introductionigunn - tt-t -- -w-*'in*. · introductionigunn" - tt-t -- -w-*'in*. at...
TRANSCRIPT
53J11SWe00S 63.1115 ALJO LAKE 010
Report on the Geophysical Surrey performed on the property of
INTRODUCTIONigunn" - TT-T -- -w-*'in*.
At the request of the Board of Directors of the Company and follow
irig the suggestion of the company engineer, a Magnetometer and Electro
Magnetometer survey was nw.de on the company's claims*
The purpose of the surrey was to attempt to correlate the geology
of the ground that is normally covered by overburden, by means of the
magnetic susceptibility and magnetite content of the underlying rocks,
and by comparing idth a previously known geological structure containing
rock*! of known type, thus preparing a complete picture of the claims.
The presence of break* in the rooks, such as faults, shears end fractures
should, also be indicated both by magnetics end E* W* conductors* The
above factor* would, then be applied with visual surface geology, under
ground maps and aerial photographs, to compile a comprehensive geological
picture of the ground, thus aiding toe search for gold bearing structures*
UGATJPJL*
The company's holdings consist of 16 unpe.tented claim* in the
Sachigo Kiver area of the Patricia portion of the Kenora-Red Lake Mining
Division in Ontario*
Claim numbers are KRL* 48046 to KRL 48060 inclusive, end remain in
good st&nding until June 1961*
The filing of this survey will qualify for one year's assessment
work, in addition*
The property was mapped by means of a picket line grid,
Pick&t linet; were cut in a true north-south direction to inter
sect the formation at right angles, and a base line v/ae run in an east-
vjest direction. Picket lines were cut at #00 foot intervals, and
station* established very 100 feet by chaining* Distance north of the
b&se line was 1,SOO feet and aouth 2,600 feet. The boundaries were tied
in by chaining.
The magnetoiseter was read on every station, and the E.W. on every
station on alternate lines, 400 foot spacing, using the parallel line
Vertical Loop transmitter, Horizontal Loop receiver*
Diurnal stations v/ere set up every 1SOO feet on the base line, and
a graph drava* based OR eight readings per base station. All magnetometer
reading*} were corrected to this graph*
used were a Sharpe A, 4 Magnetometer with scale gradation
to #O gammas, readable to plus or minus 6 gammas, line interval #00 ft.
*ith stations every 100 ft*, and a Sharpe S* F. &OQ Transistor, vertical
and horizontal loop E*M* Readings were by the Vertical Transmitter,
Horizontal Receiver, parallel line method - line interval was 400 feet,
MO stations. This shouM give e depth penetration of about 200-&76 feet
over normal terrain.
The terrain is very flat, with optiMum elevation not over SO feet
and no sharp increments of elevation were present. Outcropping its scarce
- S -
being less then l percent* Overburden appears to be between S feet and
50 feet. The lakes are shallow and silt filled* The regional geology
consists of fine and coarse grained laves (greens ton ess), with veins of
quarts and dykes of dacite:, syenite and biotite, porphyries, diabase and
diorite. The levat apparently give a mean reading of 8,500 gammas.
Based on the known susceptibilities of the rooks, we anticipate a picture
as follows*
The quarte veins will give readings in the range of 8,800 gammas,
due to the cchi&ted zone in association vdth sulphides* The diabase
dyke should exhibit more negative reaction or be conductive, while the
porphyries, ecid and consolidated, should give lower reading*. These
figures are, of course, based on assumption and prior experience in
geophysics*
E* M* The E. M* profiles revealed a normal level profile over
the majority of the property, with null angles in the range of *5 to 1*6
degrees*
However, in the north-east corner of Claims 48046, 48047 a very
large crossover with angles to 80* was encountered* This reading,
combined vdth the presence of magnetic highs, indicates a strong sulphide
zone*
These highs were preceded by bands of wide nulls and no nulls*
Other smaller conductors were noted in the area of the old
workings and on Claim 48060* Again combined with the high Mag readings
. 4 -
cm Glei w 48050 this is an area of interest. In both sections Mag highs
and lows were associated, thus implying * quarta vein in conjunction with
a n&neraliaed porphyritic dyke. In view of the association between these
structures in the original mine eone, these areas present a very strong
target for drilling*
In all, four zones of major interest are noted* The area in
ClaiR 48CM6 on Dorothy Lake should be drilled firot because of the
seasonal nature of drilling from the ice* All the other zones could
be drilled during or after break-up*
Rather than cover every feature found in the survey, refer to the
series of maps acoowpanying this report. Other than those areas spec
ifically named, the maps will clearly indicate the structure defined*
The F,*M* crossovers not numbered are suggested as being caused by wet
shears, or fracture zones*
A strong crossover shovm as X l in conjunction with magnetic eone
F is believed caused by the presence of a strong sulphide mineralisation,
Both the crossover conductor and the reverse crossover are believed to bo
significant*
Tho magnetic low indicated by B is believed to be the presence of
a dyke of syenite or andesite porphyry*
Zone A is believed to be the presence of disseminated sulphides
in a highly fractured or sheared greenstone, and also the presence of
quarts injections*
Zones H and I are assumed to be in the same pattern*
Zone I* indicated a diorite plug or intrusive*
Structural lines of weakness are expected along the sides of mag
netic contours that are elongated in a. north-couth or east-r:est direction.
EM Zone 2 it associated with the shearing and sulphides in Zone A*
Zone 8 is believed to be sheering and fracturing in association
with tho a&jor faults intersecting in Zone 4 and indicated on the map*
Zone 6 i*; believed to be a fold fracture or associate fault*
A nap with the combined features located is also included and is
believed to be self explanatory*
In correlating these results with the aerial photos, it must be
remembered that the direction of the glaciation wae North 850 East*
Lineation and structures in that direction should be ignored unless con
firmed by geophysics*
It is suggested that the original vein could have had several
factor* working on it*
Tho following should be consideredi
l* The vein was Jcaovai to pinch and ewellj a further extension could
be found with no displacement*
2* The vein was displaced to tho south on either end*
S* The vein was displaced to the north or south on the east, but not
on the vest*
4. Parallel or perpendicular associated veins should be found*
Suggested locations for drill holes are marked on the accompanying
wop* Reasons are noted on an accompanying sheet with locations on the
property grid*
. 6 ~
It is recommended toat a drilling program of 2,000 feet initially
bo implemented and extended when necessary*
The extension of the geophysical anomalies should be followed
into the recently stt&Jced ground*
Maps and interpretation sheets are appended.
ent credits will be filed from this office as soon as
possible,
Respectfully submitted,
HUGH H. SUTHERLAND, JR. P* EflQ*
Toronto, Ontario April lith, 1061*
53Jiisweee5 63.1115 ALJO LAKE 020
A Heport or* the Oeophy*ieal Survey perforated on 10 clhitafl held \y
o Hiyer Arefrj On t*
A Jfepietometer md KteotroM^notoBeter flurvey v&e conducted
over 16 eltsitw held by the ecnsjmny to the nwth wd wept, (td joining the
coM?*rgr't} original 15 ol^iwj?, f ne r^irpose ttap to wctond tJie txlitting
ion** of intorost end ittdioitt *my nwi artfte for tenrch in conjunction
with tin orifiintl IS claim** Aerifil i^otOf^Aphfl raid |rxwmd c; oology
used for correlation t-Kere
th*
The alaite earveyod ere part of e t? olui* n;roup
* ori^in*A 16 olnin fliwip OD noHhj eouth wid fce&t, fetid
in the 8schigo Kiver wos of the Pittricift portion, Konort - Ked
tf*^o Mining Metric t of Ontario*
Clf'lws f.urvoyod fere KKL 49100 to 49W5 incluslv* imd ero
valid until Miru^jy R7^ 196R. T^ii0 fsurvoy vi).), qualify for one yeer'c
Picket
The r*rop6rty *ae laapped ty neftne of c picket line 0rid*
*ere oat in o true north-south direction to intersect the
at right tininlep, *nd t featie line WAP run in nn net-vest
Picket lines *ere out Rt KX) fw*t interval^ end
evejy 100 feet by chaining*
- i-
J&stancc north of the boae lino WSB X*KOO font t*nd imuth
feet* The bounderiee vioro tied in \y opining*
The utagnototaeter *MIB re**d on every pt1 Won, tand the l* M*
on wery **tfttion or* &X tomite linos* 400 foot ftpficinf:, Ufsin0 the pertll&l
l*oop trimBwitter, HoriitontaX fjoop rdosivdr.
Wurtiul stations ware cot up every fcOO feet on tVte ba0e Hne*
p^ph dronn basod on eight re'^inga por toe* etHlon, All
were oorreote^ t^' t bit* graph*
used *-ero u Sh^rpe A*4 H^i^etoReter vlth
to KO g6mai8| rea&it&e to plus or winus 6 g&fmnj line
ft* *lth utetitme *veiy 100 ft*f end ft Sh^irpD 8*1* COO
vertioel feiid hoi'J,t.c*Rt?d loop K*K* Ref^lnp tor* ky the Vertical
nittor* fiftiitoriteil ft*De.iv*r* p/.-rellftl line wthod * line interval,
400 foot, 100 uUilionn. TiiJe phould give a depth pftnetr&tlcw of
fett
the torr^ln io fltt, *dth eo-'-tle elevaUons* On the
eido of Or^oe L^ko tlift ground rieee fflonly to * peok on lin* ?f *
000 ft. -iMwDtt tnrt f-lojtfep ctsfjy In ali directions f row Viic p(4nt*
elw*'tJori iu about 110 ft* above 6her** n l.t&e.
(mtotop^lnr le ^onroei, being less them l percent*
to bf between B fe&t wd to feet* the X*ke* ere pit 1 13 ov
filled* The regional geology ooiipi^ts of fine tind conroe grained
• s*
(con t 'd)
v.ith vein* of querti and dykAi of On ci t*,
biotit** porphyrite, dinb^&A arid diorite* Thf Iftvan uppaiM&ntly
t. HASH rodding of fc,K00 gammas* ftr/sad on the toiovm
of thu rool;s, we rmtlelpMe a pietur* M fol),owftt
fbo quiirta v*in* will (jivA ro&ding* in thA ronnA of
t,eoO fiiWD0t due to the scMfftod wvi* in eo^oei^tlon frith
Th* dlebMA dyke ehmAd Aidt&bit more neg&tiVA tvtaotlon or b*
while tt* porptyrloB, Acid fund cotir.olld'itod, tihould 0ivo lowar
?h i?s fiprAS erdt of our**, bssud on *eeuwptloh fend prior
in
E* tft Thft E.W, rAVoalod A noroid eoneictont profile
ov&r th* nsjority of tJie prop*rV* A 1*^* nuiabar of ttafell, irtftk
conductor* v.'ArA tiotod ^nd interprct^d AU frnoturos or ehep.r* da A to
folding* Thoao ere 00 fi^rkAd or ujiindie Ufl on t}* MP.
flj continuation of the siot-WAt f*ult through tbt tiorth-
fern of roster lake Wit* detected c*d ie indicated by tht eonduotor
to. 6* A oondaetor below Ho, 8 AB^ooi&tAd with thA dioritA
wot found end i e flUf.g*?ted to be it AolilDtAd or voter riiwr
whan th* diorite intmd^d the tfrowiptonc, Sfftr*n4 strong
tfo*?. 1,| l (*)t 0* 7| worA found in owitlmmtlon of the strong pulfide fcono indie d tod in t^it e-rlgirml nurvcy, end ur* bellevod to be
fttlfidA voJRB or dyke . A fsiiuilftr oonduotori Ho. Itj tap found on thA
bomtd-viy in oonjuttetion *ith t mognAtio
. 4-
fb* oontinu*itic* of both *on*8 A **ttd t on th
wro ouUinedt Th*^e urn etiuaed by difteetsinHed mil f i do*. A very strong high ros dl0oov*r*d ut 1400 K on lin* 18 e in Kono E (i6,(XX) gaum**) tnd *hcmld b* investigated* Pevond 3,ov0 mm found in
clono aneodetion *ith the !tij;h konee (O.E.), (l),)! (M. A,), (UA,), (B.F,),
ww3 citri bd ftttrlbutod to either A dipolar of foot ox* association of
structure* injootdd At th* P^S period of taov*nant* Tho dJorit* intruplv*
ixtwdod RSI Rhotm by ton* P*
A tragnttle hi{{b TOP found on th* wtet bMmdiirJoi* aho^i by 0| f-JKj in bolitvod to bf 6*ueod by dulfidoa*
Hevftml Kinetic contoure tloiigitted in en E. Vi. direction
led, f^d bfc&td on the drilling prog^ni of the orinibfcl property i
b tergtts f 01* inv*pti,Rf tion.
included r;r* bo l lav* d to b* **lf
on the l^rt^oing itifowafttion* fh* Rup of th* pr*vioui* purv*y wy b*
tiatohfd to thi* by Mditi^ to tho clsiw boutidbiltf find *up*rii|)oalntt
t h* ptr-aoturefi outlined i&py prove to bo ter#tt*i busod on th* original
drilling - no wrk nhoidM b* don* on thin ground until *
and pro&rwa* hn* boon nvolirad b*m*d en th* drill proftratiif^ on th* cri&irwl 15 ciftitais* With thla fturv*y and th* kno*l*dfi*
from iho drilJinsi fi jwotloal ipothod of datowsinlng th*
h^v* bsan evolved*
* s .
In ordw* to
(oont*d)
Surface laftpjalng *)iould b* done
outoro^s, if eny* ^th inftrr^fl g
Aepftpetf)fi)it credits will be filtd from Wile of floe*
When poBRlble Iho tmgnotlo hir!h mi line 1900 t Mi 1400 North
should be lnv*ptlgeio(5.
submit tod
mm K. , JH.fprontoi Ontario /.;-ril K
''
0G0
53J11SW000& 63.1115 Al JO LAKE
. .OliOl-OOtOAl.. SWtVJv
on VHK !iiO)*j:nvy. - v.' ./OP'.; '' - .,
jK mw-ift rii ARK A
0)30
-/'i
. io ;oon
"'of '
/1 941
of .
of .
of
tho
wtoo v' ' - 1 '; ,."' . ' .
^t c*'f .
bf
tii
to 'Oort**j l.*lt0 to.
-if - t't
ri^ '' ' . .". ' ';' i ' . . l u. ''" ' "". ''" '" , ' ';- t - ' , ', "\- ' 't], ' .~: '' ' " . '.; ' '".
of fthOi^m.'!^;^ ,jj()ar : itic? .i |000,';fc*ot .i^r,tw;o to ;' " ' ' 1 ' ' ' ' ' ' ' '
. t* till .... . .' can
' to;i-bx* l^v^'
h JU
.•of
f r
-of K
-of. , -
'
on fifteen /to
ittive .by.
io Hn'o isi^
i f noat- .^6
ccd lout-of
' ' '•'•••"'.''- . ' '*.' : - - ; " : ; ;. '-.v . : ' \-':' : ' .v.-'-'Vy'-i /.•••i'-'-'-V 1 '- ' : '.
y ' --.y; . • ; ^i*in^^^' ' ": ' -' ' ' ' ; - V ' ' ' ' ' ' '.: .' ;V ' .' ' .. ' '
y'; W/ y , , //: H' ;.; ;,T ": ' ; '
-''00 1.^iO|' '' ' '
o.^ J'^'
n t
^
: , - "; ; ' ;, " - ' ( i*o|vth : - ;C't ;^5 ; Jfeot ,; : to. :,out ', u^.' .li iz-^y '. Mtbm^d ' : tttf f" '. . , . . . ! ; ' . ' , "' ' . ' ', . ,' j :; ;i ' ' ' -' '. -. '' - - ' '- ' ' . ' ' . ' "
; ,.,, ,,, ,-.,.., . ,,, . . ,..,,:*X-
'•fi ' ' " - "' ' - " '
.•. t . ' B : ' -,' ' . . . J ' ' ' " i . v '' ' " t
c*f .the Cmt^J^OH^r'tmont y0
ye Kl.6 '.of ) 'os tor 3 -ftVyth
voin ' on ' till; tjftBt. td4o of : t\ ^J.orit-0 #.w# ^..oc-ftlert ut,.tbo ;,
cU.8tavi.oi? it6rU* of -1/1*0 tio'Ur'.iiliOi^' of rno Tor ntiB0
cO)^J*i^*^ O?'* /'or. 'c '3onth : 'of - tyZ, Toot* ' ^ .^ W' v
f*
vie/
''^
^^^^ -oi
.'.O"
* 'in
-. but
..
11 : on ^-
illiO XjtU^
S.oiw*'' : W* Km 'th ' 'OJfuKfe 'fmft so fm -thor or* van - found by t utrfrso o, ti
' ' ' ' ' ' ' . '. " ' . ' ''i :'' . '. - : : "' : ' ' ' l ( ' ' '
the?' piw.wiy ( :i.ho *iJn6 'i.feo j\ui .on it. flos iX! '^own' on
n" by
. . to theA1I,. tho
-of' .' .'" ' H'.. ' f ' ' ' ' " ; ' '. y' ' , ' ' ' . ,. ' ' J ' - ..;* ' : '
In
. xiftkof, - ut-of -iibout ^ii*. to ^i5 '-
'
Vi c
A) l . ibp '; i thin;
In
,
of '-I'Vi^.i "" :3iV'lho
r ' le |A)6\rt
'. tuff*
** ,;
-of 'UiO''urfit;:^vo torapppftft }:^r0y of IMti banker lint!
-of" l!
fcyafe * -" :: 3ta 'iho ';.tiy'ft .' f Aows ; tbb. 'fcftMrt'O feh6w '.'In |:wt6fti5 to
. .on ttio ti^xith row -Of''-'."'- ; - ,;' ;, found/In itio . fliK*' |pv\iriod itroonstono in
•••' '- .- '-- ; 'I'lortbtsast fertct of f'oss; ' '' - ' . ;' : -' ,' ' ; ; : '" '.. ', ' -
C*B t of ' U*o - J.ft vet' f ).owJ* .. |i.ro t)i J n* . ; . IVC' luff' ' '" , - . . . ' ". . : - ,. • J ,
od foy I^WJE* of -/cil^oj. fix ..ItiVfi llov/B ifltb'fi t-
foot.* '• ; : : - . v :':" ''- •"", ;' "; ••••'-.' '•/^.• :: •'•-
.of ,: ' . ' ' ' '' : " "
ttou U * ' , p?*vV ' :of . Kiit
.fiVowt. J i-ilX.. '.' ' '
-. tho vfipt : it,
t t-o
'•V:':.;*V :':^v:, .::v - :, -*v^x-;:.;;;^^^.;^u; : ;;;^;,*^;5.0 f cot, M, width i." ' : Thoy'
found . ; |.niru(!lit^';^bo;:^Jorito fee voll ufi the* . \. .'i; KorOWAtin.rook0.:ito''.itvto sbsiotat younger In iijic •them tho :, ; diorite * : 'Most' Of the* ,iMko0 voftthbr ' afliite find .'
on .*lftim" -KftX
'n .
about" K '(i00 - J^ ^iflth .Movtwiont/to -tho 'fjouth '^Irift .e'ftet*, ; ,0no : ffiuH"^6UVh 'of\tho iiorU^^ftt , :nm :of Foster .take :Ha8"'iihi;": -;
of ftbout 70' ' ' , ' . . , .
of
, to
'In
*' on.; the1 '/09 toir . ' ' ' ,
-for '* •lonc'th" 'of ;450 f poi. ; ' Ohun^i.'^A^Htt ' : of /-:,"'\".:^' : '' . . ' ..'!; . ',''" ,'."-', ••;''' ,', :' ". :"',' '' •-.'•".'••V ''. ; . : . -'' '' . : .',' ^''-.'''
'tbo.votn ;.ftv0^Dd 0*^0 ounces - gold.^or -ton Mro'st* S*. 5 'foot*
fc
lit-* JLA. -*
,tU5
, *? W|t6 iy ' ^tftH ft ; l tt ft . IJhOfiV' . •tionC' :if Hto ' "|t i#ijpppyjtjtt0 fttV^ -id
t-ho '. bin At '4toto*t '7C*
:V *
* ^ ::
rtical' imclhor J fsonttil .loathe of .'from : 3,00 . i'o'liO liotitA'
'' 'f Iho :
-'')^
ft c .0ftv . r6 o
on.iri Ions o? -of faan
f) .ova' .to. ''e ,'north tUji ' iho 4jtOito' ^orpliyriot* .itn'inoA .the* ihoy.hiud above, f nd! woj*o' Jiou in. .the
oont-aot* 'Of ^th
ox l o tod ^n oro of-'
; . ' -. ' - '/; . . '; ' : 1'?1) Oh ' th O f 'OU fill .'3 (6 VO J. , WG6 W lOftd Od . 'tO ' ' tl *
te JH'W 'tyO :0f 03TO Wftft ' 'found, l.n ^I'Otldo'tl tuff * "'" 'this
-,OJT vo.ry . ll^iltod -oxUmt .ftrid .'only - Ofttriod .fjx*rt the*, fourth' tbo. fifth
; ';v •*' p r
^fcriw&ivo
l,0o:' foot ''' ' '
^ firt VI? # ' ' of .'tin* :*^|, tt)' ' ' '
•- -. , . . .-;--- ^ v ,
' l :- ; ; - ' : . :. " - . : ' -V ,. . ' : ; . , ' -, ' /In Ho) e 'Ml' :ai ' I6p * ' Ito 1^1.' 'ibto ntf .1*1 ovit c*
^
;: - : ' ; ' ; , , , :' : V*ork il - iho ^
'I'l no
: thc'f inV. wi\i.HM ••^rJtv'^f r:lho Jlov?" le; ln ' '
;^t';3 .0 ;'
tbo -' Iowa iiway ;" f rofi ; thp;- .^ :.v
'.''••
.-1*05 os '-.i^iiili; l^ i*opct*0p^ . to ,l6c(ito',bre;'C'
.o - In ' b5 otitt)ridiorH6 j n'
two
. tu.f f ' :f ;
; -of
^ ' '
9I 0 30'9I 0 15'
540 37 l 30" —
r- ooCJroi
UJ (T
UJ
UJz(T O
54 0 30 Corking L ake
540 37 30
9I 0 309I 0 I5
LEVITT LAKE AREA M-3324
0 30
in srro ro
o:UJ^ir
crLUXen
ALJO LAKE
KENORAPATRICIA PORTION
RED LAKE
SCALE: 1-INCH — 40 CHAINS
LEGEND
;Oi.:A1 i f; ; ANT;A i v;.;" i :. f i J
JIN'I.MO \ i\'~~,\\\ S ONi V -H^A(; r ^'KM-iTS ON:.YI;\;MV\AY ^ ROUT r rsti
200
NATIONAL TOPOGRAPHIC SERIES 53JI l
M-3323
i ii i* i i ut in i-1" i mini h ii tmmt n i MI' mil fi 545912 Blow Up
ONTARIO
MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH
f SCAPE RAISE (SLALED)
monument 8 m concrete marked 31
OLD FOUNDATIONS AND SCRAPOF
SHOPS AMD HOISTROOM,COMPRESSOR
ROOMETC
Dense Bush on d M uskeg f-- 2
Dense /Uder B us
[ FloatingWusheg
FLINT ROCK MINES LTD.SACHIGO RIVER AREA
RED LAKE -PATRICIA DISTRICT
ONTARIO
PLAN SHOWING
DETAILS OF MINE AREA53J115*0005 63.1115 ALJO LAKE
SCOPE MINING AND EXPLORATION CONSULTANTS LTD
LINE:
roCM ro
o
V
a-j r
s*
r y
o roCO (D
CM C\lCM C\J O
CM CO
CM O
r h, cO CO
Oo
O
LU O UJ
CM LULU LU
CO u,cv
rv,
s c 'J ' t e r e c-
P t n
i r u c t?
s k e
•J i d t pen
t a c k
48050 48046
48049
THIS AREA SHOW/A/ I N DERAIL ON
ACCOMPANYING SHELT
AT SCALE: i"*4o F T
D r j
rn O O g- ;; -
fs
o
J f, k e q
CM
LU^rCM
LU CDCM
Ld CO Lu
O fO
LAKE
BASF:
S r.
48055:-' s ^
4805!
W (j s K
(J S k e g
48060
53JTI 5*8885 63.1115 ALJO LAKE
SCOPE MINING AND EXPLORATION CONSULTANTS LTD
SYMBOLS
STRikF tt DIP
DIAMOND OHI^L HOLE,TRUE HORIZONUL
TRAIL
CLAIM BOUNDARIES
OUTCROP 9 TOPOGRAPHICAL OIJTLINt
i
z
3
4
5
LEGEND
QUARTZ PORPHYRY,APLITF
SYEN1TF PORPHYRY
QUARTZ DIORITE PORPHYRY
QUARTZ VEIN ^^
DIORITt, BIOTITE DIORITE
GABBRO
TUFF SHFAR Z ONE
GREENSTONE
GLOLOGY pY:D W SULLIVAN P E no H PARLIMENT PEng.
FLINT ROCK MINES LTD,SACHIGO RIVER AREA
RED LAKE - PATRICIA DISTRICT
ONTARIO
GEOLOGICAL PLANSCALE l"-- 2r.L ' OC
DO
RO
TH
Y
KR
L 4
80
50
KR
L 48049
K RL
48
04
8K
RL
48
046
KR
L 4
80
54
l
KR
L
48055
H lQ ftee*ST
OW
KR
L
48
06
0K
RL
4
18
05
8K
RL
4
80
59
GE
OP
HY
SIC
AL
D
AT
A
GE
OP
HY
SIC
AL
SU
RV
EY
RE
SU
LT
S
RO
CK
LT
DP
INTS
AC
HIG
OR
IVE
RA
RE
AQ
f
i.
RE
D
LA
KE
-
PA
TR
ICIA
D
IST
RIC
T
ON
TA
RI O
O ."V
7"
t?
53
Jt1S
W0
0B
5
63. 11 IS
A
LJO
LA
KE
53J12
30
230
/
"sr-
S
x
D O
R O
T H
LA
KE
,K R
L
48050
kR
L
48
04
7K
RL
48
04
8'K
RL
48046
KR
L
48
055
L 4805
4805
X.
\K R
L
48060
N K
R L
4
80
58
KR
L
48059
SH
EE
T
M-
CO
ND
UC
TOR
S
K-
ove*s
GE
OP
HY
SIC
AL
DA
TA
LE
GE
ND
S3J11SK000S 63.1115 ALJO LAKE
GE
OP
HY
SIC
AL
SU
RV
EY
R E
SU
ITS
O
N
c
", i.
T
AM
6±
f S
?
H
S T
/t
P
4 o
r,,
i tf
X ^
c '
T r
*-
a
T"*j
^
^o
w c
/ tf
i-
J-~
r- 1-
.- * 9
^ u
^ * y
/* -
T o
J"
^"i^
j -r
. /s
C-/
J i m
r*
o f t
/C/
'
2 jo
i5o
's
o
id
O"*
"^F
LN
T
RO
CK
M
NE
S
LT
DS
AC
HIG
O
RIV
ER
A
RE
A
RE
D
LA
K E
-
PA
TR
ICIA
D
IST
RIC
T
ON
TA
RI
O
•f? /*
S f
5
j+7 A
(j
sv
4 r
-S
S
7/^
X"
*-y^-^ff
-S t
s f?
L/&
y
- V
-;
KR
L 40
KR
L
4R
Q#0
KR
L
48058
GE
OP
HY
SIC
AL
DA
TA
NC
TIC
GE
OP
HY
S
CA
L
SU
RV
EY
R E
SU
ITS
O N
fi U
'f
/k 1
o
LS
l T
Co
o * fl -n
. J(T
-.
i"5
C ^
C
2
O O
-r—
, .,.
^
C X j
' "~.
/
f/j/
^,
,
Jo
'/c/, -.
FLN
T
RO
CK
M
N
E S
LT
D
SA
CH
GO
R
IVE
R
AR
EA
RE
D
LA
KE
-
PA
TR
ICIA
D
IST
RIC
T
ON
TA
RIO
—*
Tf
t .
-J t
t-
i-
C
C,
Lj
i.
l
c w
c*
*v
c
53J11S
W000508
63.1
115
ALJ
O
LAK
E250
f
/"
/
DO
RO
TH
Y
.j*.**
KR
L
48
04
7- ist
o KR
L
48048
KR
L
48046
KR
L 4
80
54
J
KR
L
48055
L 48052
KR
L
48060
KR
L
48
05
7K
RL
48058
KR
L
48
05
9
GE
OP
HY
SIC
AL
DA
TA
ME
TE
RG
EO
PH
YS
ICA
LS
UR
VE
YR
ES
ULT
S
FLN
TLT
DR
OC
KS
AC
HIG
OR
IVE
RA
RE
A
RE
D
LA
K E
-
PA
TR
ICIA
DIS
TR
ICT
As
o *3
-r
f-i
T- ,
*. r
c,*,
± t:
1S
T f
i T
'iT
- O
'V
ON
TA
RI
O
Of-
L
,*ic
CJ f
-'
C- s
-s
t
63.1
115
ALJO
LAK
E
53J
11
SW
00
05
260
KR
L
49
20
2K
RL
49200
KR
L
49198
K R
L 4
91 93
KR
L
49
19
4
GE
OP
HY
SIC
AL
SU
RV
EY
RE
S U
LT
S
FLIN
TR
OC
KN
E S
LT
D.
B * c
\
SA
CH
IGO
AR
EA
, R
ED
L
AK
E -
PA
T R
ICI A
D
IST
RIC
TR
IVE
R
ON
TA
RIO
K R
L 49192
KR
L
49203
K R
L 49195
GE
OP
HY
SIC
AL
KR
L
49196
KR
L
49
19
0K
RL
49
2 0
5K
RL
49
19
7
S3JH
SW
0005
63.1
115
ALJ
O
LAK
E
R L
49202
KR
L
49200
x s
K R
L 49193
KR
L
49194
GE
OP
HY
SIC
AL
SU
RV
EY
R E
S U
LT
S
FLIN
TR
OC
KN
E S
LT
D.
r z
f-M-
CONO
UC.T
OAI
AR
EA
, R
ED
L
AK
E -
PA
T R
ICi A
[5
1S
TR
ICT
SA
CH
IGO
RIV
ER
ON
TA
RIO
KR
L 49195
K R
L 4
91 9
2
'
G E
OP
HY
SIC
AL
K R
L.
4 9
i 9
6
KR
L'
49205
KR
L
49 1
9 Q
J,
K R
L 4
91
93
GE
OP
HY
SIC
AL
SU
RV
EY
R E
S U
LT
S
FLIN
TR
OC
KN
E S
LT
D.
SA
CH
IGO
AR
EA
, R
ED
L
AK
E -
PA
T R
ICI A
C
lST
RIC
TR
IVE
R
ON
TA
RIO
K R
L 4
9
95
GE
OP
HY
SIC
AL
K R
L 49196
K R
L
49
19
C
-li*
0
-15
*0
-35
-Y?
"W
-77
*0
-171
*
.5*
So
-3ft
*
- 31
00
-337
C
-. 3-
too
-34
40
- JS
IO
-j***
-171
J
-JS
lo
.1*1
4*
- Jf
l*i
-J51
0
51,0
0
-jao*
-J T
O
i d f
- 3
7o o
- j w
-3 t
joO
Sfc
*
-3
3*. t
o
-31.
00
•351
0
. JS
lo
. 57
1"
.353
0
-3**
'
- l
720
.44
P*
. J'iZ
t.
L 49-2
02
K R
L 4
9 l
9 3
K R
L 49194
KR
L
4 9
! 9
2K
RL
49203
JJ-U
-J
*-*'
.371
K R
L 4
91
95
K R
t 492 0
-T
KR
L
49196
KR
L
49
20
D
Qi*
^^1
"
J9H
O.3
7*-"
•(O
D-0
-39*
*• 5
7**
• Sfl
*-3
88*
•371
0-J
*1*
*-j
rt-
-331
0
3* t*
.31*
0
-I7W
.340
.
-57
S*
•J 7
-374
0-i
Tea
-3710
-3140
- S
700
KR
L
49201
KR
L
49200
J3oa
3(
1*1
GE
OP
HY
SIC
AL
SU
RV
EY
R E
S U
LT
S
O N
FL
INT
RO
CK
MIN
ES
LT
D.
SA
CH
IGO
R
IVE
R
AR
EA
, R
ED
L
AK
E -
PA
T R
ICIA
D
IST
RIC
T
ON
TA
RIO
LE
GE
ND
^L.C
LPhl
YS
iCA
L
DA
TA
G•5
*0
C.
J .
v c
t- L
•f *
r o
*
t,.
X .1
"J
C,-
,
-9 t y
53J1
1SW
000S
003
00
PX