2·53125

SUMMARY REPORT

ON

RE-ESTABLISMENT OF CLAIM BOUNDARY

On

CLAIM 3003829

In

CARR TOWNSHIP (Larder Lake Mining Division)

NTS 42 A/09

FOR

ST ANDREW GOLDFIELDS LTD.

Report prepared by: Craig Todd, P. Geo. For: St Andrew Goldfields Ltd. 25/10/2012

o

2.53125

SUMMARY REPORT

ON

RE-ESTABLI SM ENT OF CLA IM BOUNDARY

On

CLAIM 3003829

In

CA RR TOWNSHIP (Larder Lake Mining Division)

NTS 42 N09

FOR

ST AN DREW GOLDFIELDS LTD.

Rcpon prepared by: Craig Todd, P. Geo. For: St Andrew Goldfields Ltd. 25/1 0/20 12

I

TABLE OF CONTENTS:

Introduction:

Location and Access:

Previous Work:

Regional Geology:

Property Geology:

Re-establishment of Claim:

Conclusion:

Certificate:

References:

LIST OF FIGURES

FIG 1:

FIG 2:

FIG 3:

Pg.l

Pg. 1

Pg.l

Pg.2

Pg. 2

Pg.3

Pg.3

Pg.4

Pg. 5

Property Location within Ontario

Property Location within Township

Claim showing Re-established Lines

TABLE OF CONT ENTS:

Introduction :

Locat ion and Access:

Previous Work:

Regional Geology:

Property Geology:

Re·establishment afClaim:

Conclusion:

Certifi cate:

References:

LIST OF FIGURES

FIG I:

FIG 2:

FIG 3:

Pg. I

Pg. I

Pg. I

Pg.2

Pg. 2

Pg. 3

Pg.3

Pg. 4

Pg.5

Property Loca ti on within Ontario

Property Locat ion within Township

Claim showing Rc-established Lines

1.

INTRODUCTION:

Claim 3003829 is 100% owned by S1. Andrew Goldfields Ltd. (SAS), being staked on November, 01 , 2006. The block consists of 4 unpatented mining units , approximately 64 hectares or 160 acres, in the N 112 of Lot 12, Con 1, in COOK Township, Larder Lake Mining Division. See FIG 1 for property location within Ontario. A program of re-establishing the claim boundaries was conducted on the property during mid October, 2012.

LOCATION & ACCESS:

Claim 3003829 is located in the southwest comer of Carr Township approximately 6.0 kilometers east of Matheson, Ontario. Access to the property is excellent and is via provincial highway 101 six kilometres east of Matheson. At the intersection of provincial highway 101 and 11, an all weather gravel road may be seen trending north . This road is the Taylor/Carr township line. Proceed up the township line gravel road for approximately 2.0 kilometers. At approximately the 2.0 kilometer mark, the center of the property is to the left (east). Approximately one quarter of the property adjacent the N-S access road is farm pasture. See FIG 2.

PREVIOUS WORK:

In 1947, the ODM (Ontario Department of Mines) carried out a mapping program of the area including Carr Township. During this survey, a west to northwest trending fault zone was inferred to traverse the area north of claim 3003829. This fault is believed to be the Destor Porcupine Fault Zone (DPFZ).

In 1997, St Andrew Goldfields Ltd. (SAG) contracted Quantec Geophysics to carry out a 5.7 kilometer IP survey on the property which was then claim 1027346. Several local chargeability anomalies associated with resistivity features suggest lithological changes. Localized decreased resistivity may have identified a fault or shear. As well, several localized weak chargeability anomalies may suggest massive sulphides or graphitic horizons associated with the possible fault zones. Several other increased chargeability anomalies may suggest sulphide zones associated with geological contacts. In short, several drill targets were identified for follow-up. Quantec did however suggest that a ground magnetic survey be canied out prior to drill follow-up.

In 1999, SAG carried out a geochemical survey by Dr. Serge Nadeau. The claim at that date was referred to as 1207346. The survey was carried out in October 1999 and 39 "B" soil samples were collected in zip-lock bags. The main elements being sample for were Au, As, Hg, Cd, Pb and Mo. However, a 50 element ICP package was also included. In short, Au values from <0.2 to 2.0 ppb gold were returned. A diagram/air photo was provided with the assessment report showing the sample line drawn on the photo. It appears that Mr. Nadeau sampled parallel to the Taylor/Carr

I.

INTRODUCTION :

Clai m 3003829 is 100% owned by S1. Andrew Goldfields Ltd. (SAS), be ing slaked on November, 0 I, 2006. The block consists of 4 unpa tented mining units, approximately 64 hectares or 160 acres, in the N 112 of Lotl2 , Coni, in COOK Townshi p, Larder Lake Mining Division. See FIG t for property location wi thi n Ontari o. A program af re-establ ishi ng the claim boundari es was conducted on the property during mid October, 20 I 2.

LOCATION & ACCESS :

Claim 3003829 is located in the southwest comer of Carr Township approximately 6.0 kilometers east or Matheson, Ontario. Access to the property is excellent and is via provincial highway 10 1 six kilometres cast of Matheson. At the intersection or provincial highway 101 and I I, an all weather gravel road may be seen trending north. Th is road is the Taylor/Carr township line. Proceed up the township line gravel road for approximately 2.0 kilometers. AI approximately the 2.0 kilometer mark, the cente r of the property is to the left (cast). Approxi mately one quarter of the property adjacent the N-S access road is fann pasture. See FIG 2.

PREVIOUS WORK:

In 1947, the ODM (Ontario Department o f Mines) carried out a mapping program of the area including Carr Township . During thi s survey, a west to northwest trending fau lt zone was inferred to traverse the area north of cla im 3003829. Th is fault is beli eved to be the Destor Porcup ine Fau lt Zone (DPFZ).

In 1997, St Andrew Goldfields Ltd. (SAG) contracted Quantec Gcophysics to carry out a 5.7 kilometer IP survey on the property which was then claim 1027346. Several loea l chargeability anomalies associated with resistivity fea tures suggest li thological changcs. Locali zed dccreased resisti vity may ha ve identifi ed a fault or shear. As well , severa l local ized weak chargeab ility anomalies may suggest massivc sulphides or graphitic horizons assoc iated with the poss ible fault zones. Sevcral other increased chargeabil ity anomalies may suggest sulphide zones associated with geological contacts. In short, severa l drill targets werc ident ified for follow-up. Quan tcc did however suggest that a ground magnetic survey be can ied out prior to dri ll follow-up.

In 1999, SAG carri ed out a geochemical survey by Dr. Serge Nadeau. The claim altha! date was referred to as 1207346. The survey was carried out in October 1999 and 39 "8" soil samples were collected in zip-lock bags. The main clements being sample fo r were Au, As, i-I g, Cd, Pb and Mo. However, a SO clement ICP package was also included. In short, Au values from <0.2 to 2.0 ppb go ld were retumed. A diagram/air photo was provided with the assessment report showing the sample line drawn on the photo. It appea rs that Mr. Nadeau sampled para llcllo the Tay lor/Carr

~S' Property Location

within Ontario

Re-established Claim Boundaries CARR Township Claim 3003829

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Township line/road. The sample line appears to be approximately 5.0 to 10.0 meters east of the N-S trending gravel road, two thirds which appear to be pasture. Mr. Nadeau writes in his conclusion that "several chemical elements, that although significantly above their detection limit, in both A and B soil samples probably reflect the superposition of several processes: farming, soil contamination and geological features or processes. "He suggests that the probability of gold mineralization on this claim is low. Perhaps ifMr. Nadeau sampled farther east or west of the gravel road, gold values would have been higher. His sampling survey may have been contaminated by road dust and gravel as well as by previous farming activity. Sampling away from the road may have eliminated much of the possible contamination.

In October, 2004, SAG carried out a mapping and soil sampling survey as a follow-up to Dr. Nadeau's geochem survey in 1997. The survey was conducted over 5 flagged sample lines with samples taken every 25 meters. All samples were taken at 20.0 cm depth in "B" horizon soils. The samples were taken and placed into plastic sandwich bags, dried and taken to Swastika Labs in Swastika, Ontario. Gold values from nil to 9 ppb were encountered, most being nil to 2 ppb gold with one sample at 9 ppb and a second at 7 ppb gold. The conclusion suggests that deep clay overburden may have masked gold mineralization.

REGIONAL GEOLOGY:

The property is located in the Timmins-Kirkland Lake portion of the South-Western Abitibi Greenstone Belt. The Archean rocks of the belt form a thick succession of predominantly mafic volcanic rocks with lesser sedimentary and felsic volcanic units scattered throughout the belt. The succession forms a broad, easterly plunging synclinorium stretching from the Timmins area eastward to the Noranda area of Quebec. A number of major brittle to ductile deformation zones transgress these supracrustal rocks with the DPFZ being the most significant. Gold deposits are commonly localized within and or adjacent to the DPFZ along its 200 kilometer length from Timmins through the Matheson area and eastward beyond the Destor area of Quebec. Parallel to the DPFZ and nOlih of claim 3003829 in a NW -SE direction is the Pipestone Fault. This fault hosts the Clavos Mine (SAG) to the west. Through geological mapping, diamond drilling and magnetic surveys several NE and NW trending short strike faults are also inferred.

PROPERTY GEOLOGY:

Approximately half of the property is farm pasture. The pasture fields occupy the north half of the property. The north and central part is occupied by a north trending creek with several beaver ponds. The south half of the property is flat lying with mixed deciduous and conifers. Cunentiy, the southern half of the property is undergoing selective logging. The north half of the claim block appears to be old pastures that are currently being used for hay fields. The fields are flat lying to gently rolling with some local incised gullies that host intermittent streams that are tributaries of the Watabeag River. The claim appears to be devoid of outcrop and is generally covered by overburden. Interpretation from government maps and airborne magnetics suggests that the claim is

2.

Township line/road . The sample line appears to be approx imately 5.0 to 10.0 me ters east of the N-S trending gravel road, two thirds which appear to be pasture. Mr. Nadeau writes in his conc lusion that "several chemical elements, Ihal although significantl y above th ei r detection limit , in both A and B so il samples probab ly refl ect thc superpos ition of several processes: famling, soil contamina tion and geological features or processes. "He suggests that thc probability of gold mineralization on thi s claim is low, Perhaps if Mr. Nadeau sampled farther cast or wcst of the grave l road, gold va lues wou ld have been higher. His sampling survey may have been contaminated by road dust and gravel as well as by previous farming activ ity. Sampling away from the road may have eliminated much o f the poss ible contaminat ion.

In October, 2004, SAG carried out a mapping and so il sampling survey as a follow-up to Dr. Nadeau's geochem survey in 1997. The survey was conducted over 5 flagged sample lines wi lh samples taken every 25 meters. All samp les were taken al 20.0 cm depth in "B" horizon so ils. The samples were taken and placed into plast ic sandwich bags, dri ed and taken to Swastika Labs in Swastika, Ontario. Go ld va lues From nillo 9 ppb were encountered, mos t being nil to 2 ppb gold with one sample at 9 ppb and a second al 7 ppb go ld. The conclusion suggests Ihal deep clay overburden may have masked gold mineralizati on.

REGIONAL GEOLOGY;

The property is located in th e Timmins-Kirkland Lake portion of the South-Western Abitibi Greenstone Belt. The Archean roc ks o f the be lt fonn a thick succession of predominan tly mafic volcanic rocks wilh lesser sedimentary and felsic volcani c unit s scattered throughout the belt . The succession forms a broad, easterly plunging synclinorium stretching from the Timmins area eastward to Ihe Noranda area o fQucbec. A number of major brittle 10 ductil e deformation zones transgress th ese supracrustal rocks with the DPFZ being the most signifi cant. Gold depos its arc commonly loca li zed within and or adjacent to the DPFZ along its 200 kilometer length from Timmins through the Matheson area and eastward beyond th e Destor area of Quebec. Parallel to the DPFZ and nOlih of claim 3003829 in a NW-SE di rection is the Pipestone Fault. This fault hosts the Clavos Mine (SAG) to th e west. Through geological mapping, diamond drill ing and magnet ic surveys several NE and NW trending short strike fault s arc also inferred.

PROPERTY GEOLOGY;

Approxi matcl y half of the property is fann pasture. The pasture fi elds occupy the nort h half of the property. The north and central pari is occupied by a north trending creek with several beaver ponds. The south hal f of the property is nat lying wi th mixed dec iduous and conifers. Cunently, the southern half ofthe property is undergoing se lec tive logg ing. The nonh half of the clai m block appears to be old pastures Ihat are currently being used for bay ficlds. The fi elds arc nal lyi ng 10 gently rolling wi th some loca l incised gull ies that host intermittent streams Ihal arc tributaries of the Watabeag Ri ver. The clai m appears to be devoid of outcrop and is generall y covered by ove rburden. Interpretation from government maps and airborne magneti cs suggests that the claim is

3.

underlain by variable flows of Fe and Mg rich mafic volcanic rocks from the Kinojevis Group of Archean age.

RE-ESTABLISMENT OF CLAIM BOUNDARY:

Mid October 2012, a crew from St Andrew Goldfields, of Matheson, ON, brushed, blazed and flagged the boundaries on claim 3001363, for a total of approx 3.2km. Employees were Heather Davidson and Vincent Berard. See FIG 3 for Claim Outline map showing lines that were re­established.

CONCLUSION:

The re-establishing of the boundaries was successful in identifying and physically establishing the extents of claim 3003829. This will facilitate in the planning of future exploration.

Report prepared by: Craig Todd, P. Geo. For: St Andrew Goldfields Ltd. 25/10/2012

3.

underlain by variable flows of Fe and Mg rich mafic volcan ic rocks from the Kinoj cvis Group of Archean age.

RE-ESTABLISMENT OF CLAIM BOUNDARY:

Mid October 2012, a crew from 51 Andrew Goldfields, of Matheson, ON, brushed, blazed and flagged the boundaries on clai m 300 1363, for a total of approx 3.2km. Employees were Heather Davidson and Vincent Berard. See FIG 3 for Claim Out li ne map showing lines that were re­estab lished.

CONCLUSION:

The fe-establishing of the boundaries was success fu l in identifying and physically estab li shing the ex tents of cla im 3003829. This will facilitate in the planni ng of future exploration.

Report prepared by: Craig Todd, P. Geo. For: 51 Andrew Goldfields Ltd. 2511 0/20 12

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4.

CERTIFICATE OF QUALIFICATIONS

I, Craig Todd of 22 Harding Ave, Kirkland Lake, Ontario, do hereby declare:

• I graduated from the Laurentian University in 1979 with an Honours BSc degree in

Geology.

• I have been employed full time in the Geosciences industry since graduation

• I have worked primarily in gold exploration and extraction in Abitibi Greenstone Belt for

the majority of my working career.

• I am a salaried employee of St Andrew Goldfields since October, 2008

• I am a registered member in good standing of the Association of Professional

Geoscientists of Ontario.

Signed:

Craig Todd, P. Geo.

4.

CERTIFICATE OF Q UA LIFICATIONS

I, Craig Todd of22 Harding Ave, Kirkland Lake, Ontario, do hereby declare:

• I graduated from the Laurentian University in 1979 with an Honours S Se degree in

Geology.

• I have been employed fu ll ti me in the Geosciences industry since grad uat ion

• I have worked pri maril y in gold explorat ion and extract ion in Ab itibi Greenstone Belt for

the majori ty afmy working career.

• I am a sa laried employee of SI Andrew Goldfie lds since October, 2008

• I am a reg istered member in good standing of the Assoc iat ion of Professiona l

Geosc ienti sts of Ontario.

Signed:

Craig Todd, P. Gco.

· .

5.

REFERENCES:

Ayer, 1.A., Berger & Trowel N.F.

1999: Geological Compilation of the Lake Abitibi Greenstone Belt; Ontario Geological

Survey, Map p3398, Scale 1: 100,000

Bath, A.C.

1990: Mineral Occurrences, Deposits and Mines of the Black River-Matheson Area;

Ontario Geological Survey, Open File Report 5735, 1883P.

Leahey, M.W.

2004: Assessment Report-Prospecting Report ofthe L-3001417 Property, Carr Township.

Assessment Report 2.28631 , October 20,2004.

Nadeau, S.

1999: Exploration Activities in 1999 for St. Andrew Goldfields ltd, Carr Claim 1207346

in Carr Township, Larder Lake District of Cochrane, Ontario. Tuesday, October 19,

1999.

Wayne, GRJ., Oswald, A., Legault, 1M., Blackshaw,

1997: Assessment RepOli-Quantec Geophysical Report-LP Survey, Carr Township,

Matheson, Ontario on behalf of St. Andrew Goldfields Ltd.

5.

REFERENCES:

Ayer, I .A., Berger & Trowel N.F.

1999: Geological Compilation of the Lake Ab itib i Greenstone Belt ; Ontario Geolog ica l

SlI rvey, Map p3398, Scale I: I 00,000

Bath, A.C.

1990: Minera l Occurrences, Deposi ts and Mines of the Black Ri ver-Matheson Area;

Ontari o Geological Survey, Open File Report 5735, 1883 P.

Leahey, M.W.

2004: Assessmen t Report-Prospecting Report orthe L-300 14 17 Property, Carr Townshi p.

Assessment Report 2.2863 1, October 20,2004.

adeau, S.

1999: Exp lora tion Activities in 1999 for St. Andrew Goldfie lds lid, Carr Claim 1207346

in Carr Township, Larder Lake Distri ct of Cochrane, Ontario. Tuesday, October 19,

1999.

Wayne, G RJ ., Oswald, A. , Legault, 1M., Blackshaw,

1997: Assessment RepOli -Quantec Geophysica l Rep0rl-LP Survey. Carr Township,

Matheson, Ontario on behalfofSI. Andrew Goldfie lds Ltd.