalies. Should these
samples also define geochemically anomalous or possibly anomalous zones, they too
should be prospected.
If positive results are obtained from the above programme, all soil samples
should be analysed, and a more detailed and comprehensive exploration programme
should follow.
16
COST ESTIMATES
Geochemical Analysis 500 samples @ $12.OO/sample
Prospecting
Stripping and Trenching
Assaying 200 samples @ $12.00/sample
Travel and Accommodations
Supervision
$ 6,000.00
4,500.00
4,000.00
2,400.00
5,000.00
3.000.00
$24,900.00
17
REFERENCES
Blackburn, C.E., 1976: Geology of the Lower Manitou/Uphill Lakes Area, District of Kenora, Geoscience Report 142, Ontario Division of
Mines.
Blackburn, C.E., 1982: Geology of the Manitou Lakes Area, District of Kenora, Report 189, Ontario Geological Survey.
Burden, L.D., 1985: Magnetometer and V.L.F.E.M. Surveys of the Lower ManitouLake Property, District of Kenora, Private report for Del Norte Chrome Corporation.
Burden, L.D., 1985 (a): Magnetometer and V.L.F.E.M. Surveys of the ManitouStraits Property, District of Kenora, Private Report for Silver Lake Resources Inc.
Burden, L.D., 1985 (b): Geology of the Manitou Straits Property, District of Kenora, Private Report For Silver Lake Resources Inc.
Burton, G.B. and Hodge, H.J., 1984: Report on the Manitou Straits Property,Manitou Lakes Area, District of Kenora, Private report for Del Norte Chrome Corporation.
Thomson, J.E., 1934: Geology of the Straw/Manitou Lakes Area, Ontario Department of Mines Annual Report for 1934, Vol 43, pt 4, p 1-28.
Trusler, J.R., 1984: Manitou Straits Project, Kenora Area, Ontario, Private report for Silver Lake Resources Inc.
Geophysical Map, 1160G, Department of Mines and Technical Surveys, Geological Survey of Canada 1962.
18
PERSONAL DECLARATION
I, LORNE D. BURDEN, of 27 Hollingworth Drive, Scarborough, Ontario,
DO HEREBY CERTIFY THAT:
1. I am a consulting geologist.
2. T have worked in mineral exploration since 1979.
3. I am a graduate of the University of Toronto where I obtained a B.Sc. degree specializing in geological sciences in 1981.
4. I am a member of the Prospectors & Developers Association.
5. This report is based on personal examination of the claim group inconjunction with a review of all available reports, maps and sections concerning the area.
6. I have no interest in the properties or securities of Silver Lake Resources Inc., nor do I expect to receive or acquire any.
DATED THIS 20th day of June, 1985.
LORNE,D. BURDEN, B.Sc
19
APPENDIX
wELL-YYHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187 HAILEYBURY. ONTARIO TEL: (7O5> 672-31O7
POJ IKO
June 11, 1985
Silver Lake Resources Suite 4650, Box 77 T. D. Bank Tower Toronto Dominion Centre TORONTO, Ontario M5K 1E7
Attention: Mr. Lome Burden
Gent Iemen:
As requested, this letter is to confirm that the following invoices, issued to Silver Lake Resources by Bel]-White Laboratories Ltd., have been paid in full:
-Invoice #18317, dated April 22, 1985: $4,721.60
-Invoice #17009, dated August 17, 1984: $ 286.00
-Invoice #17283, dated September 18, 1984:$ 484.00
Yours truly,
(Mrs.) P. Lafreniere Secretary
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187 HAILEYBURY. ONTARIO TEL: <7O5> 672-31O7
POJ 1KO
Silver Lake Resources !nc Suite 4650. Box 77 T. D. Bank Tcwer Toronto Dominion Centre TORONTO, Ontario M5K 1E7
INVOICE N2 18317
ORDER NO.
DATE April 22, 1985
I:RTIFICATE NO
B234-85
DATE
Apr. 22/85
DESCRIPTION
RE: Manitou Straits Project
459 Au (3 $8.50
459 sample preparations @ $1.26
BPX Charges (sec w/b *CC343467, CC3'13e-5,
L33330, CC343466. L33.il 4, 1.33316, CC343379,
CC343380, L29370, L33313, attached)
TOTAL :
-».^, *
AMOUNT
$ 3,901.50 573.75
$ 4,475.25
246.35
$ 4,721 .60
BELL-WniTE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-31O7
01?rttfiratr of AnalgataNO. B 234-85
SAMPLE (S) OF: S oil (459)
SAMPLE (S) FROM:
Page 1 of 5
Mr. Lome BurdenSilver Lake Resources Inc.
DATE: A pril 22, 1985
RECEIVED: April, 1985
RE: Mani tou Straits Project
Sample No
MS-2442345678
MS-2873 4A 4B567
MS-2880123456789
MS-2890123456
** Checked
Gold ppb Sample No. Gold ppb Sample No6444626846
108
1086428
104266466222262
MS-2897 MS-3025
6789
MS-30301234
MS-3054 MS-3056 MS-3058 MS-3060 MS-3062 MS-3064 MS-3066 MS-3068 MS-3070 MS-3072 MS-3074 MS-3075 MS-3077
89
MS-308012345
4646
148446828428426
121 2
264222426682
MS-3086789
MS-3090123456789
MS-3100123456789
MS-31101234567
Gold pj>b2~
44
166242268
1218**
2848448
14624
104664642
IN ACCORDANCE WITH LONG.ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEtN ADJUSTED TO COMPEN. JATE FOR LOSSES AND GAINS INHERENT IN THE FJRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-31O7
Qkrttfirat? 0f AnalgatBNO. B234-85
SAMPLE(S) OF: S o11 < 459 >
Page 2 o f 5
SAMPLE(S) FROM: M r - L orne B urdenSilver Lake Resources Inc.
DATE: A pril 22, 1985
RECEIVED: A pril, 1985
Sample NoMS-3118
9MS-3120
12345678
MS-3130 MS-3132 MS-3134 MS-3136 MS-3138 MS-3140 MS-3142 MS-3144
567
MS-3149 MS-3151
23
MS-3155 MS-3157 MS-3159 MS-3161 MS-3163 MS-3165
Gold ppb Sample No
464446284
1046
1064464646624264444
104
MS-3167 8
MS-3170 MS-3172
34
MS-3176 MS-3178
9 MS-3180
1 MS-3183
4567
MS-3189 MS-3190 MS-3192
3MS-3195 MS-3197 MS-3199 MS-3200
1MS-3203 MS-3205 MS-3207
89
MS-3210 MS-3212
Go 1d p pb42668266446262444262446468666644
Sampl e_No 1~'"MS 732T3™
4A 4B
MS-3216A 6B
MS-3218 MS-3220 MS-3222 MS-3224 MS-3226 MS-3228 MS-3230
123456
MS-3238 MS-3240 MS-3242
3 MS-3245
678
MS-3250 MS-3252 MS-3254 MS-3256 MS-3258 MS-3260
Gold p p _b -_........_._
668648868464864
10664264686644466
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES RfPORTED ON IIIISE bMEi-TS HAVl NOT BUN ADJUSTED TO COMPEN- vATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY, ONTARIO TEL: 672-31O7
QI?rttfkai? of AnalyateNO. B234-85 Page 3 of 5 DATE: April 22, 1985
SAMPLE (S) OF: Soil (459) RECEIVED: April, 1985
SAMPLE(S) FROM: ^ Lome Burden Silver Lake Resources Inc.
Sample No.MS-3262
34
MS-3266MS-3268MS-3270MS-3272
^ MS-3274m M S-3276
MS-32789
MS-32812345
MS-32878
MS-3290MS-3292MS-3294MS-3296MS-3298
9MS-3301
2MS-3304MS-3306MS-3308MS-3309MS-331 1
2
Gold ppb64622284442422224242242244222226
Sample No.MS-3317
8MS-3320MS-3322
3456
MS-3328MS-3330MS-3332
3MS-3335
6MS-3338MS-3340
1MS-3343
4MS-3346
7MS-3349MS-3351
2MS-3354
56
MS-33589
MS-33601
MS 3364
Gold ppb442224262246642448286
102626
1024642
Sample No."MS-~3365~
6MS-3368
9MS-3370
1234
MS-3376MS-3378MS-3380
123456
MS-33889
MS-3390MS-3392
3MS-3395
6789
MS-3400123
Gold ppb- ....__ 2__
2222644644426444622446646626426
IN ACCORDANCE WITH LONG -ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANA ORATORIES LTD.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY, ONTARIO
uf AnalgaiaNO. B234-85
SAMPLE (S) OF:
Page 4 of 5
Soil (459)
TEL: 672-31O7
DATE: A pril 22, 1985
RECEIVED: A pril, 1985
SAMPLE (S) FROM: Mr. Lome BurdenSilver Lake Resources Inc
Sample NoMS-3406
7
MS-341 12345
MS-3417 MS-3419 MS-3420 MS-3422
3456
MS-34289
MS-343123
MS-3435 MS-3437 MS-3439 MS-3441 MS-3443
4 MS-3446
78
MS-3450
Gold ppb Sample No Gold ppb Sample No,44462664224244242466424244264442
MS-3451234
MS-3456 MS-3458
9 MS-3460
1MS-3463 MS-3465 MS-3467
89
MS-34712
MS-3474 MS-3476
789
MS-3480123456789
MS-3490
44664224824442446442846622486442
MS-349123456789
MS-3500123456789
MS-3510123456789
MS-352012
Gol d_jppb26244668666446644446642262624644
IN ACCORDANCE WITH LONG -ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND CAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-31O7
(Sfcritfirafr ofNO. B234-85
SAMPLE(S) OF:
SAMPLE (S) FROM:
Page 5 of
Soil (459)
Mr. Lome BurdenSilver Lake Resources Inc
DATE: A pril 2 2, 1 985
RECEIVED: A pril, 1985
S_ample NoMS-3533
456789
MS-3530123456789
MS-35401234567
Gol d ppb
2424222424244424262424862
Sample No.MS-3548
9MS-3550
12345A5B6789
MS-3560123456789
MS-35701
GoUl_ ppb ....„
422244422424428648462466
MS-35723456789
MS-3580123456789
MS-3590123456
d__pp b24864246244224688664
144224
IN ACCORDANCE WITH LONG -ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVC NOT BEEN ADJUSTFD TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
Pen___
Ministry r>1 Natural
Ontario
Re(GiGni
52F03NE0017 2.8846 NAPANEE LAKE 900
|l mimt.r i ol mining clnini'. cxrfriK «.p;irr on this loim, nil;*' It o list. Onl\ ();iv. ripifil!. rtilmliiti'il in tin 1 "I x|>i'niiitun"." serlmn m.iv i"1 rnli'icd in 1h'- " k xpr>ml. liny. C i." rnlumiv.. l.)o not ur.c (h.uli'il flipiis liplnw
11 ivvnOii|> Ml An-.
Napanee Lakell'iiv-pf IIM'S l urrm Ni
T989
i VPP of Suivpyiil
GeochemicalClaim Holdpi(t)
Silver Lake Resources Inc.Address
Suite 4650, Box 77, Toronto Dominion Centre, Toronto, Ontario M5K 1E7Survey Compnny ll>.jtr nl j-'»t\'cy intm. .*-. ii>* llptol Milr*. t»( htir Cut
_ Silver Lake Resources Inc. j i n j 7,, ,84, | ,1.5, | $„ i 8A 110.5Name and Address of Author (of GPO Technical report)
___Lome Burden 27 Hollingworth Dr. Scarborough, Ontario____________________________Credits Requested per Each Claim in Columns at right Miniiui C'.itiiiiVi 1 lavi'isi'ii (I is1 in numcnr.'ilSpecial Provisions
For first survey:Enter 10 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse side and enter total(s) here
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
Other
Geological
Geochemical
u _._...
Geophysica,
- Electromagnetic
- Radiometric
^i 0 4 JQftK 'h"I Geological
'tl t /il''Jf}Q ('C.T'-i'i
Airborne Credits
Note: S pecial provisions i Electromagnetic: credits do not apply
Days per Claim
to Airborne Surveys. Magnetometer
Radtometrtc
Expenditures ( excludes power stripping)Type of Work Performed
Fire AssaysPerformed on Claim(s)
See Mining Claims Traversed
ColumnCalculation of Expenditure Days Credits
Total Expenditures
$ 770.00 H- 15 =
Instructions Total Days Credits may be apportioned at the c choice. Enter number of days credits per claim in columns at right. As per attachec
T ota! Days Crcdiu
51
laim holder's se ected. sheet
K 744452x 744453 .
744455 *
744461 744463,
744469'
744486
744492
..744495
744496
744497
.744504 _.
744544
744548
744551
744552
744553
744554
. J.44965
744977.
. 744990-
744991744996
t Xpf'MclD.iVi Ct.
Mtntnp CiHini 'f-1 o ] Numhfi
K 744997744998
745003
745011745012
7^5014
..745020.
745022
745029
fc xpend. Days Ct.
Total number of mining claims covered by tfiisreport of work.
Certification Verifying RerJert oI hereby certify that I have a personal and intimate knowledge of thr- (HCU set lortli in the Report of Work annexpri I or witnessed same during and/or after its completion and the annex'd report ir. tun
, having performed the work
Name and Postal Address of Person Certifying
Lome Burden 27 Hollingworth Drive ScarborouetyXltntario 1E1
13G2 (81/9)
Mining Claim
K 744488744480744481744482744491744492744493744546744547744553744554744988744996744997
Expenditure Credits To Be Distributed As Follows:
Expenditure Days Credit
24222222222222
51 day credit
Ministry ot NnUirnl Pr- -.urn..
Ontnno
Report ol Woik(Geophysical, Groli Gpochemical and t
Minimi Act
Imtitirliouv - 1'lc.v.i up' CM print'II mirnl"'i pi minmu claim pxri'i'ils HIJII-P on tlm lot in, tiltnc li i \ I IM
Notp - On!\ d.i\ ••. rtpdils colculnlnl in the "I MVMiiiliiii"." HTIIOM nt.is In- rntriril m tin- "{ xnpnd t)ays ('< " rotvimn',
- l>« not us' 1 Miaifc'tf ntpni. l)fUnv
1 VpP ot SurvryUi
Geochemical' p pi A te
i Napanee Lakeh : ioM>iN "" 's I it nu r
Silver Lake Resources Inc. . i T989Address
Suite 4650, Box 77, Toronto Dominion Bank Tower Toronto, Ontario M5K 1E7Survey Compnny In.vc »>' Smvrv ii'«"»' f . t < ' |lcii.";i M'lr%
_ Silver Lake Resources Inc. . i, v 7 M ,84, } tf 9M , ,84, J110.5Name and Ariiirevs of Autho' (o1 Gro 1 c< hniciil repoi t)
Lome Burden 27 Hollingworth Dr., Scarborough, Ontario
ot l inr Cut
Credits Requested per Each Claim in Columns al licj ! Cliiii'i 1 . 1 i.'ivi'isril (I ist in nuniciic.il sccnn-nrrSpecial Provision!.
For tirst surveyEnter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Gpophvstrnl
• E lecuomagnet it
• Magnrtomcin
• Rariiomrti ir
• Othpi
Geological
Geochemical
Man Days
Complete reverse side and enter total(s) here
Geophysical j ^ |a|n ,
j • Electromagnetir
i - Magnetomelp'
1 • Radiometnc
- Othe'
I Geological
i| Geochemical__ _
Airborne Credits
Note: Special provisions i Electromagnetic credits do not apply
11Days per
Clam-.
to Airborne Surveys. Magnetometer
Radiometr ic
Expenditures (excludes power stripping)Type of Work Performed
Geochemical AnalysisPerformed on Ctaim(s)
See Mining Claims Traversed
ColumnCalculation of Expenditure Days Credits
Total ExpendituresTotal
Days Crecms
$ 4,721.60
InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selectedin columns at right. S ee Attached Sheet
744480 •
744481 /
744482 ,/
744489 v
744490 ^
744491_J/
744492
744493 /
744495 ^
744496 "
74449?. ^
744498 ._<.
744499 ^
744503
744504 ^
744505 _
744546 '
744547 '.
744553 /
744554 _^_
744989._/..
744996 v744997 J
I MH.MH!. Day, Ci.
"AWi .'/A
Mining Claim L xppnd. l'rpti> ; Numliei Days d.
IT
I'//'
729190 Total number o* mining claims covered hy Ihii rcpori ol wor k.
23
Certification Verifying Report ofI hereby certify that I have a personal and intimate knowledge of the farts sri lorili m the Report ol Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed repon is tint
Name and Postal Address of Person Certify'np
_Lorne Burden 27 Hollingworth Dr. Scarborough, Ontario M1P 1E1
1362 ( 81/9)
••* «
Assessment Work Breakdown
Man Days are based on eight (8) hour Technical or Line-cutting days. Technical days include work performed by consultants, draftsmen, etc..
Type of SurveySoil Geochemical Survey
Technical Technical Days Line-cutting Days Credits Days
36 x 1 = 1 252 + 0
No. of Days perTotal Credits Claims Claim
s 252 +23 11
Type of Survey
Technical Technical Days Line-cutting Days Credits Days
X 7 = +
No. of Days per Total Credits Claims Claim
= •*- =
Type of Survey
Technical ' Technical Days Line-cutting Days Credits Days
X 7 = +
No. of Days per Total Credits Claims Claim
= + =
Type of Survey
Technical Technical Days Line-cutting Days Credits Days
X|7 | =
No. of Days per Total Credits Claims Claim
= + =
Expenditure Credits To Be Distributed As Follows:
Mining Claim
K 744462 A 744468 A744483 v744484 >v744486 l744488744494744500744501 <744506744508 -744509 - 744516-744517744518744519744520744521744531744532
Expenditure Days Credit
9104410442
4499
449999999999
315 days credit
Ontario
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
FUe.
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
Type of Survey(s) Fire Assays
Township or Area Napanee Lake_________
Claim Holder(s)____Silver Lake Resources Inc.
Suite 4650. T.D. Bank Tower
Survey Company_
Author of Report Lome Burden
Silver Lake Resources Inc.
Address of Author 27 Hollingworth Dr. f Scarborough
Covering Dates of Survey July 1/84 to Sept. 15/84(linecutting to office)
Total Miles of Line Hut 110.5_______________
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.
ENTER 20 days for each additional survey using same grid.
Geophysical
Electromagnetic.
Magnetometer
Radiometric
Other______
DAYSper claim.
Geological.
Geochemical.
AIRBORNE CREDITS (Special provision credit! do not apply to airborne lurveyi)
Magnetometer. .Electromagnetic.(enter dayi per claim)
HATE- June 20/85 SIGNATURE:
. Radiometric
eport or Agent
Res. Geol.. .Qualifications.
Previous Surveys File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
K 744452'(prefix)'
744453
K 744996(number)
744997
744455 744998
744461 745003
744463
.......7MM....................7.A5.QL4............
.......7A4M2.....................7.A5Q2Q.........
.......7A4.4.9.5.....................7.A5Q22.........
.......7.4449.6.....................7.A5Q29.........
.......7.4449.7.........................................
.......7.445.Q4........................................
.......7.445.44........................................
.......7.445.48........................................
........7.445.5.L........................................
........7.44552........................................
........7.445.5.3.........................................
........7445.54.................... ....
......7-4497.7..
744990
744991
TOTAL CLAIMS. 32
837 (6/79)
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS — If more than one survey, specify data for each type of survey
Number of Stations. Station interval __ Profile scale____
.Number of Readings _Line spacing ____
Contour interval.
Instrument.Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ___
Instrument
ELECTROMAGNET*Coil configuration
Coil separationAccuracyMethod: Q Fixed transmitter D Shoot back Q In line FrpnupT-y
' ' (specify V.L.F. nation)
CD Parallel line
Parameters measured.
Instrument.
Scale constantCorrections made.
^ Base station value and location.
Elevation accuracy.
Instrument ————————— Method CD Time Domain Parameters — On time ———
- Off time __— Delay time ___— Integration time
I I Frequency Domain _ Frequency ____ _ Range _______
Power.Electrode array — Electrode spacing. Type of electrode
SELF POTENTIALInstrument______ Range.
Survey Method.
Corrections made.
RAD1OMETRIC
Instrument___Values measured.Energy windows (levels). Height of instrument__ Size of detector_____Overburden ________
.Background Count.
(type, depth - include outcrop map)
OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey___________________________
Instrument _________________________ Accuracy_________________________Parameters measured.
Additional information (for understanding results).
AIRBORNE SURVEYS
Type of survey(s) ——— Instrument(s) —————
Accuracy________(specify for each type of survey)
(specify for each type of lurvey)
Aircraft used.Sensor altitude.Navigation and flight path recovery method.
Aircraft altitude.Miles flown over total area.
.Line Sparing
.Over claims only.
GEOCHEMICAL SURVEY - PROCEDURE RECORD
Numbers of claims from which samples taken.
Total Number of Samples. Type of Sample.
(Nature of Material)
Average Sample Weight——————— Method of Collection————————
Soil Horizon Sampled. Horizon Development. Sample Depth———— Terrain—————————
Drainage Development——————————— Estimated Range of Overburden Thickness.
ANALYTICAL METHODS Values expressed in: per cent
p. p.m. p.p.b.
DnnCu, Pb,
Others_
Zn, Ni, Co, Ag, Mo, As.-(circle)
Field Analysis (.Extraction Method. Analytical Method- Reagents Used——
Field Laboratory AnalysisNo. (__________
SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)
Mesh size of fraction used for analysis____
Extraction Method. Analytical Method. Reagents Used__
Commercial Laboratory (_ Name of Laboratory_ Extraction Method—— Analytical Method —— Reagents Used ____
.tests)
.tests)
.tests)
GeneraL General.
Ontario
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
File.
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
Type of Survey(s) GeochemicalTownship or Area Napanee Lake _________Claim HnlHer(s) Silver Lake Resources Inc.
Suite 4650. T.D. Bank TowerSurvey Company Silver Lake Resources Inc, Author of Report Lome Burden__________Address of Anthnr 27 Hollingworth Dr. f ScarboroughCovering Dates of Survey July 1/84 to Sept. 15/84
(linecutting to office)
Total Miles of Line Cut. 110.5
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
Geophysical-Electromagnetic.-Magnetometer_-Radiometric——-Other______
DAYSper claim.
Geological.Geochemical.
AIRBORNE CREDITS (Special proviiion crediu do not apply to airborne §urvey«)
Magnetometer. .Electromagnetic . Radiometric
DATE- June 20
(enter days per claim)
SIGNATURE:
Res. Geol.. .Qualifications.Previous Surveys
File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
K 744480 K'jp'refixj'
744481(number)
744482744489.7.44490.
744491• •••»•••••• •••••••••••*•• •••^•••••••••••••••
744492•••••!**•*«v*t**r*««t««*ti*«i*»**t«*»*««*i*«i
744493•••*••<•*>•>•>*••••»•*•*»•••»•»••••*•••****••
744495• ••*•• t • »\rtrt f»Tk i ••••*t•*•*•»••*• i •••*»t••*
744496••••»••••%•%•% r» n ••••••i•••*••••••••••*•••t*
744497•t•* I•I•!%•%§% ril»«»»**»»i»«»»»#«»»»»««i»»*»»
.7.4.^9.9..,
......7.4A5.0A.
......7.4A5.Q5..
.......744546.
..744554.744989
744996
TOTAL CLAIMS. 23
837 (6/79)
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS — If more than one survey, specify data for each type of survey
Number of Stations————————————————————————Number of Readings Station interval __________________________Line spacing_____Profile scale_______________________________________Contour interval.
C
1
u
Instrument.
Accuracy — Scale constant, Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ___
Instrument,(iZ
Coil configuration
Coil separation _______________________________________________________ Accuracy.—————————————————————————————————————————————————————_____ Method: d Fixed transmitter CD Shoot back CD In line CD Parallel line
Frequency.—————————————————————————————————— ^ (specify V.L.F. nation)
Parameters measured_______________________________________
Instrument.Scale constant.Corrections made.
iol Base station value and location,
Elevation accuracy.
Instrument _________________________________________________________2 Method D Time Domain D Frequency Domain
P Parameters — On time_____________________________ Frequency ————< s5
—Off time__________________________ Range.— Delay time ——————————————————————————
— Integration time ______________________________
Power.UD Electrode array —Q5 Electrode spacing.
Type of electrode
SELF POTENTIALInstrument——————————————————————————————————————— Range. Survey Method ———————————————————————————————————————————
Corrections made.
RAD1OMETR1CInstrument ___Values measured.Energy windows (levels) _____________________________________ Height of instrument____________________________Background Count. Size of detector__________________________________________ Overburden _____________________________________________
(type, depth - include outcrop map)
OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey_______________________ Instrument ————————————————————————— Accuracy__________________________Parameters measured.
Additional information (for understanding results).
AIRBORNE SURVEY^ Type of survey(s) ——— Instrument(s) —————
(specify for each type of $urvey) Accuracy_________________
(specify for each type of survey) Aircraft used.________________________________
Sensor altitude.Navigation and flight path recovery method.
Aircraft altitude_____________________________Line Sparing Miles flown over total area________________________Over claims only.
GEOCHEMICAL SURVEY - PROCEDURE RECORD
Numbers of claims from which samples See Mining Claim Traversed
Total Number of Samples—Q J 1
Type of Sample.
459
(Nature of Material)Average Sample Weight——————— Method of Collection——shnve.1—
1.5 Ibs
Soil Horizon Sampled. B horizon
Horizon Development——.—i—— Sample Depth. 4 ~ 8 inches
Terrain———— undulating
Drainage Development———8°Estimated Range of Overburden Thickness. __________thirty feet______
SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)
Mesh size of fraction used for analysis -80 mesh
ANALYTICAL METHODSValues expressed in: per cent
p. p.m. p. p. b.
n n
Cu, Pb,
Others_
Zn, Ni,
Au
Co, Ag, Mo, As,-(circle)
Field Analysis (- .tests)Extraction Method. Analytical Method- Reagents Used——
Field Laboratory AnalysisNo. (___________ .tests)Extraction Method. Analytical Method - Reagents Used__
Commercial Laboratory (—————————————tests) Name of T.ahnrat™-y Bell-White Labs Ltd.
Extraction MpthnH Fire assay____________Analytical MptVmH Atomic Absorption_____Reagents II«>H aquia regia
Samples were screened to -80 mesh 10 gram portions of this Fraction were used to produce a dore bead. Pore beadswere redisolved into solution with____ aqua-regia and then tested for gold by
General.
absorpt ion.
LAKE RESOURCES INC.Suite 4650, Box 77, T.D. Bank TowerToronto-Dominion CentreToronto, Ontario M5K 1E7Telephone: (416) 361-0212 ___
June 25, 1985
Ministry of Natural Resources Mining Lands Section Whitney Block, Room 6610 99 Wellesley Street West Queen's Park Toronto, Ontario M7A 1W3
Dear Sirs,
In compliance with Ministry of Natural Resources requirements, enclosed are two copies of two geotechnical reports covering one of our large claim blocks in the Kenora Mining District. Summaries of claim numbers and work performed are listed on the "Report of Work" forms sent to your office by the mining recorder.
Should you require any further information or clarification concerning these reports, please feel free to contact me at the above listed address.
Yours truly,
Lome Burden
LB/cp Encl.
JUH 2 i 1985
Mining Lands Section
Control Sheet
TYPE OF SURVEY GEOPHYSICAL
GEOLOGICAL
I/ GEOCHEMICAL
I/ EXPENDITURE
MINING LANDS COMMENTS:
Signature of Assessor
Date
5 |_'3i»'« (7 >».».+•**•»**745J«7 r 33318 733317
7*3319 I 7SJS20I 7333?! M1*22'M3S23 |
K Ik rf v k k,K, ,'I74»J03
i 746>0«! ' "'<"•' -- V -JY -—; -I- - —_-~ -" •''"'i" --r - - , ...I, _, _L. ,...
i i l <•-44S57 744*9? |/44i4B I 744643
- I . . . ,.._..7449«) T44H4 'M4M*r*»w*» .w«w»4 :7*«»f» ;'"»p ' --'T' 1 . '--••- |.-.»www •
'___ I ______I _V_ I I _ ^ I. 'V"~ IK "^ u""~ PK~TK 'K IK IK IK?460.7 - ! I t I I
745010 74600* M60OS 746007 | '^5006I F49DIZ ' f ^BIWU rI I ' -i „——— — ---•,- ^ K-r i;—- IK . ?. f.K
, Jj 74801? J7450>A|746o)sO 74^'J J7I9596 |r«»8» l9' 744I6O/J M 44M [^ ^ ^ "' "'j 744479 ' ^ * . ' ̂ 3«*l| /./^ '^ ' * [ "
~~~~" ' --- — |- V/ ' . p^ '---*,. ' ' "*,,Lvr***** "744/4«t>_J_ fy 7444«f | M44I4 "? 74J4462 I 7444J|*t '*<*''• <74'
.0,. mo».| ,74.ose ,„„« |«, 1 -- -.._ ^———— —— J..-. 1_
—— T2960I __— 4.- —» — ^~
729816 7 29BIT . '729818l"".!!-*9*^t t I .
————J Jr- — -J^— — -4 —
*M»,'^,i-- ,r ' r, " ^ t " ,' ' r 'SJ y "T;?' " 1" ..»***( /" n^w r ~"~.' s " \ — — - •• ••- — -—
^^ ^ I *.! * * • ^ />' M ' ' '^f j^^'^^l^'f^^l^A .Kf^Il^MV^!^^1 ., /T«- n - --, ^~ 1 - -Ji-^J,L-- -— J-- ---
-I- i ,«fi i ' .'i .1
_
'j^trtS^^^ '_ •/ J. — —. Jt *•»,«* k»— r- -«| ^— —4—1 — — — — — - — r— - — —— — - _
-17- l • 1 1 ' |rm«i> i ,h- "• >X• / (-*:
-/r- - ,--.",>-
,_• ' r w« • "*w-^ |
7~ ~!r 7 "r ««6J, T^J/Mt I ^" * "'* " '
, 'V ' r«i ' J, ' C^A»7tMii l !r/8*H<!'»»M4 ,*I4«»
- - - • "
-*H uIMMT US6837 , KV- -4 - - -r- ^l'.! 7 ,1"^
k n<— T-,. !-•-£.
74»||t 1^41174 I Mil? I l?4«
- /ri|» |7<''* | 7/'.S'. 72J|.,.' 7?MSI ^ •»—' —— f— "f ^ "' **•**" • r » *•"• -^k. -*^ .
U i TMT. '^r?ij ' *'* " ^"r **^^" "* "^' K • K ^ K **t'
LEGEND
. t fM L iM r. I f>WNSniP«, HAS. Mlii' \,11V, . .. i v
DISPOSITION OF CROWN LANDS
I VPt ()• l>Ot UMI N
i - a o N ' • '•! -v i i -c •-'Ml ."., I ci, ... i
MlNiN, . '
I f A',1 H' A( I 1, V '.IN'.
'll l( I \ I I K .
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REFERENCESAMI AS WMMMHAiVN MU)M I JlsMDSI f It »N
c-i ' - f n
^
SCAl t 1 lN(,H 411 ( MAINS
AH( A
NAPANEE' LAKEM N « «, 1M! NISI HA' u t US I K'" »
FORT FRANCES
KENORAI AND ' ' ' i f . " » ' • ' M < '' 'V i ' i'»n
KENORA
I'3 84 N i
G-2690
saFa3NEMI7 Z.8246 NAPANEE UAKE
•^^^^^^^"r200
t t * t t t 0 SILVER LAKE-DEL NQRTE JO
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N^Vlf 744493 *Ntf'j>*
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j." 744504 * Nx/" !V> - X-*
Grant L o K
t tINT VENTUREcT
Manitou Straits Property
Location Map40 Mll«S
Silver Lok«-Del Norte Joint Venture
Lower Manitou Lake
West Sheet
INDEX MAP
Eyelid Lake
Sample location Sample number
2 Au value ( ppb)
Silver Lake Resources Inc.MANITOU STRAITS
PROPERTYDistrict of Kenora, Ontario
N.T.S. 52F/3
EAST SHEET SOIL GEOCHEMISTRY
GOLDScale : 1 inch =400 feet (1:4,800)
ft. 400 0r 1600ft.
Checked By : L. Burdtn
Drawn By J. Meik
Date : June 1985 PLAN * J
V —V *-
V *-V —
64-100 N
60 + OCN
56+OON
TL 52tOO
48tOON
44 tOO N
40tOCN
36TOC N
26tOO N
E _ 2€+OC N
24 - OC N
2CtOO N
16 *OC N
IZ'OC N
06+OCN
04fOON
00
Syndicate Lake
traits Property
Location Map40 Miies ,
Silver LoKe-Del ^tort« Joint Venture
INDEX MAP
Lo*er Monitou Lake
2 MILES
— TN —
LEGEND
Sompie location Sample number
>4 A u volue (ppb)
Silver Lake Resources Inc.MANITOU STRAITS
PROPERTYDistrict of Kenora, Ontario
N.T.S. 52F/3
WEST SHEETSOIL GEOCHEMISTRY
GOLDScale : 1 inch = 400 feet (1:4,800)
ft.AQQ_______0 1600ft.
Checked By : L. Burden
Drawn By J.Meek
Date : June 1965 PLAN
Location Map
}, X S0878.76
i Mode Metu«olcoinc Hock! 0l> pillomdc Qmygduloidol*d voiculort porphynhcI amphitioiiiixdg mrongiy lohnitdh crytlnl lulli o»h luffI lupilh lullk tutf brtcciaI chionli 11 hit
2 Inlarinediat* 10 Ftlnc Milovolconic Rockt
b fdUSPQr [ini [ dyi yL guuiK ftldtpard riyjiol lu(»f> u»h luffI lopilli lutlg I offn chtrt militia* )«dim«nt«
Aii»r«d Mtiuvolconica I4ncii«b quortt tvriciu «chlit
Mafic lntrmiv«jab Qjutlt gabbrac dionlt
lnlc u «iv»< a oplitt
beunaory
•ubdivition boundary
rack outcrop
joint! llntl 5 Uip
fohuhon
, (HllO* t opi
lOSSO ,or k tempi*
'WVX . h.ar , un .
v U two m u
Silver Lake Resources Inc.Spruce Pine
MANITOU STRAITSPROPERTY
District of Kenora, Ontario N.T.S. 52F/3
GEOLOGY
Scale 1 Inch -200 feet (1.2400)
2 8216 NAPANEE LAKE
-_ y-
Spruce I- Pme
Spruce-Cedar
I Mof.c Mulavolcamc Hackt a muttitft 0c omygduloidal d vtiicular • parphynlic fg strongly foliartd ti cryilal lutl i o«h luff I lopilli li luff brtccia
chloriU
2 murmtdiatt Io f«i«ic M*iovolcaniC Rock*
b feldspar porphyryc Quarlt ftldtpor porphyryd irylial luff« o»h lufff I'lpllll tutf(I tulf brtccia hSpruce '- PineSpruce '- Cedar
3 antrid Mtlavolconic Rocktichiti
t> iiuurii ttncll* «chl»t
Mafic Intruti'** o QQbbro h qucirU flobbro c dioni*
5 HUic Inlru«iv4< a aphlf
tubdl«itiun boundary
rock outcrop
|omi| «|rikf tt dip
foliation dip
plong*
I0p«
, 0 c
i Spruce - Cedar
•WVX sh.o, rat,,
• « o m p
Spruce - 'Pine
55°Sllcktntid*
Plung. , |Q
Silver Lake Resources IncMANITOU STRAITS
PROPERTYJOS60
' 3OS6I
I, , 4UQrtt f|«ot W maioeMi, District of Kenora, Ontario
N.T.S. 62F/3
MAP* 2
GEOLOGY
6£F»3NE«iei7 2 8246 NAPANEE UAKE 240
Location Map
SILVER LAKF -DEI NORTF
r omygdjluiduld vtnculora porphynfic' umphihohhitd0 Mronglir lulioltd
cryitol l ull i osh tuft I lopilli lutf k luff bneeio I chlarit*
iniennMiot* in F«Uic Mtlavolconic
o^ f«ld«par porphyrye quarti ftldipnr porphyry
• 0 |h luff f Inpiih luff 0 'uff brtccia
c h«rt inltrflow »«Jim«nl«
5 Aiitrtd Mclovolcanic Roc«« 0 Itncil* ichltl b quurK »ncil« tchltl
4 Malic I nlrunvti ub qugru gabbro c dioril*
f»\tit. I ntrutivit a ophlt
""""""" "^ •ubdlvuion boundary
','' / ^ I^SOSRJ/f.i.,e / t-A <'tuffj y( \ f
Silver Lake Resources IncMANITOU STRAITS
PROPERTYDistrict of Kenora, Ontario
N.T.S. S2F/3
MAP* 3
GEOLOGY
52P»3NE»ei7 2 B24B NAPAFCE LAKE £B0
Grant L O M e
30608.06 tr malaehit* tr choicepyrlt*
Eyelid Lake
S2F»3NE««I7 2 62-16 NAPANEE LAKE
1 Mode Mtlovolcome flock*o mottlv*b piiloxdc amygduloidald v»*lculqr• porphyrilie' omphiDOliUMdg ilrangly folialidn cryital luffi o»h luflI loplll! tutfk luM DrtcclaI chlorit* )chn1
2 lnl«rm«dlol« 10 Filtic Mtlovolconic Rock*a mastiv* b ftldspor porphyry c quart! Uldtpgr porphyry d crytlol Igff• oih tuffI lopllli tuffg tuff brtcciari chtrt inltrtloM iidim«nt«
3 Alltrtd M*lo«olconlc Rock* a itricit* ichlit b quart! itriell* tchitt
4 Mafic Intrutivti o gabbra b quortt gobbro t d ionl*
5 Ftlilc Intruiixt a aplilt
Symbol*
dip
X SO669
• geological boundary
' lubdlvltion boundary
rock outcrop
joint* itnk* t»
fAliOtiort dip
piling*
pillow topi
raek tampl*
'MVW ihtor ton*
• «omp
Silver Lake Resources Inc.MANITOU STRAITS
PROPERTYDistrict of Kenora, Ontario
NTS 52F/3
GEOLOGY
II ?00I I .1
CTMCk*d ByL BURDEN
Drawn ByJ MCtKSASSOC
Dtte FEB 1985
PLAN*
