42C03NW2004 2.20116 KEATING010

TECHNICAL REPORT OP-99-161

WRITTEN AND COMPILED BY: JAYSON GERDES

QPAP 1999

Introduction

The Abbie Lake Area Claim Group is centered 15 kilometers (9 miles) to the north of the Magnacon Mine and the Mishibishu Greenstone Belt. The claims are within the Kabemmg Lake Greenstone Belt, a sequence of Archean metavolcanics and metasediments, similar to the Mishibishu Belt Greenstones.

The property consists of seven block claims numbered as follows: SSM 1163876, SSM 1221639, SSM 1221640, SSM 1164220, staked in Mar/98. SSM 1164230, SSM 1164231, SSM 1164232 were staked in the Oct/98. The total property consists of sixty two units almost 1000 ha. in area.

I had previously staked five claims in this area in 1990. In 1991,1 applied for, and received grant # OP-91 - 298. Work consisted of sampling, and a ground VLF-EM survey. The results of this survey were very encouraging, and confirmed several questionable airborne conductors. I relocated a gold showing reported by Diawan Eng. Who was working on an adjoining property to the north in 1989. After 1990, activity declined in the area, hence the road fell into disrepair, and the property lapsed. I kept this area under close observation.

The regional deformation zones which cross these Archean metasediments and volcanic flows have recently been shown to host significant gold mineralization in the Mishibishu Belt. Two properties which have developed over the past fourteen years are: the Magnacon mine, 1.4 million tons @ 0.24 opt gold, in the northern Mishibishu Deformation Zone ( MDZ ) lineament, and River Gold Mines LTD property, 5 million tons @ 0.30 opt gold, in the southern Eagle River Deformation Zones ( ERDZ).

The gold mineralization in the Mishibishu Greenstone Belt is localized in zones of intense hydrothermal alteration and quartz veining, intermittently along the regional deformation zones. The trends of these zones are well defined. They are also more extensive than previously considered.

Geophysical and geochemical surveys combined with intense prospecting and geological mapping in the past years have produced a large number of new target areas. These targets are located along shear zones and are significantly influenced by cross fault structures.

The Abbie Lake Area Claim Group described in this report is north of the Mishibishu Lake Deformation Zone ( MLDZ), but is hosted by the second major Archean Greenstone Belt in the area. Current exploration in the belt is targeted at evaluating the known shear zones, and the discovery of further structural breaks.

Location. Access and Phvsiocranhv

The Property is found on NTS map 42c76, Mishibishu Lake, and is centred about the coordinates 48 degrees 14 min N and 85 degrees 20 min W.

The claims are located about 15 kilometers north northeast of the former (past producer) Magnacon Mine site in the Mishibishu Area of Northern Ontario. The bulk of the property lies in the unsurveyed township of (Abbie Lake Area), and immediately west of keating township. The property is in the Sault Ste Marie Mining district, and in the Timmins Res. Geologist Area.

To access the property by vehicle from Wawa, you would need to drive about 50 km (30 miles) North on Hwy 17 to the Paint Lake Road (North Country Lodge is located at this corner). Turn left onto this road and head west for 36 km, here you will pass under an Ontario Hydro power line, and take the next road on the right This is a power line and logging access road, drive for approx. 2 km, here the road splits and heads north away from the power line and is used just for logging, continue north for another 4 km, stay on the main road, you should be at the center of the property.

The terrain consists of moderate to steep rounded hills and ridges in the northern portion of the property. A lake and creek system traverse the central, to southern portion of the property.

Outcrop is generally very good on the northwestern and eastern edges as well as the northern boundary area. Much of the central to south central portion of the area is overlain by either creek swamp, cedar swamp or boulder till. The south eastern portion is also overlain by swamp and boulder till. Outcrop is nonexistent in cedar swamps and varies from poor to very good within areas of boulder till.

The property was forested predominantly with jack pine and spruce, with mixed forest in the northern portion. It has been clear cut recently, and has a network of roads throughout.

model of mineralization

There is considerable controversy as to the origin of the gold mineralization within the Archean Green stone Belts. The two models for the origin of gold either have the metal as an original constituent of the rocks (syngenetic) or as a later addition (epigenetic). In the Mishibishu camp the gold is associated with highly deformed rocks, ( generally now chlorite or sericite schists), with strong overprints of hydrothermal alteration.

These schists form long linear zones, in places, cross cut the Archean volcanic stratigraphy. Intermittently along these deformation zones, there is extensive development of quartz veining, silification, sericite/chlorite development, and pyrite, arsenopyrite, galena and chalcopyrite mineralization. The mineralization is within "vein shoots" which may be up to tens of meters wide, and hundreds of meters long and deep.

The vein style mineralization is best found from detailed prospecting along the recognized structural and topographic features, with particular attention to cross cutting structures. At the Magnacon Mine (past producer) the most significant widths of vein gold mineralization are at the junction of one of the major crosscutting diabase dykes and the MDZ. Such cross cutting structures require intensive exploration.

REGIONAL GEOLOGY

The Kabenung Lake Green stone Belt (KLGB)

The KLGB is the western extension of the northwest section of the Michipicoten Green Stone Belt and trends south west for 45 km from Kabenung Lake to the stoney creek area where it terminates in a zone of supracrustal assimilation. The belt ranges in width from 8 km just west of Kabenung Lake to 4 km's near it's western termination.

The Archean stratigraphy of the belt is defined by a 5600 m thick cycle sequence of metavolcanics and metasedimentary rocks. The basal sequence is dominated by a mafic to intermediate metavolcanic sequence of mainly massive and pillowed flows which have an estimated stratigraphic thickness of 3200 m. Felsic to intermediate metavolcanic rock sequences, up to 500 meters in thickness, occur within the mafic to intermediate volcanics. A metasedimentary sequence of greywacke slate and argillite up to 1300 m's in thickness, overlies the volcanic assemblage. Laterally continuous oxide facies chert - magnetite iron formation, ranging in thickness 60 to 360 m's, occurs within the finer to medium grained clastic rocks. Coarse clastic conglomerate meta sediments overlie the sand stones and chemical sediments. These conglomerates define a sequence up to 900 m's in thickness.

The supracrustal sequence is intruded by an Archean intermediate to felsic stock at Kabenung Lake. Granitic batholiths intrude the north and south margins of the belt. Numerous Proterozoic diabase dykes dissect the supracrustal and intrusive suites.

The major structural feature of the belt, the Iron Lake Syncline, is a gently plunging easterly trending syncline which is flanked by the Nichols Lake Anticline on the north, and an as yet unnamed anticline on the south.

Exploration within the belt has been historically on iron and base metals, and gold more recently. Gold mineralization has been reported at Iron Lake just to the south east of our property by Algoma Steel Corp. and by Corona, also in the Abbie Lake area, immediately southwest of our property by Tundra Gold Mines LTD. These zones of mineralization appear to be related to a strong deformation zone which passes south of our and the former lockwood property. Shear zones and associated carbonate and silica alteration on the former lockwood property indicated potential for similar gold mineralization. Pyrite, Pyrrhotite, chalcopyrite and sphalrite mineralization occurs within the Kabenung volcanic sequence, and silver mineralization is associated with copper and gold mineralization at the west end of the belt.

The Mishibishu Lake Greenstone Belt (MLGB)

The MLGB consists of Archean mafic dykes to felsic metavolcanics and chemical and clastic meta sediments cut by mafic dykes and sills. In some areas there are a very large number of late stage diabase dykes which cross cut the belt. These appear to be related to some late stage reconcentration of gold mineralization, eg. Magnacon. Granitic plutonic rocks and batholitic rocks bound and intrude the supracrustal sequence.

The MLGB is divided into two distinct bands, separated by a central pluton and the Bowman Lake batholith. The northern belt contains a higher proportion of sedimentary rocks, and the southern part contains more mafic volcanic rocks. Iron formations are hosted within both zones.

At the western end of the belt the metavolcanic sequence is dominated by the Kink Lake Anticline, a broad northwest plunging structure. Within this structure there is a strong northwest striking axial plane foliation, which appears parallel, or at a low angle to bedding. Superimposed on this broad structure there is also a moderate east-west penetrative foliation. These foliation's appear to be related to the regional folding of the supracrustal, and it postulated to be related to the emplacement of the granitoids of the northern batholithic complex.

Three strata parallel, east trending deformation zones cross the MLGB. Two of these zones are recognized in the northern part of the belt The Mishibishu Deformation Zone (MDZ) is a

prominent trend across the north side of Mishibishu Lake. The Rook Lake Deformation Zone (RLDZ) is sub parallel to the MDZ, and is located south of Mishibishu Lake. The third zone of crustal deformation, the Eagle River Deformation Zone (ERDZ), lies along the south side of the central pluton. This zone trends westerly, with a postulated extension through the Kink Lake Anticline.

At the present time there is intense exploration in the KLGB, MLGB, ERDZ by companies such as River Gold Mines LTD., Murgor Res., Noront Res., Free west Res.

Battle Mm. Mines from Hemlo have acquired ground from Wagner Forest Products LTD. (former ACR township) and have tied onto the eastern boundary line of our property. This exploration is concentrated along the deformation zones, which locally host hydrothermal alteration with gold, silver, arsenic, moly, tungsten, lead, zinc and copper mineralitzation. The economic mineralization is generally hosted in sulphide rich quartz veins, within chlorite/ sericite schist.

PROPERTY GEOLOGY

The property is underlain by mafic to intermediate volcanic, and felsic units. These are steeply (almost vertical) dipping to the north and north west, trending from almost east-west on the western edge of the property, to northeast on the eastern edge.

Numerous dykes crosscut the volcanic stratigraphy. Preferred orientations seem to be semi parallel to the volcanic bedding and northwest to southeast trends, though some other orientations were also observed. Dykes are observed to be diabasic, gabroic, and dioritic. Plagioclase porphyry dykes were also observed.

Other dyke units were observed to have undergone some metamorphism and are thought to be synvolcanic in origin

Felsic quartz porphyry and quartz feldspar porphyry intrusives, (and possibly related quartz eye pophyry) intrude the volcanic pile. Commonly clear and blue quartz eyes were observed. Most field evidence suggests these units trend parallel to the volcanic bedding. An exception to this may occur in the western portion of the property. Many of the pronounced shears observed occur within these felsic intrusives.

Numerous volcanic units were observed. These include massive volcanic flows, highly deformed pillows, feldspar porphyry, plagioclase porphyry, gabro, schists, tuffs and crystal tuff beds. Garnets were also observed during the visit by Ann Wilson.

OP-99-161 TECHNICAL REPORT

EQUIPMENT USED:

Belnor Contracting was used for the mechanical overburden stripping throughout this project using a Case 170B back hoe excavator. A Wajax Mk HI high pressure pump was used for washing outcrop. A gasoline powered rock saw with a diamond blade provided by Echo Bay Mines was used for taking the channel samples.

PROSPECT "A"

A total of 30.5 hours was spent with the back hoe at this location in Aug.799 building a crude access road,and opening an area of approx. 50m x 20m. and 10m x 10m Exposing two separate structures. This area is located in the central portion of claim SSM 1221640 between two muskeg swamps

Structure # l (NAMED THE NOVAK SHEAR) is a large intensely sheared zone striking East- West and dipping approx. 30 degrees to the north on the western termination where it is lost in muskeg swamp, to near vertical at the eastern termination near a creek. This structure is 2 meters wide in the middle of the exposure swelling to 3+ meters on both ends. Due to the unaltered host rock it appears this could be fracture or fault filling. The shear material is composed of decomposed serisite schist at the foot wall which resembles clay, containing <l% sulphides, with abundant green malachite staining. Also an unidentified copper tone coloured mineral. A distinct chevron fold pattern is noted. Within this shear are quarts lenses of varying sizes the most significant is approx. 2m x 1m, within this lens are fragments of sheared material and up to 5*^ sulphides.also noted are small pockets or lenses of massive sulphides. Six channel samples where taken from this showing,sample# OP-100 to 105

Structure # 2 ( NAMED THE SPIDER ZONE) is approx. 100m south south east of # l structure located right on the swamp edge, a large outcrop rises to the west, geology here is very complex, and it appears to be near the contact of a diorite intrusion and porphyritic rocks, containing numerous grey coloured quartz veins of various orientations and widths, large clots of chalco. pyrite, with malachite staining are noted throughout. These quartz veins are also believed to be fracture filling. The strike and dip are not clear at this occurrence, but due to the alteration it is believed to be east- west. Gold assays in 8 initial grab samples where low but anomalous sample # OP-1 to 8. the assays returned a significant amount of silver and copper mineralization. See the attached assay certificates for the values. No channel samples where taken at this location due to the complex nature of this occurrence. Approx. lOOOcu meters of material was moved at these two locations.

SIGNIFICANT RESULTS FROM PROSPECT "A":

Gold...... Grab......163 ppbSilver... Grabs.. 22. l g/t - 41.4 g/tCopper.. Three Grab samples > G.32%, 1.2Q0/*, 1.900xb.Channel samples... no significant results

CHANGES TO PROPOSAL:

No grid extension and no geophysics or geological mapping Previous grid from OP-91-298 and GPS were used for control

Representatives of the following companies visited this showing to evaluate it's geological significance, and the possibility of an option agreement:

Richard Nemis..... President of Noront Res Ltd.Abe Ablins........... vp explorations, Noront Res Ltd.John Harvey......... President Prospectors Alliance

and geological consultant for Noront Res Ltd. Al Smith............... Sr. Project Geologist, Noranda Inc.Mike Savell.......... Geologist, Noranda Inc.Don Hoy................Geologist, Freewest Res.Wayne Reid........... Geologist, Se Pres. of exploration Echo Bay MinesBruce Durham.......Geologist, Band-Ore Res.Bob Duess........... Geologist, vp exploration Band-Ore Res.Charley Hartley.... Geologist, River Gold MinesRock Lefrancois.... Geologist, Director of exploration Aur Res.Mike Purkins........ Geologist, Patricia Gold Mines

PROSPECT "B"

This is the most important area on the property to date, as a significant new discovery has been made at this location, made possible by the funds provided by this OPAP grant. This area has been named the ( MAIN SHEAR)

Due to the encouraging assay results from previous prospecting along this structure, most of the work for this grant is focused here.

Once again Belnor Contracting was used for the mechanized stripping. A Wajax Mklll pump, and a gas powered rock saw provided by Echo Bay Mines.

A total of 40 hrs of mechanized overburden stripping was done at this location in Aug.799, opening an area 206 meters along strike and of variable widths. Exposing a complex quartz carbonate ladder vein system averaging 0.6 meters wide beside a highly compressed porpyritic quartz eye system averaging 2 meters wide, within a tuffatious shear zone, the size of this shear is not clear. The sulphide content ranges from massive clots to finely disseminated. The quartz carbonate ladder vein structures are strongly boudinaged. The dip of these systems are near vertical to slightly north, and the strike is approx. 90 degrees. Gold mineralized serisite schist alteration has been found within the shear along the foot wall contact of the ladder vein system and extending south for up to 19 meters. Also serisite alteration has been found approx. 20 meters to the north of this structure, within a felsic shear zone containing visible gold. A total of 60 channel samples were collected along this structure, as well as numerous grab samples by no less than 10 mining & exploration companies who have visited the property since the beginning of Sept/99 until the end of Oct/99. The mechanized stripping was stopped at the western termination near line 4E because of increased overburden depth, and at the eastern termination because of a creek system and muskeg swamp. All assay results at my disposal are attached as well as digitized photos. A box grid was cut on the eastern portion of claims SSM 1163876 and SSM 1221639 and cut cross lines at 100m spacing 25 m stations over the stripped area for control. Compass, hip chain and OPS were used for prospecting and mapping traverses. Dr Derek McBride Ph.D. Geol. was permitted access to the property, in particular, this stripped area for geological mapping on a regional scale, he was representing Noront Res Ltd. all I have received from him to date is a basic geological map of the stripped area which is included with this report.

SIGNIFICANT RESULTS FROM PROSPECT "B"

Gold...Channel samplesSample # OP-207 a at 213.82 g/t over 0.60 meters(visible)..OP-207 b 5.21g7t over 1.1 meters, also a grab sample of 95g7t taken by Aur Res here

OP-64 at Jg/t over 1.34 meters,OP-69 at 31 g/t over 0.50 meters,OP-74 at 24g7t over 1.00 meters,OP-77a at 4.6 g/t over 1.00 metersOP-87 at 1.6 g/t over 0.90 meters also a grab sample of 27gft also taken by Aur Res.OP-91 at 1.4 g/t over 1.50 meters

CHANGES TO PROPOSAL

No geophysics,

Representatives of the following companies visited this showing to evaluate it's geological significance, and the possibility of an option agreement:

Richard Nemis..... President of Noront Res Ltd.Abe Ablins........... vp explorations, Noront Res Ltd.John Harvey......... President Prospectors Alliance

and geological consultant for Noront Res Ltd. Al Smith............... Sr. Project Geologist, Noranda Inc.Mike Savell.......... Geologist, Noranda Inc.Don Hoy................ Geologist, Free west Res.Wayne Reid........... Geologist, 8c Pres. of exploration Echo Bay MinesBruce Durham.......Geologist, Band-Ore Res.Bob Duess........... Geologist, vp exploration Band-Ore Res.Charley Hartley.... Geologist, River Gold MinesRock Lefrancois....Geologist, Director of exploration Aur Res.Mike Purkins........ Geologist, Patricia Gold Mines

A total 20.5 hours of back hoe time was used digging several test pits along strike in an attempt to locate further extensions of this structure. Ladder vein material,(as float) was exposed approx. 75 m further to the west as well as shearing and carbonate iron formation. An area of interest was stripped further west along strike and 200 m south of the main shear beside the main road (see map) Another anomalous quartz carbonate ladder vein structure approx. 0.60 m wide was channel sampled. This structure is hosted within a mafic volcanic unit cut by a north-west trending diabase dyke. Unfortunately the back hoe threw a track here and the stripping program came to an end. Assays returned anomalous goldNo significant results were obtained here.

AREAS "C" "D" "E" (fe "F" Were not extensively investigated because there was not enough time.

Recommendations and additional work

1. Detailed follow-up prospecting, sampling, geological mapping is required over the entire property

2. Surface stripping with heavy equipment and high pressure water is recommended for detailed evaluation of these shear zones.

3. Sample collection should be made by channel sampling, using a gasoline powered rock saw with diamond blades, where feasible.

4. Blast trenching where needed.

5. approx. 50 km of additional grid lines, both cut and compass and flagging, using 100m line spacing and 25m stations, for control.

6. whole rock analysis for mineral depletion or enrichment of key elements, as indicated by the base metal results thus far. Approx. (25-50)

7. Diamond drill sampling of the main shear and a IP survey over this structure

SUMMARY

The regional deformation zones which cross these Archean metasediments and volcanic flows have been shown to host significant gold mineralization in the Mishibishu Belt. Two properties that have developed over the past fourteen years are the Magnacon Mine 1.4 million tons @ 0.24 oz/t-This is located in the northern Mishibishu Lake Deformation Zone. The second is River Gold Mines 5 million tons @ 0.40 oz/t. Located in the Eagle River Deformation Zone.

Our claims are within the Kabenung Lake Greenstone Belt, and in close proximity to the Iron Lake Deformation Zone, a sequence of Archean metasediments and metavolcanics, similar to the Mishibishu Lake Green stones just 15 km to the south.

Qualifications

I have been a prospector for fourteen years. I started working for a consultant in Wawa, Seymour Sears from 1985 until 1990 as a subcontractor. I then provided contract exploration services in the Wawa area until 1998,1 have done all types of work from grass roots to advanced exploratioa From staking, line cutting, geophysics, traditional prospecting, blast trenching, overburden stripping, geochem sampling of all types, project management and supervisory positions, diamond drilling, and have completed four preveous OPAP grants. References: Ann Wilson, Timmins. Seymour Sears, Wawa. Roy Rupert, Sudbury.

CONCLUSIONS

1. The Kabenung Lake Belt claim group is within a zone of deformed Archean greenstones. This belt is similar in geology to the Mishibishu Lake Greenstone Belt only 15 km south.

2. In the Mishibishu Lake Greenstone Belt regional shear zones have been shown to host significant gold mineralization. Shear zones south of the former lockwood property within the Kabenung Lake Greenstone Belt show similar gold mineralization.

3. A major east-west to west southwest conductor axis, that runs though the middle of the property, among numerous smaller ones, contain several shear zones of substantial width, with cross cutting quartz veins. The shears contain significant pyrite sometimes massive. The mafic metavolcanics have been converted to quartz l chlorite carbonate schists in the shears.

4. Anomalous gold values were found inplace in at least six programs of sampling two of which are independent individuals or companies visiting the property. Also two significant assays of 13.2g7t and 0.44 oz/t were obtained.

5. The large shear hosted anomalous quartz/carbonate veins found on the property have extensive pyrite mineralization and sericite alteration, this indicates a gold mineralizing environment.

6. The geophysical survey on the property although not complete indicate possible western conductors and this would indicate several targets for continued exploration.

7. The felsic volcanics are of the right age and size to host a significant base metal deposit.

8. The molybdenite associated with the values from showing "B" are similar to the Hemlo deposit

9. The property shows some similarity to the Hemlo deposit as indicated on the vertical magnetic gradient and total magnetic field gradient shaded image maps 2590-2586 of Ontario.

10. Three major types of mineralized quartz veins have been observed on the property(a) strongly boudinaged veins within the schists and porphyritic shear zones, (b) crosscutting quartz stringers and veins, (c) late stage fracture filling veins.

11. We believe that the two DDH that Noranda put down are located in the southeast corner of the property.

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— J . GERDES S ASSOC. POLYMETALIC MINERAL PROP. 7 BLOCK CLAIMS TOTAL 62 UNITS, 1000 HA.

AREA "A" STRIPPING & CHANNEL SAMPLE

LOCATIONS BASIC GEOLOGY

OF THE NOVAK SHEAR

F

GRAB SAMPLEASSAYS

TAKEN BY NORANDA AREA "A" AND "B"

M Nonnda Inc.

874 Tunptcn Strut Thunder Bay. Ontario, Canada P7B 6)3

. Te) (807)623-4339noranda f** (807)623-0452

November 16,1999

Mr. Jayson Gerties 42 Tamarak Ave. P.O. Box 1991 Wawa, Ontario POS1KO

Dear Mr. Gerdes:

Subject: Abbie Lake Property

Please find attached descriptions and analyses of samples that Mike Savelt and l collected during our visit to your property on October 15th of this year, l have divided the samples into those collected for multi-element (32 element ICP) analyses and those collected tor whole rock analyses.

Despite the interesting polymetallic mineralization you have discovered to date on this property, we are not able to consider an option at this time. As mentioned at the conclusion of the property examination, your property represents a grass-roots gold situation on which considerably more work may successfully yield economic gold mineralization. Unfortunately, significant base metal targets are not apparent on the property at this time.

We thank you for having given us the opportunity to visit your property, and wish you the best of success with it in the future. Should you uncover additional base metal (Zn, Cu) mineralization during your continued work and you are still interested hi vending the ground, please do not hesitate to call me or Mike Savell.

Yours truly,

ilnc.

Sr. ProjecfcGeologist Western Canada Region

AS

c.c. File

A9928313 - CERTIFIEDCLIENT : "NORANDA MINING AND EXPLORATION INC.# of SAMPLES: 20DATE RECEIVED : 08-SEP-1999PROJECT: "1700CERTIFICATE COMMENTS : "ATTN:MICHAEL SAVELL"

: B* PLEASE NOTE * INTERFERENCE: Cu ON Bi A P. "983 2118 2119 2120 557 2121

SAMPLE Au Ag Al As B Ba DESCRIPTION ppb ppm 07o ppm ppm ppm

176451 -e5 0.2 2.01 ^ ^0 130176452 ^ 0.6 2 ^ ^0 60176453 <5 1.2 6.7 ^ <10 60176454 290 0.6 0.55 48 *:10 10176455 20 0.2 0.82 14 *c10 20176456 ^ 0.2 1.3 ^ <10 30176457 ^ O.2 0.77 ^ <10 10176458 <5 0.6 1.3 ^ <10 20176459 910 8.8 0.48 230 *:10 40176460 360 8.8 2.58 40 ^0 10176461 620 3 0.13 202 *:10 10176462 ^ O.2 0.54 ^ <10 10176463 <5 O.2 0.22 14 <10 20176464 150 1.2 1.77 18 ^0 10176466 435 10.4 1.77 98 -dO 40176467 580 17.2 2.12 38 *:10 30176468 25 1.6 2.17 ^ ^0 10176469 1860 7 1.69 56 -c10 40176470 600 0.6 1.45 30 *:10 50176471 280 41.4 0.7 ^ *:10

2122Be

ppm0.5<0.50.5O.5O.5O.5O.5O.5<0.5<0.5O.5O.5O.5<0.5O.5<0.5<0.5O.5O.5O.5

2123Bi

ppm^<2<242^<24

28^<2<2<2<2^<2<2<2<2

Intf*

2124Ca"/o

0.120.494.476.952.672.773.651.220.073.255.570.1411.85.470.091.950.930.070.2

0.82

2125Cd

ppm0.5O.5O.5O.5O.5O.50.5O.50.54.513

13.5

21.552.546

64.544189

2126Co

ppm15244317171076

27154107142152

221121411095861

2127Cr

ppm1462061401221351198511561109123252537359365864126259

2128Cu

ppm47115341144185168105195703

28107004317

325318047704961875152

MOOOO

2150Feo/o

3.653.224.525.282.091.891.261.91

> 15.0010.156.874.147.649.48

^5.00M5.00H 5.00H5.0012.754.82

2130 2131 2132 2151 2134 2135 2136 2137Ga Hg K La

ppm ppm Vo ppm•*1 1.28 10•d 0.89 10

20 ^ 0.05 20•d 0.11•d 0.21•s1 0.28•d 0.22<1 0.21•d 0.06<1 0.07•s! 0.03<1 0.01<1 0.05•d 0.05<1 0.03•d 0.03

1 0.02<1 0.08•si 0.09<1 0.03

Mg"/o

1.371

0.160.220.380.610.360.810.081.681.820.184.032.080.480.9

0.810.330.570.35

Mnppm3953652351305470500445415793040908430542094408230

> 10000> 10000> 10000M 0000> 10000

710

Moppm102012223

•^11

*:11413

•^111^•si

12

Na"/o

0.060.070.41O.010.010.010.010.010.01O.01O.01O.010.01O.01O.01O.010.010.030.04O.01

2138Ni

ppm54881161315181213

12598153231943494027385355

2139P

ppm26046076013020027023025019015022019060170120320160360530intr

2140Pb

ppm24^^22^^^32^32^^2^^^6^^

551S07o

0.721.2

2.490.660.850.110.090.074.051.321.190.050.111.151.981.671.174.51.3

2.72

2141Sb

ppm^^^2^^2^^2^<22<2<2^6<2<2<2

2142Se

ppm1010

1212^*:17125837577783

2143Sr

ppm1620

3292824212411132236106931918157

107

2144 Ti"/o

0.220.140.2

O.01 O.01 O.01 O.01

O.01

O.01 O.01

O.01 •*:0.01 ^.01 <0.01

2145 2146 2147 2148 2149Tl U V W Zn

ppm ppm ppm ppm ppm90 ^0 26684 ^0 11030 ^0 127 ^0 89 -^10 2218 i10 225 *:10 169 ^0 24

42 -s10 354105 ^0 97222 "^10 231017 ^0 23411 -:10 78655 <10 484041 10 HOOOO47 <10 MOOOO67 <10 >1000050 -^10 >1000044 <10 410024 ^0 476

GRAB SAMPLEASSAYS

TAKEN BY NORONT RES. AREA "A" AND "B"

XRAL XRAL laboratoriesA Olvlf Ion *f SGS Cifuri* {ne.

Oci Mill*. OnlBrio C9't?Cte M39 3J4 Ttlepher*(418)445 STSS

Jfty.

From/De:

Date:

Ceplw

Bonnie White

September 24.1993

To/A: John Harvey De vex344-2777

Results for Work Order 056848

FAX TRANSMITTANCE l TRANSMISSION DE FAX

Sample *

REN-01 REN^OZ REN-03 REN-04 REN-05 REN-06 REN-07 REN-06 REN-D9 REW-10 REN-11 REN-12 REN-13 REN-14 REN-15 REN-16

REN-01 DupREN 13 Dup

: fIS CeRTPIED TO tSO9002

Au Results

4401122933S26203871064^80-

1410325839

43210

Mtmbtr of the SOt Oroup (SocUt* C*n*r*l* rf* SurvtWanct)

TOTAL P. 01

aL

XRAL XRAL UborjtorfesA DJvislon of SOS Can*d* lie.

Wot* Order: 056848 Date 29AW99

Method,Ddr.Ltm.Uutl*.

0102 OJ0405

06070809JO

l!n13*415

16 'DupOl•Dm 13

Cft ICPWl

ppm

10* 35 381821

1837577756

1018441357

1110145

mJCP7*

l

3043353029

M 68 61

14045

13254513

107

142945

CPICPW

0.5ppm695

37.366002160

118289237

48.7107

73.646.73020

160676488

125 70S 356

ZnICP70

0.5ppm

904084.4129

305027.614.0

50402660

429508012,7 5U93.618.2

26208.9sm

89.3

PARTIAJL

As CJ70ppmc3C3c3C3C313ea

C334217

c3C 3C3

59

C3C3

SeICP70

ftJppm27.632.914.95.3

26.87.05.47.6

74.53,2106

20.43.4

17.011.487.026.033

Y K3P70

0.5ppm7.66,54.11.85. B1.81,5I.*4.54.9

17.410.710.02.01.3

18.97,59.8

Zr 1CPW

04!ppBB

13.54.51.59.75.72.19,27.5

12,913,32,0

13.17.12,44.0

2.614.47.2

M* fCWO

Ippm< JciCI

2Ci

2-ci4CIcicic;ciC]

2CI

cictci

ICP780.1

ppm1.1

cO.2J0.34.4

C0.2

1,50.90.42.20.8

C 0.20.7

C0.22.01.1

0.31.10.3

tog*? of

Cd 1CP79i

pjun41ci

36ci

^1595

20

CiCiciCI10

CI42

Ci

3

SnICPW

10ppmc 10CIOCIOCIOCIO

00CIOcioCIOCIO

CIOCIOc 10CIOc 10*CiOCIOCIO

Sb ICWO

5ppmC5CSeaC5cSC5c5C5C5cSC5C5C5C5CS

C5C5C5

Ba ICP70

1PpOT

40to7

121563

253

135

1827

7li

54226

iS

SFG

MmnUr rfM SOS Onuy v'SeoWt O*** c* Jtarwftwn)

XRALWork Order:

Elcmnf. Melted. JDrCJUbi. Uail*.

0102 Q)0405

05m0809

1112131415

16•up ci

14.2 2.1 1.9

7.44.0

14.0

CIO•SJO

K10 CIO

CIO c W

<^o

XRALA OMifon ol SOflr CtMda IAO,

056848 Dater 29/09/99

l* W fbICP70 JCP70 IOP7B

•-S tO 2Ppm ppm5,96.91.82.7

113

S.I 2.8 2,7 3,2

tt

37244

ft 12

B 39 12

423

5345

PARTIAL

ttKF70

5ppm

*1NP

rv

43 ^ ^

^*INPc570O

^<5 <5

lcH

li VW***f DwtM GnuutfoaiM CMntalidt SVIWWWIM^ T} o

DETAIL OF STRIPPED AREA "B" MAIN SHEAR

CHANNEL SAMPLE LOCATIONS, WIDTH AND

ASSAY RESULTS

MINERAL PROPERTY OF J.GERDES A ASSOC. CHANNEL SAMPLE NUMBERS & WIDTH IN METERS.

QUARTZ CARB LADDER VEIN SYSTEM- MAIN SHEAROP-50-1.35OP-51-1.30OP-52-l.00OP-53-1.00OP-54-1.00OP-55-1.00OP-56-1.00OP-57-1.00OP-58-1.00OP- 59 - UNKNOWNOP-60-1.00OP-61-1.00OP- 62 - 0.90OP-63-1.00OP-64- 1.34OP-65-1.00OP-66-1.00OP- 67 - 0.70OP-68- 1.30OP- 69 - 0.50OP- 70 - 0.80OP- 71 - 0.90OP-72-1.37OP-73-1.08OP-74-1.00OP-75-1.40OP-76-1.00OP-77A-1.00OP-77B-0.40OP-78-1.60OP-79-1.10OP-80-1.20OP- 81 .1.83OP- 82 -1.40OP-83-1.60OP- 84 - 2.00OP-85-0.50OP- 86 - 0.50OP-87-0.90OP-88-1.04

OP-89-1.30OP- 90 - 0.20OP-91-1.50OP- 92 - 0.70*assay not doneOP- 93 - 1.00*assay not doneOP- 94 -1.00*assay not doneOP-95-0.80OP-95-1.20OP-96-1.00OP-97-1.00OP-98-1.00OP-99-NO SAMPLE

NOVAK SHEAROP-100-1.90OP-102-0.80OP-103-0.90OP-104-0.80OP-105-1.00SERISITE SCHIST V-G ZONE LOCATED AT APPROX. 15mw of 12+25S L-5+OOEOP-110-1.00OP-111-1.00OP-112-1.00OP-113-0.50OP-114-1.90OP-115-2.80OP-116-2.00WESTERN EXTENTIONS 500 & 1000M ON STRIKE500MOP-201-0.80OP- 202- 0.70OP- 203- 0.601000MOP- 204- 0.96OP-205-0.50OP-206-1.00

SERISITE SCHIST V-G ZONE LOCATED AT APPROX. l Omw of 12+25S LINE 5+OOEOP- 207A-0.60OP-207B-UOOPr208 -1.80OP-209 -1.20

Ocrt-25-99 O3:19P Dell p

70? -

TITLE 25-10-99 14:44:37 T99-57415.0 W. REID 20/10/99CUENT ECHO BAY MINESPROJECT GENEX fSAMPLES: 66SPECIAL VALUESIS Insufficient Sample•9 No Value Recorded

Values above the upper Hmtt are shown os *uplimtValues beta* the lower-limit are shown as -tofent (ie not detected)

DETERMINATIONSELNAME METHO ECO UNI *SAM LOLMT UPUMT COMMENTS

01AU30 FA-30EH3PPB 86 5 999908 Results Reported02 Cu AA EA1PPM 66 1 20000 Test not yet complete03 Zn AA EA1PPM 66 1 20000 Test not yet complete04 Ag AA EA1PPM 66 0.1 50.0 Test not yet complete

SAMPLE PREPS40 SAMPLE TYPE^R ROCK41 PA4* 66 CRUSH, SPLIT42 PAS* 66 PULVERIZATION

REMARKS50 V:SAMPLES OP-78 AND OP-77A ARE ERRATICS. "51 FOR SAMPLE OP-76. WE HAVE OBTAIN 942 PPB52 AND 2090 PPB. FOR SAMPLE OP-77A, WE HAVE53 OBTAIN 464 PPB, 1360 PPB AND t252 PPB.

FORMAT {1JCA8.3XAI ,3XAI ,3X,A20,1X,4(1X,A7,2X^1 (1X))BEGIN Type Free Sample ID Au30 Cu Zn74150001 OP-50 115 -9 -974150002 OP-51 7 -9 -974150003 OP-52 55 -9 -974150004 OP-53 66 -9 -974150005 OP-54 -5 -9 -974150006 OP-55 81 -9 -974150009 OP-56 19 -9 -974150010 OP-57 174 -9 -974150011 OP-58 43 -9 -974150012 OP-59 34 -9 -974150013 OP-60 17 -9 -974150014 OP-61 296 -9 -974150015 OP-62 31 -9 -974150016 OP-63 45 -9 -974150017 OP-44 7045 -9 -974150018 OP-65 503 -9 -974150019 OP-66 5 -9 -974150020 OP-67 15 -9 -974150021 OP-68 569-9-974150023 OP-69 31495 -9 -974150024 OP-70 14 -9 -974150026 OP-71 392 -9 -974150027 OP-72 493 -9 -974150028 OP-73 310 -9 -974150029 OP-74 24074 -9 -9

Oet-25-93 O3:19P Dell P .02

74150030741500317415003274150035741500307415003774150038741500397415004074150041741500427415004674150047741500467415005074150051741500537415005474150055741500567415005774150058 R74150050741500607415006374150064741500657415006674150067 R74150069 R74150070 R74150071 R74150072 R74150073 R74150074 R74150075 R74150076 R74150078 R74150079 R74150080 R 74150061 R END

OP-75OP-76OP-77AOP-77BOP-78OP-79OP-80OP-81OP-62OP-83OP-84OP-85OP-86OP-67OP-88OP-89OP-90OP-91OP-95OP-98OP-97

2 OP-98OP-100OP-101OP-102OP-103OP-104OP-105

2 OP-1 102 OP-1112 OP-1122 OP-1132 OP-1142 OP-1152 OP-1182 OP-2012 OP-2022 OP-2032 OP-2042 OP-2052 OP-206

91942*.464*

3025134

4735089449090

338387

161328

223421

1498422992

6981249119

-511223220

809115

-5-5-5-5-59

•568

-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9

-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9-9

RIVER GOLD MINES LTD ASSAY LABORATORY

127 Mission RoadWawa,Ontario, POS IKO

phone (705) 856-8274 fax (705) 856-8274

CLIENT JAYSON GERDES DATE Oct. 21,1999

Type of analysis Au - FA,gravimetric finish

CERTIFICATE OF ANALYSIS

SAMPLE Au NUMBER g/tonne

207 A 213.82 CHANNEL (0.6m)

207 B 5.21 CHANNEL (l.lm)

108 0.27 CHANNEL ( 1.8m)

209 0.55 CHANNEL ( 1.2m)

Report by:.

NDU-30-1999 12=17 FROM NEMIS-NORONT RESOURCES TO 17058564227 P.02

GRADES PROSPECT

TOTfiL P.02

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BASIC GEOLOGY A PROSPECTING

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42C03NW2004 2.20116 KEATING 020

MAPPING OF THE DISCOVERY OUTCROP

GEOLOGY REPORT

MAPC* O

Introduction

Hie single outcrop was mapped and sampled Thursday November 26,1998 by invitation of Jason and Associates.

Access to the property is achieved from Hwy 17 by turning south onto die Paint Lake Road and travelling for 36 kilometers and then turning west onto a logging road mat splays from the main road at the power transmission fine. The proerty is approximately 8 kilometers west of the power transmission fines.

Lithology - Hand Specimen Description

1. Felsic lithic Tuff

The weathered rind is mottled light brownish grey to tight brown. The matrix is tight grey and less resistive to weathering . Consequently the felsic fragments are conspicuous brown lenticular shapes embedded k die matrix . The shear planes are a brownish orange

e presents of ankerite.

The fresh rock surface is grey in colour. The aphanetic grey siliceous matrix possesses seams of very fine grained pyrite, less than 2 mm in width and less than l Vo in abundance. The felsic fragments are dark grey , lenticular with a length to width ratio of 10 : l and siliceous.

The felsic tuffis interdigitated with several minor seams of mafic ash tuff less than l cm in width. The mafic ash is dark green and chloritic. The bedding planes are cross cut by tension gashes infilled with quartz. Each tension gash is less than l cm in width.

The felsic lithic tuffis sheared at an orientation of 073 7 80 N .

2. Mafic Ash

The weathered surface is greyish green to light grey and fine grained to very fine grained. The mafic ash is mterdigjtated with several mmor Kght grey seams of felsic ash tuff less than 30 cm m width. Many of the exposed shear planes are rusty brown from the weathering of ankerite.

The fresh surface is dark green, ohloritized and pervisively sericitized.

The mafic ash is intensely sheared at an orientation of 073 1 90.

The outcrop of mafic ash possesses several veins of ankerite concordant to the strike of tile shear. One vein of ankerite is seven meters in length and less than 30 cm in width.

Quartz Veins

Hie veins of quartz are composed of white sugary l granular quartz md possess trace amounts of pyrite. There are two basic orientations of the quartz veins traced across the outcrop: concordant with the strike of the shear 073 -080 and cross cutting the strike of the shear. One quartz vein possessed a dot of chalcopyrite and pyrite 2 cm in diameter.

Quartz Tourmaline Veins

These veins are comprized of sugary l granular quartz, black fine grained to very fine grained tourmaline and trace amounts of pyrite.

Ankerite Veins

The veins of ankerite are reddish brown in colour and concordant to the strike of die shear.

Sample Number

26501

26502

26503

26504

26505

26506

26507

26508

26509

26510

26511

26512

26513

Assay g l tonne

0.03

0.03

0.03

0.14

0.1

0.03

0.03

0.03

0.03

0.03

0.14

0.03

0.07

Description

Quartz vein < 3 cm , quartz - white, crystalline

Quartz vein < 10 cm, quartz - white, crystalline tr tourmaline - bk, vfg 157 /55 W

Quartz vein -c 10 cm, quartz - white, crystalline trpy.trcpy 111 y 65 S

Quartz vein < 25 cm , quartz - white , crystaHne 140 /20 W

Quartz vein *: 10 cm, quartz - white - crystalline 123 l 70 W

Quartz vein < 15 cm, quartz - white, crystalline tr tourmaline-bk, vfg 160 790

Quartz vein < 10 cm, quartz, white, crystalline 153 1 85 W

Quartz vein -: 10 cm , quartz - white, crystalline tr tourmaline - bk, vfg 133 780 W

Quartz vein < 10 cm, quartz - white, crystalline 096 770 N

Quartz tourmaline vein -s 10 cm, quartz - whitecrystalline

< 10 % tourmaline bk. vfg 158/20 W

Quartz vein < 5 cm, quartz - white, crystalline tr tourmaline - bk, vfg

153 1 90

Quartz tourmaline vein -c 10 cm , quartz - white,crystalline

< 5 % tourmaline bk, vfg

Felsic lithic tuff - matrix - tt. grey, aphanetlc, siliceous- fragments - It. grey, LxW s 10:1

- siliceous-1 % py, vfg, diss- shear 079 1 75 N

Sample Number Assay Descriptiong l tonne

26514 0.03 Mafic ash - sheared - dk green, vfg, chloritic- ^% py vfg. diss-10 "H) ankerite - clots < 3 cm- shear 074/85 N-10'ft quartz vetoing

26515 0.14 Mafic ash - sheared w/ ankerite vein

26516 0.03 Mafic ash

26517 0.03 Felsic ash tuff

NOV-2T— PM

iinples r*c*ived Results

HIVER COLD MINES Daily Assay Report27.18

j Ne.i 01!~3T

03! 041 OS

08070809101112131415161718li

2021

2223

74

2S

It27282930

Semple Number2&50I OrttfS26502265032#50fZ #505IMW2659?2*60826501l&lO265 1/2*5(220S ft2tf rt265*265ltf266 17

Au I/tonne

•t- Oftc 0,0

0,1*1QlO

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Assay Results

AA samples -were assayed lor gold. Four specific targets were sampled, quartz veins, quartz tourmaline veins, ankerite veins and die pyritiferious felsic lithic tuff seams. Unfortunately the samples did not contain gold.

Conclusion

A single exposed outcrop was sampled. The results of the gold assays should not deter further exploration of the property.

f.

Certificate

I, Werner Wirowatz, of Ae town of Wawa, in tile province of Ontario do hereby certify that:

1.1 have been employed as a geologist with River Gold Mines since September 1994.127 Mission Road P.O. Box 1520

Wawa, Ontario POS-1KO

2.1 graduated from McMaster University, in May 1978, with a Bachelor of Science degree in Geology.

I graduated from the University of Waterloo, in May 1982, with a Honours Batchelor degree, major Chemistry.

3.1 reside at 58 Government Road Wawa, Ontario POS-1KO

4.1 have been engaged in mineral exploration and mining since 1977.

5.1 have no personal interest, nor do I expect to receive any interest in the property.

Yours sincerely;

Jffi Jf *'i0nOM5yL' Werner Wirowmz

42C03NW2004 2.20116 030

DAILY LOG

JULY 1/99.......LINE CUTTING, BRUSHING OUT AND RECHAINING BASE LINE -OJULY 2/99.......BRUSHING AND RECHAINING LINE-0JULY 24/99.......MEET BACKHOE OPERATOR TO VIEW WORK AREASAUG 9/99.......CUT LINE, TIE LINE 12+80SAUG 10/99.......CUT LINE, TIE LINE 13+20SAUG 14/99.......WORKED WITH BACKHOE, WASHING OUTCROP, MAIN SHEARAUG 15/99.......WORKED WITH BACKHOE, WASHING OUTCROP, MAIN SHEARAUG 16/99....... WORKED WITH BACKHOE, WASHING OUTCROP, MAIN SHEARAUG 17/99.......WORKED WITH BACKHOE, WASHING OUTCROP, NOVAK SHEARAUG 18/99.......WORKED WITH BACKHOE, WASHING OUTCROP, NOVAK SHEARAUG 19/99.......WORKED WITH BACKHOE, WASHING OUTCROP, MAIN ROADSEPT 3/99.......SAMPLEDNOVAK SHEAR(GRABS)SEPT 4/99.......LINE CUTTING 12+50SSEPT 5/99.......LINE CUTTING 12+50SSEPT 6/99.......LINE CUTTING 12+50SSEPT 11/99.......LINE CUTTING 7+OOE —————————SEPT 12/99.......LINE CUTTING 7+OOESEPT 14/99.......WASH OUTCROP, MAIN SHEARSEPT 15/99.......WASH OUTCROP, MAIN SHEARSEPT 16/99.......PROPERTY VISIT BY ANN WILSONSEPT 19/99.......LINE CUTTING, CHAINING 7+OOESEPT 21/99.......LINE CUTTING 6+OOESEPT 22/99.......LINE CUTTING 5+OOESEPT 24/99.......CHAIN LINE 7+OOE,6+00,5+OOESEPT 25/99.......WASH OUTCROP, MAIN SHEARSEPT 27/99.......HAND MUCK, WASH OUTCROP, MAIN SHEARSEPT 28/99.......HAND MUCK, WASH OUTCROP, MAIN SHEARSEPT 29/99.......HAND MUCK, WASH OUTCROP, MAIN SHEAROCT 1/99.......CUT LINE, TIE LINE 3+OOSOCT 2/99.......CUT LINE, TIE LINE 3+OOSOCT 3/99.......CUT LINE, CHAIN TIE LINE 3+OOSOCT 4/99.......CUT LINE, S+OOE^+OOE, CHAIN LINE 6,5,4,3OCT 8/99.......CHANNEL SAMPLEOCT 9/99.......CHANNEL SAMPLEOCT 10/99.......CHANNEL SAMPLEOCT 15/99.......CHANNEL SAMPLE

RECEIVEDFEB 2 8 2CG3

GEOSCIENCE ASSESSMENT OFFICE ^

OCT 18/99.......MAPSOCT 19/99.......MAPSOCT 20/99.......MAPSDEC 1/99.......PROSPECTINGDEC 2/99.......PROSPECTINGDEC 3/99.......PROSPECTINGDEC 4/99.......PROSPECTINGDEC 10/99.......MAPSDEC 11/99.......MAPSDEC 12/99.......MAPSDEC 13/99.......REPORT PREPDEC 14/99.......REPORT PREPDEC 15/99.......REPORT PREPDEC 16/99.......REPORT PREPDEC 20/99.......REPORT PREPDEC 21/99.......REPORT PREPDEC 22/99.......REPORT PREPDEC 23/99.......REPORT PREP

TOTAL 54 DAYS @ S100.00 per day TOTAL S5400.00

I MADE 17- 200km ROUND TRIPS TO THE PROPERTY, TOTAL 3400km @ S0.30 per km TOTAL S1020.00

HELPER GILES CHARONNEAU WORKED THE FOLLOWING DATES

SEPT 3/99.....SAMPLINGSEPT 19/99.....LINE CUTTING, CHAINING LINE 7+OOESEPT 24/99.....CHAIN LINE 7E,6E, & 5ESEPT 25/99.....WASHED OUTCROP, MAIN SHEAROCT 1/99......LINE CUTING, TL-3+OOSOCT 8/99......CHANNEL SAMPLINGOCT 9/99..... .CHANNEL SAMPLINGOCT 10/99......CHANNEL SAMPLING

TOTAL 8 DAYS @ S 100.00 per day TOTAL S800.00

GILES MADE 8-200km ROUND TRIPS TO THE PROPERTY WITH HIS TRUCK TOTAL 1200 km @ S0.30 per km TOTAL 5360.00 TOTAL SI 160.00

HELPER RICHARD THIBODEAU WORKED THE FOLLOWING DATES

JULY 1/99......LINE CUTTING, BRUSHING, CHAINING, L-0 Se BL-0JULY 2/99......LINE CUTTING, BRUSHING, CHAINING, L-0JULY 24/99......BRUSHING LINE OAUG 14/99..... BACKHOE, WASH OUTCROPAUG 15/99......BACKHOE, WASH OUTCROPAUG 16/99......BACKHOE, WASH OUTCROPAUG 17/99..... .BACKHOE, WASH OUTCROPAUG 18/99......BACKHOE, WASH OUTCROPAUG 19/99......BACKHOE, WASH OUTCROPOCT 3/99......CUT LINE, CHAIN, TL-300SOCT 4/99......CHAIN LINE 6,5,4,3OCT 8/99......CHANNEL SAMPLINGOCT 9/99......CHANNEL SAMPLINGOCT 10/99......CHANNEL SAMPLINGOCT 13/99......PROSPECTEDOCT 15/99..... CHANNEL SAMPLED

TOTAL 16 DAYS @ S100.00 per day TOTAL S1600.00

RICHARD MADE 12- 200 km ROUND TRIPS TO THE PROPERTY WITH HIS TRUCK TOTAL 2400km @S0.30 TOTAL S720.00 TOTAL S2320.00

ITSIT: JASON GEROES n: T99-57348.0 {

Intertek Testing Services5:himitec Bondar Clegg Rapport Lab Geochimie

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Ontario Ministry ofNorthern Developmentand Mines

42C03NW2004 2.20116 KEATING

Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.0.1990

Transaction Number (office use)

Assessment Files Research Imaging

subsection 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, issesment work and correspond with the mining land holder. Questions about this orthern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury,

900Instructions: - For work performed on Crown Lands before recording a claim, use form 0240.

- Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary)Name Client Number

X 33V/ 7Address Telephone Number

Fax Number

Name Client Number

Address /So* 33 (^ Telephone Number

Fax Number

2. Type of work performed: Check (S) and report on only ONE of the following groups for this declaration.Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

Physical: drilling stripping, trenching and associated assays

Rehabilitation

Work Type , * r*iflp'** Office UseCommodityTotal S Value of Work Claimed

Dates Work From Performed/IMS Year/^fC \ Month | Year

NTS Reference

Global Positioning System Data (if available) Mining DivisionM or G-Plan Number Resident Geologis

District

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)Name Telephone Number

Address Fax Number

Telephone Number

Address Fax Number

Name Telephone Number

Address Fax Number

4. Certification by Recorded Holder or Agent, do hereby certify that l havi

(Print Name)this Declaration of Assessment Work having caused the work to be performed completion and, to the best of my knowledge, the annexed report is true.Signature of Recorded Holder or Agent ^--^

facts set forth in

or after its

Agent's Addresss^,^3 //Co

Fax Number

0241 (0*97)

O i

Ontario Ministry ofNorthern Developmentand Mines

Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.0.1990

Transaction Number (office use)

Assessment Files Research Imaging

Personal information collected on this form is obtained under the authority of subsection 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, this information is a public record. This information will be used to review the assesment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines. 3rd Floor, 933 Ramsey Lake Road Sudbury Ontario, P3E 6B5.

Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary)Client Number

Ad*ess Telephone Number

Fax Number

Name Client Number

Address Telephone Number

V Fax Number

armed:2. Type of work performed: Check (-0 and report on only ONE of the following groups for this declaration.Geotechnical: prospecting surveys, assays and work under section 18 (regs)

Physical: drilling stripping, trenching and associated assays

Rehabilitation

Work Type \

Date* Work From \ To PMfomwd Day | Month | Year \ Day | Month | Year

Global Positioning System Data (if available) Township/Mea

M or G-Plan Nftmber

Office UseCommodityTotal S Value of Work ClaimedNTS Reference

Mining DivisionResident Geologist District

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surnace rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical reoprt (Attach a list if necessary)Name \

Address \

Name \

Address ' ^

Name \

Address \

Telephone Number

Fax Number

Telephone Number

Fax Number

Telephone Number

Fax Number

4. Certification by Recorded Holder or Agent \l. _________________________, do hereby certify that l have Versonal knowledge of the facts set forth in

(Print Name) Athis Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true. \Signature of Recorded Holder or Agent \

Agenf s Address Telephone Number \

Date

Fax Number

0241(03/97)

•TI

5. Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this

Mining Claim Number. Or if work was done on other eligible mining land, show in this

column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

TB 7827

1234567

1234568

//b^8?io *J^^i (o *VO*/*2/^ 3cf .

n^^^zo

Column Totals

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

f

Value of work performed on this claim or other mining land.

526,825

0

5 8,892f f

w,*99*?A9*'5799

(5

j*

V23.H8

Value of work applied to this claim.

N/A

524,000

S 4,000

6 6 poo' **&X&0 - ^#6 (/6~o ' e-e

fat (f 0V 'C**

w *(*(JV

Value of work assigned to other mining claims.

524,000

0

0

Bank. Value of work to be distributed at a future date

52,825

0

54,892

//0?#'^

0/598'"*

, do hereby certify that the above work credits are eligible under(Print Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim

where the work was done.Signature of it Authorized in Writing Date _-

6. Instruction for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check (S) in the boxes below to show how you wish to prioritize the deletion of credits:

D 1 . Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.D 2. Credits are to be cut back starting with the claims listed last, working backwards; orD 3. Credits are to be cut back equally over all claims listed in this declaration; orD 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use Only ——^^^^———^^^^^^^—-Received Stamp

0241 (03/97)

2.201

Ontario Ministry o1Northern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal information collected on this form is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, this information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 685.

Work TypeUnits of work

Depending on the type of work, list the number of hours/day worked, metres of drilling, kilometres of grid line, number of samples, etc.

Cost Per Unit of work

Total Cost

/fe? s/y-gg /we j fi use a s 7* ips/t 4g

^-

jAssociated Costs (e.g. supplies, mobilization and demobilization)

s

Transportation Costs

Food and Lodging Costs

Total Value of Assessment Work *

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 1000Xo of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 5007o of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 = Total S value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed i verification and/or correction/clarification. If verification and/or correctio or part of the assessment work submitted.

FED 25 2000

in 45 days of a request for he Minister may reject all

Certification verifying costs:

l. ,, do hereby certify, that the

6EOSC1EMCEASSESSMEMT

Tiuuillb JJflown are as accurate as may reasonably(please print full name)

be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying

Declaration of Work form as _____O x- i y ^ r r ~- pt^ '^-l^s- J TT^PffirlC^(recorded holder, agent, or state company position with signiry aiifhorftyj "~-

I am authorized to make this certification.

0212 (03/97)

0116

Ministry of Mlnistere duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road

May 29, 2000 6th FloorSudbury, Ontario

JAYSON ARTHUR GERDES P3E6B5 42 TAMARACK AVEBOX 1991 Telephone: (888) 415-9845 WAWA, Ontario Fax: (877)670-1555 POS-1KO

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2.20116

Status Subject: Transaction Number(s): W0050.00016 Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the - response date on the summary.

If you have any questions regarding this correspondence, please contact JIM MCAULEY by e-mail at james.mcauley@ndm.gov.on.ea or by telephone at (705) 670-5880.

Yours sincerely,

ORIGINAL SIGNED BYSteve B. BeneteauActing Supervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 14919

Copy fort Assessment Library

Work Report Assessment Results

Submission Number: 2.20116

Date Correspondence Sent: May 29, 2000 AssessonJIM MCAULEY

Transaction First Claim Number NumberW0050.00016 1163876

Section:9 Prospecting PROSP10 Physical PSTRIP 12 Geological GEOL

Township(s) l Area(s) StatusABBIE LAKE, KEATING ADDITIONAL Approval

Approval Date

May 24, 2000

Correspondence to:Resident Geologist South Porcupine, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):JAYSON ARTHUR GERDES WAWA, Ontario

RICHARD RENE THIBODEAU WAWA, ONTARIO

GILES G CHARBONNEAU WAWA, ONTARIO

Page: 1Correspondence ID: 14919

REFERENCES

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PARCEL •OUNOAM Y ————————— ~

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NOH^ERfNNIAL STREAM — — i —— —————. FLOODING OR FLOODING RIGHT: "iu-rj^JJix^

ORIGINAL SHORELINE

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TYPE OF POCUWNT IYMBOLrATEtfT SURFACE * M 1*(**G RWJMTS ..... ............ *

SURFACE RIGHTS O.JLY ^ .,.. A

LiASE. SURFACE M KiNtNGRfCHTS . . . .- .. .. ... B •URFACC MIGHTS ONLY , . BMINB*G"K1HT1I.O*ILV . .... r

LlCINOE O^CKJCUTAilO*! ........ ——. ,. .-.-......-, VOROCA -W 'XXJWCIL ,.™.. ....... — .......,.. OC

CAMCCLLED .. ,....... ,. . ,....... ........ ., *KANdftCHAVFI ^)

MOfC- MbMlNa MiatlTI IH FAPICELJ ^AllHTIO Utm* TD MA* * 1*1*. VICTCO It OttlQHVAL TATiHTEE BV THF PU |L tCUhwuf *CT. w.* W i*'D. CHAP jad. t(c *J. ^.'/MIC i

AREAS WITHDRAWN PROM DIVO8ITION

M-RJJ.- MINING RIGHTS OWL Y i

S^JO. - SURFACE RIOKTS ONLY [

ML* ft. - MINING AND SURFACE RKWT*

(S) 5EC35 W-LL-C1609I89 ONT MAY12S9 M&S

SCALE : 1 HUGH - 40 CHAIN!

PKT - ^^

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AREA

ABBIE LAKE

J,__

M.N.fl. ADMINISTRATIVE DISTRICT

WAWAUININ6 fi l VI S i UT.

SAULT STE MARIELAND TITUS/ REGISTRY DIVISION

THUNDER BAY

42C03HW2004 2.20116 KEATING 200

_____REFERENCES^^^^

AREAS WTHMAKH FROM DISPOSITION

M.*,0. - MINING RIGHTS ONLY

f.B.0. - SURFACE RIGHTS ON LV

M.+ S, - MINING AND SURFACE RIGHTSv

i*. Dmtm DiapodtNHi fit*

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY 16 NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUE OF THE LANDS SHOWN HEREON.

NOTESOWNED BY A C, NY. NOT OPEN FOR STAKING

UNDER OUT. MINING ACT, ENQUIRE AT A. C. RV. OFFICES AT S.STE,***RIE REGARDING STAHINGS

KEATING ADDITIONAL IS OPEN FOR STAKING UNDIH tHt ONTftUlO NlMHa ACT , - —

The 1 ft p oro* .

- Magnetic Bearing J Annual

R E cTT v t D

CHARBONNEAU TWP.

34M

RER 586I2

LEGARDE 8 LEGARDE ADD'L TWP.

HIGHWAV AND fJOUTE No OTHER ROADS TRAILS SURVEYED LINES

TOWNSHIPS. iASF L+NES, ETC

LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC

RAILWAY AND RIGHT OF WAV UTILITY LINES NON PERENNIAL STREAM FLOODING OA FLOODING RIGHT5 SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT

TYPF OF DOCUMENT

PATENT. SURFACE Si Ml*

" , SURFACE RIGHTS QNLV,, MINING RIGHTS ONLY

LEASE. SURFACE ft MINING R 1C" , SURFACE RIGHTS ONLY " .MINING RIGHTS ONLY

LtCf NCE OF OCCUPATION ORDER-IN COUNCIL ......RESERVATION ....... ,CANCELLED SAND A GRAVEL

VOTE' MINJNCI niagra 114 PAII. VeiTED Ih OKI*

SCALE: l INCH - 40 CHAINS

FEFTa i aw

O 3OC IOOOM

TOWNSHIP

MIHINC DIVISION

Ministry ofNatural

ResourcesOntario

•END

PARCELS. ETC. ———————————

-~— - ————————

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T E PLAN ^^5wsww!K?^^.

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SYMBOL

MG RIGHTS -,................. 9

50NLV. . ___ . 6

)NLY...... ........ . 9Q RIGHTS.. . .. .. ..... M3NLY...,..^. ..,............ BILV... .— .. -.,. ^..... B

-,.......... .......mM..... T.—.— ..-,.................. oc..............., ©

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42C03HW2004 2,20116 KEATING 210