r-. 91

N.T.S. 31 L/14

REPORT OF HEAVY MINERAL SAMPLING ON THE PARKMAN PROPERTY

PARKMAN, WYSE Z MCAUSLAN TOWNSHIPS', ONTARIO GRENVILLE GOLD CORPORATION - AMITA-GREENFIELD RESOURCES INC.

Prepared By: Robert J. Dillman8901 Reily Drive

Mount Brydges, Ontario

November 12, 2004

31L14SE2010 2.28918 PARKMAN 010

FRDM ' T J BEESLEYI'LL W ' i."4 J.JB:.M..

NO. NU

r.' i.,LU'j. u NL L IIL-U.'.,'JTII..PJI

rr*A 234Dec. 08 2004 05:50Pn PI

'j:..(uu 'r

OntarioMinistry of Ministere du "x-.~

Northern Development Developpement du Nord

and Mines et des Mine

Telephone: 1-888-415-9845 C^^jjAX: 1-877-670-1555

www.mndm.gov.on.ca/MNDM/MINES/LANDS/default.e.asp""

2891 8Geoscience Assessment Office1*33 Riimsey L^ike Road 6ttl Floor

Sudbury, Ontario P3E6B5

UPDATE UPDATE UPDATE UPDATE UPDATE UPDATE UPDATE UPDATE

Changes to the Assessment Work Regulations

There have beeo changes w ihc AsscssrneiU Work Regulation (O.Reg. 6/96). Th* (hinges will come into sifiees on Friday Doeemb*r Oj, 2004, Accordingly, all aswMment work performed and *;[ed on ar after December 03, 2004 \vill be repaired to comply *itfi ihs new Assessment Work RcEUUtiions (309/04) lo receive ftill jaresj.-neflt credit The most nottble changes affeci prospecting (section 9), physical wo* (section 10), drilling (section K) and ocher riijiWc work (section 18).For a summary of the major chalet to th* Asswwmrmr Wnrt Rcflnlaiioif, ?J*Mo 'jioi'.

e.asnFor* complete deaiJcd list of (he changes 16 the Asjcssnent Work R*ftulaiionj, please vjjit the Ontario E-Lsws web liter

or Tilt QniarSa fiaxrrrr. , fQOt Uc

'fill PanlJTlllr mijrrnnnin IPnmffl7ED.OIDCOl!rrn)rai'T'i'tLnfrflrll,fAfW4 Uuv 101 uie we or me Aaoursssoc^; named hflVfi, If yrtli arr nnr rhp tnrsndcd r9cipi*ot of thia fiiosiniils w tlii a^ui ui em^luvuu icsponslblc tar oeiivcnng it to the intended

recipient, you arc herby notified that any dissemination or copying of thi? facsimile is strictly prnhihiTfVl If ynn hsve received thie in frrgr, plgaM notify HO immHi.lri'ly by (r/lc^Uou* and rwtum tho ori^Kel titjiiVdly lw UJ aL Ills itluivr; ntWrm rt* l" iih you. ________ ______

L*aie: ugugi uuei fl, JJ004_____ Pages: .2.....- -

From: Joanne Levac Phone: 1-888-415-9845 ext. 5853 or 1-705-670-5853

Re: j^filicajiqnjgrj^ ^^,,,^mn^^^

[ j For Review/Information 0 PJease Reply Q As per Your Request

Mr. Beesley,

Your application for assessment work filed in our office on December 6, 2004 will require revisions. The first claim listed on your application is listed incorrect, According to the sketch, the claim should be 1163584 and not 1163984, You also have under claim number an assignment of S4727 dollars. The claim did not performe. therefore, it cannot assign any credits. Only the ones that did perform can assign credits. Piaase revise your application, then re-fax it to me at the above toll free fax number.

If you have any questions regarding this matter, please contact me at the above toll free number.

Thank you,

Joanne LevacGesolence Assessment Work Officer.

W*

416 234 9428 PAGE. 01

DEC 08 '04 15=20

INDEXPage

I. INTRODUCTION 2 Scope 2 Location and Access 2 Claim Logistics and Ownership 6 Survey Dates and Personnel 6 Geological Setting 6 History 10

II. SURVEY PROCEDURE AND RESULTS 15Logistics 15Kimberlite - Diamond 15Iron Formation Minerals 22Gold 23General Composition of the Heavy Mineral Concentrates 23

III. DISCUSSION OF RESULTS 23Kimberlite Minerals 23Iron Formation 27Gold 28

III. CONCLUSIONS AND RECOMMENDATIONS 28

REFERENCES 30

AUTHORS CERTIFICATE 32

APPENDIXElectron Microprobe AnalysesMap of Sample Locations and Results, 1:2,500 scale

FIGURESFigure 1. Location Map 3Figure 2. Claim Map 4Figure 3. Property Location Map 5Figure 4. Property Geology Map 8Figure 5. Regional Geology 9Figure 6. Drill Hole Location Map 11Figure 7. Kimberlite Mineral Locations: Green Lake Zone 17Figure 8. Pyrope Garnet and Chrome Diopside Plots 20Figure 9. Chromite and Picroilmenite Plots 21

TABLESTable 1. Claim Logistics 7 Table 2. Process of Heavy Mineral Concentration 16 Table 3. Results of Heavy Mineral Sampling 19 Table 4. General Composition of the Heavy Mineral Concentrates 25

REPORT OF HEAVY MINERAL SAMPLING ON THE PARKMAN PROPERTY

PARKMAN, WYSE 8, MCAUSLAN TOWNSHIPS', ONTARIO GRENVILLE GOLD CORPORATION - AMITA-GREENFIELD RESOURCES INC.

l. INTRODUCTION

Scope

This report summarizes a heavy mineral sampling program for kimberlite indicator minerals over a section of the Parkman Property located at the junction of Parkman, Wyse and McAuslan Townships in Ontario. The property is underlain by Proterozoic gneisses and cut by faults belonging to the Timiskaming Structural Zone which hosts several diamondiferous kimberlite fields. A strong kimberlite mineral anomaly has been detected on the property. The quantity of kimberlite minerals is suggestive of local sources. The kimberlite minerals include: pyrope garnet, chrome diopside, chromite, picroilmenite, uvarovite garnet, olivine, phlogopite and eclogite garnet. Some of the kimberlite minerals within the anomaly are pellet-shaped and have un-eroded, well-preserved magmatic features such as shagreen texture and kelyphite or calcite reaction rims on grain surfaces. The preservation of the surface features and grain shapes are additional evidence suggesting the kimberlite minerals have been eroded from local sources. Since discovery, the chemistry of 981 kimberlite minerals have been determined by an electron microprobe. Approximately 607o of the pyrope xenocryst population is derived from harzburgite paragenesis. The Parkman kimberlite anomaly also contains pyrope eclogite garnets known to be associated with diamond eclogite paragenesis. An aeromagnetic survey over the property has identified eighteen magnetic features which may represent kimberlite pipes and sources for the minerals.

Location and Access

The Parkman Property is located in the Sudbury Mining District in northeastern Ontario (Figure 1). The property is situated at the junction of the non-surveyed townships of: Parkman, Wyse and McAuslan Township's. The property can be found on the Ontario Ministry of Northern Development and Mines Claim Map: G-1666 (Figure 2).

The property is centred at Latitude 460 49'N, Longitude 790 15'W and bound between Universal Transverse Mercator (U.T.M.) coordinates: 5183500 to 5190000 m.N., 631000 to 638000 m.E. on topographic sheet: 31 L/14 Ottertail Creek.

The Parkman Property is crossed by the McLaren's Bay Road which provides year-round accessibility by car or truck (Figure 3). The McLaren's Bay Road begins at the town of Eldee on Highway 63 located northeast of North Bay. The property is situated 60 kilometres northeast of North Bay.

-2-

Bandore Pele

MountainSudbury Contact

Cabo Mining

Kirkland Lake Kimberlite Field

New Liskeard Kimberlite Field

Parkman Property

Vardy Lake Picton

* Diamond Occurrence

Kimberlite Occurrence or Field

100 200 km

Figure 1.

PARKMAN PROPERTYAMITA-GREENRELD RESOURCES INC. - GRENVILLE GOLD CORPORATION

Parkman, Wyse and McAuslan Townships Sudbury Mining District, Ontario, Canada

-3-

830000E 631000E 6320COE7915W

833000E i 834000E B3SOOOE

-N-

630000E 831000E 632000E 633000E l B34000E7915W

1000 2000 metres

635000E^'^ -^^\_^ 837000E 638000E

Source: MMR Claim Map G-1666NTS Sheet 31 L14 Ottertail Creek

Parkman Property

Figure 2.

CLAIM MAP PARKMAN PROPERTY

AMITA-GREENFIELD RESOURCES -GRENVILLE GOLD CORPORATION

Parkman, Wyse and McAuslan Townships Sudbury Mining District, Ontario, Canada

-4-

ALGONOUIN

PROVINCIAL

PARK

79"

38Source: Ontario Provincial Road Map

Allmaps Canada Limited

Figure 3.

46"

50 100 Kilometres

PROPERTY LOCATION MAF3PARKMAN PROPERTY

Parkman, Wyse and McAuslan Townships Sudbury Mining District, Ontario, Canada

-5-

Claim Logistics and Ownership

The Parkman Property covers approximately 2,848 hectares of land with 14 contiguous unpatented - non surveyed claims which encompass 178 units (Figure 2). Claim logistics are summarized in Table 1.

All titles to the claims comprising the Parkman Property are registered equally in the names of: Christopher Marmont and Rodney N. Thomas, both of Oakville, Ontario.

Survey Dates and Personnel

On September 16, 2004 the author visited the Parkman Property for 3 days on behalf of Amita-Greenfield Resources. During the property visit, the author collected 11 gravel samples.

Heavy mineral concentrates were processed by the author at Mount Brydges, Ontario between September 20 and September 27, 2004.

Heavy mineral concentrates were examined for kimberlite indicator minerals by the author between September 28 and October 5, 2004.

Kimberlite indicator minerals were submitted for electron microprobe analyses at R.L. Barnett Geological on October 6, 2004. Results of the analyses were completed by October 22, 2004.

Data processing and the report were completed by the author at various times between October 23 and November 12, 2004.

Geological Setting

The Parkman Property is located within the Tomiko Terrane in the Central Gneissic Belt of the Grenville Province (Figure 4). The Tomiko Terrane consists of abundant metasedimentary rocks which, on the basis of geochronological data (age), are unique and distinguishable from other rock types of the Central Gneissic Belt. Ages of sedimentary rocks are Mesoproterozoic, roughly 1,900 Ma and correlate to Mesoproterozoic base metal terranes in New York State, Scandinavia, South Africa and Australia.

The property is situated 30 kilometres south of the Grenville Front Tectonic Zone. The Grenville Front is a major geological boundary between Archean rock types and Proterozoic units (Figure 5).

The Parkman Property is situated within the Lake Timiskaming Structural Zone. The structure trends northwest and is considered as an old and active rift valley. In the New Liskeard- Cobalt region, the structure contains a cluster of Jurassic-aged kimberlite pipes, several of which are diamond-bearing. Wawa style diamond lamprophyre also occurs along the structure.

-6-

Table 1.

Claim Logistics Parkman Property Parkman Township, Ontario

Recorded Title Holder(s):

title in name of:

5007o title in name of:

Christopher Marmont 1165 Queen's Avenue Oakville, Ontario

Rodney N. Thomas 306 Pine Avenue Oakville, Ontario

Claim Numbers81163^84S 1174498S 1174499S 1174500S 1191991S 1191992S 1191996S 1192538S 1192539S 1192542S 1229411S 1229412S 1231284S 123128514 CLAIMS

Units

14121210121214168

1216161212

178

Hectares

224192192160192192224256128192256256192192

2348

Recording Date

2001 -APR- 112001 -APR- 112001 -APR- 112001 -APR- 112002-JUN-142002-JUN-142002-OCT-222002-JUN-142002-JUN-14

2002-MAY-091998-DEC-241998-DEC-241998-DEC-241998-DEC-24

Assessment Date

2005-APR-ll2005-APR-ll2005-APR-ll2005-APR-ll2005-JUN-142005-JUN-142005-OCT-222006-JUN-142005-JUN-14

2005-MAY-092004-DEC-242004-DEC-242004-DEC-242004-DEC-24

S Work Required

5,1103,5103,5101,8974,8004,8005,6006,4003,2004,8006,4006,4004,8004,800

S66,040

S Total Applied

11,69010,89010,89010,1034,8004,8005,600

12,8003,2004,800

25,60025,60019,20019,200

S 169,173

TOTAL RESERVE

0000000000

1,79200

2,09583,887

-7-

A*""™ vy^tk ^\ f\\ ̂ ^^U^v r^i

'" "-O- ^ye /' -P uT

^^^C^:^^~. a ^\^jn\n3^["^"~

WTO-

10 kilometPBS

Source: Card and Lumbers 1977 Marmont 1999

LEGEND

46 Quaternary39 Granite Mulock Batholith38 Mafic-Ultramafic. Fall Lake Pluton36 Quartz Monzonite Jocko Batholith35 Quartzo-feldspathic Gneiss33 Pelite Paragneissf Parkman Iron Formation (Tyrrell)

Figure 4.

PROPERTY GEOLOGY PARKMAN PROPERTY

AMITA-GREENFIELD RESOURCES - GRENVILLE GOLD CORPORATION

Parkman, Wyse and McAustan Townships Sudbury Mining District, Ontario, Canada

O 9 Jurassic

ll Slurtan

2. Proterozoic

\QfTZ

1. Archean

Ktnberite, Lamprophyre

Limestone

Gneisses, sedhnentary rocks, plutonic rocks, cartxxiatfte 9

GRENVILLE FRONT TECTONIC ZONE

Volcanic rooks, sedimentary rocks plutonic rock*

Fault

50 kilometres

Source: MNDM 1992, Map 3577

Figure 5.

REGIONAL GEOLOGY PARKMAN PROPERTY

AMnVWSREENSHIELD RESOURCES WC. - GREWILE GOLD CORPORATION

Parkman, Wyse and McAulsan Townships Sudbury Mining District, Ontario, Canada

-9-

The Parkman Property is underlain by moderately dipping interbedded quartzite, marble, amphibolite, iron formation, garnet-mica gneiss and metavolcanic amphibolite of the Mattawa Assemblage. The sequence has been intruded by lamprophyre, ultramafic dikes, anorthosite and syenite dikes of unknown age. Areas proximal to the property were intruded by quartz-monzonite of the Timber Lake Batholith (approx 1,137 Ma) and by sub-alkalic granite of the Mulock Batholith (approx. 1,244 Ma). The area of the property experienced a period of regional metamorphism and deformation between 900 - 1,050 Ma and was intruded by diabase of the Grenville Swarm at approximately 550 Ma.

The dominant geological feature on the property is the Tyrell Iron Formation (Parkman Iron Formation) (Figure 6). The unit consists of interbedded oxide and sulphide facies silicate iron formation. The principal iron-bearing minerals include pyrrhotite, magnetite and hematite. Some historic drill logs describe the nature of mineralization as thick successions ranging 228 - 274 metres (750 to 900 ft) wide of disseminated pyrrhotite and magnetite with local massive to semi- massive sections. Disseminated pyrite occurs in the unit and some references are made to traces of chalcopyrite.

Aeromagnetic surveys over the property reveal the extent of the iron formation and the degree of folding which has occurred to geological units. Folding has occurred along northeast orientated structures. Aeromagnetic data also suggests the presence of northeast faults belonging to the Timiskaming Structure and northeast orientated faults possibly associated with the Ottawa- Bonnechere Graben located south of the property.

The Parkman Property is mostly covered by the sediments of the Mcconnell Lake Moraine and older, underlying glacial tills. The Mcconnell Lake Moraine is part of the Harricana Moraine and formed by out wash processes within a split in the glacier during deglaciation of the region. Glacial till underlying the Mcconnell Lake Moraine is rarely exposed on the property. Till was deposited by 2 or 3 glacial advances of a single ice-sheet which initially advanced from the northeast and shifted to the north-northwest towards the end of glaciation. The thick section of sediments associated with the Mcconnell Lake Moraine has hindered most exploration surveys on the property.

History

Historically, the Tyrrell Iron Formation crossing the Parkman Property has been targeted as an iron prospect and little attention was given to base metal or gold exploration. The diamond potential of the Parkman Property became apparent in 1999 after Chris Marmont and Rod Thomas (current claim holders) discovered abundant kimberlite indicator minerals in Green Creek.

The Tyrell Iron Formation has been tested by 16,291 feet (4,967 metres) of diamond drilling with 41 drill holes. Work has focused on four sections of the structure: the Cook, Webb Lake, Green Lake and Bishop zones (Figure 6).

Exploration of the Tyrrell Iron Formation began in 1959 when D.A. Hardie drilled three holes into the West Limb of the Cook Zone to test for iron.

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4-N-

Iron Formation

O——i Drill Hole Location

Mb Marble

Mn Magnesium

O SOO 10OO metres

Source: Marmont, 2OOO

Figure 6.DRILL HOLE LOCATION MAP

PARKMAN PROPERTYGRENVILLE GOLD CORPORATION

Sudbury Mining District, Ontario, Canada

- 11 -

In 1960, Ventures Claims Limited preformed geological mapping and a ground fluxgate magnetometer survey over the Cook Zone. A 1,658 ft drill program consisting of 6 holes tested the West Limb. Drill logs report cherty magnetite iron formation and a 3 ft interval of massive pyrrhotite.

In 1965, the Geological Survey Canada released the results of a regional aeromagnetic survey which included Parkman Township. The extent of the iron formation in Parkman Township is depicted as a series of strong positive magnetic features.

Between 1966 to 1973, the property was controlled by Iron City Mines Limited. Work focused on testing the iron content in the Cook, Bishop, Webb Lake and Green Lake zones. Ground surveys during this time consisted of geological mapping, magnetometer surveys and a radiometric survey in 1970. Iron City drilled a total of 14,265 ft (4,348 km) in several programs, testing each of the zones with 6 to 8 drill holes. Only two holes tested the Bishop Zone. Total Soluble Iron analyses of the Green Lake Zone by the Ontario Department of Mines ranged 9.1 to 36.707o for an approximate average of 21.1 07o Total Soluble Iron. Extensive analyses of the Cook Zone showed an average Total Soluble Iron content of approximately IS.3%. The Green Lake Zone was found to contain higher manganese. Analyses of the North Limb showed an average of 4.1 07o Mn with a high value of 7.807o Mn. An assay of 507o Mn is reported over an unknown width of two iron formation horizons in a drill section through the South Limb.

In 1971, on behalf of the Ontario Department of Mines and Natural Resources, S .B. Lumbers mapped geology in the Tomiko area and included Parkman Township in the survey.

In 1973, Iron City tested a marble occurrence north of the Cook Zone with a 12 hole drill program totaling 1,507 ft (459 m).

In 1978, the Geological Survey of Canada included Parkman Township in a regional gamma ray spectrometer survey. The survey identified a radioactive response for over a swampy section of the Webb Lake Zone. The site displays elevated Total Count (TC), Potassium (K) and Thorium (Th) responses. A Uranium (U) response was detected south of the site.

Quaternary geology was first mapped in 1980 by J. F. Gartner on behalf of the Ontario Ministry of Natural Resources. He suggested ice (glacial) movement was from the north and the Mcconnell Lake Moraine was the result of a minor halt during the final phase of deglaciation.

In 1980, Charles Mortimer drilled 164 metres with 5 holes. The holes tested unknown targets situated with quartzo-feldspathic gneiss on the property.

In 1986, J. Veillette of the Geological Survey of Canada, found evidence of a widespread initial ice advance from the northeast and subsequent pulses of an advancing single ice-sheet shifting from the northeast to a direction from north-northwest. He suggested the Mcconnell Lake Moraine was part of the Harricana Moraine and coined the term: "Harricana - Lake Mcconnell Complex". The feature formed as a result of an ice-sheet splitting and out washing during deglaciation and not by convergence of one or more advancing glacial lobes.

In 1988, the Geological Survey of Canada included Parkman Township in a regional lake sediment survey. The sample results from Green Lake and Webb Lake, situated within the current claim group, are included in a U, V, Mo and As anomaly focused on the Tyrell Iron Formation.

- 12-

Green Lake also shows anomalous Cu and nearby Emerald Lake is anomalous in Pb, Cd, Ni, Mo, V, Cu, U and As.

In 1996, on behalf of the Geological Survey of Canada, J. Veillette and M.B. Mcclenaghan studied glacial transport distances in the Abitibi-Timiskaming region of the carbonate rocks derived from the Hudson Bay Basin. Quaternary geology was mapped in the Timiskaming region.

In 1998, the current claim holders, C. Marmont and R. Thomas staked 4 claims (54 units) over the iron formation in Parkman Township after recognizing the age and nature of the high grade metamorphic sequence was similar to terranes in Australia and elsewhere that host Broken Hill Type (Pb-Zn-Ag) and Osbourne Type/Iron Oxide-hosted Copper-Gold deposits. Using grants from the Ontario Prospectors Assistance Program, Marmont and Thomas preceded with various soil surveys, rock sampling and heavy mineral prospecting in an attempt to test the gold and base metal potential of the iron formation. Several types of soil surveys were used to penetrate the overburden on the property. Testing humus and B horizon soils, the surveys identified anomalous Cu-Zn-Mn over the Green Lake, Webb and Cook Zones. Heavy mineral concentrates derived from the gravels in creeks draining the property contained traces of chalcopyrite (Cu), gahnite (Zn), gold and abundant kimberlite minerals consisting of pyrope garnet, chrome diopside, chromite and picroilmenite (Marmont, 2000). Subsequent heavy mineral surveys have identified +1000's of kimberlite minerals in Green Creek. Marmont and Thomas's work was highlighted by a 9.8 kilogram sample from Green Creek containing an estimated KIM Count of 6,619 grains (RNT-028). Other samples also contained unusually high concentrations of kimberlite minerals, most of which consisted of chromite and picroilmenite. Electron microprobe analyses of the minerals identified sub-calcic pyrope garnets (G10) of type associated with diamond-bearing kimberlite. The large concentration of kimberlite minerals suggested diamond-bearing kimberlite occurs on the property or in close proximity.

Marmont and Thomas staked an additional 4 claims (48 units) in the spring of 2001 to cover potential glacial dispersion paths for the kimberlite minerals.

In 2001, the Ontario Geological Survey included Parkman Township in a regional heavy mineral exploration project. The results of the project further verified the presence of kimberlite minerals on the Parkman Property.

In the fall of 2001, P. Wood of JML Resources Ltd. collected 5 heavy mineral samples from the vicinity of Green Creek. The work was conducted on behalf of Mustang Minerals. SGS Lakefield Research identified 138 pyrope garnets, 191 chromite, 14 chrome diopside and 46 ilmenite.

In April of 2002, Lee Barker of Spartan Resources Inc. examined untested kimberlite minerals in samples RNT 023 and RNT 028, collected in November of 1999. Barker noted the preservation of kelyphitic rims and "orange peel textures" on some pyrope garnets and suggested it was evidence indicating the kimberlite minerals are derived from local sources. An additional 61 kimberlite minerals were identified using the microprobe at facilities of R.L. Barnett Geological Consulting Ltd.

Marmont and Thomas staked an additional 16 claims (224 units) between May and October of 2002.

-13-

On July 11, 2002, Grenville Gold Corporation entered into option with the property owners to gain a 6007o working interest in the Parkman Property. At the time, the property consisted of 314 units in 23 claims covering a total area of 5,024 hectares.

In July 2002, Marmont completed an air photo interpretation survey of the Parkman Property for Grenville Gold. Marmont identified several orientations of topographic lineaments possibly representing faults crossing the property. Northwest and northeast trending lineaments were identified in the vicinity of the Green Creek kimberlite mineral anomaly. The northwest lineaments are believed to be faults associated with the Lake Timiskaming Structure.

Marmont and Thomas staked an additional claim (12 units) in October 2002. The property now consisted of 24 claims (328 units) and covered an area of 5,248 hectares.

In the fall of 2002, J. Laidlaw and C. Marmont collected forty-two 10 kg gravel samples from the Parkman Property on behalf of the Grenville Gold Corporation. Some of the samples were used for pebble analyses in an effort to deduce glacial transport distances and apply the results to locate potential sources of the kimberlite minerals. Using pebble fragments from local sources, it was determined transport distances were local and ranged 1 - 2 kilometres. During the field work, several thin lamprophyre dikes striking 900 to 1250 and 1550 were found in bedrock. Similar lamprophyre pebbles are reported to have been found in Green Creek about 700 to 1100 metres south of the outcropping dikes. Petrographic and geochemical analyses of samples revealed the dikes are composed of olivine-phlogopite-diopside and show a slight Cr-Mg enrichment but below that of typical kimberlite. It was concluded the dikes were not the source of the kimberlite minerals.

In December 2002, Overburden Management processed the forty-two gravel samples for kimberlite indicator minerals and gold. Four samples from Green Creek were estimated to contain greater than +100 kimberlite grains. A second kimberlite anomaly was detected in the Big Webb Lake area. Rosterite olivine was identified with the kimberlite minerals. Olivine erodes easily and has very short transport distances. The results suggest there are potential kimberlite sources in the Big Webb Lake area. Samples from Green Creek also contained flakes of gold, traces of chalcopyrite and gahnite grains possibly derived from the local iron formation. A population of Zn~ chromites and ilmenite were identified and are potential indicator minerals of Wawa style diamond- lamprophyre. Diamond-lamprophyre occurs in the Lake Timiskaming Structure south of New Liskeard. The discovery of Zn-chromite suggests diamond-lamprophyre may occur in the area of the Parkman Property.

An aeromagnetic-electromagnetic VLF survey was completed over the Parkman Property in March, 2003. The survey outlined the extent and folding of the iron formation on the property. The survey detected 28 magnetic features possibly representing kimberlite pipes. Eighteen of the features are situated within the current claim boundary.

On December 11 th 2003, Intrepid Minerals Corporation of Toronto, Ontario was granted an option to gain a 5007o working interest in the metals portion of Grenville's interest in the property. The metals portion of the agreement excludes diamonds and all other precious or semi-precious stones.

In 2003, Intrepid Minerals drilled 557 metres with a 5 hole program. The program tested base metal and gold potential in areas proximal to the Cook and Webb Lake Zones. Best assays

-14-

came from Hole POOS and include a 1.5 metre interval assaying 0.018 ppm Au adjacent to a 1.83 metre interval of "mafic breccia" assaying 599 ppm Zn. A lower section in the hole assayed 634 ppm Cu across 1.04 metres and an adjacent sample assayed 348 ppm Cu across 1.36 metres. The hole was collared northeast of the Cook Zone. The drill program identified a number of lamprophyre dikes described as feldspar-garnet-pyroxene lamprophyre, heterolithic breccia and mafic breccia. The slight enrichment of Zn in mafic breccia rock could suggest an association of some lamprophyre on the property to the Wawa style diamond-lamprophyre.

By the beginning of 2004, Intrepid Minerals had successfully completed the option agreement and currently holds a 5007o working interest in the metals portion of the Parkman Property.

II. SURVEY RESULTS

LOGISTICS

During this survey, 11 bulk gravel samples were collected on the Parkman Property. The samples consisted of 10 modern alluvium samples and 1 sample of glacial-fluvial material.

Table 2 outlines the process of deriving heavy mineral concentrates from the bulk samples. At each sample site, 2.5 litres or the equivalent of 25 kilograms of bulk material was collected.

Heavy mineral concentrates used for kimberlite exploration consist of material ranging -1.0 to 0.18 mm in size and are based at a specific gravity (sp.g.) of 3.0 glee. Silt size fractions used for gold exploration range below 0.18 mm in size. Lithium metatungstate was used to concentrate the minerals of +3.0 sp.g.

Heavy mineral samples were examined by the author using a binocular microscope at the facilities of Arjadee Prospecting in Mount Brydges, Ontario. A total of 1,410.9 grams of material was examined.

Mineral grains were analyzed by an electron microprobe at facilities of R. L. Barnett Geological Consulting Inc. at Lambeth, Ontario. Compositions of the mineral grains determined by the microprobe are appended to this report.

Kimberlite - Diamond

Sample locations and the amount of kimberlite minerals observed in the heavy mineral concentrates are summarized in Figure 7. Nine samples were collected in Green Creek where high concentrations of kimberlite minerals have been reported. A separate sample was collected in a small stream feeding Green Creek and another sample was collected from a road cut beside the main access road on the property.

-15-

Table 2.Process of Heavy Mineral Concentration

1.) Bulk sample: 20 kg, 2.5 litres, unsorted-standard sample size.

2.) Screening on site to derive -1.0 mm fraction.-reduce sample volume for transport.

3.) Concentration of minerals using cable jig.-produces crude heavy mineral concentrate at any desired specific gravity.-removes silt fraction by screening.-silt fraction saved for examination.-light minerals discarded.

4.) Concentration by density liquid: lithium metatungstate.-refines concentrates to minerals with specific gravity of +3.0.-light minerals (-3.0 sp.g.) discarded.

5.) Remove magnetic and paramagnetic minerals from concentrates.-kimberlite minerals have a tendency to be non-magnetic.-magnetic fractions are weighed and stored.

6.) Heavy mineral concentrate examination.-examine heavy mineral concentrates using a binocular microscope and select potential kimberlite minerals.-examine grain surface features to determine transport distances.-count minerals and determine grain count estimates for abundant minerals.-select non-kimberlite minerals: gold and sulphides.

7.) Kimberlite mineral analyses.-determine kimberlite mineral compositions using an electron microprobe.

8.) Data Processing and Interpretation-compare microprobe data with known kimberlite mineral data to determine total kimberlite mineral counts.-determine diamond potential of source based on mineral compositions.

- 16-

3?? 2 -i

GLACIALADVANCE

V

X

RJDB 3.1.3MT 25 36, 2, 73 OL ——l—————"^ Cr AndUDft 5.0.1 J .x-'CrGrRNT24 33. 3. 1069. GC-2 14,S.***OL

CCM29 2,0,30,3 l\ l /lZTM.i-muVCrAnd H

.RNT23 27. 4. 583. GC~* 38. l.-CCH M 0.0. D

RNT26 31.4. 1SO OL

' PJD 10 9,1, 6 RR

•1 3,1, *39RJD 2 5, 3, 3 D1 12,2,1*UV G10 T 29 72, t, M19 OL, LP, RR

• CCU6B fi. 0.15RJD 3 7,2,4 RJD 4 5, O, 3 UV RNT 1 O, 0.1 . RWT 2 2.0. 5, GC-5 24. 2, +T7

RKT29 40.2.273 s CCH 58 1. ft 10 COM2 14. 1.4M -

cai67 4.1.10 y — \V17.0.636 RJD5 4,0,2

O 14,0,133 RJD 6 3,0,0 , RJD 7 2.0.8. UV , -~/-

t9 11.1.37RR.IP ' "^ 73 411,13

CCH 10 IB. 0.81

RNT30RMT 27 27.1,

CCU18

RJD 11CCM2S 3.

RJD 10Heavy Mineral

Sample Site

Marmont 2000. 2002 Hearst 2003 Veiltetfe 1986

CCM 25^7.2,11

pyrope Cr diopside KIM EsU Total

OL

RR

LP

X

sCr And

CrGr

uv

Alluvium Sample

Till Sample. Outwash Sample

Olivine in concentrate

Reaction Rims on pyrope

Lamprophyre pebbles in concentrate

Lamprophyre in outcrop or drill core

Aeromagnetic or Ground Magnetic Feature

Fault, interpretted from aeromagnetic data

Chrome Andradite Garnet

Chrome Grossular Garnet

Uvarovite Garnet

Figure 7.

SAMPLE LOCATIONS AND RESULTS PARKMAN PROPERTY

AMITA-GREENFIELD RESOURCE - GRENVILLE GOLD CORPORATION

Parkman, Wyse and McAuslan Townships Sudbury Mining District, Ontario, Canada

-17-

Kimberlite minerals were found in all 11 samples collected by the author (Table 3). The minerals consist of:

1.) large (xenocrystic) mantle-derived nodules or pellets and fragments of pyrope, chrome diopside, chromite, picroilmenite and phlogopite mica.

2.) abundant minute grains of chromite and ilmenite presumed to be derived fromkimberlite matrix material. The frequency of these grains increases significantly with decreasing grain size and in the most part, chromite is the main component of the high mineral counts. The grains occur as tiny spheres or pellets and well-preserved octahedral crystals ^.5 mm in size.

3.) eclogite garnet and clinopyroxene from kimberlite.

The electron microprobe determined the compositions of 134 kimberlite minerals (Figure's 8 S 9). The kimberlite minerals include: 57 pyrope garnet, 8 chrome diopside, 36 chromite, 14 picroilmenite, 3 uvarovite garnet, 3 phlogopite and 13 eclogite garnet and clinopyroxene.

Pyrope garnet populations are derived mostly from lherzolite (G9) paragenesis and partially from the sub-calcic harzburgitic (G10) paragenesis associated with diamond. This survey identified 2 sub-calcic pyrope garnets (G10). Uvarovite was also identified. Uvarovite is a rare green Cr-Ca garnet sometimes found in kimberlite.

There are several populations of clinopyroxene in the area:

1.) Bright green chrome diopside from a kimberlite source,2.) Gr augite from lamprophyre.3.) Na augite potentially from eclogite paragenesis.4.) Augite from local crustal source.

The chrome diopside grains identified by this survey were all found with pyrope garnets. The compositions have Cr:Na ratios characteristic of kimberlite. Chrome diopside with elevated (*207o) Na2O and Cr2O3 are trends commonly found with diamond paragenesis. This survey identified 5 chrome diopside with compositions akin to potential diamond paragenesis.

In the heavy mineral concentrates from Green Creek, chromite is the most abundant "kimberlite" mineral. In most samples from the creek, there is a tremendous amount of small octahedral crystals and pellets ^.5 mm in diameter. The minerals form a major component of the silt fractions in samples: RJD-04-1, RJD-04-02, RJD-04-03, RJD-04-04 and RJD-04-10. Microprobe analysis indicates some of the minute crystals are Ti-chromite derived from kimberlite and probably represent groundmass material. Xenocryst fragments of chromite have compositions overlapping kimberlitic and non-kimberlitic sources. There is a small population of xenocryst fragments approaching compositions comparable to chromite inclusions in diamond. During this survey, only a small number of chromite grains were selected for microprobe analyses and most were large grains representing the macrocrystic-xenocryst population.

-18-

Table 3.Results of Heavy Mineral SamplingParkman PropertyAmita-Greenfield Resources - Grenville Gold Corporation

Sample Number

RJD-04-01

RJD-04-02

RJD-04-03

RJD-04-04

RJD-04-05

RJD-04-06

RJD-04-07

RJD-04-08

RJD-04-09

RJD-04-10

RJD-04-11

UTM NAD27

635074E 5185780N

635037E 5185768N

635005E 51 85761 N

634980E 5185735N

634773E 51 85231 N

634669E 5185149N

634673E 5185134N

6351 97E 5186846N635243E 5186698N

635274E 5186382N

632597E 5184682N

Type

Alluvium

Alluvium

Alluvium

Alluvium

Alluvium

Alluvium

Alluvium Feeder creek with water falls

Alluvium

Alluvium

Alluvium

Glacial- fluvial outwash

4 1 mm Field weight

2.5kg

3.1kg

0.9kg

1.2kg

5.2kg

2.6kg

1.9kg

3.1 kg

2.2kg

3.5kg

5.4kg

<'\ mm +S sp.g.

HMC

220.0 g

254.3 g

153.6 g

139.9 g

195.5 g

204.9 g

138.9 g

176.9

235.3 g

271 .8 g

85.7g

Magnetic fraction

62.1 g

89.5 g

50.2 g

45.6 g

62.2 g

76.9 g

59.4 g

52.4 g

56.1 g

104.1 g

17.4 g

t 0.18 mm *3 sp.g. HMC Examined

157.9 g

164.8 g

103.4 g

94.3 g

133.3 g

138. 0 g

79.5 g

124.5 g

179.2 g

167.7 g

68.3 g

Pyrope

12

5

7

5

4

3

2

3

5

9

1

Gr CPX

2

3

2

0

0

0

0

1

0

1

0

Chromite

16

2

4

2

1

0

2

2

1

4

1

Cr-Mg ilmenite

3

1

0

1

1

0

6

1

0

1

0

Comments

2-3^0 minute chromite octahedral crystals and pellets, 2 G10 pyrope, 1 uvarovite garnet, 1 eclogite cpx. 2 gahn te. 2 Cr augite (cpx). 3.4 KIM's/ g2-30/!) minute chromite octahedral crystals and pellets. Several phlogopite. 2 Ca-Mg almandine. Shagreen on pyrope.1 uvarovite. Decreasing chromite. Large granite gneiss blocks in area. Clear- blue kyanite, spessartine.Calcite reaction rim on pyrope pellet. Good shagreen preservation. Several "fresh" fractured xenocrysts and pellets. Decreasing chromite. 1 Na cpx, 1 Ca-Mg almandine. 3 gahnite.Abundant "fresh" IF grains. Staurolite. 1 Na cpx, 1 Ca-Mg almandine. 1 apatite.If grains. 1 uvarovite. 2 Ca-Mg almandine, 1 Na cpx. 1 apatite.Abundant fresh IF grains, staurolite and garnet crystals. Large picroilmenite and chromite, slightly chipped pellets, good shagreen preservation.2 Cr augite, 1 Na cpx. Epidotite.Increasing minute chromite octahedral crystals. 1 gold grain flat 0.8x0.5 mm.2qtz- malachite.2-3^0 minute chromite octahedral crystals. Calcite reaction rim on pyrope pellet. Several pellet shaped pyrope!. Good shagreen preservation. Abundant IF minerals.Rock fragments of potential phlogopite lamprophyre. Fresh rusty dolomite?, pelilic schist rock fragments. 2 apatite, 1 Ti magnetite. 1 chlorite. 1 Cr augite.

- 19-

Cr2O3 (DXowl.)

Cr2O3

m

10

Overlap Field

G10 Harzburgite Field

N64

Pyrope

G9Lherzolite Field

Eclogite and crustal garnet

46

CaO

10 12

Jadeite - Eclogite Trend

N23

Chrome Diopside

Na2O

Source; Marmont 2003

i

Q Range of Historic Analyses

9 Arjadee Prospecting 2004

Figure 8.

PYROPE - CHROME DIOPSIDE PARKMAN PROPERTY

AMITA-GREENFIELD RESOURCES - GRENVILLE GOLD CORPORATION

Parkman, Wyse and McAusla Townships Sudbury Minig District, Ontario, Canada

-20-

Cr2O3CM.wt.) 50Field Unique to Kimberlite 8. Lamproite

30

20

Cr2O30X.wL) 3

6 8 10 12 14 16

Source: Marmont 2003

O Range of Historic Analyses

0 Arjadee Prospecting 2004

Chromite

Ilmenite

Figure 9.

CHROMITE - ILMENITE PLOTS PARKMAN PROPERTY

AMITA-GREENFIELD RESOURCES - GRENVILLE GOLD CORPORATION

Parkman, Wyse and McAuslan Townships Sudbury Mining District, Ontario, Canada

-21-

Microprobe analysis of ilmenite xenocrysts indicates there is a good population of (Cr-Mg) picroilmenite in the Parkman kimberlite mineral anomaly. The compositions indicative of a reduced, rapid kimberlite emplacement and favorable conditions prevailed for diamond preservation during transport.

Heavy mineral concentrates from the Parkman Property contain eclogite garnet and clinopyroxene. Most of the eclogite minerals consist of Ca-Mg almandine garnet and Na augite. A single pyrope eclogite garnet was found during this survey which has a composition associated with diamond eclogite paragenesis. There is also a small population of Cr-Ti pyrope eclogite garnets reported in the historical data.

Traces of large phlogopite grains up to 1 cm in diameter were found in several samples containing kimberlite minerals. The most phlogopite, 6 grains, occur in sample RJD-04-10. The phlogopite grains could be macrocrysts and xenocrysts derived from a kimberlite or similar rock types. Such large grains do not survive well during transport and probably reflect a source situated close to Green Creek. Phlogopite was also found with pyrope and chromite in a glacial-fluvial outwash sample: RJD-04-11, taken south of the B-8, B-9 and B-12 magnetic targets.

During grain selection, the author noted some preservation of certain physical features indicating the kimberlite minerals could be derived from local sources. Calcite reaction rims were partially preserved on the faces of two pellet-shaped pyrope garnets found at different locations. The author also observed the grain surfaces of many of the kimberlite minerals with well-preserved shagreen texture (orange peel texture). Some of these grains are complete non-fractured pellets and many are "fresh" fragments derived by simple, primary fracturing of much larger grains. The best preserved textures were seen in samples: RJD-04-04 and RJD-04-10. Well-preserved shagreen texture was evident also on large picroilmenite xenocrysts found in sample RJD-04-07 taken from a small creek draining into Green Creek.

Iron Formation Minerals

All the heavy mineral concentrates collected by the author contain minerals derived from the local iron formation and surrounding rock units. Minerals associated with the iron formation include: magnetite, ilmenite, pyrite, limonite pellets, pyrrhotite, rutile and gahnite. Some of the minerals increase in frequency in the up-stream direction of Green Creek. In particular, samples: RJD-04-05, RJD-04-06 and RJD-04-07, collected close to the Green Lake Iron Formation, all contain "fresh" iron formation minerals with some degree of crystal preservation. Even though it is not exposed, the preservation of the grains clearly represented the presence of iron formation in the immediate area. Sample RJD-04-10 also contains abundant and moderately fresh iron formation minerals.

Other minerals observed in abundance in the heavy mineral concentrates and which appear to be locally derived include: clear-blue kyanite, orange staurolite, orange and yellow almandine and spessartine garnet, green K feldspar, brown sphene and tourmaline. Fresh- angular kyanite and yellow garnet occur with kimberlite minerals through samples RJD-04-01 to RJD-04-04. Well- preserved subhedral orange staurolite crystals and euhedral orange garnet crystals occur with iron formation in samples RJD-04-05 to RJD-04-07. Some staurolite crystals in sample RJD-04-07 were observed in composite with white feldspar and suggest the grains are derived from a source proximal to the sample. Several coarse grains of green K-feldspar were observed in most of the

-22-

samples taken from Green Creek. Several fresh K-feldspar grains are present in samples: RJD-04- 05, RJD-04-06 and RJD-04-10.

Gold

At the time of this report, the author has examined four of the silt size fractions (-0.18 mm) derived from the heavy mineral concentrates. Gold grains were found in samples: RJD-04-09 and RJD-04-10. Both samples were taken in Green Creek in the vicinity to the apparent location of the Net Lake Fault.

Sample RJD-04-09 contains a large gold grain measuring 0.8 x 0.4 x 0.05 mm in size. The sample was collected at the location of historic sample: 99-RNT-24 which is reported to contain 98 gold grains (Marmont, 2000). The sample taken by the author also contains two silicate grains weakly coated in malachite.

Four gold grains were found in sample RJD-04-10. All the grains are smaller than 125 microns. Two of the grains partially retain some pristine features suggesting some of the gold flakes could be locally derived. Sample RJD-04-10 also contains abundant fresh iron formation minerals such as pyrite, ilmenite and magnetite.

General Composition of the Heavy Mineral Concentrates

Table 4 outlines the general composition of the heavy mineral concentrates. The data (RJD- 04-1 C) was derived from the analysis of 150 mineral grains indiscriminately selected from 5 grams of +3.0 sp.g. concentrate of sample RJD-04-1. This particular sample was collected at the same location as RNT 28 which is reported to contain an estimated *6,600 kimberlite minerals. The high concentration of kimberlite minerals in the area is reflected in the grain count. The concentration of kimberlite minerals at this particular site ranges 3.4 Kimberlite Minerals per gram in the -1.0 to 0.18 mm, +3.0 sp.g. fraction. Other minerals which occur in abundance in the concentrate but were not: selected during the count include: kyanite, staurolite and minerals related to the iron formation such as pyrite and limonite.

III. DISCUSION OF RESULTS

Kimberlite Minerals

The heavy mineral samples collected by the author contain good concentrations of kimberlite indicator minerals and the results of this investigation correlate well with historic results.

Microprobe analysis of the kimberlite minerals has shown approximately 60Xo of the xenocryst population (pyrope, chromite, chrome diopside and olivine xenocrysts) has formed under harzburgite paragenesis favorable for diamond crystallization. The Parkman kimberlite mineral anomaly also contains eclogite garnet and clinopyroxene. Several pyrope eclogite garnets have been found which are known to be associated with diamond eclogite paragenesis. The presence of harzburgite minerals and diamond-eclogite garnet are indications that diamond could be found in the kimberlite sources of the minerals.

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Table 4.General Composition of the Heavy Mineral ConcentratesParkman Property

Minerals selected from sample: RJD-04-01 Data Set: RJD-04-1C

150 Grain CountMineral Type^-^Common IlmeniteCommon MagnetiteAlmandine GarnetBlack AmphiboleChromiteSpessartine-AlmandineEpidoteTi MagnetiteQuartzSpheneFe clinopyroxene (augite)ChloriteLost GrainsNa AugitePyrope GarnetPlagioclaseGrossular-AlmandineGrossular-AndraditeRutilePicroilmeniteUvarovite GarnetChlorite H- IlmeniteGreen K FeldsparZn Spinel (Gahnite)Melanite (Ti andradite)AcmitePyrope-Almandine

Number of Grains30271514

97544443332222211111111

150

Potential SourceIron FormationIron FormationMetasedimentary UnitsMetasedimentary UnitsKimberlite, lamprophyre, peridotiteMetasedimentary gneissesGranite gneissKimberliteQuartz veins, hydrothermal zones, graniteLamprophyre?Mafic metavolcanic unitsSheared mafic metavolcanic schistsMica?Eclogite?KimberliteGranitic gneissMetasedimentary gneissMetasedimentary gneiss?Iron formation?KimberliteKimberlite, serpentiniteAltered/sheared mafic metavolcanic?Iron formationIron formationLamprophyre, serpentinite, alkaline igneous unitsLamprophyre, alnoiteEclogite?, metasedimentary units

-24-

The anomalous concentration of kimberlite minerals on the Parkman Property is comparable to the concentration of minerals one would expect in close proximity to a kimberlite source. Concentrations of kimberlite minerals similar to the Parkman anomaly have been detected by others including the author during studies of grain dispersion from kimberlite sources in complex glaciated environments. Preservation of crystal shapes and un-eroded magmatic features on grain surfaces provide some additional evidence the Parkman anomaly may be derived from local kimberlite sources. Furthermore, gravel samples collected for pebble analysis contain abundant minerals and rock fragments from geological units underlying the property and indicate that, regardless of the glacial and post glacial history, a portion of the overlying sediments is locally derived.

The depth of overburden on the property has been the main inhibiting factor in mineral and kimberlite exploration on the property. The Parkman Property is mostly covered by a thick sequence (40-50 m) of outwash material consisting of sandy gravel and cobbles overlying older till horizons and bedrock. The till was deposited during 2 or 3 events by a single glacier shifting its advance from the northeast to the north-northwest. During deglaciation, a split in the glacier occurred and became a major southwest flowing spillway as the glacier melted. The glacial-fluvial event resulted in the formation of the Harricana - Lake Mcconnell Moraine. The author suspects the strongest concentration of kimberlite minerals occur in a section where Green Creek has eroded through the thick layer of outwash material and into older till horizons and bedrock.

The kimberlite minerals in Green Creek could be derived from the erosion of a kimberlite by Green Creek. The aeromagnetic survey over the area by Grenville Gold Corporation detected two subtle magnetic features situated close to the Green Lake Zone iron formation and immediately up stream from the Green Creek kimberlite mineral anomaly. Samples RJD-04-04 and RJD-04-07, collected close to these magnetic targets, contain good quantities of xenocrysts with well-preserved magmatic surface features.

If the kimberlite minerals are derived by glacial erosion, the creek could be crossing a strong dispersion trail and likely sources for the kimberlite minerals would be situated in the northeast to northwest direction from the creek. In the New Liskeard area, which underwent similar glacial events, studies found the direction of dispersion was a common vector of the three glacial events. If so, potential kimberlite sources on the Parkman Property would be situated north to north-east from Green Creek. If the third glacial thrust occurred over the property and eroded to bedrock, then kimberlite targets could be situated northwest of the creek. The author believes this event has occurred since sample RJD-04-10 contains a good population of "fresh" iron formation grains and was collected at some distance east of known iron formation units. This particular sample also contains grains of marble which could be derived from a marble unit reported in the north region of the property and situated in a northwest direction to Green Creek.

Sample RJD-04-07 was collected in a small creek draining into Green Creek. The sample site is at an elevation of approximately 10 metres above the bed of Green Creek. The creek is fast and characterized by small waterfalls and potentially could be eroding to bedrock or a younger till horizon at some location upstream from the sample site. Well-preserved crystals of staurolite and garnet were found with abundant iron formation minerals in sample RJD-04-07 and provide some evidence that a large component of the heavy mineral concentrate is derived from the immediate area. The sample also contains a good population of xenocrystic picroilmenite and chromite. The ilmenite grains occur as moderately well-preserved pellets with good shagreen preservation. This

-25-

sample appears to contain a significantly higher picroilmenite population relative to the abundance of chromite. This is in contrast to the kimberlite indicator mineral anomaly in Green Creek. The author suggests the kimberlite minerals in sample RJD-04-07 could be derived from a different source than the kimberlite minerals found in Green Creek. A topographic feature is situated upstream from the sample site and could represent a source for the picroilmenite. If the creek is eroding a younger till horizon, a source could be situated in the north-northwest direction from the sample site.

A small quantity of kimberlite minerals were found in Sample RJD-04-11. The sample was taken in glacial-fluvial material and was found to contain locally derived schistose rock fragments and small siliceous, Fe-carbonated rock fragments. Final stages of glaciation and deglaciation (glacio-fluvial) could have dispersed kimberlite minerals from targets situated north and northwest from the sample site. The magnetic features: B-8, B-9 and B-12 are good candidates for sources of the kimberlite mineral grains.

During this survey, all pyrope garnets and chrome diopside observed in the heavy mineral concentrates were selected for microprobe analyses. The emphasis on selecting these grains was partially motivated by the ease of identification during grain selection in combination with the reliability or certainty that pyrope garnet and chrome diopside are derived only from a kimberlite source. Although chromite and to a lesser extent ilmenite, appear to be the most abundant kimberlite minerals in the samples, the minerals were mostly ignored during grain selection since the microprobe data indicates the Parkman kimberlite anomaly contains chromite and ilmenite from both kimberlitic and non-kimberlitic sources. During this survey, most of the chromite and ilmenite selected for microprobe analysis consisted of large grains (+0.5 mm) believed to represent xenocrysts from kimberlite. Several small octahedral crystals and pellets of chromite and ilmenite were analyzed from sample RJD-04-01 and included in the grain count RJD-04-1 C. With the exception of one Ti-chromite, most of the octahedral crystals of chromite were found to have compositions "overlapping" with kimberlitic and non-kimberlitic sources. In addition to kimberlite, potential sources could include such rock types as lamprophyre and peridotite. Ten metallic pellets selected from the silt size fraction of RJD-04-01 were found to be composed of simple ilmenite (RJD-04-1 B) and of little importance to diamond exploration.

Iron Formation

In addition to the anomalous concentration of kimberlite minerals, heavy mineral concentrates contain abundant minerals derived from (or potentially derived from) the iron formation on the property. Important minerals found by heavy mineral prospecting include: gahnite, chalcopyrite and gold. The minerals provide credence to the existence of Broken Hill and Osbourne type deposits by providing some evidence that the Tyrell Iron Formation or sites along the structure could host Zn-Cu-Au mineralization. The Green Lake Zone appears to hold the best promise of Zn- Cu mineralization. Moderate concentrations of gahnite and chalcopyrite have been found in Green Creek which flows close to and down-ice from the zone. Results of soil surveys over the zone also support this and enhance the Green Lake Zone as a potential drill target for a future program.

A large component of the iron formation in the area is composed of magnetite, ilmenite and pyrrhotite. Heavy mineral concentrates contain strong quantities of magnetite and ilmenite and in part, reflect the presence of iron formation in the area. During the process of concentrating kimberlite minerals, most of the magnetic minerals such as magnetite, ilmenite and pyrrhotite are

-26-

removed from the concentrates and ignored during the kimberlite mineral selection stage. A better understanding of the iron formation on the property may be gained by performing a multi-element assay on the magnetic fractions derived from each of the heavy mineral concentrates collected on the property.

Gold

Most of the gold grains found in heavy mineral concentrates from the property are considered to be reshaped or modified signifying the grains have traveled an unknown distance from source. During deglaciation, the outwash channel represented by the Harricana - Lake Mcconnell moraine extended between the property and the two prominent gold mining districts of Val D'or and Belleterre, Quebec. It is possible some gold from these regions has been transported to the Parkman Property by glacial fluvial processes. A small population of pristine gold grains found on the Parkman Property does provide some evidence of local sources. The brittle and ductile nature of the iron formation and surrounding units when subjected to extensive folding and faulting can provide structural environments and traps for gold-bearing solutions similar to those forming Osbourne type gold deposits. The Grenville Province has many different occurrences of gold associated with several gold-bearing events. The Parkman Property has suitable rock types, structures and comparative age to known gold deposits found locally and worldwide.

On the property, the majority of gold grains have been found in samples collected close to the Net Lake Fault. During this survey, several pristine-modified grains were found in sample RJD- 04-10 which was collected very close to the fault. This particular sample also contains fresh iron formation minerals including cubic pyrite crystals from a local source.

lil. CONCLUSIONS AND RECOMMENDATIONS

The Parkman Property covers a comparatively significant kimberlite mineral anomaly situated within a regional fault structure which hosts several kimberlite fields. The compositions of the minerals determined by an electron microprobe indicate some of the kimberlite minerals have crystallized under mantle conditions conducive for diamond growth. Preservation of magmatic features on a good tenor of the mineral grain surfaces in combination with the presence of easily eroded minerals such as fosteritic olivine and abundant minerals and rock fragments eroded from local geological units suggest the kimberlite minerals are potentially derived from local sources also. The results of this survey and of previous heavy mineral surveys on the property indicate further exploration for kimberlite and diamond is warranted.

Heavy mineral surveys also provide evidence of possible gold-zinc-copper mineralization occurring on the property. The iron formation and faults cutting through the property are structures where precious and base metal mineralization could occur. Additional exploration of these structures for gold and base metals is recommended.

Further diamond exploration on the Parkman Property should focus on exploring the aeromagnetic and ground magnetometer features suspected of representing kimberlite structures such as pipes. A program combining further ground magnetometer surveys with heavy mineral sampling, soil surveys and geological mapping is recommended. The results should provide adequate data for prioritizing and testing the geophysical features by an eventual diamond drill program.

-27-

Gold and base metal testing of the iron formation and fault structures on the property should consist of performing local ground VLF-electromagnetic surveys with a combination of heavy mineral, soil and geological surveys similar in technique to those used for diamond exploration. Gold and base metal exploration may also benefit by performing multi-element assays on all magnetic fractions derived from the heavy mineral concentrates collected on the property.

A budget to further testing the gold, base metal and diamond potential of the Parkman Property prior to diamond drilling includes:

Heavy Mineral Survey 100 samplesSoil Surveys (MMI, Humus and "B" Horizon)AssaysGround Magnetometer and VLF-EM Surveys

S20,00025,000

5,00025.000

875.000

Respectfully submitted,

. (Diffman

Robert J. Dillman P. Geol. Arjadee Prospecting

November 12, 2004

-28-

REFERENCES

GSC. 1965. Map 1479 G , Temiscaming; Aeromagnetic map. Scale 1: 63,360.

GSC. 1965. Map 1480 G, Ottertail Creek; Aeromagnetic map. Scale 1: 63,360.

GSC. 2002. Kimberlite Indicator Mineral Content and Geochemistry of Till Around the Peddie Kimberlite, Lake Timiskaming, Ontario. Open File 4262

Hearst, R. 2003. Interpretation of Airborne Geophysical Data, Parkman Property, Ontario. Grenville Gold Corporation.

Laronde, D., 2003. Ground Geophysical Surveys, Magnetometer Survey, Assessment Report, Parkman Township. Meegwich Consultants Inc. for Grenville Gold Corp.

Lumbers, S.B., 1971. Tomiko Area, East Half. Ontario Department of Mines, Map P.679. Scale 1: 63,360.

Marmont, C.M., 1999. Exploration Proposal for Broken Hill Type Ag-Pb-Zn andOsborne- Type Au-Cu Deposits, Parkman Township Property, Tomiko Terrane, Grenville Province, Ontario.

Marmont, C.M., 2000. Report on Geochemical Surveys: Technical Report, Parkman Township Property, Sudbury Mining District, Ontario. Ontario Prospectors Assistance Program Grants: OP-99-204 and OP-99-205. Volume 1 of 3.

Marmont, C.M., 2000. Report on Geochemical Surveys: Data Interpretation, Parkman Township Property, Sudbury Mining District, Ontario. Ontario Prospectors Assistance Program Grants: OP-99-204 and OP-99-205. Volume 2 of 3, Appendices 1 to 13.

Marmont, C.M., 2000. Report on Geochemical Surveys: Certificates of Analysis and Lab Reports, Parkman Township Property, Sudbury Mining District, Ontario. Ontario Prospectors Assistance Program Grants: OP-99-204 and OP-99-205 Volume 3 of 3, Appendices 14 to 22.

Marmont C.M., 2002. Assessment Report on Pebble Analysis of Alluvium and TillSamples, And Petrology and Geochemistry of Lamprophyre and Syenite Dikes, Parkman Township Property, Sudbury Mining District, Ontario.

Marmont C.M., 2002. Report on Microprobe Analysis of Kimberlite Indicator minerals, Parkman Township Property, Mining Claim 1174500, Sudbury Mining District, Ontario.

Marmont C.M., 2002. Assessment Report on Air Photo Interpretation and Bulk Alluvium and Till Sampling and Quaternary Mapping, Parkman McAulsan and Wyse Townships, Sudbury Mining District, Ontario.

-29-

References Con't

Marmont C.M., 2002. Assessment Report on Pebble Analysis of Alluvium and TillSamples, And Petrology and Geochemistry of Lamprophyre and Syenite Dikes, Parkman Township Property, Sudbury Mining District, Ontario.

Terraquest Ltd., 2003. Operations Report: High Sensitivity Magnetic Airborne Survey, Parkman Property, Parkman Township, Ontario.

Veillette, J. J. 1986. Former Southwesterly Ice Flows in the Abitibi-Timiskaming Region: Implications for the Configuration of the Wisconsinan Ice Sheet; Canadian Journal of Earth Sciences, Vol. 23 pp. 1724-1741.

-30-

CERTIFICATE

l, ROBERT JAMES DILLMAN, do hereby certify as follows:

[1 .] l am a Mining Exploration Geologist and that l reside and carry on business at 8901 Reily Drive, in the town of Mount Brydges, Ontario.

[2.] l have graduated in 1992 from the University of Western Ontario with a Bachelor of Science Degree and majored in Geology.

[3.] l have been practicing my profession as a Professional Geologist since 1992.

[4.] l am a Licensed Prospector in Ontario and have been actively engaged as a Professional Prospector since 1978.

[5 ] My report, dated November 12, 2004, titled: "REPORT OF HEAVY MINERAL SAMPLING ON THE PARKMAN PROPERTY, PARKMAN, WYSE 8, MCAUSLAN TOWNSHIPS', ONTARIO. GRENVILLE GOLD CORPORATION -AMITA-GREENFIELD RESOURCES INC." is based on information collected by myself between September 16, 2004 and November 12, 2004. Any other information which has been gathered from additional sources has been cited in this report.

[6.] The information given in this report is as accurate as to the best of my knowledge and l have not stated false information for personal gain.

[7.] l authorize the use of this report or any part of if proper credit is given to the original author.

[8.] l have no monetary interest in the Parkman Property nor in any company associated with the Parkman Property.

[9.] l am a member of the Canadian Institute of Mining.

[10.] l am a member of the Association of Professional Geoscientists of Ontario, APGO No. 530.

ROBERT JAMES DILLMAN, B.Sc. GEOLOGIST

Dated at Mount Brydges, Ontario This 12th day of November, 2004

-31 -

Electron Microprobe Results Parkman Property, Ontario

Pyrope Garnet1 RJD-04-012 RJD-04-013 RJD-04-014 RJD-04-015 RJD-04-016 RJD-04-017 RJD-04-018 RJD-04-019 RJD-04-0110 RJD-04-0111 RJD-04-0112 RJD-04-0113 RJD-04-0214 RJD-04-0215 RJD-04-0216 RJD-04-0217 RJD-04-0218 RJD-04-0319 RJD-04-0320 RJD-04-0321 RJD-04-0322 RJD-04-0323 RJD-04-0324 RJD-04-0325 RJD-O4-0426 RJD-O4-0427 RJD-04-0428 RJD-O4-0429 RJD-04-0430 RJD-04-0531 RJD-04-0532 RJD-04-0533 RJD-O4-0534 RJD-04-0635 RJD-04-0636 RJD-O4-0637 RJD-04-0638 RJD-04-0739 RJD-04-0740 RJD-04-0841 RJD-04-0842 RJD-04-0843 RJD-04-0944 RJD-04-0945 RJD-04-0946 RJD-04-0947 RJD-04-0948 RJD-04-1049 RJD-04-1050 RJD-04-1051 RJD-04-1052 RJD-04-1053 RJD-04-1054 RJD-04-1055 RJD-04-1056 RJD-04-1057 RJD-04-11

lherzolitelherzolitelherzolitelherzolitelherzolitelherzoliteHarzburgitelherzolitelherzoliteHarzburgitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolitelherzolite

Eclogite Garnet1 RJD-04-022 RJD-04-023 RJD-04-044 RJD-04-065 RJD-04-066 RJD-04-107 RJD-04-10

Uvarovite1 RJD-04-012 RJD-04-033 RJD-04-06

Clinopyroxene1 RJD-04-012 RJD-04-013 RJD-04-014 RJD-04-015 RJD-04-016 RJD-04-017 RJD-04-018 RJD-04-029 RJD-04-0210 RJD-04-0211 RJD-04-0312 RJD-04-0313 RJD-04-0314 RJD-04-0415 RJD-04-0616 RJD-04-0817 RJD-04-0818 RJD-04-0819 RJD-04-1020 RJD-04-1021 RJD-04-1022 RJD-04-1023 RJD-04-11

Mg-Ca AlmandineMg-Ca AlmandineMg-Ca AlmandineMg-Ca AlmandineMg-Ca AlmandineMg-Ca AlmandinePyrope Eclogite

Uvarovite garnetUvarovite garnetUvarovite garnet

Chrome DiopsideChrome DiopsideNa AugiteNa AugiteNa AugiteAugiteNa AugiteChrome DiopsideChrome DiopsideChrome DiopsideChrome DiopsideChrome AugiteChrome DiopsideNa AugiteNa AugiteNa AugiteChrome AugiteChrome AugiteNa AugiteChrome DiopsideChrome AugiteNa AugrteChrome Augite

Chromite12345678910111212131415161718192021222324252627282930313233343536

Ilmenite1234567891011121314

RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-01RJD-04-02RJD-04-02RJD-04-03RJD-04-03RJD-04-03RJD-04-03RJD-04-04RJD-04-04RJD-04-05RJD-04-06RJD-04-O7RJD-04-07RJD-04-08RJD-04-08RJD-04-09RJD-04-10RJD-04-10RJD-04-10RJD-04-10RJD-04-1 1

RJD-04-01RJD-04-01RJD-04-01RJD-04-02RJD-04-04RJD-04-05RJD-04-07RJD-04-07RJD-04-07RJD-04-07RJD-04-07RJD-04-07RJD-04-08RJD-04-10

Ti unique to kimberlite

Ti unique to kimberlite

GARNET - AMITA-GREENFIELD October 6 2004

wt CaO

RLB

ECL-GARNET - AMITA-QREENFIELD October 6 2004

0OJcoZ

*

?

u.zu

0.18-

0.16-

0.14-

0.12-

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0.06-

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o oo

o o1 l ' l ' l ' l ' l l l ' l '

) 2 4 6 8 10 12 14 1

wt 96 CaO

o RLB

ECL-GARNET - AMITA-QREENFIELD October 6 2004

z.uu

1.80-

1.60-

CM 1.40-

2 1-2 o-1.00-

0.80-

^ 0.60-

0.40-

0.20-rt rt rt

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8 10 12 14 16

wt 96 CaO

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70

60

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10

CHROMITE - AMITA-QREENFIELD October 6 2004

l ! l ' l

Diamond Inclusion Field

0 o*^ 0 o o

o oo o

2 4 6 8 10 12 14 16 18 20

Wt % MgO

o RLB

ILMENITE - AMITA-GREENFIELD October 6 2004

l O i i i i i i i——i i i i i i i i i——i r i —-7-

9

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32 - 0

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ILMENITE - AMITA-GREENFIELD October 6 2004

m

ON

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1.20

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0.80

0.60

0.40

0.20

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20 30 40 5

wt 96 FeO

o RLB

Mr. R. Dillman, October 26, 20048901 Reily Rd.London, OntarioNOL 1WOPh/Fax 1-519-264-9278

R. L. Barnett Geological Consulting Inc., 9684 Longwoods Road, RR 32, London, Ontario, N6P 1P2

Ph. 1-519-652-1498 Fax 1-519-652-1475

Dear Bob,

For your records, the nature and fate of the mineral grains in the batch of grains with letter dated October 6 2004:

RJD-04-01 - GRAINS 11,12,13 - ALMANDINE GRAIN 17 - AMPHIBOLE GRAIN 18 - EPIDOTE GRAINS 19,22 - ILMENITE GRAINS 25,26 - MAGNETITE

RJD-04-1B - GRAIN l - ILMENITE GRAIN 2 - AMPHIBOLE GRAINS 3-10 - ILMENITE

RJD-04-1C - GRAINS 2,4,11,14,15,18,19,21,24,26,28,29,33,37,38 - ALMANDINE

GRAINS 3,27 - GROSSULAR-ANDRADITE S.S.GRAINS 5,7,8,10,13,16,17 - SPESSARTINE-ALMANDINE S.S. GRAINS 9,22,36,47,130 - EPIDOTE GRAINS 12,30 - GROSSULAR-ALMANDINE S.S. GRAINS 20,60,148 - LOST GRAINS 23,31,32,39 - QUARTZ GRAINS 25,55,56,90 - SPHENE GRAINS 34,40 - PLAGIOCLASE GRAIN 35 - PYROPE-ALMANDINE S.S. GRAINS 42,44,54,59,70,79,83,88,89,111,121,142,

144,147 - AMPHIBOLE GRAINS 49-52 - Fe-CLINOPYROXENE GRAINS 53,145 - RUTILEGRAINS 57,63,64,71,74,76,82,84,91,94,95,100,102,106,

107,110,116,119,120,125,127,128,131,138, 141,143,149 - MAGNETITE

GRAINS 61,62,65,67,69,72,73,75,81,86,92,96,99,101,104,105,109,112,113,117,118,122,124,126,129,132,136,137,139,150 - ILMENITE

GRAINS 66,68,146 - CHLORITE GRAIN 77 - CHLORITE+ILMENITE GRAIN 80 - K-FELDSPAR GRAIN 87 - Zn-SPINELGRAINS 93,115,133,134 - Ti-MAGNETITE GRAIN 135 - MELANITE

RJD-04-02 - GRAIN l - SPESSARTINEGRAINS 7,8 - SPESSARTINE-ALMANDINE S.S. GRAINS 13,18 - ILMENITE GRAINS 19,20,21 - AMPHIBOLE GRAIN 22 - PHLOGOPITE GRAIN 23 - SPHENE

RJD-04-03 - GRAINS l,10 - SPESSARTINE-ALMANDINE S.S.

RJD-04-04 - GRAINS 1,3 - SPESSARTINE-ALMANDINE S.S. GRAIN 5 - GROSSULAR-ALMANDINE S.S.

RJD-04-05 - GRAINS 1,2 - SPESSARTINE-ALMANDINE S.S. GRAIN 8 - APATITE GRAIN 10 - Fe-OXIDE GRAINS 11,12 - PYROPE-ALMANDINE S.S.

RJD-04-06 - GRAINS 3,8 - SPESSARTINE-ALMANDINE S.S. GRAIN 12 - APATITE -~ GRAIN 13 - RUTILE GRAIN 14 - ILMENITE

RJD-04-07 - GRAINS 11,12,13 - MAGNETITE GRAIN 14 - ILMENITE GRAIN 15 - PYRITE-MAGNETITE

RJD-04-08 - GRAINS 10,11,12 - EPIDOTE

RJD-04-09 - GRAIN 6 - ILMENITEGRAIN 8 - AMPHIBOLE

RJD-04-10 - GRAIN 10 - CORUNDUMGRAIN 14 - ILMENITEGRAIN 15 - TOURMALINEGRAINS 22,27 - MAGNETITEGRAIN 25 - K-FELDSPARGRAIN 26 - PHLOGOPITEGRAIN 28 - SPHENE

RJD-04-11 - GRAIN 2 - SPESSARTINE-ALMANDINE S.S. GRAINS 3,5,15 - MAGNETITE GRAIN 7 - QUARTZ GRAINS 8,9 - APATITE - GRAIN 10 - AMPHIBOLE GRAIN 11 - Ti-MAGNETITE GRAIN 12 - CHLORITE GRAIN 13 - IN PLASTIC GRAIN 14 - PHLOGOPITE t/v Jv-

Sincerely,

R. L. Barnett

^YROPE. R. DILLHAN, AHITA-GREENFIELD RESOURCES, October 6 2004, R.L.B.

13102 40.94TI02 .19A203 21.52C203 4,17FEO 7,41MGO 20,43UNO .42GAO 5,43SUM 100.5!

SI 5.849 *AL .151 6.000AL 3.472 *TI .020 *GR .471 *FE .885 *MN .051 *KG 4.351 *GA .831 10,0810 24.000 *

F/H .215F/FM .177

1 RJD-04-01 GRAIN2 RJD-04-01 GRAIN3 RJD-04-01 GRAIN4 RJD-04-01 GRAIN5 RJD-04-01 GRAIN6 RJD-04-01 GRAIN7 RJD-04-01 GRAIN8 RJD-04-01 GRAIN

240.20'.

5,6.

19.,

5.99,

5,870.130

3.328.004.666.822.067

4.266.906

24.000

1

670433848183558693

t6,000

tttitt

10.061t

.208

.172

2 If MINUTE INCL345678

341,25

.1721.333.997.48

19.78.33

6.12100,45

5,901 *.099 6.000

3,496.018.451.895.040

4,217.938 10,056

24.000 *.222.181

OF CHROMITE

441,91

.3320.384.616.65

20.53.32

5,85100,58

5,969.031 6

3.389.035.519.792.039

4.358.893 10

24.000(

t.000tttttt.024t

191160

541,07

.1921,105.157.37

20.14.38

5.03100,43

5.876 *.124 6.000

3,434.020.583.882.046

4,295.771 10.031

24.000 *.216.178

640.45

.2419,436.657.26

19.05.49

6.50100.07

5,871 *.129 6.000

3,195 *.026 *.763 *.881 *.060 *

4.121 *1.011 10.058

24.000 *.228.186

741.09

.0221.365.166.93

21.62.46

3,2399.87

5,871.129 6

3,467.002.583.828.056

4.604.494 10

24.000(

i.000ttttii

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192161

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1967

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i

6.075iti*tt

9.824t

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PYROPE, R. DILLHAN, AHITA-GREENFIELD RESOURCES, October 6 2004, R.L.B.

9SI02 42,13TI02 .00A203 21.01C203 4.84FEO 7.40HGO 18.23HNO .49GAO 5.81SUH 99.91

SI 6.049 *AL .000 6.049Al 3.555 *TI .000 *GR .549 *FE .389 *HN .060 *KG 3.901 *GA .894 9.8480 24.000 *

F/M .243F/FH .196

9 RJD-04-01 GRAIN10 RJD-04-01 GRAIH11 RJD-04-1C GRAIN12 RJB-04-1C GRAIN13 RJD-04-02 GRAIN14 RJD-04-02 GRAIN15 RJD-04-02 GRAIN16 RJD-04-02 GRAIN

1041.83

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22,07.51

2.93100.11

5.917 t.083 6.000

3.654 *.003 *.393 *.806 *.061 t

4.653 *.444 10,013

24.000 t.186.157

910162345

1141.87

.2521.623.127.24

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24.000 *.213.175

1241.20

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3.512 *.008 *.542 *.856 *.063 *

4.024 *1.002 10,006

24.000 t.229.186

1340.77

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5.883 *.117 6.000

3.431 t.009 *.588 t.871 *.054 *

4,205 *.881 10.038

24.000 t.220.180

U41.12

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19.21.43

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3,663 *.009 t.368 t

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24.000 t.261.207

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3.651 *.008 *.385 *.925 *.071 t

4.200 *.778 10.019

24.000 t.237.192

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6.81100.24

5.889 *.111 6.000

3.224 *.003 *.774 *.799 *.049 *

4.148 *1.054 10.051

24.000 *.204.170

LLL PYROPE, R. DILLHAN, AHITA-GREENFIELD RESODRCES, October 6 2004, R.L,B.

L

LLii ̂

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17 SI02 40.39 TI02 .12 A203 16.68 C203 9.63FEO 6.69HGO 18.33HNO .34GAO 7.97SUH 100,15

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F/U .215F/FH .177

17 RJD-04-02 GRAIN18 RJD-04-03 GRAIN19 RJD-04-03 GRAIN20 RJD-04-03 GRAIN21 RJD-04-03 GRAIN22 RJD-04-03 GRAIN23 RJD-04-03 GRAIN24 RJD-04-03 GRAIN

18 40.

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3.511.010 .470.886.042

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PYROPE, R. DILLHAN, AHITA-GREENPIELD RESOURCES, October 6 2004, R,L.B.

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F/HF/PH

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t.000itti**

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4.104 *1.006 10.050

24.000 *.241.194

3140,84

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4,041 *.927 10.034

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3240.63

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t.OGCtttiit

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LLL PYROPE. R, DILLHAN, AHITA-GREENFIELD RESOURCES, October 6 2004, R.L.B.

L

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33 SI02 41,32 TI02 .00 A203 21,59 C203 3.99FEO 7.21HGO 20.24HNO .49GAO 5,17SUH 100.01

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P/M .214P/FM .176

33 RJD-04-05 GRAIN34 RJD-04-06 GRAIN35 RJD-04-06 GRAIN36 RJD-04-06 GRAIN37 RJD-04-06 GRAIN38 RJD-04-07 GRAIN39 RJD-04-07 GRAIN40 RJD-04-08 GRAIN

34 40,64

.06 21.81 3.758.18

19,15.54

5.7799,90

5,861 *.139 6.000

3,568.007 .428.987.066

4.117.892 10.063

24.000 *.256.204

61245121

35 40.

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6.100.

5.886.114

3.559- .021

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t6.000

tttttt

10.039t

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36 40.

21, 5,6,

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5.863.137

3.441.003 .588.771.044

4.342.860

24.000

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t6.000

tt tttt

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3 41

21 46

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5.928.072

3.500.004 .536.773.048

4.306.843

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t6.000

tt tttt

10.011t

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20 57

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6100

5.843.157

3.402.004 .587.953.066

4.104.960

24.000

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t6.000

tt tttt

10.077t

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39 40.

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5.887.113

3.274.023 .686.882.049

4.178.962

24.000

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t6.000

ittttt

10.052t

.223

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4 41

21 46

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4.31C.756

24,000

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t6.00

tt tttt

10.00t

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.169

PYROPE, R, DILLHAN, AHITA-GREENFIELD RESOURCES, October 6 2004, R.L.B.

41SI02 41.06TI02 .01A203 22.19C203 3,29FED 7,92HGO 19,29HNO .50GAO 5,49SUH 99.75

SI 5.902 tAL .098 6.000AL 3.661 *TI .001 *CR .374 *FE .952 *HN .061 *HG 4.133 tGA .846 10.0280 24.000 *

F/H .245F/FM .197

41 RJD-04-08 GRAIN42 RJD-04-08 GRAIN43 RJD-04-09 GRAIN44 RJD-04-09 GRAIN45 RJD-04-09 GRAIB46 RJD-04-09 GRAIN47 RJD-04-09 GRAIN48 RJD-04-10 GRAIN

4240,90

.0421.064.246.89

20.54.49

5,6999.85

5,877.123 6

3,443.004.482.828.060

4,399.876 10

24,000,

-

23123451

43

t.000tt*ttt.093t

202168

41

2137

19

5100

5.935.065

3.600- .015

.392

.899

.0524.206.854

24.000

.62,14.81.48.54.79.43.59.40

t6.000

tttttt

10.019t

.226

.184

4441,60

.0820.126.036.6419.63

.495.70

100,29

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3CL-GARNET. R. DILLMA1, AHITA-GREENPIELD RESOURCES, October 6 2004, R.L.B.

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SI02TI02A203C203FEOHCOHNOGAOSUN

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3LIIOPYROIEIE. R, DILLHAH, AHITA-CREENFIELD RESOURCES, October 6 2004, R.L.B.

SI02TI02A203C203FEONGOUNOGAOK20NA20

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CHROMITE, R. DILLHAS, AHITA-GREENFIELD RESOURCES, October 6 2004, R.L,B.

175102 .06TI02 .78A203 28.76C203 38.50FEO 15.06MNO .06MGD 15.95ZNO .00NIO .29SUM 99,46

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.059 t3,961 *

11.422 *4.543 *.062 t

4.131 *.021 *.046 24.246

32.000 *1.115.527

3;

125422

9

100

.013

.0553.897

11.4204.873.067

3.862.047.036

32.000

05285686133084241743

t*t**ttt

24.270t

1.279.56!

CHROHITE, R. DILLHAN, AHITA-GREEHFIELD RESOURCES, October 6 2004, R.L.B.

33SI02 .00TI02 1,56A203 31.38C203 33.60FEO 17,01HSO .13HGO 15.65ZNO .00NIO .21SUH 99.54

SI .000 *TI .277 tAL 8.732 *GR 6.273 *FE 3.359 *MN .026 *HG 5.508 *Zti .000 *lil .040 24,2150 32,000 t

F/H .615F/FH .381

33 RJD-04-10 GRAIN34 RJD-04-10 GRAIN35 RJD-04-10 GRAIN36 RJD-04-11 GRAIN

34.05

1.7218.8347.5317.25

.1014,53

.00

.25100,26

.012 *

.322 *5.516 *9,342 t3.586 *.021 t

5,384 t.000 *.050 24.233

32,000 *.670.401

2123244

35.09

1,6718.7447.6117.12

.1814.46

.00

.21100,08

.022 *

.313 *- 5.500 *

9.375 *3.566 *.038 *

5.368 *.000 *.042 24.224

32.000 *.671.402

36.00.45

13.2455.4420.46

.2410.22

.13

.16100,34

.000 *

.088 *4.072 *11.440 *4,466 *.053 *

3.976 *.025 *.034 24.153

32.000 t1.137.532

ILHENITE, R. DIILHAN, AHITA-GREENFIELD RESOURCES, October 6 2004, R.L.B.

1SI02 .00TI02 51,09A203 .44C203 .14FEO 39.81UNO .26HGO 7,72ZNO .06NIO .10N205 .13SUH 99.75

SI .000 *TI 9.989 *AL .135 *CR .029 *PE 8.656 tHN .057 *MG 2,992 *ZN .012 *SI .021 *NB .015 21.9060 32.000 *

F/H 2.912F/FH .744

1 RJD-04-01 GRAIN2 RJD-04-01 GRAIN3 RJD-04-1C GRAIN4 RJD-04-02 GRAIN5 RJD-04-04 GRAIN6 RJD-04-05 GRAIN7 RJD-04-07 GRAIN8 RJD-04-07 GRAIN

2.00

49.16.62.26

42.12.29

6,46.00.25.10

99.26

.000 *9,797 *.194 t.054

9.334.065

2.552.000.053.012 22.061

32.000 t3.684.786

2023851111735

3.00

48.38.11

1.0641.64

.187.32.04.16.43

99.32

.000 * 9.642 *

.034 *

.222 *9.229 *.040 *

2.891 *.008 t.034 *.052 22,153

32.000 *3,206.762

4.00

52.22.21.98

36.33.31

9.18.00.20.33

99.76

.000 *10.058 *

.063 *

.198 *7.782 *.067 *

3.505 *.000 *.041 *.038 21,753

32,000 *2.240.691

5.00

52.35.17

1,7334.61

.409.76.03.24.22

99.51

.000 *10.047 *

.051 *

.349 *7.387.086

3.713.006.049.025 21,714

32.000 *2.013.668

6.00

56,79.37

1.0728.05

.1212.65

.00

.17

.1599.37

.00010.508

.107

.2085.772.025

4.639 t.000 *.034 *.017 21,309

32.000 *1.250.555

7.00

46.31.10

4.9738,30

.967.59.00.16.55

98,94

.000 *9.238 *.031 *

1.042 *8.497 *.216 t

3.001 *.000 *.034 *.066 22.126

32.000 *2.903.744

8.00

54.92.28.87

30.9!.74

11.50.13.23.18

99,76

.00010.307

.082

.1726.451.156

4.278.024.046.020 21

32.0001.

tttttttit

.536t

545607

ILMENITE, R, DILLHAN, AMITA-GREENFIELD RESOURCES, October 6 2004, R,L.B.

9SI02 .02TI02 53.08A203 .19C203 .84FEO 35,51HNO .29MGO 9.72ZSO .06NIO .061205 .29SUM 100,06

SI .005 *II 10.133 tAL .057 *CR .169 *FE 7.539 tMN .062 *MG 3.678 *ZN .011 *SI .012 *NB .033 21.6990 32.000 *

F/M 2.067F/FH .674

9 RJD-04-07 GRAIN10 RJD-04-07 GRAIN11 RJD-04-07 GRAIN12 RJD-04-07 GRAIN13 RJD-04-08 GRAIN14 RJD-04-10 GRAIN

10.02

54,31.63

1.3130.91

.1711.57

.13

.18

.2899.51

.005 *10.196 *-

.185 t

.259 *6,453 *.036 *

4.305 *.024 t.036 t.032 21.530

32.000 *1.507.601

67810413

11.00

52.20.12

1.5035.39

.219,35.00.08.34

99.19

.000 t10.077 *

.036 *

.304 *7.597 *.046 *

3,577 t.000 *.017 *.039 21,694

32.000 *2.136.681

12.00

52.59.21.56

35.35.25

9,80.05.04.28

99.13

.000 t10.133 *

.063 *

.113 *7.574 t.054 *

3,742 *.009 *.008 *.032 21.730

32.000 *2.038.671

13.00

53.15.21

3,2632.16

.2110.38

.09

.17

.1599.78

.000 *10.064 t

.062 *

.649 *6.772 *.045 *

3,895 *.017 *.034 *.017 21,555

32.000 *1.750.636

14.00

47.38.12

2,1941.97

.296.77.02.17.47

99.38

.000 *9.487 t.038 *.461 *

9.345 *.065 *

2,687 *.004 *.036 *.057 22,179

32,000 *3.503.778

ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Work Report Summary

Transaction No: W0470.01924 Status: APPROVED

Recording Date: 2004-DEC-06 Work Done from: 2004-SEP-16

Approval Date: 2004-DEC-22 to: 2004-NOV-12

Client(s):

164856 MARMONT, CHRISTOPHER

201344 THOMAS, RODNEY NELSON

Survey Type(s): BENEF

Work Report Details:

Claim* Perform

S 1163584 S591

S 1174498 S591

S 1174500 33,545

S 1229412 SO

S 1231285 81,773

36,500

External Credits:

Reserve:

Perform Approve

S591

S591

S3.545

SO

S1.773

S6.500

so

Applied

SO

SO

so34,727

S1.773

S6.500

SO Reserve of Work

SO Total

Applied Approve

SO

SO

soS4.727

S1.773

S6.500

Assign

S591

S591

S3.545

soSO

54,727

Assign Approve

591

591

3,545

0

0

S4.727

Reserve

sosososososo

Reserve Approve rjue Date

SO 2005-APR-11

SO 2005-APR-11

SO 2005-APR-11

SO 2005-JAN-24 E

SO 2005-JAN-24 E

SO

Report*: W0470. 01 924

Remaining

Status of claim is based on information currently on record.

31L14SE2010 2.28918 900

2004-Dec-24 10:35 ARMSTRONGI Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2004-DEC-22

Ministere duDeveloppement du Nord etdes Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

CHRISTOPHER MARMONT 1165 QUEEN'S AVENUE OAKVILLE, ONTARIO L6H 2B3 CANADA

Tel: (888)415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2.28918 Transaction Number(s): W0470.01924

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact BRUCE GATES by email at bruce.gates@ndm.gov.on.ea or by phone at (705) 670-5856.

Yours Sincerely,

Ron C. GashinskiSenior Manager, Mining Lands Section

Cc: Resident Geologist

Timothy John Beesley (Agent)

Assessment File Library

Christopher Marmont (Claim Holder)

Christopher Marmont (Assessment Office)

Rodney Nelson Thomas (Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:20173

H f

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5193000N

5192000N

S183000N

5160000N

626000E 63000OE 631000E 632000E 633000E 634000E 636000E 6MOOOE 637000E 638000E 639000E 640000E 641000E

UTM Zone 17

Milling toiMM mining ctelrw ilsouM wntult wltnin* Provincial Mining RoeotdBiu' CXlit* o1 ihs Mlnttlryof f*wlftfttnD*vok\f^TOBi nr*1 Mine* ter**mbrnl mtemwilon oft Iho tKHui of nvph KM )m*Mofl tot nnvtjMkMMI, lUNoy, or Bwt tKte dol*fTr*wtton putpoaw Aft th* Worrrolteft *hown on Ihh mtfiktorr^lM Imm vsnous lotiie**, Comptetsne** snrt sccumey *ra witon miy j*o i* ohWinwl ihiDugniho tac*iunrt Ti*as wRogitir^Oflfca.onh* Wnmiy atH

kind t ttewn (wroon,General Information and Limitations

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Thfc map may not *how uringbuiwl MnH unim an tt, right ot**ve, tloeMing MB M*, He*ntM, e

iDnrlaln bnitt*nuraiiM Hnci urn* trot

CANADA

MINntRY OF NORTHERN

PROVINCIAL MINING RECORDER'S OFFICE

Mining Land Tenure Map

Date l Time of Issue: Wed Dec 22 09:09:06 EST 2004

TOWNSHIP l AREA PLAN PARKMAN G-1666

ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division SudburyLand Titles/Registry Division NIPISSINGMinistry of Natural Resources District NORTH BAY

TOPOGRAPHIC| : AOminirtraliY* Boundarm

ConcoMton. lot

Lartd TenurefriwhoWPatenl

nil Svrrtniai And Mining Right*

nn Surtocn Rights Ctiiy

r^j Mining Rfctita On*,.

Laasahow Patent

fjjjn Surtflc* And ninths) Risjht*

ffi"! Surt*c*RlghteOniv

ESBB B H

LAND TENURE WITHDRAWALSI33J i Araas WHhdiaiwi from

Mining Ac* WWldrxwal Typ*i

Dn)*t In CouiKl WHhtirnwo! Typos W' mi SiirtacB Aw) Uinmj myMf Wtn*a*n

'

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONSMom* tor Type Dele Description

A. P, 35237 Wsm

W-t(--C1 31 Wtrn

Jan 31. 2000 Ail 5, I*M

May 20, 16B1 Peb 26, 2QCB

AQorawl* MMtHl Pnnffl f 2525T 200001/31 'APPLICATION FOR AP JULV 5,t BM' A .P, 186*2 EMf 34 SEP 19BT

W-LL-C1 36 Wsm Toti 26. 2002 *a hrat"" Nnp;i','ww*,iTt*imflov.oB

W-LL-CtS Worn feh 2S. ZOCC td hra)-* M

W-LL-CR4* Warn Aw 19, 2WB

,DiltB' ant) h now mgubtcd at. Con. Bm,, ccraitm RocoWsr'i n bdvond life Wllhdrawal OIUBKIO

" Wtp;,J.'www,imrtirnoYoa,

Frt- X, 2WC i* MQ|B" MtpiiA

Ocl 25, S(W3 ** h lot*"

-

P131 ONT Ute wBMniwtlft.SSMMno Act RSO 1999.2(11(1*03 Boundary *ren wHMMwn cibk tovktwaclunUiea 4*.^.

P MO-OS ONT M*S wKMrawal 3,,VJ Mining Act US O 19fta I

i1-**OI..o,fl !,p-,- W-LL-P140 OWT M*G Vi*Mmw*t G.35Mtntfq Act RSO t BOS, aft'dr.'CC BourdJfy aoreraHy doptew ntoa

Wsm Jnnta, 1995

2.28918 BENEF

^—^344QOmE632800mE Sl87200mN

outwash Mfid md small cobbiss147 contorted, gray,

147a ! migmatite granitic gneiss;nlgmatitlc granite gneiss, overlain by outwash sandcontorted. No stria*. with minor pabblM

^ __^ ^ I .^.^. . __ .__-..__-, —.-.______

Clalnipost j2000mEf4* 1231284} 1200m W f2.1163584

co brown sand with 20 cm rounded cobbles RJD-04-08 3.1.3

OL36, 2, 73 (8)99 RNT 026

outwash-land •and cobbles In run

msv brown clay ,.}K i \ \ varved day forms; L. r YV aa \ \ w*** DtdJ OL, Cr And, Cr Gr blue-grey clay, \ 2,0,3 fO)T*\ \ sits of OC-2 14,5, *94

drop grains, 02 CCM 0210 \ \ T99 RNT 024 33,3,1089(98)

5,0,1(1)largeflat depression

*V r

eg outwash sand,

QC-3 UV,CrAnd27,1.+113

N syenite cobbles bi creek

iltty mg sand over :g outwash sand 22

msv blue-gray clay,cafc,H2S3 m outwash sand many

exposures v m.g. well sorted sand.nvcg outwash sand

GC-4 39,1, *6ijCrAnd 99 RNT 023 27,4, 563 (34)

1231284 02 CCM 038 0,0.0 Rhythmite, calc day40 cm dark brown clayey sandy silt

on bedrock, non oak; sand all around.198 O RJD-04-10 9, 1, (4) RR

39 l ECL, MB silty sand over clay

09 RNT 028 31, 4, 150 (17) OL nrg, sand wKh clay dasts

well sorted n*g* sai non-calc

Three parallel .i, ^ j j -w '" lamprophyre dlXes up to 60 cm wide; mgweU-aortedsand 14^ cakTmas'po, with roumted Inclusions

overlying bedrock j^^^ofplnkTspitkvhlt* 1 41 outwash sand ~ and cobbles

composttlonaUy banded qz-fsp-muse gneiss

cobble-rich outwash sand

fa weitaorted esnd to 90 cm. l 1,1,4 02 CCM (1-2 m, 8Aboulders

gneiss, mlgmatltoe.g. brown 43

outwash sand,cobblos

_ non-calc

5) cm weitoorted sand, oP-tbbles at bottom on bedrock

Kettte P on i148 * well-sorted f-mg sand Ice-smoothed outcrop ... 13 . *- ,. . sot Jh aide of road; x 1M layered sand and graveUy sand

iiAfi- annite onelss. some )ebble rich layers,KattsRcobWsarlfuvlogJaclal Interlayered

clay and elite gritty clay 44(QC*1) 3,1.+39several auger holes In

outwash sand and gravel 1200mN ,1174500054

outwash sand granitic gneiss

117450099 RNT 030 2.1,3, (20) Beach sandO 063

cobbles andlarge oobbjlM and sand , \ well layered kame (?)' \ \ gravel and sand i

\ layered— -V-.—

45 60 cm brown-gray sand,non-cate '

^RJD-04-02 5,3,3, RR 46 calc-clay, sBty sand"D-04-01 12, 2,19, (0) RR, UV, G10

A99 RNT 028 72,6,6619 (23) OL, LP, RR

RR 7, 2, 4, RJD-tM-OS RR, UV 5,0, 3, (0) RJD-04-04OUR SO 009

27,1,256(16) 99 RNT 027mg well-sorted sand, no cobbles

148b ~-i———— l48*02 CCM 068 6, 0,15 (6)sand, silt, calcareous clay

m-cg outwash sandOM fine grey sand aarid over rock and clay

01JRMA10,0,1,(0)'RNT-02-01

2,0, 5. (0)99 RNT 002^324, 2, -t-77-tp

.___ ,...l. 400mS[•11231289 057gray, clayey sand

J M.40,.2,273C 60 cm sand

148a large cobbles In gravel ph

Depth (cm) ~0-AO ——5-A1

1U-B1 4S-B2 75-Cobbles 51

1231285 02 CCM O 1 mgreyweU sorted sand 02 CCM 056 1,0,10, (0) PIPE-UKE MAGNETIC FEATURE

All Season Road Seasonal road, trail

O Claim Post, Une Post Buk Alluvium Sample Buk TO Sample Buk fluvioglacial Sample Pan Concentrate Sample Alluvial Silt Sample Auger

60cmf.g.ssnd; SRSAbouldersi

45cm Ao 36cm sand creep-lnteriayered sand,

V-3Drill HoleIran City Mmes 1966

f.fl. we! sorted pita buff sltty sand alluvial sand and

brown well sorted 62

m .g. sand02 CCM 002 14, 1499, (6)c.g. outwash aand,

round cobbles calcareous silty clayey sand; O angular musc-quartztte bouMera f 02CCM067 4,1,10,1(1)sBty sand, outwashHummocky

~ ime - EskerComplex

V-2 !Mil HolsIron City Mines 1966 slope ^O0

CCM 005 17, O, 535, (7) , 0,2

well sorted 64 brown sand 12, 3,44, (12) -GOLD

CHROMITE * PICROILMENITE CHROME DIOPSIDE

PYROPE

l Abundant Cobbles boulders,

cobbles,outwash

sand

1.6 m outwash sand over rock

RJD-04-06 3,0,0

172 Trench, DDH 69-1,*ir2i1174498 angular boulder* gneiss, outwash sand

G10 HARZBURITE PYROPE UV UVAROVITE GARNET Cr And CHROME ANDRADITE

CHROME GROSSULAR ECLOGITE GARNET REACTION RIMS, SHAGREEN OLIVINELAMPROPHYRE GRAINS MARBLE GRAINS

Boulder(s)Exposure (Quaternary deposits) OutcropDiamond Drill Hole Traverse

mg. sand with granules, cobbles;

some local angular cobbles 02 COM 007 0,0,0RJD-04-07 2,0{many cobblee In 04.

outwash sand i 02 CCM 008 14, O 133, (3)

'.ik-spring

DDH3a (iron Cite Mines, 1t [|u0 of fsp-qMnusc gneiss

gmtth? ' 'v-'"-V^ " ' :70

1moutwash sand

1.95 m -outwash[land

174 outwash sand

outwash sand 18,0,91, 0 1 02 CCM 01 0' '60 cm outwash sand

Green Lake valley 12,1041493 wider •3,1041496

02CCM0734,1, 13, (6)

1 m outwash sand and R cobbles aider

Swamp Steep Slope

BO Beaver Dam

02 CCM 015 3,0,4, (0)

50 cm pit In sity, clayey grey,very calc sand, unda by well sorted rag. sand. 02 CCM 016

spring j 02 CCM 017 1,1, 2, (0) 400 metres

CCM 023 3, 2,190, (1) irseoutw

and cobblescoarse outwash sand

Idersof mlnmatlc gneh *Sure

Catch Lake

HJOJOte OlDCOt

(130QOCE KJ10DOE

A-TN-

modified from: Marmont 2004

l m.g. pale brown sand, non-calc, scattered cobbles

31L14SE2010 2.28918 PARKMAN 210

Heavy Mineral Sample Locations Parkman Property

Amita-Greenfield Resources - Grenville Gold Corp. Parkman, Wyse and McAuslan Townships

Sudbury Mining District, Ontario