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2-51752

REPORT

On the

Geological Prospecting and Sampling

Of the

"West Hemlo" Property

For

Strike Minerals Inc.

Chris North

October 6,2011

r1~Y 042012

GEOSCIH!CE ASSESSMENT OFFICE

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2-51752

REPORT

On the

Geological Prospecting and Sampling

Of the

"West Hemlo" Property

For

Strike Minerals Inc.

Chris North

October 6,2011

fi Y 042012 GEOSCIE~ ICE ASSESSMENT

OFFICE

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SUMMARY

The Strike Minerals "West Hemlo" property is located in Priske Township approximately 10 kilometres wi thin the radius of Schreiber, Ontario. The property consists of 30 claims comprising 214 units with 7 additional patented claims. It lies within the Schreiber-Hemio Greenstone belt of the Thunder Bay Mining Division (Plan G-0631), as outlined by the Ontario Geological Survey Open File Report 5951. The area hosts the world class known Hemlo gold deposits in the area currently being operated by Barrick Gold Corporation.

p.7

On three separate occasions the author with assistance visited the West Hemlo claim group for reconnaissance prospecting and sampling. On November 3,2009, September 24 and 25 of 20 10 and Sept. 16 and 17, 201 l the author travelled to and from the property from south em Ontario and, with assistance, performed reconnaissance geological prospecting on the interior of the property and geological sampling on some of the historical showings on the property.

Outcrop covers at least 30% in the investigated areas to the north-western and south­eastern portions of the property. During the three field visits over the past 22 months a total of23 rock samp]es were collected. The laboratory results for the 23 samples from the three visits are located in the appendix of the report.

2

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SUMMARY

The Strike Minerals "West Hemlo" property is located in Priske Township approximately 10 kilometres wi thin the radius of Schreiber, Ontario. The property consists of 30 claims comprising 214 units with 7 additional patented claims. It lies within the Schreiber-Hemio Greenstone belt of the Thunder Bay Mining Division (Plan G-0631), as outlined by the Ontario Geological Survey Open File Report 5951. The area hosts the world class known Hemlo gold deposits in the area currently being operated by Barrick Gold Corporation.

p.7

On three separate occasions the author with assistance visited the West Hemlo claim group for reconnaissance prospecting and sampling. On November 3,2009, September 24 and 25 of 20 10 and Sept. 16 and 17, 201 l the author travelled to and from the property from south em Ontario and, with assistance, performed reconnaissance geological prospecting on the interior of the property and geological sampling on some of the historical showings on the property.

Outcrop covers at least 30% in the investigated areas to the north-western and south­eastern portions of the property. During the three field visits over the past 22 months a total of23 rock samp]es were collected. The laboratory results for the 23 samples from the three visits are located in the appendix of the report.

2

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TABLE of CONTENTS

SUInnlary .................... . ............. ... ..................................................... 2

Introduction ............. .... . ............................ . . . .. . .... . ...... . ............ . . .. ....... 3

Location and Access .... ... ............. . ...... . ........ .. ............ . .................. .. ...... 4

Geological Setting .. ... .... .. . .............................. . . . ..... ....... ......... .. ... . ........ 5

Regional Geology ............. ~ .. . ....................... . ... " . ............... .. ...... 5

Property Geology ............................... .. ............................... . ...... 5

Results of Geological Prospecting and Sanlpling ....... .. .... .. ........ .. ... .. .... . .. . ...... 6

Geology ......... .. ............... . ............................. .. ............... ... ..... 6

Mineralization ... . .................. . ........................................... .. ...... 6

Sanlpling Results ............................................................ .. ........ 8

Work Performed ......... . . . ............. ... ......................................... .. " . . ...... . 7

Discussion ..... . ........... .. .............. . ............... . .............................. . ........ 7

Conclusions and Recommendations ........ . ........................ .. ......... .. .... .. ....... 9

References .............. . ................................................................ .......... 10

Certificate and Qualifications ........ .. ... . ........... ... ... . ................ . .... .. .. .. ....... 11

List of Figures

Strike Minerals "West HernIa" property location map ........... . ........................... 12

Strike Minerals "West HernIa" claim location map .. ... . .... . ... . . . .......... ... '" .......... 13

P.lan of Rock Sampling, .................. . ............. ... .. .................................... .. ............... 14

List of Appendices

Appendix 1 Appendix II Appendix III Appendix IV

Figure 1, 2, 3, 4, 5 Assay Certificates Claim Abstract MNDM \\lork Assessment Work Report

p.8

3

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TABLE of CONTENTS

SUInnlary .................... . ............. ... ..................................................... 2

Introduction ............. .... . ............................ . . . .. . .... . ...... . ............ . . .. ....... 3

Location and Access .... ... ............. . ...... . ........ .. ............ . .................. .. ...... 4

Geological Setting .. ... .... .. . .............................. . . . ..... ....... ......... .. ... . ........ 5

Regional Geology ............. ~ .. . ....................... . ... " . ............... .. ...... 5

Property Geology ............................... .. ............................... . ...... 5

Results of Geological Prospecting and Sanlpling ....... .. .... .. ........ .. ... .. .... . .. . ...... 6

Geology ......... .. ............... . ............................. .. ............... ... ..... 6

Mineralization ... . .................. . ........................................... .. ...... 6

Sanlpling Results ............................................................ .. ........ 8

Work Performed ......... . . . ............. ... ......................................... .. " . . ...... . 7

Discussion ..... . ........... .. .............. . ............... . .............................. . ........ 7

Conclusions and Recommendations ........ . ........................ .. ......... .. .... .. ....... 9

References .............. . ................................................................ .......... 10

Certificate and Qualifications ........ .. ... . ........... ... ... . ................ . .... .. .. .. ....... 11

List of Figures

Strike Minerals "West HernIa" property location map ........... . ........................... 12

Strike Minerals "West HernIa" claim location map .. ... . .... . ... . . . .......... ... '" .......... 13

P.lan of Rock Sampling, .................. . ............. ... .. .................................... .. ............... 14

List of Appendices

Appendix 1 Appendix II Appendix III Appendix IV

Figure 1, 2, 3, 4, 5 Assay Certificates Claim Abstract MNDM \\lork Assessment Work Report

p.8

3

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INTRODUCTION

In July, 2011 , the author was retained by Mr. Mike Newbury, P. Eng., (President, Strike Minerals rnc.) to perfonn a short program of reconnaissance prospecting and sampling on the company's "West Hemlo" property in Priske Township, Ontario.

The \Vest Hemlo property consists of30 claims with 214 units and 7 claims patented for surface and mining rights (claim list is in the Appendix of the report). The property lies within a 10 kilometres radius of Town of Schreiber, Ontario.

During the period November 3,2009, September 24 and 25,2010 and on September 16, 17 and 182011, the author with assistance perfonned a program of recOlmaissance prospecting and sampling on some of the known shov...ings in the south­eastern and north-western sections of the property. In the South-eastern section of the claims, on the Morley polymetallic shoY-ring two chip samples across a narrow massive sulphide vein located within a rhyollite returned values of 5.5 g/t Au and 1040 glt Ag in the first sample and 3.65 g.'tonne Au and 1320 glt Ag in the second sample. Sampling of the north-western section of the prope11y revealed vg in one of the samples with values ranging fTom trace to 13.0 g/t.

p.9

The initial program consisted of reconnaissance prospecting over some of the anomalous areas of the property and selective samplings of these showings. Initial work would provide necessary assessment work requirements, as well as providing impetus for further work on the property which may include trenching, geophysics and future diamond drilling.

LOCATION and ACCESS

The "West Hernlo" property is located in Priske Tovvnship (Plan G-0631) within the Schreiber - Hernlo greenstone belt of the Thunder Bay Mining Division. The property is located within 10 kilometers of Schreiber, Ontatio and is easily accessed, firstly by gravel roads and then by bush roads followed by ATV trai]s. The route to the south­western portion of the property is via the "VI.' orthington Bay Road south of HWY 17 two kilometres west of Schreiber. Access to the north-westemportion is through the north part of the town of Schreiber then by bush which starts at the Schreiber water reservoir and proceeds along the west side of Cook Lake. Several access trails utilized by Ontario Hydro for maintenance provides access to the claim group. The area has been lumbered in the past with thick secondary growth present in most locals.

4

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INTRODUCTION

In July, 2011 , the author was retained by Mr. Mike Newbury, P. Eng., (President, Strike Minerals rnc.) to perfonn a short program of reconnaissance prospecting and sampling on the company's "West Hemlo" property in Priske Township, Ontario.

The \Vest Hemlo property consists of30 claims with 214 units and 7 claims patented for surface and mining rights (claim list is in the Appendix of the report). The property lies within a 10 kilometres radius of Town of Schreiber, Ontario.

During the period November 3,2009, September 24 and 25,2010 and on September 16, 17 and 182011, the author with assistance perfonned a program of recOlmaissance prospecting and sampling on some of the known shov...ings in the south­eastern and north-western sections of the property. In the South-eastern section of the claims, on the Morley polymetallic shoY-ring two chip samples across a narrow massive sulphide vein located within a rhyollite returned values of 5.5 g/t Au and 1040 glt Ag in the first sample and 3.65 g.'tonne Au and 1320 glt Ag in the second sample. Sampling of the north-western section of the prope11y revealed vg in one of the samples with values ranging fTom trace to 13.0 g/t.

p.9

The initial program consisted of reconnaissance prospecting over some of the anomalous areas of the property and selective samplings of these showings. Initial work would provide necessary assessment work requirements, as well as providing impetus for further work on the property which may include trenching, geophysics and future diamond drilling.

LOCATION and ACCESS

The "West Hernlo" property is located in Priske Tovvnship (Plan G-0631) within the Schreiber - Hernlo greenstone belt of the Thunder Bay Mining Division. The property is located within 10 kilometers of Schreiber, Ontatio and is easily accessed, firstly by gravel roads and then by bush roads followed by ATV trai]s. The route to the south­western portion of the property is via the "VI.' orthington Bay Road south of HWY 17 two kilometres west of Schreiber. Access to the north-westemportion is through the north part of the town of Schreiber then by bush which starts at the Schreiber water reservoir and proceeds along the west side of Cook Lake. Several access trails utilized by Ontario Hydro for maintenance provides access to the claim group. The area has been lumbered in the past with thick secondary growth present in most locals.

4

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GEOLOGICAL SETTING

Regional Geology

The Strike Minerals Inc. "\Vest Hemlo" property is regionally located in the eastern portion of the Wawa Subprovince within the Superior Province of the Canadian Shield. It is f]anked to the north by the Quetico Subprovince of metasedimentry rocks. The property is locally situated at the western limits of the Schreiber - Hernlo Greenstone belt, as outlined by the Ontario Geological Survey Open File Report 5951 & 5952 (OFR 5951 & 5952).

The properties lie in a belt of early Precambrian basic to intermediate volcanic and metavolcanic rocks lying proximal to the Terrace Bay acid batholith. Minor bands of acid volcanics and metasediments occur within the belt which has been intruded by acid to basic dykes and sills of varying composition and orientation. Thin bands of iron formation are common, and diabase dikes are reportedly the most recent intrusi ves. The majority of structures as evidence by geologic and magnetic data have indicated a northwest and northeast orientation. These aforementioned lineaments are host auriferous quartz veining.

The area is underlain by Archean aged, iron-rich, tholeiitic meta-basalts which trend roughly east-west and dip steeply north. These basalts are bisected by a proliferation of fe1sic intrusives generally along strike, and by mafic intrusives (diabase dikes) in a north-westerly direction. Structural controls appear to be the most important factor in the localization of gold-bearing quartz veins in the area.

Property Geology

Schreiber South Group

The rocks near the Morley polymetallic high grade sho'Wing have been described by Gow (1985) as containing chemical and clastic metasedimentry rocks which locally include bands of and lenses of sulphides which separate basic meta volcanics in the northwest from metavolcanics in the south. The aforementioned metavolcanics have undergone several periods of intrusions which include a granitic, dioritic and quartz feldspar porphyry. Proterozoic diabase dikes bisect the metavolcanics. The Morley high grade vein has been described by (Smick 1996) as a discordant vein structure.

Mineralization

The Morley polymetallic vein has been described by (Patterson 1984) as being either a lead-zinc-silver contact type due to it proximal relationship 'with the Terrace Bay batholith or metavolcanic type due to the presence of gold mineralization in relation to

5

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GEOLOGICAL SETTING

Regional Geology

The Strike Minerals Inc. "\Vest Hemlo" property is regionally located in the eastern portion of the Wawa Subprovince within the Superior Province of the Canadian Shield. It is f]anked to the north by the Quetico Subprovince of metasedimentry rocks. The property is locally situated at the western limits of the Schreiber - Hernlo Greenstone belt, as outlined by the Ontario Geological Survey Open File Report 5951 & 5952 (OFR 5951 & 5952).

The properties lie in a belt of early Precambrian basic to intermediate volcanic and metavolcanic rocks lying proximal to the Terrace Bay acid batholith. Minor bands of acid volcanics and metasediments occur within the belt which has been intruded by acid to basic dykes and sills of varying composition and orientation. Thin bands of iron formation are common, and diabase dikes are reportedly the most recent intrusi ves. The majority of structures as evidence by geologic and magnetic data have indicated a northwest and northeast orientation. These aforementioned lineaments are host auriferous quartz veining.

The area is underlain by Archean aged, iron-rich, tholeiitic meta-basalts which trend roughly east-west and dip steeply north. These basalts are bisected by a proliferation of fe1sic intrusives generally along strike, and by mafic intrusives (diabase dikes) in a north-westerly direction. Structural controls appear to be the most important factor in the localization of gold-bearing quartz veins in the area.

Property Geology

Schreiber South Group

The rocks near the Morley polymetallic high grade sho'Wing have been described by Gow (1985) as containing chemical and clastic metasedimentry rocks which locally include bands of and lenses of sulphides which separate basic meta volcanics in the northwest from metavolcanics in the south. The aforementioned metavolcanics have undergone several periods of intrusions which include a granitic, dioritic and quartz feldspar porphyry. Proterozoic diabase dikes bisect the metavolcanics. The Morley high grade vein has been described by (Smick 1996) as a discordant vein structure.

Mineralization

The Morley polymetallic vein has been described by (Patterson 1984) as being either a lead-zinc-silver contact type due to it proximal relationship 'with the Terrace Bay batholith or metavolcanic type due to the presence of gold mineralization in relation to

5

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the felsic volcanics. The later seems to be warranted based on the field evidence. The vein itself varies in width from 10 cm to 35 em and is exposed for at least 250 meters. The vein strikes 185 to 200 degrees and dips from subvertieal to 60 degrees west The vein is composed of galena with banded sphalerite with associated chalcopyrite and pyrite. The vein is hosted in fractured metavolcanic which has been described as a by (Gow 1985) carbonatized rhyolite agglomerate with fragmental texture. Two samples were taken directly across the vein approximately 50 m apart. Additional samples were taken on adjacent vein stringers. The results of the sampling are presented are discussed in the fo1Jowing section.

Schreiber West Group

The rocks of this group are predominantly underlain by subaqueous intermediate volcanics and pillowed flows Vvith inter-cycle iron formation. The aforementioned are bisected by gabbroic, dioritic and quartz feldspar stocks and dikes. (Carter 1988 OFR 5952) Subdivided the metavolcanics into two volcanic cycles which were separated a sulfide iron formation. During the course of prospecting and sampling the author observed the iron formation to be sulphides facies with the presence of chert, illmenite and magnetite.

Previous examination of the air photo and magnetic data by (Smick 1996 OFR 5691) indicated several major northwest trending lineaments which include Big Duck Creek and Hays Lake. A secondary northeastem trending lineament is present on the property and the resulting conjugate fault sets appear to be related to the areas of gold mineralization.

During the period of2009 -2011, the author completed reconnaissance prospecting of the property and observed that the geology conformed to the Ontario Geological Service (OGS) Open File Reports (OFR) Reports 5951 and 5952 Mineral Occurrences in the Nipigon-Marathon 1996.

Mineralization

p.11

The rocks of the north-eastern portion of the claim group are primarily volcanic to metavolcanic. The gold mineralization is generally associated with quartz and stringer veins that vary in width from 5 em to over 50 cm. The veins as evidenced during the field visits contain pyrite, chalcopyrite, tOUlmaline and in one sample native gold. The veins in the area generally strike northwest with a dips ranging 40 to 60 degrees to the west. Present during the field examination were some smalJ vein offsets that were oriented to the northeast. Noranda in 1984 had previously conducted exploration in the immediate vicinity and uncovered sulphide fades iron formation which assayed 0.07 ozlt. This has been suggested by (Twomey 1992) to be along the Grant Fault. In the area of the Schreiber-

6

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the felsic volcanics. The later seems to be warranted based on the field evidence. The vein itself varies in width from 10 cm to 35 em and is exposed for at least 250 meters. The vein strikes 185 to 200 degrees and dips from subvertieal to 60 degrees west The vein is composed of galena with banded sphalerite with associated chalcopyrite and pyrite. The vein is hosted in fractured metavolcanic which has been described as a by (Gow 1985) carbonatized rhyolite agglomerate with fragmental texture. Two samples were taken directly across the vein approximately 50 m apart. Additional samples were taken on adjacent vein stringers. The results of the sampling are presented are discussed in the fo1Jowing section.

Schreiber West Group

The rocks of this group are predominantly underlain by subaqueous intermediate volcanics and pillowed flows Vvith inter-cycle iron formation. The aforementioned are bisected by gabbroic, dioritic and quartz feldspar stocks and dikes. (Carter 1988 OFR 5952) Subdivided the metavolcanics into two volcanic cycles which were separated a sulfide iron formation. During the course of prospecting and sampling the author observed the iron formation to be sulphides facies with the presence of chert, illmenite and magnetite.

Previous examination of the air photo and magnetic data by (Smick 1996 OFR 5691) indicated several major northwest trending lineaments which include Big Duck Creek and Hays Lake. A secondary northeastem trending lineament is present on the property and the resulting conjugate fault sets appear to be related to the areas of gold mineralization.

During the period of2009 -2011, the author completed reconnaissance prospecting of the property and observed that the geology conformed to the Ontario Geological Service (OGS) Open File Reports (OFR) Reports 5951 and 5952 Mineral Occurrences in the Nipigon-Marathon 1996.

Mineralization

p.11

The rocks of the north-eastern portion of the claim group are primarily volcanic to metavolcanic. The gold mineralization is generally associated with quartz and stringer veins that vary in width from 5 em to over 50 cm. The veins as evidenced during the field visits contain pyrite, chalcopyrite, tOUlmaline and in one sample native gold. The veins in the area generally strike northwest with a dips ranging 40 to 60 degrees to the west. Present during the field examination were some smalJ vein offsets that were oriented to the northeast. Noranda in 1984 had previously conducted exploration in the immediate vicinity and uncovered sulphide fades iron formation which assayed 0.07 ozlt. This has been suggested by (Twomey 1992) to be along the Grant Fault. In the area of the Schreiber-

6

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Pyramid property there are numerous quartz feldspar porphyry (QFP) dikes which were located during field visit. The presence of the QFP's has been outlined by Twomey (1992) as potential gold targets. The results of the sampling are presented are discussed in the following section.

WORK PERFORMED

On three separate occasions from November 3,2009, September 24 and 25 of 2010 and on September 16,17 and 18 2011, the author with assistance travelled to and from the property from southern Ontario and completed reconnaissance prospecting over the interior of the propel1y on some of the historical showings. Sampling was perfOlmed on areas surrounding the historical showings. Mapping was perfOlmed using a Garmin GPSmap 60CSx on NAD 83 UTM Zone 16.

Assaying was completed at Act Laboratories, of Ancaster, and Accurassay of Thunder Bay Ontario, both accredited laboratories. All infonnation peliaining to the laboratory may be found in the appendix accompanying this repmi.

DISCUSSION

A total of 23 rock samples were taken during the three property visjts and are plotted on the sample Key Map Figure 2. 16 of the 23 rock laboratory sampLes resuLts are included in Appendix II. The South Claim Group of the property specifically the Morley high-grade zone yielded a brecciated massive sulphide vein with extremely positive results. The vein was observed in the field have a strike length in excess of ISO m with a subvertical to 60 degree westerly dip. The host rock for the massive SUlphide vein is an altered rhyolite volcanic. Two samples taken across the vein at approximately 50 m separation yielded values of 5.5 glt Au and 1040 glt Ag in the first sample and 3.65 gltonne Au and 1320 glt Ag in the second sample gold with 2.62% Zn and 1 % Pb. The results of this sampling are plotted jn Figure 3. Samples in the Central Claim group primarily from a reduction iron formation yielded low results from trace to .31 gIl Au. The results of this sampling are plotted in figure 5. In North Claim Group samples taken from altered basalts with qtz veining with sulphides ranged from trace to 13 giL The results of this sampling areptotted in Figure 4.

In the north-eastern portion ofthe property numerous hydrothennal quartz veins were 10cated. The veins and offset veins were fracture filling and trended in primarily in a north-western direction ~1th offsets in s north-easterly trend. The veins were generally associated v·lith carbonate alteration and tounnaline. Samples taken were mineralized with pyrite, chalcop),Tite and in some samples pyrrhotite. Visible gold was noted in one sample. The iron formations present in both the sections of the West HernIa property

7

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Pyramid property there are numerous quartz feldspar porphyry (QFP) dikes which were located during field visit. The presence of the QFP's has been outlined by Twomey (1992) as potential gold targets. The results of the sampling are presented are discussed in the following section.

WORK PERFORMED

On three separate occasions from November 3,2009, September 24 and 25 of 2010 and on September 16,17 and 18 2011, the author with assistance travelled to and from the property from southern Ontario and completed reconnaissance prospecting over the interior of the propel1y on some of the historical showings. Sampling was perfOlmed on areas surrounding the historical showings. Mapping was perfOlmed using a Garmin GPSmap 60CSx on NAD 83 UTM Zone 16.

Assaying was completed at Act Laboratories, of Ancaster, and Accurassay of Thunder Bay Ontario, both accredited laboratories. All infonnation peliaining to the laboratory may be found in the appendix accompanying this repmi.

DISCUSSION

A total of 23 rock samples were taken during the three property visjts and are plotted on the sample Key Map Figure 2. 16 of the 23 rock laboratory sampLes resuLts are included in Appendix II. The South Claim Group of the property specifically the Morley high-grade zone yielded a brecciated massive sulphide vein with extremely positive results. The vein was observed in the field have a strike length in excess of ISO m with a subvertical to 60 degree westerly dip. The host rock for the massive SUlphide vein is an altered rhyolite volcanic. Two samples taken across the vein at approximately 50 m separation yielded values of 5.5 glt Au and 1040 glt Ag in the first sample and 3.65 gltonne Au and 1320 glt Ag in the second sample gold with 2.62% Zn and 1 % Pb. The results of this sampling are plotted jn Figure 3. Samples in the Central Claim group primarily from a reduction iron formation yielded low results from trace to .31 gIl Au. The results of this sampling are plotted in figure 5. In North Claim Group samples taken from altered basalts with qtz veining with sulphides ranged from trace to 13 giL The results of this sampling areptotted in Figure 4.

In the north-eastern portion ofthe property numerous hydrothennal quartz veins were 10cated. The veins and offset veins were fracture filling and trended in primarily in a north-western direction ~1th offsets in s north-easterly trend. The veins were generally associated v·lith carbonate alteration and tounnaline. Samples taken were mineralized with pyrite, chalcop),Tite and in some samples pyrrhotite. Visible gold was noted in one sample. The iron formations present in both the sections of the West HernIa property

7

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were identified in the field to be sulphide facjes indicated by the presence of chert­magnetite. Samples taken from the iron fonnation generally contained >5% pyrrhotite with minor amounts of pyrite. Results from the sampling of the iron fonnations yielded positive results 'with one sample yielding 2.53 glt.

The presence of significant polymetallic grades in the south-western claim group and auriferous quartz veining at the north-eastern claim group indicate further work is required on the "West Hemlo" property.

Sampling Results

Grab Chip and Channel samples of were extracted from 23 locations within the West Hemlo Claim group. A plan map of the sample locations is included in the Appendix in Figure 3. Sample numbers, location, assay and description are shown in the following table:

Strike Mini~rals inc. 'West Hemlo· Property Rock Samples DescripHons

Sample # Location Au Assay (gpt) Description

Easting Northing

613051 16479327 5401581 <0.005 BasalUQFP contact, < 1 % py,

613052 16479318 5401506 0 .005 QFP w qtz vein, lJP to 2% py,

613053 16479324 5401455 0.007 QFP, tr py

613054 16479299 54014"16 0.007 OFP contact w'lth volcanics, tr py,

613055 15479307 5401381 <0 .005 OFP, trpy,

613056 16479361 5401506 0.010 QFP 2cm qtz vein. tr py,

613057 16479545 5401362 0.023 OFP 2-5% po, py

613058 164B3413 5405063 031 IF/Basalt contact 2·5% po tr py

613059 16483412 5405063 0.017 IFf Basalt contact, 1-3% po tr py

613060 16483411 5405063 0.015 IF/Basalt contact. 1·3% po tr py

104602 16481158 5403682 5.50 Morley East 25cm vein breccia 5%sph, py

104603 16481117 5403595 365 Morley West 20cm vein breccia 5% sph. PY

p.13

8

L-c..::' 2::...: 4,,-,5 :,,-,09'-!:p.:.::. m.::.... O:.:5--'-O:...:.4---'2:.:..0,:.::.2----L_,:.::3---11 _ _ -=4~' 6:,.::2:::6'...:..7.::.:52:::.-8 _--1~ ra Is 416-261-7528

were identified in the field to be sulphide facjes indicated by the presence of chert­magnetite. Samples taken from the iron fonnation generally contained >5% pyrrhotite with minor amounts of pyrite. Results from the sampling of the iron fonnations yielded positive results 'with one sample yielding 2.53 glt.

The presence of significant polymetallic grades in the south-western claim group and auriferous quartz veining at the north-eastern claim group indicate further work is required on the "West Hemlo" property.

Sampling Results

Grab Chip and Channel samples of were extracted from 23 locations within the West Hemlo Claim group. A plan map of the sample locations is included in the Appendix in Figure 3. Sample numbers, location, assay and description are shown in the following table:

Strike Mini~rals inc. 'West Hemlo· Property Rock Samples DescripHons

Sample # Location Au Assay (gpt) Description

Easting Northing

613051 16479327 5401581 <0.005 BasalUQFP contact, < 1 % py,

613052 16479318 5401506 0 .005 QFP w qtz vein, lJP to 2% py,

613053 16479324 5401455 0.007 QFP, tr py

613054 16479299 54014"16 0.007 OFP contact w'lth volcanics, tr py,

613055 15479307 5401381 <0 .005 OFP, trpy,

613056 16479361 5401506 0.010 QFP 2cm qtz vein. tr py,

613057 16479545 5401362 0.023 OFP 2-5% po, py

613058 164B3413 5405063 031 IF/Basalt contact 2·5% po tr py

613059 16483412 5405063 0.017 IFf Basalt contact, 1-3% po tr py

613060 16483411 5405063 0.015 IF/Basalt contact. 1·3% po tr py

104602 16481158 5403682 5.50 Morley East 25cm vein breccia 5%sph, py

104603 16481117 5403595 365 Morley West 20cm vein breccia 5% sph. PY

p.13

8

L-~' 2.:.::: 4::.:.-5 : O~9LP . .:::m :...::O::...-5--=::04=---.::.:20~' 2,-----,1----,-,, 4---11 __ --'-4 ;..::.16~26::...:., -'.:7 5:..::.28'--------..J~ ra Is 416-261-7528 p.14

104604 16481520 5403593 <0.03 Moriey IF, 2%-5% coarse po,

104605 16481414 5403608 0.63 Morley Trench IF 2-5% coarse py, cubes, po

104606 16481399 5403586 2.63 MDrley Trench IF, 2% coarse py, PY

104607 16479494 5401017 0.30 Galena breccia 2-5% galena silicified

1085974 16483550 5409683 O.OOB Sheared Basalt mlsilicified Ir py

1085975 15483924 5409508 0.029 8asalt#2 vein 12 an 1% py cupy

1085976 16483876 5409530 0.010 Sheared Basalt slic py,po, cUPY

1085977 16483712 5409438 4.00 Qtz vein 46 em 1-2% py in mv

1085978 lE4B3729 5409425 0.30 Qtz vein 40 em 1% py cubes in mv

1085979 16482088 5409378 0.701 MJ Qtz vein 30 cm tr py ca aft

1085980 16482985 5408633 13.00 MM Qtz vein 2-5% py cupy vg in mv

CONCLUSIONS AND RECOMMENDATIONS

Geological prospecting and sampling was completed at a reconnaissance scale however the sampling of the historical showings returned highly significant grades for gold silver zinc and lead on the Morley showing. Results from the sampling of the north­eastern portion were not available at the time of submission of the report however field examination of several samples indicated the presence of mineralization including one sample with visible gold. There are nwnerous gold and polymetallic ocurrences on the West Hernla property and further work is warranted on to establish the scale of the mineral ization,

The author believes that the "West Hernlo" property specifically in the south-western portion may have the potential to host a possible massive sulphide deposit. In tile north­eastern portion of the property the presence of economjcally viable auriferous quartz veining is to be determined and confirmed with laboratory results however field examination of the quartz veins was positive. The iron fannation in the south-western claim group yielded positive results and deserves some further work.

It is recommended that further work be completed on the property. Mechanical stripping using an excavator and washing of exposed rock could provide access to a structural and mineralogical definition and provide for more detailed channel sampling_ Positive results could lead to a dlill program designed to test the mineralized structures at depth.

9

L-~' 2.:.::: 4::.:.-5 : O~9LP . .:::m :...::O::...-5--=::04=---.::.:20~' 2,-----,1----,-,, 4---11 __ --'-4 ;..::.16~26::...:., -'.,;7 5:..:.28,---,~ ra Is 416-261-7528 p.14

104604 16481520 5403593 <0.03 Moriey IF, 2%-5% coarse po,

104605 16481414 5403608 0.63 Morley Trench IF 2-5% coarse py, cubes, po

104606 16481399 5403586 2.63 MDrley Trench IF, 2% coarse py, PY

104607 16479494 5401017 0.30 Galena breccia 2-5% galena silicified

1085974 16483550 5409683 O.OOB Sheared Basalt mlsilicified Ir py

1085975 15483924 5409508 0.029 8asalt#2 vein 12 an 1% py cupy

1085976 16483876 5409530 0.010 Sheared Basalt slic py,po, cUPY

1085977 16483712 5409438 4.00 Qtz vein 46 em 1-2% py in mv

1085978 lE4B3729 5409425 0.30 Qtz vein 40 em 1% py cubes in mv

1085979 16482088 5409378 0.701 MJ Qtz vein 30 cm tr py ca aft

1085980 16482985 5408633 13.00 MM Qtz vein 2-5% py cupy vg in mv

CONCLUSIONS AND RECOMMENDATIONS

Geological prospecting and sampling was completed at a reconnaissance scale however the sampling of the historical showings returned highly significant grades for gold silver zinc and lead on the Morley showing. Results from the sampling of the north­eastern portion were not available at the time of submission of the report however field examination of several samples indicated the presence of mineralization including one sample with visible gold. There are nwnerous gold and polymetallic ocurrences on the West Hernlo property and further work is warranted on to establish the scale of the mineral ization,

The author believes that the "West Hernlo" property specifically in the south-western portion may have the potential to host a possible massive sulphide deposit. In tile north­eastern portion of the property the presence of economjcally viable auriferous quartz veining is to be determined and confirmed with laboratory results however field examination of the quartz veins was positive. The iron fannation in the south-western claim group yielded positive results and deserves some further work.

It is recommended that further work be completed on the property. Mechanical stripping using an excavator and washing of exposed rock could provide access to a structural and mineralogical definition and provide for more detailed channel sampling_ Positive results could lead to a dlill program designed to test the mineralized structures at depth.

9

L-.:'~2:~4 5.:.::: 09:..!p:::.::, m::..:, O~5-..::..:04,--,-2::.:..0':..::..2 ----L-'-" 5'--11 __ 4c-' 6;....::2-,---6'_7 5_28_----'~ ra Is 416-261-7528

REFERENCES

Carter, M. W. 1988

Daniels, G. 1996

Gow 1996

Geology of the Schreiber-Terrace Bay Area, District of Tlllmder Bay: Ontario Geological Survey, Open File Report 5692

OP AP Final Report. AFR£ # 42D 15NW0009

Mineral Occurrences in the Nipigon-Marathon Area Ontario Geological Survey, Open File Report 5692

Koranda Exploration Geology and Hwnus Sampling AFRI # 42D14SE0094 Limited 1988.

Patterson 1984

Smick, M. 1996

Twomey, T. 1992

Mineral Occunences in the Nipigon-Marathon Area Ontario Geological Survey, Open File Report 5691

Mineral Occurrences in the Nipigon-Marathon Area Ontario Geological Survey, Open File Report 5691 &5692

OPAP Final Report Prospecting, Stripping and Sampling Schreiber-Pyramid Property Priske Township

p.15

10

L-.:'~2:~4 5.:.::: 09:..!p:::.::, m::..:, O~5-..::..:04,--,-2::.:..0':..::..2 ----L-'-" 5'--11 __ 4c-' 6;....::2-,---6'_7 5_28_----'~ ra Is 416-261-7528

REFERENCES

Carter, M. W. 1988

Daniels, G. 1996

Gow 1996

Geology of the Schreiber-Terrace Bay Area, District of Tlllmder Bay: Ontario Geological Survey, Open File Report 5692

OP AP Final Report. AFR£ # 42D 15NW0009

Mineral Occurrences in the Nipigon-Marathon Area Ontario Geological Survey, Open File Report 5692

Koranda Exploration Geology and Hwnus Sampling AFRI # 42D14SE0094 Limited 1988.

Patterson 1984

Smick, M. 1996

Twomey, T. 1992

Mineral Occunences in the Nipigon-Marathon Area Ontario Geological Survey, Open File Report 5691

Mineral Occurrences in the Nipigon-Marathon Area Ontario Geological Survey, Open File Report 5691 &5692

OPAP Final Report Prospecting, Stripping and Sampling Schreiber-Pyramid Property Priske Township

p.15

10

L-'.:..::.2,'-'.:45:..:.:::0-'-!9 Pc:..c' m",-, 0=5--=-0--'--4--=-:20'-'.:'2=-------.!_':.::.6 --1-1_------=4:.:.:'6::..::2.::.:6'..:..:7 5::.:::28~----1~ ra Is 416-261-7528

QUALIFICATIONS

I, Chris North, resident of 129 Midland Avenue, Scarborough, Ontario hereby certify that:

p.16

1) I am a graduate of Lake Superior State University, Sault Ste. Marie, Micrugan, U.S.A receiving an Bachelor of Science Degree in Geology in 1986

2) I am a graduate of Sault College of Applied Arts and Technology receiving a Geological Engineering Technology diploma in 1983

3) 1 have practiced my profession for 25 years, managing and supervising many Exploration and development programs.

4) During the period November 3, 2009, October 9 and 1 0 of2010 and on September 16, 17 and 18 2011, I have visited the property.

5) I have received no compensation for this report other than the normal consulting fees.

6) This report is based upon field work completed by myself and from data obtained from various geological reports and other published materiaL

Dated at Scarborough, Ontario, Canada this 6th day of October 2011.

11

L-'.:..::.2,'-'.:45:..:.:::0-'-!9 Pc:..c' m",-, 0=5--=-0--'--4--=-:20'-'.:'2=-------.!_':.::.6 --1-1_------=4:.:.:'6::..::2.::.:6'..:..:7 5::.:::28~----1~ ra Is 416-261-7528

QUALIFICATIONS

I, Chris North, resident of 129 Midland Avenue, Scarborough, Ontario hereby certify that:

p.16

1) I am a graduate of Lake Superior State University, Sault Ste. Marie, Micrugan, U.S.A receiving an Bachelor of Science Degree in Geology in 1986

2) I am a graduate of Sault College of Applied Arts and Technology receiving a Geological Engineering Technology diploma in 1983

3) 1 have practiced my profession for 25 years, managing and supervising many Exploration and development programs.

4) During the period November 3, 2009, October 9 and 1 0 of2010 and on September 16, 17 and 18 2011, I have visited the property.

5) I have received no compensation for this report other than the normal consulting fees.

6) This report is based upon field work completed by myself and from data obtained from various geological reports and other published materiaL

Dated at Scarborough, Ontario, Canada this 6th day of October 2011.

11

L---'.::12,,-,:4.::..:5 :-,-,09-,,-p:.:;c,m.:..:, O.::...5--'-04_-..::c20:..:.12=--L-.C:17_IL-_ --'4-'.::16c.:::2::..:61...:.-75:.:2.::...8 _ _ ~ ra Is

Appendix 1

Figures

416-261-7528 p.17

12

L---'.::12,,-,:4.::..:5 :-,-,09-,,-p:.:;c,m.:..:, O.::...5--'-04_-..::c20:..:.12=--L-.C:17_IL-_ --'4-'.::16c.:::2::..:61...:.-75:.:2.::...8 _ _ ~ ra Is

Appendix 1

Figures

416-261-7528 p.17

12

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':E ~". '.,

.ki!f10H

",

-,- ... ... ?-' .. ..,

....... ' .--.

Strike Minerals West Hemlo Project

Schreiber, Ontario

~ f/'f.lIo2CTJ

• - E:ea.rd~

• West Hemlo Project

- -"*

Y " " :J. . ,' ....

, ~uit SIce M~r ... , -1

'.-

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416-261-7528

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:.. ..... ... I ~ ' \'"

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p.18

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. -" - .. ~ .. : .. ;

r- ~ ..... ~ .

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':E ~". '.,

.ki!f10H

",

-,- ... ... ?-' .. ..,

....... ' .--.

Strike Minerals West Hemlo Project

Schreiber, Ontario

~ f/'f.lIo2CTJ

• - E:ea.rd~

• West Hemlo Project

- -"*

Y " " :J. . ,' ....

, ~uit SIce M~r ... , -1

'.-

.. ,

416-261-7528

~'f •

:.. ..... ... I ~ ' \'"

\ ~ . ~. i

p.18

,. i ..

. -" - .. ~ .. : .. ;

r- ~ ..... ~ .

L-'.:..::.2,-,,: 45:..:..:: 0--,-,9 Pc.:.:' m=, .::..:.05--=-0--,--4 --=-20,-,,'20--11_ '.:..::.9 -L1 __ 4,-,-'6:....:2.::...:6'--,--7 5=-=-28'--------'~ ra Is 416-261-7528

Strike Minerals West Hernlo Project

480000 I

2

j

i

483000 I

2 62

.,.,. .. ,

Lake Superior (rae Superieur)

--• .. --

Coordinate System: NAD 1983 UTM Zone 16N Projection: Transverse MercatorNorth American 1983

I I

486000 I

! Schreiber North Claims

N

s

• 0.0301 - 0.7010 D Staked Claims

• 0.7011 - 5.5000 ,": AHenations

• 5.5001 - 13.0000

I 480000 483000 486000

p.19

1- 8 C> 10 <:> ;};

o rg o o ..,. tl)

1,500 750 0 1,500 Meters Schreiber Key Map Figure 2

Drawn by: Chris North Sept. 26, 2011

Reference Scale: 1 :60,000

L-'.:..::.2,-,,: 45:..:..:: 0--,-,9 p,-",m=, .::..:.05--=-0--,--4 --=-20,-,,'20--11_ '.:..::.9--L1 __ 4,-,,'6:....:2.::...:6'--,--7 5:..:.28'---1~ ra Is 416-261-7528

Strike Minerals West Hernlo Project

480000 I

2

j

i

483000 I

2 62

.,.,. .. ,

Lake Superior (rae Superieur)

--• .. --

Coordinate System: NAD 1983 UTM Zone 16N Projection: Transverse MercatorNorth American 1983

I I

486000 I

! Schreiber North Claims

N

s

• 0.0301 - 0.7010 D Staked Claims

• 0.7011 - 5.5000 ,": AHenations

• 5.5001 - 13.0000

I 480000 483000 486000

p.19

1- 8 C> 10 <:> ;};

o rg o o ..,. tl)

1,500 750 0 1,500 Meters Schreiber Key Map Figure 2

Drawn by: Chris North Sept. 26, 2011

Reference Scale: 1 :60,000

~,-z: 4-5.-09- p.-m .-05- 0-4 -zo-'z-----rl-:cz-=-O '-1 - ----;-:4'';:-:6 Z~6';-:;75~Z8;;------""""'~ fa Is 416-261-7528 p.20

420

Strike Minerals West Hernlo Project

s

3015151

TB3798

TB38D1

T83719

.Oe5 •• •• 0.01

4BOOOO

3015150

677429 TB3808

939530 T83800

T85528 768805

i BJ122 ,

768802

TB3799 939529

• O.02~-s.--------+------f 4205993 TB3781

BJ1Z3

R665

909274

677428

LOCNO.2

R608 R606

5.5. 063 3.6 .3-

R609

909275 66

1224800

1183300 114 41

Loe NO.1 114 41

4211127 R610

Legend

~~ Lakes Rock Samples

AU_rLt1 o Patent Claims

0.0050 - 0.0300 CJ Staked Claims

• 0.0301 - 0.7010 '=J Alienations

Lake Superior (lac S Coordinate System: NAD 1983 UTM Zone 16N

• 0.7011 - 5.5000

• 5.5001 - 13.0000 P 'ection: Transverse MercatorNorth American 1983

4flOOOf) 210 o 420 Meters

Reference Scale: 1 :15,000

Schreiber South Claims Figure 3

Drawn by: Chris North Sept 26,2011

~,-z: 4-5.-09- p.-m .-05- 0-4 -zo-'z-----rl-:cz-=-O '-1 - ----;-:4'';:-:6 Z~6';-:;75~Z8;;------""""'~ fa Is 416-261-7528 p.20

420

Strike Minerals West Hernlo Project

s

3015151

TB3798

TB38D1

T83719

.Oe5 •• •• 0.01

4BOOOO

3015150

677429 TB3808

939530 T83800

T85528 768805

i BJ122 ,

768802

TB3799 939529

• O.02~-s.--------+------f 4205993 TB3781

BJ1Z3

R665

909274

677428

LOCNO.2

R608 R606

5.5. 063 3.6 .3-

R609

909275 66

1224800

1183300 114 41

Loe NO.1 114 41

4211127 R610

Legend

~~ Lakes Rock Samples

AU_rLt1 o Patent Claims

0.0050 - 0.0300 CJ Staked Claims

• 0.0301 - 0.7010 '=J Alienations

Lake Superior (lac S Coordinate System: NAD 1983 UTM Zone 16N

• 0.7011 - 5.5000

• 5.5001 - 13.0000 P 'ection: Transverse MercatorNorth American 1983

4flOOOf) 210 o 420 Meters

Reference Scale: 1 :15,000

Schreiber South Claims Figure 3

Drawn by: Chris North Sept 26,2011

L-..:.' =-=2 :4:.:::5 : 0~9 .t:.:.:p . m:::.:. O~5-~04~-2:.::.:0'~2 ---11----=2,,---, -,---I _~4'--'-"6'_=_26'_'__' ,-",752,-,--8 _ _ frals 416-261-7528 p.21

Strike Minerals West Hernia Project

433000

4258259

4256985 · . .. s

4207491

4207492

TB1049

4240565

425~7 I i

\ j

I Schreiber North Claims I i i !

·1 4246281 . 13

!

42405551 mnrnJ"!:lIrD ~VStl~~ NAD 1983UTM Zoned6N!

o

4256266

.0.008 •

4256292

Legend

Rock Samples

AUJLt1 • 0.0050 - 0.0300

--·--_---'--.-I-·~8 o to o

D Staked Claims

c:::::< Patent Claims

=--= Alienations

~

• 0.0301 - 0.7010 0 LAKES

• 0.7011 - 5.5000

• 5.5001 - 13.0000

550 275 0 550 Meters 483000 .-=:11£::::::1 ___ • Schreiber North Claims Drawn by: Chris North

Sept. 26, 2011 Reference Scale: 1 :20,000

Figure 4

I

L-..:.' =-=2 :4:.:::5 : 0~9 .t:.:.:p . m:::.:. O~5-~04~-2:.::.:0'~2 ---11----=2,,---, -,---I _~4'--'-"6'_=_26'_'__' ,-",752,-,--8 _ _ frals 416-261-7528 p.21

Strike Minerals West Hernia Project

433000

4258259

4256985 · . .. s

4207491

4207492

TB1049

4240565

425~7 I i

\ j

I Schreiber North Claims I i i !

·1 4246281 . 13

!

42405551 mnrnJ"!:lIrD ~VStl~~ NAD 1983UTM Zoned6N!

o

4256266

.0.008 •

4256292

Legend

Rock Samples

AUJLt1 • 0.0050 - 0.0300

--·--_---'--.-I-·~8 o to o

D Staked Claims

c= Patent Claims

=--= Alienations

~

• 0.0301 - 0.7010 0 LAKES

• 0.7011 - 5.5000

• 5.5001 - 13.0000

550 275 0 550 Meters 483000 .-=:11£::::::1 ___ • Schreiber North Claims Drawn by: Chris North

Sept. 26, 2011 Reference Scale: 1 :20,000

Figure 4

I

L--':.::.:2:.::..:45c..:.:09::.!p:::;., m:.:..;:' O~5--=-04:....:-2==-O':..:.2 -LI -=.:22'---.J1~_4_'6-,2,-6 '_7 5-=-28~--,~ ra Is 41 6-261-7528 p.22

10

Strike Minerals West Hernlo Project

. O_~iO.31 , .017

'TB3327

Coordinate System: NAn 1983 UTM Zone'16N Pro'ection: TranSverse MercatorNorth American 1983

N

' S

I Schreiber Central Group I,'

Legend

- ROADS Highway 17

CJ Patent Claims

• 0_0050 - 0.0300 0 Staked Claims

• 0.0301 - 0.7010 C Alienations

• 0.7011 - 5.5000 CJ LAKES

• 5.5001 - 13.0000

5 o 10 Meters

Reference Scale: 1 :500

Schreiber Central Claims Figure 5

Drawn by: Chris North Sept 26,2011

L--':.::.:2:.::..:45c..:.:09::.!p:::;., m:.:..;:' O~5--=-04:....:-2==-O':..:.2 -LI -=.:22'---.J1~_4_'6-,2,-6 '_7 5-=-28~--,~ ra Is 41 6-261-7528 p.22

10

Strike Minerals West Hernlo Project

. O_~iO.31 , .017

'TB3327

Coordinate System: NAn 1983 UTM Zone'16N Pro'ection: TranSverse MercatorNorth American 1983

N

' S

I Schreiber Central Group I,'

Legend

- ROADS Highway 17

CJ Patent Claims

• 0_0050 - 0.0300 0 Staked Claims

• 0.0301 - 0.7010 C Alienations

• 0.7011 - 5.5000 CJ LAKES

• 5.5001 - 13.0000

5 o 10 Meters

Reference Scale: 1 :500

Schreiber Central Claims Figure 5

Drawn by: Chris North Sept 26,2011

,------,-=12,--: 4 5,-,,: 0,,-9 ""p. '...:en . ..:...:05--=-0,-,-4 -....:.20:..:.12::...-.JL...::::.23---L1 __ 4.:..:.-15::....:2c::c51c.:.7:..:.5 28=--_~ ra Is

Appendix 2

Assay Certificates

416-261 -7528 p.23

13

,------,-=12,--: 4 5,-,,: 0,,-9 ""p. '...:en . ..:...:05--=-0,-,-4 -....:.20:..:.12::...-.JL...::::.23---L1 __ 4.:..:.-15::....:2c::c51c.:.7:..:.5 28=--_~ ra Is

Appendix 2

Assay Certificates

416-261 -7528 p.23

13

'-~1~2 :~4~5 ~09~p-.m~. O~5-~O~4~-~20~1~2-'~24~----~41~6~2~6~1 ~75~2~8 ----'~rals 416-261-7528 p.24

Quality Analysis ... Innovative Technologies

Date SUbmitted: 28-Jal1-10

Invoice No.: A10-0351

Invoice Date: 18-Feb-10

Your Reference: CAN DIAN STAR

Canadian Star Minerals Ltd.

129 Midland Ave. Toronto ON M1 N 3Za Canada

ATTN: Chris North

CERTIFICATE OF ANALYSIS

7 Rock samples were submitted for al1alysis.

The following analytical packages were requested: Code 1A3-Ag Au, Ag·Flre Assay Gravimetric Code 1C-Exp Fire Assay-ICP/MS

REPORT A10-()351 Code 1H INAA(INAAGEO)fTotal Digestion ICP(TOTAl)

This report may be reproduced Without our consent. If onty selectep portions of !he report are reproduced, permission must be obtained. (1 no instructions were given at time of sample submittal regarding excess material, it will be discarded wi1hifl 90 days of this report. OUf liability is limited solely to the analytical cost of these analyses. Test results are representative only of material submitted for analysis.

Noles: We recommend reanalysis by lire assay Au, pt, Pd Code 8 if values exceed uoper limn. Elements which exceed the upper limits should be analyzed by assay techniques. Some elements are reported by mu'tiple techniques. These are indicated by MULT.

ACTIVATION LABORATORIES LTD.

CERTlFIED BY:

Emmanuel Eseme, Ph.D.

Quality Control

13~6 51lJ1Ohili Drive. An""""". Ontario Ganada1.lG ""5 T£LEPHONlC "".IlO5.64a~511 Or ... '.8B8.228.5227 FAX +1.905.~~.9613

E'MAllancasterliJact,ab3lnlcoo; ACTLABS GROUP WEBSITE http:.'IV .... vr.actlabslnt.:xlm

'-~1~2 :~4~5 ~09~p-.m~. O~5-~O~4~-~20~1~2-'~24~----~41~6~2~6~1 ~75~2~8 ----'~rals 416-261-7528 p.24

Quality Analysis ... Innovative Technologies

Date SUbmitted: 28-Jal1-10

Invoice No.: A10-0351

Invoice Date: 18-Feb-10

Your Reference: CAN DIAN STAR

Canadian Star Minerals Ltd.

129 Midland Ave. Toronto ON M1 N 3Za Canada

ATTN: Chris North

CERTIFICATE OF ANALYSIS

7 Rock samples were submitted for al1alysis.

The following analytical packages were requested: Code 1A3-Ag Au, Ag·Flre Assay Gravimetric Code 1C-Exp Fire Assay-ICP/MS

REPORT A10-()351 Code 1H INAA(INAAGEO)fTotal Digestion ICP(TOTAl)

This report may be reproduced Without our consent. If onty selectep portions of !he report are reproduced, permission must be obtained. (1 no instructions were given at time of sample submittal regarding excess material, it will be discarded wi1hifl 90 days of this report. OUf liability is limited solely to the analytical cost of these analyses. Test results are representative only of material submitted for analysis.

Noles: We recommend reanalysis by lire assay Au, pt, Pd Code 8 if values exceed uoper limn. Elements which exceed the upper limits should be analyzed by assay techniques. Some elements are reported by mu'tiple techniques. These are indicated by MULT.

ACTIVATION LABORATORIES LTD.

CERTlFIED BY:

Emmanuel Eseme, Ph.D.

Quality Control

13~6 51lJ1Ohili Drive. An""""". Ontario Ganada1.lG ""5 T£LEPHONlC "".IlO5.64a~511 Or ... '.8B8.228.5227 FAX +1.905.~~.9613

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Canadian Star Minerals 129 Midland Ave Toronto, On, CAN M1N 3Z8 Ph#: (416) 261-3925 FaX#: (416) 261-7528 Email#:northA4@pnmUS.ca.vdrylie@9mall.com

Certificate of Analysis

Date Received: 0913012010 Date Completed: 10108/2010

Job #: 201044177 Reference:

Sample #: 10 Rock

Arx ~ CII~nIID Au Ag N. A. B. Be III C. Cd Co Cr Cu Fe K 1I Mg Mn Mo NI P Pb 51> Se Sn Sr "Ii TI V W Y 7n ~~%~~~~%~~~~%%~I~~_~~~~~~~~~~~~ 269339 &13051 '0.005 8.09 <1 151 <\ <5 1.62 <~ B 334 7 2.23 \.03 43 1.59 430 16 40 511 6 <> ,5 2 327 941 6 50 <In A 68 289340 513052 0.005 6.72 <2 34li <I 14 3.04 <4 17 289 15 3.25 \.71 30 1.73 047 17 51 698 6 <5 '5 2 329 2050 B 85 <\0 \1 67 289341 613053 0.007 <1 10.09 2 3\l6 12 3.52 <4 23 370 32 4.29 1.55 .3 2.45718 18 72 m II <5 <5 <I 3752010 4 1\6 '10 14 81 265>42 613~' 0.007 I 8.90 2. 388 \1 3.03 <4 25 130 32 4.15 1.62 43 2.94 718 15 106 750 11 .5 <5 2 342 1993 104 <10 Ii 64 289343 613055 <1).005 1 9.&0 <2 \&1 13 2 .3~ <4 17 466 2~ 3.51 1.56 B2 1.45 628 1~ 15 611 4 <5 <5 110 356 n <10 H 289344 813056 0.Q10 \0.77 <2 459 19 3.93 <4 29 307 40 5.14 1.62 49 <.72 731 18 65 1073 6 <5 <6 46. 2266 <1 129 <10 16 87 289345 813057 0.023 10.01 3 16Q 8 5.22 <4 30 >61 87 512 l .gS 52 3.171999 18 127 \169 10 <S <5 228 2&1 11M <IU H 10\1 289346 &1305& 0.031 4.23 28 47 <I 5 OA8 <4 8 744 16 4.74 168 15 0.24 300 29 21 <100 13 <5 <5 <I 40 1\8 .. <10 " 22 .89347 613069 I).OH 7.06 419 135 I, 250 5 35 419 \00 883 HO 22 1.39 \562 21 46 374 1\ <5 <5 122 ~198 2 181 <10 1& 71 289346 G\J060 0.015 6.2" l:l;) 112 2 2l 2.76 61 187 266 13.59 \ .06 46 2.lI223& 25 1\3 535 16 <5 <5 \06 6518 <1 272 <10 ~7 liZ 2893490up 513060 0.015 753 yg 1\4 1 17 2.25 15 118 19:1 1004 ',.49 39 1.13 1708 21 83 404 12 <5 <5 3 96 5029 <1 205 '10 21 62

PROCEDURE CODES: ALP1. ALFA 1, ALMA 1

Certlflod BY;~._ ,c:::::J

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The reaUIlS Includ.d 00 this report relal. only to lhe l\em.te,led The cortln,.t. of AMlysl. ,hQuln nOI b. r.produceU excopt In full. without Iho ",rlllon approval of InA labOratOry

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Canadian Star Minerals 129 Midland Ave Toronto, On, CAN M1N 3Z8 Ph#: (416) 261-3925 FaX#: (416) 261-7528 Email#:northA4@pnmUS.ca.vdrylie@9mall.com

Certificate of Analysis

Date Received: 0913012010 Date Completed: 10108/2010

Job #: 201044177 Reference:

Sample #: 10 Rock

Arx ~ CII~nIID Au Ag N. A. B. Be III C. Cd Co Cr Cu Fe K 1I Mg Mn Mo NI P Pb 51> Se Sn Sr "Ii TI V W Y 7n ~~%~~~~%~~~~%%~I~~_~~~~~~~~~~~~ 269339 &13051 '0.005 8.09 <1 151 <\ <5 1.62 <~ B 334 7 2.23 \.03 43 1.59 430 16 40 511 6 <> ,5 2 327 941 6 50 <In A 68 289340 513052 0.005 6.72 <2 34li <I 14 3.04 <4 17 289 15 3.25 \.71 30 1.73 047 17 51 698 6 <5 '5 2 329 2050 B 85 <\0 \1 67 289341 613053 0.007 <1 10.09 2 3\l6 12 3.52 <4 23 370 32 4.29 1.55 .3 2.45718 18 72 m II <5 <5 <I 3752010 4 1\6 '10 14 81 265>42 613~' 0.007 I 8.90 2. 388 \1 3.03 <4 25 130 32 4.15 1.62 43 2.94 718 15 106 750 11 .5 <5 2 342 1993 104 <10 Ii 64 289343 613055 <1).005 1 9.&0 <2 \&1 13 2 .3~ <4 17 466 2~ 3.51 1.56 B2 1.45 628 1~ 15 611 4 <5 <5 110 356 n <10 H 289344 813056 0.Q10 \0.77 <2 459 19 3.93 <4 29 307 40 5.14 1.62 49 <.72 731 18 65 1073 6 <5 <6 46. 2266 <1 129 <10 16 87 289345 813057 0.023 10.01 3 16Q 8 5.22 <4 30 >61 87 512 l .gS 52 3.171999 18 127 \169 10 <S <5 228 2&1 11M <IU H 10\1 289346 &1305& 0.031 4.23 28 47 <I 5 OA8 <4 8 744 16 4.74 168 15 0.24 300 29 21 <100 13 <5 <5 <I 40 1\8 .. <10 " 22 .89347 613069 I).OH 7.06 419 135 I, 250 5 35 419 \00 883 HO 22 1.39 \562 21 46 374 1\ <5 <5 122 ~198 2 181 <10 1& 71 289346 G\J060 0.015 6.2" l:l;) 112 2 2l 2.76 61 187 266 13.59 \ .06 46 2.lI223& 25 1\3 535 16 <5 <5 \06 6518 <1 272 <10 ~7 liZ 2893490up 513060 0.015 753 yg 1\4 1 17 2.25 15 118 19:1 1004 ',.49 39 1.13 1708 21 83 404 12 <5 <5 3 96 5029 <1 205 '10 21 62

PROCEDURE CODES: ALP1. ALFA 1, ALMA 1

Certlflod BY;~._ ,c:::::J

()~k. Oorn~.,if.J'J~ H (1SG • LltlOr'ltOIY M,,-:ao~

The reaUIlS Includ.d 00 this report relal. only to lhe l\em.te,led The cortln,.t. of AMlysl. ,hQuln nOI b. r.produceU excopt In full. without Iho ",rlllon approval of InA labOratOry

.109~.IOI1512010 5:04 PM

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·1 093-11/01120114:09 PM

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Tuesday. November 1, 2011

Canadian St., MIn.",I. 129 Midi<lnd Ayo Toronlo, On, CAN M1N no Ph#: (416) 261·3925 Fa.!!: (416)261.7528 Emalt cnortM4@gmaB.com, vdrylift@gmalJ.Q)O\

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Certificate of Analysis

CH.nt 10 Au Ag A! '.\

Ai 8& & 131 C$CdCoQCI,I

,. ppm ppm ppm ppm Fa

pj>b ppm ppm ppM gpm wm ppm '. 5207

o;!11t

52<142

52443

024"

52 .. 6

524480

50!41

oms 5"4~

62450

52451

52452

62453

10B.I963

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10B~58

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106m2

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1086974

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10!51l77

1085978

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1085981

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71

210

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4004

302

701

13000

I1lJO

<1 1.37

<I 1.32

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<, J.21

£ 1 O.3g

.::1 0.5:'

<01;. 1.03

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-=t 1,44

<t 0.91

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2.78

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<I 1.37

0.60

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1M)

154

1604

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792

42a

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PROCEDURE CODES: ALP1, ALFA1. AlAR 1

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TM raWlls included on 11113 report relate only 10 !he Ilem. lested The Cerllncale 01 Analysts should 1101 08 "proauCQ~ exceplln full, wllho'Jtlhe Iwillen approval "' Iho I.>bo,alory

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Page 1 of 1

Dam Re=oIve<l: 0912912011

OJ I. Cvrnplolod: 101111201 1

Job #:201110467

Reteronca: Sample#: 19

NIl Ni PbSbS. SiSuSr 'J'JTIVW ~ % ppm ppm PIl'" _ ppm % ppm ppm ppm pp!.n pprn ppm PP"\ ~

10 0.16 59

0.01

m 709

44

o.u 53 649 ue

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0.20

0.20

15 1187

61 1664

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0.27 123 821

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·1 093-11/01120114:09 PM