FIELD WORK VLF-EM SURV · 2017-01-17 · Field Work VLF-EM Survey On Claims 1163589,1163590,1163591, and 1163592 2. 219 56 Field Work Summary Date Operation Actual Time Total Hours

Results of VLF-EM Survey Performed August 28,1999 to September 8,1999

On Claims 1163589,1163590,1163591, and 1163592 In Neill Township

Sault Ste Marie Mining Division District of Sudbury

Field Work Performedby Philip Frankow

77 Elgin Street South, Chapleau, Ontario, POM 1KO

fRECEIVEDMK

QEOSCIENCf ASSESSMENT OfflCc , -— . — —

41O05NE2003 2.21956 NEILL 010

Field Work VLF-EM SurveyOn Claims 1163589,1163590,1163591, and 1163592

2. 219 56

Field Work Summary

Date Operation Actual Time Total Hours

August 28, 1999

August 29, 1999

September 03, 1999

September 04, 1999

September 05, 1999

September 06, 1999

September 07, 1999

September 08, 1999

Field VLF-EM Survey

Field VLF-EM Survey

Field VLF-EM Survey

Field VLF-EM Survey

Plot VLF-EM Readings on Gridlines



Plot VLF-EM Readings on Gridlines A Photocopy A send fax to John Walmsley

Shows

8 hours

8 hours

11 hours

10:00-22:00 l O hours

09:00-23:00 12 hours

19:00-23:00 4 hours

18:30-24:00 5.5 hours

Statement of Costs Summary

Item Total Cost

Survey: Kilometres Surveyed 11.384 km @ SI 10.00 per km 11,252.24

Travel: To Claims 4 trips @ 172 km @ S0.30 per km S206.40

Travel: To Thessalon l return trip (to pick up VLF-EM) @ 460 km @ S0.30 per km SI38.00

Meals: 9 meals @ SI0.00 per meal S90.00

Equipment: VLF-EM Rental (4days) S200.00

Report: Geophysical Report Interpretation Materials and Consulting (Pens Ink) S1000.00

Miscellaneous: Folders, Photocopies, shipping of Final reports S20.00

Total S2,906.64

9 1 9Y A/ . A/ l 57t/nsC'.

Technical Services

Invoice #: PI-05-2001Date: June 1,2001Re: VLF-EM Report

Geophysical Report and InterpretationMaterials, Consulting 31,000.00

VLF-EM Rental 4 days @ SSO/day 3200.00

Total 1 ,200.00

. -A

--*

Page l

EM1G SPECIFICATIONS 2. 219MEASURED QUANTITY

SENSITIVITY

RESOLUTION

OUTPUT

OPERATING FREQUENCY

OPERATOR CONTROLS

POWER SUPPLY

DIMENSIONS

WEIGHT

In-phase and quad-phase components of vertical magnetic field as a percentage of horizontal primary field, (i.e. tangent of the tilt angle and ellipticity) .

In-phase :

Quad-phase : 401

11

Nulling by audio tone. In-phase indication from mechanical inclino meter and quad-phase from a graduated dial .

15-25 kHz VLF Radio Band. Station selection done by means of plug-in units.

On/Off switch, battery test push button, station selector switch, audio volume control, quadrature dial, inclinometer.

6 disposable 'AA' cells.

42 x 14 x 9cm

Instrument: 1.6 kg Shipping : 4 . 5 kg

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Rugby, England Bordeaux, France

Helgeland, Norway

Moscow, U.S.S.R.

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. 21956

Results Of A VLF-EM Survey

On the

Frankow Property, Neil Township

June, 2001

By

John R. Walmsley

RR #1 Ruchards Landing, Ontario, FOR l JO

RECEIVEDAUG 2 1 200!

GEOSCIENCE ASSESSMENT._____OFFICE

41005NE2003 2.21956 NEILL 020

2 . 2195Introduction

In the spring of 2001, Pens Ink Technical Services was contracted by Mr. P.

Frankow to complete an assessment report for a VLF survey conducted on a group of

four (4) claims located in Neil Township, District of Sudbury. The VLF survey itself was

carried out by Mr. Frankow under the direction of the author and was completed in the

late summer of 1999. The current holder of the claims is Mr. Frankow.

The group of four (4) claims was staked to expand a larger group of claims also

held by Mr. Frankow, to the north and west of the currently described claims. The VLF survey was conducted largely to trace an EM anomaly delineated by an earlier VLF-EM

survey on the older claims that has an apparent strike onto the new claims.

This report describes the methods and results of the program and ties the new information in with the earlier work.

Property Description, Location And Access

The claim group described in the report is comprised of four (4) contiguous, unpatented, single unit claims, located approximately 5.5 km southwest of the northwest corner of

Neil Township (plan G-2476). The claim group is an addition to a group of 16 claims

staked at various times in 1987, 1988 and 1995 and which border the Neil/Moggy

Township border. The property is approximately 65 km southwest of the town of

Chapleau, Ontario, in the Sault Ste. Marie mining Division, District of Sudbury. Total

area covered by the four (4) claims described in this report is approximately ? hectres.See Figures l and 2 and Table l for Schedule of Claims.

Ground access to the property is by generally maintained logging roads and can be travelled by two wheel drive vehicles. Year round access is dependant on logging

activity. The Island Lake Road is taken from its junction with Highway 129, which is approximately 0.5 km south of the junctions of Highways 129 and 101, 5 km west of

Chapleau. Haifa kilometre west of Highway 129, on the Island Lake Road, the Pineal

Lake Road branches off to the southwest. Both roads converge again near the south end

of Corrigan Lake, 32 km along the Island Lake Road but the Island Lake Road is generally in better repair than the Pineal Lake Road. Two other roads also converge at

the point of intersection below Corrigan Lake: one road heads south towards Moen and Moggy Townships, and one heads southeast towards Neil Township and the herein

described property. This last road is followed for approximately 35 kilometres to the

claim group.

Table l Schedule Of Claims

Claim #_______Recorded Holder Recording Date Due DateSSM 1163589 SSM 1163590 SSM 1163591 SSM 1163592

Phi Hip Frankow Phillip Frankow Phillip Frankow Phillip Frankow

Sept. 22, 1997 Sept. 22, 1997 Sept. 22, 1997 Sept. 22,1997

Sept. 22, 2001 Sept. 22, 2001 Sept. 22, 2001 Sept. 22, 2001

Figure l Location Mapr Reprinted from MNDM Web Site)

me centre ot your map is m: u ivision: bault bte. Marie t ownship: NtiLL b -Pian: v-t4fb

lNeil Township

Moggy Township

ReportPropertyGroup

Figure 2 Claim Map(Reprinted from MNDM Web Site)

•Jt A. i

r r**. * l

TOPOGRAPHY AND VEGETATION

The claim group is of moderate to low relief with numerous, narrow, steep sided

ravines of less than 20 metre depth. The overall strike of these ravines is north/south and

east/west and appears to be generally controlled by geologic features. Intermittent

streams flow within these ravines during spring and wet periods. Drainage is mainly

northeast towards Fallwell Creek which flows southeast through the claims to the north of the group described herein. A sandy outwash plain creates a low hill in the northeast

corner of the claim group and the southern border is alder swamp.Vegetation is variably mixed poplar, spruce and jackpine and alders in the

swampy areas and ravine bottoms. Soil cover generally consists of a thick humus layer with some areas of subcrop and limited outcrop.

For a detailed description of the vegetation and topography on the rest of the property not described in this report, refer to Walmsley, 1996.

REGIONAL GEOLOGY

The property is located at the northeast corner of the Archean Batchawana Greenstone Belt. This greenstone belt extends eastward from near the shores of Lake

Superior to just east of the property boundary, a total distance of approximately 80 km. Very little detailed geological information is available for Neil Township. Grunsky

(1983) describes the supracrustal rocks of Neil Township as being "comprised of a distal

facies metavolcanic and metasedimentary succession that extends from the west."

Wilson (1983) mapped a narrowing belt of mafic to intermediate metavolcanics and

clastic metasediments into the central part of Moggy Township (immediately west of

Neill Township) but does not extend his mapping into Neill Township.Late Archean felsic plutonism has variably altered the rock suites at the east end

of the belt both metamorphically and structurally. Regional metamorphic grades range from greenschist facies to amphibolite facies, with locally higher grades closer to granitic

contacts. Grunski (9187), classifies the plutonic rocks in the vicinity of the property as granodiorites, tonalities and migmatites.

Later, intrusive rocks within the belt that are of particular significance to the property include quartz diabase, olivine diabase, felsite, and quartz porphyry.

According to Grunski (1987), the dominant structural feature in the area is a

symform that strikes generally east-west through Moggy Township and into Neil Township, just south of the property.

Both Grunski (1987) and Giblin (et al 1 979) show an east-north-east striking

lineation extending from the northwest corner of Neil Township, westward for

approximately 30 km. Hamilton (et al 1 995), have named this lineation as the "Montreal

River Fault System". A second northeast striking lineation passing the property close to

its western boundary has been called the "Toll Creek Lineament" by Hamilton (et al 1995).

See Table 2 for Table of Formations.

Table 2. Table of FormationsPHANEROZOIC

CENOZOICQUATERNARY

PLEISTOCENE AND RECENTTill, sand, silt, clay (minor fluvial, lacustrine and swamp deposits of gravel, sand, silt, clay) Unconformity

PRECAMBRIANMIDDLE To LATE PRECAMBRIAN (PROTEROZOIC)

FELSIC INTRUSIVE ROCKSDiabase, porphyritic diabase;, olivine diabase

Intrusive Contact EARLY PRECAMBRIAN (ARCHEAN)

FELSIC To INTERMEDIATE INTRUSIVE AND METAMORPHIC ROCKS Feldspar porphyry, quartz-feldspar porphyry; gneissise to metatexite quartz-feldspar rocks; quartz-feldspar intrusive rocks.

Intrusive ContactMETAVOLCANIC AND METASEDIMENTS

CHEMICAL SEDIMENTSMagnetite ironstone; chert

CLASTIC METASEDIMENTSWacke, mudstone, sandstone, conglomerate

FELSIC META VOLCANICSTuffs, crystal tuffs, metasediments

MAFIC To INTERMEDIATE META VOLCANICSMafic flows, tuffs, metasediments; pillowed mafic flows; bedded mafic tuffs; mafic to intermediate tuffs and metasediments

PREVIOUS WORK

Very little previous work has been completed on the property. The following is

mainly extracted from a compilation by Walmsley (1996).

The area was first mapped in 1936 by Keevil during a reconnaissance mapping program. Due to its remoteness, very little ground work was done in the area until Grunski in 1980

andWisonin 1983.

The Ontario Department of Mines and the geological Survey of Canada

completed airborne magnetometer surveys of the Cow River Area (1963). Other than a

mag low just to the northwest of the claims described herein and a mag high south of the

property, very little can be interpreted from the results.In 1989, the Ontario Geological Survey completed an airborne Total Intensity

Magnetic Survey and an Electromagnetic Survey of the Batchawana Area. This program covered the west and south part of the group of 16 original claims but did not cover the four (4) claims described herein. The results of this survey, reported on Map 81438, delineate several magnetic highs that roughly correspond with diabase dikes on the ground.

A Mineral Potential Map for this area has been produced by the Ontario Geologic Survey. This map rates the mineral potential for the property at 5 and 6. However, using criteria from the map and actual mapped geological contacts, the author recommends that

the mineral potential should be at least 3.The Ontario Geologic Survey also released preliminary results of the Cow River

Geochemical Mapping Projects, Batchawana Greenstone Belt.. This report "indicated high values of catchments of zinc, about 600 ppm in the Percy Lake Area (Moggy

Township." (Frankow, 1996).

The following has been extracted from an OPAP project proposal prepared by Mr. P. Frankow in 1996:

* 1981-82, stripping by E. J. Burns exposed altered andesite and diabase, mineralized quartz stringer with reported "tellurides"

* 1985, visit by Luhta and Ireland describe a massive pyrite-magnetic-

chert iron formation and assaying found traces of nickel, zinc, cobalt and

copper

* files obtained in 1983 from Hollinger Argus Ltd. Report anomalous gold, silver and lead from samples taken from the "pond" area

* 1986, airborne survey flown by Dighem Surveys for Frankow delineated

numerous EM and magnetic anomalies

* 1987, a second airborne survey by Terraquest Ltd for Frankow. Followup prospecting found anomalous copper, gold, silver, zinc and

nickel in samples taken along the conductor in the pond area.

* 1994/95, prospecting/sampling along newly constructed logging road

found anomalous copper, zinc, lead, silver, nickel and cobalt

* Propspecting along Farewell Creek has produced anomalous copper, gold, silver, cobalt, nickel and zinc

* General property prospecting has found anomalous values of copper,

gold, nickel and zinc associated with boulders of a feldspar porphyry, the source of which has been delineated by the current survey and is on the

property.

The most recent work on file at the Sault Ste. Marie Resident Geologist Office is

a report on geological mapping and a VLF-EM, conducted and described by the author in

the fall of 1996 on the 16 claims north and west of the property described herein. The geological mapping survey was conducted "to provide a geologic interpretation of the

rock assemblages on the property." No assaying of samples was done as part of the

survey. Both surveys were completed on a cut grid of 100 metre spacing. VLF-EM

readings of Cutler, Maine (NAA frequency 24.0 kHz) were taken every 25m.

The geology of the property was found to be complex with most of the property underlain by a sequence of mafic to felsic metavolcanics, volcanoclastics and associated

sediments. Granitic type intrusions underly the north and central part of the claim group. The metavolcanics and metasediment units are believed to underly the property group

described herein. A mafic feldspar porphyry was persistent throughout the property. Exposure of contacts was not good enough to determine if the occurrences were a series

of dikes or a sill. This unit often had pyrite/chalcopyrite mineralization near the contacts.Mineralization through the property was persistent, mainly pyrite and lesser

chalcopyrite and of low percentage. A pyrite/chert iron formation does appear to strike

onto the property described herein from the west-south-west. Other mineraliztion,

mainly on the eastern end of the property included sphalerite, bornite, malachite staining

and chalcocite. Quartz-carbonate veining was "noticeably absent on the property"

(Walmsley, 1996). Little mineralization was noted to be associated with quartz veining

that was observed except for one breccia unit located west of the property described herein and delineated as anomaly B described below.

The VLF-EM survey delineated two (2) anomalies, generally striking east-west

and onto the herein described property. These two anomalies are the main reason for the staking of these four (4) claims. Anomaly "A" delineated the mineralized iron formation described above. Anomaly "B" is believed to be a mineralized quartz-carbonate vein.

See Figures ? and ?.

CURRENT WORK - GEOPHYSICAL SURVEY

The VLF-EM survey was conducted by Phillip Frankow in the late summer of

1999. The survey used a cut grid with 100m grid lines and 25m stations. The instrument

used was a Geonics EM-16 (see Appendix A for specifications) and the transmitting station was Cutler, Maine (station NAA, frequency 24.0 kHz). Readings were taken

facing north on 25m centre, with 12.5m centre fill-in readings taken where appropriate. The three east-west baselines were also run using the same station. Readings from these

lines have not been interpreted due to their orientation and the skewed results that from using Cutler as the transmitting station. A total of 9.5 km of readings were taken during

the survey and Appendix B contains a print. The author was not present during the survey but did provide adequate instructions on the use of the instrument and how to conduct the survey.

Profiles of the quadrature and the in-phase have been plotted for the entire grid.

The in-phase data was manipulated with a low pass, 4 point Fraser Filter to filter noise

and accentuate anomalies. Only positive values were contoured and for interpretation

purposes, anomalous values of less than 10 are generally considered as conductive overburden.

CURRENT WORK - INTERPRETATION

The current survey delineated two (2) moderate east-west striking anomalies. The

strongest anomaly, Anomaly "A", bisects the claims east-west, almost along the middle

claim line (Baseline A) and strikes off the claim group both east and west, the strike

being concordant to what is believed to be the generally strike of the geology. This

anomaly is an extension of the VLF-EM anomaly identified as Anomaly "A" in the 1996

Report (Walmsley, Figure 6) and correlates to the mapped iron formation suggesting that

this unit continues onto and beyond the eastern boundary of the current claim group,

though it apparently is becoming weaker. The profiles suggest a near to very steeply

north dipping unit, narrow and the "parallel" nature of the quadrature in relation to the in-

phase indicates the conductor is at some depth.Anomaly "B" is concordant to Anomaly "A" at about 1+50 N and extends from

Line 11+00 E to beyond the eastern property boundary. This conductor is very weak at

the west end and becomes stronger towards the east. This anomaly is also believed to be an extension of an anomaly delineated in the 1996 survey (Anomaly "B").

Mineralization observed in a quartz-carbonate breccia during the 1996 survey has been

suggested as the possible source of this conductor. The eastern part of this Anomalya is coincident with a stream and ravene which maybe a possible explanation for it's increased strength. There is an apparent break between the 1996 anomaly which

appeared to end on Line 9+00 E or Line 10+00 E and the current anomaly which isn't interpreted as beginning until Line 11+00 E.

Figure 6

TFrazer Filter

VLF

InstrumentStationOperatorUnitsContour int.

EM16NAAT.Andersondog5 dag

Contoured In-pnose Frazer Filter

Pens Ink-for-P. Frankow

Frazer Filter VLFTwp.: Niel t Moggy Mining Division: SSM Dote Sun/.: Oct. 96 Orwn by: T.And*non

District: Sudbury Dote Croft.: Jan. 97 Scale: 1:5000 File: AU.FF.DWG

[i i

L 9*

00 E

L 10

*00

E

L1H

OO

C

Lttt

OO

E

L 14

*00 E

L 18

*00 E

LW*O

DE

L 17

*00

E

L1W

OE

L 19

*00

E

L 20

*00

E

1.9*

00 E

L 10

*00

E

L1HO

OC

Ltt*

OO

E

L1**

OO

B

L 14

*00

C

LH*O

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L17+

00 E

L1(*

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L 19

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L2D*

OO

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f!i

i i

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ri

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l l

11*1

1Ir

-

{i i

I f

I I

LBtO

OE

L 10

*00

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L 11

*00

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LtttO

OE

L1**

OO

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LWK

OE

L1S*

OO

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L 19

*00

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L 17

*00

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LU*O

OE

LW*O

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L10*

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' *

* Ij l

*

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*00 E

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LW*O

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L 30*

00 E

h i

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v i

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l11 ii i i i

n H M l

CONCLUSIONS AND RECOMMENDATIONS

The VLF-EM survey has delineated two (2) anomalies that are believed to be

continuation of anomalies identified with an earlier survey conducted in 1996. Anomaly

"A" is believed to be caused by an east-west striking iron formation and Anomaly "B" may be caused by a mineralized quartz-carbonate breccia. Previous sampling of

Anomaly "A" has found low but anomalous values of gold, suggesting that sampling be continued along its length across the current claim group and possibly two drill holes,

drilled from the north at a 45 degree angle on lines 12+00 E and 17+00 E.

Anomaly "B" should have detailed sampling and prospecting starting on Line

1 8+00 E and carried out to the eastern boundary. Prospecting should be continued

further than the eastern boundary if the ground has not been staked. Propecting VLF may also be warranted to help trace the anomaly further to the east. A drill hole may be warranted on Line 19+00 E.

For both anomalies, a check with a VLF should be conducted before any drilling is completed.

Respectfully Submitted,

John R. Walmsley, B.Sc.Geologist

June l, 2001

CERTIFICATE

With reference to my report on the exploration program conducted on the Frankow property, Neill Township for Phillip Frankow, date June l, 2001 ...

I John R. Walmsley, of the town of Richards Landing, Ontario, do hereby certify

the following to be true and accurate to the best of my knowledge:

* That I have received my Geological Engineering Technician papers from

the Sault College of Applied Arts and Technology in 1980,

* That I received a B.Se. Degree in Earth Sciences, majoring in geology,

from the University of Western Ontario in 1984,

* That I have been employed in the mining and exploration industry since

1978,

* That I am the author of the above referenced report

* That I have no interest, direct or indirect, in the four (4) single unit

unpatented mining claims described in this report.

Dated this First Day of June, 2001 Richards Landing, Ontario

John R. Walmsley, B.Sc.

Geologist

2. 219 56

Appendixes To Accompany

Results Of A VLF-EM Survey

On theFrankow Property, Neil Township

June, 2001

By

John R. Walmsley

RR #1 Ruchards Landing, Ontario, FOR l JO

RECEIVEDAC- 212001

GEOSCIENCE ASSESSMENT OFFICE

41005NE2003 2 .21956 NEILL 030

2 219 56Appendix A

VLF-EM Specifications

CJH

1

S3

W

DH

U

H

SPU

NOTES ON

STATION

NAA

NLK

NSS

CBR

FUO

JXZ

UMS

NWC

NOT

NPM

VLF TRANSMISSIONS

LOCATION

Cutler, Maine

Seattle, WashingtonAnnapolis, Maryland

Rugby, England

Bordeaux, France

Helgoland, Norway

Moscow, U.S. S. R.

North West Cape Australia

Yosami , Japan

Lualualei, Hawaii

FREQUENCY (kHz) CO-ORDINATES

17.8 67W17-44N39

18.6 121W55-48N12

21.4 76W27-38N59

16.0 01W11-52N22

15.1 OOW48-44N65

16.4 13E01-66N25

17.1 37E01-55N49

22.3 114E09-21S47

17.4 137E01-34N58

23.4 158W09-21N25

?Q

c- *H

C , w

Page 19

FIELD PROCEDURE

Orientation S Taking a Reading

The direction of the survey lines should be selected approxi mately along the lines of the primary magnetic field, at right angles to the direction to the station being used. Before starting the survey, the instrument can be used to orient one self in that respect. By turning the instrument sideways, the signal is minimum when the instrument is pointing towards the station, thus indicating that the magnetic field is at right angles to the receiving coil inside the handle.(Fig.11).

To take a reading, first orient the reference coil (in the lower end of the handle) along the magnetic lines.(Fig.12) Swing the instrument back and forth for minimum sound intensity in the speaker. Use the volume control to set the sound level for comfortable listening. Then use your left hand to adjust the quadrature component dial on the front left corner of the instrument to further minimize the sound. After finding the minimum signal strength on both adjustments, read the inclino meter by looking into the small lens. Also, mark down the quadrature reading.

While travelling to the next location you can, if you wish, keep the instrument in operating position. If fast changes in the readings occur, you might take extra stations to pinpoint accurately the details of anomaly.

The dials inside the inclinometer are calibrated in positive and negative percentages. If the instrument is facing 180O from the original direction of travel, the polarities of the readings will be reversed. Therefore, in the same area take the readings always facing in the same direction even when travelling in opposite way along the lines.

The lower end of the handle, will as a rule, point towards the conductor. (Figs.13 S 14) The instrument is so calibrated that when approaching the conductor, the angles are positive in the in-phase component. Turn always in the same direction for readings and mark all this on your notes, maps, etc.

THE INCLINOMETER DIALS

The right-hand scale is the in-phase percentagede.Hs/Hp as a percentage). This percentage is in fact the tangent of the dip angle. To compute the dip angle simply take the arc tangent of the percentage reading divided by 100. See the conversion graph on the following page.

The left-hand scale is the secant of the slope of the ground surface. You can use it to "calculate" your distance to the next station along the slope of the terrain.

Conductor Ahead

Page 21

(1) Open both eyes.

(2) Aim the hairline along the slope to the next station to about your eye level height above ground.

(3) Read on the left scale directly the distance necessary to measure along the slope to advance 100 (ft) horizon tally.

We feel that this will make your reconnaissance work easier. The outside scale on the inclinometer is calibrated in degrees just in case you have use for it.

PLOTTING THE RESULTS

For easy interpretation of the results, it is good practice to plot the actual curves directly on the survey line map using suitable scales for the percentage readings. (Fig.15) The horizontal scale should be the same as your other maps on the area for convenience.

A more convenient form of this data is easily achieved by transforming the zero-crossings into peaks by means of a simple numerical filtering technique. This technique is described by D.C. Fraser in his paper "Contouring of VLF-EM Data", Geophysics, Vol. 34, No. 6. (December 1969)pp958-967. A reprint of this paper is included in this manual for the convenience of the user.

This simple data manipulation procedure which can be imple mented in the field produces VLF-EM data which can be contoured and as such provides a significant advantage in the evaluation of this data.

cn of

Finding /~fie direction '\ Of primary fie/d

, l j / l l l 1^^lBest-survey //We' ' l l OpHmum d l ree H on \ J , direction

s ha h i on

P/anning of survey

FIG. 3 (U vQ (D-^J

2 219 58

Appendix B VLF-EM Inphase/Quadrature Readings

2. 219 56Line 09 E

Station Number4+25 S4+00 S3+75 S3+50 S3+25 S3+00 S2+75 S2+50 S2+25 S2+00 S1+75 S1+50 S1+25 S1+00 S0+75 S0+50 S0+25 S0+00

0+25 N0+50 N0+75 N1+00 N1+25 N1+50 N1+75 N2+00 N2+25 N2+50 N2+75 N3+00 N3+25 N3+50 N3+75 N4+00 N4+25 N4+50 N4+75 N5+00 N5+25 N5+50 N5+75 N6+00 N

In Phase-4

-10-5

27

11111216181818202225252510g91214161512523459172527302518112

-12-13-18

Qaudrature-8

-14-12-8-4-1

6400-2-4-4-4-3-2

0-14-18-17-13-12-9-6-8

-12-11-13-14-1

-13-11-7-4-3-2-3

11446

Line 10 EStation Number

4+30 S4+25 S4+00 S3+75 S3+50 S3+25 S3+00 S2+75 S2+50 S2+25 S2+00 S1+75 S1+50 S1+25 S1+00 S0+75 S0+50 S0+25 S0+00

0+25 N0+50 N0+75 N1+00 N1+12 N1+25 N1+38 N1+50 N1+62 N1+75 N2+00 N2+25 N2+50 N2+75 N3+00 N3+25 N3+50 N3+75 N3+89 N4+00 N4+25 N4+50 N4+75 N5+00 N5+25 N5+50 N5+75 N6+00 N

In Phase-26-22-12

-4

1368

10131615161919202412

02368

126

1068752232

12152024253330231812-2

-12-18

Qaudrature-19-18-12-10-6-6-2-1-3-1

0-2-3-2-4-3

0-9

-22-20-20-18-14-12-9-6-9

-10-9

-10-13-14-15-16-14-12-9-8-8-5-4-4-2-2

125

Line 11 E Station Number4+28 S4+25 S4+00 S3+75 S3+50 S3+25 S3+00 S2+75 S2+50 S2+25 S2+00 S1+75 S1+50 S1+25 S1+00 S0+75 S0+50 S0+25 S0+00

0+25 N0+50 N0+75 N1+00 N1+25 N1+38 N1+50 N1+75 N2+00 N2+25 N2+50 N2+75 N3+00 N3+25 N3+50 N3+75 N3S7+.5 N4+00 N4+25 N4+50 N4+75 N5+00 N5+25 N5+50 N5+75 N6+00 N

In Phase-23-20-14-7-3-1

571012151616171820259-2-1

26

1112197852356106

20241721262020152-9

-17

Qaudrature-18-17-14-10-8-8-6-3-2

12-1-2-4-5-4

2-17-26-24-21-17-13-8-4

-11-9

-10-13-14-14-14-13-11-10-8

-10-8-7-8-4-2

025

Line 12 E Station Number4+25 S4+00 S3+75 S3+50 S3+25 S3+00 S2+75 S2+50 S2+25 S2+00 S1+75 S1+50 S1+25 S1+00 S0+75 S0+50 S0+25 S0+00

0+25 N0+50 N0+75 N1+00 N1+25 N1+50 N1+75 N2+00 N2+25 N2+50 N2+75 N3+00 N3+25 N3+50 N3+75 N3S7+.5 N4+00 N4+25 N4+50 N4+75 N5+00 N5+25 N5+50 N5+75 N6+00 N

In Phase-16-17-15-10-2

471012171818202020237-6-2

158137634368131217131513111017168-2

-15

Qaudrature-8

-10-21-12-8-4-3

00241

-1-3-4-3

-11-19-18-17-16-14-9-9-9

-12-12-13-13-12-11-12-12-10-10-10-11-11-6-3-1

02

Line 13 E Station Number

4+22 S4+00 S3+75 S3+50 S3+25 S3+00 S2+75 S2+50 S2+25 S2+00 S1+75 S1+50 S1+25 S1+00 S0+75 S0+50 S0+25 S0+00

0+25 N0+50 N0+75 N1+00 N1+25 N1+50 N1+75 N2+00 N2+25 N2+50 N2+75 N3+00 N3+25 N3+50 N3+75 N387+.S N4+00 N4+25 N4+50 N4+75 N5+00 N5+25 N5+50 N5+75 N6+00 N

In Phase-15-12

-6-2

355

10131519192020212326

0-3

14

1010724357

910121414-5

57

1013126

-2-12

Qaudrature-5-4-1-1

1-1-2-1

034440

-2-3

0-19-22-18-15-11

-8-8

-10-12-12-12-12-11-12-11-10-11-11-11-11

-8-6-3

024




In Phase70

-5-2

1489

121518222422242425

82028

105345

1095

-2-5-3-3

015653

-1

0-5

Qaudrature113

-3-2-4-1

000144510

-3-3

-13-17-18-16-12-9

-12-11-12-11-8-9

-10-12-14-13-14-10

0-10-6-2-6-4

2-6



0+25 N0+50 N0+75 N1+00 N1+25 N1+50 N1+75 N2+00 N2+25 N2+50 N2+75 N3+00 N3+25 N3+50 N3+75 N3S7+.5 N4+00 N4+25 N4+50 N4+75 N5+00 N5+25 N5+50 N5+75 N6+00 N

In Phase3

-2-3-2

368

10136

202326252526281176

1115126335773200

-1

110

-5-4-4

-10-9-5

Qaudrature71

-1-3

0000124662

-1-4-2

-12-17-16-14-10-10-11-12

-9-8-5-4-8-7

-10-12-12-10

-8-10-9-7-6-3-3

2




In Phase7235587

10151820232525252628108

1017232411101085442000

-1-2-1

00

-4-15-14-10

Qaudrature9302

-2

0-3-1

023431

-1-3-3

-16-16-17-14-10

-6-10

-8-6-4-7-8-6-8-9

-10-10-9-8-6-6-3-2-4-1

4




In Phase4656788

11137

2024273238353430-1

3121915179988g631

-1-2-4-3-3-3-2

0-14-15-11

Qaudrature774211001215254

-1-1-3

-23-22-17-30

-7-7-8-7-6-8-5-7-7-g-g-8-5-6-3-3

04227




In Phase4566899

1315182022232525283430

18

1822251511109478

101

-1-1-1-2-3-2

1-5

-14-10

-8


-4-2

0-2

-24-22-18-13

-9-8-8-8-7

-10-7-6-4-7-6-8-4-3-2-1

11359




In Phase548

1078

1013151720212424222525236

1119273321131210101010633

-1-1

478

10-6

-11-15

-8


-1-3-4-5-6

-21-22-18-14

-9-9-9-9

-10-10

-7-4-3-4-4-3-4

0634256

10


4+23 S4+00 S3+75 S3+50 S3+25 S3+00 S2+75 S2+50 S2+25 S2+00 S1+75 S1+50 S1+25 S1+00 S0+75 S0+62 S0+50 S0+25 S0+00

0+25 N0+50 N0+75 N1+00 N1+25 N1+50 N1+75 N2+00 N2+25 N2+50 N2+75 N3+00 N3+25 N3+50 N3+75 N3+87 N

In Phase558

1110121312131514162020202522252212131725322218139

151493

-3-2

0

Qaudrature745653321

-1-4-1-2-5-6

-10-9-7

-10-17-19-18-16-12-13-10-10-12-10

-7-5-5-4-2-1

Maps of the VLF-EM

6+00 N

5+00 N

BaMlbwB

3+00 N

9496142*00 N

1+00 N

BaMllneB

1+00 S

2+00 S

9496193+00 S

4+00 S BaaehmA

lil ui ill l

Ill UJ 111 111 111 111 ui ui UI

UJ UI UIs UJ UJ UIf UJ UJ ui l

ui ui ui

6+00 N

6+00 N

BaaalneB

3+00 N

2+00 N

1+00 N

BaaMneB

1+008

2+003

3+008

4+008 BaaalneA

N

2. 219 51163590 Claim Number

. Claim Port

— - —i* stream

^ Swwamp—— --—— CtaimLine

Anomaly

Anomaly MonUHai

Inprwae Quadrature

Contour Interval 5*.

Scale: 1:5 000

Phillin P FrankownipVLF-EM Survey Survey Profiles

m ui ui l

Ul Ul Ul Ul Ul Ulf Ul 111 Ul

6+00 N

5+00 N

Baseline B

3+00 N

9496142+00 N

1+00 N

BaMllneB

1+00 S

2+00 S

9496193+003

4+00 S BaselneA

6+00 N

5+00 N

BattfrwB

3+00 N

2+00 N

1+00 N

Daielne B

1+003

ui Ul uiS

Ul Ul Ul Ul Ul Ulf ui ui

2+008

3+OOS

4+008 BaselneA

ui

N

2. 219 51163590 Claim Number

m CMm Poit

—,, — .. —^ Stream

^ Swwarnp——— —— Claim Line

^• ——— Anomafy

Anomaly Identifier

Quadrature

Contour Interval 5-X,

Phillip P. FranknwVLIF-EM Survey

Fraser Filter Contours

ONTMIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No:

Recording Date:

Approval Date:

Client(s):133452

Survey Type(s):

W0150.30610

2001-AUG-21

2001-SEP-20

Work Report Summary

Status: APPROVED

Work Done from: 1 999-AUG-28

to: 2001-AUG-19

FRANKOW, PHILIP LEO

VLF

Work Report Details:

Claim*

SSM

SSM

SSM

SSM

1163589

1163590

1163591

1163592

Perform

S727

S727

S727

S726

82,907

Perform Applied Approve Applied Approve

S727

S727

S727

S726

32,907

SO

SO

SO

SO

SO

soSOsososo

Assign Assign Approve

SO

SOsosoSO

0

0

0

0

SO

Reserve

S727

S727

S727

S726

S2.907

Reserve Approve

S727

S727

S727

S726

S2.907

Due Date

2001-SEP-22

2001-SEP-22

2001-SEP-22

2001-SEP-22

Status of claim is based on information currently on record.

41005NE2003 2.21956 NEILL 900

2001-Oct-01 09:34 Armstrong.d Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2001 -SEP-21

Ministers duDeveloppement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E6B5

PHILIP LEO FRANKOW 77 ELGIN STREET P.O. BOX 430 CHAPLEAU, ONTARIO POM 1KO CANADA

Tel: (888)415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2 .21956 Transaction Number(s): W0150.30610

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 LUCILLE JEROME by email at [email protected] or by phone at (705) 670-5858.

Yours Sincerely,

Ron GashinskiSupervisor, Geoscience Assessment Office

Gc: Resident Geologist

Philip Leo Frankow (Claim Holder)

Assessment File Library

Philip Leo Frankow (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16426

MINING LAND TENUREMAP

KDIIMMI DEVELOPMENTINCHIIII.

Date /Time of Issue Apr I I 2001

TOWNSHIP l AREA

NEILL

11:00h Eastern

PLAN

Q -2478

ADMINISTRATIVE DISTRICTS l D IVISIONS Mining Division Sault Ste. Marie Land Tlttes/Reglstry Division SUDBURY Mlnlttry of Nilural Rtiourc** Dlitrfct CHAPLEAU

LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL D ESCRIPTIONS

IMPORTANT NOTICES

General Information and Limitations iri land inure MJ iMcrvvtl " iiM mcHiinert*lHH*t, HIBOMIIl, rl|H DI

hum**CiPi*i. MM nth^ rif*fcf w pionikl (f iff nnhv w wake minlno tlAiH mo

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Documents

FIELD WORK VLF-EM SURV · 2017-01-17 · Field Work VLF-EM Survey On Claims 1163589,1163590,1163591, and 1163592 2. 219 56 Field Work Summary Date Operation Actual Time Total Hours