RECt:.\V t:u SFP c '-AI 11 ') ii uf/.rv -/u.j/l : "').(j /SC/- 7 ~/~ 1 tj,i? PROPERTY JOHN & MARIE BRADY

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1 RECt:.\V t:u SFP PROPERTY JOHN & MARE BRADY c '-A 11 ') ii uf.rv -u.jl : "').(j SC- 7 ~~ 1 tj,? PROPERTYLOCATONACCESS: 't e t, 'r From Capreol, On., follow highway 545 to the ronside Lake rd., a distance of 53 km north of Sudbury. From here it :is 7 km west to the end of ronside Rd.. At this point a trail leads south west to the worksite [old shaft] This property consists of2 mining claims and is located in SE Kitchener and SW Hutton townships, Sudbury Mining District. HSTORY: The original interest in the subject area focused on an 8 ft. wide sulphide zone within an altered gossanous rhyolite.. A shallow pit [+- 8ft.], locally referred to as the Copenhagen Shaft was developed at this location in the early 1900's. Zinc and Copper were the obvious targets. Mr. Harold Barry of Sudbury had verbally reported to the author that a significant GOLD intersection was obtained in one 120 ft. drill hole 'under the shaft' circa The steam drill being used broke down and no further work was done. Partial verification of this sitatement is indicated by our 'discovery' of remnants of the old drill. The shaft area was partially 'stripped' in 1996 and exposed a considerable sulfide zone 8 to 10 metres wide for metres. Additional stripping and channel sampling was undertaken in PREVOUS WORK: An Ontario Dept. of Mines report dated Kindle - page 38; - describes the above and in addition refers to old trenches in lot 12 Con. 2; Hutton Tp.- where a mineralized shear yeilded.25% NCKEL. * The MNDM Assessment files high light a report by the geologist D.A. Duff on behalf of Scotia Mines Ltd. n outlines several significant MAG and EM anomalies that were strongly recommended for drillill1g- but no drilling was performed. Also, this same report on page 4, states " Recent samples from a mineralized showing near Copenhagen Lake returned low, but interesting values in Copper*, Lead, Nickel*, Palladium*, Platinum* and Zinc." GEOPHYSCAL: Brady conducted a reconnaissance VLF survey and identified a +300 metre long E-W conductor in Rhyolite that strikes across the old 'shaft' area and is open in both directions. GEOLOGY: A small east west trending band of mafic volcanic rock [4 KM x 1.5 KM] underlies claim in Kitchener Twp. The country rock is entirely mapped as Granite. At the shaft area a narrow band of Rhyolitic rock trends westward. Prospecting has determined that the Rhyolite extends for at least 2 KM. Power stripping [2006] has exposed persistent sulfide zones, 6-10 metres wide adjacent to the conductor. Highly anomalous ZNC - +9%; CU +1 %; PB - +1 % and AG - +9 Gff along with elevated cobaltnickel are obtained within the very oxidized + 0 metre wide mineralized zones within the altered and highly oxidized Rhyolite. PURPOSE OF CURRENT WORK: To specifically determine host rock type and mineralization types [especially Sphaleritewhich is difficult to identify] of the quartz vein zones at the old 'shaft'. WORK PERFORMED: On May 24,252008, John Brady and R. Charron re-established the old excavator route [2 km] by slashing out brush and windfalls to allow ATV access. On May 26 we accessed the 'shaft' area and using chisel and sledge hammer obtained a composite sample of bs offresh rock from the north side of the ' shaft'. The area of the sample was +- 2m x 1m. The samples were assessed by O.T. Maki P.GEO. and his assessment is appended

2 COPENHAGEN PROPERTY JOHN & MARE BRADY C,.A"1 ij.c>332.lk.lon[tdj ~. (LA;11 t2t5'~41 ;<Y-Cl~(?ArW#, PROPERTYLOCATONACCESS:,- From Capreol, On., follow highway 545 to the ronside Lake rd., a distance of 53 km north of Sudbury. From here it is 7 km west to the end ofronside Rd.. At this point a trail leads south west to the worksite [old shaft] This property consists of 2 mining claims and is located in SE Kitchener and SW Hutton townships, Sudbury Mining District. HSTORY: The original interest in the subject area focused on an 8 ft. wide sulphide zone within an altered gossanous rhyolite.. A shallow pit [+- 8ft.], locally referred to as the Copenhagen Shaft was developed at this location in the early 1900's. Zinc and Copper were the obvious targets. Mr. Harold Barry of Sudbury had verbally reported to the author that a significant GOLD intersection was obtained in one 120 ft. drill hole 'under the shaft' circa The steam drill being used broke down and no further work was done. Partial verification of this statement is indicated by our 'discovery' of remnants of the old drill. The shaft area was partially 'stripped' in 1996 and exposed a considerable sulfide zone 8 to 10 metres wide for metres. Additional stripping and channel sampling was undertaken in PREVOUS WORK: An Ontario Dept. of Mines report dated Kindle: - page 38; - describes the above and in addition refers to old trenches in lot 12 Con. 2; Hutton Tp.- where a mineralized shear yeilded.25% NCKEL. * The MNDM Assessment files highlight a report by tht: geologist D.A. Duff on behalf of Scotia Mines Ltd. n outlines several significant MAG and EM anomalies that were strongly recommended for drilling- but no drilling was performed. Also, this same report on page 4, states ', Recent samples from a mineralized showing near Copenhagen Lake returned low, but interesting values in Copper*, Lead, Nickel*, Palladium*, Platinum* and Zinc." GEOPHYSCAL: Brady conducted a reconnaissance VLF survey and identified a +300 metre long E-W conductor in Rhyolite that strikes across the old 'shaft' area and is open in both directions. GEOLOGY: A small east west trending band of mafic volcanic rock [4 KM x 1.5 KM] underlies claim in Kitchener Twp. The country rock is entirely mapped as Granite. At the shaft area a narrow band of Rhyolitic rock trends westward. Prospecting has determined that the Rhyolite extends for at least 2 KM. Power stripping [2006] has exposed persistent sulfide zones, 6-10 metres wide adjacent to the conductor. Highly anomalous ZNC - +9%; CU - +1 %; PB - +1 % and AG - +9 GT along with elevated cobaltnickel are obtained within the very oxidized + 0 metre wide mineralized zones within the altered and highly oxidized Rhyolite. PURPOSE OF CURRENT WORK: To specifically determine host rock type and mineralization types [especially Sphaleritewhich is difficult to identify] of the quartz vein zones at the old 'shaft'. WORK PERFORMED: On May 24,252008, John Brady and R. Charron re-established the old excavator route [2 km] by slashing out brush and windfalls to allow A TV access. On May 26 we accessed the 'shaft' area and using chisel and sledge hammer obtained a composite sample of lbs of fresh rock from the north side of the' shaft'. The area of the sample was +- 2m x 1m. The samples were assessed by O.T. Maki P.GEO. and his assessment is appended.

3 CONSULTNG MNNG GE9LOGST Au Ag Pt Pd eu Ni Zn Co U Oliver T. Maki. P.Geo. 718 Joe Persechini Drive, Newmarket, Ontario. L3X 2S1 Tel: Fax: oliver.maki@sympatico.ca Re: Channel sampling, and Samples. John Brady. Copenhagen Property. July) To Whom it May Concern. This letter is written to attest to the fact that on or about July 2008, Mr. John Brady, did bring to me approximately 25 pounds of surface rock samples from his "Copenhagen Property, in Hutton and Kitchener townships. The pwpose of viewing the samples was to make a preliminary visual assessment of their mineral content. The sampling was carried out by persons known to the writer. The mineralization noted was contained within a greenish rhyolitic rock, weathered light brown from contained carbonates. A 5 to 6 em wide quartz vein together with quartz and feldspar fragments was apparent in one of the samples. The approximate percentage composition of the sulphide content was 0.5% chalcopyrite, 10% pyrite, 2.0% pyrrhotite~ and 5.0% sphalerite. Occasional specks of galena, together with magnetite were also noted. These figures do not construe the percentage metallic content of the contained sulphides. Yours truly, O~75}~ Oliver T. Maki... HlH3 39'dd X3WtlN S8913L1 E~:

4 : NAMEX PAGE CONSUL TNG MNNG GEOLOGST Au Ag Pt Pd eu Ni Zn Co U Oliver T. Maki. P.Geo. 718 Joe Persechini Drive, Newmarket, Ontario. L3X 2S1 Tel: Fax: olive r.m a ki@sympatico.ca Re: Channel sampling, and Samples. John Brady. Copenhagen Property. July,2008. To Whom it May Concern. This letter is written to attest to the fact that on or about July 2008, Mr. John Brady, did bring to me approximately 25 pounds of surface rock samples from his "Copenhagen Property, in Hutton and Kitchener townships. The purpose of viewing the samples was to make a preliminary visual assessment of their mineral content. The sampling was carried out by persons known to the writer. The mineralization noted was contained within a greenish rhyolitic rock, weathered light brown from contained carbonates. A 5 to 6 em wide quartz vein together with quartz and feldspar fragments was apparent in one of the samples. The approximate percentage composition of the sulphide content was 0.5% chalcopyrite, 10% pyrite, 2.0% pyrrhotite, and 5.0% spha1erite. Occasional specks of galena, together with magnetite were also noted. These figures do not construe the percentage metallic content of the contained sulphides. 01:7S Oliver T. Maki. '

5 UTM Zone 17 5DOOm grid

6 f Jllde-.,:. HfrfJ- &M4~ 07J g em-'r( 111-6'11 ULSTER MUNSTER LENSTER TYRONE KTCHENER button PARKN.. - [ P CD tj. ~ MONCREFF HESS HARTY FOY BOWELL WSNER NORMAN ~- ;; CapnJol [ HART CARTER LEVACK MORGAN LUMSDEN HANMER CAPREOL <D ERMATNGER Levack Chelmsford CASCADEN DOWLNG.. RAYSDE BLEZARD 8ALFOUR GARSON. -ndicates area of work. 1 SNDER Sudbury FARBANK CREGHTON NEELON J. BRADY PROPERTY Copper Cliff McKM Conison PROPERTY LOCATON DSTRCT OF SUDBURY DENSON GRAHAM Lively WATERS BRODER DiLL.

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