I I I I I I I I I I I I I I I I I I I RECEIVED r 72MAY 2 3 Z008. \LL LoC:rs GEOSCIENCE ASSESSMENT OFFICE

Transcription

1 \LL LoC:rs - RECEVED r 72MAY 2 3 Z008 GEOSCENCE ASSESSMENT - OFFCE

2 ntroduction Millstream Mines Ltd. Airport East Property Report on Drill Holes MAE to - 05 Claims S & , Falconbridge Township Sudbury Mining District From May to August 2007, Millstream Mines Ltd. carried out diamond drilling on the company's Airport East Property, located in Falconbridge Township, Sudbury Mining District, Ontario. Logs, plans and sections of these holes are being submitted to the Ministry of North em Development and Mines for assessment work credit. This report forms part of that submission. Number of Holes Drilled and Total Length of Drilling Five holes with a total length of 2,317.0 m were drilled. Summary data concerning the drill holes are presented in the table comprising the appendix to this report. Location of Work Area and Access The work area is located approximately 7.5 km northeast of the town offalconbridge, City of Greater Sudbury, on claims S and S The location is illustrated on the accompanying key maps. Access is by road from the town offalconbridge, through the Xstrata Nickel refinery site, thence by a series of private roads to the north-central area Falconbridge Township, where a series of bush roads and drill trails lead to the sites. Many of these roads are illustrated on the claim map of the area «Plan G-4048, Falconbridge Township). Supervision of Work, Author of Report The drill program was supervised by P. A. R Brown, P. Geo., RR 1, Corbeil, ON, POH lko. R Blais, 160 Pinewood Park Drive, Box 237, North Bay, ON, PB 8K6, coordinated later stages of the drill program. The author of this report is P. E. Giblin, 55 Kingston Court, Sudbury, ON, P3A le, who logged the core from the holes and prepared the related plans and sections. 12

3 . Summary of Exploration Work At the end of2007 the company's property included several contiguous claims in eastern Falconbridge Township. A good deal of exploration work has been carried out on the northern section of the company's property, principally on claims (L. 5, C. 6), and (L. 4, 5, C. 5) by many companies over several decades. nasmuch as this report deals with work on 2 claims in the central and eastern parts of the property, the previous work on the northern claims is not described herein. Much of the previous work by other parties may be recorded in the Assessment Work Files, Ministry of Northern Development and Mines, Sudbury, and in the Geological Data nformation Folio for Falconbridge Township (see below under References). The following summary of previous exploration work describes work carried out on or near the subject claims. Considering that many parties did considerable work over the years, the work history may be incomplete. 1984: Airborne EM and magnetometer survey. 1988: Soil geochemical survey for Au, Ag, Cu, Ni, Pt, Pd by Noramco Explorations Ltd. 1989: VLF - EM survey. 1998: HLEM, magnetometer, J.P. surveys. 2000: AeroTEM survey. 2003: J.P. Resistivity /Chargeability survey. 2004: Airborne MegaTEM survey. Date of Completion of Report This report was completed December 22, References Adlington, Richard 1981: Falconbridge Township, Sudbury District; Ontario Geological Survey Preliminary Map P.2447, Sudbury Data Series, Scale 1 :15,840 or 1 inch to Y4 mile. Data compiled /3

4 - 3 - Assessment work files, Ministry of Northern Development and Mines, Sudbury. Debicki, R. L Stratigraphy, Paleoenvironment and Economic Potential of the Huronian Supergroup in the Southern Cobalt Embayment. Ontario Geological Survey, Miscellaneous Paper p. Dressler, B. O. 1984: Sudbury Geological Compilation; Ontario Geological Survey Map 2491, Precambrian Geology Series, scale 1 :50,000, geological compilation Dressler, B. O. 1987: Precambrian Geology offalconbridge Township, District of Sudbury. Ontario Geological Survey Map P.3067, Geological Series - Preliminary Map. Scale 1: 15, 840 or 1 inch to y,. mile. Geology 1982 and Ontario Geological Survey. 1987: Falconbridge Township, District of Sudbury. Ontario Geological Survey, Geological Data nventory Folio 386, compiled by the staff of the Resident Geologist's Office, Sudbury, 34 p., 2 maps. Thomson, 1. E. 1957: Geology offalconbridge Township. Ontario Department of Mines, Annual report, Vol. LXV, Part 6. Map , Falconbridge Township, scale 1: 12,000 or 1 inch to 1,000 feet. P. E. Giblin December 22,

5 . -4- APPENDX MLLSTREAM MNES LTD. ARPORT EAST PROPERTY DRLL HOLES, 2007 DRLL HOLE SUMMARY, ARPORT EAST PROPERTY Hole Claim Coordinates of Collar AzimuthO Dipo Depth Date Date Number (m) Started Log Date Completed Completed MAE L S, E May 23/07 Sept. 11/ E, N June 15/07 MAE L S, 21+ooE May 30/07 Aug E, N June 12/07 MAE L 3+16 S, E June 18/07 Sept. 22/ E, N June 28/07 MAE L S, E N/A July 06/07 Aug E, N July 18/07 MAE L N E N/A July 19/07 Oct. 05/ E, N Aug.01/07 Total: 2, holes

6 ARPORT N,.... -<~ FALCON BRDGE MLLSTREAM MNES LTD. o, SCALE 2oo0m ARPORT EAST PROPERTY KEY MAP LOCATON OF DRLLNG CLAMS S & S FALCON BRDGE TOWNSHP. SUDBURY MNNG DSTRCT SCALE 1 :50, 000

7 \ 12149n ~~~"7 ~- jt -,--., S50768 f7 f '\) LOT i, CON 1 (~. l ',\'<~ l '}" lot 4. CON 3 '. MLLSTREAM MNES LTD. ARPORT EAST PROPERTY KEY MAP LOCATON OF CLAMS S & S FALCONBRDGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 :20, 000

8 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Township: Falconbridge Claim No. S Hole No. MAE Page 1 Collar Location: L S, E UTM: 17T E, N NAD 83 Approx. 260 m S, 170 m E of #4 post, S Azimuth: 270 Dip: 70 Total Depth: m Survey Data: See end of log Core Size: BO Date Started: May 23, 2007 Date Completed: June 15, 2007 Logged By: P. E. Giblin Date Log Completed: Sept. 11, 2007 Drilling Company: RonKor Diamond Drilling Ltd. Core Stored: Millstream Mines Ltd., Potter Mine, Munro Township, ON From - To Rock Type Descriptidn Overburden Bruce Formation Pebbly wacke, Dark gray, fine - grained pebbly wacke, sparse pebbles principally of quartz and granite, quartz minor Sudbury granules common. Bedding generally absent. Carries sparse small blebs of pyrrhotite and pyrite, rare breccia trace very fine - grained chalcopyrite. Wacke commonly exhibits crackle breccia. Sulphides often concentrated in the very thin fractures of crackle breccia, and occasionally concentrated on outer margins of some pebbles. Rock is cut by minor Sudbury breccia seams, and by generally sparse chloritic fractures often coated with thin pyrite films Sudbury breccia. Upper contact at 20, lower contact at 40 to core axis. Green aphanitic matrix, banded at 30 to core axis Sudbury breccia. Upper contact at 30 to core axis, lower contact on broken core. nternal banding and elongated fragments at 30 to core axis Possible bedding at 30 to core axis Sudbury breccia. Contacts on broken core.

9 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 2 Description Sudbury breccia zone Sudbury breccia carries fragments of pebbly wacke. Matrix commonly comprises 30%+ of rock.. Wacke fragments often exhibit crackle breccia. Sudbury breccia matrix and wacke fragments occasionally carry sparse fine - grained disseminated pyrite and pyrrhotite, and trace chalcopyrite. Sulphides also occur in very sparse, thin quartz veins. Overall «1% sulphides Foliation in Sudbury breccia at 60 to core axis Banding in Sudbury breccia at 40 to core axis Quartz - pyrite vein carries irregular pyrite bleb 20 x 20 mm across. Vein along chloritic fracture at 10 to core axis Fracture zone. Core considerably broken on fractures most commonly at 30,40,50 to core axis Foliation in breccia most commonly at 40 0 to core axis Fracture zone. Core badly to considerably broken on fractures at 20, 35, 60 to core axis Fracture zone. Core badly to considerably broken on fractures most commonly at 20, 40, 50 to core axis Several blebs and very thin veins of pyrrhotite. Trace chalcopyrite Foliation in Sudbury breccia at 80 to core axis Three quartz veins each c.5 mm thick at to core axis.

10 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 3 Rock Type Description Quartz vein 5 mm thick at 50 to core axis Fracture and fault zone Core badly broken Fault breccia. fault gouge Foliation in Sudbury breccia at 45 to core axis Fracture zone. Core moderately to considerably broken on fractures most commonly at 30, to core axis Quartz - pyrrhotite - pyrite vein 2-5 mm thick at 30 to core axis , , Quartz veins 2-5 mm thick at 20 to core axis carry minor pyrrhotite and pyrite Foliation in Sudbury breccia at 45 to core axis Several thin quartz veins c.2 mm thick. at to core axis Quartz vein 25 mm thick at 40 to core axis. Carries minor pyrite, principally in thin streaks along margins of vein Foliation in Sudbury breccia at 45 to core axis Fracture zone. Core moderately to badly broken on chloritic fracures at 0.30,50 to core axis. Many fractures coated with thin pyrite films.

11 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 4 Description Fracture zone. Core considerably to badly broken on chloritic fractures most commonly at 10,30,50 to core axis. Many fractures coated with thin films of pyrite. From c.172 Sudbury breccia commonly carries trace - c.1% fine - grained pyrrhotite and pyrite as tiny veins. Veins most commonly <1 mm thick. and are generally parallel to foliation of breccia Fracture zone. Core consideraply broken on chloritic fractures most commonly at 40, 60 to core axis Fracture zone. Core badly broken Foliation at 40 to core axis , , Fracture zones. Core badly broken Foliation at 55 to core axis Pebbly wacke. minor Sudbury breccia Upper contact at 40 to core axis. Pebbly wacke frequently exhibits crackle brecciation, carries trace - <1 % pyrrhotite + pyrite as tiny veins and disseminated grains, frequently in the thin dark fractures of crackle breccia. Wacke is cut by minor Sudbury breccia Foliation in Sudbury breccia at 40 to core axis Foliation at 30 to core axis Pink granite cobble Several thin, irregular quartz veins 2-3 mm thick Quartz vein 3 mm thick Quartz vein breccia 5-10 mm thick at 75 to core axis.

12 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE PageS From- To Rock Type Description Gray sandstone fragments exhibit crackle breccia Foliation at 25 to core axis Carbonate, pyrrhotite, pyrite, trace chalcopyrite in fracture Foliation in Sudbury breccia at 30 to core axis Fracture zone. Core badly to considerably broken on chloritic fractures most commonly at 40, 50 to core axis Fracture zone. Core badly to considerably broken on chloritic fractures most commonly at 40, 60 to core axis Fracture zone. Core moderately broken on chloritic fractures at 60 to core axis. Thin pyrite ± carbonate films on several fracture surfaces Fracture zone. Core badly to moderately broken on chloritic fractures most commonly at 40, 50, 80 to core axis Fracture zone. Core badly to moderately broken on chloritic fractures most commonly at 35 to core axis Fracture zone. Core badly to moderately broken on chloritic fractures most commonly at 40, 50 to core axis Fracture zone. Core badly broken.

13 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 6 DeSCription Fracture zone. Core badly to moderately broken on chloritic fractures most commonly at 10, 40 to core axis Fault breccia Small angular fragments of wallrock in very fine - grained matrix. Contacts on chloritic fractures at 45 to core axis Foliation in pebbly wacke at 45 to core axis Fault breccia Small angular wallrock fragments in very fine - grained matrix. Bounded by chloritic fractures at 50, 60 to core axis Several irregular masses of fine - grained pyrrhotite up to 5 x 30 mm across. Overall <1 % pyrrhotite Possible very thin bedding at 40 to core axis Gabbro (fragment?), green - gray, contacts on broken core Schistosity in pebbly wacke at 35 to core axis. axis Schistosity in wacke at 25 to core Sudbury breccia zone. Wacke, feldspathic sandstone, minor gabbro inclusions Generally dark gray - green banded matrix, which sometimes exhibits contortions. Carries inclusions of wacke, feldspathic sandstone and gabbro. Zones of varying lithology are often represented by fragments present in the breccia zone as noted below Pedominantly Sudbury breccia matrix, rounded inclusions Banding in Sudbury breccia matrix at 45 to core axis.

14 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 7 Description Pale gray - white feldspathic sandstone. Round to subround quartz grains, commonly <1 mm across, lesser subangular feldspar grains, in gray, very fine - grained matrix. Massive. Upper contact at 55 0 to core axis, lower contact on chloritic slip at 50 0 to core axis Schistose wacke, carries trace - c.1% fine - grained pyrite Schistosity at 50 0 to core axis Pale gray - white feldspathic sandstone. Upper contact sharp at to core axis. lower contact irregular Wacke Pale gray - white feldspathic sandstone. Lower contact sharp at 45 0 to core axis Dark gray uniform pebbly wacke Pale gray - white feldspathic sandstone. Lower contact sharp at 45 0 to core axis Gabbro, minor Sudbury breccia Green - gray gabbro. commonly medium - grained. Very minor gray - white zones. Carries trace fine - grained disseminated pyrite and sparse tiny pyrite veins. Cut by sparse thin Sudbury breccia seams Sudbury breccia, dominant gabbro fragments i Gabbro clasts common in green to dark gray. banded, aphanitic Sudbury breccia matrix, and comprise c.30% of rock. ndividual gabbro fragments are up to 1.5 m in core - length. Gabbro fragments commonly carry trace fine - grained disseminated pyrrhotite and pyrite. Pyrite films occur on some fractures. Fragments intermittently exhibit magnetic attraction due to fine - grained disseminated

15 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 8 Description pyrrhotite. Very sparse granite clasts also occur in breccia. Small clasts are sometimes elongated and oriented approximately parallel to banding of matrix. Sparse, fine - grained disseminated pyrrhotite and pyrite occur in Sudbury breccia matrix. Breccia is cut by very sparse, thin quartz ± pyrite veins. Very thin pyrite ± carbonate veins occur on some chloritic slips Banding in Sudbury breccia matrix at 40 to core axis Banding in Sudbury breccia matrix at 50 to core axis Foliation (small clasts and banding in matrix) at 35 to core axis Foliation (banding) in breccia at 40 to core axis Vein breccia. Small angular fragments of Sudbury breccia, up to c.10 x 20 mm across, occur in quartz - pyrite matrix. Contacts are on chloritic slips at 40 to core axis Quartz vein 30 mm thick at 60 0 to core axis Quartz vein 5 mm thick, irregular Vein breccia. Small angular fragments of wallrock in very sparse quartz - pyrite (trace chalcopyrite?) matrix. Matrix is vuggy in part Breccia zone. Small angular fragments. Chloritic fractures most commonly at 40,60 0 to core axis Very thin carbonate vein 1-2 mm thick at 50 0 to core axis. (Fault gouge?) Banding in Sudbury breccia at 60 0 to core axis.

16 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 9 From - To Rock Type Description Very sparse chloritic fractures in Sudbury breccia at 20,30,40,60 to core axis Gray feldspar porphyry. Medium - grained, gray - white feldspar phenocrysts and minor quartz in very fine - grained greenish gray matrix Banding in Sudbury breccia at 50 to core axis Fracture zone. Core badly to moderately broken on chloritic fractures most commonly at 20, 40 to core axis Feldspar porphyry fragment Fracture zone. Sparse chloritic fractures most commonly at 10, 30, 50 to core axis Pebbly wacke, minor Sudbury breccia Gray pebbly wacke exhibits crackle breccia, and is cut by dark, thin seams of Sudbury breccia Quartzite Gray - white quartzite, fine to medium - grained, exhibits crackle breccia. Upper contact gradational, lower contact fairly sharp at 40 to core axis Pebbly wacke Gray pebbly wacke is cut by minor Sudbury breccia. Wacke occasionally exhibits weak foliation.

17 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 10 Description Sudbury breccia seams at 35 to core axis. Chloritic slip at 30 to core axis Very thin fault gouge on chloritic slip at 30 to core axis Quartz vein 5 mm thick at 20 to core axis, carries pyrite bleb 10 x 20 mm across Fracture zone. Core considerably to moderately broken on chloritic fractures at 45, 60, 70 to core axis. Very thin fault gouge and quartz vein 1-2 mm thick Pink granite boulder. Upper contact on chloritic Slip at 30 to core axis, lower contact sharp, appears to transect foliation of wacke at a low angle Fracture zone. Core badly broken on chloritic fractures most commonly at 0.30,40 to core axis Breccia. Small angular fragments of green Sudbury breccia matrix in a matrix of very thin quartz - pyrite veins. Cut by chloritic slips at 55 to core axis Pink granite cobble Sudbury breccia at 55 to core axis Quartz vein 5 mm thick at 25 to core axis, carries blebs of pyrite and pyrrhotite Sudbury breccia Dark gray, aphanitic matrix carries very small to tiny fragments. which are often elongated parallel to one another and to banding. Carries trace fine - grained disseminated pyrrhotite Foliation in breccia at 30 to core axis.

18 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 11 Description Fracture zone. Core considerably to badly broken on chloritic fractures most commonly at 10,40,50 to core axis Quartz vein 10 mm thick at 60 to core axis, carries trace pyrite Fault breccia, fault Small angular fragments of wall rock and Sudbury breccia, fault gouge, minor thin quartz vein matrix. gouge Fracture zone. Core badly to considerably broken. Very sparse thin carbonate veins Banding in Sudbury breccia at 40 to core axis Fault breccia, fault gouge Small angular fragments of wall rocks Fault gouge mm thick, upper contact at 30. lower contact with Sudbury breccia on chloritic slip at 50 to core axis Pebbly wacke, minor Sudbury breccia Dark gray, very fine - grained matrix, small granite and quartz pebbles, sparse granite cobbles, rare gabbro and feldspar porphyry cobbles, common quartz granules. Carries sparse disseminated blebs of pyrrhotite. Rock is cut by minor Sudbury breccia Quartz vein breccia, thin quartz veins most commonly 1-2 mm thick at 40 to core axis UPyrrhotite - rich" section, carries trace - <1 % pyrrhotite Fracture zone. Core considerably broken on chloritic fractures most commonly at 20, 50, 60 to core axis.

19 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 12 From-To Rock Type Description Gabbro, minor Gabbro, upper contact sharp at 50 0 to core axis. Gabbro is fine - grained near Sudbury breccia contact, exhibits lenticular banding parallel- subparallel to contact, and is cut by thin green seams of Sudbury breccia at 50 0 to core axis. Sparse thin quartz veins at 70, 80 0 to core axis. End Gabbro is dark greenish gray, medium - grained, massive. Non - magnetic. Carries trace fine - grained disseminated pyrrhotite and pyrite. Rock is cut by sparse, very thin seams of green Sudbury breccia, and by sparse thin quartz veins at 80 0 to core axis. Notes 1. Casing left in hole. 2. No samples taken. ~

20 Property: Airport East Claim No. S MLLSTREAM MNES LTD. DRLL HOLE SURVEY DATA Township: Falconbridge Hole No. MAE Collar Co-ordinates: L S, E UTM: 17T E, N NAD 83 Hole Length: m Approx. 260 m S, 170 m E of #4 post, S Survey Data Survey Type: EZ - Shot Depth Azimuth O Azimuth Dip 0 As Recorded (Astronomic) (Magnetic) Magnetic Field Not recorded

21 Box No L] ~ MLLSTREAM MNES LMTED Box No's and ntervals Airport East Property Hole No. MAE nterval Box No. nterval i :

22 MAE Box No nterval Box No. nterval End

23 ARPORT, i '" \ "" \ ) N -<~ FAlCONBRDGE CJ MLLSTREAM MNES LTD. ARPORT EAST PROPERTY o SCALE 2000m KEY MAP LOCATON OF DRLLNG. 2007, CLAMS S, & S FALCON BRDGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 :

24 S50768 '{C"! '1' lot". CON 3.' MLLSTREAM MNES LTD. ARPORT EAST PROPERTY KEY MAP LOCATON OF CLAMS S & S FALCONBROGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 :20, 000

25 MLLSTREAM MNES LTD. ARPORT EAST PROPERTY #4 Post. S PLAN OF DRLL HOLES MAE , - 02, - 03 & - 04 CLAM S , FALCONBROGE TOWNSHP SUDBURY MNNG DSTRCT SCALE: 1 :2500 N MAE (- 70, 270, m) MAE (- 45, 090, m) ---; ~~ ~~~ ~----r_ _ ~--l3s 19E MAE (- 90,503.0 m) o SCALE 100m

26 Legend MAE (- 70"., 270, m) ( L 3 S E) ov Overburden Precambrian (Proterozoic) Sudbury breccia 4 Sudbury breccia Nipissing Gabbro 3 Gabbro Bruce Formation 2a Pebbly wacke, wacke 2b Paraconglomerate 2c Feldspathic sandstone 2d Quartzite 2e Arkose 2f Siltstone 4 Mississagi Formation 1 a Feldspathic sandstone. minor quartzite. wacke and siltstone 1 b Quartzite, minor wacke 1 c Wacke, minor siltstone fz Fault zone Numerous fracture zones not shown on section. qv Quartz vein zone s Sampled zone Note: Hole not straight. see plan. Section drawn on predominant azimuth m MLLSTREAM MNES L"rD. ARPORT EAST PROPERTY o SCALE 100m SECTON ON DRLL HOLE MAE LOOKNG NORTHEAST CLAM S , FALCONBRDGE TOWNSHP SUDBURY MNNG DSTRCT SCALE: 1 :2500

27 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Township: Falconbridge Claim No. S Hole No. MAE Page 1 Collar Location: L S, E UTM: 17T E, N NAD 83 Approx. 260 m S, 170 m E of #4 post, Azimuth: Dip: 45 0 Total Depth: m Survey Data: See end of log Core Size: BO Date Started: May 30,2007 Date Completed: June 12,2007 Logged By: P. E. Giblin Date Log Completed: August 14, 2007 Drilling Company: RonKor Diamond Drilling Ltd. Core Stored: Millstream Mines Ltd., Potter Mine, Munro Township, ON From - To Rock Type Description Overburden Bruce Formation Paraconglomerate, Dark gray polymictic paraconglomerate, generally sparse pebbles of quartz, granite, diabase, and minor wacke, very mafic metavolcanics, in fine - grained, dark gray, wacke matrix. Exhibits minor crackle brecciation. minor Sudbury Commonly carries trace - «1% fine to medium - grained disseminated pyrite and pyrrhotite. Some breccia pyrrhotite on fractures. Sulphides sometimes clustered about outer margins of some pebbles. Minor thin interbedded wacke. Very minor seams dark Sudbury breccia cut conglomerate and wacke Sudbury breccia Sudbury breccia, dark gray - green. Aphanitic matrix exhibits banding, most commonly at 20 to core axis. Upper contact on chloritic slip at 20 to core axis Wacke, pebbly Dark gray - black, fine - grained, very sparse subangular quartz granules very sparse granite pebbles. wacke, very minor Rare blue quartz granules. Generally massive. Wacke commonly exhibits crackle brecciation. Cut by Sudbury breccia. Sudbury breccia seams Sudbury breccia.

28 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 2 From - To Rock Type Description Diabase fragment Sudbury breccia, dark green gray aphanitic matrix Sudbury breccia, banding most commonly at 50 to core axis Thin pyrite seams comprise c.5% of section Sudbury breccia Wacke, pebbly wacke, minor Sudbury breccia Sudbury breccia Wacke exhibits crackle breccia Bedding at 40 to core axis Banding in Sudbury breccia most commonly at 25 to core axis ChloritiC fracture at 15 to core axis, coated with sparse quartz, pyrite, and trace chalcopyrite Wacke, pebbly wacke Paler gray feldspathic wacke. Crackle breccia common. Fragments commonly exhibit matching walls, are commonly 5-20 mm across, and are separated by thin (c.1 mm thick) bands of very fine - grained dark material. Sparse small quartz pebbles Thin pyrite seams most commonly at 40 to core axis, and disseminated pyrite comprise <5% of section Quartz - pyrite - pyrrhotite vein at 35 to core axis carries c. 10 sulphides.

29 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 3 From - To Rock Type Description Network of thin pyrite - quartz veins, <5% pyrite overall Paracongfomerate, Conglomerate is dark gray green, sparse granite and quartz pebbles in wacke matrix. Pebbles are pebbly wacke, very angular to subangular to subround. Pebbly wacke predominates after c.122. Wacke carries trace fine minor sandstone, - grained disseminated pyrite and chalcopyrite. Conglomerate and wacke exhibit minor crackle very minor Sudbury breccia, which appears to die out c Minor chloritic seams. Very minor thin sandstone units breccia. interbedded with pebbly wacke and wacke. Sandstone units increase in number towards bottom of section Chloritic fractures at 0, 15,30 to core axis Chloritic fractures common at wide variety of angles to core axis. Some fractures coated with paper - thin films of pyrite Pyrite grains clustered around some quartz pebbles Trace fine - grained chalcopyrite Sudbury breccia. Banding most commonly at 35,60 to core axis Pink carbonate vein at 30 to core axis Very sparse quartz - pyrite - trace chalcopyrite veining, and small irregular patches of sulphides. c.1-2% sulphides in section Sudbury breccia, banding at to core axis.

30 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 4 Description Sudbury breccia, upper contact at 40, lower contact at 30 to core axis Mafic pebble carries c.1-2% disseminated pyrrhotite and chalcopyrite Pale gray - white sandstone. Contacts sharp, upper contact at 70, lower contact at 40 to core axis Chloritic slip at 15 to core axis Quartz vein 5 mm thick Sparse, thin, irregular quartz veins 2-5 mm thick at 25,50 to core axis. Veins carry c.5-10% fine - grained pyrite and trace chalcopyrite Thin irregular quartz veins a few mm thick comprise c.5% of section, carry minor pyrite and trace chalcopyrite. Sparse chloritic slips at to core axis , Quartz pebbles are elongated, approximately parallel, at 60 and 45 to core axis, respectively Fracture zone. Core moderately broken on chloritic fractures at 0, 10,30,40,60 to core axis. Minor pyrite and quartz on chloritic fractures Gray green chert, upper contact sharp at 70 to core axis, lower contact gradational. Sparse chloritic fractures at 0, 10,30,40,50 to core axis Fracture zone. Core moderately broken on chloritic fractures at 0,20,80 to core axis. Minor pyrite films on chloritic fractures.

31 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To jmetres) Hole No. MAE Page 5 Description Gray green fine - grained sandstone. Upper contact gradational, lower contact difficult to define. nternal bedding at 50 to core axis Wacke, numerous very thinly bedded, gray to greenish gray fine - grained sandstone, siltstone units Bedding at 70 0 to core axis Bedding at 60 to core axis Gray, greenish gray fine - grained sandstone Bedding at 90 to core axis Fracture zone. Core badly to moderately broken on chloritic fractures at a wide variety of angles Vein breccia zone. Numerous thin. irregular quartz veins c.1 mm thick, comprise c.10% of section. Wallrock is brown in colour Quartz vein 3 mm thick at 50 0 to core axis Fracture zone. Core weakly broken on chloritic fractures at 0, 40, 70 0 to core axis Bedding in thin sandstone beds at 60 to core axis Thin quartz veins c.2-4 mm thick at 25, 40 to core axis. Wall rocks altered to pale green for 5-10 mm on side of veins. Cut by sparse thin seams of Sudbury breccia.

32 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 6 From - To Rock Type Description Fault zone, Sudbury breccia Fracture zone. Core moderately broken at to core axis Fracture zone. Core moderately broken Fracture zone. Core moderately broken on fractures at to core axis Sandstone ends on broken core Sudbury breccia. Dark green to pale green. gabbro fragments in generally pale green, aphanitic matrix. Matrix crudely banded, occasionally contorted. Fragments are often elongated and subparallel at c.30 to core axis Schistose, fault gouge on fracture at 30,40 to core axis Fault gouge Gabbro, minor Sudbury breccia Gabbro is gray to predominantly greenish gray, fine - grained to commonly medium - grained. Most commonly massive, rarely exhibits banding. Carries traces of fine - grained disseminated pyrite, pyrrhotite and chalcopyrite. Gabbro is commonly cut by sparse, generally thin seams of Sudbury breccia, and by generally sparse. thin, quartz. and quartz - carbonate veins, which occasionally carry minor pyrite, chalcopyrite and pyrrhotite. Gabbro is also cut by very sparse, thin, carbonate veins and quartz - hematite veins , Quartz - hematite veins, latter vein 10 mm thick at 30 to core axis Sparse thin quartz veins at 30, 50, 60 to core axis.

33 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 7 From-To Rock Type Description Banding at 70 to core axis Banding, contacts sharp. Upper contact at 60, lower contact at 90 to core axis Sudbury breccia and shear zone. Upper contact sharp at 20 to core axis, chloritic slips at 15 to core axis Very thin banding at 60 to core axis Chloritic fracture at 20 to core axis Quartz vein zone. Several quartz veins 1-30 mm thick, most commonly at 30 to core axis Chloritic slip at 30 to core axis Quartz vein, upper contact at 30 to core axis, lower contact on broken core Sudbury breccia. Green aphanitic bands, fractured quartz, trace fine - grained chalcopyrite Thin seam of Sudbury breccia, 5-10 mm thick at 20 to core axis Green Sudbury breccia Sudbury breccia seam carries bleb of chalcopyrite c.4 mm across Bleb of chalcopyrite c.4 mm cross in thin quartz vein at 30 to core axis Quartz vein 20 mm thick at 25 to core axis, adjacent to a parallel, thinner seam of Sudbury breccia.

34 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 8 Description Fracture zone. Core badly to moderately broken on chloritic fractures with minor hematite stain. Tiny carbonate veins on some fractures carry trace fine - grained chalcopyrite Chloritic fracture at 40 0 to core axis Fracture zone, chloritic fractures at 30 0 to core axis Several thin bands of medium and fine - grained gabbro, each c cm thick. Banding fairly sharp at 90 0 to core axis Quartz vein 10 mm thick at 15 0 to core axis, carries trace fine - grained pyrite Cluster of fine - grained pyrrhotite, chalcopyrite and quartz grains a few mm across Shear zone. Chloritic fractures, minor thin quartz - carbonate veins at 30 0 to core axis Quartz vein at 20 0 to core axis , Thin carbonate veins c.1 mm thick at 40,20 to core axis respectively Thin seam dark Sudbury breccia at 0, 30 0 to core axis Dark Sudbury breccia seam 15 mm thick at 30 to core axis, carries a central quartz - pyritetrace chalcopyrite vein 5 mm thick Several thin seams of green Sudbury breccia Several tiny quartz - pyrite - chalcopyrite veins in Sudbury breccia.

35 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 9 Description Several thin seams of dark Sudbury breccia, often with thin central quartz and quartz - carbonate veins a few mm thick, most commonly at to core axis Trace fine - grained disseminated chalcopyrite in gabbro Sudbury breccia Quartz vein 5 mm thick at 50 to core axis Quartz veins 2-10 mm thick comprise c.1 % of section. Veins most commonly at 0, 25,30,85 to core axis Sparse fine - grained chalcopyrite in thin Sudbury breccia seam Sudbury breccia seam 5-10 mm thick at 35 to core axis Sample R Quartz vein zone, minor Sudbury breccia Several quartz veins 2-5 mm thick, minor Sudbury breccia. Many veins carry clusters of fine - grained pyrrhotite, chalcopyrite, and pyrite. Sulphide clusters up to 10 mm across. Overall c.1-2% quartz veins and «1% chalcopyrite. Lower contact of zone on chloritic slips at 20,25 to core axis Sample R Sample R 8603 i Sample R Sample R Chloritic slip at 20, 35 to core axis Chloritic slip at 40 to core axis.

36 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 10 From - To End Rock Type Description Quartz veins, chloritic slips at 30, 50 to core axis Sudbury breccia and quartz vein 5 mm thick at 15 to core axis Sparse fine - grained chalcopyrite in gabbro Green Sudbury breccia zone at 40 to core axis, parallel chloritic slips Several chloritic slips at 0,20,40 to core axis Minor Sudbury breccia in gabbro, numerous thin quartz veins. Notes 1. Casing left in hole. 2. Assays by Swastika Laboratories Ltd., Assay Certificate no. 7W-3375-RA, Nov ~

37 MLLSTREAM MNES LMTED SAMPLE AND ASSAY DATA Property: Airport East Sample No. nterval Length Hole No. MAE Lithology Page 1 Au Au Check Pt Pd ppb ppb ppb ppb R Gabbro, very minor Sudbury breccia 24 - <5 7 R R R Quartz vein zone, minor pyrrhotite. chalcopyrite and pyrite, minor Sudbury breccia... ".... " " " ".. " ".. " " 27 - <5 < < <5 17 R Gabbro 7 - <5 7 Assays by Swastika Laboratories Ltd., Assay Certificate 7W-3375-RA Nov,01,2007

38 Company: Project: Attn: 11/81/ : SWASTKA LA8C~ATORE PAGE 81/131 Established \/28 Assay Cel:!:E[icate MD..lSTREAM Ml\'ES LTD MAE M. Martinello We hereby certify the followir.g Assay of 5 Core sample~; submitted OCT by. Swastika Lat,oratori(~s Ltd Assa.ying ~ ConsuJting Re.presentati.)!l SaJ.1)le Au Au Check Pt Pd i:c:i!! ----~ --.. ~ ~i! ~ ~~ ~,_ <:5 < <: <:3 1 ; <:S i 7W RAt Date: NOV-O _.. _ _ _ _.. _ _... _._ Cameron Ave., P.O. Box 10, Swastika, Ontario POK JTO Telephone (70S) Fax (70S)

39 Property: Airport East Claim No MLLSTREAM MNES LTD. DRLL HOLE SURVEY DATA Township: Falconbridge Hole No. MAE Collar Co-ordinates: L , E UTM: 17T E N NAD 83 Hole Length: m Depth i Approx. 260 m 5, 170 m E of #4 post, Azimuth V As Recorded (Magnetic) Survey Data Survey Type: EZ - Shot Azimuth v (Astronomic) 090 Not recorded Not recorded Dipu Magnetic Field

40 Box No i i MLLSTREAM MNES LMTED Box No's and ntervals Airport East Property Hole No. MAE nterval Box No. nterval End

41 ARPORT ;-... i '... -~ \... \ ) N -(~ FALCONBRDGE (] MLLSTREAM MNES LTD. ARPORT EAST PROPERTY o SCALE 2oo0m KEY MAP LOCATON OF DRLLNG, 2007, CLAMS S & S FALCONBRDGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 :50, 000 (

42 ~ -~"'~;~t ~Qd S ~ "-.. _.- -_._ , ~ ' \ \,) <~~ ~ '1' lot 4. CON 3... MLLSTREAM MNES L TO. ARPORT EAST PROPERTY KEY MAP LOCATON OF CLAMS S & S j- FALCONBRDGE TOWNSHP, SUDBURY MNNG DSTRCT -----~ "--...., SCALE 1 :20, 000

43 --_.- #4 Post MLLSTREAM MNES LTD. ARPORT EAST PROPERTY PLAN OF DRLL HOLES MAE , - 02, - 03 & - 04 CLAM S , FALCON BRDGE TOWNSHP SUDBURY MNNG DSTRCT SCALE: 1 :2500 N MAE (- 70, 270, m) MAE (- 45, 090, m) ---t ~~ ~~~------~~--~ ~ ~--l3s 19 E MAE ( 90, m) o SCALE 100m

44 MAE (- 45, Ogoo, m) ( L 3 S, E ) --..f)--- L 3 S ov Legend ov Overburden Precambrian (Proterozoic) Sudbury breccia 4 Sudbury breccia Nipissing Gabbro 3 Gabbro Bruce Formation 2a Pebbly wacke, wacke 2b Para conglomerate 2c Feldspathic sandstone 2d Quartzite 2e Arkose 2f Siltstone m Mississagi Formation 1 a Feldspathic sandstone, minor quartzite, wacke and siltstone 1 b Quartzite, minor wacke 1c Wacke, minor siltstone fz Fault zone Numerous fracture zones not shown on section. qv Quartz vein zone s Sampled zone Note: Hole not straight, see plan. Section drawn on predominant azimuth. o SCALE 100m ') MLLSTREAM MNES LTD. ARPORT EAST PROPERTY SECTON ON DRLL HOLE MAE LOOKNG NORTHEAST CLAM S , FALCONBRDGE TOWNSHP SUDBURY MNNG DSTRCT SCALE: 1 :2500

45 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Township: Falconbridge Claim No. S Hole No. MAE Page 1 Collar Location: L S, E UTM: 17T E, N NAD 83 Approx. 276 m S, 174 m E of #4 post, S Azimuth: 225 Dip: 60 Total Depth: m Survey Data: See end of log Core Size: BO Date Started: June 18, 2007 Date Completed: June 28, 2007 Logged By: P. E. Giblin Date Log Completed: Sept. 22, 2007 Drilling Company: RonKor Diamond Drilling Ltd. Core Stored: Millstream Mines Ltd., Potter Mine, Munro Township, ON From- To Rock Type Overburden Description Pebbly wacke, minor Sudbury breccia Sudbury breccia zone Bruce Formation Dark gray, fine - grained pebbly wacke, sparse pebbles principally of quartz and granite, quartz granules common. Bedding generally absent. Carries sparse small blebs of pyrrhotite and pyrite, rare trace very fine - grained chalcopyrite. Wacke commonly exhibits crackle breccia. Sulphides often concentrated in the very thin fractures of crackle breccia, and occasionally concentrated on outer margins of some pebbles. Rock is cut by minor Sudbury breccia seams, and by generally sparse chloritic fractures often coated with thin pyrite films Sudbury breccia and fracture zone Fracture zone. Core badly to considerably broken on chloritic fractures most commonly at 0, 10, 20, 40, 70 to core axis. Dark gray, greenish gray, tiny quartz grains in aphanitic matrix. Matrix often thinly banded. Breccia seams cut wacke. Wacke clasts often exhibit crackle breccia. Sudbury breccia often carries trace - <1 % fine - grained pyrrhotite and fine - grained pyrite, and very sparse thin quartz veins, generally a few mm thick.

46 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 2 From-To Rock Type Description Banding in Sudbury breccia at 30 to core axis Banding at 25 to core axis , Banding at 30 to core axis Fracture zone. Core weakly broken on chloritic - pyritic fractures most commonly at 10, 20 to core axis Pebbly wacke, minor Sudbury breccia Fracture and fault zone Pebbly wacke exhibits crackle breccia and carries trace - <1% fine - grained pyrrhotite and pyrite, often in the dark, very fine - grained material filling fractures in crackle breccia. Wacke is cut by minor Sudbury breccia carrying trace - <1% fine -- grained pyrrhotite and pyrite. Sudbury breccia, fractured Thin seam of fault gouge at 30 to core axis Fracture zone. Core badly to considerably broken, very thin pyrite films often coat chloritic fracture surfaces Quartz vein 5 mm thick at 30 to core axis, upper contact on chloritic slip Fracture zone. Core moderately broken on chloritic fractures most commonly at 20,30 to core axis Sudbury breccia seam 30 mm thick at 30 to core axis Fracture zone. Core weakly broken on chloritic fractures most commonly at 10, 20, 70 to core axis.

47 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 3 Description Banding in Sudbury breccia at 25 to core axis Fracture zone. Core moderately broken on chloritic fractures at 10, 80 to core axis Fracture zone. Core moderately broken on chloritic fractures at wide variety of angles Fracture zone. Core broken on fractures at 0,20 to core axis Sudbury breccia zone. FOliation at 25 to core axis Fracture zone. Core moderately broken on fractures at 10,30 to core axis Granite cobble in wacke Sudbury breccia zone Predominantly Sudbury breccia, wacke fragments Several thin bands of dark Sudbury breccia in predominantly pale green Sudbury breccia. Dark bands are 5-10 mm thick and carry trace chalcopyrite, minor pyrite. Mississagi Formation Feldspathic Gray, white to purple feldspathic sandstone. Occasionally exhibits very thin wacke and siltstone sandstone, very. interbeds. Carries trace - <1 % fine - grained disseminated pyrite. Pyrite films occur on many chloritic minor interbedded! fractures. wacke and siltstone

48 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 4 Description Bedding at 30 to core axis Bedding at 25 to core axis Fracture zone. Core considerably broken on chloritic fractures most commonly at 30 to core axis Fracture zone. Core considerably broken on chloritic fractures at 10, 30, 70 to core axis Bedding at 35 to core axis Siltstone, minor wacke lenses Bedding at 30 to core axis Quartz vein 5 mm thick at 10 to core axis Quartz veins 5-30 mm thick at to core axis Bedding at 40 to core axis Lower contact offeldspathic sandstone on chloritic slip at 50 to core axis Wacke, very minor Wacke carries trace pyrrhotite, some as very thin veins parallel to bedding. siltstone Fracture zone. Core considerably broken at 30,40 to core axis Quartz - carbonate vein breccia, vuggy, 20 mm thick.

49 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 5 Description Quartz vein 25 mm thick at 65" to core axis, carries very minor pyrite and pyrrhotite Bedding, wacke and siltstone laminae, at 20 to core axis Bedding at 35 to core axis Siltstone unit and fracture zone. Core badly to considerably broken on chloritic fractures, most commonly at , 60 to core axis Carbonate vein 5 mm thick at 25 to core axis Feldpsathic sandstone, minor wacke Wacke, minor siltstone, very minor feldspathic sandstone Gray - white feldpsathic sandstone, minor interbedded thin wacke. Upper contact at 15 to core axis, lower contact at 40 to core axis. Wacke, carries trace very fine - grained disseminated pyrite. Minor very thin siltstone beds. Sparse thin quartz veins Bedding at 50 to core axis Feldspathic sandstone. Upper contact at 45, lower contact at 35 to core axis Feldspathic sandstone. Upper contact on chloritic slip at 30, lower contact with wacke sharp at 40 to core axis Bedding at 20 to core axis.

50 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page Feldspathic sandstone. Description Feldspathic sandstone. Upper contact at 20 0, lower contact on chloritic slip at 25 to core axis Pink arkose Sudbury breccia, fracture and fault zone Very thinly banded Sudbury breccia Foliation at 30 0 to core axis Fracture zone. Core badly to considerably broken on chloritic fractures most commonly at 20, 40 0 to core axis Fault gouge 5 mm thick at 30 0 to core axis Feldspathic sandstone, minor quartzite, very minor interbedded wacke, very minor Sudbury breccia Gray, gray white, mottled pink, feldspathic sandstone, sparse red - purple laminae. Cut by minor Sudbury breccia. Upper contact at 30 0 to core axis Fracture zone, largely in Sudbury breccia. Core badly to considerably broken, most commonly at 0, 30 0 to core axis. Fractures often coated with pyrite films Fracture zone. Core moderately broken on fractures most commonly at 0,20 0 to core axis Fracture zone. Core badly to moderately broken. Fractures most commonly at 20, 70 to core axis.

51 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 7 Description Carbonate vein, vuggy, 2-5 mm thick at 40 to core axis Bedding at 50 to core axis Fracture zone. Core badly to moderately broken on fractures at to core axis Fracture zone. Core moderately to badly broken Fracture zones. Core badly to moderately broken on chloritic fractures most commonly at 0, 10, 40 to core axis Bedding at 40 to core axis Fracture zone. Core badly to considerably broken on chloritic fractures most commonly at 0, , 70 to core axis Bedding at 40 to core axis in gray white feldspathic sandstone Sudbury breccia. fault breccia Sudbury breccia zone 30 mm thick at 15 to core axis, includes parallel fault breccia 5 mm thick and quartz vein 5 mm thick. Vein carries minor pyrite and trace chalcopyrite Bedding at 30 to core axis rregular pyrrhotite grains a few mm across Wacke. carries fine - grained pyrrhotite. Bedding at 30 to core axis Wacke.

52 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 8 From - To Rock Type Description Bedding at 20 to core axis Fracture zone. Core moderately broken on chloritic fractures most commonly at 10, 30,50 to core axis Bedding at 30 to core axis Quartzite. White, fine to medium - grained. Exhibits minor crackle breccia, carries trace fine - grained disseminated pyrite and pyrrhotite. Minor hematite on fractures Quartz vein 5 mm thick at 20 to core axis Wacke Fine - grained wacke, predominantly massive, minor very thin bedding. Exhibits weak crackle breccia. Upper contact gradational Bedding at 70 to core axis Feldspathic sandstone Wacke Gray white, mottled by red - purple streaks. Short sections of quartzite. Upper contact on broken core, lower contact gradational Feldspathic sandstone Bedding at 35 to core axis. Lower contact sharp at 55 to core axis.

53 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 9 Description Wacke, minor feldspathic sandstone Feldspathic sandstone, very minor interbedded wacke Bedding at 45 0 to core axis. Lower contact gradational Bedding at 50 0 to core axis Fracture zone. Core moderately to considerably broken on chloritic fractures most commonly at 0, 15, 30, 60 0 to core axis Fracture zone. Core moderately broken on chloritic fractures most commonly at 0, 10, 30 0 to core axis Fracture zone. Core broken on chtoritic fractures most commonly at 20,30,40 0 to core axis Quartzite Wacke Feldspathic sandstone Gray white in general, minor reddish purple laminae typically 2-5 mm thick and c.20 mm apart (hematitic cross - beds?) Bedding at 40 0 to core axis. Lower contact gradational over a few cm. Wacke carries trace - <1% fine - grained pyrite and pyrrhotite as disseminated grains and in tiny fractures. Upper and lower contacts gradational. Very sparse tiny veins of pyrrhotite and pyrite Fracture zone. Core moderately broken on chtoritic fractures most commonly at 10, 30 to core axis.

54 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 10 From-To Rock Type Description Wacke Lower contact fairly sharply gradational Quartzite Quartzite, very minor interbedded thin wacke units Bedding at 40 to core axis Quartz vein. Upper contact on chloritic slip at 30 to core axis, lower contact very irregular. Vein carries trace pyrrhotite and pyrite in thin dark seams 1-2 mm thick at to core axis. Vein cut by chloritic - pyritic fracture at 70 to core axis Fracture zone. Core weakly broken on chloritic fractures most commonly at 0, 10, 70 to core axis Fracture zone. Core weakly broken on fractures most commonly at 0,30,70 to core axis Fracture zone. Core considerably to moderately broken on chloritic fractures most commonly at 0, 10, 50 to core axis Quartz vein breccia zone 10 mm thick, generally at 10 to core axis, carries trace pyrite Feldspathic , Fracture zones. Core moderately broken on chloritic fractures sandstone most commonly at 20,30,80 to core axis. End Fracture zone. Core weakly broken on chloritic fractures most commonly at 10, 20, 30 to core axis.

55 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 11 From- To Rock Type Description Notes 1. Casing left in hole. 2. No samples taken. ~

56 Property: Airport East Claim No. S MLLSTREAM MNES LTD. DRLL HOLE SURVEY DATA Township: Falconbridge Hole No. MAE Collar Co-ordinates: L S, E UTM: 17T E, N NAD 83 Hole Length: m Approx. 276 m S, 174m E of #4 post, S Survey Data Survey Type: EZ - Shot Depth Azimuth O Azimuth 0 Dip" As Recorded (Astronomic) (Magnetic) Magnetic Field

57 Box No ~..-~ !---= ! ~. 22 i Ts i 29! 30! ~ MLLSTREAM MNES LMTED Box No's and ntervals Airport East Property Hole No. MAE nterval Box No. nterval ! End

58 ARPORT N -(~ FAlCONBRDGE MLLSTREAM MNES LTD. ARPORT EAST PROPERTY o, SCAlE 2000m KEY MAP LOCATON OF DRLLNG, 2007, CLAMS S & S FALCONBRDGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 : r "

59 \ 12149n " '1~" l '1" lor 4. CON 1 MLLSTREAM MNES LTD. ARPORT EAST PROPERTY KEY MAP LOCATON OF CLAMS S & S FALCONBRDGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 :20, 000

60 ---- # 4 Post. S MLLSTREAM MNES LTD. ARPORT EAST PROPERTY PLAN OF DRLL HOLES MAE , - 02, - 03 & - 04 CLAM S , FALCONBRDGE TOWNSHP SUDBURY MNNG DSTRCT SCALE: 1 :2500 N MAE (- 70 0, 270, m) MAE (-45,090,401.0 m) ---t ~ ~~ ~~--+_ ~ ~~l3s 19 E MAE ( - 90, m) o SCALE 100m

61 SCALE: Legend ov Overburden Precambrian (Proterozoic) Sudbury breccia 4 Sudbury breccia Nipissing Gabbro 3 Gabbro 245 -_""1:""---- Bruce Formation 2a Pebbly wacke, wacke 2b Paraconglomerate 2c Feldspathic sandstone 2d Quartzite 2e Arkose 2f Siltstone Mississagi Formation 1 a Feldspathic sandstone. minor quartzite, wacke and siltstone 1 b Quartzite, minor wacke 1 c Wacke, minor siltstone fz Fault zone Numerous fracture zones not shown on section. qv Quartz vein zone s Sampled zone Note: Hole not straight, see plan. Section drawn on predominant azimuth. o SCALE 100m m 1a,C, b.4 MAE (- 60,225,413.0 m) (l S E) ov MLLSTREAM MNES LTD. ARPORT EAST PROPERTY SECTON ON DRLL HOLE MAE LOOKNG NORTHWEST CLAM S , FALCONBRDGE TOWNSHP SUDBURY MNNG DSTRCT 1 :2500.L- ~

62 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Township: Falconbridge Claim No. S Hole No. MAE Page 1 Collar Location: L S, E UTM: 17T E, N NAD 83 Approx. 260 m S, 70 me of #4 post, S Azimuth: N/A Dip: 90 Total Depth: m Survey Data: See end of log Core Size: BO Date Started: July 06, 2007 Date Completed: July 18, 2007 Logged By: P. E. Giblin Date Log Completed: August 25, 2007 Drilling Company: RonKor Diamond Drilling Ltd. Core Stored: Millstream Mines Ltd., Potter Mine, MUnro Township, ON From - To Rock Type Overburden DeSCription Pebbly wacke, minor Sudbury breccia Bruce Formation Pebbly wacke characterized by dark gray, fine - grained matrix, sparse quartz and granite pebbles, rare gabbro pebbles, sparse granite cobbles, and very rare boulders. Wacke is generally massive, rarely exhibits bedding. Rock commonly exhibits crackle brecciation. Very minor pyrite and pyrrhotite occur as disseminated grains and less commonly in tiny fractures. Numerous thin seams of dark Sudbury breccia cut wacke. Wacke is commonly fractured by sparse chloritic slips, some of which are coated with thin films of pyrite. Wacke occasionally exhibits schistosity Fracture zone, core moderately broken Tiny pyrite veins Very sparse fine - grained pyrite and pyrrhotite Fracture zone. Core moderately broken, fractures most commonly at 20, 30, 40 to core axis Gray - brown arkose boulder Fracture zone. Core weakly broken on fractures at 20 to core axis.

63 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 2 From- To Rock Type Description Dark green Sudbury breccia Fracture zone. Core moderately to badly broken, strong crackle breccia in pale brown pebbly wacke, very thin seams of dark Sudbury breccia in crackle breccia Fracture zone. Core moderately to considerably broken on fractures most commonly at 0, 10, 40 to core axis Fracture zone. Core considerably broken on fractures most commonly at 10, 20 to core axis , Fracture zones, core moderately to considerably broken on fractures at 15, 30, 80 to core axis Fracture zone. Core badly to considerably broken on fractures most commonly at 10, 50 to core axis Fracture zone. Core considerably broken on fractures most commonly at 15, 20, 60 to core axis Fracture zone. Core considerably to badly broken on fractures most commonly at 25, 35, 60 to core axis Wacke carries trace - <1 % fine - grained pyrite and pyrrhotite as disseminated. grains and as tiny streaks.. / Fracture zone, core considerably broken on fractures at 20,60 to core axis.

64 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE ;., 04 Page 3 Description Sudbury breccia. Thin green aphanitic bands Gray granite boulder Fracture zone. Core considerably to badly broken, most commonly on fractures at 20,50 to core axis Fracture zone. Core moderately to considerably broken on fractures most commonly at 20,30 to core axis Schistosity at 30 0 to core axis Fracture zone. Core moderately broken on fractures most commonly at 20 to core axis Fracture and fault zone Fracture zone. Core considerably to badly broken on fractures most commonly at. 40 to core axis. ncludes fault breccia as noted below Fault breccia. Small angular wallrock fragments, up to 25 mm across, in dark green gray, very fine - grained matrix (fault gouge?) Fracture zone. Core moderately to badly broken on chloritic fractures most commonly at 30,40,60 0 to core axis Fracture zone. Core moderately broken on fractures at 30,40,50 to core axis Fracture zone. Core moderately to badly broken on fractures most commonly at 15, ' 20, 40 to COre axis.

65 MLLSTREAM MNES LMTED DAMOND DRilL RECORD Property: Airport East From - To Rock Type Hole No; MAE Page 4 Description Trace chalcopyrite with pyrite on chloritic fracture , Very thin bedding in wacke at 30 to core axis Wacke carries several granite cobbles Wacke carries tiny streaks of pyrite and pyrrhotite as well as fine - grained disseminated pyrite and pyrrhotite. Sulphide streaks are most commonly in dark fractures at 30 to core axis. Sulphides comprise <1 % of section Pyrite vein <1 mm thick at 85 to core axis.. Sudbury breccia prominent, wacke clasts Sudbury breccia zone Foliation due to parallel Sudbury breccia seams, and some parallel clasts, at 40 to core axis Granite fragment Banding in Sudbury breccia at 40 to core axis Pyrite film on chloritic slip at 40 to core axis Pebbly wacke Mid- gray to dark gray, small granite and quartz pebbles; Foliation due to numerous very thin, dark seams at 25 to core axis. Carries trace very fine - grained disseminated pyrite.

66 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 5 From- To Rock Type Description Sudbury breccia zone Dark thin seams of Sudbury breccia, wacke clasts Several grains and tiny streaks of fine - grained pyrite Foliation at 25 to core axis Fracture zone. Core badly to considerably.broken. Fractures most commonly at 40 to core axis , Fracture zones, core moderately broken on fractures most commonly at 30,40 to core axis Pebbly wacke, minor Sudbury breccia Wacke exhibits minor intermittent crackle breccia, and also intermittent schistosity. Carries trace fine - grained disseminated pyrite and trace pyrite in tiny veins. Wacke cut by generally very thin seams of dark green Sudbury breccia, and is also cut by occasional chloritic fractures Fracture zone. Core moderately broken on fractures at 30,40,60 to core axis Arkose Pale gray to mottled gray - white and dark green - gray. Angular gray - white feldspar grains up to 4 mm across comprise c.50% of rock, with minor fine - grained quartz in a very fine - grained matrix; Rock is commonly fractured at 30, 40, 50 to core axis. Upper contact is gradational, lower contact on Sudbury breccia fracture zone Sudbury breccia Wacke, granite and quartz fragments, often round to subround,some clasts elongated, elliptical, in generally dark gray to dark green aphanitic matrix. Matrix is often banded. Breccia matrix often carries trace fine - grained pyrite.

67 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 6 From - To Rock Type Description Fracture zone. Core badly to moderately broken Fracture zone. Core moderately broken Fracture zone. Core badly to moderately br9ken on fractures most commonly at O. 10, 40 to core axis Fault and fracture Fracture zone. Core badly broken. Rock is in part silicified. vuggy. carries trace pyrite zone in tiny veins Fault breccia. Small angular fragments of green aphanitic Sudbury breccia matrix material, tiny pyrite seam Fracture zone. Core considerably broken Fracture zone. Core considerably to badly broken Foliation in Sudbury breccia at 40 to core axis rregular pyrite vein 1-2 mm thick rregular quartz vein Quartz vein 15 mm thick at 90 to core axis, carries minor pyrite.

68 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 7 Description Wacke, minor Sudbury breccia Fine - grained, dark gray, massive, cut by minor seams of green aphanitic Sudbury breccia. Wacke carries trace fine - grained pyrite ,309.37, Quartz veins 5,2 and 10 mm thick respectively, at 90,30,70 to core axis respectively. ' Fracture zone. Core considerably broken on fractures most commonly at 0,40,50 to core axis Sudbury breccia zone Upper contact at 40 to core axis. Generally dark gray, very fine - grained to aphanitic matrix that often exhibits contorted banding. Carries numerous clasts of gray granite in upper part ohection. Clasts are subround to angular, some internally brecciated. Larger clasts c.s - 20 mm predominate to c.333, thereafter pebble-sized clasts most common. Wacke, quartz, sparse granite and very sparse sandstone clasts dominate most of section. Breccia matrix carries trace pyrite and pyrrhotite. Sparse very thin quartz veins present. Thin pyrite films often coat chloritic fractures Trace chalcopyrite in thin pyrite film on fracture at 90 to core axis Banding in Sudbury breccia at 60 to core axis Banding at 50 to core axis c Fracture zone. Core badly to considerably broken on chloritic fractures most commonly at 10, 40, 50, 80 to core axs Fracture zone. Core moderately broken on fractures at 0, 50, 60, 70 to core axis.

69 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Foliation at 50 to core axis. Hole No. MAE Page 8 Description rregular quartz vein Quartz vein 10 mm thick at 40 to core axis Several quartz veins 2-15 mm thick at to core axis Banding in Sudbury breccia at 40 to core axis. c c Trace - «1% fine - grained pyrrhotite + pyrite in fractures, and in very thin quartz veins Trace chalcopyrite associated with pyrrhotite h"t quartz vein 5 mm thick at 40 to core axis Fault and fracture zone Fracture zone. Core considerably to moderately broken on fractures most commonly at 0, 10,30,70 to core axis Fracture and fault zone. Core badly to considerably broken, short sections offault breccia and fault gouge as noted below Quartz vein 3 mm thick at 60 to core axis; Carbonate - quartz vein 5 mm thick at 80 to core axis Fault breccia and fault gouge.. Contacts at 60 to core axis , Thin seams of fault gouge 2-3 mm thick at 60 and 75 to core axis respectively.

70 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 9 Description Fault breccia. Small angular fragments of wallrock in fault gouge. Trace pyrite. Upper contact at 70 to core axis. Lower contact on chloritic slip at 45 to core axis. c c Several thin quartz - carbonate veins at to core axis Banding in Sudbury breccia at 65 to core axis Fracture zone. Core weakly broken on chloritic fractures at 0, 25, 60 to core axis Banding in Sudbury breccia ~t 50 to core axis Quartz vein breccia. Several very thin quartz veins, 1-3 mm thick Pebbly wacke, minor Sudbury breccia Sparse granite cobbles, common quartz granules in dark fine - grained matrix. Wacke exhibits crackle breccia, carries trace fine - grained pyrrhotite, and is cut by minor Sudbury breccia Fracture zone. Chloritic fractures at 10 to core axis Carbonate vein 10 mm thick at 60 to core axis Quartz vein mm thick at 60 to core axis, carries c.5% pyrrhotite Fracture zone. Core weakly fractured on chloritic slips at 20,60,70 to core axis, Very sparse thin quartz veins Thin green Sudbury breccia seam 5 mm thick at 50 to core axis. i

71 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 10 From- To Rock Type Description Green Sudbury breccia Thin irregular quartz vein carries considerable pyrrhotite Carbonate vein 2-5 mm thick at 45 to core axis, exposed on fracture surface at 60 to core axis. Vein carries several grains of galena, trace chalcopyrite, pyrrhotite and pyrite. Nearby fractures carry trace pyrrhotite Sudbury breccia, carries minor pyrrhotite Sudbury breccia, green aphanitic matrix exhibits subparallel banding at 80 to core axis Gabbro, quartz Dark green gray, fine to medium - grained. Cut by minor thin quartz and quartz - carbonate veins, and gabbro, minor by minor Sudbury breccia seams. Contacts of gabbro are in Sudbury breccia zones. Sudbury breccia Sudbury breccia, thin seams of green Sudbury breccia most commonly at 50, 80 to core axis. Numerous thin subparallel quartz veins cut banding of breccia Gabbro is cut by very numerous thin, generally subparallel, carbonate veins, which comprise c % of section rregular quartz vein and thin seam of Sudbury breccia Thin carbonate veins generally parallel at 70 to core axis.

72 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 11 Description , rregular quartz vein Sudbury breccia Upper contact at 25 to core axis. Banding in breccia parallel to contact. Cut by c.2-5% thin irregular quartz veins and by minor thin carbonate veins Quartz vein 5-10 mm thick at to core axis, carries minor pyrite Banding in breccia at 30 to core axis Banding in breccia at 35 to core axis. End Notes 1. Casing left in hole. 2. No samples taken.

73 MLLSTREAM MNES LTD. DRLL HOLE SURVEY DATA Property: Airport East Township: Falconbridge Hole No. MAE Claim No. S Collar Co-ordinates: L S, E UTM: 17T E, N NAD 83 Hole Length: m Approx. 260 m S, 70 m E of #4 post, S Survey Data Survey Type: EZ - Shot Depth Azimuth O Azimuth Dipo Magnetic Field As Recorded (Astronomic) (Magnetic) (?} Not available

74 Box No. 1 ~ i r ! ~ i MLLSTREAM MNES LMTED Box No's and ntervals Airport East Property Hole No. MAE nterval Box No. nterval. Lmetrest

75 MAE Box No ~ r--rs nterval Box No. nterval End

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78 ----- #4 Post MLLSTREAM MNES LTD. ARPORT EAST PROPERTY PLAN OF DRLL HOLES MAE , - 02, - 03 & - 04 CLAM S , FALCONBRDGE TOWNSHP SUDBURY MNNG DSTRCT SCALE: 1 : N MAE (- 70, 270, m) MAE (- 45, 090, m) ---; ~~ ~~~ ~----+_ _ _--L3S 19 E MAE ( - 90, m) o SCALE 100m,

79 Legend ov Overburden - Precambrian (Proterozoic) Sudbury breccia 4 Sudbury breccia Nipissing Gabbro 3 Gabbro Bruce Formation 2a Pebbly wacke, wacke 2b Paraconglomerate 2c Feldspathic sandstone 2d Quartzite 2e Arkose 2f Siltstone Mississagi Formation 1 a Feldspathic sandstone, minor quartzite, wacke and siltstone 1 b Quartzite, minor wacke 1 c Wacke, minor siltstone fz Fault zone Numerous fracture zones not shown on section. qv Quartz vein zone s Sampled zone Note: Hole not straight, see plan. Section drawn on predominant azimuth. MLLSTREAM MNES LTD. ARPORT EAST PROPERTY SECTON ON DRLL HOLE MAE LOOKNG EAST CLAM S , FALCONBRDGE TOWNSHP SUDBURY MNNG DSTRCT SCALE: 1 :2500 fz MAE ( - 90, m) (L 3 S, E) m fz - fz: 2a,4... "'" ov 2a, r- 2a _4 2a,4 ~ ~ 2e 4 :... 2a,4 '"- 4,2a o SCALE 100m ' _--_1. L

80 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Township: Falconbridge Claim No. S Hole No. MAE Page 1 Collar Location: L 8+00N,15+25E UTM: 17T E, N NAD83 Approx.260mS,20mWof#1post,S Azimuth: N/A Dip: 90 Total Depth: m Survey Data: See end of log Core Size: BO Date Started: July 19, 2007 Date Completed: August 01, 2007 Logged By: P. E. Giblin Date Log Completed: October 05, 2007 Drilling Company: RonKor Diamond Drilling Ltd. Core Stored: Millstream Mines Ltd., Potter Mine, Munro Township, ON From- To Rock Type Description Overburden Pebbly wacke, very minor quartzite and Sudbury breccia Bruce Formation Pebbly wacke characterized by dark gray, fine - grained matrix, sparse quartz and granite pebbles, very sparse granite cobbles, and very rare boulders. Wacke is generally massive, rarely exhibits bedding. Rock commonly exhibits crackle brecciation. Very minor pyrite and pyrrhotite occur as disseminated grains and less commonly in tiny fractures. Numerous thin seams of dark Sudbury breccia cut wacke. Wacke is commonly fractured by sparse chloritic slips, some of which are coated with thin films of pyrite. Wacke occasionally exhibits schistosity Fracture zone. Core moderately to badly broken on chloritic fractures most commonly at 20,30,60 to core axis Fracture zone. Core considerably broken on chloritic fractures at 0, 10,40,70 to core axis Fracture zone. Core weakly broken on chloritic fractures most commonly at 10, 40, 60 to core axis.

81 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 2 From- To Rock Type Description Bedding at 65 to core axis Fracture zone. Core considerably broken on chloritic fractures most commonly at 10, 20, 30, 60 to core axis Sudbury breccia seam 30 mm thick, quartz vein 2 mm thick parallel to banding at 30 to core axis Bedding at 35 to core axis Considerable pyrite on chloritic fractures at a, 10 to core axis Quartz vein 5 mm thick at 55 to core axis carries trace pyrite Quartz vein in fracture zone, vein bounded by chloritic slips at 20 to core axis Fracture zone. Core considerably broken on chloritic fractures most commonly at to core axis Fracture zone. Core weakly broken on fractures at to core axis Quartzite. Pale gray. cream. in colour with irregular reddish purple marginal zones a few cm thick. Carries minor disseminated pyrrhotite and pyrite Arkose Arkose is cut by many very thin quartz veins generally <1 mm thick.

82 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From - To Rock Type Hole No. MAE Page 3 Description Fracture and fault zone, fault breccia Fault breccia 35 mm thick, small angular fragments in patchy irregular quartz. matrix, bounded on both margins by fault gouge c.10 mm thick. Foliation in gouge at 60 to core axis Fracture zone. Core badly broken Pebbly wacke, Sudbury breccia, very minor quartzite and feldspathic sandstone Pebbly wacke cut by minor Sudbury breccia. Very minor interbedded quartzite and sandstone , Fracture zones. Core considerably broken Fracture zone. Core considerably broken on fractures most commonly at 30 to core axis Quartz vein 1-3 mm thick at 30 to core axis, carries trace pyrite and exhibits bleached wallrock zones 2-5 mm thick Quartz vein 10 mm thick at 25 to core axis carries trace - <1% pyrite, wallrocks bleached to pale gray for c.10 mm on each side Disseminated pyrrhotite comprises c.1 % of section Quartzite, pale gray, trace - «1% disseminated pyrite. Upper contact sharp at 40 to core axis, lower contact gradational Pebbly wacke carries c.5% disseminated pyrite Breccia, quartz c.1 % pyrite over section.

83 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 4 Description Thin bands of green Sudbury breccia 5 mm thick, quartz vein 5 mm thick, minor pyrrhotite. Breccia seam and vein both at 25 to core axis Quartz vein 20 mm thick at 30 to core axis Quartz vein 5 mm thick at 25 to core axis, carries trace pyrite Quartz vein 5 mm thick at 20 to core axis, carries sparse pyrrhotite, pyrite, and trace chalcopyrite (?) Quartz vein 20 mm thick at 25 to core axis Quartz vein 10 mm thick at 20 to core axis, trace pyrite Pebbly feldspathic sandstone, pale gray - white. Exhibits crackle breccia. Upper contact at 25() to core axis, lower contact gradational Fracture zone. Core weakly broken on chloritic fractures most commonly at 0, 10, 20 to core axis Breccia zone, dark gray, foliation at 50 to core axis, carries c.2-4% pyrrhotite and lesser pyrite, trace chalcopyrite Quartz vein 20 mm thick carries minor pyrite. Upper contact on chloritic slip at 45, lower contact at 45 to core axis Blebs of disseminated pyrrhotite comprise c.1-2% of section.

84 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 5 Description Fracture zone. Core weakly broken on chloritic fractures most commonly at OS, 20, 65 to core axis Quartzite, pale gray - white. Minor pyrrhotite in a fracture. Upper contact sharp at 35 to core axis, lower contact on chloritic slip at 60 to core axis Feldspathic Pale gray - white. Upper contact at 80 to core axis, lower contact irregular. sandstone Pebbly wacke, very Pink granite boulder in wacke matrix. minor Sudbury breccia Quartz vein 5 mm thick at 40 to core axis Quartz vein 10 mm thick at 45 to core axis carries minor pyrrhotite, Fracture zone. Chloritic fractures at 15 to core axis, parallel quartz - pyrite vein 5-10 mm thick Fracture zone. Core moderately broken on chloritic fractures most commonly at 50, 60, 80 to core axis Fracture zone. Core badly to weakly broken on chloritic fractures most commonly at 15, 30, 45 to core axis Quartz vein 15 mm thick at 85 to core axis.

85 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 6 From- To Rock Type Description Sudbury breccia seam, pale green,s mm thick at 65 to core axis Foliation (weak schistosity and parallel elongated pebble) at 30 to core axis Bedding at 30 to core axis , Quartz veins 5, 10 mm thick at 80,90 to core axis respectively Fracture zone. Core moderately broken on chloritic fractures most commonly at 30, 40, 50, 70 to core axis Fracture zone. Core badly to moderately broken on chloritic fractures most commonly at 0, 20, 60 to core axis Quartz vein 10 mm thick at 30 to core axis carries minor pyrrhotite and pyrite , Quartz veins 5 mm thick at 20 to core axis carry minor pyrrhotite Feldspathic sandstone. Upper contact at 55 to core axis, lower contact gradational Trace chalcopyrite in crackle breccia Quartz vein breccia 20 mm thick at 70 to core axis, carries trace pyrite. i Quartz vein 2-5 mm thick at 80 to core axis in thin breccia zone mm thick.

86 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East From- To Rock Type Hole No. MAE Page 7 Description Fracture zone. Core moderately broken on fractures most commonly at 15 to core axis Gray granite boulder. Contacts are chloritic slips at 60 to core axis Quartz vein 15 mm thick at 20 to core axis Foliation in wacke at 50 to core axis Schistosity at 50 to core axis Quartz vein 5 mm thick at 30 to core axis carries trace pyrrhotite Quartz vein 2 mm thick at 40 to core axis carries trace chalcopyrite Fracture zone. Core weakly broken on chloritic fractures most commonly at 0, 10, 20 to core axis Fracture zone. Chloritic fractures at 30, 90 to core axis Foliation at 30 to core axis Foliation at 50 to core axis Gray granite boulder. Upper contact on fracture zone, chloritic slips at 40 to core axis, thin seam of green Sudbury breccia 60 mm thick with 5 mm - thick quartz vein. Lower contact on dark crackle breccia matrix Fracture zone. Core considerably broken on chloritic fractures most commonly at 10, 40,50 to core axis.

87 MLLSTREAM MNES LMTED DAMOND DRLL RECORD Property: Airport East Hole No. MAE Page 8 From- To Rock Type Description Schistosity at 40 to core axis Breccia zone 10 mm thick at 30 to core axis. Brecciated quartz vein in dark aphanitic matrix carries trace pyrrhotite and epidote Schistosity at 60 to core axis. Pebbly wacke is weakly schistose, exhibits crackle breccia to end of hole. Carries trace - <1 % disseminated pyrite and pyrrhotite, sparse quartz veins 1-2 mm thick Fracture zone. Core moderately broken on chloritic fractures most commonly at 0, 70 to core axis Schistosity at 50 to core axis. End Notes! 1. No samples taken. ~

88 Property: Airport East Claim No. S MLLSTREAM MNES LTD. DRLL HOLE SURVEY DATA Township: Falconbridge Hole No. MAE Collar Co-ordinates: L N, E UTM: 17T E, N NAD 83 Hole Length: m Approx. 260 m S, 20 m W of #1 post, S Survey Data Survey Type: EZ - Shot Depth Azimuth O Azimuth Dip 0 As Recorded (Astronomic) (Magnetic) Not recorded Magnetic Field

89 Box No MLLSTREAM MNES LMTED Box No's and ntervals Airport East Property Hole No. MAE nterval Box No. nterval /2

90 MAE Box No nterval Box No. nterval End

91 N ARPORT,... -(~ FALCONBRDGE MLLSTREAM MNES LTD. ARPORT EAST PROPERTY o SCALE 2OO0m KEY MAP LOCATON OF DRLLNG, 2007, CLAMS S & S FALCONBRDGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 :

92 \ 12149n " S50768 '~\. -, ': \ \ '-).J7 f 'e. f <L~" l <r lot 4. CON 3 '... MLLSTREAM MNES LTD, ARPORT EAST PROPERTY KEY MAP LOCATON OF CLAMS S & S FALCONBRDGE TOWNSHP, SUDBURY MNNG DSTRCT SCALE 1 :20, 000