RPT ON THE STURGEON NARROWS PROP SIX MILE L · PDF filel l l l l l l l l l l l l l l l l l l...

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52G15NW08I04 2 .12812 S IXMILE LAKE

REPORT' ON THE

STURGEON NARROWS PROPERTY

SIX MILE LAKE AREA

PATRICIA MINING DIVISION

ONTARIO

FOR

PRIMROSE GOLD RESOURCES INC.

RECEIVED

JAM G 1989

MINING LANDS SECTION

Prepared by:J. W. Redden, E .Se.

010

'CSt-

Box 117Wabigoon, Out.POV 2WOtel. (807) 938 6915

11 *11111111111111111

H Illnl HiS2G 1 5NWa004 2.12012 SIXMILE LAKE

TABLE Or ^m r,ni o

1 1 oiii page

] nt roduct J on 1

Location ]

Access 3

Physiography 1

fi aim;; 2

Previous Work 3

l\eg i O IK! 1 Goo] oqy 3

Loononn e Gee.] oqy 4

Di souss i on ol Previous Work T)

Magnet j c Surveys 5VI,}' 1 Survey 5 In a iTiond Dri 1 1 i ng 5Stripping and Trenchinq 6Sam p 3 i nq 7

f one 3 mn o; us 8

Is'eeoinii'iondat ; ons 9

Pi'fjposcd Kxpl or at i on Programme 9

Table

'1'alile 1 C*) aim Status Summary 3

Append i x

Appendix ] - Sainjile. Descriptions andAssay Results 10

] , 3 s t of Fig u j- e s (at e n d o f r e p o r t )

}'ig. 1 Area Location Map

L ig. '/. C J tt i in H lock and General Geology

Fiq. 3 Slrippincj Locations

010C


INTRODUCTION

The i-mibor carried out a review of previous work on the properly. A strapping programme was then carried out to expose a number of mineralized zones on the property. Tin s. report summari:;'.es the work carried out on the claim lil o c k i (j d al f?.

UX'A'HON

Tin- property in located on Sturgeon Narrows, which separates the north and south parts of Sturgeon Lake, a hou t 29 km south of Savant Lake. Ontario (Fig.J). Savant Lake is a hamlet; located on the main Canadian Na llonal Railway line approximately midway between Winnipeg. Manitoba and Thunder Bay, Ontario.

ACCFSS

The claims ea li most easily be reached by motor vehicle via Ilie Six Mile Lake Road. 15 km from Highway 599. A

i i ail from this road leads to the shore of Sturgeon Narrows a distance of 250-800 m.

The iunet. :ion of the Six Mile Lake Road and Highway 599 j s 25 km south of Savant Lake and 305 kin north of Ignace vi a l! i g h way 599 .

Scheduled a'i r service is available to Dryden and Sioux Locikout . 230 and 155 km. respectively, by road from the p) ope) t y .

The S J x Mile Lake Road j s not regularly maintained. A snow machine Is required t.o access the property inw i n 1 e r .

For access a l OIK,; the shore line. a boat can be portaged along the trail to the lake. Boats and motors can also be rented from several lodges and outfitters in the .-i r ea. Sturgeon Lake is a large lake and due caution must be exercised on the lake, particularly in windy or stormy weather .

}'!IYS]OGK'A1 1HV

The claim group is largely covered by water. The shoreline consists of areas of boulders alternating with (t.teas c-..f outcrop. The area back from the shoreline is generally rolling with low hills covered with thin overburden. Areas of swamp and rock ridges are also present . bur.ing July of this year, a severe wind storm uprofiled 20 -- 50?;'. of the t.rees growing on the claims. The resulting windfalls make traversing slow and difficult .

W. Redden - Geologist, p a gel

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PK'F.VlOUf; WOK'K

( old w:*r. first discovered in the Sturgeon Lake Area in the 1890';;. During this early period the present claims were prospector! and several pits and trenches were dug. No documentation of this early work exists.

Hi nee that time exploration for gold has been carried out in i ho area as t Vi e interest in gold rises and falls.

The main showing on the property was apparently a patented mining location for many years. The earliest documented work was carried out in 1969 hy W. G. Wahl Ltd. Fxploration lias also been carried out in the immediate area by Falconbridge Nickel Mines Ltd. and Abermin Corporation. Work to date lias included magnetic and VLF surveys. geological mapping and diamond dr i l l ing .

Twelve* of the present claims were optioned by Primrose Gold Resources Inc. in the spring of this year. The additional twelve claims were staked in July of this year. To date Primrose has carried out a stripping programme and a preliminary evaluation of the property.

RLGTONAL GFOLOGY

The property is underlain by an assemblage of metavolcanics. metasediment^. alkalic intrusives and ga bin o (see Fig. ?.) . The volcanics are predominantly mafic, with only a limited intermediate component. The m c t a s o d .i m e i ri. s c o n s i s i m a i n 3 y of c o n g l om e r a t e . Mi n o r siliceous bands are present within the conglomerate as are local concent rat i ons of magnetite. Graphitic: zones are present along the northern contact, of the sediments wit li the. vt i '.carries in the northwest corner of Pa 704623. Peg ional mapping suggests the sediments form a synclinal core within the volcanics.

The south shore of Sturgeon Narrows is underlain by an alkalic complex. The contact with the sediments and volcanics lies beneath the Narrows. The Narrows has been interpreted as a rift valley by some.

Feldspathi o dykes cutting the metasediment^ on the claims are believed to be related to the alkalic complex. Gold occurrences discovered to date on the property are associated wit Vi pyrite within these f e l clspa t hie dykes .

A small gabbro intrusion has been mapped as occupying 1 he neat hern part of claim Pa l Of.i291 7, .

W. Redden - Geologist, page 3


TICONOMJC fiFOJ.OGY

Gold occurrences discovered i ri the immediate drea l, o date can he characterized as pyr i t i c zones within f e l dsp, "tt hi c dykes. Pyritie. carbonated shear 2 one f. within the .sediments are sometimes anomalous for gold. To date, no significant gold values have been found in these shears.

Two significant gold occurrences are known to exist within feldspathic dykes on the property. The larger is t. he gold showing on Pa 704623. The- other is only known 1 T out dr i l l ho] f-s .

Hot h occurrences have several features in common:

significant carbonate content (5-20?o)

significant pyrite content (2-10^.)

approximate east- west strike

t r a c es o f f l u or i t e

Other If-atures are not common to both:

Main Showing

present

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mi i ioi a l i x a t i on ?. - ::tm y, o i \ e w i t h i n t he dyke

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d. W. Redden Geologist pago4

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DISCUSSION OF PREVIOUS WORK

Magnet i o Surveys.

('round magnetic surveys. over part- of the property have been earried out by Falconbridge and Aberrnin. Only the Fa leonbr idgc survey covered lake.

The magnetics indicate the main showing as a magnetic low striking to 1 lie east . The survey stations were too far apart to trace the '/.one for any distance under the lake. Severe) cither magnetic lows on the property may represent. o1 her gold hearing zones.

VI,F Surveys

Ahermin conducted a VI,F survey over a part of the land portion of the property.

The survey identified the conducting zone drilled by So l co. It also outlined the shearing associated with the feldspathic- dyke exposed in trench 44. The data also suggest f; a conductor lies under Sturgeon Narrows.

Tin.' survey did not. respond to the main showing.

l H amond P r i ; 3 ing

W. O. WaVil Ltd. drilled 4 holes on the present claim group in 1969. Two of these holes were drilled to the east from t lie point south of Pa 704623. The holes were drilled to determine the source of an airborne magnetic anomaly under Sturgeon Narrows. Technical problems stopped the first hole. A second hole (69-2) was drilled to a total depth of 1702'. This hole was logged as having encountered conglomerate at the top of the hole and volcanics towards the bottom. Alkalic dykes became more common towards the end of the hole.

Hole 69 3 was drilled to intersect an EM conductor located near the 413 post of Pa 704623. The hole was drilled at --I' 1 degrees to the north. The hole reached bedrock ri t S4 ' and immediately entered a feldspathic dyke containing carbonate and pyrite';. The conductor was located further down the hole, but was not of interest.

Tlole 69 .'l VMS drilled at 45 degrees to the south and mf ei sect od the full width of the feldspathic dyke. Assays o:! the dyke were 0.10 oy, ./ton Au over 3.5' and 0.07 ox./t on Au over the following 3' . No further work was dome due. lo the low price of gold at that. time.

W. Redden - Geologist page 1 !


Aneithet IK* It- (('9 r)) was drilled on the south F; j de of fMurueon Narrows during this came programme to :i nvf -st i gat o for rare earths.

Cor'*-- from til] 1 hese holes was found on the south shore of t ho lake this summer. A11.hough some of the core had de:'ii dumped . it was possible to retrieve 51 boxes of undisturbed core. The core was transferred to new core boxes and tiansported to the north side of the lake for examination and sampling. An early snowfall makes it impossible lo examine and sort the core in the field. The core will lie transported to suitable facilities this winter for examination. splitting and assaying. Except for the 6 . ri noted above, the core was not assayed for no l d .

fie] co drilled two holes for base metal s on an EM conductor just to the north of Pa 704628. One of these holes (242-23) entered Pa 704623 at depth. Several pyritic and graphitic /'.ones were intersected. The drill log r; indicate samples were taken. however they do not i n d i c,: 11 e i f ( \ o l d wa s o n e o f t. h e d e t e rm i n a t i o n s c a r r i e d out. The core is still located at the site. The early snowfall also prevented the re-sampling of this core.

Ea l conbr i dye drilled 8 holes on the present' claims. The location of the core is noted on Fig. 3. Feldspathic dykes we r*-: intersected in several of t,he holes. Assay results were low. It was assumed that all the holes :i n1 ei sect eel the same feldspathic dyke. Plotting of the vertical pi o.iect i ons of the holes indicates that several different dykes were intersected.

Abermin drilled several short holes on the main showing. All five ho'ies were vertical. Assays were low. Due to the nature of the mi nera l i xoit i on, it is likely the holes were not drilled to best advantage to assess t.he show inu .

'"U.r i ppi ng and Trenching

Ahorniin cleaned out and sampled the original trenches on 1 be main showing. Their results indicate a xone approximately 1 2 x "J !3m containing from 1250 to h800 ppb Au. The y.one is open to the east.

Tlie main showing and other locations were stripped this past summer by the author to further evaluate the nri ner a l i xat 'i on . Locations and sampling sites are shown on Fi o. 3.

d . W . R e d d e n - - G e o 3 c' g i s 1 P age 6


The main shoving i r; he a vi ly leached. To obtain fresh unweathered rook, considerable excavating would have bc MI required. 11 was considered t.oo expensive and tori risky to d r j l l and h l a s l to fresh rock, particular J y as the fresh t nek woi.i ] d most likely lie below water' level.

Tli*' (illiej feldspathic dykes exposed were somewhatcarbonated but not to the degree of the main showing.Pyj j t. e was sparse or absent .

'I'lle stripping exposed several sheared and carbonated ;:-,oi!fs wit Inn the sediments. Pyrite was present, in minor concentrations only. The shears were vertical with :: -, t r 3 k e s f r or i O G O t o 080 d e g r e e s ,

Sever S l j shear -/.ones were also exposed containing ankerite ve-.in s up to 6" thick. Pyrite, when present, was sparse.

A unique rusty mass was exposed in trench #4 at the site c-'f sample SN- .1 h . The surrounding rock to the north, south rind cast was dark green sediments. Rock to the west was covered with overburden. No fresh source rook for the rusty material was evident, A portion of the iu s t y mnt c - r j a l wa s m i xe d with round ed g r e en s tone cobbles. The mass may represent an older till unit or. less likely, a residual deposit. Additional excavating w:i l l lie required to clarify the origin of this material.

Samp l i no

Thirty four samples were collected from the property during the piesenf evaluation. Samples SN-1 to RN-30 were collected from the stripped areas. Samples SN- 31 lo SN- 3--1 were collected from the additional claims staked to -.he northeast . Descriptions of the samples and the analytical results are given in Appendix I.

The result;:-, confirm the presence of high grade gold values at the main showing. The highest, values appear lo Vie associated with coarse pyrite although exceptions do occur . The weathered nature of the rock did not l ier m i t r e l :i a b l e channe l samp l i ng .

The shears in the sediments returned several low anomii j ous go] d va l ues .

The ether feldspathic dykes returned a few slightly anomalous gold values.

.1. W. Redden - Geologist page?

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The rusty xone (HN--35) returned comparatively high La f J r:./! Op] -mi) a M d Oe nyyopprn) values plus Th of MOpprn, U of /!'/ . '/.\ . pin and P of 8000. These results suggest. a carbonatite or ) elated rock type to lie the source. Further work is required to assess the significance of t liese va l ues .

I-Kimp] f - f ;N- 'VI returned l 230pprn As with negligible gold.

'i . Two go l d- 'hear i nq feldspathic dykes are known to occur (in t IK"- c l a i ins .

;: . Previous work lias indicated that additionalfeldspathic dykes and other structures, possibly gold- bearing, occur on the claims.

':i. Additional exploration is necessary and warranted to test, the known structures and to discover new zones.

.1. W. Kedden - CJeologist page B


RECOMMENDATIONS

1 . The land grid should be extended on the j re to cover Hit: cut:; re property. The area near the known showings mn d possible extensions to the east should lie o t J') Oro intervals with other lines at 100m :i n1 ervc'-i Is.

?. . Detailed magnetic and VI,F surveys lie carried out over the grjd. A sparing of l '2 . 5m between readings on a l l the lines should provide sufficient, detail to define iow magnet]e areas. Where low magnetics are encountered, a 6.25rn spacing and intermediate lines may be requ j red .

S. All linear magnetic lows should be detailed by I. P.

A. A preliminary diamond drilling programme be carried ( ut 1 h :i s winter to test anomalies defined by 1 . a nd '/. . a bove. It is expected that linear magnetic lows eoinc'jdenl with a strong T.P. response would be the pr ime t ar g e t s for d r i l l i ng.

r s . Core from the Wahl and Se leo drilling be examined and samples sent i or a ssay.

O. Additional work would lie based on t.he results; from 2 .1 o 'j . a l love .

PROPOSED EXPLORATION PROGRAMME (Phase I only)

fa) ri f i d. magnetic and VLF surveys,drafting and report 15,000

(It) I.I 1 , survey l f i .000

(c) pt e]i mi nary djamond drilling (2000 1 ) 70,000

Subtotal 300.000

Contingency 10,000

TOTAL f,U 0.000

.1. W. Redden - Geologist page Q


APF'ENDTX T

PRIMROSE GOLD RESOURCES INC.

SAMPLE DESCRIPTIONS AND ASSAY RESULTS

f IN -1 c,rt "bonat cd shear zone in conglomerate, minor Kyr; i e, o a r; l end of trench 4t l , w i di h of 0.2--0.3m

SN 2 oorbonat ed shear zone j n conglomerate, minor pyril^ . 8' from e ci B t, end of trench #1 . width of 0. -} fim

SN- 3 ea rlif *nat ed shear zone in conglomerate, minor pyrite, 2 2' from east end of trench #1, w i di h of l . 1rn

SN- -'1 earbonal od shear zone in conglomerate, minor pyrite. 30' from east end of trench #1, w i (H h of O . firn

SN- h carbonated shear zone in conq l ornerate , minor pyr:ite. 1 fun from east end of trench #1 , w i di h of O . 6m

SN 6 carbonated shear zone in conglomerate, minor pyrite, 3 [mi from east end of trench #1, w i d t li ci f O . 3m

SN 7 carbona t ed shear zone j n conglomerate, minor pyrite. 3'iim from east end of trench t J . width of 0.9m

SN 8 carbonated shear zone in conglomerate.trench 4(2. width of 0.3m, strike 080 degrees, d -i p vert T ea 3

SN- O feneijzed. carbonated shear zone in conglomerate, minor pyrite. 7m northwest of SN-8, strike 080, dip vertical, width of 0.6m

SN- 10 carbonated shear zone in conglomerate, pyrite and carbonate in wall rock, l . 'im NW of SN-9. strike 060, dip vertical, width of 0.45m

SN- 11 irregular' carbonated zone with pyrite andcrirboiiate in conglomerate wall rock. 0.6m zone ad i a cent to SN- 10

SN- l/' shea) ed conglomerate with carbonate str nyr i t e. in wa l l rock

.1 . W. Redden ~ Geologist page 1 O


;";N 13 0.3m pyr :i t j c shear .in conglomerate, trench #4 - - 6m from south end

:; ;N 3 4 silicified sediment, trench 4t4 - 8m from south <" t id

TIN K) rusty zone, trench 4)4 - 26m from south end

flN 36 siliceous sediment with } "(, d isseminated pyriteand pyrrhotite, site of an old pit. trench 4-A - -14m from soutli end

:: ;N 17 rusty, fonetized zone, trench 414 - 49m from south end

f!N- If! fend i zed rusty zone adjacent t.o feldspathic dyke, trend! 414 - 'i 3 m from south end , feldspathic dyke to 66m in trench #4

f-iN-19 wliite and red feldspathic dyke, strike 080, dip vertical, width 2-3m, trench #b

;~;N -'M t rench 416, 0,4 rjm vertical chip. 3m NW of old pit., msl y feldspathic with carbonate

f IN- /'l Irencli 416. oral) sample, very rusty feldspathic dyke- mat.{'r i a l

f.lN- ?.','. I rt.'iK-h 416, 0.3m horizontal chip, 2m E of old pit. feldspathic dyke material

TIN 23 trench 4t 6, O . 6rn horizontal chip, NE corner of old pit. feldspathic dyke material

TIN ?A t rencl'i t)6. qrab sample, fairly fresh feldspathic dyke ma t e r i a l w i t h ( 1 S; pyr i t e

f;N- 2!t t rone}] 4t6, qrab sample, rusty feldspathic dyke material v?ith 2-3^.'. disseminated pyrite

F'lN-26 trench :H 6. grab sample, very rusty feldspathic dyke ii'tator ia l , visible gold in leached, pyrite cav.i t. ^ e s

riN -27 trench -t! 6, 0.45m vertical chip, 8m from HE corner of old pit, rusty feldspathic dyke material

f-iN--28 trench 416. grab sample, feldspathic dyke material coni,a i n i j ig f)- 1 OX coarse pyr i t e

f'!N 29 "trench :#6. grab sample, feldspathic dyke material coni uining 10-20/b very coarse pyrite

f;N :U) i ; cnch 4t6. grab sample, very rusty feldspathic dvke material

, l , W . K' e d den G e u l o g i s t page3 3


f!N ;!l '! ' sheared, c f) rhonat .eel mafic volcanic, trace of pyrite and cha l copyr 31 1*.. o n shore at lTi-f30E

UN ''.'! 'i' shear od. carbonated mafic volcanic, trace of pyrjte. on shore at 32H50E

f!N' ''''T slic-ared mafic acig l omerat e , di P P o mi nated and b l o bf of pyrite, on shore at. 9-t93E

SN- Oi-1 sheared, ajfered inafjc volcanic now chlorite seh'Sl, disseminated pyrite crystals to 2cm, loc.ist; angular blocky appear to be frost heaved, on slio) e at. 9480E

J. W . Kedden Geologist

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is

PRIMROSE GOLD RESOURCES INC,LOCATION MAP

STURGEON NARROWS PROPERTY PATRICIA MINING DIVISION

ONTARIO

scale 1:500000

Fig. l

XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX^XXXXXXXXXXXXXXXXXXXXXXx x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x x

"V

/.:-fiiii 'tV.ini.

' ; ::.)i [,)i i. i l

i';i t MJI i i .1 j :K -:; i

l M ) ; i

DU r A i. ' '..I:.; i:'

^i^ 'HI i.'j"/, s

l i' i i ' j 1 1' ;,\!;' [

t .l

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'r/i: us' r,\w W -'

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i' r\ l : ;.;-\') i i''[..; (r --.;: ; -, ;;; : .*

H'v i j' i !. i.'^:.'11

•'•'M ^!'T yii/U:-. 'A'/^

x x x x x x x x x x x x x x x x x x x xxxxxvXX

Xx

X;vX

l

(AI)U!

AOrE

M HI.-:;

; --'.L

. /.!. l ^'

m l

i.)

; o IDA M i.

•x'T.'U X

X X Xx x x x

IJ Xx x x x x x x x x x x

XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX.XXXXXXXXXXXX:;AXXXXXXXX.AXXXXXXXX

Ministry of Report of Work . .. . Northern Development

Mines (Geophysical, Geological, j Otffario ' ..; Geochemical and Expcndi^ircs'lfjK

52G15NW0004 SIXMILE LAKE 900

Claim Holder(s)

Addressc.

Prospector's Licence

7" Jr/ 2. 3

Survey Company Date of S urvey ( from 6* to)

Day l Mo. l Yr. l Day l Mo. l Yr.Name and Address of Author ( of G eo-Technical report)

J.uJ.

Total Miles of (ine Cut

Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

RECEIN/DEC 19 t

MINING LANDSAirborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysica!

- Electromagnetic

i c r\r* -iMpgnetometer

- Radiometric

B8 0- Other

sWftJNGeochemical

Electromagnetic

Magnetometer

Radiometric

Days perClaim

Days per Claim

——— ———

Days per Claim

Expenditures ^excludes power stripping)Type of Work Performed

t

Performed on Claim(s)

S/ZCTioS 71 -Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

S 7^07. 8 5Instructions

Total Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

Date Agent (Signature)

Certification Verifyincp-ffeport of Work

Mining Claims Traversed (List in numerical sequence)

Total number of mining claims covered by this report of work.

l hereby certify that l have a personal and intimflte knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Marne and Postal Address of Person Certifying

Date Certified

1362 (85/12)

Ontario

Ministry ofNorthern Developmentand Mines

Ministere duDeveloppement du Nord et des Mines

February 9, 1989

Mining Lands Section 3rd Floor, 880 Bay Street Toronto, Ontario M5S 1Z8

Telephone: (416) 965-4888

Your file: W8803-278 Our file: 2.12012

Mining RecorderMinistry of Northern Development and MinesCourt HouseP.O. Box 3000Sioux Lookout, OntarioPOV 2TO

Dear Madam:

Re: Overburden drilling and Data for Assaying submitted under Section 77(19) of the Mining Act R.S.O. 1980 on Mining Claims PA 815754 et al in the Area Six Mile Lake_________________________________________

The enclosed statement of assessment work credits for assaying samples has been approved as of the above date.

Please inform the recorded holder of these mining claims and so indicate on your records.

Yours sincerely,

W. R. CowanProvincial Manager, Mining LandsMines A Minerals Division

Enclosure (2)

cc: Resident GeologistSioux Lookout, Ontario

Primrose Gold Resources Inc. 500 - 67 Richmond St. West Toronto, Ontario M5H 1Z5

J. W. Redden Box 117Wabigoon, Ontario POV 2WO

Ministry ofNorthern Development

inesOntario

and^lii

Technical Assessment Work Credits

Date

February 9, 1989

File

2.12012Mining Recorder'! Report of Work No.

W8803.278

Recorded HolderPrimrose Gold Resources Inc.

Township or AreaSix Mile Lake

Type of survey and number of Assessment days credit per claim

Geophysical

Magnetometer days

Other days

Section 77 (19) See "Mining Claims Assessed" column

Geological days

Geochpmical days

Man days [J Airborne Q]

Special provision | | Ground [X]

| | Credits have been reduced because of partial coverage of claims.

Q] Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

S9,407.85 SPENT ON OVERBURDEN DRILLING AND ASSAYING SAMPLES TAKEN FROM MINING CLAIMS:

PA 815754 704623

627 DAYS CREDIT ALLOWED WHICH MAY BE GROUPED IN ACCORDANCE WITH SECTION 76(6) OF THE MINING ACT R.S.O. 1980.

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claims

PJ not sufficiently covered by the survey | | insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical -80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.

828 J85/12)

Fourbay Lake Q91900' 90*?45'

50000'—n

O) J*o

tOacQ)

Q.

4905230 :-B

7(9586^ . - — . L

Po PO , P ' 642986

7IS954 ' 642975 64JS7B SI2O66 6*O4JO 640399

l, '08^43 J (oai244

224 P02II746 lPo?IIT53 U

ICLM. B 225

CLM'255 f

X ABITIBI/ POWER and PAPER CO. LTD.Po 1X5710 0237*2 j P. Z2S740 |p

NO. 7Swamp t*

-50000'

59'

58'

57

56

55

54

53

91*00' 57 56'55 54 53' 52'

Bell Lake

51' 50' 49' 48'47 46 90045'

52GI5NW000t S .12812 S IXMILE LAKE eoo

oO)

a;1Co

COO)

O

498904

LEGEND

HIGHWAY AND ROUTE No. ^

OTHER ROADS

TRAILSSURVEYED LINES:

TOWNSHIPS, BASE LINES, ETC.LOTS, MINING CLAIMS. PARCELS. ETC.

UNSURVEYED LINES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSHOR MUSKEG MINES TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT, SURFACE ft MINING RIGHTS___..........l— 0" .SURFACE RIGHTS ONLY..__....__......... O*" , MINING R1GHTSONLY ___....._......,m. ©

LEASE, SURFACE ft MINING RIGHTS———.-....——. H-" .SURFACE R IGHTSONLY.__...........l.....™. B

" , MINING RIGHTSONLY-._______.—..-__. H LICENCE OF OCCUPATION .__....___...,,__.___. TOHDER-IN-COUNC1L ..__,._...___..............._. OCRESERVATION _________._......._...^....m.

CANCELLED ^_________.......^.....Jm....... ®

SAND St GRAVEL ___m._____.____.___.- ..

NOTE: MINING RIGHTS IN PARCELS PATENTED PRIOR TO MAY 6,1913. VESTED IN ORIGINAL PATENTEE BY THE PUBLIC.

______LANDS ACT. R.S.q 1970. CHAP MO. SEC. 83. SUBSEC 1.

REFERENCESAREAS WITHDRAWN FROM DISPOSITION

M.R.O. - MINING RIGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

M.+ l. - MINING AND SURFACE RIGHTS

Orrfw M*. DM D iwMltton PNi

SAND AND G RAVE L

GRAVEL FILE NP 19II7Z

28/67

SCALE: 1 INCH = 40 CHAINS

FEETO 10OO 2000 4OOO 6OOO ooo

O 700 METRES

1000 M KM)

20OO (2 KM)

AREA

SIXMILE LAKEM.M.R. ADMINISTRATIVE DISTRICT

IGNACEMINING DIVISION

PATRICIALAND TITLES/ REGISTRY DIVISION

KENORA/THUNDER

Ministryof L and Natural Mtnagamtn

Resources ' BranchOntafio

D*li FEBRUARY, 1984. Ninbtr

G-

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