Geophysics Report on Monmouth and Cardiff Twps

Home , Monmouth

PO Box 219, 14579 Government Road, Larder Lake, Ontario, P0K 1L0, Canada Phone (705) 643-2345 Fax (705) 643-2191 www.explorationservices.ca

SKEAD HOLDINGS LTD.

Magnetometer Survey Over the

EMPIRE-B ZONE Cardiff-RE Property Monmouth and Cardiff Townships, Ontario

Magnetometer Survey SKEAD HOLDINGS LTD. Cardiff-RE Property Cardiff and Monmouth Townships, Ontario

TABLE OF CONTENTS

1. SURVEY DETAILS ...... 3 1.1 PROJECT NAME ...... 3 1.2 CLIENT ...... 3 1.3 LOCATION ...... 3 1.4 ACCESS ...... 4 1.5 SURVEY GRID ...... 4 2. SURVEY WORK UNDERTAKEN ...... 5 2.1 SURVEY LOG ...... 5 2.2 PERSONNEL ...... 5 2.3 SURVEY SPECIFICATIONS ...... 5 3. OVERVIEW OF SURVEY RESULTS ...... 6 3.1 SUMMARY INTERPRETATION ...... 6

LIST OF APPENDICES

APPENDIX A: STATEMENT OF QUALIFICATIONS APPENDIX B: THEORETICAL BASIS AND SURVEY PROCEDURES APPENDIX C: INSTRUMENT SPECIFICATIONS APPENDIX D: LIST OF MAPS (IN MAP POCKET)

LIST OF TABLES AND FIGURES

Figure 1: Location of Empire-B Zone within Cardiff RE Property ...... 3 Figure 2: Claim Map with Empire-B Traverses ...... 4 Figure 3: Magnetic Plan Map over Cardiff-RE Property ...... 6 Figure 4: Summary Interpretation ...... 7

Table 1: Survey Log ...... 5

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1. SURVEY DETAILS

1.1 PROJECT NAME This project is known as the Cardiff-RE Property – Empire-B Zone.

1.2 CLIENT SKEAD HOLDINGS LTD. 28 Ford St. Sault Ste. Marie, Ontario P6A 4N4

1.3 LOCATION The Empire-B Zone is located on the township boundary between Monmouth and Cardiff Townships with the traverse area covering a portion of mining claims 4217448 and 4211818, within the Southern Ontario Mining Division.

Figure 1: Location of Empire-B Zone within Cardiff RE Property

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Figure 2: Claim Map with Empire-B Traverses

1.4 ACCESS Access to the property was attained from Highway 121 approximately 19.3km west of its intersection with highway 28. From here, Legacy Road was used for the final ½ kilometer north to the property.

1.5 SURVEY GRID The traversed lines were established using a GPS in conjunction with the execution of the survey. The GPS operator would establish sample locations while remaining approximately 12.5m in front of the magnetometer operator. GPS waypoints and magnetic samples were taken every 12.5m along these controlled traverses. The GPS used was a Garmin GPSMAP 62s with an external antenna for added accuracy.

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2. SURVEY WORK UNDERTAKEN

2.1 SURVEY LOG Date Description Line Min Extent Max Extent Total Survey (m) April 30, 2012 Mobilize from Larder Lake to Bancroft.

May 1, 2012 Locate survey area, access and begin survey. 0 500S 62.5N 562.5 100E 500S 125N 625 200E 500S 0 500 300E 500S 0 500 400E 500S 0 500 500E 450S 0 450 600E 425S 0 425 0N 0 600E 600

May 2, 2012 Locate access on north end of survey area. Local claims road is private and chases crew from bush. Crew returns to south access and completes survey. 0 187.5N 400N 212.5 100E 225N 400N 175 200E 0 400N 400 300E 0 400N 400 400E 0 400N 400 500E 0 800N 800 600E 0 800N 800 700E 500S 325N 825 800E 500S 300N 800 900E 500S 150N 650 1000E 500S 0 500 0N 600E 1000E 400

May 3, 2012 Demobilize from Bancroft to Larder Lake. Table 1: Survey Log

2.2 PERSONNEL Tyler Potts of Larder Lake, Ontario conducted all the magnetic data collection with Mark Geddes also of Larder Lake responsible for the GPS control and GPS waypoint collection.

2.3 SURVEY SPECIFICATIONS The survey was conducted with a GSM-19 v7 Overhauser magnetometer with a second GSM-19 magnetometer for a base station mode for diurnal correction. A total of 10.525 line kilometers of no grid mag was performed between April 30th and May 3rd, 2012. This consisted of 842 magnetometer samples taken at 12.5m intervals.

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3. OVERVIEW OF SURVEY RESULTS

3.1 SUMMARY INTERPRETATION

Figure 3: Magnetic Plan Map over Cardiff-RE Property

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Over the survey area, some magnetic variance can be seen. It is most predominant in the northern regions with the strongest region located in the vicinity of the creek system north of the baseline.

Figure 4: Summary Interpretation

The magnetic survey indicates the presence of north-easterly trending linear features throughout the survey area. The strongest of these occur near the baseline region and have been labeled A. Com- paring the current magnetometer dataset to a historic spectrometer dataset indicates a relationship between the elevated magnetic regions and the elevated uranium and thorium ppm counts. This may indicate that there is a marked increase in the magnetic response of the pegmatic uranium ore zone. This allows for an additional survey to be performed in a reconnaissance mode to better isolate areas with better mineral potential. I would recommend further magnetic surveys over the property along with some additional work along these magnetic highs.

Magnetic unit B is a magnetically depressed region. Based on the geology maps, this magnetic unit most likely represents a syenite unit.

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Magnetic unit C dominates the southern part of the survey area. From field observations and comparison to the geology map, this magnetic unit most likely represents a gneiss. Through this appears magnetically elevated regions labeled D. These regions appear to be labeled as marble on the geology map; however, no evidence of this was seen in the field. I would recommend further magnetic and spectrometer surveys in the region. Both of these tools appear to successfully highlight regions of pegmatite. This in turn will leave to targets for further exploration.

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APPENDIX A

STATEMENT OF QUALIFICATIONS

I, C. Jason Ploeger, hereby declare that: 1. I am a geophysicist (non-professional) with residence in Larder Lake, Ontario and am presently em- ployed as Geophysical Manager of Canadian Exploration Services Ltd. of Larder Lake, Ontario.

2. I graduated with a Bachelor of Science degree in geophysics from the University of Western Ontario, in London Ontario, in 1999.

3. I have practiced my profession continuously since graduation in Africa, Bulgaria, Canada, Mexico and Mongolia.

4. I am a member of the Ontario Prospectors Association, a Director of the Northern Prospectors Associa- tion and a member of the Society of Exploration Geophysicists.

5. I have no interest, nor do I expect to receive any interest in the properties or securities of Skead Hold- ings Ltd.

6. I am responsible for the final processing and validation of the survey results and the compilation of the presentation of this report. The statements made in this report represent my professional opinion based on my consideration of the information available to me at the time of writing this report.

Larder Lake, ON May 2012

C. Jason Ploeger, B.Sc. (geophysics) Geophysical Manager Canadian Exploration Services Ltd.

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APPENDIX B

THEORETICAL BASIS AND SURVEY PROCEDURES

TOTAL FIELD MAGNETIC SURVEY Base station corrected Total Field Magnetic surveying is conducted using at least two synchronized magnetometers of identical type. One magnetometer unit is set in a fixed position in a region of stable geomagnetic gradient, and away from possible cultural effects (i.e. moving vehicles) to monitor and correct for daily diurnal drift. This magnetometer, given the term ‘base station’, stores the time, date and total field measurement at fixed time intervals over the survey day. The second, remote mobile unit stores the coordinates, time, date, and the total field measurements simultaneously. The procedure consists of taking total magnetic measurements of the Earth’s field at stations, along individual profiles, including Tie and Base lines. A 2 meter staff is used to mount the sensor, in order to optimally minimize localized near-surface geologic noise. At the end of a survey day, the mobile and base-station units are linked, via RS-232 ports, for diurnal drift and other magnetic activity (iono- spheric and sferic) corrections using internal software. For the gradiometer application, two identical sensors are mounted vertically at the ends of a rigid fiberglass tube. The centers of the coils are spaced a fixed distance apart (0.5 to 1.0m). The two coils are then read simultaneously, which alleviates the need to correct the gradient readings for diurnal variations, to measure the gradient of the total magnetic field.

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APPENDIX C

GSM 19

Specifications Overhauser Performance Resolution: 0.01 nT Relative Sensitivity: 0.02 nT Absolute Accuracy: 0.2nT Range: 20,000 to 120,000 nT Gradient Tolerance: Over 10,000nT/m Operating Temperature: -40°C to +60°C Operation Modes Manual: Coordinates, time, date and reading stored automatically at min. 3 second interval. Base Station: Time, date and reading stored at 3 to 60 second intervals. Walking Mag: Time, date and reading stored at coordinates of fiducial. Remote Control: Optional remote control using RS-232 interface. Input/Output: RS-232 or analog (optional) output using 6-pin weatherproof connector. Operating Parameters Power Consumption: Only 2Ws per reading. Operates continuously for 45 hours on standby. Power Source: 12V 2.6Ah sealed lead acid battery standard, other batteries available Operating Temperature: -50°C to +60°C Storage Capacity Manual Operation: 29,000 readings standard, with up to 116,000 optional. With 3 VLF stations: 12,000 standard and up to 48,000 optional. Base Station: 105,000 readings standard, with up to 419,000 optional (88 hours or 14 days uninterrupt- ed operation with 3 sec. intervals) Gradiometer: 25,000 readings standard, with up to 100,000 optional. With 3 VLF stations: 12,000, with up to 45,000 optional. Omnidirectional VLF Performance Parameters: Resolution 0.5% and range to ±200% of total field. Frequency 15 to 30 kHz. Measured Parameters: Vertical in-phase & out-of-phase, 2 horizontal components, total field coordinates, date, and time. Features: Up to 3 stations measured automatically, in-field data review, displays station field strength continuously, and tilt correction for up to ±10° tilts. Dimensions and Weights: 93 x 143 x 150mm and weighs only 1.0kg. Dimensions and Weights Dimensions: Console: 223 x 69 x 240mm Sensor: 170 x 71mm diameter cylinder Weight:

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Console: 2.1kg Sensor and Staff Assembly: 2.0kg Standard Components GSM-19 magnetometer console, harness, battery charger, shipping case, sensor with cable, staff, instruction manual, data transfer cable and software.

Taking Advantage of a “Quirk” of Physics Overhauser effect magnetometers are essentially proton precession devices except that they produce an order- of magnitude greater sensitivity. These "supercharged" quantum magnetometers also deliver high absolute accuracy, rapid cycling (up to 5 readings / second), and exceptionally low power consumption. The Overhauser effect occurs when a special liquid (with unpaired electrons) is combined with hydrogen atoms and then exposed to secondary polarization from a radio frequency (RF) magnetic field. The unpaired electrons transfer their stronger polarization to hydrogen atoms, thereby generating a strong precession signal-- that is ideal for very high-sensitivity total field measurement. In comparison with proton precession methods, RF signal generation also keeps power consumption to an absolute minimum and reduces noise (i.e. generating RF fre- quencies are well out of the bandwidth of the precession signal). In addition, polarization and signal measurement can occur simultaneously - which enables faster, sequential measurements. This, in turn, facilitates advanced statistical averaging over the sampling period and/or increased cycling rates (i.e. sampling speeds).

• The unique Overhauser unit blends physics, data quality, operational efficiency, system design and op- tions into an instrumentation package that ... exceeds proton precession and matches costlier optically pumped cesium capabilities

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APPENDIX C

GARMIN GPS MAP 62S

Physical & Performance: Unit dimensions, WxHxD: 2.4" x 6.3" x 1.4" (6.1 x 16.0 x 3.6 cm)

Display size, WxH: 1.43" x 2.15" (3.6 x 5.5 cm); 2.6" diag (6.6 cm)

Display resolution, WxH: 160 x 240 pixels

Display type: transflective, 65-K color TFT

Weight: 9.2 oz (260.1 g) with batteries

Battery: 2 AA batteries (not included); NiMH or Lithium recommended

Battery life: 20 hours

Waterproof: yes (IPX7)

Floats: no

High-sensitivity receiver: yes

Interface: high-speed USB and NMEA 0183 compatible

Maps & Memory: Basemap: yes

Preloaded maps: no

Ability to add maps: yes

Built-in memory: 1.7 GB

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Accepts data cards: microSD™ card (not included)

Waypoints/favorites/locations: 2000

Routes: 200

Track log: 10,000 points, 200 saved tracks

Features & Benefits: Automatic routing (turn by turn routing on roads): yes (with optional mapping for detailed roads)

Electronic compass: yes (tilt-compensated, 3-axis)

Touchscreen: no

Barometric altimeter: yes

Camera: no

Geocaching-friendly: yes (paperless)

Custom maps compatible: yes

Photo navigation (navigate to geotagged photos): yes

Outdoor GPS games: no

Hunt/fish calendar: yes

Sun and moon information: yes

Tide tables: yes

Area calculation: yes

Custom POIs (ability to add additional points of interest): yes

Unit-to-unit transfer (shares data wirelessly with similar yes units):

Picture viewer: yes

Garmin Connect™ compatible (online community where yes you analyze, categorize and share data):

• Specifications obtained from www.garmin.com

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APPENDIX D

LIST OF MAPS (IN MAP POCKET)

Posted profiled TFM plan map (1:2500)

1) SKEAD-CARDIFF RE-EMPIRE-MAG-CONT

Grid Sketch on Claim Map (1:20000)

2) SKEAD-CARDIFF RE-EMPIRE-GRID

TOTAL MAPS=2

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40 47 50 07 SKEAD HOLDINGS LTD. 0

- 5464 5 4 5 2

9 5529

8 3 0

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458 46 0 50 L 5 5 4 5 -

300

4 6 3

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0 7 5 7 EMPIRE B ZONE 40 59 8

5 0 1

546 E 0 0 5459 CARDIFF RE PROPERTY 0 681 464 54 5 0 Monmouth and Cardiff Townships, Ontario -50 L 7 2 455 0 5 0 0 0 E 4 5 4 423 5 5

4 4986000 TOTAL FIELD MAGNETIC CONTOURED PLAN MAP L 0 0 0 0 0 435 0 8 0 0 0 5 4 7 6 5 0 Base Station Corrected E 4 0 L 5 4 4 5 -5 815 5 1 547 0 0 Posting Level: 0nT 7 E

4986000 2 546 Field Inclination/Declination: 74degN/12degW -500 L 0 Station Seperation: 12.5 meter E Total Field Magnetic Contours: 100nT 721000 721250 721500 721750 722000 GSM-19 OVERHAUSER MAGNETOMETER/VLF v7

Scale 1:2500 Magnetometer Operated By: Tyler Potts 50 0 50 100 150 GPS Operated By: Mark Geddes Processed By: Claudia Moraga (meters) Map Drawn By: C Jason Ploeger NAD83 / UTM zone 17N May 2012

Drawing: SKEAD-CARDIFF RE-EMPIRE-MAG-CONT L L 6 5 0 0 0 0 E E

L L L 9 7 8 0 L4 0 0 L 0 0 0 E L 3 0 E E L 2 0 0E L100 1 0 0 0 0 E L 0 E 0 E 0 E E L0N

N L1000 L0 L 40 L 0 L L 9 E 6 L 8 0 E L 0 7 0 0 5 0 0 0 E 0 E 0 E L 0 E L 300 E L 2 L 1 0 0 0 0 E E 0 E E