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BERLAND RESOURCES LTD.
SWOLE LAKE PROPERTY
ONTARIO
NTS 42L/5
2 .22389
GEOPHYSICAL REPORT
SUBMITTED BY:
WILLIAM MCCRINDLE, P. ENG.
November, 2001
42L05NW2007 2.22389 JUNIOR LAKE 010
CF ASSESSMENTf— ———— f
TABLE OF CONTENTS
INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3
LOCATION AND ACCESSIBILITY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3
PROPERTY DESCRIPTION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3
CLAIM LIST: . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3
HISTORY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4
GEOLOGICAL SETTING . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4
DEPOSIT TYPES . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4
FIELD METHODS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4
FIELD PERSONNEL . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
DISCUSSION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
RECOMMENDATION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5
CERTIFICATE OF QUALIFIED PERSON . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6
Appendix I Logistic Report
Map Pocket 6 figures at a scale of l :5,000
-2-
INTRODUCTIONIn September of 2001, Berland Resources Ltd. signed a letter agreement with Ninety Nine Resources Ltd. of Thunder Bay, Ontario to option the 7 claim property with nickel, copper and platinum group element potential. Berland can earn a 10007o interest subject to certain net smelter royalties by making cash and share payments over three years.
The property consists of 7 unpatented mining claims, 91 units and covers 3,640 acres in three separate blocks located in the Junior lake (G-57) and Falcon Lake (G-35) claim map areas of the Thunder Bay mining Division. All work described in this report was conducted on the east block of 5 claims and specifically on claiml238090.
In September of 2001, Berland contracted Voyageure Exploration Service of Thunder Bay, Ontario to cut a baseline and grid totaling 9.5 km. This work was completed on September 26, 2001. Mtec Geophysics Inc. of Thunder Bay was contracted by Berland Resources Ltd. to conduct ground magnetic and HLEM surveys on the cut grid. The logistics and results are reported in the appended report by Mtec. Mr. W. Mccrindle of Berland planned, supervised the field program and submits this report.
LOCATION AND ACCESSIBILITYThe property is located approximately 30 kilometers east and north of Lake Nipigon, north of Toronto Lake in the Junior Lake claim map area. The property is accessible by an all weather gravel road running east from Armstrong for 100 km. From the end of a secondary logging road, the Swole Lake grid and showings are accessed by a 300 meter trail and short boat ride across Swole Lake
PROPERTY DESCRIPTIONThe property is comprised of 7 unpatented mining claims, 91 units, covering 3,640 acres in three separate claim blocks, (see figure 2) The claims are listed in table #1. Each claim block was staked to cover a geologically significant mafic-ultramafic intrusion. The central core of the east block is covered by mature spruce and poplar. Swole Lake and its marginal bog cover the east portion of the block. Outcrop is sparse throughout the property but the overburden is thin over the central upland area.
PROPERTY LOCATION MAPIncluded in Logistics Report in appendix I
CLAIM MAPIncluded in Logistics Report in appendix I
CLAIM LIST - table #1
Claim Number
1238090
1239892
Township
Junior Lake
Junior Lake
Number of Units
16
16
Recorded Date
September?, 1999
November 18, 1999
Expiry Date
September 7, 2002
November 18,2001
Berland Ownership
iooo7o, NSR'S
10007o, NSR 's
-3-
1239893
1239897
1239898
1220824
1239925
Junior Lake
Junior Lake
Junior Lake
Falcon Lake
Falcon Lake
16
12
4
12
16
November 18, 1999
December 13, 1999
December 13, 1999
February 1 7, 2000
December 5, 2000
November 18,2001
December 13,2001
December 13,2001
February 17,2002
December 5, 2002
10007o, NSR'S
1000Xo, NSR's
10007o, NSR's
lOOVo, NSR's
100"Xo-2"7oNSR
Total 7 claims, 91 units, 3,640 acres.
HISTORYProspectors found very old blasted pits near the new showings. No record of these pits was found in the assessment files.
In 1983, Kerr Addison Mines filed work on reconnaissance exploration in the Summit Lake area consisting of geological mapping and soil sampling. The northwest corner of the survey area overlaps the southern claim of Berland's east block.
Initial prospecting by Inco Ltd. and Ninety Nine Resources Ltd. in 1999 revealed anomalous values in nickel, copper and PGE elements from the eastern Swole Lake block. Results were subsequently filed for assessment.
OGS report #55 and accompanying map - Crescent Lake Geology map # 2100 by E.G. Pye, 1968 describes the geology of the claims.
1989 airborne electromagnetic and total intensity magnetic geophysical survey of the Tashota- Geraldton-Longlac Area flown for the Ontario Geological Survey at a scale of l :20,000 covers the area.
GEOLOGICAL SETTINGEach claim block covers a mafic to ultra-mafic intrusion situated within a sedimentary and volcanic sequence of rocks of archean age. Each block hosts sulphide mineralization containing anomalous values in nickel, copper and PGE's or untested airborne geophysical electromagnetic anomalies detected by the recent OGS airborne geophysical survey.
DEPOSIT TYPESThe primary focus of the exploration is to locate a gabbroic intrusive bearing a nickel copper, and platinum group element (PGE) deposit and/or a layered gabbro with reef type mineralized layers.
FIELD METHODSSee the Logistical Report in appendix I
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FIELD PERSONNELSummary of field work days
Voyageure Eplorations Ltd. September 15 to 26, 2001- Scott Mortson + partner
Mtec Geophysics Inc. September 26 and 27, 2001- Cal Debman, Matt Lambert
DISCUSSION HLEM ResultsThe HLEM survey, which was conducted by MTEC Geophysics Inc., detected a single weak anomaly which'extends from L99+00-N to L92+00-N, a distance of 700 meters. This anomaly is extremely weak, detectable by the 1760 and the 3520 Hz frequencies and not the lower frequency 440 Hz. The HLEM anomaly coincides with low elevation muskeg swamp and is open-ended to the north under Swole Lake. The weak signature of the anomaly is likely caused by weakly conductive overburden. A more detailed interpretation of the cause of the source of the anomaly should be investigated by a qualified geophysists.
Magnetometer Survey ResultsA base datum of 57,000 nT was utilized and the resulting posting contoured using a 100, 500 and 2000 nT contour interval. The most obvious feature is a magnetic high centered on L97+00-N at 100+00-E and trending grid northeast to the shore of Swole Lake. This magnetic feature can be attributed to the moderate to strong magnetism associated with the hornblendite phase of the Swole Lake intrusion. The magnetic high is flanked to the west by a magnetic low and matched the inferred contact area between the Swole Lake intrusions and the flanking metasediments. More detailed contouring would be required for structure and lithological interpretation.
RECOMMENDATIONA geological mapping survey to be conducted simultaneously with prospecting the grid is recommended.
Respectively Submitted by,
BERLAND RESOURCES LTD.
William McCrindle, P. Eng.
-5-
CERTIFICATE OF QUALIFIED PERSON
I, William McCrindle, P. Eng., of the City of Thunder Bay, do hereby certify that:
1. I planned and supervised the contractors on behalf of Berland Resources Ltd.
2. I am the President, a Director and shareholder of Berland Resources Ltd.
3. I hold a Bachelor of Applied Science degree in Geological Engineering from the University of Toronto (l 961).
4. I am registered as a member of the Association of Professional Engineers of Ontario and have been since July 27th , 1984.
5. I worked as a geologist in education and as a consultant from 1961 to 1982. From 1983 to October 1997, I was an Officer and from 1983 to the present, a Director of Cumberland Resources Ltd. I retired from my involvement in education in February, 1995. In October 1997,1 was appointed President and Director of Berland Resources Ltd.
Dated at Thunder Bay, Ontario
this 4th day of November, 2001
William McCrindle, P. Eng.
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LOGISTICAL REPORT
Swole Lake PropertyFor
Berland Resources Ltd.
by Mike Milani
Mtec Geophysics Inc
October, 2001
42L05NW2007 2.22389 JUNIOR LAKE 020
TABLE OF CONTENTS
1.0 Introduction.............................................................. 12.0 Location and Accessibility............................................ 13.0 Property Description.................................................. 14.0 Survey Procedures.................................................... 5
4.0.1 SurveyDescription................................ 54.0.2 Data Processing and Presentation............ 5
5.0 Personnel................................................................ 66.0 Summary................................................................. 6
FiguresFigure 1 Location Map Swole Lake Property 2
Claim Map Swole Lake Property 3
Attachments Appendix 1
Specifications Gem Systems GSM19 7Appendix 2
Specifications Maxmin l Electromagnetic 10 System-Apex Parametrics Limited
MapsTotal Field Posted Data Scale 1:5000 Total Field Contoured Data Scale 1:5000 Total Field Profiled Data Scale 1:5000 HLEM Survey - 440 Hz Scale 1:5000 HLEM Survey - 1760 Hz Scale 1:5000 HLEM Survey - 3520 Hz Scale 1:5000
1.0 Introduction
In September of 2001, Berland Resources Ltd. signed a letter agreement with Ninety Nine Resources Ltd. of Thunder Bay, Ontario to option the 7 claim Swole Lake property with nickel, copper and platinum group element potential. Berland can earn a 100*56 interest subject to certain net smelter royalties by making cash and share payments over three years.
The property consists of 7 unpatented mining claims, 91 units and covers 3,640 acres in three separate blocks located in the Junior lake (G-57) and Falcon Lake (G-35) claim map areas of the Thunder Bay Mining Division. Work described in this report was conducted on the east block of 5 claims and primarily on claiml 238090.
Mtec Geophysics Inc. was contracted to undertake ground magnetic and HLEM surveys for Berland Resources Ltd. Field work was carried out between September 26, 2001 and September 27, 2001.
2.0 Location and Accessibilty
The property is located approximately 30 kilometers east and north of Lake Nipigon, north of Toronto Lake in the Junior Lake claim map area. The property is accessible by an all weather gravel road running east from Armstrong for 100 km. The Swole Lake grid and showings are accessed by a 300 meter trail and short boat ride across Swole Lake from the end of a secondary logging road.
3.0 Property Description
The property is comprised of 7 unpatented mining claims, 91 units, covering 3,640 acres in three separate claim blocks, (see figure 2) The claims are listed in table #1. Each claim block was staked to cover a geologically significant mafic- ultramafic intrusion. The central core of the east block is covered by mature spruce and poplar. Swole Lake and its marginal bog cover the east portion of the block. Outcrop is sparse throughout the property but the overburden is thin.
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Swole Lake Property
BERLAND RESOURCES LTD.Figure 1
Property Location Map Thunder Bay Mining Division, Ontario
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42QQQQmE 43QQQO mE
FalconLake
Tape Lake
OS8SS
North Lamauns Lake
Swole Lake
2.5
kilometers
Claim MapSwole Lake PropertyFigure 2
420000 mE 430000 mE
CLAIM LIST - table #1
Claim Number
1238090
1239892
1239893
1239897
1239898
1220824
1239925
Township
Junior LakeJunior LakeJunior LakeJunior LakeJunior Lake
Falcon Lake
Falcon Lake
Number of Units
16
16
16
12
4
12
16
Recorded Date
September 7, 1999November 18, 1999November 18, 1999December 13, 1999December 13, 1999
February 17, 2000
December 5, 2000
Expiry Date
September 7, 2002November 18, 2001November 18, 2001December 13, 2001December 13, 2001
February 17, 2002
December 5, 2002
Beriand Ownership10007o,
NSR's100^0, NSR's1000/*), NSR's10007o, NSR's100^0, NSR's
10007o , NSR's
10007o - 207o NSR
Total 7 claims, 91 units, 3,640 acres.
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4.0 Survey Procedures and Equipment
4.0.1 Survey Description
The magnetometer and HLEM surveys were conducted on the claims on cut-line grids. Magnetic surveys were carried out using a GEM Systems GSM-19 Overhauser magnetometer measuring variations in the total field at 12.5m intervals on the cross lines as well as the baseline of the grid, with a sensitivity of 0.01 nT. Readings were recorded digitally, as were the corresponding diurnal variations, which were monitored and recorded using a base station.
The HLEM survey employed a MaxMin l instrument with a coil separation of 150m, with measurements of the in-phase and quadrature values at 440, 1760 and 3520 Hz at 25m station intervals, with an intrinsic resolution of +/-1 Vo.
4.0.2 Data Processing and Presentation
The digitally recorded magnetic data were corrected for diurnal variations by subtracting the base station values. The resulting corrected data were gridded and contoured using Geosoft software. The posted magnetic data and the contoured data are presented on separate maps at a scale of 1:5000.
The HLEM data are presented in standard fashion as in-phase and quadrature profiles, with a profile scale of 1cm = 1007o for all frequencies. The results can be seen on separate maps for each frequency at a scale of 1:5000.
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5.0 Personnel
The following Mtec Geophysics Inc. personnel were employed on this project.
Max-Min l Survey, Magnetometer Survey:
Cal Debnam 642 Mud Lake Rd. Murillo, ON. (807) 935-3180
Matt Lambert North Branch Rd. Thunder Bay, ON.
Shawn Roberts 682 Strachan Ave. Thunder Bay, ON
6.0 Summary
The following chart details the grid that was surveyed.
CLAIMS/
GRID
Swole Lake
Totals
KM LINECUTTING
—
—.
KM MAG
9.3
9.3
KM HLEM
8.4 (150m coil separation)8.4
With the submittal of this report and the accompanying data diskettes the obligations of Mtec Geophysics Inc. have been fulfilled for the Swole Lake Property.
Oct., 2001 M. MilaniMtec Geophysics Inc.
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Appendix 1 (7)
M ACNETOMBTERS
GSM-19O VBRHA&SB& Magnetometer/
VLF System
GSM-19OVSKHAUSERSystem
Features
- Sensitivity — 0.02 nT
* Absolute Accuracy — 0.2 nT
- Sample Rates tip to S Hz
* Low Power Consumption
General"Ovcrhauscr" Once you experience it, you'll never go back to proton, Ovcrhauscr technology brings you sensitivities one to two orders of magnitude better than proton, yet in a light weight package. This is because tt consumes an order of magnitude less power than proton, allowing a lighter weight for batteries.
What is the Ovcrhauscr technique? The Ovcrhauscr sensor contains the electrons' fluid that has been added to a hydrogen rich m the form of* "free radial". The resulting mixture yields a sensor with 5000 tones gain hi proton polarization. Since the Ovcrhauscr polarization effect docs not require static magnetic fields, but uses radio frequency
bc done concurrently with polarization. The result is a sensor with much greater sensitiv ity, that can bc sampled much more rapidly than the standard proton sensor.
Ovcrhauscr systems therefore maximize resolution while minimizing power consump tion. Even with Walking (Gradiometer
systems, sampling at rates of once per second or bcttcrarc posiblc; Even in cokt tempera- hires of minus 40 zero degrees Celsius and greater, the internal rechargeable battery can still bc relied on for a 10 how day, or longer.
The GSM-19 Ovcrhauscr magnetometer is thus truly a Sluie-of-the-Art Magnetometer/ VLF system. The GSM-19 afters the data quality, reliability, and extensive list of* capabilities, and options, that allow it to meet a very wide spectrum of applications.
Standard FeaturesThe GSM-19 console features a real time graphic display of the current profile. In addition digital display of the current reading, current position, and warning messages arc provided. The console design, with internal rechargeable battery pack, allows the unit to bc completely scaled against the elements. With the built in heater for the display the OSM-19 is ready to go wherever your surveys may take you.
Tuning is automatic worldwide, with provision for manual override. In high gradient conditions the OSM-19 monitors the signal decay rate and displays a warning message when the gradient becomes too great Filters for rejection of 50 or 6O Hz noise arc provided.
Diurnal corrections may bc done m traditional fashion with one unit as a base station and a second unit used as the mobile field unit At die end of the survey the two itn its arc connected and the field unit creates a corrected data file (which stilt includes the
raw data file) based on the temporal drift recorded by the base station.
As a standard feature the GSM-19 also otters the capability of making tic point measure ments for automatic diurnal corrections. To use this feature the operator records a base value and then loops back to this point periodically dor-fang the survey to record another measurement, and thus build a file of the drift In this way a single instrument may bc used to make diurnal corrections.
The RS-232 port on the OSM-19 will output data as it is collected. This allows interface to OPS loggers that will accept RS232 data. The standard GSM-19 may bc operated hi a remote mode via computer. Memory storage is 512 K m the standard unit, and may bc upgraded to 2 MB
Grid coordinates arc stored with cither numeric or compass designations. A seven digit number may bc used to designate lines and positions. Line and position spacing is entered so that with every reading the position may bc automatically updated. An End of Ltnc feature allows the next line to be quickly selected, phis changes die sign on the position spacing. If die previous line had been adding positions as the operator moved, then on the next line, positions wilt bc subtracted as the operator moves. The operator may also easily manually enter his grid position for cases where gaps in the line arc necessary.
Terraplus Inc.52 Vfcrt Beror O. Rd. #17, Richmond Hill, ON. Canx). L4B IL9
Tel: 905-764-5505 Fax:905-764-8093
Email: [email protected] j Vifebsite: www.tenaiJus.com^^^^^^)
M AGNETQMBTERS
Equatorial SensorIn equatorial regions, generally 30 degrees north or south of the equator, magnetic fields reach a nearly horizontal angle with the earth's surface. This requires a conventional proton sensor to bc used in an inverted position, and requires the operator to collect data only on cast/west lines to maximize the magnetic signal. This is a problem that is a magnitude worse for cesium magnetometers.The OvcrhottscT technique allows design of an optional sensor completely free of this problem, a sensor that requires no orientation no matter what the latitude of your explora tion. This can bc a major advantage when working in diverse areas around the world, and when needing to train local operators whooc fin* language may not bc your own.
"Walking Mag Optra*"
The OSM-19 magnetometer was the fust to offer the "Walking Mag" concept The reason fer this is die outstanding advantage die Ovcrhauscr sensor nan in dais application. With the "Walking Mag" option the operator may select a sample rate of up to two samples per second. At this rate Ovcrhauscr technol ogy can still dclh/cr a noise kvcl that is quite acceptable, about O. I nT, and the tower power consumption means that a full day of surveying can still bc done with just the internal recharges bk battery.As shown in Figure l the near continuous data from the "Walking Mag" technique provides increased definition for any type of survey. For surveys with densely spaced grids, such as archaeological or environmental surveys, field productivity is markedly improved, typically by a factor of five.When in the Walking Mag mode die operator still presets his line and station spacing. When a known station is passed a grid update key is pressed and the current reading is tagged with this station. Readings taken between these marked positions arc then linearly interpolated for their grid position when data is transferred to a computerA farther refinement of die Walking Mag concept is the Hip Chain Option. This option uses a hip chain to trigger the magnetometer to take a reading at discrete intervals. A ffy Chain consists of an optical encoder that records revolutions of a wheel wound with
Near*C onthuoueSuiveyB In pmve Defhidbn of H agnetfc A nora a JBS
J 6" Ja eiooo -j —JE. un
7S 100
disposable cotton string. The string is tied off at the beginning of a line, and as the operator walks the string is pulled out, and the magnetometer is automatically triggered. With the Hip Chain option sample rates up to five samples per second arc supported.
Oawftdircetioaal VUFThe GSM-19 VLF features a throe coil design, with new larger coils in 1997, to achieve a non orientation capability with excellent sensitivity Up to three VLF stations may bc recorded* along with the magnetic reading, with the pressing of a single key.As each VLF station is read the total field strength is displayed. This value may bc used to determine if a station's signal is strong enough to obtain useful data. At the end of each reading me m phase, out of phase, and horizontal components arc displayed and recorded for each station.To determine what stations arc available the Scan feature may bc used. The entire VLF spectrum is seamed and stations with their corresponding signal strength arc displayed Automatic tilt compensation is provided up to ten degrees. Beyond mis a warning message appears with display/ of the amount of tilt m each direction, enabling the operator to correct his position and take the reading again.For Walking Mag applications a Walking VLF option is also available. With this option a single VLF station may bc measured at sampling rates up to once per second. In this mode both magnetic and VLF readings may
I7S 200
bc collected at the one hertz rate.
Simultaneous GradtomctcrMany mining, environmental, and archaeo logical applications may benefit from using the gradient measurement. For near surface anomalies, generally twenty meters depth or less, the gradient anomaly will bc larger, and narrower, than the total field anomaly. This permits the more accurate location of the target, and gives better sensitivity. The gradient measurement has the added value of being free from diurnal drift.The most accurate gradient measurements arc made when both sensors arc polarized and measured at precisely the same time. In this way any slight movement of the sensor staff pole will not affect the reading. With the OSM-19 Gradiometer Option the pressing of a single key will initiate measurement of both the total field and gradient. Both reading!; arc displayed and stored.
Integrated DGPSWith me OPS Log Option the QSM-19 will display and store OPS data using standard NMBA format Position accuracy is depen dant on the user's OOPS system.Also offered is an internally mounted OPS board mat may bc integrated with radio modem for DGPS mode. A range of OPS boards may bc offered to meet customer specified accuracy. These arc quoted on a case by case basis to take advantage of current technology. Complete systems, w ith base station, and DGPS software arc provided.
f Terraplus Inc.Li2 Went Beaver Cr. M. tin, Richmond Hill, ON. Cam du I/IB 11.9
Tel: 905-764-5505 Fax:905-764-8093
Email: [email protected] VVfebsdte: www.tenaphis.ccBH
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Extended Remote ControlAs an option the GSM-l9 may bc completely controlled through the RS232 interface. This option includes atl controls available from the keypad, such as power on/off, tuning, etc. This option is most useful for observatory applications.
Marine MagnetometersThe Ovcrhauscr effect is a major benefit in marine applications. The (5SM-19 has been developed into two marine models; the GSM- 19M for shallow tow applications with cable lengths of up to 100 meters; and the standard GSM-19 for tow applications with cable lengths ot'JOmctcra. Please ace pages ?? for the QSM-19M.A standard GSM-19 may be used with a marine sensor with up to a 30 meter cable. En this way the same console may bc used for both land and marine applications- Users considering this option may want to focus on also including the Walking Mag option so mat they will have sample rates that arc more appropriate for marine applications.
Ovcrhauscr Performance
Resolution: 0.01 nT Relative Sensitivity: 0.02 nT Absolute Accuracy: 0.2nT Range: 20,000 to 120,000 nT Gradient Tolerance: Over lO.OOOnT/m Operating Temperature: -40"C to *60"C
Operation ModesManual: Coordinates, time, date and reading stored automatically at min. 3 Mcond interval.
Base Station: Time, date aod reading stored it 3 to 60 second intervals.Walking Mag: Time, dale 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.
Opcratiag ParametersPower Consumption: Only 2Wj per reading. Operates continuously for 43 houn, on standby.
Power Source: 12V 2.6Ah sealed lead acid battery standard, other batteries available
Operating Temperature: -50"C to +60PC
Storage Capacity
Manual Operation: 29,000 readings standard. with up to 1 16,000 optional. With 3 VLF stmionv 1 2.000 standard and up to 48,000 optional.
Base Station: 105,000 readings standard, with up lo 419,000 optional (88 hours or 14 days uninterrupted operation with S tec. interval
Gradiometer 25.000 readings standard, with up to 100,000 optional. With 3 VLF station*: 12,000, with up to 45,000 optional.
Performance Parameters: Resohition O.SH and range to -*-20(W*i of total field Frequency 15 lo 30 kHz.
Measured Parameters: Vertical in-phase A otrt- of-phase, 2 hocizontftl component^ total field coonHnatefi, date, and time
Features: Up to 3 station!; measured auromaticaljy, in-field data review, display* station field strength cojitinDonsry, and tilt correction for up to -HO0 tilts.Dimensions and Weights: 93 v 143 x tSOmm and weighs only l .Okg.
MAGNETOMETERS
Dimension and WeightsDimensions:Console: 223 x 691 240mm
Sensor 170* 71mm diameter cylinder
Wflgkl:
Consolc: 2. Ikg
Sensor and Staff Assembly: 2.0kg
Standard ComponentsQSM-19 console, harness, battery chaffer, shipping case, xentor with cable, Klaft, ijutiuctioA manual, data transfer cable and software.
Ordex±ng informationDescription Order Number
350-170-0051 3SO-BO-OOJ2
Memory qpgrate per St2 . . . . 350-170-0065 . . . 39B-IJD-OHD . . . 3ED-BD-OM3
. . 350-170-0073OEM-19 OeaUnr Marine Mao .350-170-0101
. 3
Terraplus Inc.West Beaver Cr. Rd. 017. Richmond Hill. ON. Canada L4B 119
Tel: 905-764-5505 Fax:905-764-8093
Email- toiq}[email protected] l Wehsite: www.taiqAis.com_____J
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FREQUENCIES 110,220.440.000.1700.3S20.7MO* 14009Hz.
COIL ttTNO. 1: 12.*. 2S. SO. 7S. WO. 125. ISO. m. ScPARA* FOttSr 29v. 300 MM 400 MMVM (iBVnmMiVMQ.
SETN02 W. 20. 40. O*. W. 100.128.11*. 200,24* md 320 Mf
EETM0.3: 50. NO. 20*. 3W. 410, 900. MO. m. 10*0. 12*0 1*4 1*00
TRANSMITTER 11* Hr 220 A*r"DIPOLE 220HT 2tSA*a'MOMENTS: 440Hi: 2IOAto'
OMHr. 200A*K*
17MHEMOMII* 3620 Hr BOAtB3 7B40H*: *Ata'
MOHHz: ZOAte*
MODESOF yAXl:IUrtaaMH*B*rrt^Mi-*) OPERATION: MNlnaiiMraHptaMtlHitZMriBliMlc
PARAMETERS MEASURED:
READOUTS:
RAMGESOf READOUTS:
RESOLUTION:
REPEATABILITY:
SIGNAL FILTERING:
WARMING LIGHTS:
i*4 qndratara coapwwb of the aipnic*|M.i*K otpiHnay**M
i Krkt-
*M*r
SURVEYDEPTH Fn PENETRATION:
REFERENCE CABLE:
INTERCOM:
RECEIVER BATTERIES:
TRAH3MITTER BATTERIES:
TRANSMITTERBATTERYCHARGERS:
RECEIVER WEIGHT:
11* 1.Sl tan*t ml 0.7S
KM 12V-
12 V -14 Ak
14.4VO)1-2SA.I MV.MMMlai
1 HI.120 Md 220-240 VAC.H-
6(11
TRAttayRTTERWT:
SWPPIH6 WEIGHT:
STANDARD SPARES
OPTIONS AND ACCESSORES, PLEASE SPECFY:
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APPENDIX 2 (10)
ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES
Transaction No: Recording Date: Approval Date:
Client(s):
400275
Survey Type(s):
W0140.31058
2001-NOV-07
2002-JAN-04
Work Report Summary
Status: APPROVED
Work Done from: 2001-SEP-15
to: 2001-SEP-27
NINETY-NINE RESOURCES LTD.
EM LC MAG
Work Report Details:
Claim*
TB 1238090
TB 1239892
TB 1239893
Perform
S6.920
SO
SO
16,920
Perform Approve
56,920
SO
SO
S6,920
Applied
SO
S520
56,400
S6,920
Applied Approve
SO
S520
S6,400
S6.920
Assign
56,920
50
50
56,920
Assign Reserve Approve Reserve Approve Due Date
6,920
0
0
56,920
SO
SO
SO
SO
SO 2002-SEP-07
SO 2001-NOV-18
SO 2002-NOV-18
SO
Status of claim is based on information currently on record.
42L05NW2007 2.22389 JUNIOR LAKE 900
2002-Jan-07 03:27 Armstrong-d Page 1 of 1
Ministry ofNorthern Developmentand Mines
Date: 2002-JAN-04
Ministere duDeveloppement du Nord et des Mines Ontario
GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5
NINETY-NINE RESOURCES LTD. 5560 HOLT AVENUE RICHMOND, BRITISH COLUMBIA V7C 5C8 CANADA
Tel: (888) 415-9845 Fax:(877)670-1555
Dear Sir or Madam
Submission Number: 2.22389 Transaction Number(s): W0140.31058
Subject: Approval of Assessment Work
We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.
At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.
If you have any question regarding this correspondence, please contact BRUCE GATES by email at [email protected] or by phone at (705) 670-5856.
Yours Sincerely,
Ron GashinskiSupervisor, Geoscience Assessment Office
Cc: Resident Geologist
Ninety-Nine Resources Ltd. (Claim Holder)
Assessment File Library
Ninety-Nine Resources Ltd. (Assessment Office)
Visit our website at httpi/Awww.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16702
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