GEOLOGICAL REPORT ON THE VANESSA NORTH GROUP, ONTARIO … · 1. GEOLOGICAL REPORT on the VANESSA NORTH GROUP, ONTARIO Introduction A geological mapping survey was completed on claims

52JetSW8*eS Saj02SEee49 SESEGANAGA LAKE 010

GEOLOGICAL REPORT

ON THE

VANESSA NORTH GROUP, ONTARIO

by

Owen L. Younge

August 7, 1971

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TO FOLLOW

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1.

GEOLOGICAL REPORT

on the

VANESSA NORTH GROUP, ONTARIO

Introduction

A geological mapping survey was completed on claims held by

Amax Exploration, Inc., referred to as the Vanessa North Group, in the

Seseganaga Lake Area of Northwestern Ontario.

Outcrop mapping was done on a one inch to 400 foot scale

during the period June 15th to 30th, 1971. Use was made of picket lines

and baseline which covered the claims. Outcrop is very sparse within

the 8 claims.

Object of the survey was to detail the geology of the claims as

an aid in interpretation of previous geophysical surveys in order to

locate and evaluate any base metal deposict which may exist there.

The Vanessa North Group consists of 8 contiguous unpatented

mining claims numbered as follows:

Pa 226387 Pa 226391Pa 226388 Pa 226392Pa 226389 Pa 226393Pa 226390 Pa 226394

Location and Access

The Vanessa North Group of claims is located approximately 64 air

miles west of Sioux Lookout on Vanessa Lake in the Seseganaga Lake Area

(see Location Map).

Access to the property is most convenient via float or ski-

equipped aircraft to Vanessa Lake from Ignace, about 70 miles to the South-

west on the Trans-Canada highway.

Previous Work

No record of previous assessment work is known to the writer.


GEOLOGICAL REPORT

on t h*

VAKESSA ttORTH CROUP. OKTARIO

Introduction

A geological Mapping survey was completed on claims held by

Aaax Exploration, Inc. , referred to at tba Vaaaaaa Horth Croup, In the

Seseganaga Lake Area of Northwestern Ontario.

Outcrop mapping vaa done on a one Inch to 400 foot scale

during the period June 15th to 30th, 1971. Die vat made of picket linea

and a baseline wblch covered the claims. Outcrop i t very nparse within

the 8 clalsis.

Object of the survey vat to detail the geology of the clalsis aa

an aid lo interpretation of previous geopbyalcal surveys in order to

locate and evaluate any base Metal deposit* which auy exist there.

The Vaaessa Borth Group consists of 8 contiguous uapaeeated

Inlng claims numbered as follows:

Pa 226387^ Pa 226391 "'Pa 22638f ̂ Pa 226392 *'Pa 2263*9 M P* 226393*tPa 226390 - ^ Pa 226394"*

Location and Access

The Vanesaa Borth Croup of claim Is located approxinately 64 air

iles west of Sioux Lookout on Vanessa Lake In the Seseganaga Lake Area

(see Location Map).

Access to the property Is vost convenient via float or ski-

equipped aircraft to Vanessa Lake fro* Ignace, about 70 miles to the South-

west on the Trana-Canada highway.

Previous Work

No record of previous assessment work is known to the writer.

2.

Topography and Drainage

Most of the claims area is covered by a large outwash sand

plain which forms a shallow bay with sand bottom to the south and lines

the shore with a narrow sand beach. Together with an alder swamp lining

a creek which drains into a small lake to the north, this sand plain

almost completely covers the rocks.

Relief is low and gentle in the claim group.

Geology

The rare outcrops are confined to the southwest corner of claim

226389 and close to the baseline in the southeast corner of claim 226388.

The rocks which outcrop are all basic metavolcanics.

The basic metavolcanic rocks are schistose, aphanitic or fine

grained, dark green to grey on the weathered surface. They have a chlorite-

hornblende-biotite-feldspar matrix. The strike of the schistosity is ap

proximately N20 0 and dips 76 0 to 83 0 West.

There is some jointing in the metavolcanics. Joints are 070 0

strike and 80 0 North dip.

In the bay just northeast of our claims, there is a large outcrop

of basic metavolcanic rocks. Most of the claims are overlain by sand and

sandy boulder overburden of an old outwash plain.

Mineralization

There are no visible exposures of sulphide mineralization in the

rare exposures seen on the claims.

Conclusions

Lack of rock exposure made correlation with the EM and magnetometer

surveys previously done on the claims, impossible.


TO FOLLOW

Topography and Drainage

Mott of the dal** area l* covered by a large oucwaah aand

plain vhlch forme a hallow bay with aand bottom to tha aouth and line*

tha shore with a narrow aaad beach. Together with an alder swamp lining

a creek which drains Into a avail lake to the north, thia sand plain

almost completely cover* the rocks.

Relief la low and gentle In tbe claim group.

Geology

The rare outcrop* are confined to the aouthwent corner of claim

226389 and cleat to the baseline In the southeast corner of claim 22*388.

The rocks which outcrop are all basic metavolcanlcs.

The basic metavolcanlc rocks are acblstoae, aphanitic or flne-

gralaed, dark green to grey on the weathered surface. They have a chlorite*

hornblende-blotIte-feldspar matrix. The strike of the schistosity la ap

proximately K200W and dips 760 to 830 West.

There is some jointing In the matavolcanlcs. Joints are 0700

atrlke and 80O Worth dip.

In the bay Just northeast of our claims, there la t l arge outcrop

of basic metavolcanlc rocks. Host of the claims ara overlain by sand end

aandy boulder overburden of an old outwash plain.

Mineralisation

There are no visible exposures of sulphide mineralisation in the

rare exposures see* on the claims.

Conclusions

Lack of rock exposure made correlation with the EM and magnetometer

aurveya previously done on the claims, impossible.

Reconunendations

Because of the lack of outcrop, it is recommended that a geo

chemical soil survey be carried out on the Vanessa Group claims

Pa 226389 and 26388 West of the baseline, in order to try and

interpret conductor zone 'A 1 and its possible extension to the south.

August 7, 1971 Owen L. Younge Geologist.

Ree ndttlons

of the lack of outcrop, it la recoMeoded that a veo-

chewical soil survey be carried out on the Vanenaa Croup cUias

Pa 226392, 226389 and 226383 West of the baseline, in order to try and

Interpret conductor lone 'A' and its possible extension to the south.

August 7, 1971..

. TfoOven L. Tounge , Geologist.

52J*1SWe005 52jei2SEe049 SESEGANAGA LAKE 020

REPORT ON

CRONE RADEM GEOPHYSICAL SURVEY

VANESSA NORTH GROUP

SESEGANAGA LAKE AREA

DISTRICT OF THUNDER BAY

PATRICIA MINING DIVISION, ONTARIO

Amax Exploration, Inc., Room 204, 231 Arthur St., Thunder Bay (P), Ontario, August 16, 1971

J.E. Steers,


TO FOLLOW

XZPOHT OH

CROC tADCM CEOPBTSICAL SUtVKT

RECEIVED

AUS l 9 1971PROJCCTS SECTION

VAVISSA VOfTB GtOOP

SSSCCABAGA LAB AHA

DisnicT or nuvKi BAT

PATRICIA KIVZVG D IT IS I OB, ONTARIO.

Aaax Exploration, Inc., too* 204, 231 Arthur St., Thunder Ety (P), Ontario, August 16, 1971.

J.E. Statra.

Introduction

During the period from May 31st to June 4th, 1971, linecutting

and a Crone Radem VLF Survey were carried out over a group of 8 contiguous,

unpatented mining claims, numbered as follows: Pa 226387, 226388, 226389,

226390, 226391, 226392, 226393, 226394, registered in the name of Amax

Exploration, Inc., Suite 1302, 7 King St. E., Toronto, Ontario.

Linecutting was only carried out over 4 claims: Pa 226387 - 226390

inclusive. Linecutting on the remaining 4 claims was carried out during the

winter of 1970 and was previously reported.

Location and Access

The claim group is located on the West shore of Vanessa Lake and

is shown on O.D.M. Plan Seseganaga Lake, District of Thunder Bay, Patricia

Mining Division, Ontario.

Most convenient access is by float or ski-equipped aircraft from

either the Town of Ignace or Sioux Lookout, Ontario.

The group is approximately 70 miles Northeast of Ignace and 60 miles

East of Sioux Lookout.

Previous Work

To the writer's knowledge, the only previous work of record is a

magnetometer and Crone JEM Survey performed during the winter of 1970 on

the southern four claims.

Numerous pits in the area attest to previous prospecting years

ago, but no written record of the work is available.

Instruments Used S Sruvey Method

The entire survey was carried out with a Crone Radem VLF receiving

unit utilizing the transmitted field from Balboa, Panama as the primary

source.


TO FOLLOW

lctroductlop

Durfcjc th* period fro* M*y 31it to June 4th. 1971, Unecuttin*

and t Crone E* d e* VLF Survey ve r* carried out over a *roup of P contiguous,

unpatented mining claims, numbered as follows: PA 22*3*7? 2263P? 1 '' 2263*9, '(

22f390, 226391, 226392,' 226393',' 226394, registered In the ne*e of Amax

Exploration, Inc., Suite 1302, 7 King St. E.. Toronto, Ontario.

Linecutting was only carried out over 4 claisis: PA 226387 - 226390

Inclusive. Linecutting on the revaluing 4 claims was carried out during the

winter of 1970 and wss previously reported.

Location and Access

The claim group la located on the Vest shore of Vanessa Lake and

Is shown on O.D.M. Plan Seseganaga Lake, District of Thunder Bay, Patricia

Mining Division, Ontario.

Most convenient access la by float or aki-equipped aircraft frosi

either the Town of Ignace or Sioux Leokout, Ontario.

The group la approximately 70 miles northeast of Ignace and 60 miles

East of Sioux Lookout.

Previous Verk

To the writer's knowledge, the only previous work of record is a

magnetometer and Crone JTM Survey performed during the winter of 1970 on

the southern four claims.

Numerous pits in the *rea attest to previous prospecting years

ago, but no written record of the work la available.

Înstrument Used t, Survey Method

The entire survey was carried out with a Crone lad** VL7 receiving

unit uttltilng the transmitted field from Balboa, Panama as the primary

source.

Base stations were established along a northerly-bearing base

line.

The dip angle and the horizontal component of the magnetic field

were read at 100-foot intervals (closer station spacing was used in anomalous

areas).

The dip angles are plotted on the accompanying map in annotated

profile form and a map of the horizontal component of the magnetic field is

presented in contour form. Utilizing control stations established on the

baseline, all the horizontal field strength readings were corrected for

drift.

3. l miles of line were cut and 409 stations established. 818 read

ings were taken.

Survey Results

5 distinct conductive zones, labelled A to F inclusive on the

accompanying map, were delineated.

All conductive zones have magnetic association; however, no zone

is exposed. It is likely that all zones are caused, at least in part, by

sulphide mineralization.

Since none of the zones outcrop, further work, prior to drilling

is warranted.

Summary and Conclusions

Five zones which may be in part the result of sulphide mineraliz

ation were delineated.


TO FOLLOW

last stations ware established along a northerly-bearing base-

The dip angle and tbe borisontal component of the magnetic field

were read at 100-foot intervals (closer station spacing was used in anomalous

reas).

\~~ Tbe dip angles are plotted on tbe accompanying map in annotated

v profile fora and a map of tbe horlsontal component of tbe magnetic field Is

\ presented In contour fens. Utilising control stations established on the

baseline, all tbe borisontal field strength readings were corrected for

drift.

3.1 miles of line were cut and 409 stations established. 818 read

ings were taken.

Survey Jesuits

3 distinct conductive sones, labelled A to r inclusive on tbe

accompanying map, were delineated.

All conductive sones have magnetic association; however, no s one

is exposed. It Is likely that all comes are caused, at least in part, by

sulphide mineralisation.

Since none of the sones outcrop, further work, prior to drilling,

is warranted.

Summary and Cone 1usions

yive sones which may he In part the result of sulphide mineralis

ation were delineated.

It is recommended that the area receive careful geological

mapping and soil geochemis-ry before consideration is given to testing

the zones by diamond drilling.

Respectfully submitted,

Thunder Bay, Ontario August 16, 1971

J.E. Steers, FGAC, P. Eng, Geologist.


TO FOLLOW

It Is recos**e*ded that the erea receive careful

mspîan cod toil geochemistry before consideration is niven to testing

the soaes by d i Mond drill las.

.C '.t f r ,. ^V, * f-.-- - —".'-.l,. * le spect f itHT^fObtil 11 ed,

Thunder Rey, Ontario, August 16, 1971.

J.E. Geologist.

C, P.Eng.

sajeisweees ssjesssewa SESEGANAGA LAKE 300 I'KRlORMANCr. fc COVI.KAf.K CRI.DIIS

ASSI.SSMKNl WORK ni.TAIl.S

.ivnship o, \,,M Seseganaga Lake '-"' """-",alh

Tvpe ot Sm-vi-K GeologicalA M-|urjif lorm is rrtjiiirrd lor rjct) H |'i i'l 'urvrs

Chief Line Cutteror Contianor N"'nr

. \ddrctt

Partv Chief Owen Young*, HSeN.irm-

166 Metcalfe Ave. . Carton. OntarioAddress

Consultant J. E. SteersAmax Exploration, *W6. ,

204 -231 Arthur St., THUNDER BAY (P)j Ont.Address

CO VK R INC, DA I K S

Line Cuiiiiu'

Kidd J""* 5th - Bth, 1971Insinttnrn! \vnrk, ^c'olopital m.ipping, jumpling r t c.

Offirr

1

INSTRl'MKNT DATA

Make, Model and Tvpe.

Scale Constant or Sensitivitvf'r firni'irlr cn/'y of instrument ilnla f mm \\aniiliiclnrcr' x I'tncl'iirc.

K-ifliiimi-lrir li irl m i uinil fniint

Number of Stations Within Claim Group —————————

Number of Readings Within Claim Group —————————

Number of Miles of Line cut Within Claim Group

Number of Samples Collected Within Claim '",roup , ,, , , ,

CRF.DITS RKOl'KSTKD 20 DAYS -10 DAYS Includesper claim per claim H.ine cuttingJ

Geological Survey SO CD

Geophvsical Suivcy CD CD show 1 ' Check y

:ochemical Survey 1 i Î*-r—~'~Q-^/Tv*tfr "AV\ /v1 S —— "- , \

.MVTK June 21. 1971 f p S, ' - J'

Kir-.vi.-i> f '-:^-:;\ ( . f 'i ,V J

' 1 226387

226388

*\*t f. IQn..2.2.6382............. .......,.............................

226390

226391

226392

226393

226394

*

•-•-•-R^C-SW-ii^---------"..............AUe..V8.192A..........................

PROJECTS.....................ste.TlON...............................

THTM 8

Send in duplicate lo: fXI.D W. M.VnilKWSsfi'i.itMsoi'. I'Ko.ji.crs si.cnoNDI.I'Al: IMI.XI 01 MI.M.S K: NOKllll.RX A FI- AIRS uiniMY I;I.*K:K ijl'l I.X'S I'\KK lOIUiMO. ONTARIO

j:^?5

5V

1

IM.RIORMANCK fc COVKRAGI. CRF.DHS

ASSESSMENT WORK DETA11.S.

li.\\nship or Ate:! Seseganaga Lake

Type of Survey Rade* "VLP" ElectrojCjiagLetic——————A sriuratr l orin is rnitiirrd tot r.irh type nl survrv

Chief Lino Cmi.-r R.J. Penney or Contractor N.inic

Inglevood Creac. , Thunder Bay "P".Addre.s

Partv Chiof R. J. PenneyNjmr

•t aboveAddress

Consultant J.E. Steera.Amax Exploration, Inc.204 - 231 Arthur St., THUNDER BAY (P). Ontario.

Address

COVKRIXC DATES

Line Cm t inc. 31 " -*upe 3' incl * 1 971

Field June 4. 1971Instnimcnt work, geological mapping, sampling etc.

orfirp June 14. 15, 16. 1971.———————————

INSTRUMENT DATA

"* Make, Model and Typr Crone Radea "VLF"

Scale Constant or Scnsitiviiv, JL l

409

Or p rovide (~op\ nj instrument itatfi /ror: 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 Chshn Group————i..

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

818

CRF.nrrs RKOUF.STED

Geological Survey

Geophysical Survey

Geochemical Survey

20 DAYS per claim

a40 DAYS Includes per claim (Line cutting)

nShow Check J

DATE 1971

SIGNEDRote:- lines cut on 226387 to

MIXING CLAIMS l RAVF.RSF.D List riiimcrit .illv

226387

226388

40 day*

40

226389

226390

40

40

226391 - 20

226392 20

226393 - 20

226394 - 20

) i ' ' :'i '\uii 20 rf c^'.- ' ' ^tfcv, f/i** -i^r

TOTAL 8 claias - 240

Send in duplicate lo:JUKI) W. MA'IT!IK\\'S SL'I'ILRX'ISOK-l'ROH.CrS SUCTION DKI'ARTMtNT OK MINKS 8: NOKTIir.KN AFFAIRS WIHTNKY IJI.OCK QL'KF.N'S PARK TORONTO. ONTARIO

C, -line cutting on 226391 to 226394 previously

CRONE GEOPHYSICS LIMITED

Nth ...:,-;.?:; Effective Ju;io l

Phone: 270-0096 UNTIL l;-;EN USE

973 La:.cch:.-c w. EastP " - 1 f* i *. * vi i orcj.t (hiTia

3607 WOLFEDALE ROAD, MISSISSAUGA, ONTARIO, CANADA.

FIELD STRENGTH meter

BATTERY test and "STEADY" or "KEYED" signal switches

INCLINOMETER

FIELD STRENGTH range switch

VOLUME CONTROL ON-OFF switch

STATION SELECTOR switch

BATTERY COMPARTMENT (inside)

- CONDUCTOR DIRECTION ARROW- SPEAKER

This is a rugged, simple to operate, ONE MAN EM unit. It can be used without line cutting and is thus ideally suited for GROUND LOCATION OF AIRBORNE CONDUCTORS and the CHECKING OUT OF MINF.RAL SHOWINGS. This instrument utilizes higher than normal EM frequencies and is capable of detecting DISSEMINATED SULPHIDE DEPOSITS and SMALL SULPHIDE BODIES. It accurately isolates BANDED CONDUCTORS and operates through areas of HIGH HYDRO NOISE. The method is capable of deep penetration but due to the high frequency used its penetration is limited in areas of clay and conductive overburden.

The DIP ANGLE measurement detects a conductor from a considerable distance and is used primarily for locating conductors. The FIELD STRENGTH measurement is used to define the shape and attitude of the conductor.

SPECIFICATIONS

Source of Primary Field:

Number of Stations:

VLF Communication Stations 12 to 24 KHz

7 switch selectable

Stations Available: The seven standard stations arc Cutler, Maine, 17.8; Seattle, Washington, 18.6; Collins, Colorado, 20.0; Annapolis, Md., 21.4; Panama, 24.0; Hawaii, 23.4; England, 16.0. Alternative stations which may bc substituted arc: Gorki, Russia, 17.1; Japan, 17.4; England, 19.6; Australia, NWC, 22.3 KHz.

Check that Station is Transmitting: Audible signal from speaker.

Parameters Measured and Means:(1) DIP ANGLE in degrees, from the horizontal of the magnetic component of the VLF field. Detected by minimum on the field strength meter and read from an inclinometer with a range of ±80" and an accuracy of :tVi e .

(2) Field Strength (total or horizontal component) of the magnetic component of the VLF field. Measured as a per cent of normal field strength established at a base station. Accuracy ±2% dependent on signal. Meter has two ranges: O — 3009& and O — 60095*. Switch for "keyed" or "F.S." (steady) signal.

(3) Out of Phase component of the magnetic field, perpendicular in direction to the resultant field, measured without sign, as a per cent of normal field strength. This is the minimum reading of the Field Strength meter obtained when measuring the dip angle. Accuracy ±^

Operating Temperature Range:

Dimensions and Weight:

Shipping:

Batteries:

-200 to 4-HO0 F.

3.5" X 7.5" X 10.5" — 6 Ib.

Foam lined 'vooden case — shipping wt. — 15 Ib. .

2 of 9 volt: Eveready 216, Burgess 2U6, Mallory M-1604Average life expectancy — 3 weeks to 3 months dependent on amount of usage.

Units Available on a Rental or Purchase Basis. Contract Services Available for Field Surveys.

r

416 965-69J8

\~ \t. *.'-

April 3, J

Mr. W. A. Buchan Mining Recorder Court House Sioux Lookout, Ontario

Dear Sir:Re: Mining Claim PA. 226391 et al Seseganaga Lake and Squaw Lake File 2.569__________________

The Geophysical (Electromagnetic) and Geological assessmentwork credits as listed with my Notice of Intent dated March16, 1972 have been approved as of the. date above. Pleaseinform the recorded holder and so Indicate on your records.

* j

Yours very truly,

Fred W. MatthewsSupervisor

Projects Section

OJ/mh

cc: Amax Exploration, -Inc. Toronto, Ontario

cc: Amax Exploration, Inc. Thunder bay "P", Ontar:

Utn: Mr. J.E. Stters

APR 101272 *

cc: Mr. H. L. KingResident Geologist . 808 Robertson Street Kenora, Ontario

-*o*.s

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^fes l D IP A N G, te s I N De c-iRe

PROFILE: SCÛET o l ~ 2O

ELECTROMAGNETIC

for

AMAX EXPLORATION

by

SURVEY

NC

OFR J Penney, Contractor

OF

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AMAX EXPLORATION, INC

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52J01SW0005 S2J02SE0049 SESEGANAGA LAKE

Scale : 1" r 400

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GEOLOGICAL REPORT ON THE VANESSA NORTH GROUP, ONTARIO … · 1. GEOLOGICAL REPORT on the VANESSA NORTH GROUP, ONTARIO Introduction A geological mapping survey was completed on claims