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WESTERN TROY CAPITAL RESOURCES INC.
1992 EXPLORATION PROGRAMME ON
THE MENARY TOWNSHIP AREA PROPERTIES
KENORA MINING DIVISION
ONTARIO
prepared by:
Christopher A. Wagg Wayne E. Holmstead
January 31, 1993
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, 52FCMSW0002 2.15292 MCLARTY 01 0 P
FABLE OF CONTENTS
INTRODUCTION ........................................... 1
PROPERTY DESCRIPTION .................................... 3Location and Access ..................................... 3Claims and Ownership .................................... 4
REGIONAL GEOLOGY ....................................... 5
PREVIOUS WORK .......................................... 7
1992 EXPLORATION PROGRAMME .............................. 9Geological Mapping .................................... 10
Mafic to Intermediate Metavolcanics ...................... 12Felsic to Intermediate Metavolcanic Rocks .................. 13Granitic Intrusive Rocks ............................. 14Mafic Intrusive Rocks ............................... 15Overburden Geology ................................ 15
Prospecting and Sampling ................................. 16North Property ................................... 17South Property ................................... 19
Mechanical Outcrop Stripping .............................. 21Dillman Shear Zone Showing .......................... 21Dillman 1 and Dillman 2 Showings ........................ 21Agassiz West Showings .............................. 22Wagg North Area .................................. 23
Diamond Drilling ...................................... 25Bulk Sample ......................................... 26
DISCUSSION ............................................ 29
CONCLUSIONS ........................................... 32
RECOMMENDATIONS ...................................... 34
BIBLIOGRAPHY .......................................... 35
CERTIFICATE ........................................... 36
Appendix 1: Appendix 2: Appendix 3:
Assay Results Diamond Drill Logs Metallurgical Report
APPENDICES
FIGURES
Figure 1. Property LocationFigure 2. Location of Claim groupsFigure 3. Regional GeologyFigure 4. Lithostratigraphic Subdivisions of Metavolcanic RocksFigure 5. Gold Showings and 1992 Mechanical Stripping LocationsFigure 6. Dillman Shear Zone, Geology and SamplingFigure 7. Dillman #1 Gold Showing, Geology and SamplingFigure 8. Dillman #2 Gold Showing, Geology and SamplingFigure 9. Agassiz West Gold Showings, Trench 1Figure 10. Agassiz West Gold Showings, Trench 2Figure 11. Agassiz West Gold Showings, Trench 3Figure 12. Wagg North AreaFigure 13. Bulk Sample Trench Plan
TABLES
Table 1. Original Claim Group InformationTable 2. New Claim Group InformationTable 3. Lithologic Units
MAPS
Map 2. Geology: Northern Property, West Part and Southern Property, North PartMap 3. Geology: Southern Property, South PartMap 5. Sample Locations: Northern Property, West Part and Southern Property, South
Part Map 6. Sample Locations, Southern Property, South Part
Claims and Ownership
The northern claim group, which includes the original property, consists of 140 contiguous units covering a portion of the townships of Menary, Claxton, McLarty, and Senn. The southern claim group consists of 75 contiguous units covering a portion of Menary and Potts Townships. (See Figure 2)
All mining claims presently held by Western Troy in the vicinity of Menary Township are unpatented mining claims on Crown Land except for claim 1079876. This claim was surveyed in the spring of 1992 and an application to bring the claim to lease was made on September 13, 1992. The company holds a 100% interest in the claim groups subject to a 3% Net Smelter Return, and all claims are presently in good standing with regard to assessment work requirements.
The group of thirty claims which were recorded in 1989, and which were the subject of the 1989 and 1991 exploration programmes, were not substantially re-examined during the 1992 reconnaissance programme. These claims have been included in the Tables below, however, because a limited amount of follow-up sampling was completed in several areas where 1991 work had returned anomalous gold or base metal values. In addition, mechanical stripping and bedrock sampling was undertaken on two of the claims after the completion of the reconnaissance portion of the present programme.
OGS Study 56 — Map 2Western Troy Properties 49°00'
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Felslc Intrusive Rocks
Intermediate Intrusive Rocks
Mafic and Ultramaflc Intrusive Rocks
Clastic Metasedlmentary Rocks
Felslc to Intermediate Metavolcanlc Rocks 20km
vw Mafic Metavolcanlc Rocks
Figure 1. Property Location
McLarty Twp.Claxton Twp
N o r t h\ e r n Prooert
Menary Twp.
Original Property
Batholith/ MaficMetavolcanics
Southern.-•Property
kilometres
Fleming* Twp.Figure 2
Little Pine Lake
Location of Claimgroups
Road Trail Power line
_ _ — Geological contact
TABLE 1: ORIGINAL CLAIM GROUP INFORMATION
CLAIM # UNITS DATE RECORDED109263310926341092635109263610926371092638109263910926401092641112025811202591120260112026111202621120263112026411202651120266107986810798691079870107987110798721079873107987410798751079876107987710798781079879
111111111111111111111111111111
17-Jan-8917-Jan-8917-Jan-8917-Jan-8917-Jan-8917-Jan-8917- Jan-8 917-Jan-8917-Jan-8907-Jul-8907-Jul-8907-JU1-8907-Jul-8907-JU1-8907-Jul-8907-JU1-8907-JU1-8907-JU1-8907-JU1-8907-JU1-8907-JU1-8907-JU1-8907-JU1-8907-Jul-8907-JU1-8907-Jul-8907-JU1-8907-JU1-8907-JU1-8907-Jul-89
TOWNSHIPMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARY
TOTAL 30 CLAIMS
TABLE 2: NEW CLAIM GROUP INFORMATION
NORTH CLAIM GROUPCLAIM
1149481114948211494831149484114948511494861149487114948811494891149492114949311494941149495114949611494971149498114949911495001149501114950211495031149504114950511495061149509114951011495121149513
TOTAL
# UNITS1111111128442933422
1222
121622
101
110
DATE RECORDED09-Jul-9109-JU1-9109-Jul-9122~Oct-9122-Oct-9122-Oct-9122-Oct-9122-Oct-9122-Oct-9l22-Oct-9112-NOV-9112-NOV-9112-NOV-9112-NOV-9112-NOV-9112-NOV-9112-Nov-9112-NOV-9112-NOV-9112-Dec-9112-Dec-9112-Dec-9112-Dec-9112-Dec-9112-Dec-9112-Dec-9129-Jan-9229-Jan-92
CLAIM UNITS
TOWNSHIPMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARY-CLAXTONCLAXTONCLAXTONCLAXTONMENARY-CLAXTONCLAXTON-MCLARTYMCLARTYSENN-MCLARTYMCLARTYMENARYSENNSENNSENNSENNSENNCLAXTONCLAXTONMENARYMENARY
SOUTH CLAIM GROUPCLAIM
1149514114951511495161149517114951811495201149529114953011495211149522
TOTAL
TOTAL ALLGROUPS
# UNITS448
10161212621
75
215
DATE RECORDED07-Feb-9207-Feb-9231-Jan-9231-Jan-9231-Jan-922 3 -Apr-9 218-Jun-9209-Jul-922 3 -Apr-9 223-Apr-92
CLAIM UNITS
CLAIM UNITS
TOWNSHIPPOTTSPOTTSMENARYMENARYMENARYMENARYMENARYMENARYMENARYMENARY
REGIONAL GEOLOGY
The Western Troy properties are situated along the margin of a greenstone belt which forms part of the Wabigoon Structural Subprovince of the Archean shield. As is typical of most greenstone belts in this district, the grade of metamorphism within volcanic rocks increases from lower greenschist facies in the middle of the belt, to lower amphibolite facies near the felsic intrusions at its margins (Blackburn 1976).
As shown in Figures 1 and 2, the metavolcanic rocks trend northeasterly between two large intrusive complexes. The Sabaskong Batholith, in the northwest, is broadly trondhjemitic in composition, while the Jackfish Lake Complex, in the southeast is predominantly syenodioritic. The metavolcanics maintain their trend northeast of Burditt Lake, eventually merging with the Pipestone Lake and Kakagi Lake greenstone belts in a "Y"-shaped junction approximately 10 kilometres north of the boundary of Figure 2.
The regional geology, depicted in Figure 3, lies within the area covered by Ontario Division of Mines Geoscience Report 140, and Map 2325 at a scale of 1 inch to 1 mile, (Blackburn, 1976). To the northeast, 1 inch to 1/2 mile mapping was completed by the Ontario Geological Survey in 1975 (Edwards, 1981).
Blackburn's work has identified four felsic stocks which intrude the metavolcanics within the area of Figure 3. These are the late tectonic Burditt Lake, Finland, and Black Hawk stocks, composed of quartz monzonite and granodiorite, and the small, syntectonic body of monzonite at Beadle Lake. An intrusive breccia, which typifies the syntectonic intrusive, occurs sporadically along a lineament extending northerly from the monzonite to the contact of the Sabaskong Batholith.
In the vicinity of the properties the metavolcanic succession has been interpreted to be homoclinal and southeastward facing, and to consist of two distinct cycles (Blackburn, 1976). An upper sequence of mixed mafic to felsic metavolcanics overlies an older sequence of massive, pillowed, and porphyritic mafic flows. The lower sequence is host to numerous dykes, sills, and small stocks of felsic porphyry, believed to be have been emplaced concurrent with the second cycle of volcanism.
The metavolcanic stratigraphy has been further subdivided by Blackburn (1976) into a number of geologically distinct zones, as shown in Figure 4. Each zone is characterized by one or more predominant rock types. Both Western Troy properties encompass a portion of each of the five zones constituting the lower volcanic cycle, and a small portion of the upper cycle, Fl felsic zone is included in the easternmost claim of the northern property. Each of these zones will be discussed in further detail later in this report.
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Dinbase Dike _Quartz Moozonito Figure 3 . R egional GeologyTronctijcmi tcHonzonitc after Blackburn, 1976.Syeoodiori tcFctsic HctovotconicsMafic Hctovolconics
Claim Block Geological Contoct Fault Rood
cO Lake
10 I ? 3 4 5
Figure 4 -Zonal distribution of metavolcanic rocks, Off Lake-Burditt Lake area.
after Blackburn, 1976
Northwest trending diabase dykes postdate regional metamorphism and all felsic intrusive activity. Northeast-southwest shearing likely accompanied dyke emplacement, as indicated by the minor offsets of some dykes along northeasterly trending lineaments.
Unconsolidated Pleistocene deposits, consisting of boulder and cobble dominated sandy tills, occur as a thin discontinuous layer of bedrock cover in the area northwest of Burditt Lake. Sands and clays are present in minor amounts in low lying, well drained areas. Recent sediments consist of organic debris which has been accumulating in swamps and bogs.
PREVIOUS WORK
The first recorded exploration work in the region dates from the 1930's, when a copper-gold showing was discovered in a metavolcanic xenolith within the Jackfish Lake Complex. Sporadic diamond drilling, which has been carried out since the mid 1950's in search of base metals, has been directed primarily toward chalcopyrite mineralization in felsic metavolcanic rocks. No mineral production had been recorded from the Off-Burditt Lake area prior to 1992.
A reconnaissance overburden geochemistry programme was completed in Off-Burditt Lake area and surrounding region by A.F. Bajc, and the results published in 1988 by the Ontario Geological Survey. Till samples returning anomalous gold grain counts are located on and adjacent to the property.
An airborne magnetometer and VLF-EM survey, which covers portions of topographic map sheets 52C/13 and 52F/4, includes the Off-Burditt Lake area. The survey was flown for the Ontario Geological Survey, and the maps published in 1990. Most of the conductors shown as occurring within the boundaries of the Western Troy properties have been investigated to some degree by previous operators or the current property owners. The work has revealed numerous zones of stratabound pyrite-pyrrhotite mineralization locally containing several percent sphalerite and chalcopyrite (Wagg and Holmstead, 1991).
Within the boundaries of the Western Troy properties, the only significant previous exploration work was undertaken during the early 1970's and 1980's.
In 1974, Hudson Bay Exploration and Development drilled two diamond drill holes totalling 509 feet near the northwest corner of current claim 1120265, within the gridded portion of the property. The holes intersected pyrite, pyrrhotite, minor sphalerite, and trace chalcopyrite across ten feet (Sullivan, 1974).
Between 1983 and 1985, Agassiz Resources explored claims on and around the gridded portion of the current property in search of base metals. Magnetometer, VLF-EM, geological, and bedrock geochemistry surveys were completed, and follow-up horizontal loop (EM) work and overburden stripping examined disseminated sulphide mineralization associated with tuffaceous horizons Studemeister, 1985). The Agassiz gold showing was discovered during this programme.
An initial group of thirty claim units, located in the northeastern portion of Menary Township, was geologically mapped and covered by ground magnetometer and VLF-EM surveys during 1989 by Western Troy. A follow-up programme of prospecting and geophysical anomaly investigation, initiated in May of 1991, resulted in the discovery of three zones of native gold bearing quartz veins early in the year.
Additional claims were subsequently staked in order to expand the company's land position around the most prospective of the new showings. Two additional zones of gold bearing veining were discovered on the new claims shortly after staking began (Galbraith A and B gold showings). Meanwhile, a stripping and sampling programme underway at the Wagg showing was revealing the presence of high-grade native gold mineralization. The stripping uncovered six somewhat interconnected bodies of quartz which appear to be the result of folding and faulting of a single larger structure (Wagg and Holmstead, 1991). Claimstaking has since been extended in both directions along the strike of the batholith contact, for a total distance of about 18 kilometres around the initial discoveries.
1992 EXPLORATION PROGRAMME
The 1992 exploration programme was conducted by C.A. Wagg (geologist), Mr. Robert Dillman (geologist) and Mr. Mel Galbraith (prospector) under the supervision of W.E. Holmstead. The reconnaissance mapping and prospecting portion of the programme was completed from early May to August.
The mechanical stripping portion of the programme was completed in August. Five separate gold showings were stripped, mapped, and sampled. A skidder mounted backhoe, owned and operated by Norman Alexander of Stratton, Ontario, was employed.
A bulk sample consisting of 250 tons was extracted from Veins A, D, DE and F of the Wagg Showing on Claim 1079876 and three short diamond drill holes were drilled by Nighthawk Diamond Drilling in the vicinity of Vein F at the Wagg showing in order to define tonneage for the bulk sample programme.
Geological Mapping
The reconnaissance mapping phase of the 1992 exploration programme commenced in early May on the northern Western Troy claim block. As mapping and prospecting were carried out concurrently, regularly spaced, linear traverses were not the rule. Instead, the property was divided into a series of blocks separated from each other by topographic features such as roads, powerlines, creeks, and bodies of water. Within each block, an attempt was made to examine all significant bedrock outcrops. Important geological contacts or units were frequently traversed at right angles, or were more commonly traced along strike, in order to ensure the accuracy of their placement.
Adequate control on the placement of outcrops on maps was achieved by means of pace and compass measurements from notable topographic features or claim posts, or by means of direct observation of topography, using both air photos and contoured 1:20 000 scale base maps derived from air photos. Outcrops were plotted in the field directly onto 1:20,000 scale base maps, produced by the Surveys and Mapping Branch of the Ontario Ministry of Natural Resources, and published in 1984.
In general, mapping progressed from west to east across the northern claim group, and from northwest to southeast across the southern claim group. Table 3 presents a list of the lithologic units which were encountered, and Maps 1 to 3 display the geology of the properties. The legend used on the maps was modified only slightly from that developed by Blackburn (1976) for the Off Lake -Burditt Lake Area.
10
Table 3: Lithoiogic Units
PHANEROZOICPleistocene and Recent
till, sand, gravel, clay, organic debris
UnconformityPRECAMBRIAN
Proterozoic
Mafic Intrusive Rocks
Diabase dykes
Intrusive Contact Archean
Intermediate to Felsic, Syntectonic, Intrusive Rocks
Equigranular trondhjemite, granitic dykes, equigranular monzonite and intrusive breccia
Intrusive Contact
Felsic Metavolcanic Rocks
Medium grained to porphyritic rhyolite and dacite, quartz feldspar porphyry dykes
Mafic to Intermediate Metavolcanic Rocks
Fine to medium grained basalt and andesite,gabbro, pillowed basalt, porphyritic basalt,pillowed and porphyritic basalt, pillowed variolitic basalt, spheruliticbasalt, tuff, tuff breccia, and lapilli tuff
11
As Maps 1-3 illustrate, the subdivision of the metavolcanic rocks into the zones shown in Figure 4 is a logical and practical way of describing the metavolcanic succession. Each of the zones found on the properties constitutes a coherent block of metavolcanic strata, differing markedly from the zones adjacent to it. Compositional and textural variations within each zone are either negligible, as in zones M2 and M4, or are on such a scale that detailed mapping of individual flows would be necessary in order to further subdivide the zone, as in the Ml, M3, and M5 zones.
Top determinations by Blackburn (1976) and others indicate a younging direction to the southeast. No unconformable relationships were observed, either within or between zones, during the mapping. Foliations in the metavolcanics generally strike between 210 and 230 degrees, with dips varying from vertical to 70 degrees southeast. To the south of Little Kishkutena Lake, foliations vary considerably as the Sabaskong Batholith is approached, tending to parallel the contact in its immediate vicinity.
Metamorphic grade within the metavolcanics appears to be in the range of upper greenschist to lower amphibolite facies across most of both groups of claims. Pervasive chloritization observed near Burditt Lake on the northern property, and throughout most of the southeastern half of the southern property, indicates a grade of mid to lower greenschist facies in these areas. No major folds or faults were observed during the reconnaissance mapping, other than the previously known fault trending northwesterly through the southwest corner of claim 1149520. Conclusive evidence of two separate deformational events was observed at only one location, in the southeast corner of claim 1149521, west of Beadle Lake. Here, a foliation in chloritized gabbro of the M4 zone strikes northeasterly at 40 degrees, and dips subvertically to steeply southeast. An S2 fabric, consisting of a crenulation in the SI foliation, strikes 85 degrees and dips southerly at 80 degrees.
Mafic to Intermediate Metavolcanics
The Ml zone underlies a portion of four claim units in the northwestern corner of the southern property, and underlies about half the area of the northern property, where it occurs as a two kilometre wide band over about six kilometres of strike length. This zone is characterized by thin, fine to medium grained, pillowed and massive flows.
Medium to coarse grained massive units, likely representing metamorphosed, subvolcanic stocks and sills, were encountered in this zone on both properties. Fine grained, pillowed flows exhibit variable degrees of stretching parallel to the northeasterly regional foliation trend. Poorly developed variolitic textures were observed relatively frequently in the most northwesterly pillowed flows on the northern property, but were not observed on the southern property. Mafic to intermediate volcaniclastic rocks, ranging from agglomerate to tuff, occur as thin units near the contact with the younger M2 zone to the east.
12
The boundary between zones Ml and M2 is marked by the abrupt transition from non- porphyritic to porphyritic lavas. The M2 rocks are characterized by the presence of 10 to 40 percent subhedral to euhedral feldspar phenocrysts ranging from 1 to 5 centimetres in diameter. The flows within this zone consist primarily of large, undeformed pillows, although massive sections are not uncommon.
The M3 zone is marked on its northwest by the reappearance of pillowed and massive, non- porphyritic metavolcanics. Southeastward toward the boundary with zone M4, pillowed units occur less frequently, and massive units become progressively coarser grained. An amphibolite unit, with several percent fine grained garnet and local migmatitic features, was observed in the central part of the southern property along the boundary with the M4 zone.
The M4 metagabbro zone underlies 50 to 60 percent of the southern property, and less than 5 percent of the northern property. The northern portion of the zone consists entirely of a series of medium grained flows or sills. In contrast, on the southern property, a great many sills and dykes of medium grained felsic porphyry are present within the metagabbro, and massive, pillowed, and spherulitic basalts have been observed in a few outcrops to the south and southwest of Beadle Lake.
The metagabbro is characterized by a spotted appearance on both fresh and weathered surfaces, due to the presence of 30 to 70 percent uniformly sized, evenly distributed, hornblende pseudomorphs after pyroxene. The relict phenocrysts range in size from 1 to 10 millimetres in diameter. In virtually all outcrops of this zone, the groundmass has been completely altered to a fine grained, schistose, chloritic matrix.
The lower boundary of zone M5 is marked by the reappearance of fine grained pillowed and massive flows in the sequence. The zone underlies about seven claim units in the southeastern corner of the southern property, where pillowed, fine grained, and medium grained flows are about equally abundant.
In contrast, the zone M5 rocks on the northern property are predominantly medium to coarse grained, with lesser fine grained, pillowed, and rare pillowed, porphyritic flows occurring along the margins of the zone. As the boundary with the felsic to intermediate Fl zone is approached, poorly exposed mafic to intermediate pyroclastic rocks were observed at several locations within the sequence. Pervasive shearing and chloritization are prominent features of this portion of zone M5.
Felsic to Intermediate Metavolcanic Rocks
The only rocks of this group which were encountered during the survey were found along the shore of Burditt Lake, in the southeastern corner of claim 1149506, on the northern property.
13
In this area, felsic lapilli tuff and medium grained quartz-feldspar porphyries, which may be either sheared dykes or banded flows, occur with minor chlorite rich tuff-breccia.
The contact with zone M5 rocks does not outcrop on the property, but was observed to occupy a linear topographic low about 10 metres wide. Although shearing and chloritization are well developed on both sides of the contact, no sulphide mineralization was observed in the immediate area.
Granitic Intrusive Rocks
Rocks of the Sabaskong Batholith underlie the margin of the northern property along its northwestern and northern boundaries. The batholith's trondhjemitic composition and equigranular, weakly foliated texture, show very little variation across the property. A notable exception to this occurs in the most northwesterly portion of the property, where some assimilation of the metavolcanics has occurred, and no dominant foliation orientation is evident. Contorted mafic xenoliths alternate rapidly with irregular bands of contaminated trondhjemite. The rock was mapped as a granitic intrusive breccia on the northwest of the contact, and as a gabbroic textured hornfels containing numerous felsic dykes to the southeast of the contact.
Narrow, granitic textured, offshoots and dykes, striking subparallel to the metavolcanic- batholith contact are found all across the northern property within a few hundred metres of the batholith boundary.
The only significant zone of alteration found within the batholith is located near the northwest corner of claim 1149506. In this area replacement of mafic minerals .by iron carbonate occurs in association with a northerly trending zone of quartz veining.
Portions of the northern property are underlain by a zone of intrusive breccia, which extends from a brecciated monzonite plug underlying the northern end of Beadle Lake, northerly across claim 1149512 and claims 1149484 to 1149487. In most exposures of this unit, unaltered xenoliths of metavolcanic country rock are separated from each other by an interconnected network of white weathering, granitic textured stringers. The monzonitic groundmass rarely constitutes more than 10 to 20 percent of the volume of the breccia.
On claims 1149484 to 1149487, in proximity to the Sabaskong batholith, the breccia is monolithic, and occurs only in places along a major topographic lineament. On claim 1149512, only a few kilometres north of the monzonite, the breccia becomes locally heterolithic, and occupies a zone 500 to 600 metres in width. Gabbroic xenoliths are predominant at its centre, with pillowed and porphyritic, pillowed, and fine grained massive xenoliths becoming predominant near its margins.
14
Mafic Intrusive Rocks
Post-tectonic diabase dykes occur in a number of areas on the properties. The dykes weather to a brownish-orange colour, and are composed primarily of plagioclase and pyroxene (Blackburn, 1976). Most diabase exposures located during the mapping appear to belong to dykes already identified by Blackburn.
On the northern property, one wide and apparently continuous dyke crosscuts mafic volcanics and the Sabaskong Batholith southeast of Little Kishkutena Lake. A second narrower and apparently discontinuous dyke outcrops on claims 1149483 and 1149512. On the southerly claim the dyke appears to have intruded along the eastern contact between brecciated and non-brecciated metavolcanics. Numerous small, randomly oriented dykes are also present in this area.
On the southern property, a single fairly wide diabase dyke was observed on claim 1149529, near the south end of Beadle Lake. In contrast to those on the northern property, this medium grained dyke weathers a speckled white and brown. Its relatively unaltered subophitic texture is evidenced by radiating whitish plagioclase laths intergrown with grains of relict pyroxene.
Overburden Geology
As Maps 1 to 3 illustrate, outcrop exposure is good to excellent across both properties. Surficial deposits appear to rarely exceed several metres in thickness, other than in areas of extensive swamp. Overburden consists primarily of sandy, boulder and cobble tills, within which locally derived subangular to angular rock fragments predominate. A few areas where abundant sand and gravel were encountered are shown on the geology maps. Clay rich soils of lacustrine origin were encountered only on the southern property in the .vicinity of Little Pine Lake.
15
Prospecting and Sampling
Thorough prospecting of the Western Troy properties was carried out concurrently with reconnaissance mapping from May to August. Although vein hosted gold mineralization was the primary target of the prospecting, sampling included zones of shearing and/or alteration related disseminated sulphides, whether or not any associated veining or silicification was present. Due to space constraints, it was not possible to plot every quartz vein which was observed or sampled on the geology maps. However, over 95 percent of the samples shown on the sample locations maps are from quartz veins, and areas of abundant veining are indicated on the geology maps. (See Appendix 1)
A total of 565 rock samples were collected from the properties, including 143 samples from areas where mechanical stripping was undertaken. Sample locations are shown on Maps 4, 5, and 6 (back pocket). Not alt samples from the vicinity of stripped areas are shown on the maps due to space constraints, however, all samples from these areas are shown in Figures 6 through 12, and are discussed under the heading Mechanical Stripping in the next section. Figure 5 is an index map presenting gold showing locations and identifying areas where bedrock stripping was completed in 1992.
For the purposes of discussion, anomalous sample results are presented in three categories: those from the original (gridded) property, those from elsewhere on the northern property, and those from the southern property. Several areas are mentioned where quartz veins are abundant, but where no gold mineralization has as yet been discovered. Identifying and delineating these areas where hydrothermal fluids were preferentially channelled may allow for a clearer understanding of the factors governing the location of quartz vein and shear zone development. Comparison of areas of barren veining to zones of gold bearing veining may yield valuable data to guide future exploration on the property.
Samples assaying in excess of 1000 ppb (0.03 oz./ton) gold are considered anomalous. Because samples containing native gold commonly show high variability in grade when subjected to repeat analyses, "check" assays were requested for samples returning anomalous gold values. All samples collected during the programme were analyzed by Accurassay Labs, of Thunder Bay, a Division of Assay Laboratories Services Inc. Gold assays were performed using a traditional fire assay with an atomic absorption finish. Samples from sulphide zones where copper or zinc values might be expected to occur, were analyzed for gold by the method mentioned above, and for 29 other elements by the ICAP (geochemical) method.
During the fieldwork, an anomalous sample result warranted a return to the sample site, thorough resampling, and further prospecting in the immediate vicinity. Initial sampling of the most promising appearing quartz veins was generally by means of a selected grab sample, and a representative chip or composite sample. All the samples collected were relatively large, typically weighing 1.5 to 2.5 kilograms, due to tendency of native gold mineralization to be erratically distributed.
16
North Property
Several locations on the gridded portion of the northern property were re-examined in the early stages of the 1992 exploration programme. On claim 1092641 at the roadside vein, a showing discovered in 1991, sample 77694 assayed about 0.36 oz./ton gold across 30 cm from. Grab sample 77773 assayed 1550 ppb gold, from stringers hosted by the same structure. The weakly sheared structure occurs within massive to pillowed metabasalt, and hosts a discontinuous vein which has been traced about 30 metres south from sample 77694. The vein is widest at its north end where the structure disappears under overburden.
Immediately west of the Agassiz West showing, on claim 1092637, two samples were collected from a sugary, fine grained, silicious body. In 1991, grab sampling had returned one value of 1467 ppb from three samples (Wagg and Holmstead, 1991). The highly weathered quartz pod approaches 2.5 metres wide where exposed, and is associated with granitic and porphyry dykes. The two grab samples collected, 77775 and 77776, assayed 945 and 438 ppb gold respectively from weathered quartz containing less than one percent pyrite.
At the Wagg showing on claim 1079876, samples 77735 to 77738 were collected from the "A" vein. The area was previously unsampled due to being flooded during the autumn of 1991.
None of the samples analyzed by ICAP returned anomalous base metal values, from this or any other portion of the property.
Elsewhere on the northern property, preliminary chip sampling at the Galbraith A showing, on claim 1149485 returned one anomalous value of 0.034 oz./ton gold across 0.4 metres. Grab sampling in 1991 had returned values of 2418 ppb and 3.038 oz./ton gold from two separate veins (Wagg and Holmstead, 1991). Seven samples were collected from the area in order to determine if mechanical stripping was warranted. Although the values obtained from the recent sampling are surprisingly low, the veins in the area appear promising, and the presence of porphyry dykes resembling those at the Wagg showing is encouraging. Further work will be necessary to properly evaluate the significance of the showing.
No resampling was completed at the Galbraith B showing, which is located 400 metres north of the #3 post on claim 1149492. The narrow vein/stringer within which native gold has been observed assayed 2.859 and 1.868 oz./ton gold from 1991 grab samples (Wagg and Holmstead, 1991). Many relatively small veins and pods occur within a few hundred metres of the showing, but none of those sampled during the 1992 programme returned anomalous values. One grab sample numbered 77829, which was collected about 350 metres south- southeast of the Galbraith B assayed 1146 ppb (0.033 oz./ton) gold. The sample was obtained from a 1 metre wide, weakly sheared zone hosting several narrow quartz stringers. As both this zone and the Galbraith B vein strike about east-west, further work in the area should pay particular attention to structures crosscutting the northeasterly trend of metavolcanic units.
17
Approximately 450 metres north-northwest of the Galbraith B showing, just north of the south boundary of claim 1149489, prospecting uncovered an odd shaped (stocklike) body of quartz measuring about 2 metres by 5 metres. The body has highly irregular fracture controlled contacts, with many finger-like splays along its north side, and is in contact with a contorted porphyry dyke along its eastern side. The occurrence was named the Galbraith C showing. Of the seven samples collected from the exposure, numbered 8154-8156 and 218853-218856, grab sample 8155 assayed 5050 ppb (0.153 oz./ton) from a grab sample taken near the porphyry contact, and grab sample 218856 assayed 33,267 ppb (1.008 oz./ton) from a grab sample of quartz rubble uncovered about 3 metres south of the exposure. The other samples all assayed less than 750 ppb gold. Traces of pyrite were the only mineralization observed within any of the samples.
Despite spending several days prospecting the area for additional veins, which are common to the areas east and southeast of the showing, no additional anomalous values were obtained. One vein which strikes about east-west, located on claim 1149492 about 250 metres southeast of the Galbraith C showing, displayed virtually all of the characteristics observed in the veins at the Wagg showing. The vein occurs within a variolitic pillowed flow, appears podiform, and is well fractured perpendicular to its contacts. On surface it is sugary to glassy textured, weathers a mottled white to red, and was observed to contain up to 1 percent pyrite and chalcopyrite, with traces of covellite and malachite. Samples 218532 and 218533, however, both ran only about 80 ppb gold.
No other anomalous results were obtained from the sampling conducted on the northern property, although several areas of frequent veining are worthy of mention.
Within the easternmost unit of claim 1149497, numerous northeasterly to northwesterly striking quartz veins are exposed. The largest half dozen range from 0.3 to 0.5 metres in width. The veins in this area strongly resemble those which host gold mineralization elsewhere on the property. About two hundred metres to the north, a small area in the south- central portion of claim 1149495 was also observed to host a number of sugary textured veins of varying widths within pillowed metavolcanics.
Within the east-central portion of claim 1149496, about 400 metres west of the #3 post of claim 1149499, a number of quartz veins of promising appearance were encountered. One poorly exposed vein in the vicinity of samples 8145-8147 was estimated to be up to 2.0 metres wide. This area is located about one kilometre south of the veins in claim 1149497, at the same position in the metavolcanic sequence.
Thin pillowed and massive mafic flows are the most common rock types and are host to the veins in all three areas, while infrequent mafic to intermediate tuffaceous horizons occur nearby, they do not appear to have any direct relationship to the veining.
18
The two more southerly areas are situated just west of (below) the transition from non- porphyritic to porphyritic volcanism. This transition marks the boundary between the Ml and M2 lithostratigraphic zones. All of the showings and areas of barren veining mentioned previously occur within the Ml zone.
The M2 through Fl zones were largely barren of both veining and sulphide zones across the remainder of the northern property. The porphyritic M2 zone and the gabbroic M4 zone were found to be particularly devoid of any features of interest, which may indicate that the more heterogeneous M3 and M5 zones offer a slightly higher potential to host mineralization. No veining, alteration, or sulphide mineralization was observed within the felsic metavolcanic Fl zone.
South Property
On the southern property, a rather similar pattern was observed in the distribution of quartz veins across the various zones in the metavolcanic succession. Quartz veining was found to be most abundant within the Ml zone, which underlies the northwest corner of the property. The M2 zone was essentially devoid of both veining and sulphide zones, and a few quartz veins were found scattered throughout zones M3, M4, and M5.
Aside from the Dillman 1 and 2 showings located in zone Ml, and the Dillman shear zone located in zone M4, all of which are discussed in the Mechanical Stripping section to follow, only two samples returned anomalous gold values. Both samples were obtained from narrow easterly striking quartz veins occurring within the M4 gabbro zone.
Sample 218127 assayed 1123 ppb (0.034 oz./ton) gold from a 5 to 10. centimetre wide stringer located near the south boundary of claim 1149521. No other veins were observed in the area, but an east-west trending swamp-filled valley, located a short distance to the north, may hold some potential.
About 300 metres southwest of the Dillman shear zone, within claim 1149518, sample 218770 assayed 1622 ppb (0.049 oz./ton) gold. The sample was obtained from a small, iron stained, quartz stringer hosted by a sheared quartz-feldspar porphyry dyke. The dyke occurs alongside and parallel to a major lineament extending southwesterly from Beadle Lake. The lineament is coincident with a major swamp to the southwest of sample 218770. No evidence of movement or intense deformation was observed in outcrops along the edge of the lineament, however, the subparallel orientation and close proximity of the Dillman shear zone to the lineament, suggest that the shear may be related to movement along the larger structure. The lineament itself may therefore hold some potential for gold mineralization.
19
One additional area of veining on the southern property is worthy of mention. The area is located on claim 1149520, about 500 metres southwest of the Dillman 1 and 2 showings. Two east-west striking veins, situated just northwest of the boundary between zones M1 and M2, exhibit textures and mineralization similar to that found at the Wagg showing. The larger of the veins is up to 0.5 metres wide and was traced for about 15 metres. Of the ten samples taken from the veins, the highest assay was 465 ppb gold, from sample 218115.
20
Mechanical Outcrop Stripping
Mechanical stripping and outcrop washing was completed in five areas of the property where vein hosted gold mineralization had been found. The three gold showings on the southern property were discovered during the 1992 prospecting, and visible gold had been observed in all three. The two areas on the northern property had been the subject of preliminary manual stripping during 1991, and the recent work was undertaken in order to extend the strike lengths of the mineralized /ones.
Dillman Shear Zone Showing
At the Dillman Shear Zone, located in the east-central part of claim 1149518, stripping revealed a 5 to 15 centimetre wide quartz vein heavily mineralized with pyrite, which was traced for about 40 metres along strike. The vein occurs within a zone of sheared and chloritized gabbro averaging 0.5 metres or lessin width, striking 055 degrees and dipping between vertical and 85 degrees to the southeast. Very fine native gold was observed at several places within the quartz-pyrite vein. As shown in Figure 6, the shear and vein appear to pinch out at the eastern end of the trench, but to continue beneath overburden at the western end of the trench.
Assay results range from below detection to 0.03 oz./ton gold in grab and chip samples of sheared wallrock. Chip samples across the shear and vein assayed from 0.004 to 0.587 oz./ton gold, with most falling between 0.02 and 0.138 oz./ton. Analysis of grab and chip samples consisting entirely of quartz and pyrite returned gold values ranging from 0.006 to 1.578 oz./ton, with most samples assaying about 0.50 oz./ton. One sample from the area (sample 220435) returned a value of 0.081 oz./ton gold from loose dioritic bedrock containing a few percent disseminated pyrite as smears along joint planes.,
Dillman 1 and Dillman 2 Showings
At the Dillman 1 and 2 gold showings on claim 1149520 (Figures 7 and 8) stripping revealed two quartz vein exposures which may be parts of a single structure. The veins both fill fracture/jointing controlled dilation zones, and both maintain a strike of 080 to 090 degrees despite containing a series of small open folds. The two veins are separated by about 100 metres of intervening ground where outcrop is sparse. Both showings are hosted within pillowed to massive mafic volcanics, and both display similar, varying degrees of oxidation and alteration of wallrock for a distance of up to 0.5 metres on either side of the vein. Wallrock alteration consists of variable silicification. chloritization, and a peculiar banding due to "gneissic" segregation of feldspar and mafic silicates.
21
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At the more easterly of the showings, a 5 to 20 centimetre wide quartz vein has been traced for a distance of about 38 metres. At both ends of the stripped area the vein disappears, and may be offset beneath relatively deep overburden. Grab samples of altered wallrock have returned gold values ranging from 0.002 to 0.081 oz./ton. Chip samples including wallrock and quartz have assayed from 0.002 to 3.043 oz./ton gold, most commonly returning values around 0.20 oz./ton. Chip and grab samples consisting solely of quartz have assayed between 0.001 and 8.837 oz./ton gold, with most values occurring between 0.20 and 0.75 oz./ton.
At the westerly showing, a 5 to 45 centimetre wide quartz vein has been traced for a distance of about 20 metres along strike. At both ends of the stripped area, the vein appears to pinch out against northeasterly trending zones of shearing, at the edge of areas covered by relatively thick overburden and jumbled bedrock. Assays here ranged between 24 ppb and 1366 ppb (0.033 oz./ton) gold for altered wallrock, with most values below 100 ppb (0.003 oz./ton). Representative samples across the altered wallrock and vein returned values ranging from 713 ppb (0.023 oz./ton) to 0.431 oz./ton gold. Grab and chip samples consisting entirely of quartz returned assays ranging from 0.03 to 2.822 oz./ton gold, with most assays falling between 0.30 and 0.70 oz./ton.
Agassiz West Showings
Within the initial group of thirty claims on the northern property, three trenches were dug to expose bedrock in the area which has come to be known as the Agassiz West showing. As shown in Figures 9, 10, and 11, stringers, small lenses, and contorted veins of quartz occur in association with zones of fracturing and chloride shearing. Country rock in the area consists of massive and pillowed metamorphosed mafic flows, which are intruded by a number of quartz-feldspar porphyry and granitic dykes striking subparallel to foliation in the metavolcanics.
The northern and central trenches, shown in Figures 9 and 10, expose what appears to be a single structure, within which quartz has filled fracture controlled dilation zones. Wallrock and small stringers returned anomalous gold values ranging from below detection to about 0.032 oz./ton. Grab and chip samples consisting entirely of quartz, and obtained from within the main structure, assayed between 0.036 and 1.47 oz./ton gold. Representative samples including both quartz and wallrock returned gold values ranging from a low of 46 ppb at the north end of the northern trench, to a high of 2.99 oz./ton in the centre of the central trench. The highest assay came from a 0.9 metre chip which included only one 5 centimetre wide stringer of quartz. This result is indicative of the highly erratic nature of gold distribution in the area of the three trenches.
22
Figure 9. Agassiz West Gold Showings Trench 1 (North)
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Within the southernmost of the three trenches, shown in Figure 11, two subparallel quartz veins trending northwest-southeast are cut by several quartz feldspar porphyry dykes. Visible gold has been observed at several locations within each vein. Mineralization and textures exposed in this trench resemble those observed in the previous trenches, and assay results suggest a similarly erratic distribution of gold. The trench is approximately 20 metres long, and each vein has been exposed for a length of about 11 metres.
Samples consisting entirely of wallrock assayed from around 50 ppb up to 435 ppb (0.013 oz./ton) gold. One sample of silicified chlorite schist occurring adjacent to the northern vein assayed 0.780 oz./ton gold, however, other samples of rocks adjacent to vein contacts returned uniformly low gold values. Grab samples of vein material returned values ranging from a low of 76 ppb to highs of 2.06 and 2.36 oz./ton. Results of chip sampling across the veins and adjacent wallrock suggests that gold mineralization is most abundant in the central and southeastern parts of the exposure. Northwest of the westernmost porphyry dyke, assays of quartz typically ran less than 0.075 oz./ton, while southeast of the dyke assays were typically between 0.075 and 0.20 oz./ton, with occasional higher values.
Wagg North Area
In the area immediately north of the Wagg showing, 1991 work had uncovered more than a dozen angular blocks of vein quartz in the vicinity of grid co-ordinate 36+25 N, 12+15 E, on the margin of an area covered by deep overburden (Figure 12). A representative sample, numbered 11316, and composed of chips obtained from most of the blocks, assayed 0.328 oz./ton gold (Wagg and Holmstead, 1991). The area is directly along strike from the northern tip of the "F" vein at the Wagg showing, and quartz stringers and porphyry dykes characteristic of the showing had been observed in metavolcanic outcrops in the intervening 25 metres. Given the southerly direction of ice advance during glaciation, it was assumed that the source of the float was a previously unexposed vein lying under the overburden near sample 11316.
The area exposed by the 1992 stripping measures 3 to 5 metres wide, and extends about 30 metres downslope from L 36+15 N, 12+30 E to L 36+30 N, 12+10 E. As shown in Figure 12, the exposure consists primarily of pillowed mafic metavolcanics containing infrequent quartz stringers. The northern half of the trench was difficult to examine in detail because irregularities in the bedrock surface prevented thorough cleaning.
Although the stripping unearthed several scattered blocks of "showing type" quartz from within overburden, the programme was unsuccessful in locating the source of the float.
Overburden removal had progressed from south to north, down a moderate slope through an increasingly thick sand and boulder till. Stripping was suspended a short distance north of the location of sample 11316, where large metavolcanic boulders are stacked against a north facing cliff in the bedrock topography. The boulders could not be dislodged by the relatively light equipment being utilized.
23
T rench Plan
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The two veins shown to occur near the middle of the trench are of a different texture, and are far too narrow to be the source of the vein quartz debris. The two veins carry minor feldspar and pyrite, and resemble barren veins occurring elsewhere in the area, which have been interpreted to postdate gold mineralization. The dyke which crosses the stripped exposure is granitic textured, and intermediate to felsic in composition. It is grouped with rocks of the Sabaskong Batholith as map unit 5, and is not considered related to the quartz feldspar porphyries occurring within the Wagg showing. No samples were collected from this exposure.
24
Diamond Drilling
Three short holes totalling 120 feet were drilled in May of 1992, at the Wagg gold showing, located on claim 1079876. The holes were drilled in order to test the width of the "F" Vein, in an area where it was proposed to remove a portion of the bulk sample. Because of the inconclusive results, the drilling was abandoned.
As indicated on the drilling plan map, a two metre deep trench has since removed the vein in the area targeted by the drilling. As blasting progressed across the area in early September of 1992, it became evident that the vein was complexly folded downdip as well as along strike. It is now apparent that the vein was cut off just below surface in the vicinity of the drilling, by a porphyry dyke encountered in hole WT-92-01.
The holes intersected metamorphosed pillowed basalts which displayed a weakly variolitic texture around pillow margins, and exhibit a weak to moderate foliation. A narrow, weakly foliated, feldspar porphyry dyke was intersected in hole WT-92-01. Several narrow quartz veins, largely barren of mineralization, were intersected in holes WT-92-01 and WT-92-03. The geology and structure of the holes are diagrammed in the drill sections.
It is apparent from an examination of outcrops in the vicinity, that the foliation strikes about 025 degrees and dips subvertically to 70 degrees westerly, becoming variable near the margins of veins. Pillows have been flattened subparallel to the foliation, and appear to have been stretched to a slightly greater degree downdip than along strike. The porphyry dyke which crosses the area strikes about 020 degrees and appears to dip near vertically.
Detailed Diamond Drill Logs with a plan and sections are included in Appendix 2.
25
Bulk Sample
A 250 ton bulk sample was collected from Veins A, D, DE and F at the Wagg Showing on Claim 1079876 (Figure 13).
Preliminary metallurgical work was completed in February 1992 by Edward Ludwig of Nighthawk Diamond Drilling, (see Appendix 3) He examined reject material from seven samples collected from the Wagg Showing in 1991. He concluded that the gold bearing quartz at the Wagg Showing was "a very free milling ore which will require grinding to approximately 100% minus 100 mesh".
The quartz was found to be annealed with intense hairline fracturing. Gold was found to surround individual quartz grains and as wires protruding from larger pieces of quartz. Digestion of the sulphides by nitric acid did not yield any gold suggesting gold is contained only in the quartz vein material. Under the microscope, about 67% of the gold was found to be between -60 mesh and +100 mesh. The silver content was found to be very low, averaging about 0.05 oz/ton.
Ore was removed from the trenches by blasting from holes produced by a hand plugger powered by a 175 CFM Compressor. The ore was moved to the mill area by a Davis Front End Loader. Some ore was removed from the trenches with the help of a Case Backhoe. Preliminary crushing was done with a 10x12 inch Jaw Crusher. The mill feed crushed to about 0.25 inches was then transferred to a one ton ore bin by a small bucket elevator. The 6'x3' mill was fed by a rheostat controlled vibrating chute that could be adjusted to control the feed rate of the ore. The ore that entered the ball mill was then mixed with water and ground into a slurry. The fine overflow from the ball mill flowed into a 6' sluice lined with 3M Nomad carpeting. Material too coarse for the sluice was separated by a screen classifier and collected in a wooden box to be fed back into the ball mill. The carpeting was found to be very effective for catching gold grains. Discharge from the sluice box emptied into a 2" slurry pump where it was pumped to a 6" cyclone classifier. The fine fraction was discharged to the tailings sluice which was also lined with Nomad carpeting in order to catch any remnants of gold remaining in the tailings. The tailings were then discharged to a holding pond where they would settle out of the water. The coarse fraction from the cyclone classifier would then be recycled back into the ball mill for further size reduction.
Water for operation was taken from the tailings pond therefore the water used was constantly being recycled. The crusher, bucket elevator, vibrating chute, ball mill and slurry pump were all powered by a 75 KW diesel generator. The cyclone was powered by water pressure from the slurry pump. Other water pumps were gasoline powered.
26
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The top piece of Nomad carpet in the sluice at the end of the ball mill was washed into a 5 gallon plastic pail every hour when the mill was in operation. It was found that most of the gold was caught on this carpet. The remaining carpets in the ball mill sluice and the carpets in the tailings sluice were cleaned at the end of the day in the same manner.
The concentrate from the carpets was then screened into different size fractions and the heavy portion was removed by hand panning or with a mechanical spiral panner. Reject material from the panning was then returned to the mill for further processing. The heavy portion recovered in the panning was dried and the magnetic portion was removed by the use of a magnet to be saved for gold removal at a later date. The dried, nonmagnetic, heavy fraction could then be hand panned to a concentrate that consists of about 90% gold. This step was found to be facilitated by the use of a suction device for separating the pure gold from the remaining waste material.
The 90% gold concentrate was then mixed with a flux consisting of borax, potassium nitrate, soda ash and silica in a clay crucible and melted in an oven capable of maintaining a temperature of about 2,000 degrees F.
To date all of the gold has not been removed from the concentrate therefore exact figures of gold recovery from the bulk sample are not available at the time of this report. To date about 75 troy ounces of gold have been recovered. A total of 247 tons of material were processed by the mill; 42% from Vein A, 32% from Vein F, 14% from Vein D, 5% from Vein DE and 7% composite material from all of the veins.
Three tailings samples (920708, 920721A and 920721B) were subjected to ICP analysis at Bondar Clegg in Ottawa with the following average results;
Gold (ppb) 2651Aluminium (%) 0.24Iron (%) 1.22Manganese (ppm) 129Magnesium (%) 0.21Calcium (%) 0.38Sodium (%) 0.04Potassium (%) 0.05Scandium (ppm) < 5Vanadium (ppm) 9Chromium (ppm) 39Cobalt (ppm) 9Nickel (ppm) 22Copper (ppm) 110Arsenic (ppm) < 5Strontium (ppm) 2Yttrium (ppm) < 1
27
Molybdenum (ppm) 4Silver (ppm) <0.2Cadmium (ppm) <0.2Tin (ppm) <20Antimony (ppm) < 5Tellurium (ppm) < 10Barium (ppm) 3Lanthanum (ppm) < 1Tungsten (ppm) < 20Lead (ppm) 11Bismuth (ppm) < 5Zinc (ppm) 8Mercury (ppb) <5
28
DISCUSSION
The work by Western Troy Capital Resources in the vicinity of Menary Township has been carried out across an area which has seen little or no previous exploration. Prior to 1989, only one relatively insignificant gold showing was known within the boundaries of the company's claims. The 1991 exploration programme resulted in the discovery of the Agassiz West, Galbraith A, Galbraith B, Roadside vein, and Wagg gold showings, bringing to six the total number of gold occurrences in northeastern Menary Township.
The 1992 first phase mapping and prospecting, across 180 claim units, resulted in the discovery of the Galbraith C, Dillman shear zone, Dillman #1, and Dillman #2 gold showings. This totals 10 previously undiscovered gold occurrences and is testament to the excellent potential of the property for further gold discoveries.
Mechanical stripping was undertaken on four separate areas of the property, and some form of further work appears to be justified in each area. Initial stripping at the three Dillman showings (two areas), and at the Agassiz West area, revealed anomalous to ore-grade gold values over significant strike lengths. At the Wagg showing area, stripping did not reveal any veining, but further stripping in search of a northern extension remains a high priority.
The Roadside vein and Galbraith A, B, and C gold showings remain relatively untested. Narrow widths and/or erratic gold values, as well as budget constraints, are the reasons for not stripping these areas in 1992. There is little doubt, however, that as work progresses on the property, they will each be the subject of some sort of further work.
Geological mapping at a scale of 1:20,000 has produced a preliminary geological map of the properties, and has refined the locations of outcrops and geological contacts shown on Blackburn's 1976 map at a scale of 1:63,360. The mapping has revealed that there is a definite spatial association between gold bearing and barren veining, and certain geological units.
With the exception of the Dillman Shear Zone, all of the showings discovered to date on the Western Troy properties are situated within the lowermost M1 lithostratigraphic subdivision of the mafic metavolcanics. Similarly, quartz veins and small zones of shearing and alteration are far more abundant within the Ml zone than within any of the succeeding zones.
The Ml zone consists primarily of thin pillowed, massive, and pillowed variolitic flows. No one rock type hosts all of the showings, and in fact rapidly alternating sequences may be preferred areas for vein formation. There appears to be some correlation between areas containing variolitic textured pillowed flows, and areas containing abundant veining. However, this relationship may be only a function of the detail of investigation into the areas hosting numerous veins.
29
The showings hosted within rocks of the Ml zone all contain quartz veins of a similar appearance, texture, and mineralogy. Wallrock to the veins is essentially unaltered, with the exception of the Dillman #1 and #2 veins, and at most showings shearing is present, but not particularly prominent, and not apparently significant in terms of vein emplacement.
The veins all appear to have filled fracture controlled dilation zones. In some areas, such as at the Roadside vein and the Agassiz West #1 and #2 trenches, and possibly at the Dillman #1 and #2 veins, a single reasonably planar structure has been interpreted. Elsewhere, such as at the Galbraith A and Wagg showings, and at the Agassiz West #3 trench, multiple dilation zones developed. These showings have been subjected to significantly more post- emplacement deformation than the single vein showings. This may not reflect a greater absolute age for the highly deformed veins, but it likely indicates that vein formation continued over a longer period, and seems to indicate a greater potential for gold mineralization to occur within them.
The showings which consist of multiple veins, the Agassiz West, Wagg, and Galbraith A, are the closest of the many showings to the contact of the Sabaskong Batholith. The showings' position within the lower portion of the Ml zone is interpreted to be due to conditions prevailing at the time of initial vein formation, rather than to conditions prevailing during the intrusion of the Sabaskong Batholith. Veins relating directly to the intrusion of the batholith are uniformly white, glassy to crystalline, are associated with zones of granitic dykes, and return negligible gold values. Clusters of barren veins formed prior to the intrusion of porphyry dykes, and found within the upper portions of the Ml zone, are in some cases closer to the batholith than many of the single vein showings. The barren veined areas appear to have undergone considerably less deformation than the areas of multiple vein showings.
Evidence of post-emplacement brittle and ductile deformation was observed at all of the showings within the Ml zone. In addition, porphyry dykes are present in the immediate vicinity of all the showings, and frequently crosscut quartz veins. The dykes are relatively undeformed, and no evidence was observed to indicate that they may have had any role in the introduction of gold mineralization, other than that of causing local remobilization. The porphyries are interpreted to occur in association with both gold bearing and barren veins because of pre-existing zones of weakness in the areas of veining. If as the author believes, Blackburn's interpretation of the origin and timing of the porphyry intrusions is correct, and they are the intrusive equivalent of the metamorphosed felsic volcanics located along Burditt Lake, then it appears that gold bearing vein formation had largely concluded prior to the commencement of the second cycle mafic to felsic volcanism. This interpretation suggests that the veining may be the result of hydrothermal fluids moving through a cooling volcanic pile, and that although the Batholith might be the initial source of the fluids and gold at depth, the present distribution of veins and gold mineralization is essentially unrelated to the intrusion of the Batholith and concurrent regional metamorphism.
30
The Dillman Shear Zone, located within the mixed pillowed to gabbroic textured M3 zone, contains a small bluish grey quartz vein which is heavily mineralized with pyrite, and contains traces of very fine native gold. The different nature of the quartz and mineralization may be due to having a different host rock than the other showings, however, this is the only showing in which shearing crosscutting the regional foliation is prominent. The showing may be related to a major topographic lineament, and is tentatively interpreted to be younger than the other known showings. It is notable that a porphyry dyke, occurring alongside a portion of the zone of shearing, is somewhat folded, while the chloritic shear itself is a linear structure. While this is by no means conclusive evidence for the following interpretation, it is postulated that the Dillman Shear Zone formed during the late stages of the regional metamorphic event.
Although all of the showings on the property have returned at least one anomalous value from sampling, the erratic nature of native gold distribution prevents an accurate determination of grade without exhaustive sampling. In addition, the relatively small size of individual veins, and the complex deformation which most of the showings display, presents a substantial challenge to diamond drilling programmes. Consequently, overburden stripping and rock trenching may be the most efficient and cost effective means of making a preliminary evaluation of the gold showings on the property.
31
CONCLUSIONS
The results of the 1992 reconnaissance mapping and prospecting programme clearly indicate that the pillowed and massive metabasalts of the M1 lithostratigraphic zone represent the area of the Western Troy properties with the highest potential to host gold bearing quartz veins. Nine of the ten gold showings known to exist on the property occur within the Ml zone, which occurs along the northwestern margin of both Western Troy properties.
Eight of the nine showings contain quartz veins filling fracture-related dilation zones, and all have undergone varying degrees of brittle and ductile deformation. A greater degree of deformation seems to correspond with more consistent gold values along strike of a vein, and occasionally correspond to higher gold grades.
Of the ten known showings, seven are known to contain visible gold, and nine have returned at least one assay in excess of 1 oz./ton gold. Four of the showings have yet to be tested by mechanical stripping, and six occur in areas not covered by the 1989 ground geophysical surveys.
Although both veining and sulphide mineralization are uncommon to the southeast within the overlying zones of the metavolcanic sequence M2-F1, the area should not be dismissed as totally without potential. The Dillman shear gold showing occurring in the central portion of the southern property has been interpreted as being younger than the group of zone Ml showings, and as having been formed under a different set of prevailing tectonic conditions. The showing occurs within the M3 zone of mafic metavolcanics, from which two anomalous gold samples were collected on the southern property. Limited potential also exists within the M2 to Fl metavolcanic zones for shear zones to occur along a number of major topographic lineaments within which bedrock is largely obscured by overburden.
The rocks of the Sabaskong Batholith do not appear to have been a particularly favourable site for the development of quartz veins. The few samples collected from veins within the granite all returned uniformly low gold values, however this type of mineralization has not been thoroughly investigated and can not be completely ruled out. Similarly, it appears that no veining or mineralization occurs in association with diabase dykes.
The results of the limited diamond drilling are inconclusive. Because only three short holes were drilled, all collared within an area less than 8 metres in diameter, it is judged unreasonable to apply the results obtained at the southern end of the "F" vein to the remainder of the vein, or to the other veins at the showing.
32
The bulk sample programme was successful in demonstrating that the gold at the Wagg Showing was free milling and that a gravity separation circuit could be set up to remove the gold with little or no significant impact to the surrounding environment. The process of extracting the gold from the concentrates is ongoing at the time of this report, therefore the total gold recovered is not known at the time of writing. It is known, however, that the majority of the gold was free milling and very little gold was being lost to the tailings therefore the final gold recoveries are expected to be satisfactory.
33
RECOMMENDATIONS
1. AH of the present claim groups should he retained in good standing.
2. A grid with lines spaced 100 metres apart should be cut over the portion of the properties underlain by rocks of the metavolcanic Ml zone. The lines should be extended 100 to 200 metres beyond the contact with the M2 zone, and a similar distance into the Sabaskong Batholith on the northern property.
3. Geological mapping, soil geochemistry, and magnetometer and VLF-EM surveys with a 25 metre station spacing should be completed over the gridded area.
4. Mechanical stripping, outcrop washing, mapping and detailed sampling should be completed at the four previously unstripped gold showings.
5. Additional mechanical stripping should be completed at the Dillman #1 and #2, and the Agassiz West gold showings. Bedrock trenching should be completed, and large representative samples collected, prior to commencing exploratory diamond drilling.
6. Prospecting, and ground magnetometer and VLF-EM surveys should be completed over a flagged grid at the Dillman Shear Zone gold showing, and over selected portions of several major lineaments located within zones M2 to M5.
Several areas of abundant quartz veining which returned negligible gold values from within the Ml zone on the northern property should be examined further. Gold bearing veins may be found within or peripheral to the areas, and further study may reveal critical factors governing the localization and emplacement of gold bearing quartz veins. „
Detailed diamond drilling should be done on the veins of the Wagg showing in order to define the down dip continuity and consistency of gold grades in the veins.
The bulk sample programme should continue with sampling of veins that were not sampled in 1992. Larger, more representative samples should be taken from the veins that were sampled in 1992. The existing mill on site should be upgraded to a minimum 10 ton per day set-up by improving the efficiency of the grinding circuit.
34
BIBLIOGRAPHY
Bajc, A.F.1988: Reconnaissance Till Sampling in the Fort Frances-Rainy River District, in Summary
of Fieldwork and Other Activities 1988, Ontario Geological Survey MiscellaneousPaper 141, pp. 417-420.
Blackburn, C.E.1976: Geology of the Off Lake-Burditt Lake Area, District of Rainy River; Ontario Division
of Mines Geoscience Report 140, 62p.Accompanied by Map 2325, scale 1 inch to 1 mile (1:63 360).
Clarke, J.G.1989: Evaluation of the Exploration Potential of the Menary Township Property, District of
Kenora, for Western Troy Capital Resources Inc., 20 p.
Edwards, G.R.1981: Bethune Lake; Ontario Geological Survey Map 2430, Precambrian Geology Series,
scale 1 inch to 1/2 mile. Geology 1975.
Ontario Geological Survey1990: Airborne Electromagnetic and Total Intensity Magnetic Survey, Rainy River Area.
Studemeister, P.A.1985: Report on the Hodge Property, Menary Township, Ontario, for Agassiz Resources
Ltd., Assessment Files, Kenora Ministry of Northern Development and Mines.
Sullivan, J.R.1974: Diamond Drill Logs of Perkins Option Drill Program, Assessment Files, Kenora
Ministry of Northern Development and Mines, 8 p.
Wagg, C.A., and Holmstead, W.E.1991: Exploration Programme on the Menary Township Property, Menary Township,
District of Kenora, Ontario, for Western Troy Capital Resources Inc., 25 p.
35
CERTIFICATE
I, Christopher Anthony Wagg, residing at R.R. 1, village of Denbigh, in the Province of Ontario, KOH 1LO, do here by certify that:
1... I hold a Bachelor of Science degree (Honours Geology) received at the University of Western Ontario in 1989.
2... I have been employed as a consulting geologist since 1987, and have been practising my profession continuously since 1989.
3... My report on the Menary Township Area Properties of Western Troy CapitalResources Inc. is based upon a review of published and unpublished information concerning the property and surrounding area, and upon personal knowledge of the geology of the property obtained over the course of approximately three months of fieldwork completed between May and August of 1992.
4... My report on the Menary Township Area Properties has been written entirely, and in all respects, as an independent consultant.
5... I hold no interest, direct or indirect, in the properties or securities of Western Troy Capital Resources Inc., or in any adjacent properties, nor do I intend to acquire any such interest.
Dated at Denbigh, Ontario, this 31st day of January, 1993,
Christopher A. Wagg, B.Sc.
36
06/06x1994 19:40 FROM HOLMSTERD £ RSSOCIRTES TO 17056705863 P. 02
GEOPHYSICAL SURVEY
Beepmbs were qarried by all personnel doing the prospecting. The Beepmat is a geophysical instrument that is dragged over the ground and measures surficial conductivity and (magnetics.
Areas if surficial conductivity were noted on the enclosed maps.
APPENDIX 1
ANALYSES
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
NUMBER7765177652776537765477655776567765777658776597766077661776627766377664776657766677667776687766977670776717767277673776747767577676776777767877679776807768177682776837768477685776867768777688776897769077691776927769377694776957769677697776987769977700777017770277703
CLAIM11494841149484114948411494841149484114948411494871149487114948911494891149489114948911494891149487114948711494861149492114949211494921149492114949211494921149492
1149496114949611494961149496114949611494961149492114949211494921149492114949211494921079871114949211494921149492114949211494921092641109264111494971149497114949711494971149497114949711494941149497
WIDTH(CM)DESCRIPTION GRAB QV GRAB QV GRAB QV GRAB QV GRAB QVGRAB QV 10-15 CMGRAB LARGE QV IN SOFT CHL SH AT OR NEAR GR CONTACT GRAB LARGE QV IN SOFT CHL SH AT OR NEAR GR CONTACT GRAB LARGE QV IN SOFT CHL SH AT OR NEAR GR CONTACT GRAB LARGE QV IN SOFT CHL SH AT OR NEAR GR CONTACT GRAB LARGE QV IN SOFT CHL SH GRAB SOFT CHLORITE SHEAR GRAB QV IN AREA OF 657-661 GRAB DISS. PY IN BASALT GRAB DISS. PY IN BASALT GRAB QV TR CHLORITE GRAB QV SMOKEY QUARTZ 1-3% CHL GRAB QV 2xl5M TR PY CP GRAB SAME AS 668 GRAB QV 15-20CM TR PY CP GRAB QV 6MX20-30CM 20M SW OF 670 GRAB STRINGER ZONE 3M WIDExSM TR COARSE PY GRAB QV 10MX30-40CM GRAB QV 3MX30CM GRAB QV 10-30CMX3M TR EPIDOTE GRAB PELS1C SHEAR QTZ SER MINOR PY CHL GRAB SAME AS 676 GRAB STRINGERS IN SHEAR GRAB QTZ PODS IN FEL-INT SH GRAB QTZ STRINGERS IN GABBROIC VOLC GRAB QV 2MX30-50CM TR PY CP GRAB QV 20CMx4M TR PY GRAB SMOKEY QUARTZ PODS GRAB QV NARROW FOLDED GRAB QVGRAB LOOSE QTZGRAB SMOKEY QTZ STRONG HEMATITE STAIN GRAB QTZ PODGRAB QTZ POD 30CM WIDE TR PY CP MINOR CHL GRAB QV NOSE OF FOLD GRAB QTZ FLOAT GRAB QTZ STRINGER IN GABBRO GRAB QV 25 CM WIDE GRAB QV NORTH END ROADSIDE VEIN GRAB ROUNDED QTZ BOULDERGRAB QV 75CMxlOM TR PY VARIOLITIC WALLROCK GRAB QTZ FLOAT LOCAL ORIGIN GRAB QV 2-3% PY+CP GRAB SAME AS 698GRAB QTZ STRINGER ZONE IN HORNFELSED GABBRO GRAB QTZ POD WITH COARSE CALCITE GRAB QV 1M WIDE TR PY GRAB QV 30CMxlOM TR PY CP
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
NUMBER218533218534218535218536218537218538218539218540218541218542218543218544218545218546218547218548218549218550218751218752218753218754218755218756218757218758218759218760218761218762218763218764218765218766218767218768218769218770218771218772218773218774218775218776218777218778218779218780218781218782218783218784218785
CLAIM114948811494921149492114948911494921149492114949211494891149486114950611495061149506114951211495121149512114951811495161149514114951411495151149515114951511495141149514114951411495141149514114948911495181149518
1149529114951811495181149518114951811495181149518114951711495171149517114951711495291149529114952911495201149520114952011495201149520
WIDTH(CM)DESCRIPTIONGRAB CHLOR WALL TO 532GRAB QV 10CMx2MGRAB CONTORTED QV 5-60CM WIDEGRAB QV 20CM WIDEGRAB QV 10-40CM WIDEGRAB QV 20-30CM WIDEGRAB SIL ZONE IN VOLC 3-4% PYGRAB SHD GAB VOLCGRAB SHD VOLCGRAB SHEAR IN GABBROGRAB QV IN ALT SHD GABBROGRAB RUSTY SCHISTGRAB BRECC VOLCGRAB QV 30CM WIDEGRAB QV 20-50CM WIDEGRAB FLOAT ALT GABBRO 5% PYGRAB FLOAT 1-2CM QTZ STR IN VOLCGRAB NARROW QVGRAB QV 15CMGRAB QV FLOAT CHERTYGRAB QV FLOAT 15CMGRAB WALL TO 752GRAB QV 10CM AND STRGRAB QTZ STR IN GABBROGRAB QV 15CMGRAB QV 10-15CM WIDEGRAB QV IN GABBROGRAB QV 10-20CM WIDE CHL PY CPGRAB PORPH DIKE WITH FINE PYGRAB ALT GABBROGRAB QTZ FLOATGRAB QV 10-15CM WIDEGRAB QV 20CM WIDEGRAB QTZ STRINGERS IN SHD GABBROGRAB QTZ FLOATGRAB QV IN PORPH FLOAT PY MO GRAPHITEGRAB WALL TO 768GRAB QTZ STR IN PORPH DIKEGRAB ALT GAB FLOAT 2-3% PYGRAB QV 5-20CM WIDEGRAB WALL TO 772GRAB QV 10-15CM WIDEGRAB SHD VOLC 1-2% PYGRAB QTZ FLOAT TR PYGRAB QTZ POD TR PY CPGRAB QTZ STR IN VOLCGRAB QTZ STR IN PORPHGRAB SHD PORPH FLOATGRAB QTZ STR IN SHD VOLCGRAB QV 10-15CM WIDEGRAB SAME VEINGRAB SAME VEINGRAB SAME VEIN
SAMPLE DESCRIPTIONS - WESTERN TROY 992
NUMBER CLAIM WIDTH(CM)DESCRIPTION218786 1149520 GRAB PY PO CP TRACED 30M218787 1149520 GRAB SAME VEIN218788 1149520 GRAB SAME VEIN218789 1149520 GRAB SAME VEIN218790 1149520 GRAB QV 30CM IN SHD VOLC218791 1149520 GRAB QV 30CM IN SHD VOLC218792 1149520 GRAB QV 30CM IN SHD VOLC218793 1149520 GRAB QV 10-20CM WIDE TRACED 30M218794 1149520 GRAB DILLMAN 1 20CM218795 1149520 GRAB DILLMAN 1 20CM218796 1149520 GRAB QV IN SHD ALT VOLC218797 1149520 GRAB QV IN SHD VOLC218798 1149520 40 DILLMAN 2218799 1149520 55 DILLMAN 2218800 1149520 GRAB DILLMAN 2 WALLROCK218851 1149489 GRAB QV 10-50 CM WIDE218852 1149489 GRAB QV 10-50 CM WIDE218853 1149489 GRAB GALBRAITH C TR PY CP218854 1149489 GRAB GALBRAITH C CHIPS ALONG STRIKE218855 1149489 GRAB GALBRAITH C CHIPS ALONG STRIKE218856 1149489 GRAB PIT 5M S OF VEIN QV 30CM WIDE218857 1149518 GRAB LARGE QTZ FLOAT218858 1149518 GRAB ALT VOLC FLOAT218859 1149518 GRAB CHLOR SHEAR IN GABBRO DILLMAN SHEAR218860 1149518 GRAB QTZ STR IN VOLC218861 1149517 GRAB QV 15CM218862 1149517 GRAB LARGE ALT VOLC FLOAT218863 1149517 GRAB QV 10CM IN PORPH VOLC218864 1149518 GRAB SHEAR IN GABBRO 5-10CM QV218865 1149521 GRAB SHEAR IN GABBRO218866 1149517 GRAB SHEAR 30CM WIDE IN VOLC218867 1149517 GRAB QV 15CM IN SHEAR218868 1149529 GRAB QV 20CM IN SHD GABBRO218869 1149518 GRAB CHERTY NON-LOCAL FLOAT218870 1149529 GRAB SHEAR IN GABBRO218871 1149529 GRAB SHEAR IN GABBRO218872 1149529 GRAB SHEAR IN GABBRO218873 1149518 GRAB BIOTITIC FLOAT QTZ STR TR PY218874 1149529 GRAB QV 10CM WIDE218875 1149529 GRAB QV 15CM WIDE218876 1149529 GRAB QTZ STR ZONE218877 1149529 GRAB WALL TO 876218878 1149529 GRAB QTZ IN SAME SHEAR AS 877218879 1149529 GRAB QTZ IN SAME SHEAR AS 877218880 1149529 GRAB QTZ IN SAME SHEAR AS 877218881 1149529 GRAB RUSTY VOLC218882 1149520 GRAB QV218883 1149520 GRAB QTZ CALC STRINGERS218884 1149520 GRAB SAME AS 882 883218885 1149520 GRAB QV 20CM WIDE218886 1149520 GRAB QV AND STR IN SHD GABBRO218887 1149520 GRAB DILLMAN QTZ AND WALL218888 1149520 GRAB QTZ AND CALCITE SAME SHEAR AS 887
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
NUMBER218889218890218891218892218893218894218895218896218897218898218899218900218101218102218103218104218105218106218107218108218109218110218111218112218113218114218115218116218117218118218119218120218121218122218123218124218125218126218127218128218129218130218131218132218133218134218135218136218137218138218139218140218141
CLAIM 1149520 1149520 1149518 1149518 1149518 1149518 1149518 1149520 1149520 1149520 1149520 1149520 1149520 1149520 1149520 1149520 1149520 1149520 1149520 1149520 1149529 1149529 1149529 1149529 1149529 1149520 1149520 1149516 1149516 1149516 1149516 1149516 1149531 1149531 1149531 1149531 1149531 1149529 1149529 1149529 1149529 1149529 1149529 1149529 1149529 1149529 1149520 1149520 1149520 1149520 1149520 1149520 1149520
WIDTH(CM)DESCRIPTION GRAB QV 20CMGRAB QV 20CM MINOR PY TR CP GRAB DILLMAN SHEAR FIG 6 GRAB DILLMAN SHEAR FIG 6 GRAB DILLMAN SHEAR FIG 6 GRAB DILLMAN SHEAR FIG 6 GRAB DILLMAN SHEAR FIG 6 GRAB QTZ FLOAT
7777
FIGFIGFIGFIG
2 LOOSE QTZ 2 LOOSE QTZ
GRAB DILLMANGRAB DILLMANGRAB DILLMANGRAB DILLMANGRAB DILLMANGRAB DILLMANGRAB QV 15CMGRAB NARROW SHEAR IN VOLCGRAB SHD ALT VOLCGRAB LOOSE QTZ FROM SHEARGRAB SHD ALT VOLCGRAB QTZ AND CALC IN SHD ALT VOLCGRAB QTZ FLOATGRAB SHEAR IN GABBROGRAB CALCITE ON GABBRO SHEARGRAB QTZ FLOATGRAB LARGE QTZ FLOATGRAB ALT VOLC MINOR PY CPGRAB QV BLUE GREYGRAB QV 30CMGRAB RUSTY VOLC FLOAT RESAMPLE 8174GRAB RUSTY VOLC FLOAT RESAMPLE 8174GRAB SHEAR 1M WIDEGRAB QV 40CM WIDEGRAB QV 15CMx20MGRAB QV 15CMx20MGRAB FLOAT QTZ STR IN VOLCGRAB FLOAT QTZ STR IN VOLCGRAB FLOAT SHD ALT GABBROGRAB INT-FEL SHD VOLCGRAB QTZ STR RESAMPLE OF 218865100 STRINGERS AND SHEAR100 STRINGERS AND SHEAR
GRAB FLOAT ALT BASALT WITH QTZ STR GRAB QV 15CM WIDE GRAB QV 5-20CM SAME AS 130 131 GRAB QV 25M N OF 132 GRAB QV SAME VEIN 60M N OF 132 GRAB DILLMAN 1 FIG 7 GRAB DILLMAN 1 FIG 7 GRAB DILLMAN 1 FIG 7 GRAB DILLMAN 1 FIG 7 GRAB DILLMAN 1 FIG 7 GRAB DILLMAN 1 FIG 7 GRAB DILLMAN 1 FIG 7
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
1 FIG 1 FIG FIG FIG FIG FIG FIG FIG
111111
777777777
NUMBER CLAIM WIDTH(CM)DESCRIPTION218142 1149520 GRAB DILLMAN 1 FIG218143 1149520 GRAB DILLMAN218144 1149520 GRAB DILLMAN218145 1149520 GRAB DILLMAN218146 1149520 GRAB DILLMAN218147 1149520 GRAB DILLMAN218148 1149520 GRAB DILLMAN218149 1149520 GRAB DILLMAN218150 1149520 GRAB DILLMAN
8106 1149496 GRAB QV 1M WIDE8107 1149496 GRAB BRECC WALL TO 81068108 1149496 GRAB QV 1M WIDE8109 1149496 GRAB QV 1M WIDE8110 1149496 GRAB QTZ FLOAT8111 1149496 GRAB QV 80CM8112 1149496 GRAB ABUNDANT QTZ FLOAT8113 1149496 GRAB QV 10CM IN VOLC8114 1149496 GRAB QTZ FLOAT8115 1149496 GRAB QV 10CM IN PORPH VOLC8116 1149496 GRAB ALT VOLC8117 1149492 GRAB QV 20CM8118 1149492 GRAB QTZ STR8119 1149492 GRAB QV 1M WIDE8120 1149493 GRAB QV 1.5M WIDE8121 1149492 GRAB STR IN ALT VOLC8122 1149492 GRAB QTZ VEIN AND PORPH DIKE8123 1149492 GRAB LARGE QTZ FLOAT8124 1149509 GRAB QV 30CM8125 1149509 GRAB QV 30CM8126 1149509 GRAB QTZ FLOAT8127 1149509 GRAB QV 30CM8128 1149509 GRAB QV 30CM8129 1149509 GRAB QV 5-10CM8130 1149509 GRAB QV 40CM8131 1149489 GRAB QTZ POD8132 1149489 GRAB QTZ STR ZONE8133 1149489 GRAB QTZ STR ZONE8134 1149489 GRAB QTZ STR ZONE8135 1149506 GRAB ALT VOLC8136 1149506 GRAB QV MINOR PY8137 1149506 GRAB QV 70CM WIDE8138 1149506 GRAB QTZ FLOAT8139 1149503 GRAB QV 40CM WIDE8140 1149499 GRAB QV8141 1149512 GRAB ALT PORPH VOLC8142 1149512 GRAB QTZ FLOAT 15CM8143 1149512 GRAB QV 30 CM WIDE8144 1149496 GRAB QV FLOAT 10CM8145 1149496 GRAB LARGE QTZ FLOAT 1M8146 1149496 GRAB LARGE QTZ FLOAT 1M8147 1149496 GRAB QTZ STR ZONE IN VOLC8148 1149496 GRAB QTZ FLOAT8149 1149496 GRAB QTZ FLOAT
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
NUMBER81508151815281538154815581568157815881598160816181628163816481658166816781688169817081718172817381748175817681778178817981808181818281838184818581868187
220401220402220403220404220405220406220407220408220409220410220411220412220413220414220415
CLAIM WIDTH(CM)DESCRIPTION11494961149496114949211494891149489114948911494891149492114949211494881149506114950611495121149512114951211495121149512114951811495181149518114951611495161149516114951611495161149516114951611495161149516114951511495151149515114951611495181149518114951811202581120258114952011495201149516114951611495161149529114952911495201149520114952011495201149520114952011495291149521
GRAB QV 40CM IN SHD VOLCGRAB QV 40CM IN SHD VOLCGRAB QTZ FLOAT 20CMGRAB QV ON PORPH DIKE CONTACTGRAB QV 80 CM FOLDEDGRAB QV 80CM FOLDEDGRAB QV 80CM FOLDEDGRAB QV 20 CMGRAB QV 3 5 CMGRAB QV 10 CM TR PYGRAB QV 10 CMGRAB QV 50 CM IN SHEARGRAB QTZ STR IN SHEARGRAB QTZ STR IN PORPH FLOATGRAB QV 20 CM IN 1M SHEARGRAB QTZ STR IN VOLCGRAB QTZ STR IN VOLCGRAB QV 15 CMGRAB QV IN ALT VOLC FLOATGRAB QTZ FLOATGRAB QTZ FLOATGRAB QTZ STR IN CHL SHEARGRAB QTZ STR IN SHD GABBROGRAB SHEAR ZONE IN GAB VOLCGRAB QTZ FLOAT 20CMGRAB CHERT HOR IN VOLC TR PY POGRAB ALT ZONE IN VOLCGRAB STRINGERS IN GABBROGRAB QV 10-40CM IN GAJWROGRAB QTZ FLOAT 20CM+GRAB QTZ FLOAT 20CM+ SAME LOCATIONGRAB SHD ALT GABBROGRAB SHEAR ZONE IN VOLCGRAB QV 10CM IN SHD GABBROGRAB SHD GABBROGRAB QV 20 CMGRAB QV NO MINERALIZATIONGRAB QV NO MINERALIZATION 36N 17EGRAB SHEAR ZONEGRAB SHD ALT VOLCGRAB QV 15CMxl5M PY TR CPGRAB QV 15CMxl5M PY TR CPGRAB QV 15CMxl5M PY TR CPGRAB SHD SIL VOLCGRAB CHL SHEAR IN VOLCGRAB DILLMAN 1 FIG 7GRAB DILLMAN 2 FIG 8GRAB DILLMAN 2 FIG 8GRAB DILLMAN 2 FIG 8GRAB DILLMAN 2 FIG 8GRAB QTZ STR IN ALT VOLCGRAB SIL SHD QTZ PORPHGRAB DISS PY CP IN VOLC
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
NUMBER220416220417220418220419220420220421220422220423220424220425220426220427220428220429220430220431220432220433220434220435220436220437220438220439220440220441220442220443220444220445220446220447220448220449220450216651216652216653216654216655216656216657216658216659216660216661216662216663216664216665216666216667216668
CLAIM WIDTH(CM)DESCRIPTION11495211149520114952011495201149518114951811495181149518114951811495181149518114951811495181149518114951811495181149518114951811495181149518114951811495181149518114951811495181149518114951811495181149518114952011495201149520114952011495201149520114952011495201149520114952011495201149520114952011495201149520114952011495201149520114952011495201149520114952011495201149520
GRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRAB
QTZ POD WITH PORPHQV IN PORPH 100M SQV IN PORPH 100M SQV IN PORPH 100M SDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANALT VOLC
DILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMAN
SHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEARSHEAR1 FIG1 FIG1 FIG1 FIG1 FIG1 FIG1 FIG1 FIG1 FIG1 FIG1 FIG1 FIGW OF
2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG
ZONEZONEZONEZONEZONEZONEZONEZ<-w:ZONEZONEZONEZONEZONEZONEZONEZONEZONEZONEZONEZONEZONEZONEZONEZONEZONE777777777777
DIKEOFOFOFFIGFIGFIGFIGFIGFIGFIG!•' I GFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIG
DILLMAN
8888888888
DILLMAN 2DILLMAN 2DILLMAN 26666666666666666666666666
1
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
NUMBER216669216670216671216672216673216674216675216676216677216678216679216680216681216682216683216684216685216686216687216688216689216690216691216692216693216694216695216696216697216698216699216700216701216702216703216704216705216706216707216708216709216710216711216712216713216714216715216716216717216718216719216720216721
CLAIM WIDTH(CM)DESCRIPTION11495201149520114952011495201149520114952011495201149520114952011495201092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637109263710926371092637
GRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRABGRAB
DILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANDILLMANAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZAGASSIZ
2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIG2 FIGWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWESTWEST
8888888888
FIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIGFIG
9-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-119-11
SAMPLE DESCRIPTIONS - WESTERN TROY - 1992
NUMBER CLAIM WIDTH(CM)DESCRIPTION216722 1092637 GRAB AGASSIZ WEST FIG 9-1-1216723 1092637 GRAB AGASSIZ WEST FIG 9-11216724 1092637 GRAB AGASSIZ WEST FIG 9-11216725 1092637 GRAB AGASSIZ WEST FIG 9-11216726 1092637 GRAB AGASSIZ WEST FIG 9-11216727 1092637 GRAB AGASSIZ WEST FIG 9-11216728 1092637 GRAB AGASSIZ WEST FIG 9-11216729 1092637 GRAB AGASSIZ WEST FIG 9-11216730 1092637 GRAB AGASSIZ WEST FIG 9-11216731 1092637 GRAB AGASSIZ WEST FIG 9-11216951 1149509 GRAB QV 25CM216952 1149509 GRAB QV 40CM216953 1149509 GRAB LARGE QTZ FLOAT216954 1149509 GRAB QTZ STR ZONE IN ALT GABBRO216955 1149486 GRAB QTZ STR IN VOLC NEAR GALBRAITH B
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
15-Jun-92
Page: lCopy: 1 of 1Set : 1
Attn= Mr. Wayne Holmstead Project: PO
Job: 924207T
Sample
8106810781088109811081118112811381148115
8116812181238124812581268127 812«81298130
8131813281338134218501218502218503218504
Received: 4-Jun-92 10:37
Status: FinaL
AU FA/AA3 PPb
12342418<5
197190<542<5
<55331238HO85
38913
362232
453181967
21451413
Roc
Au Calc. oz/T
<0.001<0.001<0.001<0.001<0.0010.0060.006<O.OO10.001<0.001
<O.OO10.002<O.0010.007O.O03O.OO20.011<0.0010.0110.007
0.013<0.001<0.001<O.O01<0.001O .006O.O15<O.O01
Rock Samples
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
15-Jun-92
Page: 2Copy: 1 of 1Set : 1
Attn: Mr. Wayne HolmsteaProject
Job:
Sample
2185O52185062185072185082185O9218510218511218512218513218514
2185152185162185172189512189527778577786777877778877789
7779077791777927779377794777957779677797
:
924207T
AuFA/AA3PPb
6177
118219
120612466466
1366<5666<5<5<5
71215<5<51369
AUCalc ._.OZ/J __
<O.OO1O.O05O.O34<O.O01O.004O.O18O.OO10.002<0.001<0.001
<O.OO1<0.001<0.001<0.001<0.001<0.001<0.001<o .001<O.OO1<0 .001
<0.001<0 .001<0.001<o .001<0.001<O.OO1<0.001< 0.001
PO #:
Rock Samples
Received: 4-Jun-92 10:37
Status: Final
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
15-Jun-92
Page: 3Copy: 1 of 1Set : 1
Attn: Mr Project:
Wayne Holmstead Received: 4-Jun-92 10:37PO
Job: 924207T Status; Final
Rock Samples
Au FA/AA3
Sample PPD
77798777997780077801778027780377804778057780677807
77808778097781077811778127781377814778157781677817
7781877819811781188119812O8122218518
7<56<5<5<51O1096
15696
16597<5<56
7151034916706
Au Calc . oz/T
<O.001<0.001<0.001<O.O01<O.OO1<0.001<O.OO1< 0.001<O.OO1<0.001
<O.001<O.O01<O.OO1<O.O01<O.O01O.O02<O.OO1<O.O01<O.O01<O.O01
<O.OO1<O.O01<O.001<O.O01<O.O01<O.O010.002<0 .001
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
15-Jun-92
Page: 4Copy: 1 of 1Set : 1
Attn: Mr. Wayne Holmstead Project:
Received: 4-Jun-92 10:37PO #:
Job: 924207T
77820778217782277823778247782577826778277782877829
Status:
AuFA/AA3
•** r^f^t*^
<530131667979
1146
AuCalc .oz/T
<0.001<O.O01<0.001<0.001<0.001<O.O01<0.001<O.O01<O.OO1O.O33
_Fin_al_
Rock Samples
77830 10 <0.001
ACCURASSAY LABORATORIES^ ^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
15-Jun-92HOLMSTEAD1074 Di llingham StreetKingston, ONK7P 2P4
Attn: Mr . Wayn©Project
Job:
Sample
81118112811681218123777987781277819
Sample
Sill8112811681218123777987781277819
Sa_mpjL_e_
8111811281168121
.:
924207T
MoI CAPPPm
754426
226
MnICAPpptn
109129407944118319189375
BiICAP
...__P.PnL_. _
589797192
Holmstead
CuICAPppm
1O9128370791
19912160673232
FeICAP%
1 .241 .223.819.181 .65
17.624.754.31
VICAP
.._PP1!
20194O69
Page:Copy:Set :
51 of 1
2
Received: 4-Jun-92 1O:37
Rock
PbICAPppm
836<14
21283
AsICAPppm
44662643
CaICAP%
O.12O .141 .643 .72
PO #:
Samples
ZnICAPppm
1310319210
481320O202
Hg . .ICAPppm
121
<11122
PICAP%
<O.O1<O.O1O.O20 .02
AgICAPppm
0.50.60.61 .42.21 .51 .20.3
SrICAPppm
121961525
10
LaICAP_ppm
2332
Status:
NiICAPppm
4444729230147
" 12269
CdICAPppm
<1<2<11<158
<1
CrICAPppm
424393243164
Final
CoICAPppm
17162741151377936
SbICAPppm
541
<34
1032
MgICAP%
O.220.290.322.24
ACCURASSAY LABORATORIES^ ^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HGLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
15-Jun-92
Page: 6Copy: i of 1Set : 2
Attn: Mr. Wayne Holmstead Project: PO
Received: 4-Jun-92 IO-37
Job: 924207T Status: Final
BiICAP
SampIe ppm_
8123777987781277819
Sample
81118112811681218123777987781277819
Sample
81118112811681218123777987781277819
<4213
BaICAPJBEm __
67142913342272
BeICAPppm
1112
<1112
V ICAP ppm
13 32 22 55
Ti ICAP
Rock Samples
Ca P ICAP ICAP
0.47 0.23 0.57 0.68
B ICAP
0.01 0.03 O.O6 O.03
Al ICAP
La ICAP ppm
3
18 5
Na ICAP
Cr ICAP ppm
326 150 234 201
Si IC~AP
% ppm % % %
00O0oo00
.02
.02
.10
.05
.09
.09
.09
.16
212166
564118
2292681231
00110001
.32
.37
.70
.71
.12
.72
.44
.12
00000
<00o
.01
.01
.18
.02
.02
.01
.05
.03
00O0O00o
MgICAP
0.14 O.37 0.17 0.45
W ICAPppm
.05
.04
.06
.08
.01
.01
.06
.03
<2282
< 11111211
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Diiiingham streetKingston, ONK7P 2P4
16-Jun-92
Page: lCopy: l of 1Set : I
Attn: Mr. Wayne Holmstead Project:
Received: 10-Jun-92 11:57PO
Job : 924230T Status: Final
Sample
21851921852O218521218522218525218526218527218528218529218530
218531218532218533218534218535218536218537218538218539218540
2185412185422185432189552189562189572189588136
AUFA/AA3PPb
241213
20939392528399
1889829
1512
14612157
79
3110265151058
Rock Samples
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD 1074 Dillingham Kingston, ON K7P 2P4
Street
16-Jun-92
Copy: i of 1Set : 1
Attn: Mr Project:
Wayne Holmstead Received: 10-Jun-92 11:57PO #:
Job: 924230T Status: Final
Rock Samples
Sample
8137813881398140814181428143814481458146
8147814881498150815181528153815481558156
815781588159816081618135
Au FA/AA3 PPb
65111
97
13349182821
9139<5<5282499
5050324
99
<5154391O7
Sediment Samples
218523
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1O74 Dillingham StreetKingston, ONK7P 2P4
16-Jun-92
Page: 3Copy: 1 of 1Set : 1
Attn= Mr. Wayne Holmstead Project:
Job: 92423OT
POReceived: lO-Jun-92 11:57
Status: Final
Sediment Samples
AUFA/AA3
Sample ppb
218524 <5
ACCURASSAY LABORATORIES^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
I6-Jun-92
Page: 4Copy: 1 of 1Set = 2
Attn: Mr. Wayne Holmstead Project: PO #:
Received: 10-Jun-92 11:57
Job: 924230T Status: F1na1
Sample
218527218533218539218540218541218542814181568135
Sample
218527218533218539218540218541218542814181568135
Sample
218527218533
MoICAPppm
65
115
147486
MnICAP
__pjpjp2329113104207221646196637473
8iICAPPP_m
<3<3
CuICAPPPm
156O396
112855815441
193289
9
FeICAP%
9.596.406.264.O15.3310.522.354 .63
12.38
VICAPppm
33106
Rock S
PbICAPppm
192823222423194025
AsICAP_ppm
82235192124101820
CaICAP%
0.421 .31
samples
ZnICAPPPm
47588
739221864911912842
HgICAPPPm
<3<3<3<3<3<3<3<3<3
PICAP%
O.040.03
AgICAPppm
0.82.41 .71 .31 .21 .3O.51 .11 .6
SrICAPppm
99
2210252784
10
LaICAPppm
2< 1
NiICAPppm
14959
125912925697823
CdICAP
__jP_pm
42
21125
< 113
CrICAP
. PPm ..
29O181
CoICAPPpm
1233895453842244865
SbICAPppm
31418165
24677
MgICAP%
0.421 .96
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
16-Jun-92
Page: 5Copy: 1 of 1Set : 2
Attn: Mr. Wayne Holmstead Project:
Job:
PO #:
Sample
218539218540218541218542814181568135
Sample
218527218533218539218540218541218542814181568135
Received: lO-Jun-92 11:57
Status:___Final
Bi ICAP ppm
BaICAP
J2P.QL.
V ICAP ^Pm
<3<3<3<3<3<3<3
Ti
794O
1152904192
178
ICAP
213251202322152725
%
000000000
.10
.15
.01
.11
.09
.16
.06
.12
.25
Rock Samples
Ca P ICAP ICAP % %
0.1 .3.4.0.0.0.
AlICAP%
0.2.2 .1 .2.4 .1 .1 .1 .
726OO960523582
O34901642672219743
0.080.03O.090.030.020.030.04
NaICAP%
0.01<O.O10.060.030.05<0 .010.04<O.01<O.O1
La ICAP ppm
SiICAP%
0.0.0.0.0.0.0 .0.0.
41
15<1<1<1<1
03O406040604020203
Cr ICAP ppm
1241638562
170• 393120
WICAPppm
1811
21512414298
MgICAP %
1 .1 .1 .3.0.1 .1 .
BeICAPppm
20419213666536
132137134
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD 1074 Dillingham Kingston, ON K7P 2P4
Street
16-Jun-92
Page: 1Copy: 1 of 1Set : 1
Attn: Mr. Uayne Holmstead Project:
Received: 22-May-92 O7:59PO
Job: 924157T
Sample
77740777417774277743777447774577/46777487774977750
77751777557775777758777597776077768777697777077771
7777277773777747777577776777777777877782
AuFA/AA3
___£Rb ——
<565685272128<521<5
496
<51243<577
46<5
<5155O226945438
7<56
Status:___Final
Rock Samples
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
16-Jun-92HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
Page: Copy:Set :
i of21
Attn: Mr. Wayne Holmstead Project:
Received: 22-May-92 07:59PO
Job: 924157T
Rock Samples
Sample
777837778477785
AuFA/ A A3 ppb
<5 10 <5
ACCURASSAY LABORATORIES^ ^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1O74 Dillingham StreetKingston, ONK7P 2P4
16-Jun-92
Page: 3Copy: i of 1Set = 2
Attn: Mr. Wayne Holmstead Project: PO #:
Received: 22-May-92 O7:59
Job: 924157T .Status: __Final
Sample
77747777527775377754777567776177762777637776477765
7776677767777797778077781
Sample
777477775277753777547775677761777627776377764
AuFA/AA3PPb
8536<513<5
174<5<512<5
856712<5<5
Co1CAPppm
2217241318751«1O
MoICAPppm
151383172256
9774
353
MnICAPppm
4521O7O101410591139
552159
2650
Rock :
CuICAPppm
31636183
1191059
146
7291114461302O6
FeICAP%
7.744 .093.955 .096.650 .560.26O .681 .44
Samples
PbICAPppm
61417175222
1127
1917159
21
AsICAPppm
9<2<2684
<2<27
ZnICAPppm
31503056.
103635319
5150551852
SrICAPppm
713434121
71154
AgICAP
_fipm
1<000
<07
,<o<001
01000
CdICAPppm
.5. l.2.6. 1.2.1. 1.3.5
.6
.5
.6
.2
.6
111111
(1< 1( 1
NiICAPppm
37698113579421911433O
2755803322
SbICAP_ppm
31O1O7
<259<2<2
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
16-Jun-92
Page: 4Copy: 1 of 1Set : 2
Attn: Mr. Ulayne Holmstead Project: PO #:
Received: 22-May-92 07:59
Job : 924157T Status: Final
Sample
777657776677767777797778077781
Sample
77/47777527775377754/77567/7617776277/6377/6477/65
///6677/6777779///80/7/81
Co Mn ICAP ICAP ppm ppm
112525864
8iICAPPPm
12<3<3<3<3<35
<3<3<3
<3<3<3<3<3
60647
119504197182
VICAPPpm
12526313914817841910
1212634965
Rock Samples
Fe As ICAP ICAP % ppm
1 .390.691 .503.3O2.493.77
CaICAP%
1 .156.876 .275.14O.350.02O.O10.030.012.04
0.060.540 .930.240 .47
126
111177
PICAP%
0.030.010.010.01O.O3<O.O1<O.O1O.02<O.010.03
0.02<O.010.01O.O10.03
Sr ICAP PPm
76795310
LaICAPppm
1111
<1< i10< 112
41
< 1< 12
Cd Sb ICAP ICAP ppm ppm
<1< i< 1<1< 1<*
CrICAPPPm
1417711193184489244100568176
324288334206121
4<2<2<2<2<2
MgICAP%
O.642.541.972 .462.60O.O4O.010.07O.020.70
0.02O .161 .320.810.58
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
16-~Jun-92
Page: 5Copy: 1 of 1Set : 2
Attn= Mr. Wayne Holmstea>Project
Job:
Sample
77747777527775377754777567776177762777637776477765
7776677767777797778O77781
Sarn_e.ie.
77747777527775377754777567/761777627776377764
:
9241S7T
BaICAPPPm
1411122014123181723
14476
18
HgICAP
....._PPJ!IL__-....-
<3<3<3<3<3<3<3<3<3
TiICAP%
0.270.01<0.010.010.14<0 .01<0.01<O.O1<0.01<0.01
<0.010 .01O.070.120.21
POReceived: 22-May-92 07:59
Status: Final
Rock Samples
AlICAP%
1 .071 .331 .471 .802.770 .050.02O.210.080 .20
O.O90 .591 .61O .981 .05
NaICAP%
O.O2O.010.030.060.01<O.O1<0.01<O.01<0.010.06
0.05<0.010 . 02O.030.04
siICAP%
O.O70.040.050.070.040.020.010.020.05O.O4
0.040.030.05O.O80.07
WICAPPPm
2934
<2<2
- <2<2<2<2
<2<2<2<2<2
BeICAPppm
31114<1<1<111
1122.2
ACCURASSAY LABORATORIES^ ^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
16-Jun-92 HOLMSTEAD1074 Dillingham Street Page: 6 Kingston, ON Copy: 1 of 1 K7P 2P4 Set : 2
Attn: Mr. Wayne Holmstead Received: 22-May-92 07:59 Project: PO tt:
Jobi__-_224_i§ZI_________________________________Status: Final__..
Rock Samples
Sample
7776577766777677777Cy
7778077781
Hg ICAP ppm
<3<3<3<3<3<3
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1O74 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 1Copy: 1 of 1Set : 1
Attn: Mr Project:
Wayne Holmstead Received: 12-May-92 16=58PO
Job: 924123T Status: Final
Rock Samples
Sample
77651776537765477655776567765777660776617766377666
77667776687766977670776717767277673776747767577678
7/68O77681776827768377684776857768677687
AuFA/AA3_P£t>
<5<5
147<5<5<5<59
<5<5
<5171294288
<528612
61141
11167<57<5
AuCalc .oz/T
<0.001<0.001O.OO4<0.001<0.001<0 .001<0.001<0.001<O.O01<0.001
<O.OO10.005(0.0010.001
<0.001<0.001<0.001<0.001<0.001<0.001
<o .0010 .033
<0.001<0.001<O.O01<o .001<O.OO1<0.001
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
. PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1O74 Diliingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 2Copy: 1 of 1Set : 1
Attn: Mr. Wayne Holmstead Project:
Received: 12-May-92 16=58PO
Job: 924123T Status: Final
Sample
77689776907769177692776937769477696776977769877699
77700777017770277703777047770577707777087770977712
7771377714777157771677717777187771977720
Au FA/AA3 ppb
7<5<5<528
12356<5<5<5<5
<5144<51188
<5<5<5<5
<59V<576
<5<5
Au Calc . oz/T
<0<0<0<0<0O
<O<0<O<0
<00
<0<0<0<0<o<0<0<0
<0<0<0<0<0<0<0<0
.001
.001
.001
.001
.001
.360
.001
.001
.001
.001
.001
.004
.001
.001
.001
.001
.001
.001
.001
.001
.001
.001
.001
.001
.001
.001
.001
.001
Rock Samples
ACCURASSAY LABORATORIES^ ^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD 1074 Dillingham Kingston, ON K7P 2P4
Street
18-Jun-92
Page: 3Copy: 1 of 1Set : 1
Attn: Mr. Wayne Hoimstead Project:
Received: 12-May-92 16:58PO
Job: 924123T Status:
Sample
77721777227772477725777267772777728777297773177732
7773477735777367773777738
AuFA/AA3Ppb
11<5<5<5<59
<5<5<560
28719O1
1180205718897426
AuCalc ._2ZZ!__
<0.001<0.001<O.O01<0.001<0.001<0 .001<0.001<o .001<0 .0010.002
O.O080.0553.4421 .6682 .842
Final
Rock Samples
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 4Copy- i of 1Set : 2
Attn: Mr Project:
Job:
Wayne HolmsteadPO
Received: 12-May-92 16:58
Status: Final
Sample
77652776587765977662776647766577676776777767977688
776957771O7771177723777307773377739
Sample
77652776587765977662776647766577676
AU FA/AA3 ppb
421580<567
129
<56
<577<512<5
45860
NiICAPPPD)
265790213853431
Au Calc . oz/T
0.001<O.OO10.002<O.OO1<O.OO1<0.001<O.O01<O .001<0.001<O.O01
<0.001<O.O01<0.001<O.OO1<O.001<O.O011 .338
CoICAPppm
13339519432014
Rock £
Mo ICAP ppm
241< 1< 1< 13
<1237
<1422324
MnICAP
__EEnL___ _
23215117244027571
258
Samples
Cu ICAP ppm
156154
136723
1811144331863936
4987718716176939
56772
FeICAP%
3 .023.157 .813.054 .272.043.86
Pb ICAP ppm
4<2<22
<22
32<294
<2<25<2<2<2<2
AsICAP
2<2<25
<225
Zn ICAP ppm
14232587305
~ 3441063
2719
89552111634718
563
HgICAP
—BPm _ _ _
<3<3<3<3<3<3<3
AgICAP ppm
0.10.30.80.20.30.10.50.60.20.2
0.10.30.20.60.30.4
72.9
SrICAPPP_m
316361116234
ACCURASSAY LABORATORIES_ ^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAO1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 5Copy: 1 of 1Set : 2
Attn: Mr. Wayne Holmstead Project:
Job: 924123T
Sample
77677776797768877695777107771177723777307773377739
Sample
77652776587765977662776647766577676776777767977688
776957771O7771177723
Ni ICAPppm
49203819613628157085
CdICAPjppm
<1< 1< 1< 1< 1< 123
< 11
<!32
< 1
Co ICAPPPm
166
16314116178
1936
SbICAPppm
45<2<2<23<2<2<26
<2<2<2<2
PO #:
Rock Samples
Mn Fe ICAP ICAPppm
322605315868137607299
175993
BiICAPppm
<3<3<3<3<3<3<3<3<3<3
<3<3<3<3
%
6.201 .90O.954.043.803.076.994.154.0912.15
VICAPppm
30305966642044842916
462O3462
Received: l2-May-92 16:J
Status: Final
As ICAPppm
4<22<2<2<2<2<2<2<2
CaICAP%
0.250.210 .360.320.360.210.110.220.07O.04
0.55O.13O.160.43
Hg ICAPppm
<3<3<3<3<3<3
' <3<3<3<3
PICAP%
0.020 .030 .06O .080.020.030.030 .030.020 .01
O.07O .040 .02O.05
Sr ICAPppm
31O297663
281
LaICAPppm
1< 1< 112< 1< 15
< 121
<17
< 1< 1
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 6Copy: 1 of 1Set : 2
Attn : Mr . Wayne Project :
Job: 924123 I
HolmsteadPO #:
Received: l2-May-92 16:5!
Status: Final
Rock Samples
Sample
777307773377739
Sample
77652776587765977662776647766577676776777767977688
7/69577/107771177/237773077/3377/39
CdICAPPPm
<1<13
CrICAPPPm
347341187528192212168360322461
196268356118/9113222
SbICAPPPm
<2<2<2
MgICAP
___% ____ .
0.22O.410.442.461 .890.191 .261 .170.130.06
0 .290.260.321.71O.46O .890.16
BiICAPppm
<3<3
2180
BaICAPppm
159017
20423221413103
1513143314756
VICAPppm
292810
TiICAP%
0.070.110.14O.17O.130.070.160.100.070.03
0.19O.100 .130.120.140.010.01
CaICAP%
0.300.430.05
AlICAP%
0.340.450.671 .361 .130.331 .361 .460.250.10
0.450.420 .522.38O.840.850.23
PICAP%
0.030 .21O.O1
NaICAP%
O.O10.010.01o .010.010.020.01O.O10.010.02
0.030 .010.010 .040.01O.O10.01
LaICAPppm
<11
<1
SiICAP%
0.010.010.01O.010.010.010.010.010.01O.01
0.010.010.010.010.010.010.01
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD 1074 Diilingham Kingston, ON K7P 2P4
Street
18-Jun-92
Page: 7Copy: 1 of 1Set : 2
Attn: Mr Project:
Wayne Holmstead Received: 12-May-92 16:58PO
Job: 924123T Status: Final
Rock Samples
Sample
77652776587765977662776647766577676776777767977688
77695777107771177723777307773377739
W ICAP ppm
37435<2<2<2<2<2
<2<2<2<2<2<2<2
Be ICAP _ppm
11121
<111
<1<1
1<11111
<1
ACCURASSAY LABORATORIESA DIVISION OP A55AY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
l8-Jun-92
Page: 8Copy: 1 of 1Set : 3
Attn: Mr. Wayne Holmstead Project: PO #:
Received: l2-May-92 16:58
Job: 924123T St-a.tu[§_:___Final
Soil Samples
Sample
#O1#02#03#04#05#06#07#08#09#10
#11#12#13#14#15#16#17#18#19#20
#21#22#23#24#25#26#28#29
AuFA/AAPPb
22131015812<917<6<8
<6<6832814121O12<9
<1610139
<6<6128
MoICAPppm
1232
< 1< l< 1< 11
<1
<1< 11222
< 1231
3211
< 111
< 1
CuICAPppm
12867911058516214176317
545476427313772917333
451991847446105993
PbICAPppm
<2<29<25<2710<210
10676
10174141316
93
117
<21037
ZnICAPppm
22327250
22319353476749
65423753444133877149
7768
11273
1153O6136
AgICAPppm
0.30.2O.20.30.20.2
" O.IO.I0.20.3
0.20.10.10.20.10.30.20.40.21 .3
0.40.20.40.30.10 .30 .2O .3
NiICAPppm
45
13114298119
294
121O4134142323197
51533527539
1815
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 9Copy: 1 of 1Set : 3
Attn : Mr . Wayne Project:
Job: 9241231
Sample
4*30
Sample
#01#02#03#04#05#O6#07#08#09#10
#11#12#13#14#16#16#17#18#19#2O
#21#22
AUFA/AAppb
<6
CoICAP
__ppm
<1<135
16771411123
865969
1813126
4226
Hoimstead
MoICAPppm
2
MnICAP_ppm
38419547
43O36281215634220145
8862781146655
17911193152
1476884
Soil
CuICAPppm
35
FeICAP%
2 .504 .172.903 .023 .885.201 .341 .242.521 .77
2 .312 .531 .573 .192.922 .692 .672.783 .611 .15
3 .143 .05
PO #:
Samples
PbICAPppm
5
AsICAPppm
<2<263
<2<2<2<25<2
4<23561046710
85
Received: 12
Status :
Zn AgICAP ICAPppm ppm
30 0
Hg SrICAP _ ICAPppm ppm
<3<3<3<3<3<3<3<3<3<3
<3<3<3<3<3<3<3<3<3<3
<3<3
-May-92 16:5!
Final
NiICAPppm
.4
CdICAPppm
445491098
116
4334447864
813
1O
<1<1<1<12<11111
111
<1<1<11112
1<1
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 10Copy: i of 1Set : 3
Attn: Mr Project:
Ulayne HolmsteadPO #:
Received: 12-May-92 16:58
Job: 924123T Status:___F i na 1
#23#24#25#26#28#29#30
#01#02#03#04#Ob#O6#07#08#09#1O
#11
#13#14#lb#16#!/
Co I CAP ppm
14229298
154910
SbICAP
.-BE™
<2<236353<2<2<2
<2<274422
Mn ICAP ppm
101635631494104316935291
BiICAP
_.PJ?m.
<3<3<3<3<3<3<3<3<3<3
<3<36<3<363
Soil !
Fe ICAP %
3.872.534.411 .883.112.361 .39
VICAP
_p.e.m .... ..45665252707425255537
39523063503167
Sample
As ICAP ppm
CaICAP%
0.0.0.0.0.0.0.0 .0.0 .
0.o .0.0.0.o .0 .
!S
<22
<2<25<23
04040604131718111506
05040505O6O423
Hg ICAP ppm
PICAP%
0.0.0.0.0.0.0.0.o.0.
0 .0.0.0.0.o .0.
<3<3<3<3<3<3<3
03050709110903020305
060108040605Ol
SrICAP Ppm
8837675
LaICAPppm
55775
117
1047
1369671O7
Cd ICAP ppm ...
<1<1<12
<111
CrICAP_p_pm
18242625644717194416
20311434202853
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Diilingharn StreetKingston, ONK7P 2P4
18-Jun-92
Page: nCopy: 1 of 1Set : 3
Attn: Mr. Wayne Holmstead Project: PO #:
Received: 12-May-92 16:58
Job: 924123 Status: Final
Sample
#18 #19 #20 #21 #22 #23 #24 #25 #26 #28
#29 #30
Sample
#O1#02#03#04#05#06#07#08#O9#10
Sb ICAP ppm
2 2 2 22 2
<2 <2 <2 3
7 2
MgICAP%
0000o0000o
.13
.09
.24
.16
.83
.26
.21
.28
.76
.17
Soil Samples
Bi V Ca ICAP ICAP ICAP ppm ppm %
5 36 3
<3 <3 <3 <3 3 <3
<3 <3
Ba ICAPPP.m
10011578
10413522787836499
31 7126 51 58 54 43 98 23 69
40 31
Ti ICAP%
00000o0ooo
.01
.03
.04
.03
.14
.05
.03
.04
.12
.03
0.10 0.06 0.07 0 .16 0.38 0.17 0.24 O.ll 0.11 0.12
0.15 0.10
Al ICAP%
2122320121
.01
.92
.73
.97
.20
.98
.71-Ol.10.11
P ICAP
0.03 0.04 0.06 0.04 O.O6 0.08 0.05 0.02 0.01 O.03
0.04 0.02
Na ICAP%
0.010.010.01O.010.010.010.01O.010.01o .01
La Cr ICAP ICAP ppm ppm
7 26 6 44 7 14 4 5O
18 38 10 35 8 28 2 132 4 22 8 37
9 19 4 14
Si Ul ICAP ICAP%
000000o0o0
F
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
spm
<2<2<2<2<2<2<2<2<2<2
#11 O .19 154 0 .02 1 .93 O.O1 0 .01 <2
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 12Copy: 1 of 1Set : 3
Attn: Mr. Wayne Holmstead Project: PO #:
Received: l2-May-92 16=58
Job: 924123T Status: Final
Sample
#12#13#14#15#16#17#18#19#20#21
#22#23#24#25#26tt^8#29#30
SampJLe.
#01#02#03#O4#O5#06
Mg ICAP
0.0.O.0.0.1 .0.0.0.0.
0.0 .o .1 .0.o.o .0 .
BeICAP
_EEBL_
25083613190329411265
2214347630412121
-—
121222
Ba ICAP ppm
71904991
13345
1369972142
2251461551165411911189
Soil Samples
Ti Al ICAP ICAP
0000000000
0O00O000
.04
.01
.05
.02
.02
.04
.05
.06
.01
.04
.03
.03
.04
.12
.03
.06
.04
.03
1121212202
32130211
.39
.54
.30
.97
.70
.77
.85
.70
.85
.25
.42
.25
.83
.15
.69
.23
.44
.06
Na Si W ICAP ICAP ICAP % % ppm
00O00000o0
00ooo0o0
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
0.010.010.010.010.010.01O.010.010.010.01
0.010 .010.01O .010.010 .01O.O10 .01
<2<24<252
<23
<22
4<2<2<2<2<2<2<2
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 13Copy: 1 of 1Set : 3
Attn: Mr Project:
Wayne Holmstead Received: 12-May-92 16:58PO #:
Job: 924123T Status: Final
Soil Samples
Sample
BeICAP pp.m
#07#08#09#10#11#12#13#14#15#16
1111211212
#17#18#19#20#21#22#23#24#25#26
2221122121
#28#29#30
211
ACCURASSAY LABORATORIES^ A DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1O74 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 14Copy: 1 of 1Set : 4
Attn: Mr. Uiayne Holmstead Project: PO # '-
Received: l2-May-92 16:58
Job: 924123T Status :____Final _
Sample
BG01BG02BG03BG04BG05BG06
Sample
BG01BG02BG03BG04BG05BG06
Sample
BG01BG02BG03BGO4BG05BGO6
AU NA
ppb
6223
1024
NiNA
ppm
<20<20<20<20<2051
AgNA
ppm
<2<2<2<2<2<2
Na NA
<0<0<0<000
ZnNA
ppm
CdNA
ppm
Humus 5
Ca NA
.01 O.7
.01 <0.5
.01 0.7
.01 <0.5
.11 1.8
.79 1.0
AsNA
ppm
41 <156 <122 <143 <1<2O 1<2O 4
SbNA
ppm
<2 <0.1<2 0.1<2 0.2<Z < 0 . 1<2 0.4<2 0 .5
Samples
Sc NA ppm
<0.2<0.2<0.2<0 .24 .59.6
SeNA
ppm
<2<2<2<28
<2
BaNA
ppm
<100<100<10010014068O
Cr NA ppm
2112
188O
BrNA
ppm
12321O3
LaNA
ppm
< i< 1< i2344
FeNA
<0<0<0<001
RbNA
ppm
CeNA
EP.m
.05
.05
.05
.05
.39
.51
<20<20<2O<20<2030
<1< 1< 1< 13453
Co NA ppm
MoNA
ppm
<0<0<0<01
<0
SmNA
ppm
<0<0<0<035
<1<1< 1<1416
.5
.5
.5
.5
.O
.5
.1
.1
.1
.1
.4
.1
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORIES SERVICES LTD.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
18-Jun-92
Page: 15Copy: 1 of 1Set : 4
Attn: Mr. Wayne Holmstead Project: PO #;
Received: 12-May-92 16:58
Job : 924123T Status: Final
Humus Samples
Sample
TaNA
ppm
W IrNA NA
ppm ppb
HgNA
ppm
ThNAppm
UNA ppm
BG01 8G02 BG03 BG04 BG05 BG06
<0.5 <0.5 <0.5 <0.5 <0.5 1.0
21
<0.5 <0.5 <0.5 <0.5 <0.5 <0.5
<0.5<0.5<0.5<0.53.36.6
1 .6 2.7
ACCURASSAY LABS^ A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HULMS i b.AO 1 o/ 4 L> A i i 1 ng na.rn Kingston , ON K/P 2P4
t r eet, Page: 1Copy: i of 1Set, : 1
At,tn: Mr Project.:
Wayne Hoimsteaci Received: 24-Juri-92 11:44PO
Job Status: Final
sa.rnjD.Le.
AU. hA/AA3
........ep..!?...-.......IbO
/bb
1 b <b <b 64
<b <b
4 V 6
Rock Samples
ACCURASSAY LABS^ ^ A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HULMSI LAD1 o / 4 \.j i JL 11 n g n a (ii b t r e e tKingston, ONK/P 2P4
Page: Copy:bet :
i of
Attn: Mr. Wayne Hoimstead Project: PU
Keceived: 24-Jun-92 11=44
Status: Final
Hock Samples
Sample..
...18546
218548218549
2 1 H / b b
218/b/
218/6O 2.18/61
218/63
Au hA/AAb
<b
24 13 <b <b <b <b 6
1O <b
<b I ; <b
1622 1 b < b <b
ACCURASSAY LABSJ^ A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HOLMS i t.Ai )10/4 I.) i i, i ing ham street ,\i ngston , ON K/P 2P4
Page: 3Copy: 1 of 1Set : 1
Attn: Mr . Project:
wayne Hoimstead Keoeiveci: 24-Jun-92 11:44po
Status Final
Kock Samples
AU A/AA3
<b 22
4V/1 /560
3326 /10 /52
25545 7-fS-
218/68
4V 10 < b
21 b i 2
ACCURASSAY LABSJL A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
l O/4 u.x l 1 1 ngharn street.K i ngston ; ONK/P 2P4
Ar.r,n= Mr. wayne HolmsteadProject: Pi) #:
.J0t>: V2428V 1
Kock Samples
MO cu Pb /. nA.CAP 1CAP 1CAH 1C AH
sample ppm ppm ppm ppro
8166 <1 3/ l/ 3281/4 < 1 V82 b4 2881/b 4 248 bl 3OO81/6 3 Ibl 28 Vb818.1 1 18b I/ /48.184 6 1 36 b 16 bO218b44 3 264 23 6V218b4b 2b 24O 2 4()2l8b48 2 431 4 4221 88b3 1O 4O'-/ 3 3O
M n t- e As H gJ. CAP 1CAP 1C AH 1C AH
Sample ppm % ppm pprn
3166 13'-xb 6.00 <2 <3ol/4 bbb 13 .62 1C) < 3Hi. ,/b 3^X 4 ,. /b 16 <3Hi / t^ 4O/ 4 . r~> ,.' S< < .-!
o i H i 86O 6-33 6 < 3Hi 84 432 6 . 2tr> / <3
2 J H:->44 323 .".-, . 4/ / <3
21 8;. 4::, ;i.o4^ o . oo \2 < 3,/ i H--,4H ] bn;-, i O .31 <2 <3218HSH 3Vo 4 . 4'H / < >:
Page : 4c.opy : 1 of 1Set : 2
Received: 24-Jun-V2 11:44
AgiCAHppm
< o . ;i< O . 1O .4
< O . 1< O . 10 .6
< 0 . 1< O . 1< O , 1O .2
Sr1C AHpprn
2420;i i2b
i ,-i1 8
4 '~i \
1286V
Status: hi nal
(Ni Co1CAP 1C AHppm ppm
33 16V 4
4O 2262 2336 2224 2124 13
28 b 41b3 b3bl bV
Cd Sb1CAH 1CAHpprn Ppm
< 1 < 2< 1 6
1 1 1< 1. 3
< 1 < 2{ I, .' '
< 1 4\ ] <. /
<. 1 < 2
< J 3
ACCURASSAY LABS^ A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HOLMS 1 t.Al)l o / 4 i)i i i i n g r, a in s r r e e r.Kingston , UNK/P 2P4
Attn: r-rr . wayne HolmsteaaProject. :
Job : 9242b9 1
tii. Vit; AH it; AH
Sample ppm Ppm
b!66 <3 6/bl/4 <3 13/bl/b b 3bbl/6 b b4blbl <3 1O6blb4 b 2O221bb44 <3 /b2Jbb4b <3 9/2ibb4b <3 3/b2). bbbb b 93.
hi a 1 lI.CAH K;AP
Sample pprn %
M J. f-> l-> 2 4 O . (.).-'
bl/4 3 0 , J. 3
M i ../.'> I/' 0 . IV
bl/6 !T, v) . 2/H ! H i i 6 O .24blb4 4b O . J22.1 w',44 42 o . 302 !.bb4'. b 0 .042 1 H-4H riO O . l;i
21 bbbb 2V O . 21
Rock
Cait; AH
-if,
4 .980 . 9 10 . 6/O . 6O1 .03O .490 .33V .43b . 1 61 .33
AlK;AH
•"n
O . A)i .6b0 . IbJ . b /2 . 6()J . / bI . 6 32 .O/
2 . VbA . 2 1
HO # :
Samples
p1CAP%
6 ./94 .433 .253 .444 .6/3 . 1 b3 .OO
1 b . /1 1 .O3 .69
NaJ.CAP-^
< O .O 1u> .0:1.O .060 .ObO .OlO . O3O .O/
\o . 01< O . O .1O . Ol
Page : bcopy : 1 of lset ; 2
Received: 24-Jun-92 11=44
status: Kinal
La. Cr Mgit; AH it; AH 1CAPppm ppm %
1 66 O.O/<1 54 0.81I/ 45O 1 .t)92 - 239 1.324 23O 1 . /Ii „ 139 1 .O«
A. 1 3 1 O 1 . 1 2
1 59O /.9/< 1 162 3.632 1/b 0.91
si w beJ.CAP 1CAP i(JAP"A pprn pprn
O .Ob <2 2o .03 b.i. 4O.O/ 26 2O . O4 / 2O .06 b 30.04 3O.O 6 / 2o . o;i < 2 .;0 .03 <2 VO . O3 < 2 2
ACCURASSAY LABS^ A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
KocK Samples
ACCURASSAY LABSA DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
Copy: 1 OT
Keceived : 7-J'ui-92 07 : 4 1
Status: Final
Au. FA/AA3
KOCK Samples
ACCURASSAY LABSA DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
.1 O f 1
K e c e i v e ci: / - J LI 1 - '-> 2 07:41
Fi nal
sarnp i e
KOCK samples
Mo (,u •-' • / n Ag Ni1C AH ..LCAt-:i 1C«^ it; AH 1C AH 1C AHoom pofTi ooff. oor.i op in ppm
< 1 J.. 6 / < 2 f~> I 1 „ b 48< i '. •' /' •'•.-. \ ,.•; : . / 1,6 32
1 1HO S V4 <O.l 33
Co1C AHpom
;, ss 114
I - Ci
iCAHD D ffi
H/ r-U)
ACCURASSAY LABS^ A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
bt.at. us r i rial
ba i i1CAP iCAP
^ a rn o i a p o m .. jL.......
KOCK
A 1.(.CAP
X;
Samples
N a s iICAP .U..:AP
"o •'•::•
W beICAP i CAPppm pptn
ACCURASSAY LABSA DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P78 6G3
(807) 623-6448 FAX 623-6820
HOLMSTEAD1074 Dillingham StreetKingston, ONK7P 2P4
28-Jul-92
Page: iCopy: 1 of 1Set : 1
Attn: Mr. Wayne Holmstead Project:
Job: 924343T
POReceived: 13-Jul-92 ll:4O
Status:___Final
Sample
2181012181O22181O32181042181052181062181072181O8218109218110
21811121811221811321811421811521811621811721811821811921812O
218121218122218123218124218125218896218897218898
Rock Samples
AuFA/AA3ppb
931404743315
151336281O
2369
18<51636
4656
135181
79
7022268497
163658206011O
ACCURASSAY LABS^ ^ A DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HOLMSTEAO1074 Dillingham StreetKingston, ONK7P 2P4
28-Jul-92
Page: 2Copy: i of 1Set : 1
Attn: Mr. Ulayne Holmstead Project:
Received: 13-Jul-92 ll:4OPO
Job: 924343T Status:___Final
Rock Samples
Sample
218899218900220401220402220403220404220405220406220407220408
0
2204O922041022O411220412218794218795218796218797218798218799
302301627O1366
652127
3683O86115
105701158O
218800 166
ACCURASSAY LABSJ^ A DIVISION OF ASSAV LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HOLMSTEAD 1074 Dillingham Kingston, ON K7P 2P4
Street
28-JU1-92
Page: 3Copy: 1 of 1Set : 2
Attn: Mr. Wayne Holmstead Project:
Received: 13-Jul-92 11--4OPO
Job: 924343T Status: Final
Sample
2181O7218H4218H522040922O41122O412
Sample
2181O7218114218115220409220411220412
Sample
2181072181142181152204O9220411220412
MOI CAPppm
953533
MnICAPppm
962538476
2192O2
BiICAP
_ epjn _...__ ._<3458
<3<3
CuICAPppm
2689697O9135359498
FeICAP%
2.713.212 .360.873 .894 .20
VICAPppm
447916163233
Rock S
PbICAP
-J2BSSL . .
2O6
1611119
AsICAP
._.P.pm
1817142O1410
CaICAP%
0.100.460.03O.O8O.310 .32
amples
ZnICAPppm
4144136
2920
HgICAPppm_
<3<3<3<3<3<3
PICAP%
O.llO.O60.020 .010.05O.O5
AgICAPppm
0.90.3O.82.11 .01 .1
SrICAPppm
75
<1<133
LaICAPppm
7<1<11
<1<1
NiICAPppm
431086842
- 6593
CdICAPppm
<1<1<1<1<1<1
CrICAP
_ epm_.____34
13935
1319O
108
CoICAPppm
215131182542
SbICAPppm
297
2421<26
MgICAP%
0.35O.7O0.150.080.53O.44
ACCURASSAY LABSA DIVISION OF ASSAY LABORATORIES SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HOLMSTEAO1074 Dillingham StreetKingston, ONK7P 2P4
28-Jul-92
Page: 4Copy: 1 of 1Set : 2
Attn: Mr. WayneProject
Job:
:
924343T
HolmsteadPO #:
Received : 13-Jui-92 ll:4<
Status:
Rock
Sample
21810721811421811522O409220411220412
BaICAP
_ ppm ,
183281O5453
TiICAP%
O.O.0.0.o.0.
1614O2O21917
AiICAP%
0.1 .0.0.0 .o.
441624139378
Samples
NaICAP%
O.O40.06<0.01<0.01<0.01<O.O1
SiICAP%
0.O.o.o.0.o.
020202 '020202
WICAPppm
7243
187
17
Final
BeICAPppm
<<
121111
Geochemlcal Lab Report
BONDAR-CLEGG
NUMES
920^213
'V.O < COV\.:!E )
ELE«fN; A! FeONUS PC< PCI
Kn HgPPS PCI
.JPROJECI: NONE
Ca NaPCI PCT
KPCI
ScPPN
VPPH
PAGt 1A
Cr CoODW OOW rrn rrn
0,08 i.030,23 i.CI0,51 1. 53
9^ 0.0^110 0,20:83 0,35
0,05 0.0^0. i3 0,040.70 0,04
0,030.030,08
<5<5<5
t(9
15
33 430 1053 K
Bondar-Clegj; & Company Ltd.5420 Oinotok Koail Ottavu. < !»KM or, 2"•I: i MM 744 222(1
,\ i(i!3i 749-7170
Geochemical Lab Report
BONDARCLEGG
920708920721A9207215
SAMPLE ELEtfENf Ni NUMBER UNITS ??!»
Cu PPH
65147119
Zn P^M
911
As PPM
<5 <5 <5
PP!iY
PPH PAg
PP?iCd
PPH
<0.2 <0.2
Sn PPH
<20 <20 <20
PPH
k'gK & Company Ltd.54:0 Canolck Road Ollaua. < "" no Ki.l 4(i:•'Vi: (613) 749-;2:o
.iv: Kii3) 74M-7I70BONDARCLEGG
Geochemical Lab Report
REPCfT; 092-^17
SAMPLE NOKBER
920708 920721A 9207213
61.0 i. COv_E T E }
ELEMENT Te
<1°0
i i
Sd L3
PPii PPH
2 <1 4 <1
'•,PP(«
<20 <20
Pb PP?,
10Q
14
r.JPR
Si PP*
<5 <5
n ~'t , "' T i 'U J L _. ! , :
PPS
<5
<5
NONE PAGE 1C
Au PP5
1554 2969 3430
ACCURASSAY LABSr, D IVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
13-Aug-s>2HOLMS'I tAL.)10 74 OHKingstonK7P 2P4
A 1 1. n : W .Project :
1. 1 ngham, ON
street Page: iCopy: i of 1Set : 1
t. . Holmstead Received: lO-Aug-92 0V : 22
Job: 9244631
Sample
220413.'.20 4 142.2O415'22O41622O4172.204 1H22O4192 2O 4 2022O42122O422
22O42322O42422042522O42622O42722O42H,^.2042922043O22O43 I22043^
2204 So^<'O<1342^O4-ib22O4,-<'->22Oa.3/xVo4:-iH22O4o«sX2044O
A 1.1FA/AA3ppb
19V610
38 O7
/24«147
l/b2V25
1623654 lib34465
2O6911612
11. 735Hb
201 1«
4 bOOj . H94s- / f-> <'
7O1VI
106127
.1 2-^
PU ft :
Status: Final
KocK Samples
AnCalc .oz/T
<() . 001<0 .001<o .001<O .001O . 0 1 1<0 .001O . 2 1 10.004O . b 1 1<0 .001
O .4/41 .57b1 .00 50 .0060 .OO3«) .001<o .001O .05.!.O . OO3O .587
O . 1 '-1 J .O . O5bO . 0,-ij.O .O2O0 . OO3O . O31
<o .00 iO . O()4
ACCURASSAY LABS/•. D IVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HOLMS I (r.Al)10/4 Diiiingham streetKingston, ONK/P 2P4
13-Aug-92
Page: 2Copy : 1 of 1set = 1
Attn: W. Project:
Holmstead Received: iO-Aug-92 09=22Po
Job: 924463 Status:
Rock Samples
sample
220441?2044222044322044422O44522044622044/22044822044922O45O
2181262 1 8 1 2 /21812821812921813O2 J. 8 1 3 12181322 1 H .1. ^ : •}218.1.34218135
21813621813/218.1 ^o; 1 H 1 3V21814O2 1 3 1 4 12 1 8 1 4 2/ . 1. « .1. 4 S
AU FA/AA3
.._..£P_b— _..._
4/23677
61V8195
25318911825 /1OO99251296416
421123149161922241312
3O29/O
b^.^/195^92 i6^
556O44 2 1 82b2
1043 I/
AUCalc oz/
o .0.o .0 .o .o .o .0 ,0 .0 .
o .0 .o .<o .<o .<o .<o .<() .< o ..8 .
O .O ,O ,0 .1 .o .o .3 .
T
138020152O060/4260241295/33IS./
OO1033OO400 1OO 1001OO1OO 1O0183 /
153OO61 1 4002622123OO804:-!
ACCURASSAY LABSr. DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HULMS It. A U1 074 o 1 1 l 1 n 9 h a rnKingston , ONK/P
Street
13-Aug-92
Page: 3Copy: i of 1Set. : 1
Attn: W . tv Project:
Hoimsteacl Received: 10-Aug-92 O9:22PC
Job : Status: Final
Rock Samples
A LI
PA/ A A3AU
Calc.
218144:M81452181462 1814 7218148
266221585/33111/
77
O .0070 .646O .1670.0330 . 002
ACCURASSAY LABSA D IVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
HOCK oampies
r> t- 3 t - U : i - \~ 1 )"l ':'• L
ACCURASSAY LABSA D IVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
1 o r .!..
l- ina i
KOCK bampies
ACCUR ASSAY LABS,-. D IVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
OT
KOCK Samples
.inai
ACCURASSAY LABS. D IVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
(807) 623-6448 FAX 623-6820
I i. VIQ i "I -3 fi'l '~> r. 1" £'• <-: I JI --J
H U
• A/ HA--i
....ee.ii..................
Samples
APPENDIX 2
DIAMOND DRILL LOGS
N -*• 8
$ 0
0
0
O p °. 4
£oo
^
8 L ^
cu n (»
^
i^
£. r
" O
|0 -V o 0 mtv
. A
HOLE # WT-92-01
CLAIM # : 1079876 PROPERTY : Menary Township Area, NorthTOWNSHIP: Menary NTS MAP #: 52 C/13GRID CO-ORDINATES: Line 35+45 N, Stn. 12+18 EAZIMUTH: 330 degrees INCLINATION: -75 degreesLENGTH : 55 feet OVERBURDEN : nilCASING : AGX core 1 3/16" ELEVATION : surfaceDATE DRILLED : May, 1992DRILLED BY : Nighthawk Diamond Drilling, Timmins OntarioDATE LOGGED : January 29, 1993LOGGED BY : C.A. Wagg, B.Sc.CORE LOCATION: Denbigh, Ontario
From(ft) 0.0
1.0
5.66
10.1
To(ft) Eield Name (legend) 1.0 Casing, loose bedrock
5.66 Variolitic, Pillowed BasaltWeakly to moderately foliated at 20 to 30 degrees to core axis. Foliation and varioles best developed near pillow margins. Pillow cores rather massive, fine to medium grained.
10.1 Feldspar Porphyry DykeFine grained. Weakly foliated at 40 to 50 degrees to core axis
55.0 Variolitic Pillowed Basalt
End of Hole
SAMPLES
Sample #77726 2.65
From 2.80
77727 10.0 10.5
To Width Description 0.15 2 inch wide quartz vein.
No mineralization. 0.5 Wedge shaped intersection of "F"
vein. Sample 60% quartz with trace fine gold.
C,lAJ=*
uuxA ?- v C
•^—
- (
?'/V
o ^.c,
HOLE it WT-92-02
CLAIM # : 1079876 PROPERTY : Menary Township Area NorthTOWNSHIP: Menary NTS MAP #: 52 C/13GRID CO-ORDINATES: Line 35 + 50 N, Stn. 12 + 10 EAZIMUTH: 160 degrees INCLINATION: -70 degreesLENGTH : 40 feet OVERBURDEN : nilCASING : AGX core 1 3/16" ELEVATION : surfaceDATE DRILLED : May , 1992DRILLED BY : Nighthawk Diamond Drilling, Timmins OntarioDATE LOGGED : January 30, 1993LOGGED BY : C.A. Wagg, B.Sc.CORE LOCATION: Denbigh, Ontario
From(ft) To(ft) Field Name (legend)
0.0 0.5 Casing, loose bedrock
0.5 40.0 Variolitic, Pillowed BasaltWeakly to moderately foliated at 60 degrees to core axis. Moderate to strong foliation and abundant varioles developed near pillow margins. Pillow cores rather massive, fine to medium grained.
End of Hole
SAMPLES
Sample # From To Width Description
No Samples
o < tf- I
0 K
\ (v b
0-
:̂ -
-\
',
RH" + T
iQ
^)
HOLE ff WT-92-03
CLAIM ff : 1 079876 PROPERTY : Menary Township Area NorthTOWNSHIP: Menary NTS MAP #: 52 C/13GRID CO-ORDINATES: Line 35+51 N, Stn. 12 + 11 EAZIMUTH: 125 degrees INCLINATION: -45 degreesLENGTH : 25 feet OVERBURDEN : nilCASING : AGX core 1 3/16" ELEVATION : surfaceDATE DRILLED : May , 1992DRILLED 3Y : Nighthawk Diamond Drilling, Timmins OntarioDATE LOGGED : January 30, 1993LOGGED BY : C.A. Wagg, B.Sc.CORE LOCATION: Denbigh, Ontario
From(ft) To(ft) Field Name (legend)
0.0
1.0
.0
25.0
CasingLoose bedrock.
Variolitic, Pillowed BasaltWeakly to moderately foliated at 60 degrees to core axis. Moderate to strong foliation and abundant varioles developed near pillow margins. Pillow cores rather massive, fine to medium grained.
End of Hole
Sample # 77728 11.0
From 11.6
To 0.66
77729 13.3 14.2 0.9
SAMPLES
Width DescriptionContorted 2 inch wide quartz vein
at 30 to 40 degrees to core axis,and altered wallrock.
6 to 7 inch wide quartz vein atabout 45 degrees to core axis.Trace pyrrhotite.
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IMPROVEMENT DISTRICT! OF i
Ministry ofNorthern Development
•d MinesOntario
Report of Work Conducted After Recording Claim
Mining A<
Personal information collected on this form is obtained under the authority of th this collection should be directed to the Provincial Manager, Mining Lands, Sudbury. Ontario, P3E 6A5. telephone (705) 670-7264.
52FWSWOOQ2 2.15292 MCLARTY" qn/-\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.- 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 Holder(s) Client No.
Address Telephone No.
C '7 /2 <C 0i Mining Division Township/Area M or G Plan No.
Dates From: TO d a
Work Performed (Check One Work Group Only)Work Group
I"
H
''Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other Authorized Work
Assays
Assignment from Reserve
Type
GEOLOGY / i> /: c s /v c-r/^f 6-
"7/1Total Assessment Work Claimed on the Attached Statement of Costs $ / ~> C
Note: 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 Address
A
(attach a schedule if necessary)
Certification of Beneficial Interest * See Note No. 1 on reverse side
I 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 Recorded Holder or Agent (Signatu/e)
Certification of Work ReportI certify that I have a personal knowledge of 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 of Person Certifying
Telepone No. Date" Certified By (Signature)
=or Office Use OnlyTotal Value Cr Recorded [Date Recorded
I Deemed Approval Date
'ate Notice for .Vnerfdrrfents Sent
Mining Recorder
Date Approved
Received.Slarnp , : />
JAN26b94PM
-*eS id 11 12 . 2345f .
l (C3 J'i
Ontario
Ministry ofNorthern Developmentand Mines
Ministere duCf ipement du Nordeiv , x mines
Statement of Costs for Assessment Credit£tat des couts aux fins du credit devaluation
Mining Act/Loi sur les mines
Transaction No./N° de transaction
Personal information collected on this form Is obtained under the authority M the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager. Minings Lands. Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.
Les renseignements personnels contenus dans la presente formule sont recueillis en vertu de la Lol sur let mines et serviront a tenir a jour un registre des concessions minieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains minlers, ministere du Developpement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/CoQts directs
Type
Wages Salalres
Contractor's and Consultant's Fees Drolls de ('entrepreneur et de I'expert- conseil
Supplies Used Foumltures utilities
Equipment Rental Location de materiel
Description
Labour Main-d'oeuvreField Supervision Supervision sur le terrain
Type 6£a.tG?/ rVo»jrcr/wG
Type ft.?5Ar
Co*i<><Jt44 Qt-£-
E ^PL-c ?,*£.£
Type6-(Lc>P4r*'c4L-
Amount Montant
<\t,m
11, ?2V5"?S
274
24i<2
Total Direct Costs Total des couts directs
Totals Total global
lj*» **«!•;;;:, ..i- ^'fflB-tr. J "-'
W»,
SjliEW$WP / *WNflF !^ -
PM* «*&;.*•m^&
2. Indirect Costs/Couts indlrects* * Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admissibles en tant que travaux d'evaluation.
Type
Tra Tra
importation "•^l.jc,':
}j$3&- JA^
AM789 10 1
4Food and Lodging Nourrlture et hebergementMobilization and Demobilization Mobilisation et demobilisation
DescriptionTypejV tWt'FgrH./i/X
— -' ^«JSjj|
2 6 WS4PM
1 12 1 23456 «
f}C(. 0/100X71 od
Ps-oD
Amount Montant
/%23 1
76-17 7<?c>7
Sub Total of Indirect Costs Total partlel des coflts Indlrects
Amount Allowable (not greater than 20% of Direct Costs) Montant admissible (n'excedant pas 20 H des couts directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and Allowable d'evaluation Indirect colt*) (ToMI dM eofttl direct*
Totals Total global
;ffc.-v!-'3i'»s*j. !
t&$l$$&
|*--i -:.,,-•",•
^.,7f5
l?6,7tltt Indlraets wtmlitlblM
iote: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 Jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux d'evaluation presentes.
•'illng Discounts Remises pour depot
. Work filed within two years of completion is claimed at 100% of the above Total Value of Assessment Credit.
1. Les travaux deposes dans les deux ans suivant leur achievement sont rembourses a 1 00 % de la valeur totale susmentionnee du credit d'evaluation.
:. Work filed three, four or five years after completion is claimed at 50% of the above Total Value of Assessment Credit. See calculations below:
olal Value of Assessment Credit Total Assessment Claimedx 0.50
2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a 50 % de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.
Valeur totale du credit d'evaluation Evaluation totale demandeex 0,50 -
Certification Verifying Statement of Costs Attestation de I'etat des coQts
hereby certify:ml the amounts shown are as accurate as possible and these costs /ere incurred while conducting assessment work on the lands shown n the accompanying Report of Work form.
lat as(Recorded Holder, Agent, Position In Company)
make this certification
J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.
I am authorized Et qu'a titre de je suis autorisd(titulaire enregistre, representant, poste occupi dans la compagnie)
a faire cette attestation
Signature
:12(04W1) Nota : Dans cette formule, lorsqu'l! dtolgne des pel , le HNisculin est utilise au sens neutre.
itario
Ministry ofNorthern Developmentand Mines
Ministere duDeveloppement du Nord et des Mines
Geoscience Approvals Office 933 Ramsey Lake Rd. , 6th Fl, Sudbury, Ontario P3E 6B5
Telephone: (705) 670-5853 Fax: (705) 670-5863
Our File: 2.15292 Transaction #: W9410.00004
June 27, 1994
Mining Recorder Kenora
Dear Mr. Rivett:
RE: Approval of Geological survey on mining claims K 1149484 et al. in Menary Township.
The deficiencies in this submission, as outlined in the Notice of Deficiency dated April 19, 1994 have been rectified.
The assessment work credits listed on the original submission have been approved as of June 23, 1994.
If you have any questions please call Dale Messenger at (705) 670-5858.
Yours sincerely,
rJ^C^^fV'Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
EM/vni
cc Assessment Files Office Idbury
Resident Geologist Kenora
FEB 4 '94 10:45 F ROM MIN. RE C/GE OL-KE NORhl TO MINING LflN FJ HGE .
V 2,
WORK KEPT, f
CLAIM NUMB.
t CLAIM UNITS
WORK DONE
VALUE VALUE APPLIED ASSIGNED
fi
1149484114948511494861149487114948811494891149492114949311494941149495 114949? 114950011495121149513
1149514114931511495161149517114951811495201149529114953011495211149522
111112844232
101
448
10161212e21
$1,179 $1,179 $1,179 $1,179 $1,179 $2,358 $9,432 $4,716 $4,716 $2,358 $3,537 $2,358
$11,790 $1,179
$4,716$4,716$9,432
$11,790$18,864$14,148$14,148$7,074$2,358$1,126
$1,179 $1,179 $1,179 $1,179 $1,179 $2,358 $9,432 $4,716 $4,716 $2,358 _ $3,537 , $2,358
$11,790. $1,179
$4,716$4,716$9,432
$11,790$18,864$14,148$14,148$7,074$2,358$1,126
$0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0
$0 $0 $0 $0 $0 $0 $0 $0 SO $0
RESERVE
$0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0 $0
$0$0 $0 $0 $0 $0 $0 $0to$0
24 116 136711f CLAIMS i CLAIM WORK
UNITS DONE
136711 0 0 VALU8 VALUE
APPLIED ASSIGNED RESERVE
Credits you are claiming In ftfe report may be cut back." In order to minimize tt» adverve effect* of *ocr) dotation*, ptMt* Indicate from which claims you wish. To pfiOfiz* m» daMon o» credits. Please mark (^) one of !ti« following:1. D Credit* are to b* cut Nick tUrting with the claim litted last, working backwards.2. OlSodite are to be cut back equally over an dalm* contained In this report of work.3 D Cradftc re to ba cut bar* •• prtortzed on the attached appendix.
In the *v«nt that you have notspecified, your choice of priority, option on* wit) EM implemented.
Motel: Stawptea of benaOdal Intacaat are unrecorded tnrnfgr*, option •greementa, memorandum of »vr»»mama, etc., with r»»pe«t to «M mtmng etatma,. .^ ;
• • .; '> o v-v'^' • t Noia f. « worn hM'li**!! performed en pata^lad or te**»d land. ptoaM complai* the following:
or MM) knd at th* finw the wo* wat Mribtmed.Signature 6at»'
** TOTPL PfiGE.002 **
TOW.NS H I P: oo -
vffr ffi'^- 1 ' '""}'&>t®:m
----r^" V'l.
^;rjWv//*• r x :'^ "TX^ /'
TONSHIPTOWHS'HIP
Ministry ofNaturalResources
Ministry ofNorthern Developmentand Mines
Ontario
INDEX TO LAND DISPOSITION
PLAN
G-3832TOWNSHIP
SENN
M.N.R. ADMINISTRATIVE DISTRICT
FORT FRANCESMINING DIVISION
KENORALAND TITLES/REGISTRY DIVISION
RAINY RIVER
Scale 1:20000
MMrm1000 1000 2000
Fwt1000 1000 2000 3000 4000 $000 7000 WOO 9000 10000
Contour Interval 10 Metre*
SYMBOLSBoundary
Township. Meridian, Baseline. ..........
Road allowance; surveyed ..............shoreline ..............
Lot/Concession; surveyed .............unsurveyed ...........
Parcel, surveyed ......................unsurveyed ....................
Right-of-way; road .....................railway ...................utility. ....................
Reservation ...........................
Cliff, Pit, Pile .............................
Contour .................................Interpolated ...........................Approximate ..........................Depression ............................
Control point (horizontal) ..................
Flooded land .............................
Mine head frame .........................
Pipeline (above ground)
Railway, single track .....................double track ......abandoned ..............
Road; highway, county, township ...........access ............................trail, bush ..........................
Shoreline (original). .......................
transmission Imp
Wooded area .............................
A
DISPOSITION OF CROWN LANDSPatent
Surface & Mining Rights ..............................Surface Rights Only...................................Mining Rights Only.....................................
LeaseSurface & Mining Rights ................................Surface Rights Only....................................Mining Rights Only ................
Licence of Occupation ....................................
Order-in-Council .........................................
Cancelled ...............................................
Reservation................................... ..........
Sand & Gravel............................................
.£
C
..Ba
..T
.OC
®
.<D
AREAS WITHDRAWN FROM DISPOSITIONMRO - Mining Rights OnlySRO - Surface Rights OnlyM + S - Mining and Surface Rights
Description
®
Order No.
•V-K-20-/97
(tote
SRO
Flto
I99I80
TH f INFORMATION THAT
OM SOURCES-AND ACCURACY IS NOT-auAWISHING TO STAK.: MIN- ^fi CLAIMS 5HOUI 0 CON- M, T WITH THE MININGS LOHOER. MiNismv OFNORTHERN D-VF; A OP MI NT AND MINE^V P°R A° "
fifATUS OP THF SHOWN HERf ON
DATE OF ISSUEMAY 2 01998
PROVINCIAL RECORDING OFFICE-8UOBURY
NOTES
ISLANDS IN .LtAV.vAl ' H I AKE REFLR i. ^ H. AN SM I28 IN ADDl'lON TQ THE LC^S ON "LAN SM li?8
KhSORl -,0V Pn t RFSORT RE' ' •
Map base and land disposition drafting by Surveys and Mapping Branch, Ministry of Natural Resources.
The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only
G-3818 MC LARTY TWP. G-3816Ministry ofNaturalResources
Ministry ofNorthern Developmentand Mines
SYMBOLS DISPOSITION OF CROWN LANDS
Ontario
INDEX TO LAND DISPOSITION
PLAN
G-3818TOWNSHIP
LARTY
M N Ft ADMINISTRATIVE DISTRICT
FORT FRANCESMINING DIVISION
KENORALAND TITLES/REGISTRY DIVISION
RAINY RIVER
Scale 1:20000
1000Metres
1000 0 Feel M M M H M f—
1000 2000
1000——I
2000 3000—r
4000 $000 6000 7000
Metre*
8000 8000 10000I .. Z- ""——-i '~ Feet
Contour Interval 10 Metres
BoundaryTownship. Meridian, Baseline
Road allowance, surveyed shoreline
Lot/Concession, surveyed., urisurveyed
Parcel, surveyed ...........unsurveyed .........
Right-of-way; road ........railway .utility .........
Reservation ..........
Cliff. Pit, Pile ............
Contour ........... .Interpolated .............Approximate ............Depression........ ......
Control point (horizontal) .......
Flooded land . .........
Mine head frame ...........
Pipeline (above ground) ........
Railway; single track. .double track.......abandoned.........
Huacl, highway, ^.uuiiiy. lownsnip access .................trail, bush................
Patent
Surface & M ining Rights
Surface Rights Only .
Mining Rights Only.
LeaseSurface & Mining Rights Surface Rights Only . Mining Rights Only........
Licence of Occupation . ...
Order-in-Council. .........
Cancelled
Reservation ........ ........
Sand & Gravel .......TOURIST CAMP (OP-OUTPOST)..
9 v
Ba T
oc ®© a
AREAS WITHDRAWN FROM DISPOSITIONMRO - Mining Rights OnlySRO- S urface Righis OnlyM i S - Mining and Surlace Rights
Description Order No. Date Disposition
fur INFORMATION I HAT Af'PF "Arts ON THIS MAP >'A', P.FLN COMPn I ii
Map base a.id land disposition drafting by Surveys and Mapping Branch. Ministry of Natural Resources
The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only
Shoreline (original)
Transmission line
Wooded area
AND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKf MIN ING CLAIMS SHOULD CON SUIT WIIH THF: MINING FtEcoHDtn MiNi'.rnv orNOH I HfcHN IK VI LOP MTNT AND MINI :. FOR AD DlTlONAI INI I'HMATlON ON rilf STAID.', OF THF LANDS SHOWN HFRFON
'[HIS MYLAR PUT INTO SERVICE FFFECTIVE MARCH 28. 1995
TOWNSHIP
TOWNSHIP
S2F04SWOn02 •> 1 S?92 MCLARTY
b-3799 O_AXTQN TWP G-3799Ministry ofNaturalResources
Ministry ofNorthern Developmentand Mines
SYMBOLS DISPOSITION OF CROWN LANDS
Ontario
INDEX TO LAND DISPOSITION
PLAN
G-3799TOWNSHIP
CLAXTON
M.N.R. ADMINISTRATIVE DISTRICT
KENORA / FORT FRANCESMINING DIVISION
KENORALAND TITLES/REGISTRY DIVISION
KENORA /RAINY RIVER
Scale 1:20 000
1000 1000 2000 __1 M»tr»$
Fe«l1000 1000 2000 3000_ 4000 5000 8000 7000
Contour Interval 10 Metres
8000 9000 10000. — i Fml
Map base and land disposition drafting by Surveys and Mapping Branch, Ministry of Natural Resources.
The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only.
BoundaryTownship, Meridian, Baseline
Road allowance; surveyed . shoreline
Lot/Concession, surveyed., unsurveyed
Parcel; surveyed ....unsurveyed .........
Right-of-way, roadrailway utility ......
Reservation
Cliff, Pit. Pile ..................
Contour ......Interpolated .........Approximate ...............Depression ................
Control point (horizontal) .....
Flooded land..................
Mine head frame .........
Pipeline (above ground) ........
Railway, single track.double track.........abandoned...........
Road; highway, county, township access . trail, bush...............
Shoreline (original).......
Transmission line ...........
Wooded area
I'atfintSurface & M ining Rights Surface Rights Only Mining Rights Only
LeaseSurface & Mining Flights Surface Rights Only Mining Rights Only.
Licence of Occupation
Order-m-Council .........
Cancelled ...........
Reservation .......
Sand & Gravel...
no
. T
OC
©
AREAS WITHDRAWN FROM DISPOSITIONMRO M ining flights Only
SRO - Surface Rights OnlyM t S - Mining and Surface Rights
Description Order No Date Disposition Fil
PARK RESEBVE 'A'
PARK R tSERVE C'
PAHK RESERVE '0'
MN.R. RESERVE ( M . I (, PLAN P 7465-11
SKC-42/60 3 / U / 6 9 SRO 16347?
THE INFORMATION THAT APPEARS ON IHIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCE, AND ACCURACY IS NOT GUARANTEED. THOSf WISHING TO STAKE M!N-,,,.- .-, V M< - SHOULD CON. _SULT WfTH THFTfllNTNG RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES. FOR AD niTIONAL INFORMATION ON THE STATUS OF THE I ANDS SHOWN HFRFON
THIS MYLAR PUT INTO SERVICE EFFECTIVE MARCH 28. 1995
DATE OF ISSUE20
OFFICE-SUDBURV
''''" x ••<•" ' I
GODSON A TOWNSHIP 1'"\ ' / v , .. " •" i / T\.
'<
,'•$ 'Jobaskong
E\ 4 •»"£ / / ' •*•%*/ L /' BO 1 \
PROVilNClAL,
"\ / </ i x
TOWNSHIP
TOWNSHIP
^-~ "—' 1 >r^ "—' \
II05273
208B78
6 -2 8 0
6I279"
3 2 8 ,
49689
TOWNSHIP
Ministry ofNaturalResources
linistry ofNorthern Development and Mines
Ontario
INDEX TO LAND DISPOSITION
PLAN
G-3826 ______TOWNSHIP SERVICE DATE
POTTS
M.N.R. ADMINISTRATIVE DISTRICT
FORT FRANCESMINING DIVISION
KENORALAND TITLES/REGISTRY DIVISION
RAINY RIVER
Scale 1 20 000
1000 1000 ?nooMetres
1000 0F««t M M H M M 1—
1000 2000 3000—I
40001——
sooo 6000f——
7000 8000i
9000 1 0 000 Feet
Contour Interval 10 Metres
SYMBOLS
AREAS WITHDRAWN FROM DISPOSITIONMRO- Mmi'iii Rights OnlySRO - Surtace Rights. OnlyM + S - Mining and Surface Rights
Description Order No Date Disposition File
M.N.R. RESERVE 06iS8
\ SECTION 35 W-K-24/97 24/10/97 M+S 195150Boundary
Township, Meridian. Baseline
Road allowance, surveyed shoreline
lot/Concession; surveyed, unsurvoyod
Parcel; surveyedunsurveyed .........
Right-of way; road
railway utility
Reservation ...........
Cliff. Pit. Pile
Contour ......................Interpolated ................Approximate Depression
Control point (horizontal)
Flooded land
Mine head frame ......... .
Pipeline (above ground)
Railway, single track double track
abandoned
Hoad; highway, county township
access trail, bush
Shoreline (original)
Transmission line
Wooded area
as W-K-Pb &t Pft/IO/97 M*9 195150
O-K-9/98 03/30/96 M8S 195130
DATE OF ISSUEMAT 2 01996
DISPOSITION OF CROWN LANDSPatent
.Surfare & Mining Rights
Surface Rights Only
Mining Rights Only
LeaseSurlace & Mining Rights
Surface Rights Only Mining Rights Only
I icenc:e of Occupation
Ordei-m-Council
Canrnllerl
Reservation
Sane) & Gravel ...........
aW
HyT
oc ®© ©
\J X
I01 00no CD
oHH CO
THE INFORMATION THAT APPEARS ON THIS MAPHAS BEEN COMI'll t() FROM VARIOUS SOURCES AND ACCURACY is NOT GUARANI t f I; THOSE WISHING TO STAKi MIN ING CLAIMS SHOULD CON SULT WJTH THh MINING RECORDER. MINISTRY OF NORTHFBN DEVELOP MENT AND MINES TOR AD DITIONAI. INFOFIMATION ON THf STATUS OK IHh LANDS SHOWN HERFON
Map base and land disposition drafting by Surveys and Mapping Branch, Ministry u( Natural Resources
"I he disposition of lanu1 , location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only
CD I
CM 00no
52F04SWD002 2 15292 MCLARTY 230
S H IT
-:/-, • -w*^X*'--r*™1»T'~ .™- . .i>i)h- \
. ..1149487 1149492 ,, ih 1 .«.;*- .•-..
_. ir""; -,,\m W -u,- V. , • .1 ," V^a fa-l:
, " I 1164232'-""
.'I 1079874 f ,1120359 -| 1120284'
Zttef?
'H05447•;--'• J
. — —— _—1_
IGJ072I'052 4
- AX .no\ fiend I e \^~~~~~~~~
114929'
1105432
M CJ-LLD
Ontario
Ministry ofNorthern Developmentand Mines
INDEX TO LAND DISPOSITION
PLAN
G-3819TOWNSHIP
MENARY
M.N.R. ADMINISTRATIVE DISTRICT
FORT FRANCESMINING DIVISION
KENORALAND TITLES/REGISTRY DIVISION
RAINY RIVER
Scale 1:20000
v»«tre«1000 1000 2000
_____ r-] Matre*
F*«l1000 1000 2000 3000 4000 SOOO 6000 7000 8000 9000 10000
Fml
Contour Interval 10 Metre*
AREAS WITHDRAWN FROM DISPOSITIONMRO- Mining Rights Only
SRO - Surface Rights Only
M + S - Mining and Surface Rights
SYMBOLS Description Order No. Date Disposition File
Boundary
Township, Meridian, Baseline..
Road allowance; surveyed
shoreline
Lot/Concession; surveyed... unsurveyed
Parcel, surveyed .... unsur/eyed .........
Right-of-way; •>.-!•.
railway ... .Jtility. ..........
Reservation. ....
Cliff, Pit. Pile ..............
Contour ...... .....Interpolated ..............
Approximate ...........Depression. .................
Control point (horizontal) .....
Flooded land..................
Mine head frame ........
Pipeline (abo\£ ground) ........*3
Railway, single t^ack............double track..........abandoned......
Road, highway, county, township access .................trail, bush.......
Shoreline (original) .............
Transmission line.....
Wooded area .................
DISPOSITION OF CROWN LANDSPatent
Surface & Mining Rights Surface Rights Only.
Mining Rights Only
LeaseSurface & Mining Rights
Surface Righis Only
Mining Rights Only
Licence of Occupation ..
Order-m-Councii
..B
..a
..T
.00
Cancelled
Reservation.
Sand & Gravel.
EFFECTIVE DATE
IHf INF: ORMATK)N 1HAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES. AND ACCUMACY IS NOT <~,UARANIEED THO5if Wir.MINC. TO STAKE MIN- INC, CLAIMS SHOULD CONsun WITH THE MININGIUCORDER. MINISTHY OF NORTHERN OfVELOP MFNT AND MINTS. FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON
^ cO / /
'\~ai&4K.r UA •J-- ,<X") la"-/^"Cy 7, MIM, i^ai&NrO^ ^ »̂ s ^X l '\ -'/^ \ xO-l
^ <>*'$)^ JH 'Vl//
: \
Mc.Ka.ry
L IT HO:. ; : I.:AL r. F.CE
M a r i. ,:: I n t n Q i. v e Rocks
itr Dyke;
i n t r v. o i •/ o • ^ 1 1 1 a c c
C, r ,1 n i t i o 1 1 :. r • is i v i- ? o c k s
5 d T r o n d 1 j e m i t e , J r a n i u Dykes
StriKo and Uj.p uf Beddinq
Sti'ikc and Dip of t'yliuLion
Strike and Dip of Shearing in i- I'D _^ i. ve to n L a c t
t'olsic to intermediate Nctavo. can ic. Rocks
2b f-orph'. ritic Khyoliticand D t c i t i c Lavas
2 c o u a r t ; - ].•' e 1 d s p a r P o r p h y r y[ ) y k e f o c k 3
Bedrock Outcrop Small, Large Cla impos t
M a f-" i o to i r L e r m e d i a t fe t a v o 1.: j a i .; Roc k s
ii bdi vide (a I-' i. n e u, i-i •-• i i n m (J t a i n e d
Ma s :-; i v.j B a o u 1 t.T r ^ e i : r a i ri t: d G a b b r o i i:
T c x t u t e d D a s a 1 r I b ' 1 1 o r n f i? 1 >:, e d G a 1:> 1^ r o i c
'f'e :< t u to u n a d a 1 t I c r o r p h y r i. t i c Mafic Lavas Id I'll lowed Ma fir: T.avas 1 d ' r1 1 1 1 o w e 1 a n d V a L j. o 1 i 1 1 c
i-! a f i c L ^ v a s e P i 1 I o w o .) and i 1 o t p h y r i t i c
. -i a f i c L i v a ;;1 r u f 1 - h L- •.• c c i a , L a p 1 1 1 1 Tuff
i n d T u f i: .•'•. in p h i b o i 1 1 e
j. .: p h e r u 1 1 c i c Mafic Lavas
L=.-f
,200WESTERN TROY CAPITAL RESOURCES
MENARY TOWNSHIP PROPERTIES
.15292 MULAKTY 250
MAP No. 2-
I 9 9 2 Survey: C . A . H a rj g , D . S c . G e o 1 o g
I:THOLCGICAL LEGEND
SYMBOLS
—f— Strike and Dip of Bedding
•«—I—T- S trike and Dip of Foliation
.^/•H-- Strike and Dip of Shear inc
——— , — — — Geological Contact observe-d, interpreted
in • - Lithostratigraphic 2one Boundary
1149400 (2) Claim Number, Number of Claim Units
X <C\__y Bedrock Outcrop Small, Large Q C lairapost
A u. G 31 d Showing
e
Mafic Intrusive Rocks
8 Diabase Dykes
intrusive contact
Granitic Intrusive Rocks
5a T r ondh j emi t e , Granitic Dykes
intrusive contact
Felsic to Intermediate Metavolcanic , R o c k s
2b Porphyritic Rhyoliticand Dacitic Lavas
2c Quar t 2 -Fe 1 dspar PorphyryDyke Rocks
Mafic to Intermediate yietavolcanic Rocks
1 Hncubd : . v idedla Fine to Mediun Grained
Massive Basalt 1b Coarse Grained Gabbroic
Textured Basalt 1 b ' Hor n f e 1 s ed Gabbroic
Textured Basalt Ic Porphyritic Mafic Lavas 1d Pillowed Mafic Lavas Id'Pillowed and Variolitic
Mafic Lavas 1e Pillowed and Porphyritic
Mafic Lavas If Tuff-breccia, Lapilli Tuff
and Tuff Ig Amphibolite li Spherulitic Mafic Lavas
WESTERN TROY CAPITAL RESOURCES
MENARY TOWNSHIP PROPERTIES
MAP No.
1992 5 • : r v ft y : C.A. Wagg, 3 . S c . Geolygis
I/
o
r,?F04SWOOO^ ^ 1W92 MCLAR TY 260
SYMBOLS
r e t e c
5tri'<e'?Tv' Dip of Bedding
Stride r.id Dip of ?oliatior.
Strips and Dip of Shearing
j — — — G eological C or. t act observed, i n t e r p
Lithostra*. igraphic Zone Boundary
1 ' 4 9 4 C 0 ( 2 ) C 1 a i a Number, Number of Claia Units
Bedrock Outcrop Saali, Large Claiaposi.
Gold Showing
IT.HCLCGICAL LEG
Kafic Intrusive Rock
8 Diabase n y * e s
intrusive conta
Granitic Intrusive ?. oc'ns
intr'js : ve contact
i • to Intermediate K e *. a volcani
2b F c ; p h y :• tic P. hyoiitic and '. ;- •; i - La va i
2<- £u* - • j..; = .-:_ r ; =r Dhyry
Mafic to In", ir^ediata M e t a v o ' c a : ; ~ ?. o c !< s
1 U n r. u b d i v i r j dla Fii-a to >; •. i i u 3 Grained
.v. j j ; i •/ e Basaltrsa Grained Gabbrcic
Textured Basalt Ib'Hornfalsed Gabbroic
T tur=d Basalt Ic P z p h y r : t J c Xafic Lavas Id Pillowed Mafic Lavas Id Pillowed and Variolitic
Mafic Lavas )e Pillowed and Porphyritic
.V i f i c Lavas If ?u f f - E r •.? c = i a , Lapilli Tuff,
and ? u T
S£A/A/ Twp
i S c h e r •• 1 t ic Mafic Lavas
WESTERN TROY CAPITAL RESOURCES
MENARY TOWNSHIP PROPERTIES
MAP No. |
1992 Survey: C . A . Wage, 3 . s c . Geologist<-^ 3" — "- " *
IL
S£A/A/
_TwRjvj£A/ARY TwP , [a-^4-t.<i Ja.:
o
52F0^5VVCOC2 2 15292 MCb!,R"Y 270