31M04SE0108 2.386 GILLIES010C

OLA8 PUHTON, p. ENO

GEOPHySlCAl, .SURVEYS '

COBALT. ONT

31Me4SE0108 2.386 GILLIES 010

HEI'ORT ON THB VLF AND THE MAGNETIC

GJSOJ HYS1CAL SURVEYS ON THE PROPERTY OF

N1CKKL HIM MINUS LIMITED

1H BLOCKS 83 AND 84, GILLIES LIMIT. ONTARIO

APR 2 91971PROJECTS SECTION

TABLE OF CONTENTS

DIGKST

Location, Area and Accessibility The Land Survey

TtIK GI^LOGY

Geophysical Correlation with the Geology Governmental Maps and Reports Regional and Local Geology Economic Geological Conditions

tJKilCAi, SURVEYS

GeneralThe V1F Method and Procedure for Geophysical

Prospecting The Magnetic Method

Tiih RESULTS OF THB GEOPHYSICAL b

The Maps (numbered 70-72-1. i^ The Results of the VLF Survey" The Results of the Magnetic Survey

CONCUSSIONS AND RECOMMENDATION

f:*

3iM04SEeiee 2.ass GILLIES010C

OLAS BURTON. P. ENO.

SURVEYS

COCALT. ONT

2.see GILLIES 010

KM'ORT ON THE VLF AND TOE MAGNETIC

GKOJr HXS1CAL SURVEYS ON THE PROPERTY OF

NICKEL RIM KINES LIMITED

IN BLOClUi 83 AND 84, QILUES LIMIT. ONTARIO

APR 2 9 1971PROJECTS SECTION

TABLE OF CONTENTS

DIGEST

INTRODUCTION

Location, Area and Accessibility The Land Survey

TilE GI&LOGY

Geophysical Correlation with the Geology Governmental Maps and Reports Regional and Local Geology Economic Geological Conditions

Tiib GKOi: dYSICAJ, SURVEYS

GeneralThe VLF Itethod and Procedure for Geophysical

Prospecting The Magnetic Method

Tlffi RESULTS OF THE GEOPHYSICAL bURVEYS

The Maps (numbered 70*72-1. -2 and j The Results of the VLF Survey The Results of the Magnetic Survey

CUNCUjJSlONS AND RECOKMENDATIOHS

DOUGLAS BURTON, P. ENQ,

GEOPHYSICAL SURVEYS

COBALT. ONT

REPORT ON THE VLF AU) THE MMJNBTIC

GEOPHYSICAL SURVEYS ON THE PROPER1T OF i

MICKEL RIM KIMB8 LIHITEJ) :

IN BLOCKS 83 AND 84, GILUB5 LIMIT* OHTAKIO

pfe-

During fourteen field day* i

October. 1970. magnetic intensities and VLF

were determined on 19.8 miles of taped picket lines in

Blocks 83 and 84 in Qillies UMt township, about eight

miles south of Latchford, Ontario, ty vay of Highway 11.

A number of VLF anomalies are recorded* usually

in the area of the aagnetio basic rook**

Several drill holes are reopmmended in order to

evaluate the geophysical anomalies in terms of sulphide

minerals.

DOUOUAS BUHTON, P.' ENO.

REPORT ON THE y If AN) THS, JftGNETIC,

l-:"

m

Efvvfc

lGEOPHYSICAL SURVEYS ON THE PROPERTY OF

KICKEL RIM MINES LimTED

IN BLOCKS 83 AND 64, GULLIES LIMIT, "oNTA.110

INTRODUCTION

Through the dates Septeaber 3rd to Qjstobej-' H' ." " ' - ' 'i.*-' ' ' \

1970. a Very Low Frequency (VLF) and aphotic geophysical

survey was completed on a 12-olaia group in Blocks 83 and

84 in Gillies Limit township, Ontario.

Mr. Ralph Benner, your consulting geologist, '

arranged for this survey and the line cutting to position

the geophysical observations* He reveiwed the geophysical

results and advised about the correlation into geological

terms and possibilities. Hit cooperation is greatly: -.- ' ",," :: . \appreciated. ."..-'- ' ' k , 1'.;-' ; '-. : .' ''' ;' v'^: ; '-'-;^,;;

Nickel and copper are found south of this area

exandned in an east-west f One along the south contact of

an ultrabasic mass of pyroxenite and anphibOlite. A " r

similar mass is found in the area surveyed and it^was

believed that similar minerals may be found nearby.

The weather was rainy and this delayed the

line cutting the geophysical field work* Black flies

and mosquitoes were absent, but hornets were f*und in

f*..3'- f V

^?*i

- 2 -OOVOUA0

GEOPHYSICAL

nests built about three feet above the ground on brush

and trees. At times these were vicious and persistent r f

Location. Area and Accessibility ? ,

The area surveyed straddles Highway Mo. 11 about' "' ' ' ' ' - "L \ ' " , ' .

eight miles south of .latchford/ Mor^ thanten j'ai Ll "

were covered) an area of about 440 acres,

The Land Survey

The taped and picketed Unas, laid oat, 200 faat,

aj&Ek were brushed out to carry on straight lines, and to

facilitate movement along the lines for the personnel op

erating the geophysical apparatus.

An east-west base line was laic

along the south boundary of Blocks 83 and BU for 6400 feet^•^••^•i^-^-i^-B-M^^iHBBHBMMBBBI^^^^^^^^^^^^-^^^^^^^^^^^^^^^^^^^^^^^B*

with taping pickets every 100 feet. The 32 survey lines :.. - -V-MMMH^W ^-^-••^-^-•iv - . . .. •.-. .' ,. ' "',- ' - '.'"•-''.

were tuned off at right angles every 200 feet and extended•'•- ••"/•. . • .'l :'-'*^f^^^?*ft\??3S;i-'j..'t-- '*

north for about 2700 feet to a second east-west base line

laid out to det,ej^je^fre^aEajiJjBgJE8tw^^ at the;* ' - '\' ' ''~*'-';- -"''' "- '- ' ' ^

north end. In addition six lines WHOP to W5400 were

extended an additional 1000 feet. .s ' -., , - . M w i1 , '^ ,' '--

In total. 19.8 miles of profile line;yere out

and taped and geophysical aaasurenents :were aafle at 5Q and

100 foot intervals. Topographical and geological

were related to these lines.

- 3 ~

oDOUGLAS BURTON. *". ENO

- . GEOPHYSICAL SURVEYS

' ' T. ONT

THE OEOIffiY

Geophysical Correlation with the Qeolojor

Geophysical measurement* act ag la-gid.de to Indicate

hidden geological and mineralogical conditions at depth in an' ' " ! ,- - •'". ' -, 'i Vi ' ."/' ;':' * "";"J - V:v

area considered to be favorable for the deposition of or* '

minerals.: t f. ' - ;- ; -; : \ * V |.) " - 'V "7 T

Geophysical results must be prepared and mapped in

such a way that they may be translated into geological tei*as

and possibilities in order to be of assistance in the explor

ation and testing of a mining prop^Hy. Some {feoloj^al'know

ledge must be available in order to derive the aaxisjum benefit

from a geophysical examination.

Governmental Maps and Report e 'V'V'; '/V'" 1'

- ' ' '-' t-**. "V '. "\ " ' h -' :

There is One map of this area *ith its acoompanying

report. This is the one inch equal* one mile amp entitled

"Map of the Cobalt-Nickel-Arsenic-Silver Area near Lake

Temiskaming, Ontario11 , to accompany the 4th JBdition of ';

Report by Willett G. Miller, Provincial Geologist, in V' r V,. .

Part 2 of the Nineteenth Report of the Bureau of Mines,

1910. . '

An aeromagnetic map, scale one inch (iquals one

mile, covers the area. This ie Sheet 31 - V/k, "Tiaagami11 ,

Geophysics Paper No. 510.

-. i"

•' nji-'./i-'-ii't i p J , .I't.t I 'i;t,'"5 N1 i. ,. ^ 1,1 i'ji.^,1;* ;,.;-i\ . . . , ..-, - i f? .- y., ' .^'.ij.}'

bOUOLAS BURTON. P. ENO

. 4.

The Regional and Local Geology

The basement Keewatin rocks are composed of a series

of acid to basic lava flows with interbedded tuffs and breccias,

These formations have been viciently folded until now they ara ,- -" ' -- " 'i ' ." h -*1 ;-'' '' f . ,."--. f\. , , r l'"' - 7' v " " 4 - s*.

in a more or less vertical attitude. Their strik* is generally

east-west with large variations, and they may tie overfoldfd^ |sf

Masses of magnetic basic rock complicate

In Huronian time Cobalt Series pedia^ntji were laid

down on the erosional surface of the baseBMiftt rocks. Erosion

and glaciation then removed nost of the sediments so that

day we find large windows in these sediments

older rocks. ; . "-, - . . *', ; -'.;V; -. , *-'- . , .'V-"'^''

Younger dikes out across all of t lie older formations" . '••'-" ' *' ' ' ' . ff* k ";

usually with a vertical attitude. In

traced in a more or less straight line

places these .dikes are magnetic. : - ^ -^ , ( ,,

large outcrops of Alg{*n*n A.^

south and west of the area-L aikftiinl nejd ~* Xn

granite outcrops on the pro^ei^w bj|tw*eri -: fll!

The south central portion of, the area exaajned has

-S&.~^ifcf-~

The remainder of the area has outcrops of conglomerate and^^•••••BJHHSMs^B^SMBJSjBVeVBHMlMsVBlpHs^^ " ''^ :*f

greywacke. ' - . :- ;.- : -."- . - ;' "; ' I'-.&i^ffitf^

^..'s&.'MsSy:

- 5 ~ DOUGLAS BURTON. P. Ena

GEOPHYSICAL SURVEYS

COBALT. ONT

"conomic Geological Conditions

About 3000 feet south of the area of the present

survey geological condition* favorable for the deposition of

nickel and copper sulfides are found near the south contact

of the large basic mass on this property.

As a result of geophysical surveys, drilling has

located massive sulfides in a number of places along an east-

vest zone more than 5000 feet long. At this time nickel and

copper values are of less than economic grade,

The present survey covers the northern edge of this

basic mass, and was laid out in order to determine if con

ductive sulfide deposits also occur nearby.

- 6 - DOUGLAS BURTON. P . ENS.

GEOPHYSICAL SURVEYS

COBALT. OUT

THE GEOPHYSICAL

General

Two geophysica^aethodg. are used for this examination,

The Very Low Frequency (VLF) method, made possible by

the development of the RonkaEtt^rgggijej^ is used to indicate

the location of zones of relatively higher conductivity; usually

caused by shearing, faulting, fracturing and conductive sulfide*

in the bedrock.

The accurate recording of the vertical component of

the earth's magnetic field at the surface will show the relative

distribution of magnetic minerals in the underlying bedrock.

This knowledge will assist in the interpretation of the geo

physical data into geological terms and possibilities.

The writer, Douglas Burton, supervised theJyiF

the magnetic field observations .during the course of the

physical exandnation-PJLJ-hiB property,

The VLK Itethod and procedure for Geophysical Prospecting

Many Very Low Frequency (VLF) transmitters are located

all over the world. These transmitters origin&te Morse Code and

pulsed continuous wave carriers. Their particular application

is for world-wide communication with submarines! under conductive

seawater. VLF radiation has.considerable penetration into the

earth.

~ 7 ~ DOUGLAS BURTON. F. ENQ

GEOPHYBICAlr SURVEYS

COBALT. ONT

The radiation is vertically polarized and propagates

radially in straight lines concentrically from, the transmitter.

The radiation is characterized by low path attenuation which is

relatively stable with time,

Changes in the usual propagation pattern of VLF radia

tion are introduced by such factors as land-sea boundaries, and

changes in the ground characteristics. Good conductors in the

earth such as sulfides and graphite cones, and shears and faults

of some considerable dimension, will have a tendency to concen

trate and locally distort VU radiation. Artificial conductors1 " " " * L ' . *

such as pipe lines, fences, electric lines and railroad tracks•' * ' ' " - ' ' f,'-'-'

distort these fields. '•••* - - "' -.' ":- -' " -. *'*- ' : ' -VLF transmissions are most strongly concentrated by

electrically conductive zones with a strike or longitudinal

dimension along the radial path of propagation from each trans

mitter. In order to adequately explore an ftre.it where the strike

of conductive zones nay be at any angle it is advisable to use

two transmitting stations so that the radiation direction is

at right angles in order that the conductive zones may develop

strong anomalous conditions.

The Ronka EKL6 receiver for VIF radiafrien* haa two

directional antenna at right,anslgB,.- It will determine the

dip of the field and the phase difference from point to point

in the area of survey. Usually two transmitting stations arfl-

used for determining these parameters. Readings are usually

~ 8 - DOUGLAS BURTON. P. ENO

GEQPHVSICAL S URVEYS

COALT, ONT

taken at ICO foot intervals along a profile line crossing

the general geological strike of the area examined. Con-

ductive zones are indicated by anomalous dips of the field

in the vicinity, with a vertical orientation directly over

a conductive zone. When the dips are recorded and plotted

on a map the approximate position of a conductive bod/ is

indicated, and possibly the dip of the conductive zone is

shown.

The Magnetic Survey

The recordings are made by means of on accurate

vertical component Eero balance adjusted to a sensitivity of

ten gammas per scale division.

The magnetic intensity at any point on the surface

will usually differ from the average value for the region.

Anomalous intensities are caused by changes in the magnetic

minerals below. The magnetic susceptibility ( of rocks is

generally accounted for by the contained magnetite although

other magnetic minerals such as pyrrhotite may contribute to

the observed intensity.

This method is used for the direct location of

magnetic minerals such as magnetite. Magnetic surveys may

assist in geological mapping. The plotted results, when

compared with the known geological conditions, frequently

yield information for the solution of geological problems,

especially where rook outcrops are hidden by overburden.

- 9 " DOUGLAS BURTON. P. ENS

GEOPHYSICAL SURVEYS

COBALT, ONT

Magnetic anomalies are oftwi found associated with forrtational

contacts and structural features. Dikes and faults nay be

located and traced.

Zones of stronger magnetic intensity indicate con

centrations of magnetite and pyrrhotite. These often accompany

valuable non-magnetic mineral concentrations. On the other

hand lower magnetic intensities nay indicate important zones

of alteration where magnetite is changed to non-magnetic

minerals.

- 10 - . . DOUGLAS BURTON. P. ENQ

',': , ; ', GEOPHYSICAL SURVEYS

COBALT, ONT

THE RESULTS OF THE GEOPHYSICAL SURVEYS

The Maps (numbered 70-72-1. -2 an^ -3)

Accompanying this report are three maps drawn on a

scale of one inch equals 200 feet . On these maps the taped

and picketed north-south lines are shown with their eastHjest

base- and tie-lines^. Lakes, creeks and marked topographic

relief are shown, together with roads and access trails, the

gas pipe line, and mining claim numbers.

Map70-72-l shows the results of the magnetic

examination. The relative magnetic vertical component in

tensity is shown in gammas on the profile lines examined.

Lines of equal intensity are drawn. Areas with less intensity

than 7600 gammas are tinted in red. The contour lines of 9000

gammas and above are colored blue.

In order to avoid continuous repetition in the

mapping of the magnetic results, 50,000 gammas are deducted

from the calculated magnetic intensity.

Maps 70-72-2 and -3 show the results of the VLF

examination from two VLF transmitters with the Konka EML6

receiver. Map 70-72-2 shows the results frcj fl^ Craelc.

Washington to the wegfr, and, Map 70-72-3 shows the results

from Balboa in the Panama Cana^^jfiii^Jt^^hesouthj The dip

of the VLF field together with a quadrature phase difference

has been plotted along the profile lines and distinctively

colored.

- H - - DOUGLAS BURTON. P. ENQ

GEOPHYSICAL SURVEYS

COBALT. ONT

The interpretation of the geophysical results are

shown on all of the maps. Fault nones and dikes a&gnetieally

indicated are shown as well as the conductive cones indicated

by the VJJ1' cross-overs.

The locations chosen for exploration are shown on

all of these maps,

The Results of the VLF Surveys

The VLF radiation from

west, and from ^^Sm^^^^

distorted in a few places to indicate conductive tones. V1F

anomalies have been selected for further exploration by drilling.

The electrically conductive gas pipe line on the east

portion of the property distortsy^the VIF field so strongly

that naturally conductive zones that may be in the ground nearby

are completely masked.

The Results of t he Magnetic Survey

The magnetic intensities in the area surveyed varied

from 5000 gammas to 20,000 gammas with an average value of about

8000 gammas. The large variations are caused 'tjy a mss of mag

netic basic rock in the south central portion of the area. The

greater portion of the property has a magnetic variation between

#000 gammas and 8500 gammas indicating weakly inagnetic rooks

such as greywacke and conglomerate, and granite.

Two locations believed to be worthy of further explora-1 - "' '" " .

tion for sulphides are related to thi strongly |i^gnjtie basic

rock mass.

- 12 -DOUGLAS BURTON, P. ENG

GEOPHYSICAL SURVEYS

COBALT. ONT

CONCLUSIONS AND RECOMMENDATIONS

Three sections have anomalous conductive and magnetic

conditions that are believed should be further tested by drill

ing. The targets selected in the order of their priority are

centered at the following coordinates:

(1) W2600 N550 and west(2) W5500 W)(3} W4700 N2400

These anomalous zones nay be most conveniently examined

by drilling from east to west from drill locations at i

Dip of Hole Azimuth Horie. and slope Direction Distance

(1) W2500 N620 -45* and 65*(2) W5260 N640 -45 e(3) Vi4600 N2540 -45*

240" 285* 220*

250'jibo*250'

350' 420' 350'

600'

When the results of this drilling is available and

combined with the results from the geophysical survey just

completed, further exploration may be recomBHfnfleoV

In the meantime, this report is,

Respectfully

Douglas Burton, Geophysicist

Cobalt, Ontario, October 27th, 1970

lUrvey.Type

4 Township or Area.

ASSESSMENT WORK DETAILS

Magnetoaeter-—-^^-^——-—A separate form is required for each type of tui 31M04SE0188 2.386 GILLIESGillies Limit 900

Chief Line Cutter. or Contractor

John N. FrenchName

Latchfordt Ontario

Party Chief.

AddressDouglas Burton

NameCobalt, Ontario

Consultant.

AddressRalph I. Benner

NameBox 208, Cobalt, Ontario

Address

Geological field mapping by.Name

Address

COVERING DATES

Line Pitting Aug.24th to Sept. 28th, 1970

Sept. 3rd to Sept. 29th, 1970Instrument work, geological mapping, sampling etc.

Sept. 30th to Oct. 7th, 1970

INSTRUMENT DATA

Make, Model and Tyr V***. Component-Zero Bal.

Scale Constant or activity 10 g*"""* P** *cale divisionOr provide copy of instrument data from Manufacturer's brochure.

1056

Radiometric Background Count

Number of Stations Within Claim Group

Number of Readings Within Claim Group

Number of Miles of Line cut Within Claim Group 19 f 6

Number of Samples Collected Within Claim Group """

1056

CREDITS REQUESTED

Geological Survey

Geophysical Survey

Geochemical Survey

April 23/71 SIGNED

20 DAYSper claim

40 DAYS per claim

D

- Includes (Line cutting)

Show Check^

MINING CLAIMS TRAVERSED _____List numerically ^^^

L-263912

263913

263915

.2639jL6.,

.JMftftW,

263918****i*********i

263919*••••••••••••*i

263920*fti**********i

263921

part of 265341rk 1 1 * * * * i 1 * * * * t f * * * * * * 411 AuHf 1111 i

part of 265342

TOTAL *~!T ATMS 12

Send in Duplicate to:FRED W. MATTHEWS , SUPERVISOR-PROJECTS SECTION DEPARTMENT OF MINES fc NORTHERN AFFAIRS WHITNEY BLOCK QUEEN'S PARK TORONTO, ONTARIO

Performance and coverage credits do not apply to airborne surveys

SUBMISSION OF GEOLOGICAL, GEOPHYSICAL AND GEOCHEMICAL SURVEYS

AS ASSESSMENT WORK t ! ' *

In order to simplify the filing of geological, geochemical and ground geophysical surveys for assessment work, the Minister has approved the following procedure under Section 84 (8a) of the Ontario Mining Act. This special provision does riot apply to airborne geophysical surveys. -. i i ^

If, in the opinion of the Minister, a ground geophysical survey meets the requirements prescribed for such a survey, including:

. .L -. ' ; . , :. . . , : -'i. '...'-' .

(a) substantial and systematic coverage of each claim(b) line spacing not exceeding 400 foot intervals(c) stations not exceeding 100 foot intervals or(d) the average number of readings per claim not less than 40 readings

it will qualify for a credit of 40 assessment work days for each claim so covered. It will not be necessary for the applicant to furnish any data or breakdown concerning the persons employed in the survey except for the names and addresses of those in charge of the various phases (linecutting contractor, etc.). It will be assumed that the required number of man days were spent in producing the survey to qualify for the specified credit. - -- - . :v

Each additional ground geophysical survey using the same grid system and otherwise meeting these requirements will qualify for an assessment work credit of 20 days.

A geological survey using the same grid system, and meeting the requirements for submission of geological surveys for maximum credits will qualify for an assessment work credit of 20 days. If line cutting has not previously been reported with any other survey and is reported in conjunction with the geological survey a credit of 40 days per claim will be allowed for the survey. *

Similarly, a geochemical survey using the same grid system with the average number of collected samples per claim being not less than 40 samples, and meeting the requirements for the submission of geochemical surveys for maximum credits, will qualify for an assessment work credit of 20 days. If line cutting has not previously been reported with any other survey and is reported in conjunction with the geochemical survey a credit of 40 days per claim will be allowed for the survey.

Credits for partial coverage or for surveys not meeting requirements for full credit will be granted on a pro-rata basis.

If the credits are reduced for any reason, a fifteen day Notice of Intent will be issued. During this period, the applicant may apply to the Mining Commissioner for relief if his claims are jeopardized for lack of work or, if he wishes, may file with the Department, normal assessment work breakdowns listing the names of the employees and the dates of work. The survey would then be re-assessed to determine if higher credits may be allowed under the provisions of subsections 8 and 9 of section 84 of the Mining Act.

If new breakdowns are not submitted, the Performance and Coverage credits are confirmed to the Mining Recorder at the end of the fifteen days.

Type lurvey.

ASSESSMENT WORK DETAILS

Electromagnetic_^__^

Township or Area.A separate form is required for each type of lurvey

Gillies Limit

Chief Line Cutter, or Contractor

John N. FrenchName

latchford, Ont.

Party Chief.Address

Douglas BurtonName

Cobalt, Ontario

Consultant.Address

Ralph I. BennerName

Box 208, Cobalt, OntarioAddress

Geological field mapping by.Name

Address

COVERING DATES

Line fitting August 24 to September 28. 1970 JField Sept. 3rd to Sept. 29th, 1970

Instrument work, geological mapping, sampling etc.Sept. 30th to Oct. 7th. 1970——————

INSTRUMENT DATA

Make, Model and Tyr Honka Mk 16 (VI**)

1056

Scale Constant or Sensitivity—————————————— Or provide copy of instrument data from Manufacturer's brochure.

Radiometric Background Count

Number of Stations Within Claim Group

Number of Readings Within Claim Group

Number of Miles of Line cut Within Claim Group 19*6

Number of Samples Collected Within Claim Group ——————

2112

CREDITS REQUESTED

Geological Survey

Geophysical Survey

Geochemical Survey

nATF April 23/71

20 DAYS per claim

D

D

D

40 DAYS per claim

••-- Includes (Line cutting)

Show Check/

SPECIAL PROVISION CREDITSfor

PERFORMANCE fc COVERAGE

" MM HH Alv* * *,^i,* ••••^•••••••i(******it*i*

263914 t*fr*Y*nKnmii*iti**"*4**i**i***4*****i*****

.263815

Mm6,..;U.L263917

263916

263919

263920

••••••**t*B

'

TOTAL rr.ATMS 12

Send in Duplicate to:FRED W. MATTHEWS SUPERVISOR-PROJECTS SECTION DEPARTMENT OF MINES Se NORTHERN AFFAIRS WHITNEY BLOCK QUEEN'S PARK TORONTO, ONTARIO

i

Performance and coverage credits do not apply to airborne surveys

4,*.

SUBMISSION OF GEOLOGICAL, GEOPHYSICAL AND GEOCHEMICAL SURVEYS

AS ASSESSMENT WORK -

In order to simplify the filing of geological, geochemical and ground geophysical surveys for assessment work, the Minister has approved the following procedure under Section 84 (8a) of the Ontario Mining Act. This special provision does not apply to airborne geophysical surveys. i -

If, in the opinion of the Minister, a ground geophysical survey meets the requirements prescribed for such a survey, including:

(a) substantial and systematic coverage of each claim(b) line spacing not exceeding 400 foot intervals(c) stations not exceeding 100 foot intervals or(d) the average number of readings per claim not less than 40 readings

it will qualify for a credit of 40 assessment work days for each claim so covered. It will not be necessary for the applicant to furnish any data or breakdown concerning the persons employed in the survey except for the names and addresses of those in charge of the various phases (linecutting contractor, etc.). It will be assumed that the required number of man days were spent in producing the survey to qualify for the specified credit. 5 - "t" * "

Each additional ground geophysical survey using the same grid system and otherwise meeting these requirements will qualify for an assessment work credit of 20 days.

A geological survey using the same grid system, and meeting Ae requirements for submission of geological surveys for maximum credits will qualify for an assessment work credit of 20 days. If line cutting has not previously been reported with any other survey and is reported in conjunction with the geological survey a credit of 40 days per claim will be allowed for the survey.

Similarly, a geochemical survey using the same grid system with the average number of collected samples per claim being not less than 40 samples, and meeting the requirements for the submission of geochemical surveys for maximum credits, will qualify for an assessment work credit of 20 days. If line cutting has not previously been reported with any other survey and is reported in conjunction with the geochemical survey a credit of 40 days per claim will be allowed for the survey.

Credits for partial coverage or for surveys not meeting requirements for full will be granted on a ro-rata basis.

If the credits are reduced for any reason, a fifteen day Notice of Intent will be issued. During this period, the applicant may apply to the Mining Commissioner for relief if his claims are jeopardized for lack of work or, if he wishes, may file with the Department, normal assessment work breakdowns listing the names of the employees -and the dates of work. The survey would then be re-assessed to determine if higher credits may be allowed under the provisions of subsections 8 and 9 of section 84 of the Mining Act.

If new breakdowns are not submitted, the Performance and Coverage credits are confirmed to the Mining Recorder at the end of the fifteen days.

25 ADELAIDE ST. WESTSUITE 416

TORONTO l, CANADA

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