AEM SUR FILE NO: 15027

41P14NE0216 8.1514 HALLIDAY

JUL.8 1974

PROJECTS UNIT

010

AIRBORNE ELECTROMAGNETIC SURVEY

GRANGES EXPLORATION CANADA AB

ENGLISH TOWNSHIP AREA

FILE NO: 15027

QuestorSurveysLimited,20CansoRd.,Rexdale,Ontario,Canada.

l- l -

l l l l l

l l

!

l

INTRODUCTION

l This report contains our interpretation of the

results of an airborne electrfcmagnetic survey, flown in————————————————————————————A.

the English Township Area, Ontario, on September 11, 12,

m 13, 14, 16 and 17, 1973. A brief description of the sur

vey procedure together with recommendations for ground

l follow-ufe is included.

The sujrgg^ôjâ^jj^^l^^lêiiii.les and was per

il formed by Questor Surveys^Limited. The survey aircraft was

ta a Shorts Sky van, CF-QSL and the operating^base was Timmins,

Ontario.

m The area outline is shown on the 1:250,000 N.T.S.

maps 42A and 4IP at the end of this report.

MAP COMPILATION

The base maps are uncontrolled mosaics constructed

from Ontario Department of Lands and Forests l" * 1/4 mile

photographs. The mosaics were reproduced at a scale of l"

equals 1320 feet on stable transparent film from which white

prints can be made.

Flight path .recovery wagLflccojoaaLlfiJied bv comparison

of the prints of the 35mm film with the mosaic in order to

locate the fiducial points. These points are approximately

one mile apart.

- 2 -

SURVEY PROCEDURE

~" Terrain clearance was maintained as close t

l feet as possible, with the E.M.Bird at approximately 150

feet above the ground. A normal S-pattern flight path

l using approximately one mile turns was used. The equipment

operator logged the flight details and monitored the instru

ments .

l A line spacing of 1/8 mile was used.

l

l

l

l

l

l l

l

l

l

l l

l l

INTERPRETATION AND RECOMMENDATIONS

References: Aeromagnetic Sheets 41 P/14 6 42 A/3.

Ontario Preliminary Geology Map No.P 151.

Ontario Preliminary Geology Map No.P 141.

Ontario Preliminary Geology Map No.P 490 Semple T.P.

Ontario Preliminary Geology Map No,P 454 English T.P.

Ontario Preliminary Geology Map No.P 455 Zavitz T.P.

Ontario Preliminary Geology Map No.P 491 Hutt T.P.

A considerable amount of work has been done in these

survey areas and a great many of the conductors that have been

outlined have been drilled in the past. However, from the ref

erences listed above, it would appear that there are still some

good targets that have not been tested. The apparent weak

anomalies may also be significant and should be given some

attention whether they have been discussed or not. It is felt

that most, of the INPUT anomalies that have been plotted have

their source in bedrock.

The area is underlain by interstratified metavolcanic

sequences and in Hutt Township, rhyolite interbeds are often

associated with narrow lenses and zones of graphitic schists

l - 3 -

lm 4fc and slate containing disseminated to massive pyrite with minor

pyrrhotite and chalcopyrite. Discontinuous narrow lenses of

l low-grade iron formation, also occur within the area and these

respond electromagnetically in some areas.

l Serpentinized peridotite is also prevalent, espec-

M ially in Zavitz Township and in places this peridotite is a

fair INPUT conductor. However, it would not respond well to

l conventional ground E.M. systems unless there are discrete

sulphide lenses present,

l - Even though conductor Zones 6, 7, 9, 10 f 11 and 14

'H in Area 2 appear to be discrete conductors, they are on strikel ——~""""— and are apparently associated with an iron formation which

l trends north-south through the area. Similarly, Zones 8, 12

and 13.-are on strike and are associated with a minor iron. —i J formation again tending north-south.

l— The following is a discussion of various conductor

™ systems, some of which have apparently been explained by pre-

•j vious work but are left in for the sake of completeness. An

investigation of the assessment files should be made to ensure

l that these conductors have been explained with confidence and

they can also be used as a guide to explaining the other zones.

l It is difficult to rank these zones with regard to

m priority selection in the ground follow-up, but Zones 10 and

^14. in J^cej^l, do stand out as top priority targets, provided

l that they have not been previously explained.

ii^

i

ll

- 4 -

AREA 1.

l Zone l

The two anomalies (1G and 2D) which make up this

l conductor are weak but appear to have their source in bedrock.

m Since they are bedrock anomalies and in an area of felsic

volcanic rocks, ground work is suggested. There is no evi-

l dence of previous work.

Zone 2

l ' This conductor^which lies on the border between

l li l i l i i i

i

l this long conductor, and sulphides are suspected to be a cause.

m There is some magnetic correlation at the east end of this

zone. The two anomaly responses on the south lines and one on

l

Halliday and Midlothian Townships is weak but appears to have

its source in bedrock. Ground work is recommended. Felsic

volcanics have been mapped in the area.

Zone 3

Anomaly intercept 6A appears isolated but the adja

cent lines do not extend far enough south to intersect the

anticipated conductor axis. A value of 9mhos has been cal

culated for this anomaly. Ground work is suggested.

Zone 4

This short conductor which parallels zone 5 to the

north i exhibits moderate conductivity and has some magnetic

correlation. Since this zone does not appear to have been

worked on and it is a short discrete conductor, it should be

investigated.

Zone 5

Good conductivity-thickness anomalies characterize

l

l

i k l l iji

the north indicate a dip to the north. It is recommended that

both ends of the conductor be investigated.

Zone 6

A horizontal loop survey is suggested to be carried

out over this cluster of anomaj.ies, in an effort to resolve

l and further evaluate the zone. Moderate to good conductivity-

i thickness values are shown by the anomalies and there is mag-

l

B

netic correlation with some of the anomalies. Sulphides are

expected to be present.

Zone 7'H\m The poor definition of anomaly 4 3A, probably resulted

from striking the conductor at a poor coupling angle. Poss-

I ibly a fold exists in the conductor at this location. An

m orientation survey is suggested prior to line cutting to

ensure the optimum coupling angle in a ground survey. There

l is some small indirect magnetic association with the zone

suggesting that minor sulphides are a cause. Ground work is

l recommended.

l. Zone 8

™ This zone is discussed under Zone 50; Area 3. Better

definition resulted in the other direction.

Zone 9

Discussed under Zone 53i Area 3.

l

l

AREA 2.

Zone l

ll l

Diamond drilling by Spirit Lake Mines on this cluster

l of good conductivity-thickness anomalie,s indicate that pyrite

and some chalcopyrite is the cause of the conductivity. This

B zone within the mafic and felsic metavolcanics has been intru-

M ded by a diabase dike; hence the discontinuity in the middle

of the conductive zone. Since this zone has obviously been

l explained, no further work is recommended.

Zone 2

l This single line conductor lying to the east of the

m zone is weak but appears to have its source in bedrock. The

weakness of this anomaly may be due to a poor coupling angle,

l ie., the strike of the conductor axis is in question. Since

the conductor does not appear to have been worked on and lies

l within a good geologic environment, ground work is recommended.

B Zone 3

Considerable diamond drilling by Daniel Mining Company

l in j-967, intersected some pyrite and nickel mineralization.

The poor conductivity-thickness anomalies indicate that massive

l sulphides do not exist and the E.M. responses are probably due

— to disseminated sulphides within the peridotite. No further

" work is recommended.

l Zone 4

Discussed under jone 22; Area 3, this anomaly is

l poorly defined in this direction.

ll Zone 5

M The anomalies in this zone are weak but apparently

™ of bedrock origin. Minor sulphides could be the cause. Ground

l work is recommended ̂ on a low priority basis.

Zone 6

l This strong good conductivity-thickness ̂ conductor

. is associated with a high magnetic linear. Sulphides assoc-

™ iated with an iron formation is the probable cause of the

l conductivity. Ground work is recommended at the southern end

of this zone where the conductivity-thicknesses are the highest,

l Zone 7

' Hollinger Gold Mines has done work In the vicinity

™ of this ônductor. but the evidence indicates that only the

|| northern portion has been investigated, so it is therefore

recommended, that the southern portion be checked. The zone

l is made up of moderately strong anomalies with magnetic cor-

i relation similar to those that result from sulphides. A

B diamond drill hole in the northern part intersected magnetite,i

pyrite and chalcopyrite.lZone 8

l The strong influence of the nearby hydro line has dis-

i. torted the anomaly shape and has masked out any possible exten-

I sion of the conductor to the north. However, this anomaly is

M obviously a bedrock one and the direct magnetic correlation adds

interest. A horizontal loop survey utilizing a system such as

l the Geonics E.M. 17, which minimizes the hydro effects should

be used to check this conductor.

l

l

l'

L*i

Zone 9

The regional magnetics indicate that this conductor

l is on the same horizon as Zones 6- 7. 10 and 11., all of which

B are associated with an iron formation. No further work is

" suggested on this section.

l Zone 10

Conigo Mines Ltd. , has worked on this portion of

I - the iron formation and magnetite, pyrrhotite and pyrite have

i been found in trenches. These sulphides are obviously the

i l l h ll formation and on strike with Zones 8 and 13. The anomalies

L are somewhat distorted due to the proximity of the strong

hydro line. Ground work on a low priority is recommended.

l Zone 13

cause of the conductivity. The conductive zone does not

correspond to the peak of the high magnetic anomaly suggest

ing that the conductor is caused by sulphides on the flank

of the iron formation.

Zone 11

This is a further extension of the iron formation.

Possibly intercepts 138A and B^should be included in ground

work.

Zone 12

This conductor is apparently associated with an iron

Similar to Zone 12, this conductor is associated

with the iron formation. Ground work is recommended to cover

anomalies 165A and 166A^ which are strong, good conductivity-

thickness anomalies.

ll

- 9 -

Zone 14

This conductive zone is an extension of Zone 11

l and ground work should be carried out to include anomaly 164A.

H Zone 15

Vertical diamond drill holes have intersected mag-

I

l l l

i

l l l l

l

l

notite, pyrrhotite and pyrite in the vicinity of this

iAREA 3.

but apparently no work has been done on intercepts 14OA and

141B,which are moderate conductivity-thickness anomalies.

Ground work is therefore suggested to cover these intercepts,

Massive and porphyritic dacite have been mapped in the area.

The weak intermittent zone within the confines of

Muskasenda Lake are poor conductivity-thickness anomalies

reflecting lake bottom conductivity.

^ Zone l Same as Zone 1; Area 2.

Zone 2 Same as Zone 6; Area 2.j MMMMMMMMMBV

l Zone 3 Same as

Zone 4 Same as Zone 9 f Area 2.

Zone 5

This is the same as Zone 8 ;^ Area, JSi however, more

anomalies^ have been intersected and it would appear that there

are two conductors present striking east-west. The anomalies

are well defined in this direction because there is poor coup

ling with the hydro line.

l - 10 -

l ^P* Zone 6

This zone may be connected to ZoneS but the hydro

l line has masked any possible anomalies which may exist between

m the two zones. The anomalies are distorted but they are def-

inate bedrock responses. Similar to Zone 5 , it has to be

i i l i

Zone 7 Same as Zone 14; Area

l regarded highly in a ground program.

l

l

k k l l

i

Zone 8 Same as Zone 15 f Area 2.

Zone 9

The shape of this single intercept is severely dis

torted from the hydro influence but it appears to have a gen

uine bedrock source. Similar to Zones 5 ancLJL, this conductor

will be difficult to assess on the ground because of the prox

imity of the hydro line, however, an attempt should be made.

Felsic metavolcanics and an iron formation has been mapped

immediately to the east of the anomaly.

Zone 10

The conductor has to be regarded as a high priority

^ target because it is isolated, has good conductivity-thickness

" values and it is in a good geologic environment, ie., inter-

I mediate to felsic volcanics. Apparently no previous work has

been done on the conductor,

l Zone 11

Some work has been done in the past by Phelps Dodge

in this area but the diamond drill holes do not plot on the

same location as the E.M.anomaês. For this reason, a fur

ther investigation is required. Moderate conductivity-thick

ness values have been calculated for the anomalies and there

is some magnetic association with the intercepts.

lIntermediate metavolcanics have been mapped in the area.

Zone 12

l Diamond drilling by Hollinger on the western por-

•j tion of this zone revealed pyrite and graphite; however,

there is no indication that the eastern part, which appears

l to be discontinuous with the western part has been investi

gated. As a result, an investigation is warranted. The

l zone appears to be made up of at least two parallel conductors

M of varying strength. Intermediate to felsic metavolcanics

* have been mapped in the vicinity.

l Zone 13

The conductivity-thickness product is consistent

l l l l

li

along the strike of this curved conductor^lying within the

intermediate and felsic metavolcanics. Considerable diamond

drilling by Hollinger has intersected pyrite, graphite and

some chalcopyrite and it would appear that sufficient work

has been done to adequately explain the conductor.

Zone 14

This conductor which is lying near the contact of

the massive andesite and rhyolitic flows exhibits excellent

l conductivity-thickness values. Since the conductor is isolated

and is similar to those that result from massive sulphides, it

l has to be regarded as an excellent target.

Zones 15 and 16

These two zones are probably connected but the hydro

line has masked out any possible bedrock conductor indications

between the two zones. The conductor is caused by sulphides

within the peridotite rather than the serpentinized peridotite

li i

l l

i l i

- 12 -

itself.

Diamond drilling has been done on the western

portion and some pyrite has been intersected but apparently

no work has been done on the eastern and longer portion

(Zone 16) .

l The double anomaly response on some of the south

lines indicates a dip to the north rather than two separate

l conductors. Ground work on a medium priority basis is sug-

m gested on Zone 16.

Zone 17

l Apparently no previous work has been done on this

conductive zone which parallels Zone 16, and which lies within———————————— ——————the intermediate metavolcanics. Ground work is recommended.

B Zone 18

™ Minor sulphides near the contact of the felsic

and intermediate metavolcanics are possibly the cause of the

conductor. There is some magnetic association with the con

ductor.

Zone 19

™ These anomalies are weak poor conductivity-thicknessl

l value responses, however, they appear to indicate a bedrock

conductor. Possibly minor sulphides along a fault zone are

l the source. Ground work on a low priority is suggested,

i Zone 20 Same as Zone 5; Area 2.

Zone 21

This single intercept conductor is weak and exhibits

a poor conductivity-thickness value. A low priority is given

to the conductor.

l

l l

- 13 -

Zone 22

Apparently no previous work has been done on this

l conductor which lies within the intermediate metavolcanics

but close to the contact with the serpentinized peridotite.

l A good conductivity-thickness value has been calculated for

m intercept 2 04H . Ground work is definately warranted.

Zone 23 Discussed under Zone 3 ; Area 2 .

l Zone 24

The poor conductivity anomalies in this zone are

l probably caused by serpentinized peridotite, or minor sulphides

. within the peridotite. Diamond drilling in the area has re-

™ vealed nickel mineralization. No further work is recommended.

l Zone 25

Amax has apparently drilled this conductor and inter-

J sected pyrite and pyrrhotite within the felsic volcanics. The

— conductivity-thickness values which have been approximated for

" the anomalies are representative of a sulphide zone, but since

l the conductor has apparently been explained, no further work

is suggested.

l Zone 26

^ Mineralization has been noted in trenches in the

" vicinity of this weak INPUT conductor, but from the responses

m it is apparent that this zone is quite small and the mineral

ization is disseminated. The conductor lies in complex geology

l of intermediate and felsic metavolcanics and serpentinized

ultrabasic rocks.

k i

- 14 -

i l l l

i

l li l l i

Zones 27 and 28

The anomaly, intercepts of these two zones exhibit

l poo;: to moderate conductivity-width values with some erratic

m magnetic correlation. Pyrite has been trenched in the vic

inity of conductor 28, however, Zone 27 does not appear to

l have been investigated. Intermediate and felsic metavolcanics

have been mapped in the area,

l Zone 29

j Intercept 216.CL is a reasonably strong fair conduc-

B tivity-thickness value ainomalv^ with no magnetic correlation;

l whereas the adjacent anomalies are of a poorer quality.

Ground work is recommended.

Zones 30 and 31

These two zones are probably the same conductor * but

the hydro line has obliterated any intercepts between the two.

Amax Exploration has drilled some holes and has obviously

explained the conductor. Pyrite, pyrrhotite with some copper

mineralization has been encountered. The anomalies are strong

and are representative of massive sulphides. No further work

is recommended.

Zone 32

Graphite may be the cause of this strong multiple

ônductinq zone within the sediments. However, a horizontal

loop E.M. survey is suggested to further define and evaluate

the zone for massive sulphide possibilities.

l

l

- 15 -

Zone 33

Ground work is recommended on a medium priority

l basis on this arcuate conductor,

l Zones 34 and 35

These moderate conductivity-thickness JSigffigjjigg,

l which are associated with high magnetics are probably caused

by serpentinized peridotite which has been mapped in the area,

l Zones 36 and 37

— Ground work is recommended on a medium priority basis

* on these two zones

Zone 38

This large mass of annnî -j^g I-JOQ within the acid

l metavolcanics and graphitic schists and slates containing

m massive pyrite and pyrrhotite is the obvious explanation of

B the conduction. It is recommended that the higher conduc-

I tivity-width anomalies be investigated.

Zones 39 and 40

l

l

l

l

l

massive pyrite and pyrrhotite in a bed of cherty rhyolite

l breccia which also contains copper. The anomalies are not

strong but are obviously bedrock and the coincident magnetic

These two zones are in a similar environment to Zone

38 and graphite and massive sulphides are probably the cause.

Zone 39 should be investigated.

Zone 41

This zone is a marginal bedrock conductor but it

should be considered in a ground program. Minor sulphides

beneath the overburden could be the cause.

Zone 42

Voyager Exploration has encountered disseminated to

l

i l i l i l l i il

il ^^ anomalies are probably due to pyrrhotite. Since the conductor

has been explained, no further work is recommended.

Zone 43

l The conductivity-width values vary from poor to good

along the strike of this long conductor. Portions of this

l horizon have been investigated and copper and silver have

— been encountered; however, pyrite and pyrrhotite would appear

* to be the main constituents of the conductor. Possibly the

west end of the conductor should be investigated where it

appears that no previous work has been done.

Zone 44

There is no evidence that any previous work has been

done on this strong multiple conducting zone within the felsic

volcanics. The anomalies are strong and similar to those that

result from massive sulphides. Ground work is definately war

ranted on the entire zone.

Zone 45

This zone should be regarded as a high priority tar

get. Good conductivity-thickness values have been calculated

for the responses and are similar to what would be expected

from massive sulphides. Chalcopyrite has been encountered

directly to the south in association with Zone 43, therefore,

if this zone has not been tested, it is a good target.

Zone 46m

Since this zone is not part of a long conductor,

exhibits good conductivity and has some magnetic association,

it is a good sulphide target. Pyrrhotite and pyrite have been

noted in the felsic metavolcanics nearby.

l

l l l l

- 17 -

Zones 47 and 48

Apparently diamond drilling has explained these

moderately strong conductors.. Pyrite and graphite have been

observed in the drill core.

Zone 49

l Pyrite and graphite have been encountered in a

diamond drill hole on this conductor. Therefore, no further

l work is recommended,

l Zone 50

Sulphides could be the cause of this bedrock con-

I ductor with some flanking magnetic correlation. Ground work

is recommended,

l Zone 51

m No further work is suggested on this zone because

it has obviously been explained. Pyrite and graphite have

l been encountered in the diamond drill holes.

Zone 52

g This good conductivity-thickness response does not

l

l

l l l l

appear to have been explained in previous work. Ground work

is warranted.

Zone 53

Ground work is suggested on a medium to low priority

basis on this double conductor zone. Interbedded mafic, inter-

mediate and felsic metavolcanics have been mapped in the vicinity.

l l l l l l l l l l l l l l l l l l l

- 18 -

Zone 54

A horizontal loop survey is suggested on this mul

tiple conducting zone within the rhyolite. Massive sulphides

are expected to be the cause.

D. Watson

ll

APPENDIX

l

&UIPMENT•••••••PHI^^MHBMIMt

The aircraft are equipped with Mark VI INPUT (R)

l airborne E.M. systems and Barringer AM-10^L or AM-101A

m proton precession magnetometers. Radar altimeters are

used for vertical control. The outputs of these instru-

I ments together with fiducial timing marks are recorded

by means of galvanometer type recorders using light

l sensitive paper. Thirty-five millimeter continuous

strip cameras are used to record the actual flight path.

(I) BARRINGER/QUESTOR MARK VI INPUT (R) SYSTEM

The Induced Pulse Transient (INPUT) system is l 1

f particularly well suited to the problems of overburden

— penetration. Currents are induced into the ground by

™ means of a pulsed primary electromagnetic field which

l is generated in a transmitting loop around the aircraft*

By using half sine wave current pulses and a loop of

J large turns-area, the high output power needed for deep

B penetration is achieved.

" The induced current in a conductor produces a

l secondary electromagnetic field which is detected and

measured after the termination of each primary pulse.

g Detection is accomplished by means of a receiving coil

towed behind the aircraft on four hundred feet of cable,

l l l

(ii)

and the received signal is processed and recorded by

l equipment in the aircraft. Since the measurements are

in the time domain rather than the frequency domain

l common to continuous wave systems, interference effects

m of the primary transmitted field are eliminated. The

secondary field is in the form of a decaying voltage

l transient originating in time at the termination of the

transmitted pulse. The amplitude of the transient is,

l of course, proportional to the amount of Current induced

j into the conductor and, in turn, this current is propor

tional to the dimensions, the conductivity and the depth

l beneath the aircraft.

The rate of decay of the transient is inversely

l proportional to conductivity. By sampling the decay

m curve at six different time intervals^ and recording

the amplitude of each sample, an estimate of the rela-

I tive conductivity can be obtained. By this means, it

is possible to discriminate between the effects due to

l conductive near-surface materials such as swamps and

g lake bottom silts, and those due. to genuine bedrock

sources. The transients due to strong conductors such

l as sulphides exhibit long decay curves and are therefore

commonly recorded on all six channels. Sheet-like sur

face materials, on the other hand, have short decay

. curves and will normally only show a response in the

™ first two or three channels.

l

l l

(iii)

l l l l l i l i i i l l lM l l l l

The samples, or gates, are positioned at 260, 480,li.

755 , 1100, 1575 and 2100 mi^rg-^f conds after the cessation

of the pulse. The widths of the gates are 225, 225, 320 ,

410 , 500 and 540 micro-seconds respectively.

For homogeneous conditions i the transient decay

will be exponential and the time constant of decay is

equal to the time difference at two successive sampling

points divided by the log ratio of the amplitudes at

these points.

(II) BARRINGER AM- 104 OR AM-101A PROTON PRECESSION MAGNETOMETER

The magnetometers which measure the total magnetic

field have a sensitivity of 5 gammas and a range from

20/000 gammas to 100.000 gammas.

Because of the high intensity field produced by

the INPUT transmitter, the magnetometer results are re

corded on a time-sharing basis. The magnetometer head is

energized while the transmitter is on, but the read-out

is obtained during a short period when the transmitter is

off. Using this technique, the head is energized for 1.15

seconds and then the transmitter is switched off for 0.15

seconds while the precession frequency is being recorded

and converted to gammas. Thus a magnetic reading is taken

every 1.3 seconds .

li l l l l l l l l l l l l l l l l l

(iv)

DATA PRESENTATION

The symbols used to designate the anomalies are

shown in the legend on each map sheet, and the anomalies

on each line are lettered in alphabetic^

direction of flight. Their locations are plotted with

reference to the fiducial numbers on the analog record.

A sample record is included to indicate the method

used for correcting the position of the E.M. Bird and

to identify the parameters that are recorded.

All the anomaly locations, magnetic correlations,

conductivity-thickness values and the amplitudes of

channel number 2 are listed on the data sheets accom

panying the final maps.

GENERAL INTERPRETATION

The INPUT system will respond to conductive overr

burden and near-surface horizontal conducting layers in

addition to bedrock conductors. Differentiation is based

on the rate of transient decay, magnetic correlation and

the anomaly shape together with the conductor pattern and

topography.

Power lines sometimes produce spurious anomalies

but these can be identified by reference to the monitor

channel.

i i i i i i i i i i i i i i i i i i i

(v)

Railroad and pipeline responses are recognized by

studying the film strips.

Graphite or carbonaceous material exhibits a wide

range of conductivity. When long conductors without

magnetic correlation are located on or parallel to

known faults or photographic linears, graphite is most

likely the cause.

Contact zones can often be predicted when anomaly

trends coincide with the lines of maximum gradient along

a flanking magnetic anomaly. It is unfortunate that

graphite can also occur as relatively short conductors

and produce attractive looking anomalies. With no other

information than the airborne results, these must be ex

amined on the ground,

Serpentinized peridotites often produce anomalies

with a character that is fairly easy to recognize. The

conductivity which is probably caused in part by magnetite/

is fairly low so that the anomalies often have a fairly

large response on channel #1; they decay rapidly, and

they have strong magnetic correlation. INPUT E.M. anom

alies over massive magnetites show a relationship to the

total Fe content. Below 25 - 3(^ f very little or no re

sponse at all is obtained, but as the percentage increases

the anomalies become quite strong with a characteristic

rate of decay which is usually greater than that produced

by massive sulphides.

l (vi)

l *m Commercial sulphide ore bodies are rare, and those

l that respond to airborne survey methods usually have

medium to high conductivity. Limited lateral dimensions

Jj are to be expected and many have magnetic correlation

— caused by magnetite or pyrrhotite. Provided that the

' ore bodies do not occur within formational conductive

l zones as mentioned above/ the anomalies caused by them

will usually be recognized on an E.M. map as priority^

g targets.

l l l l l l l l l l l l

Power Lint Monitor•M^

l

*

4 Input EM * channels

i

EMAmplitudeiOOOp.p.m.

— 500' Radio

— 400* Altimeter

— 500'

Magnetometer Fine Scale 100 Gamma*

Magnetometer Coarse Scale

5000 Gamma

Fiducial Timing Mark

ote.Ml

Anomaly Location

Representative INPUT,Magnetometer and Altimeter Recording

i7^*^?*^'** - ' -y***i-*v#S(*fir-i 'Til '-fit-''" '

CcrUUvO "tkiL

43-izo-Z 43-

45063t3 63

•Z

Z- 933Z-Z-

h

!3

G

A-351

cJM •-if.'.

^^^••^^^;c :4 ~' ^KV/""* '

o.. ,. •-... .j... '..- '

i:f--.'.:i ( :.X.:v-" :-;-H-^ :VV'. L , 4ji ^MiJ'' , '/fJ-'T' .'4 ; ' , .'

?R ^^'^.^jîf.-^-.î.-r-^^v. ; ;-; -i-. ; '' Jr ''' l''i'' "' "

^^^mm^^W * it*l^^^: rv-:/^.?^^.^;^'^-,''- - ffP^!^^

r File.

O GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC.

Type of Survey Airborne Electromagnetic Township or *™-" English TWP. Area ————

CImm SEE ATTACHED LIST

Author of Report———P, Watson.20 Cnnso Road. Rexdale. Ontario

Covering Dates of Survey.

Total Miles of Line cut. —(linccutting to office)

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer—.—Radiometric———Other—————.

DAYS per claim

Geological.Geochemical.

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer____Electromagnetic 40 Radiometric

MINING CLALMS TRAVERSED List numerically

(number)

•fi

.Electromagnetic 40 (enter days per claim)

: July 4.1974 SIGNATURE:.Author^f Report J

PROJECTS SECTION Res. Geol. ———,———

"T

Qualifications.Previous Surveys

Checked by. .date.

GEOLOGICAL BRANCH.

Approved by_L. .date.

GEOLOGICAL BRANCH.

Approved by. -date.TOTAL CLAIMS.

CLAIM HOLDERS LIST

Simon Ouellet Roger Laramee Adrien Cote Luc Proulx Irenee Cyr Pierre Proulx Georges Lacoursieres Roland Sevigny Roland LeBlanc Jos MowattEdouard Morrissette

Fernand Dicaire

AIRBORNE SURVEYS

Type of survey(s) Airborne Electromagnetic

Instrument(s) Induced Pulse Transient System.

Accuracy ________m____________-————.

Aircraft used Shorts Skvvan

Sensor altitude 150 feet above ground.

Navigation and flight path recovery method Radar altimeters,Fiducial Timing by galvanometer type recorders and 35 mm continuous

strip cameras. Aircraft altitude 400 feet_____Line spacing 1/8 mile.

Miles flown over total area 2195 Over claims only 234.5

®*P 36o e

P:

P3bc P3kc P3&1

(S^* S&L

i :^ ^L i.t. inL^^Z

.1

f

/B

Q /B

/A

M M

3e

-^

13

*?t

3&7&&S

-^

2- tt? of Z

327

367 tt

L.

l

3 # W/ .T

^ 3&7/3J i- 387/3ZL 367X 3^ '^ 3&7X3?

^337/36

3^7/4 o 3#7

t. 387

l 307/^3

A1

/Uf

307 /^f

M

M

M

M

/l

M

M

P 36-7/70

P 3^7/77

^307/73

'/76

30*7/79

s-; 119

S W?/0s

03 tt? /g

t. 327/07 L~'fo7J00 L

M

M AT

x//

c

3^7/^7

a

A /Ba/s s

s te

e^ '567200 b ^?071uo/ *?

^7^3

(L) -36732

Z

1-387340

/S

8e e.E Se

t- ^3*73

7 ^^ 8

x^ 3673 ^f

38-7^6

^367^73

f

M.

'3,

3872

387 3V

367 M4

'i-C

X//M*

X//

307 x//x// i x//

ve?

i///3073^-2- 307 &-S

367 aP^P

36'?

7

38-? 3 3B

o

38 7 JUS /vT 2.30734 j///

xv/iX// i

X// //*

b

35^-2-

36.7

307

//--c

^

"7 370 367 37 y

^ 36573-^ 307376 ^3*373-7-7

t 3^7 37^

U. i

3^7

'i ~

^ ^01363 jo

^-36273^-7

3^7 39

3^7 390

307

pp p

t

L "309 ̂ i L "3874 4? "7

L

L. LL

387479

38748*

L ,'

L "36 7487L 387488

L

U 3 87^ f S

6.e

s e

e 8e i e ' s

e666e g

6e

3S7

38)76*716 l

LL 387^10

f,6 se i

L 38-?t ̂ 86734

L

sea 790

n"

X//

CO

eft

f

CH2.AMP1-1

'm1tB

11111111111111111

^ 001A^ 001B

001COOID001E00 IF001Q00 1H002A002B002C002D002E00 3A004A00 5 A006A006B

01 3A

017A020A021A021B022A02 3A02 3B024A024B024C02 5A02 SB025C026A026B026C027A027S02 TC027-0028A028B029A029B029 C029 D029 E030 A030B030C030D030E031A031B031C031D031E031F

898.45898.57898*80898*90899*23899*53899*8?900*40910*29910*52911*039 1 1 * 28911*98891*12925*3494T.03901.03901*50

,

15*39

42*9224.2379.1679.3441*5298*2498*3654.3358*7058.77

121*20121.50125*2771.9076.2376.36

143.19143*39147.40147.6088.7093*05

159.05159*30163*25163*46163*82106*90107*431 1 1 * 69111.79112*90174.23174.401 78 . 69178.82179.05179.20

333443343424332353

2

242343234 .44366444465654455456552566654

6558934829146315

123

l

1524

113346674

1838

5997

268

3915109

20IS

629443840

27

5635233112

2122212422

NC937

NC291

NC

NC3

NC134

NC35252

14196732

H1220

7336766

15S5

NC86

1011

54

0.000.000*000.000*000.00o.oo

900*40910*25910*45

0*000*00

911.800*000*00

947*050*000*00

0*00

0*0024*3078*950*000*000*000*000*000.00

58.800.000.000*000*000*000*00

143.100.000.000.000*00

93.050.00

159.250.000.000.00

106*95107.50111.70

0.00113.10174.15

0*000*000*00

179.000.00

0000000

101010

00

2000

1000

0

02525

000000

10000000

100000

100

15000

501525

06015

000

800

11''iiiiiiiiiiiiiiiii

ANOM

032Al 032B

033A033B033C 033D 033E033F034A 034B034C034D 034E034F035A035B 035C035D035E 035F035G036A 036B 036C036D037A 037B037C037D 037E 037F038A038B 038 C038 D038E 038F 039A039B 039 C 040A040B040C 040D041A041B 041CAAPAW"* C* ri

042B042C 04 3 A043B043C 043D044A044B 044C044D044E

FID CHS CH2.AMP

129.73 6134*48 4 188.64 4188.88 5189.46 4 189.93 2 194*58 6194* TO 6150.77 6 151.12 5151*32 4151*43 6 156.20 3156*50 3203*30 5203*52 5 204*02 4208*94 5209*05 5 209 * 50 5209*67 5166*40 6 166*90 6 171*58 3172*00 6217*47 4 218*00 4218*27 4222*88 4 223*09 5 223*70 3182*21 3182.46 5 182.56 6187*23 2187.50 3 188.00 5 233.32 3233*50 4 237.90 5 197.63 4197.90 4202*75 3 202*93 3211*50 4211.90 4 216.60 4246.84 3247*15 4251*73 4 225.73 5230.40 3230.62 5 231.05 4259.70 4259.87 4 260.03 3260.17 3260*43 3

7837

1010

1 422886 138

15 67

1314 103934 211017 18

732111398

24 25

33 38

26

17 44

38 1316

5 6

3415 1626

15 10

320

669 433

MHOS

13S 2

102

NC 998 59

10 21

128 266 86

15 14

283 134 8 214 6

NC2 4 24 4 34l 124 4233

1046 563 114

MAG VALUE

129.65134*50 188.70

0.00189.30 189.85 194.65o.oo150*75

0.00151.35

0*00 156*05

0*000*000*00

203*65208*85

0.00 0*00

209.60166.50

0*00 171*50

0.00217.60

0.00218.40222.65 223.00 223*80182*15

0*00 0*000*00

187*50 0*00

233.400.00 0.00

197.500.00

202.60 0.000.00

211.75 216*65246*85247*05251*70

0*000.00

230.70 0*000.000*00

260*050*00

260*50

7045

1300

30 15

1000

40 0

1000

25000

20500 0

2020

0 200

030 0

38040 25 4030

0 00

135 0

1600 0

300

60 00

35 18040

20030

00

520 000

10500

260

1111111111111111111

ANGM

044F

045B046A046B047A047B048A048 B049A049 B053A053B

059A068A068B069A069 B069 C070A0708070C070D070E071A071B072A072B072C072D072E073A073B074A074B075A09 6 A09 6B

09 7A098A099A100A101A102A103A104A105A105B106 A107AMA12A12B13A14A16A17A

FID

260.62245*28245.68258.40258*90271*19271*64269.80269.97279.35279.88837*60837.87

861*16921.03924*86984.20984.36988.23933.21933.50937*88937*97938.20996.33996.47945.90946.09949*90951*34951*44

9.009.28

960.65965*69

21*48100.73100.82

166*52113*28181*95125*48199*20137*32216*90152*98234.57234*65169.93252.53288.90219.37219.43307.68237*04254.84354*66

CHS

2343333446432

3236543266655323665222344

5543233644234453234

CH2.AMP

248853363

55779

222

168731

29251395422

3223

8112477

81083233

14362349

123187

MHOS

NC24233326

1222

NC

7NC

212

744

NC1214121111

2NC

7121813NCNCNC

377

21H97

NC47

145

10NC

495

137

NC37

MAG

0.000*00

245*75258.45258*95271*05271.45269*70

0*00279*20279*60

0*00837*90

0*00921*05924*90984*20

0*00988*30

0*00933*55

0*00937*95

0.000.00

996*550.00

946*10950*20951.35

0.000.009.35

960.65965.55

21*500.00

100.85

166*55113*35182*00125*50199*20137.45216*90153*05234.35234.65169.95252*55288.90219.40

0.00307.75237*10254*90354*65

VALUE

0

250250200210340270

0240500

03000

080

190300

025

075

0650

00

10000

401500

75000

150070

24020

01100

1000860560430400500250300250120330490460520

0130

401270800

1-3

1111111111111l11111

,. ANOM

A118A M21A

189 A130A130B131A131B132A138B133A133B133C134A134B135A136A136B137A137BI38A138B

139 AUOA140B141A141B142A142B142CUSA144AU4BU4CUSAUSBU6AU6BUTAUTBUTC148 A148B148CUSD149 A149B149 C150A1SOB153A156A160A161A162A163A163B163C163D

FID

872*98 399.62495*8740 T* 29407*40521.28522.57431*26431*40546*1054T* 1 1548*80451*42454*50573*32478.9548 1 . 50595*30598*02503*43503*52

620*16525*44528 * 52645*50648*30552*89552*99555*32670.85576*07579.85586*49691*90693.20601*13602.62712* TOT12.80714*14625*33626*88627*04629 * 20731*40733*03734.60651.10654.96765.48722*00772.53823*39791.89809.34810*90811.00812.53

CHS

3 45554545324222224555

4435433224322346454433222432223343352

CH2.AMP

3 4B9

11766

103282232l4897

564

1044422

153228

1114

412

67442224622153

1964

142

MHOS

13 96

129496

117

NC4

NCNCNCNCNC

97

1814

797

10923

NCNC

4l

NCNC

28

10119S574

NCNCNC184

NCNCNC

53533

10NC

MAG

273*05 399.65495.70

0*00407*60521.10522.60

o.oo431.60546.00547*30548.80451*60454*65573.20478.9048 1 . 60595.35598.05

0.00503*50

620.20525*25528*55645*55648 * 50

0*00553*00555*45670*95

0*00579*95586*50691.90

0*000*00

602.600*00

712*850*00

625*20626*85

0*00629.20731.25733.05734.90650*80655*05765*40722*10772*45823*50791*80809*25

0*00811*00

0*00

VALUE

11012003000

035002370

3200

10001100

904040

200020

340230380

300

260

250140300360400

0400100280

0100

30300

00

3900

2200

1200700

110150

3012501080

1709590

130180180140

01170

0

1-4

1iiiii

iiiiiiiiiiiiiii

ANOM

164AM64B

165A165B166A166B166C166RA166RB167A171A172A1?3A174 A17*B175A1T5B1T6A1T7A1T7B178A176B179A179B180A180B181A182A182B182C182D183A183B184A18 4B184C184D18 5A186A186B18 7A190A190B190C191A191B191C19SA192B192C192D192E192F192G19 2H19SJ19 3A19 3B193C

FID CHS CH2.AMP

838^88840*40 826*76828*51843.50845*22845*32856.49856.09316.07362.40376.43323*13394.63394.70412*51413*00336*6343). 66431*90347.76353*47450.57450.70364.70364.86475*53382.53362.69382.83383*26496*12496*43400.96401*23401*40401*54517*49419*60419.73540*97456*60457*60465*70590*70591*0659 1 . 50475*95476*47476.74476*88485*99486*16486*24486*34486*64608.41608.77618*30

63646443523266645666564456656535634554233322436523455554642

163

214

32574

17121

252419

510211222

974

335

1224101814

32018

25

109

14563

104245

6724

2347

101112

318

52

MHOS

154

141112

3579

NC7

NC161211

36

129

11111814

61018101511

746

H73673

NC111

NCNC

9155

NC467

119

13683

NC

MAG

838.90840.55 826*75828*50643.50845*25

0.00856*55856*10316*10362*45376*45323*15

0.00394.75

0*00413.05336.65431*75

0*00347*95353*85450*40

0*000*00

365*10475*25

0*000*00

382*80363*30496*00496*30

0*00401.25

0*000*00

517*70419.55

0.00541.10456*65457*75465*75

0*000*000*00

475*900*000*000*000*00

486*200*000*00

486*65608 * SO608*75618*20

VALUE

1150220 500730850750

0560

1000110380180700

01700

01500

701200

0100

14002500

00

8090

00

2080

10090

0200

00

140170

0270

1050370280

000

20000000

120000

50700

50170

11i1111111111111111

ANOM

19 4A%9/lB

194C194D194E 19 5A19 5B196A196B196C196D19 7A 197B197C19 7D 19 7E197F1970197H197J197K198A 198B198C1980199A199B200A200B200C200D200E 200F201A201B201C201D201E201F201Q202A202B 202C202D202E202F20 3A203B203C 203D203E203F203G204A204B204C204D204E204F

FID

496*75497.00498.55508.25508 . 44 648.04649.33518.40519.80530.69530.82667*29 668.05668.14668.62 668.72677*306T7.80679*83680*87661*07542*39 543.06555*07555.24707*83713*39565.70566*16566*59568*60568*93 569*63745.32746.10746*49746.79749.10749 . 38749*73591.64592.44 592.90593.23594*40595*70779.31780.10780*50 78 1 . 78781.91783.50783.90620.33620.70621.04622.47622.66624.14

CH!

44233 2552354 4556222323 3563555233 2333334535 4334233 3533434454

MAG VALUE1-6

15152322

5315

3263799

122252333

1212

3109

1124

1322

118428

143

12943

202934

1144345

1078

4 4

NC 4 7

NC 5 4

NC78

14466

12 NC NC NC

7NC

4 l 9

12 4

11 6 6

NC 2 2

NC 7 l1224749334 3

NC l 7 7 9 7 7 623372

496.750.00

498*500*00

508*50 648.05

0.000.00

519.85 530.70

0.00 667*50

0*00 668*10 668.70

0*00 677*20

0*00 679.70 680*95

0*00 542*25 542*95 555*05 555*25 707*65 713*40

0*00 566*10

0*000*00

568*85 569*55 745*10 746*10

0*00 746*70 748*90

0*00 749.75 591*80 592*40 592*65 593*25 594*20 595*65

0*000*00

780* 350.000*000*00

784.100*00

620.65O.QO

622*300.00

624*10

2500 O

60 O

170160

OO

280150

O470

O900410

O1500

O300130

O200460440100

55800

O410

O O

25002000

253000

O3000

700O

1000200

1200160

3040

3500 O O

4000 O O O

1800 O

900 O

130O

2000

11111l1111111111111

, ANOM

f4G4H

204J80 5A20SB205C205D206A206B206C206D206E206F206G20 7 A20 7B207C207D20 7E207F207G207H20 7 J208A208 B208 C208 D208 E208 F208 G208H208 J209A209 B209 C209 D209 E209 F2IOA210B2IOC2UA2MB211C2I1D211E211F211G21 1HS11J212A212B812C212D21 3A213B213C21 3D213E

FID

624*93625*05625*58813*97816*51816*80818*50650*40650*64650*72650*96652*52656*80657*10838*33847*00847*10848*33852.70852*90854*20854*60855*18682*10682*60682*70682*94684*15689*43689 * 6069 T* 64697*80884*01866*78866*90889*47889.65890*96T15.02716*60721*92911.03911.16912.20912.45918.49921*80924*50924*67928.82751*30755.16755* 80760.70950.60955.24957*94958*18958.33

CHS

45333343334433433323233345343455222236533554642223333643332

CH2.AMP

483244642279664433232637682

103

129522222

2618

39

2312

7164132

10334

15142432

MHOS

912

4271527325314213

NC4

NC312577414

1110NCNCNCNC

210

841982

129

NCNCNC

2341

134314

NC

MAG

0.00625.10625*55813*95

0*00816*90818*70

0*000*000*000*00

652*35656*70

0*00838*35847*00

0.00848.15852.80

0.000*000*000*00

682.050.00

682.700.00

684*200.00

689.80697*70697*85

0*00866*65886.90889.50889*85891*05715.20716*30722.30

0.00911*35

0*00912*50

0.00921.95924.45

0.00928.80751*40755*30

0.000*00

950.900.00

957.900.000*00

VALUE

0110520270

0550200

0000

630150

0290200

0300

600000

100

200

700

160310

500

6050

1504508060

470260

0500

070

03055

0402590

00

1600

5000

1-7

111111111111l111111

ANOM

213F

^213G 21 3HS M A214B214C 2 MD21 /IE214F 21 5ASI SB215C215D21 SE21 5F21 SG 216A216B216C 216D216E216F217ft21TB217C217D 21 ?E2i?F217G217H21 7J218A818B 218C218D218E 218F218Q218H218J218X219A219B 219C2190219E 219F219G219H219J219K219L219M 219N220A220B220C220D220E

FID

960. 58960. T2 961*40765*45786.97789.38 792*60792.87795.99 994.50995*29999.09999*20

0.7-32.492.73

820.00820*15821.82 826.30827.0282T.90

32*3033*2833.9334.09 36.2838.7939*0540*5840*90

855.73856.93 856.13857*60860*00 860*09862.21863*00864*00870.88

60*8861*24 61*4661.5768. 82 69*0969.9270.0977.2677.5077.6077.80 77.98

892.71893.11893.44894.06897*13

CH

33 2223 322 2522335 645 3622656 4434666 443 4563244 442 3S56665 666623

3322222322

1622

1017171323182

4112

38B16 6 8 3

299071241594107

40 4 2 5 43434 10 14 24 23 21 20 17 59 41 13

l 7

l l

NCNCNC

72

NCNCNC

7NCNC

2l9S387

10NCNC102116

5433695337479l

NC 7 4 6 8

NC 2

1011 11 11 106

125

20 11 NC

2

0*000.00

961*50785*60786*65789.35792.70

0.00795.85994*65

0.00999.05

0.000.002.450.000.00

820.300.000.000.00

828.000.00

33.500.00

34.3036.500.000.00

40.550.000.000.00

856.100*000*000.00

862.00863*40

0.00871.05

60*9561*350*000*00

68*600*000*000.000*00

77.550*000*000*000.00

893.050*00

894.10897*15

VALUE

OO

20015

8009020

O1030

10 O

1300 O O

30 O O

45 O O O

35 O

50 O

160130

OO

40 O O O

55 O O O

530310

O12025

100OO

350 O O O O

50 O O O O

80 O

8040

1111111111111111111

ANOM

^leoG220H220J220K221A281B221C221D221E221F2810281H22 1J22 IK82 1L22 1M221N221P222A822B222C222D222E222F2286222H222J222K222L223A223B283C223D823E223F224A824B224C224D224E224F284022 5A88 5B285C885D226A226B226 C286D28 7A227B227C227D227E227F2270287H

FID CHS CK2.AMP

900*13 6 32900.27901*02907.90909.1096.9097.09

105*53105. T3106.22106.40106.50106.67109*78113*69113*92114*13114.50114*63930*53930*70931*07931.39935*08935*23937.80938.20938.70938.80939.18143.30143.63143.83150.38150.60150.87967*07967*58968*03971.70978.80974.33974.801 78 . 28180.13186.50187.80

3*874.184*484.88

214.88815*08215*28218*53883*32883.53283.80823.94

4422324445464366566665253635444434666488558536666244424466

922

11227739

111983

2663232617436814

2172

32277

169

128

1023833119

21

30164

186

27262732

46

1181

11263661

MHOS

1133

NCNC

2NC

22664

1094

1016

310189

168

NC18

2927722323

1912132

NCNC

34

NC80

88101718NC

232

NC4l

8715

MAG

0.000.000.00

907.90o.oo0.000.000*000*00

106*050*000*000.00

109.90113*70

0.000.00

114*400.000.000.00

930.95931*60935*15

0*00937*85

0*00938*65938*85

0.000.00

143*70143*95150*35

0*000*000.00

967.40968.00

0*000.00

974.250.000.00

180.25186*80

0.003*950*000*004*950*00

215*050*000*00

223*400.000*000.00

VALUE

000

2000000

65000

70210

00

60000

55520

300

500

8040

00

2080

1250000

302850

00

13000

4501380

030

00

7800

1000

60000

1-9

1111111iiiiiiiiiiii

ANOM

228 A|B28B

228 C228 D228 E228 F228 G228H228 J228 K229 A229 B229 C229 D229 E229 F229 G229H229 J230A230B230C230D231A231B231C231D231E231F231G231H231J232A232B232C232D232E232F232G23 3A233B233C2330233E233F233G233H234A234B234C234D234E234F234G234H234J235A23 SB235C

FID

41.7342*0542.3842.6042.7943.0043.3947*8050.8451.00

251.03251*18252.14252.48252.63259.06259.28259.48259.8079.0979.4085*8387.33

286*40286*48286*6028 T* 98288.27293.57293*82294.87295.08115*98117.29120.69122.53123.98124.11124*22322*60323*58323*70324.05324*29326*33329*80331*22152*76154*22157*561 59 . 491 59 * 72160*00160*78160*90161*60358.43359.63360*62

CHS

56666642555435645543565663352334454645634456353333644352346

CH2.AMP

16129433243011

214253012

46

208

121298

1934251820

43

11348

103520

930

41212

365

1624

713

4336

558

158

14127

44

MHOS

78

151510

63

NC884229

1048931678

1112

735

NC225283

1349

131576818213262415

NC25

11

MAG

41*800*000*000*000*000.000.000.000*000*00

250*950*00

252*050*00

252*800*00

259*20259*50

0*0079.050*00

85*750*000*00

286*550*000.00

288.400*000.00

294.950.00

116*150*000.00

122.350*000*00

124*250*00

323.350*000*00

324*550*000.00

331.15152.75154.20157.60159.25

0*000*000*00

160*90161*65358*40

0*00360*60

VALUE

40000000000

200

300

5300

20100

250

50000

5000

60000

500

3500

75000

300

9000

72000

302020

180640

000

3010020

090

1'1

111111111111l1111

ANOM

^2350^2 36 A

236B236C236D236E237A237B237-C238A238B238 C239A239B239 C239 D240A240B240C240D240E241A242A24 3A24 3B244A244B245A245B245C245D245E246A246B246C246D24 7A247824?C24 70247C247?2473247H246A248 B248 C248 D248 E248 F249A249 B249 C249 D249 E249 F250A250B250C

FID CHS CH2.AMP

362.84188.49196.19197.00197.33198.16396.73396*92405.10224.70232.58232.92432.56433.03438.75440.98260*32260*49262*64262*80268*43481*97298.70523*40523.56333*22335*00557*38561.00561.17563*03563*33368.95369.40371.30379.40590*30590*42592* 26600.21600*46600.62600*83600*96405*20405*42405*90406*00414*20415*90620*30622*55622.68629*88630*60630*90442.49442*73443.33

25433433663352554556366553626544646465233664556524244656444

31514

43848

3747124

102

1912

71620152

15341912

593

237

91010312326191812

18

10B

402110154726

Q16

249

441331

71062

MHOS

NC7223421

1217

126

NC13

5576

212

1314

682

12NC2512

34

131

125

108

NC11

1310

367

126

NC4

NC97

1257432

MAO VALUE

0*00188*45196*25196*90

0*00198*00396*65397*05

0*00224*85232*50233*00432*50433*10

0*00440*95

0.00260.75

0.000.000.000*000*00

523*150.00

332*900*000*000*000.000.00

563*250*00

369*250.00

379*40590.25

0.00592*30

0.000.00

600.650.00

601*050*00

405*45405*75

0*00414*05

0*00620*45622*55622*80

0*000.00

630.800.000.000*00

020

25060

0703055

030

1503030

1900

1200

10000000

2000

9000000

750

700

30500

57000

1000

150

2050

0840

060

200370

00

15000

1-11

1111111111111111111

ANOM

o5oDîsOE

250F250G250H250J250K250L250M251A251B251C251D251E251F251G251H251J251K251L252A252B252C252D252E252F252G252H252J253A253B253C253D253E253F2530253H254A254B254C254D254E255A255B255C255D255E255F255G256A256B256C256D256E256F257A2578257C257D

FID CHS

443. 49443.83443*92448*30448.80449.27450*80451*86453.27650*72650*90651.60652*23653*08653*18654*57654*80655*08660*18660.33491.90492*10492*27498*30500*10501.13501.97502.77503.16680.88681*43681*67683*38684.74684.93690*23690*38528*62534.50536*18537*65537.93712.79T13.16713*53T15.80716*03721.10721.22566.28566*38572.18574.56575*30575.76742.68T42.93743.60745*37

64423362333335533366654453442233234556532332223454453243432

CH2.AMP

911111

133

232875255

14642

50988725141010

67

11123324

101522421043431325

111912

920

6343632

MHOS

2333

NC14

17NC

22233

105222767525

10173

NCNC

44

NC45

107

1010

2NC

71

NCNCNC

53838

102

NC4763

NC

MAG VALUE

0*000*000*00

448.300.00

449.30450.70

0.000*000*000*000*00

652.50652*90653*40

0*000*00

655*050*00

660*25o.oo0*000*00

49 8. 30499.90

0.00502.25

0*000.000.00

68 l . 400.00

683*500.000.000.000.000.000.00

536*05537*50537.80712*85713*10713*70

0*000*000.000.000.000.000.00

574.60575.15

0.00742.70743.05743.35745*25

000

300

15330

00000

50066090

00

100

20000

2090

050

000

600

110000000

651508050

180900

0000000

60020

02075

500250

1-12

1111111111111111111

ANOM

rt57E*57F

257G257H258A258B258C258 D258 E258F259 A259 B259 C259 D259 E259 F259 G260A260B260C260D260E260F261A261B261C261D261E262A262B262C262D262E262F262G26 2H262J26 3A26 3B263C26 3D263E26 3F26 3G26 3H26 4 A264B264C264D264E264F264G265A265B26 5C265D266A266B266C

FID CHS CH2.AMP

745.93746. 10751.39751.51602.33603.28604*01604.39605.97606.53773.10773.20773.83775.15775.27775.42775.60632*33632.57633.90634.10634.49636.25796.73796.99798.36798.48798*80662*33662.46663*37663.57663*78664*05665*33665*67665*98819*84820*00820*43821*60821*70821*90822*00823*06693*28693*43694* 18694*52694*92696*56696* 80843*60843*96844* 11845*60724*84725. 12725.30

44445254634435666354663334535533466364644444455354364354455

69

101617

213

615

2444

16371420

236

54724

8249

228

1613

67

195511

211

311

41420129

2840149

1653

25636

109

1117

MHOS

5525

12NC

85

107993

108

1110

773

1016

323352481138

142

13599434335727

121

1453

164354

MAG

0.000.000.000*000.00

603.400*00

604*35605*85606*80

0*00773*25774*05

0*00775*25775*50

0*000*000*000*00

634*25634*55636*00796*65

0*00798*15798*45798.95662*35

0.00663.15663*55

0*00663*95

0.00665*55666*20819.75

0*00820.45

0*000.00

821.850.00

822.800.00

693*65694.10

0.00694*85696*65697*10843*75

0*00844*20845*55724*90

0.00o.oo

VALUE

00000

400

2807090

065

11000

190280

0000

80200

1050120

065759020

013040

030

01100

175110

01050

00

600

500

13020

035

130125330

01100

30200

00

1-13

l'1

11111111111111111

wO W ^J

^((•O O M

266F26 7A26 7B267-C267D267E267F268A268B268 C268 D268 E269A269 B269 C269 D269 E269 F269 G269H269 J270A27OB270C27OD270E27OF2700270H270J271 A271B271C271D271E271F271 G27iH271J271K272A272B272C272D272E272F27SG273A273B273C273D273E273F273G273H2 7* A274B

727*06727*50738*22865*70866*00866*62866*84868*99669*15755*77-757*68758.08759.27759.40890.07890*14891*23891.35891.75892.80892.90893*40893.52778.58778.88779.30779 . 52780.74781.13782.58782.72787*17909*69913.73913*93914.90915.02915*20915*30916*52916.70917.23801.66801.89802.22803*29803*63803*98805*239 38 . 50938.80940*00940*10940.50941.38941.65941.77825*04825*23

23363233434566665535534644646663333555545454536543366334633

355

224266876

39745247461523

71419

4101114

42313457612234447

1218

832

612

423

5199

10349

13397

1845

NC34

174

NC334254

24161112

472

1111

33

131991

121082112

1216

8119529452

1311

312

1111

117923

727. 150*00

728*30865.75

0.00866.55

0.000.00

869.10755*55757*70

0*000*00

759.450.00

890*150.000.00

891.95892.75892*90

0.00893.50778.45778.85

0.00779.45780*75

0.00782*60

0*00787*30909.60913*80

0*00914*75o.oo

0*000.000.00

916*750*00

801*750*00

802*15803*30

0*00804*25

0*000*000*00

940*000.00

940.35941*45941*70

0*000*000*00

2300

3080

020

00

410160190

00

1100

13000

1070600

600

1905555

01250

1000

500

8080150

6300000

11000

2600

800190

0600

000

1100

540160180

000

1111111111111111111

. ANOM4

^274D274E2T4F274G27-4H275A275B275C275D275E275F2 76 A276B276C27-6D276E2 77 A277B277C277D277E277F277G27^H278A276B278C278D278E279A279B279C279 D280 A28 OB28 1A28 IB28 1C28 ID28 2 A28 2B28 3A28 3B28 3C28 4 A28 4B28 4C28 4D28 4E28 5A28 SB28 5C28 5D28 6 A29 3A

FID

825.50825*80826*53826*70827*03628*56962*90963*22964*38964*54964*89965*88848.92849.37849.99850.35851.72986.78986.90987.05988.05988.30988.60989. 15989.55873.60873.94874.50874.83876.10

10*4010.5412*4312*60

896*87899.19225.72225*92226*13226.30921.12921.57945.36945*80947.87249.95250.58250*75251.08251.24969.30969.60971.00971*60995*11288.82

CHS CH2.AMP

3 23226624444343456566332334425655334644446664223352323322

423

5814

179

1084

133

141035

81918

342468

201

12511010

339

234B56

68173724

2134

102324

1042

MHOS

21

NCNC1215NC

77742213

1010

78

1142

NC2222

NC5

181010

333

119666

13964

NCNC

326

NC1

NC31

NCNC

MAQ VALUE

825*40 250825*90

0*00826*75827*25

0.00963*00o.oo964.30

0.00964.60965.75849.00849.45850*00

0*00852*00

0*00986*90

0.000*000.00

988.55989.05989.45873.60874.05874.55

0*000.000.000.000.00

12.75896.70

0.00225*70

0*00226.10226.35921*00921.80945*25945.75947*80250*15

0*00250*65251*10251.30969.20969.70971.10971.55995.15288.80

1900

730120

025

040

0530

75420140450

060

030

000

350170410330110400

00000

540200

070

0570

6012090

350190

10470

03008090

24050302015

135

1-15

Same as 253F

1l1 1

1111111111111

t*

*

^ ANOM

7A23C29F 37DX37FX41D 47BX55A9 7 AX102B104B115A122A 128A128B136AX 155A162B198CX 199BX202G207BX209AX 209AY213J214DX216CX231K232EX 233BX235CX243C243D 2 4 SAX246DX256AX 261CX 263J265E265F 267EX2 6 SAX268BX 5fiQRX

FID CHS

962.84098.62164.00 218.45223.31216.90 271.40896.36166.43137.50153.09333.56316.74 382.40382.54475.80 785.45793.50545.89 709.82596.79838.60875.16 875.28965.75792.05820.39295.25123.18 322.93360.36525.39525.56 553.00629.63566.00 797.18 823.24846.60846.76 867.14755.54756.32 891.60

233 243 3243622 222 2422322 223342 2333 243 2 433 242 3

CH2.AMP

132 274 3232912 222 2

1024222 222632 2667 173 2 822 242 3

MHOS

NC77

NC42 1

NC147

11NCNC NCNCNC NC4

NC NC7

NCNC NCNC735

NC NC332

NC44

NC 477

NC4

NC 3

MAG

0.000.00

164.25 0.000.00

217.29 0.00

896.350.000.000.00

333.50316.85

0.000.00

475.90 785.40793.45545.85 709.80

0.000.00

875.20 0.000.000.000.000.000.00

322.750.000.00

525.60 553.00

0.000.00

797.25 823.20846.50846.75 867.35

0.00756.45

0.00

VALUE

00

50 00

100 0

150000

230580

00

20 90

9201600 1700

00

140 000000

1500

60 6500

800 15

11070

15000

550 0

CM

HUTT Twp. M-943

———L—~-H.-l L, i L. l L

353658 1393697L

IL. i

353656 l353S55

293571 t 293570293663 l 298949

9X- - ____U™.

416,780 l .V- Annie

29894L l 298948

293575 l 291998 255464 | 255465293564 l 299423^.:" 299430

2920001 2^92001

413144 |4I3I5I

L. ' L

4 ' 5 " 32004.320.4(3145 ' 413150 1413195

L

299792' 527367 1413146 Ul3K9 .413192 J 4lS I5S

413115 413116 413123 "'3124 ,4I3I3I ——— ———. ^

l 332711 ! 54, 5 l ^N i h

c^r-r/*——~-

413126 |4!3I29 l 413134 1413137 1415142413110 , 413 II 3 '413118 .41312 l-—— - T- - --i — - hL. iL l L. l L L. -.L- "L. i".,

4I3I28\ '413138 UlSI 36413111 i 41 3UZ j4l3H9 1413 120 |*I3IZ7 ^

L i L. i L. (L. i L. L \. * 1 \332739 l 33273.' * l332740 i ^JS* ~^~

L

|4I3\IB8 413169 l3l66 l 4DI73-- .^

413199 1443164 [4131 67 (413172 l 413175

413161 l 413162 j 413169413178 413169 413180 .41*193

30"

47* 50' 35"

MOND Twp. M-870

41P14NG6216 2. ISM HALLIDAY 200

NOTES

400' surface rights reservation along the shores of all lakes and rivers.

- MINING LANDS iDATE OF ISSUE

SEP-3 1874MINISTRY

OF NATURAL RESOURCES

LEGEND

PATENTED LANDPATENTED FOR SURFACE RIGHTS ONLYLEASE

LICENSE OF OCCUPATION

CROWN LAND SALES

LOCATED LAND

CANCELLED

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

HIGHWAY a ROUTE NO.

ROADS

TRAILS

RAILWAYS

POWER UNES

MARSH OR MUSKEG

MINES R

*used only with summer resort locations or when space is limited

TOWNSHIP OF

HALLIDAYDISTRICT OF

SUDBURY

LARDER LAKEMINING DIVISION

SCALE : l INCH - 40 CHAINS (1/2 MILE)DR. R.W.N

DATE . 2,71.PLAN NO. M-910

ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

McArthur Tp. -M. 298

O ro

cu> oen

382747 '382746 |1J402 2 94 4 O 2/2 931 402288 f' ^

83057 ' 83056— — — J- — —

[7.8219 fc, "O" , 59088 D ~ ~VT~ ~ T ~ ~ ~

•m.3827511^ ' S 1 75186 ,\75I85

1357177 382750.,?

English Tp. -M.78741P14NE02I6 2.1514 HALLIDAY 210

K. K.

THE TOWNSHIP OF

BARTLETTDISTRICT OF

TIMISKAMING

PORCUPINE MINING DIVISION

SCALE:I-INCH-4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLEDPATENTED S.R.O.

or (g) C.S.©Loc.L.O.

M.R.O. S.R.O.

NOTES

400' Surface Rights Reservation along the shores of all lakes and rivers.

PLAN NO.-M-262

. ONTARIO


Musgrove Twp. M.304

OJ O)

o.

o(O (Oo

N- 00

.52"5*c

LU

480 Ol' 00"

Bl" 20' 00"

Moher Twp. M. 868

41P14NE0216 2.1514 HALLIDAY 22ORF.K,

THE TOWNSHIP OF

BEEMERDISTRICT OF

SUDBURY

LARDER LAKE MINING DIVISION

SCALE: 1-INCH-4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED

C.S

NOTES

400' Surface Rights Reservation around all lakes and rivers.

Flooding Rights tn Peterlong 8k Kapiskong lakes assigned .'y H.E.P.C. L 0^191 File. No.1162 Vol.4.

DATE OF ISSUE

MINISTRY OFNATURALRKOURCB

PLAN NO . 656

o\T\Rlo


FALLON TWP M.278

--13623(3 362312 382311

l l3BJ2269 1382270,

4- -4 — — i~ - — — —i

[&5.2-? 1?-!- ..-^"i 3a231T l W - 4- - ——— ' i L \7\ l L , L r L l

[ |

Little Nighthowk

Lake

i381B 93 '327427 J3\2\7426 ! 327425 |

, 3799TO iL —— J

Oom

o:h-

UJzo

48*06'06"Approx.

80 056'36"Approx

S TWR M.223

4IPI4NE6216 2.1514 HALLIDAY 230

NOTES

400* surface rights reservation along the shores of all lakes and rivers.

- MINING LANDS iDATE OF ISSUE

AUQ 3 O 1074MINISTRY


LEGEND



CROWN LAND SALES

LOCATED LAND

CANCELLED

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

HIGHWAY i ROUTE NO.

ROADS

TRAILS

RAILWAYS

POWER LINES

MARSH OR MUSKEG

MINES

*used only with summer resort locations or when space Is limited

TOWNSHIP OF

CLEAVERDISTRICT OF

TIMISKAMING


SCALE : 1 INCH - 40 CHAINS (1/2 MILE)DR.

D.KflVANAGHDATE 29/I/7I

PLAN NO. M269ONTARIO


5

l

Q.

(DE(D O)

CD

Bartlett Twp.-M.262

\ IM____

i li^yfe8^75^l /\ /j /V

fflxixi

f- i-;

38TI9B '387197 3BT244

XXX XX XXX

Semple Twp.- M. 1100

O)CO

l ci

N

DM

THE TOWNSHIP OF

ENGLISHDISTRICT OF

SUDBURY ,


SCALE:1-INChM4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LAND "" -LICENSE OF OCCUPATIONMINING RIGHTS' ONLY 'SURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED

c.s.

NOTES

This township l\es within the TEMAGAMI PROVINCIAL FOREST

400' Surface Rights Reservation ar'oynd oil lakes and -rivers.

"". MINING LANDS *DATE OF ISSUE

SEP " 3 1874MINISTRY

OF NATURAL RESOURCES,. i ^*^mf*i*^*i^ "'

PLAN NO.- M.787r IN'T \ T? l r)

MINISTRY OF NATURAL RESOURCESAND MAKING BRANCH

41PI4NE6216 2.15M HALLIDAY

74

1307771 lx)T766 l 30776S 307760 3O7759'

'* ̂ ^30777A 1507769 1^307768 13O776S i 5O7762 |307797* " ~"~ "~

i; !:^.;-}-

Pi v ' (" ' v YS,i;.;':i Y^-'

; ' 1 ''''

1:1 : v,l, : - . y M:''- ;!' : -';:^ ; ^^#.L^,- :T:"tfc:-.^tr;'^1 i'f^- i ; w^ f ! !:t '..;,f;^;;^: V. Y ,4?; S^^Sffilv^^ff ̂ |j|' K^f

,-

PLAN NO

ONTARIO

MINISTRY OF NATURALSURVEYS AND MAPPING BRANCH.

C eaver Twp. McNeil Twp.

McWtmoms•"^

L

Esker Cr. 74755 I37475^_l 374749 ti ~Â"^"7 -^^ ''

374757 (373965 1374731-L r—-f—r- i i i

j l 3739661374738 j i 374752 l

40(299 1401673 , 374019

IL L iL

— ._L K- ~ J L~ I~~~

j^373485 .401298 4OI297 401296

(L , L l

382484 i 382485 1382486

1 Montrose Twp.B. ISM HALLIDAY

THE TOWNSHIP

HINCKSDISTRICT OF TIMISKAMING


SCALE 1-INCH* 40 CHAINS

LEGENDPATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYS POWER LINES MARSH OR MUSKEG MINES

NOTES400 Surface rights reservation around all lakes and rivers.

* MINING UNDTs DATE OF ISSUE

JUL 111974MINISTRY


PLAN NO- M.223ONTARIO

MINISTRY OF NATURAL RESOURCESAND MAPPING BkANCH

O O

Q.

H

UJ-l Q.

UJ (O

ZAVITZ TWP. M-II89

HALLIDAY TWP. M-910

41P14NE621B 2.1514 HALLIDAY 270

NOTES


n A T i- -T •*t™1'* * DATE OF ISSUE

LEGEND



CROWN LAND SALES

LOCATED LAND

CANCELLED

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

HIGHWAY A ROUTE NO.

ROADS

TRAILS

RAILWAYS

POWER LINES

MARSH OR MUSKEG

MINES ^

'used only with summer resort locations or when space Is limited

TOWNSHIP OF

HUTTDISTRICT OFSUDBURY


SCALE : 1 INCH 40 CHAINS (1/2 MILE)DR. R. NOBLE

DATE MAY 5, 7IPLAN NO. M-943

ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BÂNC;

MONTROSE TWP. (M.237)i^T "l 4M. 3 1/2 mV-\^ 3M.

5I/2M

Boot Boy

647388646 'J 358 7 13583

Sifofa L~. iL '36(6994 '366993/366996 .L 1. XL '

MR37Z939 1372941 13316

P 298904 298909

81 M,--293226 ' 293Z2S l 293224

1293217) , 293216 , 293219

367006 4738747385 Z0030

^ 297603129796811297969/1297970

--~ 367007 l 47390 l47389ST-47BB8 316446i T r **W4

L Marshall L 'u- -- -l- -367015 i 367013 l 3617009354172 , 367019 ( 367017

l 297921 l 297920 1/297919 IO40 3OI039 l354173 l 367020 | 367018J.

363531 i 363952 l 363353363524 ' 363523 , 363326

365544 365545 363547-——----"-- ———————r——

363548 l 363649 , 363550 l

MT. COLLINS 1700'

306793 j 306796 j 306797 | 30879B

RAYMOND TWR (M.244)

41P14NE*216 2.1514 HALLIDAY 280

THE TOWNSHIPOF

MIDLOTHIANDISTRICT OF

TIMISKAMING


SCALE: 1-INCH-4O CHAINS

LEGEND


C.S.

Loc.L.O.

M.R.O. S.R.O.

NOTES

400'surface rights reservation along the shores of all takes and rivers.

Areas withdrawn from staking under Section43 of the Mining Act ( R s o mo).

Order NO. File Date DispositionW.44/74 143762 8/8/74 S.R.O.

.DATE OF ISSUE

2 8 1974MINISTRY

NATORALRESOURCK

PLAN NO. M. 23 5

ONTARIO


o*00 l

CL *

Oo

BEEMER TWP. M-656

o o

a. *UJ.jQ.ZUJ CO

81*20'

47*55' 45"

APPROX.

NURSEY TWP. M-I03I

41PMNE02I6 2.1514 HALLIDAY S30

NOTES

400' surface rights reservation along trie shores of all lakes and rivers.

Flooding rights to H.E.P.C. on Kapiskong Laketo contour elevation 113'

L.0.7191 File-1162, Vol.4

T MININGDATE OF ISSUE

SEP *31974MINISTRY


LEGEND

PATENTED LANDPATENTED FOR SURFACE RIGHTS ONLY

LEASE


CROWN LAND SALES

LOCATED LAND

CANCELLED

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

HIGHWAY a ROUTE NO.

ROADS

TRAILS

RAILWAYS

POWER LINES

MARSH OR MUSKEG

MINES *R

'used only with summer resort locations or when space is limited

TOWNSHIP OF 7.-I5H

MOHERDISTRICT OFSUDBURY


SCALE :1 INCH 40 CHAINS (1/2 MILE)DR. R.W. NOBLE

DATE MAR. 31, 71.PLAN NO. M-868

ON i -\KIO


Hincks Twp.

'S M

. .3814^ 3ft7l06 1*87107 38710*

387161 38716

Bannockburn387087J 367(066 (38/70B9 387090 J3870ID .SOIV9IJ J3B1UWI

(387094 1387093 (387092-I- — ———— ~

387137 l^'^^B^~~L . T L^ i u -

^ \^N34 1387135 |3B7I38 .387141 X \—__ . .—. .- . J ___ -__ l ,___ ___1^ __^ ___ * —— \i

i T i i L ' L ^ T~~ ^m* ' VL^ *. w--i *. x i v^x ^

M5JL8"^LI —-u2^ki ~i~ ~ ~ r±~*Ast ii3M1W!360I66-!A^13*0.6

Q.

JDoO

oOD

IM

Midlothian Twp.4IP14NEC216 2.1514 HALLIDAY 300

THE TOWNSHIP OF

MONTROSEDISTRICT OF TIMISKAMING


SCALE : HNCH-40 CHAINS

LEGENDPATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'5 HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINES

C.S.©

Loc.LO.

M.R.O. SR.O.

oj;

NOTES400' Surface rights re&ervation around all takes qnd* rivers.

- MINING LANDS aDATE OF ISSUE

JUL 1 1MINISTRY


PLAN NO- M. 237ONTARIO


FRIPP TWP. M.28I

5M.- -

AM.

inC\J

^

mH LU

3 M.

O O

L - - - -L?™?2 - l P ""l P ~ l i "l.966100 , 366103 l|

ei" 2o'oi"

BEEMER TWP. M.656

48" 06 l?

41P14NE0216 2.1514 HALLIDAY 310

THF TOWNSHIP OF

MUSGROVEDISTRICT OF

TIMISKAMING

PORCUPINEMINING DIVISION

SCALE: 1-INCH 40 CHAINS

LFGEND

PATENTED LANDCROWN LAND SALE

LEASESLOCATED LANDi ICENSf-r OF OCCUPATIONMINING RiCHTS ONLYSURFACE RIGHTS ONLV

ROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYS

POWER LINES

MARSH OR MUSKEGMINESCANCELLED

NOTES400' Surface Rights Reservation around all lakes and rivers.

Flooding R'^hts ( n Peterlong T M'ca lakes attuned to H E P C LO 719!

File 1162 Vj; 4

.MINING IAND5 "DATC OF ISSUE

JUL 1 1MINISTRY

Of NATURAL RBOURCiS

PLAN NO M. 304

ONTARIO


00 CO GO

(T UJX O

ENGLISH TWP. M-787

387056.3^7057L

3BW8

ei 0 12'is"

SOTHMAN TWP. M-II2I

NOTES


. MINING LANDS 9

DATE OF ISSUE

SEP "3 1974MINISTRY


LEGEND

PATENTED LAND

PATENTED FOR SURFACE RIGHTS ONLYLEASELICENSE OF OCCUPATION

CROWN LAND SALES

LOCATED LAND

CANCELLED

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

HIGHWAY S ROUTE NO.

ROADS

TRAILS

RAILWAYS

POWER LINES

MARSH OR MUSKEG

MINES ft

'used only with summer resort locations or when space is limited

TOWNSHIP OF

SEMPLEDISTRICT OFSUDBURY


SCALE ; 1 INCH 40 CHAINS (1 12 MILE)DR. R.W. NOBLEDATE APR. 22, 71

PLAN NO. M-l 100ONTARIO


41PMNE0216 2.1514 HALLIDAY 320

ro O

i ci5 I-

(Din

Semple Twp.-M.liOO

(318550 2 *-x lr ~ - 7 | L~ ~ r fc--.T -V

360469 3804881

3Z758Q l 3678ZO l , 367821

'242422 1242423

1 l l2662891 266288 | 266287

242*05 1242904--Xt^-L7-L nra j 1528*1 ^

- . .1213690 hSothman

299791 299790" 'l 1296936 1896937

4- ILl ' S 1296930 1296939

//.Mining Ac c* 11 RoadFilt No. 126.14 2M

Kemp Twp.-M.966K. Kol

41PMNEW16 2.1514 HALLIDAY 330

THE TOWNSHIP OF

SOTHMANDISTRICT OF

SUDBURY


SCALE:1-INCH^4O CHAINS

LEGEND


NOTES

400* surface rights reservation along the shores of all lakes and rivers.

Flooding Rights- L.O. 7191 File N* 1162 vol. 4.

- MINING LANDS JDATE OF ISSUE

JUL 11 1974MINISTRY


PLAN NO. M-II2I

ONTARIO

MINISTRY OF NATURAL RESOURCE*SURVEYS AND MAPPING BRANCH

THE TOWNSHIPor 'Geikie Twp.( M.

, CAVANA a, WATSON OUS.

iDISTlWGT OFSUDBURY

LARDER LAKE DIVISJON

SCALE: WNCH 4fl

LOCATEDLICENSE ;0F 6CCUPATIQM? MINING EIGHTSSURFACE RlSHTfi ONLY ROADSIMPROVED R&AQS,

1 "i"L0 L 29170* i ̂ s? POWER LINES MARSH ,pR

-^ *w tf

;—Tjr-tL1371,81 /|,'353IW

OFJSSl/E

*3lB7Sr -

-t - '-*\t^ f^L

397321 t387320 3B71OO 367S99 *-

3B7063 l 367064 387N065 - —J ~-

L. ". T. 351322 354315 3S43I6

354321 l 354075 '3^.1317 i ,38l3lt

PLAN NO

Hutt Twp.(M.943)MINISTRY OF NATURAL RESOURCES

SURVEYS AND MAPPING BRANCH

41P14NE0216 2.1514 HALLIDAY

350

"W

l i

4IP14NE0E16 2.1514 HALLIDAY360

•^•KiAfcM-————- m- y i .j .

l52W-~*~.....

MUSG GLISHBEEMERTP

—r"""?1 t'/i', , " ^!;^'*f-;:'^@S

• l ' t***fc.*-~l|lMIIII ^ll n

F

t. '

BEEMER

11PUNE02IB 2.1514 HALLIDAY 370

l.)

X

tr.

S t

4IP14NE0216 a.1514 HALLIDAY

BARTLETT

pie TPi"

380

X fc* ; j

(HJTft'TI

f-*'..,*

S 2 S\**/ —— 00 N

O'. ̂

' jCO ^ CO 2LO JO N GOo o o oCO C\J CM

, i W JO* h . /n?

41P14NE8216 2,1514 HALLIDAY 330•fli^âtMaâ-^f'^JK-iîrfi!^^^ ; ' .-''Will

.VJ.'^ i'. r "j' rf"J ' '• -^--''''-'

fi. -i.il' W Ir," '•l*

T.L293

Z CO 2 CO00 O) O — (MLO If) CD CD CDOJ (M OJ C\J CM

LO COCD COOJ CJ

r:* v*yj®^\^ Sfc'iK"W' *

.1*.

IS) r

cv;

n

4IPI4NE8216 2.1514 HALLIDAY

,' ' l'

400

t

c: f a i m s h e i ci o t hers

l i fir. T'"' Ml' f f *"~-——*"m J —"— .T-j-K**t.A. ..31 .Î ,^ T i^r'Nar I ^- jo-vi-fi

107E I06W

ijjsit, .nMW"i****au.*

E TT

ODm roea : OJ c\i

Documents

AEM SUR FILE NO: 15027