WORK REPORT on the

BRISTOL TOWNSIDP PROPERTY PORCUPINE MINING DIVISION

for LIBERTY MINES

Submitted by: Steve Anderson 2041663 ONTARlO LTD. VISION EXPLORATION 637 Algonguin Blvd. E P.G. Box 1080 Timmins, Ontario P4N-7H9 Phone: 705-360-7722 Fax: 705-360-7733 E-mail: vision-x@ntl.sympatico.ca Website: www.duenorth.netlvision

May, 2005

1 2 2 2 3 3 4 5 5 6 6 7

1 2 3

A

1

Appendices

TABLE OF CONTENTS

Introduction Location and access Personnel Previous work General Geology Claims Work program summary Work program Magnetometer Results Recommendations and Conclusions Certificate

Location map Regional location map Grid and Claim Sketch

GSM-19 magnetometer

Posted and contoured magnetometer map

1 INTRODUCTION

The following report will deal with the results of a magnetometer survey carried out on Bristol Township Property. This property consists of two separate block mining claims (15 units) located in central portion of Bristol Townships, Porcupine Mining Division, Ontario (Figure #3). This work was carried out on a contract basis by Vision Exploration on behalf of Liberty Mines.

A total of approximately 12.7km of chain saw cut grid lines were established to cover a specific portion of the claim group. These lines were then covered with a magnetometer survey. This work was carried out on May 17 and 18,2005.

The purpose of this survey was to provide reconnaissance magnetic data that may aid in the geological interpretation of the area, specifically, any geophysical signatures that may indicate the contact shown to occur between the Mafic Volcanics and sediments. This area is of particular interest as it is situated approximately 5km Northeast of the Holmer Prospect currently being developed by Lakeshore Gold

This report will deal with the results of the magnetic survey carried out on the above­mentioned grid.

® Ontario

J

J J J LEGEND"

PHANFR0701C': MESOZOIC

CRETACEOUS

J Sedimentary rocks

PALEOZOIC

lllliVONIAN Sedimentary rocl<.s

J ORDOVICIAN

_ sedImentary rocks

J CAMBRIAN D Sedimentary rocks

PRECAMBRIAN C;iH/:;NVlU/:; I'HUVlNC/:;

J PROTEROZOIC NEe- TO MESOPROTEROZOfC

_ Migmatitic rocks and gneisses

_ Malle to ultramafic plutonic

J , .......

_ Felsic plutonic rocl<.s. derived gneisses and rrigmatiles

MetlMllCanic and metasedirntQary rocks

GEOLOGY AND PRINCIPAL MINERALS

OF ONTARIO

SUPERIOR AND SOUTHERN PROVINCES NI:O' TO MI:~OPROTr:RO£OIC.

_ Felsic Intrusive rocl<.s

CJ Malic infrusive rocks

_ Volcanic and sedimentary rocks

PALEOPROTEROZOIC _ MafIC intrusive rocks

_ :Se<imentary and metavolcanic

&UP&:RJOR PROVINe&:

ARCHEAN NEe- TO MESOARCHEAN _

MassIve 10 foliated OIlInodiolile to granite

--Foliated to gneiSSIC tonal~e to or$l~ilA

Metasedmentary rocks and derived gneisses

Metavolcanic and metasedimentary rocks

HUDSON

BAY

Major MInerai Deposits Past and Present

e Gokl

• Sliver ... Iron

" Copper·NicJlel

• Zinc·Copper

e Platmum·Paliadlum

+ Uranium

* Industrial MInerals

Seal. 1 : 8 000 000

~ 0 '-0 tOO ,w ?OO 1( ; lc.~"""lIf"" , 50 o 50 , . .

PROPERTY LOCATION

QueBEC

U.SA.

100 ,

LIBERTY MINES BRISTOL TWP. PROPERTY

LOCATION MAP FIGURE #1

150 Miles

2

LOCA nON AND ACCESS

The Bristol Township Property consists of two separate block-mining claims located in the central portion of Bristol Township. The property is situated approximately I3km Southeast of the city of Timmins (Figure #2).

Access to the work area was gained by taking Hwy 101 west from the city of Timmins for approximately 13km. Both claims lie just north of the Hwy and were accessed by foot (Figure #3).

survey.

PERSONNEL

The following people were directly involved in carrying out the total field magnetometer

Project Manager Geophysical Technician Geophysical Technician

Steve Anderson Glenn Okeefe Andre Belisle

PREVIOUS WORK

Timmins Timmins Timmins

This is the first phase of exploration to be conducted by Liberty Mines. This area is of particular interest as current work programs are currently being carried out in the immediate are by Tom Resources, Lakeshore Gold and Probe Mines. The focus of these programs tends to be focused on the contact between the mafic volcanics and sediments. Compilation maps of the areas show the current claim group to occupy approximately 1km of this contact.

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LIBERTY MINES BRISTOL TWP. PROPERTY REGIONAL LOCATION MAP

1:600,000 FIGURE #2

II

3 GENERAL GEOLOGY

The Bristol Township Property is shown by OGS Map # P3436 Timmins west - Bristol and Ogden Townships, Precambrian Geology, to be underlain primarily by Mafic to Intennediate Volcanics. This map also shows the southeast comer of Claim #3002710 to be underlain by sediments, and hosts approximately 1 km of the resulting geological contact.

CLAIMS

A total of 2 claims (15 units) were covered or partially covered by this work program. Both are located in Bristol Township, Porcupine Mining Division and are as follows.

3002710 3002711

Bristol Twp. Bristol Twp

, • '. • ... . .... .... r- .... .

)012021 I ',. ,

3016743 ' P85~1 ~ PB5:l '1 ' I

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3016558

LffiERTY MINES BRISTOL TOWNSHIP PROPERTY

CLAIM AND GRID SKETCH 1:20,000

FIGURE #3

General Information:

Survey Dates: Survey Period: Survey Days: Weather/down days: Survey Coverage:

Personnel:

Project Supervision:

WORK PROGRAM SUMMARY

May 17 and 18, 2005 2 day 2 day o days I2.7km Linecutting 12.7km ma!,rnetometer

Geophysical Technician: Steve Anderson Glenn Okeefe Andre Belisle Geophysical Technician

Survey Specifications:

Line Interval: Reading Interval: Parameter Surveyed: Diurnal Correction:

Instrument:

Magnetometer: Base Station:

Surveyed by:

200 meters 12.5 meters Earth's total magnetic field Base station, 30 seconds

GSM-19T Proton Precession Magnetometer GSM-19T Proton Precession Magnetometer

2041663 ONTARIO LTD. VISION EXPLORATION

637 Algonquin Blvd. E P.O. Box 1080

Timmins, Ontario P4N-IGI

Phone: 705-360-7722 Fax: 705-360-7733

E-Mai1: vision-x@ntLsympatico.ca Website: www.duenorth.netlvision

4

5 WORK PROGRAM

The work program involved establishing 12.6km of chainsaw cut grid lines over two separate claims. The grid specifications were set up to provide a base line at north 70 degrees east with perpendicular lines every 200m. This grid was then picketed usmg a 25m-station interval. The purpose of this program was to provide reconnaissance magnetometer data for the area that may help with the geological interpretation.

The following is a brief description of the geophysical methods and parameters used:

MAGNETOMETER THEORY

A GEM GSMT-19 Proton Precession magnetometer was used to carry out the magnetometer survey. The instrument is synchronised with a GEM GSMT-19 recording base station to help eliminate magnetic diurnal variation. This should ensure an accuracy ofless than 1.0 Nt.

The Proton Precession method involves energising a wire coil immersed in a hydrocarbon fluid. This causes the protons in the proton rich fluid to spin or precess simulating spinning magnetic dipoles. When the current is removed the protons precess about the direction of the earth's magnetic field, generating a signal in the same coil which is proportional to the total magnetic field intensity. In this way, the horizontal gradient of the earth's magnetic field can be measured and plotted in plan form with values of equal intensity joined to form a contour map.

This presentation is useful in correlating with other data sets to aid in structural interpretation. Individual magnetic responses can be mterpreted for dip, depth and width estimates after profiling the

data.

The following parameters were employed for the survey:

Instrument - GEM, GSMT -19 Proton Precession Magnetometer Reading Interval- 12.5m Line Interval - 200m Diurnal Correction Method - GEM GSMT-19 Recording Base Station Data Presentation Data posted and contoured plan map

- 1 :5000 scale - Contour interval = 50 nano-teslas

SuRVEY RESULTS

The magnetometer survey conducted on the subject property was successful in outlining a number of features that may be marking geological units.

The most dominant magnetic featured show up as highs, primarily on claim #3002710.

6

Although these appear to be one line anomalies the may be marking north-south striking diabase dikes in the area. Due to the large line separation it is difficult to determine an accurate strike direction for these features.

The magnetics located within the southeast comer of claim #3002710 tend be slIghtly lower and fairly flat. These may be markmg the sediments shovvn to occur within this ponion of the claim. The resulting geological contact is a favourable exploration target.

RECOMMENDA TIONS AND CONCLUSIONS

As described under the results, this work program outlines what would appear to be contact between the mafic volcanics and the sediments. Several, strong one line magnetic anomalies are likely the result of north-south striking diabase dikes.

To start with this data should be compiled with any historic geological of geophysical data that may be available. Additional work should take the form of fill-in lines, incorporating 100m line spacing. This would help in more accurately outlining the diabase dikes in the area.

As it appears as though a portion of the property covers the geological contact that is of interest, and induced polarization survey should also be considered. This method may respond to zones of disseminated sulphide that may not have been detected by the conventional magnetic and electromagnetic methods used thus far.

Due to this properties proximity to the Holmer Prospect any unexplained anomalous zones outlined by this or future programs should be further tested. If any remain unresolved they should be tested with diamond drilling.

CERTIFICATION

I, Steve Anderson of Timmins, Ontario hereby certify that:

1. I hold a three-year Geological Technologist Diploma from Sir Sandford College, Lindsay, and Ontario, obtained in May 1981.

2. I have been practising my professIOn since 1979 in Ontario, Quebec, Nova Scotia, New Brunswick, Newfoundland, NWT, Manitoba, Saskatchewan and Greenland.

3. I have been employed directly with Asamera Oil Inc. Urangellschaft Canada Ltd. Nanisivik Mines Ltd., R.S. Middleton Exploration Services Ltd., Rayan Exploration Ltd and I am currently co-owner of Vision Exploration.

4. I have based conclusions and recommendations contained in this report on knowledge of the area, my previous experience and on the results of the fieldwork conducted on the property dunng May 2005.

Dated this 20th day of May, 2005

AtTlmmm~

APPENDIX "A" GEM-GSM-19

GEM GSM-19

INSTRUMENT SPECIFICATIONS

MAGNETOMETER I GRAOIOMETER

Resolution:

~ Range: Gr.f.dient Tolerance:

. Opefating~ .

InputfOutput: Power Requirements:

Power Sauro=:

Operating Ranges:

Stotdge Temperature:

Display:

Dimensions:

VLF

0.01 nT Cgammal, magnetic field and gradient.

0.2 n T 0V'ef operating range.. 10,000 to 120,000 n1: :._~~.s:.~ .. ~

oVer 10(000 nT/m . _

: 3 seconds minimum, faster optional. Reading:; initiated from keyboard • ·~·tTi~ 'or ~ ~""ia RS-232-C.

6 ~.~ mnneonr.. RS-231C, and {optional} -analog output.

12 v,.~OO rnA peak (d~ring polarizationt 30 rnA Standby. 300mA peak in gfadiomet£r mode.. .

Intef{lal12 ~ ~.q .An sealed Jead..add battery standard, others op-. tiona!. An Exteinal12V powetsoorce can also be used.

Input 110 V~C: 60 Hz. OptiOOal ~10/220 VAC, SO{60 Hz.

Output: dwl level charging. Temperature! -40 -C to +6O-c.. Battery Voltage: ~ 0..0 V rriiiUmurn to 15V ~mum. Humidity: up to 90% rclafive, non condensing.. -500c to +E)5OC

La): 14-0:x: 64 pixels.. or 8 x30 characws.. Built in heater for opera­tion below -2Q<>C

Console: 223 x 69 x 24Omm.

-SenSor staff: :4._~4~O':'ll}-5eI;1ions.. Sensor. 170 ~ n mm d.ia..

.. ' ~ght: Console 2.1 kg. StmO.9kg.5ensors 1.1kg each.

Frequency Range: " 15 - 30.0 kHz. ParameI:eai Measured: VerticallCljJhase and Out-of-phaSe a:nnponents as perc:entage of total

field. .

Resotutkm: Number of Stations: Stnrage:

2 compOnents of hotiz.onta1 field. Absolute ampUtude of totll fieki. O.1~

Up 1D 3 ata time. . ~with: time. ~ magnetic fiek:VgraOtent,.sklpe, EM ~ frequency, in- and C?Ut-of.phase vertical, and both horizontal

. . componemsfur each ~stmon. Terrain Slope Range: ~ - 9(JO {entered mam..ta11}1. • Sensor Dinlensions: 14 x 15 X 9 an.. (5.5 X 6 x 3 ioches). Sensor Weieht: 1.0 b! (2.2 fh1. .

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