Killbear quarry by kamrang

41H08NW0002 ? 16427 CARLING

010

GEOLOGICAL SITE PLANS OF POTENTIAL DIMENSION STONE QUARRIES ON THE KILLBEAR POINT PROPERTY THE PARRY SOUND DISTRICT OF ONTARIO

by f -

JAMES R. TRUSLER

R E C E l V E LV

MINING LANDS BRANCH

LONG.: 80 0 13'44"W - 80 0 15'30"W LAT.: 45 3 21'33"N-45 0 23'31"N NTS: 41H/8

x 7"- ---'' V DATE:"Ja'ffijary 29,1996

GEOLOGICAL SITE PLANS OF POTENTIAL DIMENSION STONE QUARRIES ON THE KILLBEAR POINT PROPERTY THE PARRY SOUND DISTRICT OF ONTARIO SUMMARY The Parry Sound area of Ontario is underlain by complex gneisses and migmatites of Middle to Late Proterozoic age which are part of the Ontario segment of the Central Gneiss Belt of the Grenville Structural Province. A working model of thrust plates (called domains and sub-domains) which are separated by ductile thrust faults and moved in a northwesterly direction upon each other has been postulated by Davidson et al (1982). Easton (1992) has improved this model in his synopsis using a hierarchy of terranes and domains wherein the terranes indude domains of similar age which are autochthonous with respect to each other. Age dating has indicated that four of these large scale terranes or plates are stacked on each other with the base being near Sudbury at the Grenville Front and the top being near Kingston.

Despite the recent wealth of scholarly publications a comprehensive geological map has not yet been made available for the area. However, the limited information available has enabled the dear identification of potentially favourable conditions for both flagstone and dimension stone. Several flagstone occurrences cluster along Davidson's thrusts and several potential dimension stone prospects have been identified within the interior of particular domains. Although one may ordinarily not expect to find dimension stone within tectonite terranes, it is evident that the autochthonous nature of some of the domains combined with annealing effect of later superimposed amphibolite facies metamorphism preserved large competent blocks of migmatites and gneisses. As a result of mapping dimension stone potential, nine sites exposing migmatitic orthogneisses in the Britt domain were sampled producing encouraging results on sawing and polishing. Subsequently six of the properties examined and three properties identified in government research have been staked. One of these properties is the ten claim unit, 500 acre, Killbear Point property. The property is underlain by massive to gneissic pink granite gneiss, migmatite and a purple and pink migmatite all of which are flat lying or gently dipping to the southeast. A study of the joint spacings indicates average spadngs of 2 metres for horizontal joints and over 5 metres for vertical joints. Four prospective products , two of which are unique, attractive, red, textured granites have been identified in five potential quarry locations. A high yield rate of 30 tonne blocks is inferred.

Face i

During 1995, three sites were mapped at an approximate 1:500 scale using a pen notebook computer and Field Notes software. Site plans showing 1 metre contours, the existing ground conditions and joints were produced. The three sites designated Killbear 1, 2 and 3 respectively contain purple and pink migmatite, pegmatite breccia, and purple and pink breccia intermixed with pegmatite breccia. Each site is very prospective for dimension stone and 30 tonne blocks are apparently quarriable with low waste factors. Killbear 1 was sampled, and a preliminary set of ASTM tests conducted by Inchcape Testing Services NV Ltd. achieved satisfactory results. Drilling of Killbear 1 and 2 are planned. It is strongly recommended that test quarrying be conducted on Killbear 1 and Killbear 2 . Permitting through the Ministry of Northern Development and Mines and public information meetings will be required steps before quarrying. Further site planning, calculation of waste factors and costs for each quarry test and permit applications are to precede an effort to finance this next stage.

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TABLE OF CONTENTS

SUMMARY . ... .. .. . . . . ... . . . . . . . . . . .. . . . .. . . . . . .. .. .... .... . . .. Page i ?

z i

INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 1

LOCATION AND ACCESS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 1

PROPERTY . . . . . . . . . . . . . . . . . . . .................. . . . . . . . . . . . . . .

Page 3

DATES WORKED METHODS USED ON CURRENT PROJECT . . . . . . . . . . . Page 4 PREVIOUS GEOLOGICAL WORK . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 5 2 o

REGIONAL GEOLOGY . . . . . . . . . ... . . . . . . . . . . . .

. . . . . . .. . . . . .. . . ..

Page 5

DESCRIPTION OF ROCK UNITS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 9

PROPERTY GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 13

POTENTIAL DIMENSION STONE SITES . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 14

CONCLUSIONS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 21

RECOMMENDATIONS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 21

REFERENCES . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . ...........

Page 22

AUTHOR'S CERTIFICATE . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page 27

LIST OF FIGURES Figure 1: Figure 2: Figure 3: Figure 4: Figure 5: Figure 6: Figure 7:

Location Map . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Property Map ..... . . . . . . . . . . . . . . . . . . . .. . ...... Lithotectonic terranes, domains Central Gneiss Belt . .. Geology of the Britt Domain (Easton (1992)) ... .. .. .. Site Plan Killbear 1, Vertical Joints 1:518 ... . . . .. . . . . Site Plan Killbear 2, Vertical Joints 1:507 . . . . . . . . . . . . Site Plan Killbear 3, Vertical Joints 1:500 . . . .. . . . ... .

. . . . . .. . .. . .. . . . . . . . .... .... . . . . .. .... . . . . . . . . . . . . . . . . . .

. . . . .. . . . . .

Page 2 Page 3 Page 6 Page 8 Page 15 Page 18 Page 20

LIST OF TABLES TABLE 1: KILLBEAR POINT PROPERTY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 3 TABLE 2: TABLE OF ROCK UNITS FOR THE PARRY SOUND AREA . . . . . Page 11

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LIST OF PHOTOS Photo 1:Killbear#1 Site looking north . . . . ... . . .. .... . . . .... ... .. . . Photo 2:Killbear #1 Site: Example of purple and pink migmatite breccia .. . Photo 3:Site Plan Killbear # 2 looking northeast ... ... . .. . ... . .... . .. Photo 4: Killbear 2 Site Plan area looking southeast at clff face ... . .. . . . . Photo S.Killbear 3 Site Plan area looking east northeast at cliff face . . . . . .

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Page Page Page Page Page

16 16 17 19 19

INTRODUCTION

In 1991, the writer commenced a project to evaluate the flagstone and dimension stone resources of the Parry Sound area. At the same time efforts by government geologists, principally Chris Marmont and Dave Villard, were being made to outline the substantial potential for these stone resources and make the public aware of the opportunity. In 1992, the regional investigation of flagstone resources by the writer proved discouraging. It was decided late in the field season to focus solely on the dimension stone potential. By the end of 1992, many prospective dimension stone sites had been identified by either government publications or by the writer's prospecting. Nine of these dimension stone properties have now been staked by the writer, and an initial evaluation of each property involving geological mapping of the outcrops at a scale of 1:5,000 has been conducted. The work provides an initial evaluation of potential quarry sites on each property. The project has been supported by the Ontario Prospector's Assistance Program in 1992, 1993 and 1995. In October 1991, the first portion of the Killbear Point property was acquired for its dimension stone potential. Additions to the property were made in 1992. Geological mapping was carried out initially in 1992 and a Preliminary map was prepared and submitted with the final report for the OPAP grant in 1992. This work was supplemented in 1993 with additional mapping on the property resulting in a more detailed interpretation of the northeast comer of the claim group and a revision of the Legend and a geological report on the property was completed (Trusler, 1993b). This study is a detailed geological evaluation of three sites using a field pen notebook computer to map the joints and ground conditions. The data obtained will enable planning for the removal of dimension stone blocks from each site. The format of the report is in compliance with requirements for submission of a geological report for assessment purposes. LOCATION AND ACCESS

The property is located in Carting Township, Parry Sound District, Southern Ontario Mining District, and Algonquin District Regional Geologist's area approximately 150 miles (240 km) north of Toronto (Figure 1). The property is bounded by longitudes 80"-15'30"W on the west and 80 0 -13'-44"W on the east and latitudes 45 0 -21 '-33"N on the south and 45 0 -23'-31" on the north. The corresponding UTM co-ordinates in metres are 558,100 on the west, 560,370 on the east, 5,022,840 on the south and 5,027,320 on the north. The property is within National Topographic System area 41H/8 and is recorded on claim map M2297. The property can be accessed from Hwy 559, the Pengallie Bay Rd. and the Snug Harbour Rd by first leaving Hwy 69 some 10 km north of Parry Sound and travelling 19 km west on Hwy 559. Due to an old road and relatively flat outcrop the bulk of the property is currently accessible to 4-wheel drive vehicles. Page I

"*Figure 1: LOCATION MAP

PROPERTY The Killbear Point property comprises approximately 500 acres and is more particularly described in TABLE 1 (Figure 2). Assessment was applied to the daims in 1993, and this report will be filed for assessment. As a result sufficient credits should be available to keep the entire claim group in good standing for some three years from date of filing.

Claim No

Township

Lot

1151129

Carling

1151135 1151136

Carling Carling

66 XI 66 X 64 X 64,65 IX

Cone.

Area Recording Date 200 ac 100 ac 200 ac

KILLBEAR 3 SITE PLAN KILLBEAR 1 SITE PLAN

KILLBEAR 2 'ISITE PLAN^O

Scale: 1:20.000

Figure 2: Property Map

Page 3

Oct.23, 1991 Nov. 5, 1992 Nov. 5, 1992

DATES WORKED METHODS USED ON CURRENT PROJECT

Preparation work on the project commenced in September, 1995, the field work commenced on Oct. 19,1995 and the map drafting and report writing was completed on Jan.29, 1996. Actual work days for assessment purposes break down as follows: Killbear Point Property: Claims SO1151129,1151135,1151136 Preparation: Sept. 29, Oct. 4, 25, 28, 29, Nov.3,4.5,8,12 4 15, 1995 (11 days) - Field: Oct. 19, 20, Nov. 20,21 ,A 23.1995 (5 days) /Drafting: Dec. 19 1995 (1 day) Reporting. Dec.14, 18,26,27,28,1995; Jan. 28, 29, 1996 (7 days) Sample Preparation and Testing: Dec. 5, 12, 15, 1995 S Jan. 8, 1996 ( 1V& days )

The magnetic declination used in the field work is 10"-5'W. After selecting several candidate sites for 1:500 mapping, the air photo enlargements were scanned at high resolution (600 dpi) and digitized as a tif file for use with digitized Ontario Base maps in a pen notebook computer. Field Notes , the Windows based software was used directly in the field to coordinated the image files created from digitized air photos, the vector file layers of OBM data, the database and drawing input layers. The field data was directly output on a Canon BJC-600 Bubble Jet Printer. The digital data has been saved as dxf and dwg files for use in AutoCAD . Two difficulties were experienced with the system. Initially the image scanned was over a large area so that the resolution of the image file was poor below a 1.2000 scale. This was remedied by scanning select portions of the air photo enlargements at 600 dpi. The second difficulty was that the computer functioned poorly in freezing weather. That was remedied by converting the tif files to gif files using Graphic Workshop and massaging these files in L View Pro to produce a high resolution image at 1:500 scale. This image was printed out on the Bubble Jet Printer and used for direct field mapping in the cold weather. The data was then transcribed onto the computer in the evenings. These difficulties and a few more comprised about half of the project preparation time. Three sites were mapped at an approximate scale of 1:500 enabling the construction of site plans. Samples comprising 150 kilograms were collected from the area of the Killbear #1 site plan and transported to Smith Monument Co. for sawing. Most of the samples were cut to specifications under the direct supervision of the writer and then transported to Inchcape Testing Services. The writer attended on the sample testing for half a day.

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PREVIOUS GEOLOGICAL WORK

A traverse of the shore of Georgian Bay was made by Alexander Murray in 1848, and he gives a brief account of the geology of the shoreline (Murray 1848. p.45,46). The shoreline of Georgian Bay was again examined by Robert Bell in 1876 (Bell 1876, p. 198-207). The Huntsville -Bracebridge area was investigated by W.A. Parks (1900, p. 121126), and brief notes on the geology are given. Further field work was done in the area in 1905 by T.L. Walker (1905, p. 84-86). The International Geological Congress had a field excursion in Parry Sound area in 1913. Some local geological features are described by T.L. Walker (1913, p. 98-100). Trusler and Villard (1980) conducted detailed geological mapping in the Parry Sound-Sans Souci area.Trusler (1992, 1993a, 8t 1 993b) conducted regional prospecting and mapped the property geologically on a 1:5,000 scale. The first comprehensive reconnaissance mapping in the area was done by Satterly (1942) who visited all the local known mineral deposits. Satterly (1955) also mapped Lount Twp. in detail showing for the first time the existence of mappable units in the Parry Sound area. Hewitt (1967) was able to accurately identify the complexity of petrographic units and correlate some of these in a reconnaissance mapping program. Greater interest in resolving the geological complexity of the area was kindled by Lumbers who was progressively mapping Grenville terrains in Ontario from the Grenville Front to the south Lumbers (1975) and by Wynne-Edwards (1972). Wynne-Edwards suggested the first interpretive framework for the Central Gneiss Belt of the Grenville Structural Province. The controversy which arose from Wynne-Edwards "Sea of Gneisses" lead a profusion of other researchers into the area who have conducted specific detailed and reconnaissance mapping and synoptic studies. Since 1972 M. W. Schwerdtner and students have concentrated on resolving many of the structural geology problems of the area contributing a great amount to the understanding of the geology of the Central Gneiss Belt. The framework for all current work in the area was provided by Davidson et al. (1982). This has been modified subsequently by Davidson and other workers, and Easton (1992) has provided a coherent review, but the tectonic terrains and domains separated by shear zones have become imbedded in the literature. REGIONAL GEOLOGY

The Muskoka-Parry Sound region is part of the Ontario segment of the Central Gneiss Belt in the Grenville Structural Province (Wynne-Edwards 1972). No detailed geological map of the whole region, which was included in a recent major project on the Ontario Gneiss Segment by the Geological Survey of Canada, has been published to date. Recent mapping by Davidson et al. (1982) has led to a tectonic model in which the thickening of Proterozoic crust is accomplished by deep-level thrusting and Page 5

associated reverse ductile shearing (Davidson 1984a, 1984b). According to this model, major crustal slices (called domains and sub-domains, (see Fig.3)) have been translated over large distances toward the margin of the Superior Structural Province. Age of crust or major period of moQmoffsrn 1170 to IKDO Ma

ISOO to MOO Ma

1300 to 1250 Ma

27OO to 23OO Ma

I45O to OSO Ma

Paleozoic cower rocks Terrane boundary Domom boundary

Paw, Sound

Terrane

;MoznM

Abbreviations A Ahmic Domain B Britt Domain Be Beoverstone Domain CMB6Z Central Meiased i memory Belt Boundary Zone F Fishog Domain GFTZ Grenville Front Tectonic Zone

GH H K Me Md. MR N

terrane

Go Home Domain Huntsville Domain Kiosk Domain McQaney Domain Mcclintock Domain Moon River Domain Novor Domain

NE O P PS R S TL

Nepewassi Domain Opeongo Domain Powassan Domain Parry Sound Domain Rosseau Domain Seguin Domain Tilden Lake Domain

Figure 3: Lithotectonic terranes.domains Central Gneiss Belt (Easton, 1992)

This view has been further modified by some more local studies by Hanmer (1988) and Schwerdtner (1987). According to Hanmer the southeast to northwest thrusting was initiated at approximately 1160 Ma and continued for 100 Ma. However he claims that subordinate northeastward thrusting was coeval and that late synmetamorphic extensional shears cut these major thrusts and thrust sheets but are in turn cut by late movement on the thrusts. He further alludes to the comparison to the structural style of the Central Gneiss Belt and the Himalayas suggesting that the Grenville exposes the architecture and processes presently active in the roots of younger mountain belts. Schwerdtner^ Page 6

observations agree with Manner's respecting a northeasterly component to deformation which he invokes to explain north-south buckle folds. However, Schwerdtner observed that not all foliations can be explained by the thrust model and that three sets of folding are superimposed and cross the domain boundaries. He claims that all the structural facts can be explained without large differential translations of crustal slices and most discordances in the regional gneissocity could have been created by decollement and repeated buckling. Easton (1992) synthesized all previous studies stating that, "Recorded within the Grenville Province is the tectonic evolution of the southeast margin of Laurentia during the Mesoproterozoic. The Grenville Orogeny has overprinted the structural trends and metamorphic effects of the Archean and Paleoproterozoic geological province of Laurentia. It is now generally accepted that this orogenic event or events involved northwest directed thrusting and imbrication of the entire crust, presumably as a result of a terminal collision at about 1100 Ma. with a continental landmass somewhere to the southeast. The Central Gneiss Belt consists mainly of upper amphibolite and local granulite facies, quartzo-feldspathic gneisses, chiefly of igneous origin with subordinate paragneiss. Distinctive lithotectonic terranes, some further subdivided into domains, have been identified within the Central Gneiss Belt. The terranes and domains are distinguished by differences in rock types, internal structure, metamorphic grade, geological history, and geophysical signature and are bounded by zones of intensely deformed rocks traceable for tens of kilometres." The Algonquin terrane consists of 1800 to 1600 Ma gneisses intruded by 1500 to 1400 Ma granitic and monzonitic plutons that may represent an extension of the Eastern Granite-Rhyolite Province. Although imbricated by later thrusting the Algonquin terrane is probably parautochthonous. The Britt and Rosseau domains are part of the Algonquin terrane. The Britt Domain (Figure 4) comprises a complexly deformed and metamorphosed series of rocks. Although some of the rocks are metasedimentary in origin the preponderance of the rocks were originally plutonic, but have been changed by dynamic and thermal metamorphism. The final stages of this metamorphism appear to have annealed the rock into a compact and durable material having some relict textures and many overlapping and lively features. Dips of these rocks are generally flat to 10 0to the southeast. Some units are entirely composed of isoclinal sheath folds whereas other units are evidently deformed megacrystic granitic plutons.

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A R

Gcocftronolopc

lompw tocanon

1MWM rott RB-Sr tmtliod

U-Pb iran mefhad

Legend Straight gneisses and related tectonics

Monocychc, circa ) 45O million -r*or-old gronitoKts

UnsutodivKted gneisses

Sand Boy gneiss association- quortzofektapothic stfrocrusto) gneiss, scfttst, ompnoohie, quartzite and martrie Ojibwoy gneiss assoaatiort and

g/onodKnte - tonalite,

Key Hortxx* gneiss ossoaaiKMt Kucocrotic granite - gronodonie gneiss mm suprocnjstoi gnens and jotiigcr and older ontwgnpss Nepheline

syenite

AnarthOMfe and gubbro

Run

Gnauoxty. w-tti dp

Figure 4: Geology of the Britt Domain (Easton (1992)) The Parry Sound and Moon River domains consist chiefly of juvenile crust 1450 to 1350 Ma in age and are parallochthonous. The Parry Sound domain rocks comprise dense high metamorphic facies rocks (amphibolite and granulite facies) which are emergent on the other domains. The rocks in the Parry Sound domain are dominantly amphibolite and pyroxenite gneisses which strike to the north east and dip 20 0 -60 0to the southeast (at a much steeper angle than the postulated shear couple accompanying thrusting). The bedrock largely comprises veined, banded and homogeneous pink and grey Page B

migmatitic gneisses produced by injection and granitization of metamorphic gneisses of various types. The rocks are mainly of upper amphibolite and granulite metamorphic facies. Hypersthene-bearing chamokitic gneisses are present in the area. The origin of much of the amphibolite gneiss is obscure. Some which is associated with bands of marble is thought to be paragneiss whereas some is proximal to large bodies of gabbro and anorthosite and thought to be orthogneiss. Trusler and Villard (1980) found evidence that some of the mafic and felsic rocks are of volcanic origin. The high metamorphic grade of the rocks is attributed to a deep seated origin possibly involving underplating at an early stage. The Bolger pluton in the Britt domain is dated at circa 1450 Ma and underlies the Black Lake, Woods Road and Shebeshekong Lake properties (Figure 4). The Dillon Road property is underlain by both the Bolger pluton and the Ojibway gneiss association. The Killbear Point and Jacknife Harbour properties are underlain by the Sand Bay gneiss association. The Grundy Lake property is underlain by an unnamed V-shaped pluton believed to be circa 1450 Ma. Comparable regional maps do not cover areas about the Turtle Lake property and the Burnt Lake property which are situated in the Rosseau and the Moon River domains respectively. DESCRIPTION OF ROCK UNITS

Since no detailed geological maps have been produced for the Parry Sound area, none of the previous workers have made an attempt to construct a table of rock units. Since each domain postulated by Davidson has been transposed over a large distance none of the rock units are correlative across domain boundaries. Trusler and Villard made an attempt to derive a Table of Rock units for the Parry Sound -Sans Souci area in 1980 and some of that information is used here to produce Table 2. These Formation names are not used in the mapping. However, the property is principally underlain by rocks that correlate with the Killbear Point Formation and to a lesser extent with rocks of the Bateau Island Formation. Culshaw et al. (1991) correlate these rocks with the Sand Bay Gneiss Association. The rocks on the property have been subdivided into mappable units as follows: granite gneiss, purple and pink migmatite, migmatite and coronitic metagabbro. The granite gneiss is a pink, layered to massive rock, varying from fine grained to coarse grained from one area to another and comprising quartz, plagioclase and microcline with minor biotite and variable accessory magnetite, hematite and almandine. A significant portion of this rock unit is demonstrably composed of breccias cataclastically derived from granite pegmatites. The purple and pink migmatite is a composite layered rock generally containing medium to coarse grained layers of the granite gneiss and a regular fine to Page 9

medium grained purple or mauve layer comprising quartz, feldspar, biotite, almandine and hematite. Frequently a milky to buff rock of medium to coarse grained granulated late tectonic pegmatite forms layers within the purple and pink migmatite. Pinch and swell of the late tectonic pegmatite and brecciation or crenulation of the purple constituent are common variations of this rock unit. The migmatite is a generally coarse grained composite layered rock comprising a generally mafic paleosome biotite or hornblende dominant material and a neosome late tectonic pegmatite. Coronitic metagabbro has been found in two isolated segments on the property. The rock is commonly mafic to ultramafic and coarse grained. In many cases, especially towards the core of an intrusion, relict clinopyroxenes have been preserved generally rimmed by amphiboles.

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TABLE 2: TABLE OF ROCK UNITS FOR THE PARRY SOUND AREA PHANEROZOIC CENOZOIC Quaternary Recent swamp, lake, and stream deposits

Pleistocene bouldery, cobbly and silty sand till, silt sand, pebble gravel, and cobble gravel _________Unconformity (possible regolith)________ PALAEOZOIC Cambro - Ordovician Calcareous fracture fillings _________Unconformity_________ PRECAMBRIAN

Late Precambrian Late Breccias- thin mylonites; quartz veined dilatant breccias of unknown origin Late Pegmatite massive granite pegmatite dikes _________Intrusive Contact______ High Rank Regional Metamorphism Middle to Late Precambrian Tectonites Mylonite: very fine grained massive to thinly to thickly laminated rock frequently exhibiting compositional and graded layering and containing rotated porphyroclasts; generally marginal to schistose and gneissic rocks; matrix minerals generally are siliceous and comprise quartz, microperthite, biotite and/or amphibole and/or pyroxene Tectonic Breccia: brecciated rock comprising lithic clasts within a fine to coarse grained schistose to gneissic cataclastic matrix with quartz, perthitic microcline, biotite and/or amphibole and/or pyroxene __________Sheared ContactSyenite and Monzonite Suite Intrusive Rocks pink to grey and green, massive to porphyritic to lineated and gneissic biotite, homblende-biotite and hornblende syenite and monzonite, charnokite and mangerite. _________Intrusive Contact_________ Face 11

Anorthosite Suite Intrusive Rocks Anorthosite- massive to gneissic labradorite anorthosite, andesine anorthosite with up to 10*56 pyroxene, and gabbroic anorthosite _________Intrusive Contact -^^ Gabbro- massive to gneissic fine to coarse grained, black pyroxenite, anorthosite gabbro and gabbro _________Intrusive Contact_______^^^^ Tonalite- massive to strongly lineated and gneissic light to dark grey pyroxene tonalite and diorite with minor gabbro _________Intrusive Contact ^ Quartz Monzonite - Syenite Suite Intrusive Rocks massive to gneissic medium to coarse grained biotite quartz monzonite, pyroxene quartz monzonite and foliated granite pegmatite, pyroxene syenite and foliated syenite pegmatite; megacrystic granite and derivatives. _________Intrusive Contact- ^^^ Parry Sound Group Metavolcanic Rocks1 Spider Lake Formation1 : intermediate to felsic rocks, medium to coarse grained generally porphyritic, massive to gneissic rocks containing quartz, feldspar, almandite, amphibole and pyroxene; some fragmental units present Parry Sound Formation1 : mafic, medium to coarse grained, schistose to gneissic, pyroxene-feldspar and amphibole-feldspar bearing massive and fragmental rock Sans Souci - Killbear Point Group Metasedimentary Rocks1 Unsubdivided: thinly laminated to extremely thickly layered; interiayered medium to coarse grained schists and gneisses; lower amphibolite to granulite facies; intercalated with metavolcanics above Killbear Point Formation1 : thinly to extremely thickly layered, schistose and gneissic medium to coarse grained biotite, quartz, feldspar rocks Bateau Island Formation1 : very thickly layered, medium to coarse grained felsic gneiss with mafic biotite and amphibole rich parting planes; variously interpreted as an arkose or granite; cataclastic textures. 1 The formation names have not been accepted and criteria for introduction of these names into the literature have not been fulfilled. Identification as to origin is tentative

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PROPERTY GEOLOGY

The property principally is underlain by felsic rocks of unusual character of Middle to Late Precambrian age. The pre-metamorphic origin of these rocks is obscure. In addition, the degree of thermal and dynamic metamorphism to which these rocks were subjected through multiple stage or polyphase deformation is difficult to determine in the field. The individual rock units were described under the heading DESCRIPTION OF ROCK UNITS on Page 9 of this report. The granite gneiss is generally hypidiomorphic granular. Several features of this rock unit infer at least a partial metamorphic origin: cataclastic textures including tectonic grain gradation characterize the fine grained portions of the unit and frequently occur wrth regularly spaced biotite and amphibole rich partings; the cataclastic grain classification forms a strong gneissic foliation in portions of the unit; significant portions of the unit comprise a matrix supported, pegmatite breccia which consists of apparently unstrained microcline porphyroclasts in a gneissic, fine to coarse grained, granitic ground mass. The genesis of this material would also be obscured except for some textbook quality examples in road cuts near the property on Hwy 559 where a well constituted coarse grained granite pegmatite grades laterally into a pegmatite breccia. A portion of both the fine and coarse grained varieties have purple to dark red speckles of hematite. Despite the apparent role of dynamic metamorphism in the genesis of this rock unit several large outcrops expose uniform occurrences of massive, equigranular granite possibly suitable for monument stone. In the purple and pink migmatite, the granite gneiss appears to form the introduced neosome constituent which appears to have been reduced in grain size by cataclasis (many examples of syntectonic pegmatites reduced to fine grained neosome constituents are evident in the region within both the Britt domain and the Moon River domain). The paleosome layer in a few places still contains over 1 Q07o biotite and exhibits a relict foliation; however, this material appears to be a schlieren produced by the process of granitization. The hematite which macroscopically appears to follow the biotite foliation or occur in streaks parallel to the gneissic foliation, microscopically coats the grain boundaries of all the other minerals and is translucent in character. The hematite spotting which is very strong in this unit is a regional feature of the area and is frequently erroneously attributed to almandite. In a variety of the pink and purple migmatite a pale to buff medium to coarse grained pegmatite forms lit par lit stringers parallel to the gneissic foliation. This material is of late tectonic origin and forms some very attractive textures. Frequently the late tectonic pegmatite exhibits pinch and swell textures over very large areas. This might provide a target material for quarrying. A very attractive, voluminous, and somewhat unique variety of the pink and purple migmatite is a breccia or crenulation of the purple material in the pink granitic or the buff pegmatitic materials.

Page 13

The more common migmatite contains thick paleosome sections from 2 cm thick to 2 metres thick in a lit par lit arrangement with late tectonic, quartz-rich, pink to grey granite pegmatite. The paleosome is generally over 5007o mafics with biotite being more frequently the mafic mineral than amphibole. The migmatite is frequently flanked by the purple and pink migmatite giving the impression that the varieties of rock evidence gradational granitization. The general pattern displayed by the gneissic foliations on the property is of a relatively structurally uniform sequence which is flat lying to gently southeast dipping. In descending order the three most prominent joint directions on the property are at 1500 , 75 0 , and 25". With total outcrop exposure approaching 700Xo over the whole property it is very encouraging to note that the average horizontal and sub-horizontal joint spacing on the property is 2 metres from observable surfaces and the vertical joint spacing averages over 5 metres. Indeed many areas were seen with joint spacings in excess of thirty metres. POTENTIAL DIMENSION STONE SITES

At least four distinctive potential dimension stone products may be found in various locations on the property. Although there are a large number of potential quarry sites, five appear to be more outstanding due to existing vertical faces or the presence of a steep hill. Three of these sites were mapped on an approximate 1:500 scale and a site plan has been produced for each area. The first site plan (Killbear#1) (Figure 5) is located at the west side of lot 66, Concession 10, claim S01151129 . The site plan covers an area 140 metres X 50 metres and a vertical rise of 5 metres, and its location is indexed on Figure 2. The site exposes some lit par lit purple and pink migmatite and brecciated purple and pink migmatite which are continuous in outcrop over large portions of a hill which is 400 metres X 500 metres and rises 10 to 15 metres above the surrounding drainage. Sub-horizontal joint spacings exceed 2 metres and vertical joint spacings are from 2 to 30 metres. The major joint strikes between 160 0 and 180 0 parallel to the axis of the hill. Three minor discontinuous cross joints were seen at azimuths ranging from 60 c to 80". The gneissic foliation is uniform at 000 0 dipping 20"E. A subhorizontal joint is apparently parallel to the gneissic foliation. It is apparent that the joint separation on the sub-horizontal set is possibly up to 4 metres. A drill hole is planned to confirm this joint separation. The existing data is to be evaluated using AutoCAD in order to design the test site and estimate waste factors. Photos 1 depicts the site plan area of Killbear #1 looking north and Photo 2 shows the purple and pink migmatite breccia in outcrop some 70 metres east of the site plan area. A sample (Killbear #1) was collected from the cliff face for ASTM tests for water absorption and bulk specific gravity, modulus of rupture and compressive strength. The test results were satisfactory. Page 14

19Tm 139m

Concession 1O

Lot ea Claim 1151129

196m

O i z3*B

195m

LEGEND contour

Co* Wooded

Note: UTM Coordinates for the AOutnwest corner of the map sheet

ssseeem E; 5O2-4136m N

JR TRUSLER SITE PLAN KILLBEAR 1 Carlin Twp, Ont VERTI AL JOINTS Date Dec 28. 1995 JRT

Photo 1: Killbear #1 Site looking north; note the cross joint separation exceeds 30 metres. Photo 2: Killbear #1 Srte 70 metres east of mapped portion; example of the purple and pink migmatite breccia; also note the large joint spacing.

Page 16

The best area noted for extraction of pegmatite breccia ( Photo 3 ) is located in the middle of concession 9 at the junction of lots 64 and 65. wrthin daim SO1151136 A north facing cliff nses 5 metres above a winter road on the southern fringe of a swamp Designated as Site Plan Killbear 2 on Figure 6 an area 120 metres square has been mapped on a scale of 1:507 The location is indexed on Figure 2. The pegmatrte breccia is very consistent and extensive covering an area 400 metres X 300 metres wrth up to 10 metres of relief All vertical joint spacings exceed three metres with the prominent joint directions being 20 , parallel to the diff. 80 C to 100 C and 135 The upper sub-horizontal joint spacing where exposed in the diff is 4 metres whereas betow that several discontinuous joints have 1 to 2 metre spacing (Photo 4). A dnll hole is planned here to test the sub-horizontal joint spacing in preparation for a future quarry test Site Plan Killbear 3 ( Figure 7) is located at the west side of lot 66. Concession 10, daim SO1151129 approximately 50 metres north of and on the same extensive hill as Killbear 1 The rock exposed is chiefly a pegmatrte breccia wrth purple migmatite intermixed and brecciated as well The site covers an area 100 metres X 140 metres and has a relief of 6 metres A four metre diff (Photo 5) trends at 165 : parallel to a prominent vertical joint The other vertical joints trend at 80 to 110 : . 120' and 15 Most of the joints are widespaced .and the recovery of large dimension stone blocks would be favourable

PhotoS S.io ,^r. Kiilbear 2 looking northeast, the cliff faces northwest and its lip is in the background. Page 17

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Claim 1 151 13O

Photo 4: Kiflbear 2 Site Plan area looking southeast, note the upper portion or 4metres of the cliff does not have a joint The winter road leads approximately 250 metres from Hwy 559 to this point. Photo 5: Killbear 3 Site Plan area looking east northeast at a cliff face with no exposed sub-horizontal jointing . the diff rises 4 to 5 metres.

Page 19

196m 197m 193m

2OOm

195m

Claim 1151129 Concession 10

Lot ea

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LEGEND Tra*l Lot Itrto Wooded

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JR TRUSLER SITE RLAN KILLBEAR 3

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C arling Twp., Ont,

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Date;Dec 28.1 995 JRT

Figure 7 Page 20

CONCLUSIONS The Britt domain comprises a complexly deformed and metamorphosed series of rocks. Although some of the rocks are metasedimentary in origin the preponderance of the rocks were originally plutonic, but have been changed by dynamic and thermal metamorphism. The final stages of this metamorphism appear to have annealed the rock into a compact and durable material having some relict textures and many overlapping and lively features.

The Killbear Point property comprises 500 acres, and is underlain by complex migmatites of Middle to Late Precambrian age. A study of the joints and joint spacings suggests that most of the property would yield a high percentage of 30 tonne blocks of dimension stone. Four potential product lines have been identified in five potential quarry sites. Two of the potential product lines are unique and the other two are similar to other stone already being marketed. All of the stone appears to be of good quality and very attractive. Three sites were mapped at an approximate scale 1:500 and site plans showing 1 metre contours, the existing ground conditions and joints were produced. The three sites designated Killbear 1, 2 and 3 respectively contain purple and pink migmatite, pegmatite breccia, and purple and pink breccia intermixed with pegmatite breccia. Each site is very prospective for dimension stone and 30 tonne blocks are apparently quarriable with low waste factors. Killbear 1 was sampled, and a preliminary set of ASTM tests conducted by Inchcape Testing Services achieved satisfactory results. Drilling of Killbear 1 and 2 are planned. Further site planning, calculation of waste factors in a test quarry and permitting are to precede an effort to finance this next stage. RECOMMENDATIONS

Efforts are to be concentrated on further testing and development of the purple and pink migmatite and the pegmatite breccia: 1. Killbear 1, on claim 1151129, is to be drill tested. An assessment of waste and cost factors involved with a quarry test and permitting through the testing stage are recommended. The quarry test will involve the removal of approximately 3,000 tonnes in 30 tonne blocks from the site. 2.

Killbear 2, on claim 1151136, is to be drill tested. An assessment of waste and cost factors involved with a quarry test and permitting through the testing stage are recommended. The quarry test will likely require removal of some 1,000 tonnes of material in 30 tonne blocks from the site.

Killbear 3, on claim 1151129, should have the site planning exercise completed on it involving an assessment of waste and cost factors associated with a quarry test.

Initial licensing should proceed with the Minister of Northern Development and Mines to licence two sites for removal of up to a 3000 tonne test sample at each site; public information meetings will be required.

Page 21

REFERENCES Bell, R. 1876. Report on geological researches north of Lake Huron and east of Lake Superior; in Geological Survey of Canada Report on Progress 1876-77. Bennett, P. J. 1975. The deformation of the northern half of the Brandy Lake Complex, Port Carling, Ontario. M.Sc. thesis, Department of Geology, University of Toronto, Toronto, Ont. Bright, E.G. 1987. Precambrian geology of the Whitestone Lake area, District of Parry Sound; Ontario Geological Survey, Map P.3095, Geological Series-Preliminary Map, scale 1:15,840, geology 1986. Culshaw, N.G., Davidson, A., and Nadeau, L. 1983. Structural subdivisions of the Grenville Province in the Parry Sound-Algonquin region, Ontario; in Current research , pt. B, Geological Survey of Canada, Paper 83-1B,p.243-252. Culshaw, N.G., Corrigan, D., Drage, J., and Wallace, P. 1988. Georgian Bay geological synthesis: Key Harbour to Dillon, Grenville Province of Ontario; in Current research, Part C, Geological Survey of Canada, Paper 88-1 C, p. 129-133. Davidson, A. 1984a. Identification of ductile shear zones in the southwestern Grenville Province of the Canadian Shield. In Precambrian tectonics illustrated. Edited by A. Kroner and R. Greiling. E. Schweizrbart'sche Veriagsbuchhandlung (Nagele u. Obermiller), Stuttgart, Germany, pp. 263-279. 1984b. Tectonic boundaries within the Grenville Province of the Canadian Shield. Journal of Geodynamics, 1: 433-444. 1986. New interpretations in the southwestern Grenville Province, edited by J.M. Moore, A. Davidson and A Baer, Geological Association of Canada, Special Paper 31,p.61-74 Davidson, A. and Morgan, W.C. 1981. Preliminary notes on thegeology east of Georgian Bay, Grenville Structural Province, Ontario; in Current research, pt. A, Geological Survey of Canada, Paper 81-1A,p.291-298. Davidson, A, Culshaw, N. and Nadeau, L. 1982. A tectono-metamorphic framework for part of the Grenville Province, Parry Sound region, Ontario; in Current research, pt.A, Geological Survey of Canada, Paper 82-1A, p.175-190. Fahrig, W. F. and West, T. 1986. Diabase dyke swarms of the Canadian shield; Geological Survey of Canada, Map 1627A, scale 1:4,873,900. Fouts, C.R. and Marmont C. 1989. Gneisses of the Parry Sound-Muskoka Area; Flagstone resources, Ontario Geological Survey, Open File Report 5725 Page 22

Garland, M. 1987. Graphite in the Central gneiss belt of the Grenville Province of Ontario; Ontario Geological Survey, Open File Report 5649. Hanmer, S. 1984. Strain-insensitive foliations in polymineralic rocks; Canadian Journal of Earth Sciences, v.21, p.1410-1414. ______ 1988. Ductile thrusting at the mid-crustal level, southwestern Grenville Province; Canadian Journal of Earth Sciences, v.25, p. 1049-1059. Harrison, J.C. 1977. Geology and structure of the Go Home Bay area, District of Muskoka, Ontario. B.Sc. thesis, Department of Geology, University of Toronto, Toronto, Ont. Hewitt, D.F. 1967. Geology and mineral deposits of the Parry Sound -Huntsville area; Ontario Geological Survey, Geological Report 52, 65p. Innes, D. G. 1992. Assessment Work Report, Ardbeg Property, Burton Township, Ontario, 1886 Holdings Ltd. Ont Min of Nor Dev and Mines Asssessment files. Lacy, W.C. 1960. Geology of the Dunchurch area, Ontario; Geological Society of America Bulletin, Volume 71, p. 1713-1718 Lashbrook, Raymond L. 1990a. Geological Report on The Woods Road Property, Carling Township, Ontario. 1886 Holdings Ltd. Ont Min of Nor Dev and Mines Asssessment files. 1990b. Geological Report on Burton Township, Ontario. 1886 Holdings Ltd. Ont Min of Nor Dev and Mines Asssessment files. Lindia, P.M., Thomas, M.D. and Davidson, A. 1983. Geological significance of the Bouger gravity anomalies in the region of the Parry Sound domain, Grenville Province, Ontario; in Current research , ptB, Geological Survey of Canada, Paper 83-1 B, p. 261-266. Lumbers, S.B. 1975. Geology of the Burwash area; Ontario Division of Mines, Geological Report 116,160 p., with Map 2271 scale 1:126,720. Macfie, R.I. 1988. Preliminary investigation of the Parry Sound -Seguin domain boundary; in Summary of field work and other activities 1988, by the Ontario Geological survey, Ontario Geological Survey, Miscellaneous Paper 141, p.315-318.

Macfie, R.I. and Dixon, J. M. 1990. Tectonic relations among Parry Sound domain and Seguin and Rosseau sub-domains Grant 370; in Geoscience Research Grant Program Summary of Research 1989-1990, Ontario Geological Survey, Miscellaneous Paper 150, 1990, p.200-212. Page 23

Marmont, C., Zuberec, P.M., and Conrod, W.D. 1988. Industrial minerals, rare-earth elements, and building stone in the Districts of Muskoka, Parry Sound, and Nipissing and the County of Haliburton; in Summary of Field Work and Other Activities 1988, by the Ontario Geological Survey, Ontario Geological Survey, Miscellaneous Paper 141, p.319-325. Marmont, C. 1992. Industrial minerals and building stone in the Districts of Nipissing, Parry Sound and Sudbury;in Summary of Field Work and Other Activities 1992, Ontario Geological Survey Miscellaneous Paper 160, p.261-265. 1992. Building Stone Opportunities in Central Ontario -1991 Supplement. Ontario Geological Survey, Open File Report 5825, 20p. 1993. Exploration Guidelines and Opportunities for Dimensional Stone in Central Ontario. Ontario Geological Survey, Open File Report 5853, 83p. McRoberts, G., Macfie, R.I. and Hammar, D. J. 1988. Geology of the Manitouwabing Lake area, District of Parry Sound; in Summary of Field Work and Other Activities 1988, by the Ontario Geological Survey, Ontario Geological Survey, Miscellaneous Paper 141, p.309-314. McRoberts. G., and Tremblay, M.L, 1988. Precambrian geology of the Ferrie River area, District of Parry Sound; Ontario Geological Survey, Map P. 3123, Geological SeriesPreliminary Map, scale 1:15,840 Murray, A. 1848. On an examination of the shores, islands and rivers of Lake Huron including parts of the east coast of Hudson Bay and the Spanish Riven in Geological Survey of Canada Report of Progress 1848-49. Nadeau, L. 1984. Deformation of leucogabbro at Parry Sound, Ontario. M.Se. thesis, Carlton University, Ottawa, Ont. Parks, W.A. 1900. Work in the Muskoka district, Ontario; in Geological Survey of Canada, Summary report for 1900, part A pp. 121-126 (pub 1901). Satterly, J. 1942. Mineral Occurrences in Parry Sound District, Ontario Department of Mines, v.51,Part 2,41 p. with Map 1942-2. Satterly, J. 1955. Geology of Lount Township; Ontario Department of Mines Annual Report, v.64, Part 6, 43p.. with Map 1955-4, scale 1:31.680. Schwerdtner, W. M., and Bauer, G. 1975. Tectonic significance of mylonite zones. Neues Jahrbuch fur Mineralogic, Monatshefte, No. 11: 500-509. Schwerdtner, W.M., and Mawer, C.K 1982. Geology of the Gravenhurst region , Grenville Structural Province, Ontario. In Current research, part B. Geological Survey of Canada, Paper 82-1 B, pp. 195 - 207. Page 24

Schwerdtner, W.M., and Waddington, D.H. 1978. Structure and Lithology of Muskoka southern Georgian Bay region, Central Ontario. In Toronto 78 Field Trips Guidebook. Edited by A.L. Currie and W.O. Mackasey. Geological Association of Canada, pp. 204-212. Schwerdtner, W.M., Waddington, D.H., and Stollery, G. 1974. Percrystalline pseudomorphs as natural gauges of incremental paleostrain. Neues Jahrbuch fur Mineralogie, Monatshefte, No. 3/4: 174-182. Schwerdtner, W.M., Bennett, P.J., and Janes, T.W. 1977. Application of L-S fabric scheme to structural mapping and paleostrain analysis. Canadian Journal of Earth Sciences, 14: 1021-1032. Schwerdtner, W.M., Mawer, C.K., and Hubbs, A. F. 1981. Geology of the Gravenhurst region, Grenville Structural Province,Ontario: Preliminary mapping results. In Current research, part B, Geological Survey of Canada, Paper 81-1B, pp. 167-169. Schwerdtner, W. M. 1987. Interplay between folding and ductile shearing in the Proterozoic crust of the Muskoka-Parry Sound region, central Ontario; Canadian Journal of Earth Sciences, v.24, p. 1507-1525. Tajerian, Taline and Jones V. W. 1996. Testing of Two Sets Of Dimension Stone: Woods Road #1 and Killbear#1; Inchcape Testing Services NA Ltd. Jan. 15, 1996 Tremblay, M.L. 1988. Remote sensing study of curvilinear, structural features in the Parry Sound domain, Grenville Province; in Summary of field work and other activities 1988, Ontario Geological Survey Miscellaneous Paper 141 pp.326-329. Trusler, J.R. and Villard, D.J. 1980. Geology of the Parry Sound-Sans Souci map area; scale 1:31,680, unpublished manuscript and map done for the Ontario Ministry of Natural Resources. Trusler, J.R. 1992.Prospecting Programme for Flagstone and Decorative Stone in the Parry Sound District of Ontario. OPAP File No.: OP92-174

1993a. Geological Reconnaissance for Flagstone and Dimension Stone in the Parry Sound District of Ontario; Regional survey submitted to Assessment Files, Ontario Geological Survey. Trusler, J.R. 1993b. A Geological Survey of the Dimension Stone Resouces on the Killbear Point Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. 1993c. A Geological Survey of the Dimension Stone Resouces on the Black Lake Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. Faae 25

Trusler, J. R. 1993d. A Geological Survey of the Dimension Stone Resouces on the Burnt Lake Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. 1993e. A Geological Survey of the Dimension Stone Resouces on the Dillon Road Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. 1993f. A Geological Survey of the Dimension Stone Resouces on the Shebeshekong Lake Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. 1993g. A Geological Survey of the Dimension Stone Resouces on the Grundy Lake Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. 1993h. A Geological Survey of the Dimension Stone Resouces on the Jacknife Harbour Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. 1993i. A Geological Survey of the Dimension Stone Resouces on the Turtle Lake Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. 1993j. A Geological Survey of the Dimension Stone Resouces on the Woods Road Property, Parry Sound District of Ontario; survey submitted to Assessment Files, Ontario Geological Survey. van Berkel, J.T., and Schwerdtner, W.M., W.M. 1986. Structural geology of the Moon River area. Ontario Geological Survey, P2954(with marginal notes). van Breeman, O., Davidson, A., Loveridge, W.D. and Sullivan, R.W. 1986. U-Pb zircon geochronology of the Grenville tectonites, granulites and igneous precursors, Parry Sound, Ontario; in The Grenville Province, edited by J.M. Moore, A. Davidson and A. Baer, Geological Association of Canada, Special Paper 31, p. 191-208. Waddington, D. H. 1973. Foliation and mineral lineation in the Moon River synform, GrenvilleStructural Province, Ontario. M. Se. thesis, University of Toronto, Toronto, Ont.

Walker, T. L. 1905. The Muskoka district, Ontario; in Geological Survey of Canada, Summary report for 1905, p.84-86, (published 1906) _______ 1913. The precambrian of Parry Island and vicinity; in Geological Survey of Canada Guide Book No. 5., p. 98-100. Wynne-Edwards, H. R. 1972. The Grenville Province; in Variations in tectonic style in Canada, edited by R.A. Price and R.J.W. Douglas, Geological Association of Canada, Special Paper 11, p263-344. Paae 26

AUTHOR'S CERTIFICATE

This report was prepared by: James R. Trusler P.Eng. Principal, J R Trusler and Associates 143 Temperance St. Aurora, Ontario L4G 2R5 (416) 727-5084 GEOLOGICAL ENGINEER,

Qualifications:

B A Se - Geological Engineering, University of Toronto, 1967 MS- Geology, Michigan Technological University, 1972 Professional Engineer - Ontario Fellow - Geological Association of Canada Member - Canadian Institute of Mining, Metallurgy and Petroleum c.

This report is based on a review of all available relevant data; historical, and geological, on personal involvement as Regional Geologist, Algonquin Region, Ministry of Natural Resources from 1974 to 1980, and on a program of field mapping conducted within the area of this report in 1993. l have personally examined the properties and the surrounding area in the field.

l have used my experience gained in geological mapping, the exploration for minerals, visits to most dimension stone quarries in North America, the definition of mineral deposits and the evaluation of properties (over 30 years) in preparation of this report.

l hold an undivided 1000Xo interest in the claims mentioned in this report, but do not expect to receive any remuneration for the report or as a result of statements made in this report. Signed

Dated:January 29, 1996 . ,

'~ James R. Trusler M.S., P.Eng.

FEB. -061 96 (M) 11 = 46 Mtntofi y d Northern Doviilopfrient and Mine*

RECORDING OPPICE TOR

TEL:4I6 314 3789

Report of Work Conducted After Recording Claim

Ontario

P. 001

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Mining Act

2.1842?

- Please type or print and submit In duplicate. - Refer to the MInmg Act and Regulations for rea* Recorder. - A asperate copy of this form must be complete) - Technical reports and maps must accompany t) - A sketch, showing the claims the work le

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ot*: The Minister may reject for assessment work credit afl or part of the assessment work tubmttled if the recorded holder cannot verify expenditures claimed m the statement of costs wftNn 30 days of a request for verification. end Survey Company Who Performed the Work (Give Name and Address of Author of Report) —————Nimi——————————————————————————————————— —— Address

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Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following: 1. 2. 3.

D Credits are to be cut back starting with the claim listed last, working backwards. ©"Credits are to be cut back equally over all claims contained in this report of work. Q Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented. Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims. Note 2: If work has been performed on patented or leased land, please complete the following: l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature

Date

Ontario

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Northern Development and Mines

for Assessment Credit

Ministers du Developpemenl du Nord et des mines

tlat des couts aux fins du credit devaluation Mining Act/Loi sur les mines

Transaction No./N 0 de transaction

2. 164

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager. Minings Lands. Ministry of Northern Development and Mines. 4lh Floor. 159 Cedar Street. Sudbury. Ontario P3E 6A5. telephone (705) 670-7264

Les renseignements personnels contenus dans la presente lormule sonl recueillis en vertu de la Lol sur les mines el serviront a lenir a jour un registre des concessions minieres. Adresser toute question sur la collece de ces renseignements au chef provincial des terrains miniers. ministere du Developpement du Nord el des Mines. 159. rue Cedar. 4* elage. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264

1. Direct Costs/Couts directs

2. Indirect Costs/Couts indirects Amount Montan!

Description

Type

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 admissibtes en lant que travaux devaluation.

Totals Total global

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Wages Salalres

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Valeur totale du credit devaluation (ToUI d** codu directs M Indirect* dmbtMM

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Q Mate A Le Ukik re enregistre sera tenu de verifier les depenses deimanrJeas dans Note: The recorded holder will be required to verify expendi res claimedjn this statement of costs within 30 days of a request fc vetSiicftienPlf ~ " '""^lens nt etat des couts dans les 30 jours suivant une d emande a eel effef? S la verification n'est pas etlectuee. le ministre pe ut rejeler tout verification is not made, the Minister may reject for a; essment work all or part of the assessment work submitted. aartie des Iravaux d 'evaluation presentes.

MINING LANDS BRAWtJfl6

Filing Discounts

Remises pour depot

Work filed within two years of completion is claimed at 1000xfa of the above Total Value of Assessment Credit.

1 . Les travaux deposes dans les deux ans suivant leur achevement sont rembourses a 100 4b de la valeur totate susmenlionnee du credt devaluation

Work filed three, four or five years after completion is claimed at SO^ti of the above Total Value of Assessment Credit. See calculations below:

2. Les travaux deposes trois. quatre ou cinq ans apres leur achevement sont rembourses a 50 "to de la valeur totale du credit devaluation susmentionne Voir les caJculs ci-dessous.

Total Assessment Claimed

Total Value of Assessment Credit

Valeur totale du credit devaluation

Evaluation totale demandee

x 0.50

Certification Verifying Statement of Costs

Attestation de I'etat des couts

l hereby certify: that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

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 devaluation sur les terrains indiques dans la for mule de rapport de travail ci-joint.

l am authorized

Et qu'a litre de ___________________ je suis autorise

that as

(Recorded Holder. Agent. Position m

(Ululajie anregistrt. representant. poste occupA dans la compagrae)

a faire cette attestation.

to make this certification

Date

0212(04^1)

Nota : Dans cette

ne des personnes. le masculin est utilise au sens neulre.

PROPERTY

The Killbear Point property comprises approximately 500 acres and is more particularly described in TABLE 1 (Figure 2). Assessment was applied to the daims in 1993, and this report will be filed for assessment. As a result sufficient credits should be available to keep the entire claim group in good standing for some three years from date of filing. TABLE 1: KILLBEAR POINT PROPERTY

Claim No

Township

Lot

1151129

Carling

1151135 1151136

Carling Carling

66 XI 66 X 64 X 64.65 IX

Cone.

Area Recording Date 200 ac 100 ac 200 ac

KILLBEAR 3 SITE PLAN KILLBEAR 1 SITE PLAN

Scale: 1:20.000 ", -*

Figure 2: Property Map ?aae 3

Oct.23, 1991 Nov. 5. 1992 Nov. 5. 1992

Ontario Mn , . Northern Development and Mines

Geoscience Assessment Office g33 Ramsey Lake Road g^n pi oor

n, dU ,H K. H Developpement du Nord et des Mines

Sudbury, Ontario P3E 6B5 Telephone: (705) 670-5853 Fax: (705) 670-5863 April 30, 1996

Our File: 2.16427 Transaction #: W9690. 00008

Mining Recorder Ministry of Northern Development St Mines MacDonald Block, Room M2-17 900 Bay Street Toronto, Ontario M7A 1C3 Dear Mr. Denomme: SUBJECT: APPROVAL OF ASSESSMENT WORK CREDIT ON MINING LAND, CLAIMS SO. 1151129 6 1151135 IN CARLING TOWNSHIP

Assessment work credit has been approved as outlined on the Declaration of Assessment Work Form accompanying this submission. The credit has been approved under Section 12, Geology, of the Assessment Work Regulation. THE APPROVAL DATE IS APRIL 29, 1996.

If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5858. Yours sincerely, ORIGINAL SIGNED BY:

Ron C. Gashinski Senior Manager, Mining Lands Section Mines and Minerals Division LBJ/jl

cc: Resident Geologist Sudbury, Ontario

ssessment Files Library Sudbury, Ontario

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