August 21, 2007

BRIAN FOWLER

Magnetic Survey Killala Lake Property

Killala Lake Area Claim Map G-0596

Schreiber - Hemlo District Thunder Mining Division

Ontario

42 E /02 SE UTM 531000E, 5434000

REPORT REC

Oc I 1 8 2007 '1vv

GEOSe, He! ASSEssrJ)::::r'n OF ICE

2-36125 Mike Vumbaca, B.Sc.

Mountain Valley Geophysics Corp

Office Toronto Ontario (416) 249-6664 1 (866) 452 3804

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TABLE OF CONTENTS

PAGE

1. INTRODUCTI01\J ............ , ................ , ............. , .............................. ', .. ", ................... 5

2, PROPERTY, LOCA nON AND ACCESS ............................................................. 5

3. CLAIMS ................ , ...................... , ... " ................... , ...... , ........................................... 6

4. PERSON1\EL AND INSTRUMENTATION .......................................................... 6

5, INSTRLTMENTATION ... , .......... , ....... , ........... , ........................................ , ................ 6

6. BASE Sl·ATION ... , ............................ , ......................... , ..... , ................. , .. ,., .............. 7

7. SENSOR ORIENTATION ......... , ..... , ........................................ , ..... , ........................ 8

8. SIGN CONVENTION ..... , ........... , ........ , ........... ', ................ " ... , ................. , ... , ......... 8

9. DILTRNAL CORRECTIONS ........... , .... ,., ............................ , .......... , ........................ 8

10. FIELD WORKSTATION ........................................................................................ 8

11. PREVIOUS WORK ............................................................... , ...... , ....................... , .. 8

12. REGIONAL GEOLOGY ............................................. , ........................................... 9

13. PROPERTY GEOLOGY ......................................................................................... 9

14. FIELD WORK AND PROCEDURE ....................................................................... 9

15. 'NIAGNETIC SURVEy ..................... , ...................................................................... 10

15.1 Purpose of the Magnetic survey and methodology ................................................................ J 0

15.2 Presentation of the results ...................................................................................................... 10

15.3 Results of the Magnetic survey .............................................................................................. 10

16. DISCUSSION OF THE GEOPHYSICAL RESULTS ............................................ 10

17. CONCLUSION and RECOMYfENDATIONS ........................................................ IO

18. ST A TEJ'v1ENT of COSTS ........................................................................................ 11

3 LIST OF MAPS

CERTIFICATE OF QUALIFICATIONS

APPENDIX A : CLAIM MAPS AND ABSTRACTS

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LIST OF MAPS

Scale: 1 : 2 500

Magnetometric

Magnetic Contours

Magnetometric

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1 INTRODUCTION

At the request of Mr. Brian Fowler, a Magnetic survey was performed on the Killala Lake Property. The geophysical survey was calTied out in April 2007 and it included a Mag survey over various grid lines . The survey grid totalled 6.5 km. This property is located southwest of the Manitouwadge camp, a few kilometers southwest of the Killala Lake Alkalic Complex. A Mag survey was performed over two (2) new grids to highlight areas of potential mineralization.

2. PROPERTY, LOCATION AND ACCESS

The Killala property is located in the KillaJa - Vein Lake area of the Thunder Bay .\!fining District, approximately 60 km southwest of Manitouwadge and 240 km northeast of Thunder Bay. The property can be accessed by logging roads on Hwy 17. The logging roads are then travelled for aboUl 30 kilometers north to the property.

Superior Lake Figure 1. Localization of the Killala Lake Property

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3. CLAIMS

The Killala Lake property consists of 10 claim units located in the Killala Lake area of the Thunder Bay Mining District, approximately 60 km southwest of the Manitouwadge camp area.

List of Claims

T.B. 3016093 3016094 4211920 Registered in the name of Brian Fowler (33%), Patrick Dick (33.3%), and David Wrona (33.3%).

TB 4214266 Registered in the name of Brian Fowler (100%).

4. PERSONNEL AND INSTRUMENTATION

The following instruments were used for the Magnetometer survey:

Two Scintrex ENVI Proton Magnetometers, a mobile and base station.

5. INSTRUMENTATION

Model:

Type:

Total Field Range:

Total Feld Accuracy:

Sensitivity:

Sample Rate:

Tuning:

Reading Period:

Cycle Time:

Cycle Delay:

Scintrex ENVI MAG sensor Part Number 788001

proton magnetometer, Part Number 788 020

20,000 to 100,000 nT.

± 1 nT.

0.1 nT at 2 second reading time, reduced at other reading times.

2 per second

Fully solid state. Manual or automatic; keyboard selectable

0.5, 1, or 2 seconds

External any, as long as it exceeds the reading period and is initiated by a command at the RS-232 interface.

minimum determined by the reading 8 sec in 1 ms intervals

Data Acquisition System: LCD 8 by 40 Super-twist electronics console, Part Number 788013

Data Memory: 151,000 - 750,000 readings

Data Presentation: Up to 178 readings in graphic mode.

Data Output Format: Data dump in memory or on a line by line basis in digital or hardcopy formats.

Power Supply: 2.3 Ah Lead Acid battery. 12 V at 0.65 Amp

Environmental Range: -40° to 60° C. Humidity 0 - 100% Fully sealed desiccant cartridge.

6. BASE STATION

Same as above (section 5) except for;

Cycle Time:

Data Memory:

Power Supply:

Internal - minimum is determined by the reading period, max 9999 sec in 1 sec intervals

28,000 - 140,000 readings.

12 V external battery

The base station was located approximately 50 m away from the edge of a base cabin at

coordinates approximately 531311E and 5434636N (UTM ZONE 16 NAD 83).

The base station magnetometer recorded the diurnal variations of the earth's magnetic field

each day. The base station clock was synchronized with that of the mobile ground

magnetometer to permit subsequent removal of diurnal drift.

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7. SENSOR ORIENTATION

Optimal signal strength was achieved by orienting the base station and the portable sensor

along magnetic north. The Scintrex ENVI MAG proton magnetometers require that the

sensors be aligned along magnetic north for maximum field strength coupling during data

acquisition.

8. SIGN CONVENTION

All survey lines in the claim ran in an North South direction. A positive (North and East)

and negative (South and West) sign convention was adopted for all survey readings.

9. DIURNAL CORRECTIONS

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Diurnal variations caused by atmospheric effects such as ionospheric activity were accounted

for in the data each day by correcting the mobile data against base station data. Magnetic

corrections were part of daily QC/QA data checks.

10. FIELD WORKSTATION

A Intel P4 laptop was used onsite to verify data quality and completeness. Base stations and

mobile readings were transferred from the ENVI data consoles to a laptop and imported as

xyz's into a Geosoft Oasis Montaj database. The database enabled visual on screen display

of both positional and geophysical data for quality control purposes.

Lastly, the report was written by Mike Vumbaca B.Sc. and Pierre Simineau, geol. M.Sc.

The maps were drawn up by Pierre Simoneau.

11. PREVIOUS WORK

Only government geological surveys have been worked in the general area of the Killala Lake Property, namely:

1966 Coates, M.E. Killala-Vein Lakes area, District of Thunder Bay in Summary ofField Work, 1966 by the Geological Branch, E.G. Pye (Ed.); Ontario Department Mines, P.R 1966-1, November 1966, p. 23-25

1967 Coates, M.E. Killala-Vein Lakes area, District of Thunder Bay; Ontario Dept. Mines, Prelim Geol. Map P382, scale 1 inch: 1 mile.

1970 Coates, M.E. Geology of the Killala-Vein Lakes area, District of Thunder Bay; Ontario Department of Mines, Geological Report 81, 35 p.

12. REGIONAL GEOLOGY

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The bedrock is predominantly of Precambrian age and may be considered in five distinct groups: metavolcanics, migmitites, granitic rocks, mafic intrusive rocks, and alkalic rocks.

Aprroximately sixty percent of the entire area is underlain by granitic rocks which may represent three ages of intrusion.

Each of the previously mentioned rock types have been cut by diabase dikes of the porphyritic and non-porphyritic type.

The youngest rocks within the area are those of the Killala Lake Alkalic Complex, northeast of Killala Lake.

13. PROPERTY GEOLOGY

The property is situated west of Killala Lake, southwest of the Killala Alkalic Complex.

The geology id dominated by a northeast-southwest striking sequence of migmatites.

A considerable amount of mineral exploration has been done in the Killala Lake area and several small copper showings have been found. Some of the occurrences are found at the boundaries of diabase dikes while others are located along strike shears in the metavolcanics or migmatic rocks.

14. FIELD WORK AND PROCEDURE

The geophysical operator moved to the property and the grid was done from mid to late April 2007.

The lines were cut and gridded with a 25m long chain. Two separate grid were cut and bth extend in an N-S direction. The western grid extends E-W 8+00W to 5+00 W and from 0+00 to 5+00S with 100 meters between each line. The eastern grid extends E-W with N-S lines from 6+00E to 14+00E with 100 meters between each set of lines with chaining from 0+00 to 4+00N or 6+00N. A baseline intersects the grid at 0+00.

The magnetic survey covered the lines of the grid for a total of 6.5 km. Measurements were taken every 25 meters between stations.

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15. MAGNETIC SURVEY

15.1 PVRPOSE OF THE MAGNET]C SVRVEY AND METHODOLOGY

Magnetic surveys are useful in exploration as magnetic anomalies mostly represent changes in the physical properties of subsurface rocks. The property of a rock determines its magnetic effects and the intensity of its magnetization. During a survey, the total magnetic field is measured and a total field map is processed and produced that allows for the definition of both near-surface magnetic bodies.

The measurements for the magnetic total field were taken at a two (2) second sampling rate between a 25 m station to station spacing interval along ali lines.

15.2 PRESENTATION OF THE RESULTS

Geophysical data were processed and presented on maps using the computer software programs; Geosoft and MicroStation.

The magnetic results are presented on a profile map (no. 1) and a total field contour map (no. 2) at the metric scale of 1 : 2 500. The profiles appear as red lines at a vertical scale of 1000 gammas per centimetre, with a base value of 0 gammas.

15.3 RESULTS OF THE MAGNETIC SURVEY

The property magnetic background is around 57,700 gammas with a maximum of 59,243 gammas and a minimum of 57,154 gammas. The Magnetic colour contour map shows that the migmatite is magnetic since the northwest corner of the eastern grid where the migmatite is crossing shows high magnetic values (Mag-5). Under this assumption, one might also determine that the western grid is also underlain by migmatites (Mag-l and Mag-2) from the strong magnetic signature

16. DISCUSSION OF THE GEOPHYSICAL RESULTS

The geophysical survey covers five (5) magnetic horizons.

The survey arca is characterized by a series of three (3) high magnetic anomalies that may correspond to the migmatites horizons that are crossing the grid. Two magnetic anomalies CMag-2 and Mag-3) may follow dikes that could be carrying sulphides.

17. CONCLUSION and RECOMMENDATIONS

The Magnetic survey gives a good image of the geology and helps to discriminate numerous magnetic horizons.

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Prospecting and sampling will follow with an emphasis on the areas of higher magnetism.

A tighter station to station spacing of 10m or 12.5m rather than 25m would enhance the higher frequency and shallower wavelengths in the order of five (5) meters. A tighter, more detailed survey should be run in the future to enhance smaller scale anomalies, less than five (5) meters.

18. STATEMENT of COSTS

MobilisationiDemobilisation

Geophysical operator, 3 days @ $300

Mag rental, 3 days @ $150

Mag calibration

Report

SUBTOTAL G.S.T

TOTAL

$ 300.00

$ 900.00

$ 450.00

$ 105.00

$ 635.00

$ 2390.00 $ 143.40

$ 2533.00

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APPENDIX A

Claim Maps and Abstracts

Mining Claim Client Reports

THUNDER BAY Mining Division - 133247 - FOWLER, BRIAN DAVID

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CERTIFICATE of QUALIFICATIONS

I, Michael Vumbaca do hereby certify that:

1. I have graduated with a B.Sc. Degree in Geophysics from University of Toronto, Toronto, Ontario in 1994 and a diploma in Environmental Engineering (in progress, 2008) from Humber College Institute of Applied Technology.

2. I am a practicing consulting mineral and environmental geophysicist resident in Toronto, Ontario.

3. I have been actively consulting in the environmental and mineral exploration industry in and across Canada and internationalIy since 1995.

3. I am presently the owner and director of Mountain Valley Geophysics Corp. of 15 Hunting Ridge Drive, Toronto, Ontario.

4. I own no direct, indirect or expect to receive any contingent interests in the subject property or shares or securities from Mr. Brian Fowler.

5. The information contained in this report was obtained from the geophysical magnetic survey conducted on the Killala Lake property carried out by Michael Vumbaca and informations obtained from the Assessment files and from Brian Fowler.

6. I am a member in progress ofthe Professional Geoscientists of Ontario (P.Geo), a member of the Canadian Exploration Geophysics Society (KEGS) and Associated Environmental Assessors of Canada (ASAC).

7. I have disclosed in this report all relevant material which, to the best of my knowledge. might have a bearing on the viability of the project and the recommendations presented.

8. I consent to the use of this report by Mr. Brian Fowler for any Filing Statement, Statement of Material Facts, Prospectus, filing of assessment work of for any other reason deemed necessary by the company,

Dated at Toronto, this 21 st day of August, 20076. Respectfully submitted,

Michael Vumbaca, B.Se. Principal and Geophysicist 15 Hunting Ridge Drive Etobicoke, Ontario Canada M9R IB6