RESULTS OF STRIPPING AND TRENCHING CONACHER TOWNSHIP PROPERTY

FOR CONSOLIDATED NORTH COAST INDUSTRIES

AND LANDORE EXPLORATION INC.

August 31, 1996

Claude LaroucheOvalbay Geological Services Inc.1070 Lithium Drive, Unit # 3Thunder Bay, OntarioCanada, P7B 6G3Tel: (807) 623-3770 Fax: (807) 623-2335

52B09NE0091 W9640.00508 CONACHER 010

CONSOLIDATED NORTH COAST INDUSTRIES 1070 Lithium Drive, Unit # 3 Thunder Bay, Ontario P7B 6G3

Shebandowan property: Conacher - Hagey townships

COST OF WORK

Line cutting + chainingl km @ $475.00/km ........... . . . . . . . . . . . . . . . $ 475.00

Stripping (Skidder, M. Bouleau Drilling) Including mobilization and demobilisation

36 hours @ $100.00/hr . ... . . . . . . . . . . . . . . . . . . $ 3,600.00Hand cleaning, washing, driling and blasting2 men @ $150.00/day/man(Daniel Calvert+Jeremie Larouche)

20 days @ $300.00/day ...... .. . . . . . . . . . . . . . . $ 6,000.00Rental Air compressor 4- hoses + drill

4 days @ $300.00/day . . . . . . . . . . . . . . . . . . . . . . . $ 1,200.00Dynamite . . . . . . . . . ...... .......... ....... . . . . . . . . ^ 100.00Transportation (road)

2916 km @ $0.30/km ......................... $ 874.80Food . . . . . . . . . . . . . . . . . . . . . . . . . . . .. ... . . . . . . . . . . . . ^ 540.00Mapping - prospecting - research - drafting

Geologist 2.4 days @ $350.00/day ........... $ 865.00Photocopies and reproduction .................... $ 59.50Administration office ........................... $ 685.70

$14,400.00

_Claude LaroucheOvalbay Geological Services Inc.

Figure 1: Location Map

4

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REBAGL1ATI GEOLOGICAL CONSULTING L

North Coast Industries Ltd. Vancouver, British Columolo

LOCATION MAP

Hag Lake PropertyCONACHER S HAGEY TOWNSHIF Thunder B ay Mining Division. On rcr:

Dot*: January. 1988 l NTS:

5S7I3I 886676 l 557123

l 1082853* J___^ .L.--—r '

Figure 2: Sketch of Claims

RECENT WORK

During the period of October 01, 1994 to September 01, 1996, prospecting and stripping + trenching has been conducted intermittently on the Conacher and Hagey townships mining claims. Following a detailed compilation and a re- evaluation of the available data, it became evident that the claims under study cover geological structures of significant potential for the discovery of mineralization of economic interest in gold and base metal. Attached to the present study is a copy of the report entitled:

Evaluation of Previous Exploration WorkandPotential for Gold ExplorationConacher - Hagey PropertiesforLandore Exploration Inc.

The work described in the following pages has been centered on two old trenched areas which have been opened and detailed in order to acquire geological and structural informations needed to continue the systematic evaluation of the mining property under study.

The work has been carried out under the supervision of Claude Larouche of Ovalbay Geological Services Inc, Thunder Bay, Ontario, Canada. Daniel Calvert of Murillo Ontario and Jeremie Larouche of Thunder Bay, Ontario were involved with the field work beside the author.

The claims are registered under the names of:1-) Consolidated North Coast Industries

1070 Lithium Drive, Unit # 3 Thunder Bay, Ontario P7B 6G3

2-) Daniel CalvertP.O. Box 32, MurilloOntarioPOT 2GO

The stripping has been completed by a skidder owned and operated by M. Boileau Diamond Drilling of Val D'Or, Province of Quebec. An air compressor was also used to move some of the overburden and to drill short holes for blasting. The areas were mapped in detail, see attached maps.

Map 1: Trench straddling the claim boundary between claims TB-1195669 and TB-1209701. This trench is of interest because of the fragmental unit also containing fragments of massive pyrite. This unit is a marker which has been intersected further east, just north of the Bandore Zone # 4 which contain geological reserves of 1.4 Mt grading 0.12 opt Au.

Map 2: Trench located on claim 1210004. The area is underlain mainly by the Shebandowan Lake Stock which is highly fractured and schistose. The area is possibly located very close to where the Bandore Zone #4 shear zone would intersect the Shebandowan Lake Stock.

It is recommended to systematically cover the block of claims with a detailed ground magnetic and Em survey. Geological mapping would follow along with more diamond drilling on the known gold showings and the better geophysical anomalies. A budget of $250,000. is recommended for the next phase of exploration.

agnetic Axl Diabase ?

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EVALUATION OP PREVIOUS EXPLORATION WORKAND THE

POTENTIAL FOR GOLD EXPLORATION CONACHER-HAGEY PROPERTIES

FOR LANDORE EXPLORATION INC.

CLAUDE LAROUCHE, P. Eng. November 30, 1995ANDREAS LICHTBLAU, MSc. Geol.Ovalbay Geological Services Inc.1070 Lithium Drive, Unit #3Thunder Bay, OntarioP7B 6G3

PREVIOUS WORK

The first recorded work on the present claim group was performed by Ourgold Mining Co., who blasted eight trenches on what is now claim #557151. Lobanor Gold Mines Ltd, drilled 14 holes (totalling 3657.6m) along the Conacher/Hagey township line, south of Hag Lake, in 1944. The original discovery in this part of the area came in hole #2, with intersections of:

0.099 opt AU/4.28HI,0.148 opt Au/l.OSm and0.080 opt AU/0.34HI.

Lobanor experienced legal difficulties in the late 1940's and was subsequently forced to terminate work. When the property was acquired and staked by Greenwich Lake Exploration Ltd, in 1980, the original Lobanor holes were not all found in the field and their data was found to be incomplete a*hd self-contradictory.

1980-

1981-

1982-

1983-

1984-

1985-

1986-

The following list summarizes work done since 1980:

Greenwich Lake Exploration options the property to Mattagami Lake Exploration Ltd.

Mattagami performs 74.3km Mag, 67.6km IP and a soil survey (?)Mattagami drills 4 holes (totalling 533.7m); GW-81-1 returns 0.798 opt Au74.03m (uncut)

Mattagami conducts a detailed IP survey and drills afurther 6 hole (833.8m). GW-82-5 intersects 0.17 optAu72.02m.Mattagami drops the option

Geological mapping is carried out over the newly acquired Halverson claims, by Greenwich Lake

a "B" soil horizon survey is conducted over the property (Au, Cu, Zn) by the newly restructured GLE Resources. the property is optioned to Lincoln Resources Inc.

Geological mapping is carried out over the property for Lincoln Resourcesdetailed Mag, VLF, and IP (llkm) are conducted over one claim covering the original Hag Lake occurrence Lincoln Resources drills 3 holes (527.9m) based on a new structural interpretation from geophysics

Lincoln drills a further lithology/structure

3 holes (551.1m) based on

a limited IP survey is performed for new option partner North Coast Industries, followed by an 8 hole (1276.3m)

program

1988-

drill

The property has remained idle since 1988.

REGIONAL GEOLOGY

The Shebandowan portion of the Wawa subprovince is a 16km X 10km lozenge, bounded by dextral NW trending faults (Crayfish Creek) and sinistral ENE faults (Postans). Lower mafic to upper felsic volcanics comprise several extrusive cycles in the Burchell and Greenwater assemblages underlying the belt.

The Archean units are represented by two oppositely facing assemblages (Burchell and Greenwater) and a younger third (Shebandowan), unconformably overlying the first two (a "Temiskaming" type assemblage). The younger Shebandowan suite comprises sedimentary and volcanic rocks, including units of alkalic affinity, that unconformably overlie, and locally straddle, the boundary between the Burchell and Greenwater assemblages.

Classic mafic to felsic cyclic volcanism characterize both the Burchell and Greenwater assemblages. Three, basal mafic through to upper felsic, cycles have been mapped in these assemblages. The Greenwater, facing south, generally south of Shebandowan Lake; the Burchell facing north, north of the lake. The Shebandowan Lake Pluton has been*intruded into the lower portion of basal Cycle l of the Burchell assemblage.

Landore's Shebandowan property straddles the contact between the Shebandowan Lake pluton, and Burchell Cycles l and 2. The top of Cycle l is characterized by felsic tuffs exposed immediately north of their contact with the pluton which underlies the lake. A sulfide-bearing heterolithic breccia marks the hiatus between the felsics of Cycle l and the predominantly mafic base of Cycle 2. This unit can be traced 5km along strike in the southern portion of the Landore property.

J _^ ^ QUETICO FAULT'"" ""~~~~~—-

^Shebandowan Lake Pluton (Tonalite)

WABIGOONSUBPROVINCE

QUETICO SUBPROVINCE

——— SUBPROVINCE —— MAJOR FAULTfm PROTEROZOIC COVER

SHEBANDOWAN GREENSTONE BELT SUNBAR-BATWING LAKES COMPLEX

Quartzita Mma . Au Occurrence

———— geological contact——— unconlormity^— — major fault

•' MINE (past producer)A gold occurrence

GRANITE. SYENITE. MONZONITE, DIORITE. Some pluton* complex, and some Include malic to ultramafic phasesMassive to foliated, undilferentialed QUARTZ DIORITE. TRONDHJEMITE. GRANODIORITE. GRANITE and GNEISS. Light lines indicate foliation traces.

Mainly volcanic and sedimentary rocksPROTEROZOIC SEDIMENTARY and INTRUSIVE ROCKS

•TIMISKAMING-TYPE* VOLCANIC and SEDIMENTARY ROCKS

'OLDER* METAVOLCANIC ROCKS and METADIABASE - - FELSIC QUETICO METAGREYWACKES pass gradationally into migmatite and then granite

Generalized geological map of the western part of the Shebandowan Greenstone Belt. General tectonic setting shown In Inset.

DEFORMATION

Early deformation (DI) throughout the subprovince produced sinistral ENE faults parallel to the Postans and Quetico Faults, due to NW/SE directed shortening. Continued deformation developed a second set of, this time, dextral faults trending NW, parallel to the Crayfish Creek Fault, and displacing the first set. The Burchell and Greenwater assemblages were juxtaposed and the Shebandowan Lake pluton were intruded at this time.

The Temiskaming-type assemblage was deposited on top of the first two assemblages in linear, probably rift-related, grabens. Deformation culminated (D2) with the folding of this latest assemblage along SE trending axes.

ALTERATION

Zones of intense ankerite-sericite alteration are closely associated with the early set of sinistral E/ENE faults. These, predominantly ductile, shear zones are particularly concentrated in an area NE of lower Shebandowan Lake, underlying Landore's property. The Shebandowan Lake pluton was affected by this early sinistral stage and may have acted as a competent "augen" within the the shear system; the deformed, east-projecting tail through lower Shebandowan Lake representing a tail or wing of the augen.

Significantly, the NE flank of the pluton may have been located in the pressure shadow of the augen during the sinistral regime (Chorlton, 1987) . Fluid-fl'ow was channeled into this area, being forced-out of areas more involved in deformation and crustal shortening. Resulting hydrothermal alteration is concentrated along the E/ENE ductile shears (the ankerite-sericite schist zones) cutting the volcanics of Cycles l and 2, and the northeastern periphery of the pluton. This area encompases 13km, from Pistol Lake in the west, to the eastern tip of Shebandowan Lake, and comprising the property under review.

Later dextral NW faults flexed and rotated the ankerite- sericite schist zones and developped brittle quartz-filled fractures within these altered zones. Chorlton (1987) concluded that most, if not all, gold mineralization in this immediate area is controlled by this later series of brittle, NW trending faults, cutting the somewhat older ENE ductile shears. Areas of intersection of NW with ENE shears may have been particularly permeable, structurally induced, conduits for gold mineralizing fluids.

PROPERTY GEOLOGY*

Most of the property is underlain by north facing and steeply north dipping mafic metavolcanics of Burchell Cycle 2. The extreme southern portion of the claim block is occupied by the Shebandowan Lake pluton. To the immediate north lies the top ofCycle l, represented by felsic to intermediate tuffs. A distinctive, sulfide-bearing heterolithic breccia marks the hiatus between the two cycles. This marker unit can be traced from the Bandore #4 zone westwards for 4km, all on Landore ground.

The Shebandowan Lake Pluton underlies most of this portion of middle Shebandowan Lake, and forms the base of the volcanic succession on the Landore property. The pluton is tonalitic (qtz-diorite) in composition, coarse grained and equigranular. Small, partly digested volcanic xenoliths are locally present.

The eastern and northeastern contacts of the pluton are affected by both ductile and brittle E-W structures. These are accompanied by intense carbonatization and local sulfide mineralization, including pyrite, arsenopyrite and molybdenite. Even outside these altered zones, much of the northeastern portion of the pluton is affected by some degree of sericitization and carbonatization.

Cycle l felsics are found in a thin (Om-500m) discontinuous band along the north shore of Lake Shebandowan, on the northern contact of the pluton. The heterolithic marker directly overlies the felsics, and has been traced 4km along strike, from Blizzard Bay to Rossmere Bay, Shebandowan Lake.

The Marker is typically 100m thick and contains large fragments and blocks of massive pyrite, highly sericitized basalt, siliceous rock and unaltered basalt, in a sericitic and pyrite-rich matrix. Its eastern extremity was drill-intersected by Mattagami and Noranda, and found to contain graphitic interbeds. The first exposures to the west occur on claim #557151 of the Landore property. Here, the breccia consists of 20cm blocks of massive pyrite (with minor pyrrhotite), and rhyolite; a 10m wide, EW shear zone in the breccia hosts feldspar porphyry and lenticular quartz veins. Five trenches and a pit attest to previous exploration work, probably by Ourgold Mining.

Cycle 2 volcanics are characterized by mafic to intermediate flows and sills, and comprise the northern 2/3 of the property. Pillowed flows face steeply north; minor tuff and lapilli tuff form interflow units.

Plagioclase, and locally quartz-phyric, felsic dykes; metadiabase; gabbro and minor lamprophyre intrude the mafics of Cycle 2. Orientation is generally E-W, with steep dips to the north. Gabbro comprises the bulk of the intrusives. Quartz veining is common in most of the gabbro outcrops. In places large blocks of andesite are found rafted into the gabbro near the contacts.

MINERALIZATION

Gold mineralization is extensive on the property under consideration. Numerous carbonate-sericite shear zones occur in all lithological types. 1,400,000. tons have previously been drill- indicated on the eastern boundary of the claims. Drilling on the Landore and adjoining property has traditionally followed the EW shears, without regard for controlling cross-structures.

Massive sulfide potential in the area has been almost completely ignored. The felsic volcanics at the top of Cycle l, and

the massive sulf ide-bearing heterolithic breccia marking the hiatus between cycles, offer unique and significant potential for hosting volcanogenic massive sulfide deposits.

GOLD MINERALIZATION

Analyses of ankerite-sericite schist zones have returned generally background gold values ^lOppb) except in areas of quartz(-carbonate) veining and pyritization. Structural considerations (Chorlton, 1987) indicate that veining occurred during a late, brittle stage, after development of sinistral ductile shears hosting ankerite-sericite alteration zones. High gold values come, for the most part, from the quartz(-carbonate)- pyrite(-chalcopyrite) vein association that is hosted by, or traverses, the schist zones.

PISTOL LAKE

The property is underlain by Cycle 2 mafic volcanics of the Burchell assemblage. These are intruded by the Pistol Lake trondhjemite stock, feldspar porphyry dykes, quartz-syenite (latite) dykes and minor lamprophyres.

All of the Pistol Lake stock has been affected by pervasive sericite-ankerite-albite alteration. This alteration episode was an early one, unrelated to the east-trending, heavilly altered, ductile shear zones elsewhere on the property. Gold values are associated with quartz(-carbonate)-sulfide veinlets; areas of pervasive alteration, without veining, carry background values.

The southern margin of the Pistol Lake stock is overprinted by a strong sericite-ankerite schist zone; gold is associated with late stage quartz-sulfide veining. Previous operators have confirmed mineralization along a 750m E-W strike and down to 180m depth within the shear and adjacent footwall volcanics.

BANDORE #1

Mafic volcanics at the base of Burchell assemblage Cycle 2 are intruded by east-trending diabase and feldspar porphyry dykes. The porphyry is in fault contact with the diabase and gold mineralization occurs along this ankerite-sericite schist zone. The schist zone terminates with the feldspar porphyry to the east; in the west it is dextrally offset about 1km onto Landore's property, along a NW trending fault.

The main showing occurs in a steeply north-dipping E/ENE sericite-ankerite schist zone hosting narrow (cm-scale) quartz- pyrite veinlets. Two foliation parallel mineralized zones 0.5m apart, comprise highly deformed veins and seams containing pyrite- sphalerite-chalcopyrite. Structural analysis shows the veins to have been produced by a dextral deformation regime; minor dextral offsets along a NE direction are in evidence cutting the veinlets

and schistosity.

BANDORE #4

Gold mineralization is localized in an extensive (500m) E-W ductile shear zone, hosted within felsic tuffs at the top of Cycle l of the Burchell assemblage. A steeply south-dipping heterolithic breccia forms the immediate northern footwall and represents a massive sulfide bearing pyroclastic episode culminating Cycle l activity.

The east trending shear zone has affected felsic ash to lapilli tuffs and altered them to ankerite-sericite-chlorite schists. Gold mineralization is closely associated with quartz veining and flooding containing pyrite, and to pyritized wall-rock. Most veining is brittle fracture related, and does not appear to be multiple-injection/crack and seal type.

Two E-W, foliation parallel mineralized zone, Im-lOm wide have been interpreted by previous operators: an upper, quartz-vein related zone (184,820 tons @ 0.12 opt Au) and a lower, more quartz- flooded, silicified, pyritized zone (465,240 tons @ 0.15 opt Au). Both dip at approximately 70 0 -80 0 N, and are truncated or terminate, at the 80" south dipping pyroclastic breccia contact.

The plan projection of the zones clearly shows an ENE trending, right-stepping en echelon pattern within the confines of the known (ie. drilled) northern portion of the shear zone. The mineralized zones would then represent gash or extensional veins formed during a sinistral regime. North dipping zones suggest the north block has moved up relative to the south.

Landore's Shebandowan property now includes the western third of the Bandore #4, west of Mattagami Grid L42E.

*

CAL-CHRIS SHOWING

This occurrence is located 250m south of the Pistol Lake stock, localized within a zone of quartz veined shearing in host mafic flows. On surface, anomalous gold values occur over a strike length of 2 5m. Drilling by Lincoln Resources in 1986 intersected an altered schistose unit within the volcanics to the north of the Cal-Chris, perhaps showing that the structure is more shallow dipping than previously thought. This orientation is sub-parallel to the Pistol Lake structure; alteration consists of hematite and ankerite, with chlorite-muscovite schists, again suggesting strong similarity with the Pistol Lake environment. Anomalous, but sporadic gold values were intersected in the limited drilling: the showing is open in all directions. Its similarities with Pistol Lake indicates a good potential for significant gold mineralization along strike and at depth.

Northern Development and Mines

Ontario

Report ot Vw wrx After Recording Claim

Mining Acfl Jf9^c

Personal Information collected on this form Is obtained under the authority of the this collection should be directed to the Provincial Manager. Mining Lands. M Sudbury. Ontario. P3E 6A5. telephone (705) 670-7264.

52B09NE0091 W9540.00508 CONACHER900Instructions: - 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.

Work Performed (Check One Work Group Only)Work Group

Geotechnical Survey

Physical Work. Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

./f*o Type {/*4rKit*](Sr*tJtMj\ f

StftipipiiOA //^SjOcJ^ifV G

Total Assessment Work Claimed on the Attached Statement of Costs S .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

Af*** ^ '^^——/^v l T"*"f -*-^" *—————*-

l^B^ ftVjtffi/r-A

A

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sidel 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. ——^————————

Certification of Work Reportl certify that l 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

Bfr9 /c^~ynnFor Office Use Only CLfis

^*f—Total Value Gr. Recorded Date Recorded

Deemed Approval Date

Mining Recorder

Date Approved

•""^ ^^ ^ w fDate Notice for Amendments Sent

Received Stamp

Thunder B ayMining Division

SEP - ? 1QQR*"-' J 1330

RECEIVED0241 (03/91)

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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. D Credits are to be cut back starting with the claim listed last, working backwards.2. D Credits are to be cut back equally over all claims contained in this report of work.3. D 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

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t hoCredits you are claiming In this report may be cut back. In order to minimize the which claims you wish to priorize the deletion of credits. Please mark (^) one of1. D Credits are to be cut back starting with the claim listed last, working backw2. D Credits are to be cut back equally over all claims contained in this report of3. ID-Credits are to be cut back aaipriorlzed on the attached appendix.

elfled y

adverse effects of such deletions, please Indicate fromfollowing:

rds. work.

O In the event that you have not specified your choice of priority, option one will be Implemented.

tote 1: Examples of beneficial Interest are unrecorded transfers, option agreement to the mining claims.

tote 2: If work has been performed on patented or leased land, please complet

, memorandum of agreements, etc., with respect

the following:

l certify that the recorded holder had a beneficial Interest In the patented or leaned land at the lime the work was performed.

Signature Date

Ontario

Ministry ofNorthern Developmentand M ines

Ministere du Developpement du Nord et des mines

Statement of Costs for Assessment Credit

Etat des couts aux fins du credit devaluation

Mining Act/Loi sur les mines

Transaction No./N 0 de transaction

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, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presente formula sont recueillis en vertu de la Loi sur le* 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 miniers, 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 Salalras

Contractor's and Consultant's FeesDrolls de ('entrepreneur et de I'expert- consell

Supplies UsedFoumlturasutilities

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Type

1106

Loo

Amount Montant

/53V

Total Direct Costs Total des couts directs

Totals Total global

2. Indirect Costs/CoOts 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 devaluation.

Type

Transportation Transport

Food and Lodging Nourriture et hebergementMobilization and Demobilization Mobilisation et demobilisation

DescriptionAmount Montant

&9.

Totals Total global

Sub Total of Indirect Costs Total partlel des coOts indlrects

Amount Allowable (not greater than 20tt of Direct Costs) Montant admissible (n'excedant pas 20 H des coOts directs)Total Value of Assessment Credit (Total of Direct md Allowable Indirect costa)

Valeur totals du creditdevaluation(Total dw coOtt direct*at Indlracta adn

Note: 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 deoenses demandees dans le present etat des coOts dans les 30 jours suivant une demande a cet effet. Si la verification n'est pas effect uee, le ministre pout rejeter tout ou une partie des travaux d'evaluation presentes.

Filing Discounts Remises pour depot

1. Work filed within two years of completion is claimed at 10007o of the above Total Value of Assessment Credit.

1. Les travaux deposes dans les deux ans suivant leur achevement sont rembourses a 100 "to de la valeur totale susmentionnee du credit d'evaluation.

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

Total 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 "to de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.

Valeur totale du credit d'evaluationx 0,50

Evaluation totale demandee

Certification Verifying Statement of Costs Attestation de l'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.

that as(Recorded Holder, Agent, Position in Company)

to make this certification

J'attests par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont ete engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formula de rapport de travail ci-joint.

l am authorized Et qu'a titre de . je suis autorise(titulaire enregistre, representant, posts occup6 dans la compagnie)

a faire cette attestation.

0212(04/91) Nota : Dans cette formula, lorsqu'il designe des personnes, le masculin est utilise au i neutre.

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