KLONDIKE GOLD CORP. Magnetometer, VLF EM, GPS and HLEM Surveys Over the. MATARROW MINE PROPERTY Yarrow Township, Ontario

Transcription

1 PO Box Government Road Larder Lake, Ontario PK L, Canada Phone () Fax () - KLONDIKE GOLD CORP. Magnetometer, VLF EM, GPS and HLEM Surveys Over the MATARROW MINE PROPERTY Yarrow Township, Ontario

2 TABLE OF CONTENTS. SURVEY DETAILS.... PROJECT NAME.... CLIENT.... LOCATION.... ACCESS.... SURVEY GRID.... SURVEY WORK UNDERTAKEN.... SURVEY LOG.... PERSONNEL.... SURVEY SPECIFICATIONS.... OVERVIEW OF SURVEY RESULTS.... SUMMARY INTERPRETATION... LIST OF TABLES AND FIGURES Figure : Location of the MATARROW MINE PROJECT... Figure : Yarrow Area Claim Map with Matarrow Mine Grid... Table : Survey Coverage... 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) August ii

3 . SURVEY DETAILS. PROJECT NAME This project is known as the MATARROW MINE PROJECT.. CLIENT. LOCATION KLONDIKE GOLD CORP. - West Hastings Street. Vancouver, British Columbia VB N The is located in the Yarrow Township within the Larder Lake Mining Division. This is approximately km southwest of Matachewan, Ontario and the grid covers claim L. Figure : Location of the MATARROW MINE PROJECT August

4 Figure : Yarrow Area Claim Map with Matarrow Mine Grid. ACCESS Access to the property was obtained via the Asbetos Mine Road which heads southwest from highway, three kilometers west of Matachewan, Ontario. The Matarrow Mine Grid crosses the road and can be located approximately km along the Asbestos Mine Road.. SURVEY GRID The grid consisted of. kilometers of grid lines. The grid lines are spaced meter increments with stations picketed at m intervals. The baseline ran at N for a total length of m. August

5 . SURVEY WORK UNDERTAKEN. SURVEY LOG Date Description Line # Min Max Total (m) April, Start Max Min survey. Extreme heat and rough terrain slows crew. E S N BL W E April, Continue Max Min survey. E.S N. E S N April, Continue Max Min survey. E S N E S N April, Continue Max Min survey. E S N E S N April, Complete Max Min survey. E S N E S N S W E Begin walkmag and VLF surveys. BL E E E S N E S N S E E E S April, Complete walkmag and VLF surveys. E S N E S N E S N E S N E S.N. E.N. S E E April, New line E cut. Return and read proper line with both max min, walkmag and VLF. E S N June, Begin Max Min survey on detail m lines. E S N E N N June, Continue Max Min survey. E S N E S N E S N E S N E S N June, Continue Max Min survey. E S N S E E N E E June, Conduct walkmag and VLF survey over detail lines. E.S N. E S N E S N E S N E S N E S N E S N E S N S E.E. N E E Table : Survey Coverage August

6 . PERSONNEL Mason Maki and Justin Lehti both of Kirkland Lake, Ontario, operated the MaxMin receiver and magnetometer with Yvan Veronneau of Gogama and Karl Zancanell of Larder Lake, Ontario, operating the MaxMin transmitter.. SURVEY SPECIFICATIONS The survey was conducted with an APEX PARAMETRICS MAXMIN II. Frequencies Hz, Hz, Hz, Hz and Hz were used with a m coil separation. A Suunto PM- clinometer was used to measure slopes between picketed stations. These slopes were averaged over m to determine the correct tilt readings. The magnetometer survey was conducted with a GSM v Overhauser magnetometer with a Scintrex Omni as a base station for diurnal corrections. The GPS survey was conducted with a Garmin with an external antenna for added accuracy. A total of. line kilometers of walkmag was read on April th to June th,. This consisted of magnetometer samples at one second sample intervals. A total of. line kilometers of VLF was read on April th to June th,. This consisted of VLF (NAA, NLK and NML) samples at.m sample intervals. A total of. line kilometers of GPS survey was read between May th and April th of. This consisted of samples at m sample intervals. A total of. line kilometers of HLEM) was read between April rd and June st of. This consisted of samples or.km at m intervals and samples or. at.m intervals. August

7 . OVERVIEW OF SURVEY RESULTS. SUMMARY INTERPRETATION An intense magnetic region occurs in the area of the baseline over the west portion of the grid. This region resulted in greater than % changes within the magnetic field over a period of one second. Intense EM conductors also appear coincident with this. These most likely represent an area of sulphides, such as pyrrhotite, pyrite or iron formation. Interestingly enough the EM response appears to extend beyond the magnetic region. This indicates a possible change in the composition of the sulphides. Another magnetic region appears offset and to the north west of this baseline anomaly. This has no coincident EM response yet mirrors, albeit weaker, the magnetic response of the primary anomaly. This may indicate a narrow band of mineralization. Another extremely (>% change in sec) strong magnetic area occurs in the region of tieline S. Again this does not have any EM response, yet the magnetics indicate a subtle change. These two areas should be examined with prospecting to identify the source of these magnetic regions. The region on S and to E should be near surface and easy to find with trenching and or prospecting. An additional EM response occurs near S across the property. This seems to be coincident with a low swampy area and may be a result of this. August

8 APPENDIX A STATEMENT OF QUALIFICATIONS I, C. Jason Ploeger, hereby declare that:. I am a geophysicist (non-professional) with residence in Larder Lake, Ontario and am presently employed as president of Larder Geophysics Ltd. of Larder Lake, Ontario.. I graduated with a Bachelor of Science degree in geophysics from the University of Western Ontario, in London Ontario, in.. I have practiced my profession continuously since graduation in Africa, Bulgaria, Canada, Mexico and Mongolia.. I am a member of the Ontario Prospectors Association.. I have an interest in some of the properties and securities of KLONDIKE GOLD CORP.. I am responsible for the final processing 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 July C. Jason Ploeger, B.Sc. (geophysics) President of Larder Geophysics Ltd. August

9 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 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- ports, for diurnal drift and other magnetic activity (ionospheric 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 (. to.m). 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. VLF Electromagnetic The frequency domain VLF electromagnetic survey is designed to measure both the vertical and horizontal inphase (IP) and Quadrature (OP) components of the anomalous field from electrically conductive zones. The sources for VLF EM surveys are several powerful radio transmitters located around the world which generate EM radiation in the low frequency band of -khz. The signals created by these long-range communications and navigational systems may be used for surveying up to several thousand kilometres away from the transmitter. The quality of the incoming VLF signal can be monitored using the field strength. A field strength above pt will produce excellent quality results. Anything lower indicates a weak signal strength, and possibly lower data quality. A very low signal strength (<pt) may indicate the radio station is down. The EM field is planar and horizontal at large distances from the EM source. The two components, electric (E) and magnetic (H), created by the source field are orthogonal to each other. E lies in a vertical plane while H lies at right angles to the direction of propagation in a horizontal plane. In order to ensure good coupling, the strike of possible conductors should lie in the direction of the transmitter to allow the H vector to pass through the anomaly, in turn, creating a secondary EM field. The VLF EM receiver has two orthogonal aerials which are tuned to the frequency of the transmitting station. The direction of the source station is locate by rotating the sensor around a vertical axis until a null position is found. The VLF EM survey procedure consists of taking measurements at stations along each line on the grid. The receiver is rotated about a horizontal axis, right angles to the traverse and the tilt recorded at the null position. August

10 HLEM Electromagnetic The HLEM method involves the use of a pair of separated horizontal coils (Figure MMI). Most commonly, the surveys are conducted in the frequency domain. In this method, a sine wave of variable frequency is sent through one of the coils to create a time-varying vertical magnetic dipole source. The second coil is a receiver which detects both the primary signal from the transmitting coil and a secondary signal created by magnetic induction in a conductive target in the earth. The HLEM method requires that a sample of the transmitted signal be sent along a wire to the receiver where it is used to synchronize the phase of the receiver with the transmitter. This permits the receiver to remove the effect of the transmitter signal (primary field) and to split the remaining secondary field into two components. One phase with the primary field (in-phase component). The second component is the portion of the secondary field which lags the primary field by one quarter cycle ( - quadrature component). The ratio of the in-phase to quadrature components is used to determine the electrical conductance of a target. MMI: HLEM source field HLEM instruments remove the primary filed from the signal to leave only the secondary field. By convention, a secondary field in the same direction as the primary field is recorded as positive while a secondary field in the opposite direction to the primary field is recorded as negative. HLEM data is commonly plotted as profiles with the reading plotted at the midpoint between the transmitter and receiver. The reason for this is that the response from a steeply dipping conductor, the most common target of this method, is strongest when the two coils straddle the conductor. August

11 APPENDIX C GSM Specifications Overhauser Performance Resolution:. nt Relative Sensitivity:. nt Absolute Accuracy:.nT Range:, to, nt Gradient Tolerance: Over,nT/m Operating Temperature: - C to + C Operation Modes Manual: Coordinates, time, date and reading stored automatically at min. second interval. Base Station: Time, date and reading stored at to second intervals. Walking Mag: Time, date and reading stored at coordinates of fiducial. Remote Control: Optional remote control using RS- interface. Input/Output: RS- or analog (optional) output using -pin weatherproof connector. Operating Parameters Power Consumption: Only Ws per reading. Operates continuously for hours on standby. Power Source: V.Ah sealed lead acid battery standard, other batteries available Operating Temperature: - C to + C Storage Capacity Manual Operation:, readings standard, with up to, optional. With VLF stations:, standard and up to, optional. Base Station:, readings standard, with up to, optional ( hours or days uninterrupted operation with sec. intervals) Gradiometer:, readings standard, with up to, optional. With VLF stations:,, with up to, optional. Omnidirectional VLF Performance Parameters: Resolution.% and range to ±% of total field. Frequency to khz. Measured Parameters: Vertical in-phase & out-of-phase, horizontal components, total field coordinates, date, and time. Features: Up to stations measured automatically, in-field data review, displays station field strength continuously, and tilt correction for up to ± tilts. Dimensions and Weights: x x mm and weighs only.kg. August

12 Dimensions and Weights Dimensions: Console: x x mm Sensor: x mm diameter cylinder Weight: Console:.kg Sensor and Staff Assembly:.kg Standard Components GSM 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 orderof magnitude greater sensitivity. These "supercharged" quantum magnetometers also deliver high absolute accuracy, rapid cycling (up to 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 frequencies 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 options into an instrumentation package that... exceeds proton precession and matches costlier optically pumped cesium capabilities. August

13 APPENDIX C ENVI GEOPHYSICAL SYSTEM SPECIFICATIONS Total Field Operating Range:, to, nt (gammas) Total Field Absolute Accuracy: ± nt Sensitivity:. nt at second sampling rate Tuning: Fully solid state. Manual or automatic, keyboard selectable Cycling (Reading) Rates:., or seconds Gradiometer Option: Includes a second sensor, /m ( inch) staff extender and processor module VLF Option: Includes a VLF sensor and harness assembly WALKMAG Mode: Continuous reading, cycling as fast as. seconds Digital Display: LCD Super Twist, x dots graphics, line x characters alphanumerics Display Heater: Thermostatically controlled, for cold weather operations Keyboard Input: keys, dual function, membrane type Notebook Function: characters, userdefined MACRO s for quick entry Standard Memory Total Field Measurements: Gradiometer Measurements: Base Station Measurements: VLF Measurements:, readings, readings, readings, readings for frequencies RealTime Clock Records full date, hours, minutes and seconds with second resolution, ± second stability over hours Digital Data Output RSC interface, to, Baud, or data bits, start, stop bit, no parity format. Selectable carriage return delay ( ms) to accommodate slow peripherals. Handshaking is done by Xon/Xoff. High speed Binary Dump. Selectable formats for easy interfacing to commercial software packages Power Supply Rechargeable Camcorder type,. Ah. Lead acid battery. Volts at. Amp for magnetometer,. Amp for gradiometer. External Volt input for base station operations. Optional external battery pouch for cold weather operations. Battery Charger: Operating Temperature Range: Dimensions & Weight Console: Magnetic Sensor: Gradiometer Sensor: Sensor Staff: VLF Sensor Head: VLF Sensor Electronics: Volt Volt, / Hz - to C mm x mm x mm ( x x. ). kg (. with rechargeable battery mm x mm (. d x ) kg (. lbs) mm x mm (. d x. ) (with staff extender). kg (. lbs) mm x m ( d x ). kg (. lbs) mm x mm (. d x. ). kg (. lbs) mm x mm x mm ( x. x ). kg (. lbs) August

14 APEX PARAMETRICS MAXMIN II Specifications Advanced spheric and powerline interference rejection results in faster and more accurate surveys, particularly at the larger coil separations. The Maxmin Computer or MMC is offered for digital data processing, display, storage and transfer. The MMC displays and stores the inphase and quadrature readings, their standard deviations, and the corresponding apparent ground conductivity values. Rough terrain surveys are also simplified with the MMC. Data interpretation and presentation programs are available for layered earth parametric soundings and discrete conductor surveys. Frequencies,,,, Hz Coil Separations,, meters (selected with grid switch in receiver) Modes of Operation MAX : Horizontal loop or slingram Transmitter and receiver coil planes horizontal and coplanar. MAX : Vertical coplanar loop mode Transmitter and receiver coil planes vertical and coplanar. MIN : Perpendicular mode Transmitter coil plane horizontal and receiver coil plane vertical. MIN : Perpendicular mode Transmitter coil plane vertical and receiver coil plane horizontal. Parameters Measured In-phase and quadrature components of the secondary magnetic field. Measures percent of primary field. Readouts Analog direct edgewise meter readouts for in-phase, quadrature and tilt. Additional digital LCD readouts provided in the optional MMC computer. Interfacing and controls are provided for ready plug-in of the MMC. Ranges of Readouts Switch activated analog in-phase and quadrature scales: ±%, ±% and ±%, and digital ±.% autorange with optional MMC Analog tilt ±% and ±% grade with MMC. Resolution Analog in-phase and quadrature. to % of primary field, depending on scale used, digital.% with August

15 autoranging MMC; tilt % grade. Repeatability. to % of primary field typical, depending on frequency, coil separation and conditions. Signal Filtering Powerline comb filter, continuous spheric noise clipping, auto adjusting time constant, and more. Warning Lights Receiver signal and reference warning lights to indicate potential error conditions. Survey Depth Penetration From surface down to. times coil separations for large horizontal targets, and. times coil separation for large vertical targets are typical values. Reference Cable: Lightweight unshielded / conductor teflon cables for maximum operating temperature range and for minimum pulling friction. Intercom Voice communication link provided for operators via the reference cable. Temperature Range: - to + degrees Celsius, operating range. Receiver Batteries Four standard V -. Ah alkaline batteries. Life: hours continuous duty, less in cold weather. Optional. Ah extended life lithium batteries available (recommended for very cold weather). Transmitter Batteries Standard rechargeable gel-type lead-acid V- Ah batteries ( x V -. Ah) in nylon belt pack. Optional rechargeable long life V- Ah Nicd batteries ( x.v - Ah) with Nicd chargers (best choice for cold climates). Transmitter BatteryChargers Lead acid battery Nicd battery charger with. V nominal output. Operation from and -VAC, -Hz, and VDC supply Receiver Weight Kg carrying weight (including the two ferrite cored antenna coils), Kg with MMC computer. Transmitter Weight Kg carrying weight Shipping Weight Kg plus weight of reference cables at.kg per meters, plus optional items if any Shipped in two aluminum-lined field I shipping cases. August

16 APPENDIX C GARMIN GPS GPS Performance Receiver: WAAS-enabled, parallel channel GPS receiver continuously tracks and uses up to satellites to compute and update your position Navigation Features Waypoints/icons: with name and graphic symbol, nearest (automatic), proximity Routes: reversible routes with up to points each, plus MOB and TracBack modes Tracks: Automatic track log; saved tracks let you retrace your path in both directions Trip computer: Current speed, average speed, resettable max. speed, trip timer and trip distance Alarms: Anchor drag, approach and arrival, off-course, proximity waypoint, shallow water and deep water Tables: Built-in celestial tables for best times to fish and hunt, sun and moon rise, set and location Map datums: More than plus user datum Position format: Lat/Lon, UTM/UPS, Maidenhead, MGRS, Loran TDs and other grids, including user grid Acquisition times Warm: Approximately seconds Cold: Approximately seconds AutoLocate : Approximately minutes Update rate: /second, continuous GPS accuracy Position: Velocity: WAAS accuracy Position: Velocity: < meters, % typical*. meter/sec steady state < meters, % typical*. meter/sec steady state Power Source: Battery Life: Two "AA" batteries (not included) Up to hours Physical Size: Weight:."W x."h x."d (. x. x. cm). ounces Display."W x."h (. x. cm) x pixels, high-contrast August

17 FSTN with bright backlighting Case: Interfaces: Antenna: Differential: Temperature range: Dynamics: User data storage: Fully gasketed, high-impact plastic alloy, waterproof to IEC IPX standards RS with NMEA, RTCM DGPS data format and proprietary Garmin Built-in quadrifilar, with external antenna connection (MCX) DGPS (USCG and WAAS capable) F to F ( C to C) g's Indefinite, no memory battery required Specifications obtained from August

18 APPENDIX D LIST OF MAPS (IN MAP POCKET) Posted contoured TFM plan map (:) ) #-KLONDIKE-MATARROW-MAG-CONT Posted profiled/fraser filtered contoured VLF plan maps (:) Posted profiled/ HLEM plan maps (:) ) #-KLONDIKE-MATARROW-VLF-NAA ) #-KLONDIKE-MATARROW-VLF-NLK ) #-KLONDIKE-MATARROW-VLF-NML ) #-KLONDIKE-MATARROW-MM ) #-KLONDIKE-MATARROW-MM ) #-KLONDIKE-MATARROW-MM ) #-KLONDIKE-MATARROW-MM ) #-KLONDIKE-MATARROW-MM TFM colored Fraser Filtered NAA plan map (:) ) #-KLONDIKE-MATARROW-MAG-AXIS TOTAL MAPS= August

19 (meters) NAD / UTM zone N Scale : MAX-MIN PROFILED PLAN MAP Hz - m Cable Seperation In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Calculated Elevation: Black Solid Vertical Profile Scales:. %/mm Vertical Quadrature Profile Scales:.%/mm Vertical Elevation Profile Scales: m/mm Station Seperation: meters Posting Level: APEX PARAMETRICS MAXMIN II KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario Drawing #-KLONDIKE_GOLD-MATTAROW-MAXMIN Reciever Operated By: Mason Maki Transmitter Operated By: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to June, LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE B B TS TS LN LN LS LS

20 (meters) NAD / UTM zone N Scale : MAX-MIN PROFILED PLAN MAP Hz - m Cable Seperation In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Calculated Elevation: Black Solid Vertical Profile Scales:.%/mm Vertical Quadrature Profile Scales:. %/mm Vertical Elevation Profile Scales: m/mm Station Seperation: meters Posting Level: APEX PARAMETRICS MAXMIN II KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario Drawing #-KLONDIKE_GOLD-MATTAROW-MAXMIN- Reciever Operated By: Mason Maki Transmitter Operated By: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to June, LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE B B TS TS LN LN LS LS

21 (meters) NAD / UTM zone N Scale : MAX-MIN PROFILED PLAN MAP Hz - m Cable Seperation In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Calculated Elevation: Black Solid Vertical Profile Scales:. %/mm Vertical Quadrature Profile Scales:. %/mm Vertical Elevation Profile Scales: m/mm Station Seperation: meters Posting Level: APEX PARAMETRICS MAXMIN II KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario Drawing #-KLONDIKE_GOLD-MATTAROW-MAXMIN- Reciever Operated By: Mason Maki Transmitter Operated By: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to June LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE B B TS TS LN LN LS LS

22 (meters) NAD / UTM zone N Scale : MAX-MIN PROFILED PLAN MAP Hz - m Cable Seperation In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Calculated Elevation: Black Solid Vertical Profile Scales: %/mm Vertical Quadrature Profile Scales: %/mm Vertical Elevation Profile Scales: m/mm Station Seperation: meters Posting Level: APEX PARAMETRICS MAXMIN II KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario Drawing #-KLONDIKE_GOLD-MATTAROW-MAXMIN- Reciever Operated By: Mason Maki Transmitter Operated By: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to June, LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE B B TS TS LN LN LS LS

23 LE LE LE LE Scale : (meters) NAD / UTM zone N LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LN LN B B LS LS TS TS TOTAL FIELD MAGNETIC nanotesla KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario TOTAL FIELD MAGNETIC CONTOURED PLAN MAP Base Station Corrected Posting Level: nt Field Inclination/Declination: degn/degw Station Seperation: Walkmag second interval Total Field Magnetic Contours: nt GSM OVERHAUSER MAGNETOMETER/VLF v Magnetometer Operated By: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to June, Drawing #-KLONDIKE-MATARROW-MAG-CONT

24 LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LN LN B B LS LS TS TS TOTAL FIELD MAGNETIC nanotesla VLF AXIS HLEM AXIS KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario TOTAL FIELD MAGNETIC COLORED PLAN MAP ELEVATION CONTOURED PLAN MAP INTERPRETED EM AXIS Elevation: Contoured at meters Magnetic Field Inclination/Declination: degn/degw Station Seperation:. to meters Scale : (meters) NAD / UTM zone N Elevation from GPS Measurements GSM OVERHAUSER MAGNETOMETER/VLF v Apex Parametrics Max-Min II Magnetometer Operated By: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to June, Drawing #-KLONDIKE-MATARROW-MAG-CONT

25 LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LN LN B B LS LS TS TS IP OP Fraser Filter Crossover Direction negative-positve KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario VLF IN PHASE/OUT PHASE PROFILE VLF FRASER FILTERED CONTOURED PLAN MAP.kHz NML - LaMOURE, NORTH DAKOTA, USA In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Vertical Profile Scales: %/mm Contour Interval:,,,,,,, Station Seperation:. meters Posting Level: Scale : (meters) NAD / UTM zone N GSM OVERHAUSER MAGNETOMETER/VLF v VLF Operator: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to, Drawing #-KLONDIKE-MATARROW-VLF-NML

26 LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LN LN B B LS LS TS TS IP OP Fraser Filter Crossover Direction negative-positve KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario VLF IN PHASE/OUT PHASE PROFILE VLF FRASER FILTERED CONTOURED PLAN MAP.kHz NLK - SEATTLE, USA In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Vertical Profile Scales: %/mm Contour Interval:,,,,,,, Station Seperation:. meters Posting Level: Scale : (meters) NAD / UTM zone N GSM OVERHAUSER MAGNETOMETER/VLF v VLF Operator: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to, Drawing #-KLONDIKE-MATARROW-VLF-NLK

27 LE LE LE LE LE LE LE LE LE LE LE LE - - LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LN LN B B LS LS TS TS IP OP Fraser Filter Crossover Direction negative-positve KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario VLF IN PHASE/OUT PHASE PROFILE VLF FRASER FILTERED CONTOURED PLAN MAP.kHz NAA - CUTLER USA Projection: NAD, Zone In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Vertical Profile Scales: %/mm Contour Interval:,,,,,,, Station Seperation:. meters Posting Level: Scale : (meters) NAD / UTM zone N GSM OVERHAUSER MAGNETOMETER/VLF v VLF Operator: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April, Drawing #-KLONDIKE-MATARROW-VLF-NAA

28 (meters) NAD / UTM zone N Scale : MAX-MIN PROFILED PLAN MAP Hz - m Cable Seperation In Phase: Posted Right/Bottom (Red) Out Phase: Posted Left/Top (Blue) Calculated Elevation: Black Solid Vertical Profile Scales:. %/mm Vertical Quadrature Profile Scales:. %/mm Vertical Elevation Profile Scales: m/mm Station Seperation: meters Posting Level: APEX PARAMETRICS MAXMIN II KLONDIKE GOLD CORP. MATARROW MINE Yarrow Township, Ontario Drawing #-KLONDIKE_GOLD-MATTAROW-MAXMIN- Reciever Operated By: Mason Maki Transmitter Operated By: Karl Zancanella Processed by: C Jason Ploeger, B.Sc. Map Drawn By: Micheline Desgagné April to June, LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE B B TS TS LN LN LS LS