rpt on the geol on the geol of a group of cls nairn twp · 2017. 1. 17. · similar to tmk south...
TRANSCRIPT
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Com* K i Mtl UNITED WOLOI 36 CLAIMS i M THE
or NAIM TOWJI&HI*, DIKTKICT or Supsv*v.
THC PROPCATV 19 LOCATfiD flVK MILKS SOUTHlAUT Of IMro*TA*T
UBAOUH DEPOSITS AT THE CASE Of TMC SEDIMENTARY MATINEKOA FO*M*TIO*.
tT IS HICHLY MDSAftLE THAT THE KATI1E10A FORHATIOM OOC* U*DE*LIC
THE PROPERTY* THE1E tt AEASOR TO SELICVE THAT THE DEPTH fAOH fydfACC
TO THE 0*8* Of THE rOAMATlO* (THE MVOURASLE HORIZON fOK KAOtO'CTIVE
CfO**T9) IR MOT CICmiVE, OUT THE ACTyAL OC^TM, EATCdT AND
or tAoioAeTUE otrojiTo CAM m cmnnmeo ONUY ir OIAMOHO
OlAHONO OKIULIKQ AT THtt tTAftt II HIGHLY SPECULATIVE AVO SHOULD
ee r-nEceotD tr A PCTAILCO STUDY or (ROLOOICAL STHUCTUAC, TO PERMIT A
*0*E INTCLLifiCNT IELECTIOU Or DRILL 8ITC6.
THE COST or THE ttOtOQioAL KTUOY WILL DE ArmoxiHATELY i 2500. 00.
THE COM* A * Y HOLDS 36 CLAIHS KEOCHTLY STAKED* in THC
BAIT or HAIHH TownsHi^, DISTRICT or Duoeunv, Pnovmcc or OITAWIO,
NV^OIKIO ft- 143 1 r; TO &-K52I2 iNCLueivc, THEY COIDIST or OKI KLOCK or
24 CONTI6UOVS CLAIMS, COVEX1K9 t- ALL Or LOTS 3, i AKO 6) COKCCSSIOH VI]
WEST MALr or MOUTH n*Lr COMCESSION VI i AU o ALL or LOT 5* Concession V.
THE OTHEN TVD CLAIMS, SOT CONTIftUOVt TO THC ADOVC, COVE* TMC
KOATH XAtr Or THE HOUTH HALr Of LOT 7, COUCCSSIOH IV*
THE &OUTHEAH SOUMOAtY Of THE MO^EKTY II LCSS THAN ONE MILE
of T*t* CAHAOIA* PAoirio RAILWAY A*C T*A*a CAHADA HICHWAY No. 17, At MAIIM
CCHTfE, AOMOAIHATKLY 30 Mlttf WEST OT SUOBUKY.' '
ft OOOKN : ; .-. ,. ; ; ,: .' iVv,.-'. '.^t'-'V;-
.;: - ;'VjlL!-;̂ :^-^'^.i-^'#^^f^^'^^^-/ !^v:'-^)-'.'^-;--?.' ^v-^^ : k'.C'.^^4.4;^'*^
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Moir or THE MOFtwrv (J3 or 36 CL.AIHB) tits NOKTM or THC Sum*
AkO HAY IK ftCACNCO IV A NCV ROAD WHICH LCAVC8 THE TftAK* CAVAOA
HiCHVAY IMMCOIATCVV WC8T Of THC KMHIftH RlVC* CftOBtlHO AND VJHt IN A
f/OATMCASTKHLY DlfttCTlOM* A^^ffOX INATCUY MRALLKL TO THC ^'A*l |M ft i
MA* 9CCN 6WIWT TO fAClUTATC TNC CO***TKUCt 1 0*1 Of A *6W Ct.CC T* l C
L INC.
ID 10 IKCOKO Or ANY ^RCVIOUV niNCKAt OCVCIOPXCNT Off Or AKY
Of POTENTIALLY VALUAtLC HtKCH#U 01 THCIC
THK OCOLOOY or THC AYCA HAS veen HAPPED OK A GCALC or one IKCM
TO OXK HAtr HILC AY TNC OCOLOOICAU DRAHCN or TNC OUT AU t o OEPANTKCHT or
MlMC9 AMD W*fl PU6LICHCO I N 1963 ** CCOLOOICAL flCPOWT NO.M f WITH MAP
hO.r-055, OOVCRINO ItYxA* AND DftUMY TOWHUHIPt, ANO GcOLOOlCAt RC^OMT S0.3D,
HiTH HA* No. 2062, covcftiNO HAINM AMD LORVC TovneHipa. THC roLcowiva micr
DSftCftlPTIOl Or THC C*OLOftY It MUD miNtl^ALLY OH TMC6I KC^ONTl AMO MA^O.
THC OCOMOCK IR TMC AHCA OOHHtTB Of mCCAHVNIA* tCOIKSHTAtY AND
HAflC INTKUtlVff MOCK9* THC BCOIHCNTAMY KOCXS rOltH FAMT Or THC HURONIAN
SYITC1, ANO *CiT ON A SAICMC4T or OUOC* VOLCANIC NOCK* WHICH MAVC ICC*
iwvAcco *Y OMANITIO INTHUSIVCJ*
THI oT*ATio*ArHio eueecitiOM IN THC AHCA 1 0 A B roLtovs, MOM
THC VOUH3MT T O TMC OLOC8TI-
HALKT. BUOAOHVMT ft OOOCN
-
OUVIHK OimiE CYKCC
GA9PRDIC iNtaUBIVCO
INTRUSIVE CONTACT
QUARTZiTE (StRr^NT FORMATION)
AftOitUTC, CALCAREOUS (CBFANOLA
CONGLOMERATE (BRUCE FOftHATiOl)
HlCW-E i^UANTXITK (MlfttlBIAtl FORHATtOM)
CXCYWACKK AtOICLITC (PCCOftt
COMOUOHCOATC (WHIBKCY
Love* AROILLITC (NOHOI
LOWH sUABTZtTC (MATIKtWOA
ORANITE, VOLCANIC AND SEDIMENTARY ROCK
THE SEDIMENTARY ROCKS ARE quiTc met* AMP RELATIVILY
GUT THEY AftX INTERRUPTED SY A SERIES Or rAULTS S1RIKIN4 tAftT-NOR WAST,
iteiOitOlMft TO TNE MUft*AV-*OALOWIN CREEK - FAIRBANK L*KC FAUV.T CVIVEM,
THE roRHATioxQ H&VC tccn roLCCD INTO A ICRICS or UHOAO ANTICLINC&
Alp 6VNCLINE* KMICH HAVE OCEN OREATLY COM^CICATEO BY THC rAWTlN*,
MAO 6NSATLY OISTUR9KD ADJACENT STRATA, AND DY *UVtCqUE*tT C*COROiC i
THERE ARE TWO DISTINCT TYPES or MINERAL OOOSITS in THE
NICKEL SULPHIDE MINEIALlZATION Or THE SUDBURY TV?K OCCURS ON TNE
ROCKS* OUT NO COMMERCIAL DEPOSITS ARE KNOWN IN THE IMMEDIATE
of NAIRN TOWNSHIP*
URANIUM AND THORIUM MINERALIZATION OCCURS IN RELATIVELY THIN SEOS
or QUARTS PESSLK COWLOXERATE HEAR THE SASE or TNC HATIRENDA FORMATION
(UowtR QUARTZITE)* OtOLOotcAL REPORT Ho*l* or THK ONTARIO DEPARTMENT or
HlNES (I960) MOOR l tt* A HUMSE* Of THESE OCCURRENCES IN
HAVKT, OftOADHuiuT A OODEN' :. .••..•'.i'--vV-^-"-^'''' : •'••••'•^''• ; -- '- - .v ; •"•••••••'- -~ .' ••'•'.-; •v.^M,/^,-;^^^^•^^^^^•!i),A^.i?v; --o-:; .:,,:,v- : ..--^i*. :;v.,. -' .t,-,i:-;.v^.te^S
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•-
TO TNS WSST Of HA l KM TOWVlMlP* AHO l* HYHAN AXO DRURY TOW*S*lf TO TMC
NOtTW AKO NORTHEAST.
THESE DEPOSITS AR* SIMILAR IN LITMOLOCY, STRATIGRAPHY AND
MIMCML09Y TO 7KB WRANIUH ORES Of TMC OtlNO RlVfR - U.LIOTT LAKE DISTRICT,
cost 50 h i its TO rut WUT. THE RADIOACTIVE CO^UOMCAAU t eoa OCCUR AT ox
*CA* TMC CAftt Or TMK tUTHtCHOA FORHATIOH| KM l CM UtB UKCOXrOtTMALCY O* TNC
DA9CHCKT COMPtKX. TNC CONOLO^XAATC BCOfl A ftK W8U*UY C ONCCVTMATCO WITH IK
)CO rCCT Of THK CAftKXCHT, 8 0T TMWS A*K M AH^OW HTTEHOED* Of COmOMCfATt
wi THIN THE quAnraiTC roA MUNOUKDB Of fEET ABOVE THE KASEMCIT. THE
THICKNCdt Of TMK V ftAIIUM B CARIRQ e CDg O X KECfl VAHC9 CUCATLYy C UT THI
CCTTC* ORADC9 ANK USU/U.LY C OMflNCO TO WIDTHS Of 5 fCCT OD LC89, A ND RAVCtY
ur TO 12 rccT.
THE KAOIOACTIVft NIHEtAtt OCCUR A* VERY SMALL CM lira IM THE tATNiX
AMO INCI.UOC MONAZITE, Tno*i*niTe, UnAHiniTfl, 'PAAHNEDITK' ADO A VARIETY or
PBOOUCT8 Of THCKR MIKCRALtl OTHER HHTEHALa ARE PVfliTE, MAAXETITC|
) ATATITK AND Jincox.
THE oEfosiT* Ane ocuttveo TO tt or SEOIMENTAITV ORIGIN (riAcc*)
SIMILAR TO TMK SOUTH A/RICA* COLD ANO UftAMIVH BCARINQ COKSLOHCAATCS* TMU
rnonAOLY MKABS THAT BUCK DEPOSITS MILL se WIDESPREAD, e UT IT KAY ALSO OK
EXPCCTEO THAT EOOJIWIC COKCEKTRATIOR8 Of RAHOAOTIVE HINERALO WITMIM THCH
WILL St RCLATIVCtY ITAXC.
AccOftOIKO TO TNC AftNUAL Rtf-ORT Of KERR AOOISO* HlttO LlNITCD f O*
1966 |KFO*TA*T OCfOSITS Of THIS TYFE NAVC SEEK IXOICATEO IV CXTCHSIVC
OtAXOMO O* ILL l *0 IN KOATM CtBTffAL KVXAM TOWNSHIr (CONCESSION V, LOT* 6 4 7)*
THIS LOCATION l* AfMOXIHATCLV 5 WILCS WORTH-MOBTWtIT Of TMC
CLAIKfi NCLO PY I^OtDA COMCA H IR El, ANO WNIOM A*C THC SUOJfCT Of TNI9 ftC*0*T.
HAIKT. DIOADHUMT A OODCN; ;,~-." " - . \ , •''•'• ; :.:'. ; .^ ..y "i ^ " : '
;. :'~ . jJ..;-^: ~ ..'--. ' r '^' — rf^s-vO-V^'v -..^ -- ^*vv^'A ^ f':--.- r .... -. .
-
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o? THETHC MOUTH BOUNDAftV Of TNC MAIN CLAIM t*0u' (34 CLAIMS) It ALSO
THC HODTK BOUNDASYCr KA It* TOWVSNIP, AND A FOVTIOM Of THE 0KOUP CXTKNO*
i-OUTHWAeD TO THC fMKieH RlVtR { l K LOT G). A BIZCAftLC BODY Of
(JlCCY LAKC) LIE* IH THg Ar?*OXIMATC EABT-WCST CCNTAK Of THC
OfOWOCK II KCLL rxPOSCO AWOUMO THf IHONK OF J l COY LAKC, IUT
flATNCH FOMtLY CK^OACO 14 TNS RCHAIHDSn Df TNK 8KOU^* (T COVSItTi AL108T
CXCUUS l VCLY Of TNX 6EOIHC1TARY QOCK& OF TM8 LOWt^ AHO ILL l Tl U*IT
fORKATIO*)) - AdOILLITfif QRCYVACCC AHO SCHIST, TwEKf A*C tOHC MINDM GAOBftO
THU1IVK9 AMD 01S Of TMC LA T C OlAtAIC OY K tt C*0*8CO TNC P*OTC*TY f*OM
?.! 0*Ttiirt9T TO SOUTHIA8T. TNS STRATA tTMIXC MOHTMKAOTttLY, AVD TNC MCCORDCO
01^8 ARK CMICrUT TO TMK KOSTH. THCY ftANOt f R W* NORIZONTAL TO VCMTlCAL,
OUT TNC HAjoniTY Of 09SCHVAT l OH l APPtAR TO DC IN THC AAKttC Or 40 TO CO
DCOftCCt ItORTH*
TWO MAJOI KOATNCAST fAULTS C*05* THC MO*e*TY f ROM KOUTHWCIT TO
NORTH tACT. THK KOATHCMLY FAULT ft CAUCD THC FAIR0ANK UXC FAULT AVO THC
TOUTNCftLY 0"C THC JlOtY UXC FAULT. &OTH ARC RCOIONAL rCATUKCB AND BOTH
ARC eHAKCHCa Of THC STILL CUCATCR Ht/MAY FAtt/r, HOftT Of TNC fROTCNTY l*
IN THC BLOCK eCTWKCB THf TWO FAULT*.
THC exALLCft OROU? of TWO CLAIM* IN LOT 5, Concession IV, LICA TO
THI COVTH Of TMC HURRAY FAULT. THE O COROCK AT THC B YWfACC Of THIB IROUF
l* QA9DXO, PROBABLY A eiU*H.IKC UTRU9IVC* THC AX|Q Of A MAJOR A WTICLINC
10 WOWH M lBillft THROWN TMC SOUTNCAIT COANCN w P *KI* BLOCK.
HALKT, BHOADHUHIT A OODCN
-
^V-1.-,-^-'.. : 'i;;
t** 6 ***
.PpSSID.iLITIE3 OP T?t;- PROffiTTYt
Txc ceoxonio rosBisitmcs or TMC MO*C*TY DCRKMO o* TMC
t*
?. t
3*
OOtS THC KATIICNOA FOtKATIOK U80HH.lt TMC **0*CRTY?
OOCB IT CONTAIN US A HI UK ItAAIVf eOHCLONKMTC OC09 Of SVTICICVT
(MDft TMICKMCt* AKO CXUVT?
Do TMitf OC^OSIT* OCCUR AT MCAtONAttc DEATHS ron CCONOHIC
tXTXAOTIOH?
Tnt UHfACC *OCKI ItXOMfi TO TMC NOKDIC FOKnATlOH t Dft L Owl*
AftOILUTC UNIT, VHICM OVCRUCt THC KATINCNOA* TMC THICKKES9 Of TMII
vAHdes M OM 100 rctr ON tees ro XOMK TMAH 1500 r err. On TMK
THC TMICKXCbt lit UXKNOVX ANO TNC rROftC(H 10 COMPLICATED IY
Howtvtn, COKE OUTCROPS or SUO-^RCYWACKC (3*) MA ve cerx
RCCOKOCO 11 THK CtHTCt Or LOT 2| COKCftOIOH VI, IMMEDIATELY CAST Of
THC E A ft T aOVHOAffV Of TMC CLAIM ftdOU^, THC 8UO-OftCYWAC*l j O KUC^OItO TO
tt TMC yrps^KOsT MCMBC* of rue MriMCNOA TCAHATION* Ir THIS ihTtnnrr-
ATI01 IB COrtneCT, TNS LOMCR AHOIUITC IS fttXAflVCUY TMI* IN THE CA9TCRK
l*Ant Or Th* PROMRTY fl) LCAtTf
TMC THICKVtfiS 07 TMC PATINCNOA FORMAT l OH 11 THIB AREA IB At e O
li &OUTNWC9TCRH HTHAW TOVICHIP ITB TMICKfitftB 10 ABOUT 400 fCITT
in OHUKY TowxsNii* ABOUT 000 rcrr* I n THC Pu no Riven ARCA TNC
fORHATIOH TNICKCWD COUTMWARO, AMD A TNICKNKBB Of 1 000 fCCT OR SO WBVtO
SK 60*eCIVABtC IN TUX NORTMtRN MRT Of KAIRR TOVWDHir, Howmi, THIS It
OKtv eonjcoTURti TNC THICMCSB oovto SK MUCH BRCATCR THAN 1000 fcrr OB
LCB8| e UT THe fROtABItlTY THAT TNC SA6C Of TNC f B AHA T l O* tICB AT
Of UtBS TNAK 2000 rf(T BCtOW BURfACC, A^fCARB TO BC ftCABONABLY
0000* - ••'.':;-. v .'';-': '"'"\';.-''' :,' :i : ;: ' :/'
ifc^^' :^v.-^-i;:--•Vi**V. ,-'?.i ;l .? ^ '/*X'--^ .'.-.Vv.\.^V\'' *.-. l; . : J' v ",. ''. .
HALCT. BnoADHurur A OODIN
-
TNt OCOUMCKCti MTWT AND quAUTY Of MOtOACTIVE
6 EOS XCAt TMt t ASH Of THK fOUHATlON CAN CC COTAftUWEO OH LV BY 0*IUUN4,
fometY TO OE*TNS of 1000 net oa MO*K. AT A LOCATION rive MILCS
TMC HlAMCar KNOVN MINCKAU Otl*0*ITt Of TMIB TVfK, OK l U. l WO WOULD BC A
niem.v tosovLATivc VCWTURK AT TNC MKHC^T
TMC HCRiro of THE MOPMTV w au m*TuAu.v HAVC TO IK Tcmo
CXFtOSATOty OIAMOMO OftlUIHO, WHICH WILL AU B O Bf ACQUIRED TO
A8iC38tCWT MMK WC^UI RCMCXT).
Dcrons Atrv DKiuuma is ATTKMPTCO, THKAI gtio'juo ec A
traonr or THE *u*fAcc ctotoor, WITH HAMIKO AT A &CHUK or ^00 peer 70 TMK
men, WITH MRTieuuAd cn^HAnia on STRATIGRAPHY AKO fruucTyof 11 THE
CAaTCftn MftT Of TMB MOPIJITY*
TMR r.n^T of THE OCOUOOICAU HTUDV OHOJUO na AOOUT vSSOO.OO,
TMU MIUU fCtHiT A **pfit urirt.uiORVT teieoTiOM Of sites AND PAOOAAUC
Of C*fH.O^ATO)*V OftlUU
R, A. COMiUUTINft
mm'-: J,\
010ADMUMT A OODtN
^;^^^;^^4'-;^.:^: ; " * --^vvv. .'^'v-^v'^^j^Si'^X'^, ;;v ^-.a.y. . Jt.V^^ ^±*-^!*a!.,, :f~.*.,,*,r,^t,!t,.*-,*,^ t^yW^fc4A^aitoi.i^jA2li-diy*.-!r*.'si.^
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J-flln* . JCi * ' , ' ' . ' ' ' ' ~:-
4iiesseeea8 NAIRNISBI NAIRN 020
RONDA COPPER MIMES LIMITED, i -r r- ii* in in i n ,n - (((
URANIUM PROPERTY
NAIRN TOWN&IIP, SUDOURY DISTRICT, ONTARIO
; DY
MICHAEL OGDEN, D.A, Se., P.Enc.
CONSULTING GCOUOCIST, ,
' " ,j ~ f'if ' -.
•*w;^ •,--,,'-;V': - ' J~-A.:-'.\--'-I-m^^^-y^W^f^:^ ̂ ••^•:^f*m®ti^#s•Al^-fe^^^::;
'fVy'-JOnONTO^-'ONTARIO ' ' :'*"V AUCUST 16. .1967." ' 'V v ^
*- i , .^j.Y't* . •-.••- -U'V,v-'::-i - V'..'*--? 1''
'feli^'^i^^^Wf^St^^
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FOLLOWING THH ACQUISITION or TIU: PFJOPI f;iv IM TMC O^IINC
Of THIS YCA^i IT WAS RCCOMHF.NOCD DY On. f*. A. llAl.nT THAT A cr.OI.OC l CAL
on COHOUCTCO oven MOST or THE GROUND TO ASCCIITAHJ TMT ACCKOXIHATC
TO TMI: uRAHirtnouo PCOOLC CONCLOUCKATH nofiijon WHICH r'.^pA'-LY
i/ND'Z'U.IES T"C CLAIMS. TlIC OrOL.OC|CAL STUDY, WAD COUOUCTO TV l :*.
WIITC'I V/ITd LOCAL ASSISTANTS, AND MAG UCL'N ADLf. TO l.CTAPt. l en THAT
fo.'TioNs or TIIC rnopcnTY AND it's CNVIRONG Anc cioo r c.n rj :r,^ T O IJASCHCHT
POC.(?, TO RTACII THCM WITH A LIMITCO DRILLING PHOGPA'l. A S":oilT, Of TWO
di T'trtrc n oLcn Ait pfioi'or.ro rou/iorAL KOOTAGI: or A M. MIT pooo n T, AT A
r o-, T or ^.| l ,000.
1) GEOLOGICAL KAP, WCOT SIICCT, 200 r,*: ALI:, cicr.cn, AUCUI.T I9G7.
2) GroLOCicAu HAP, CAST SIICCT, 200 ccALr;, Ococu, AUGUST 1907
3) REPORT ON GKOLOCY or A GROUP OF CLAIMS MCLD OY RONSA COPPCR MIMC3 LIMITCO, R. A. HALLT, JUNI: 2, l'"'-'/
4) HEOLOOICAL f?rronT, //35, 0,0. M. HA inn A-m LOHMC Tm^cniPO, •^- OY R, H. GINN, OOfi
0- ' - 5) GEOLOGICAL RCPORT, #34, O.D.M. HYMAN AND O.-JURY TOWNSHIPS, ^,v OY K. D. CARD, 1965.":K 'f ; 6) GCOLOOICAL RCPORT, //l, O.D.M. URANIUM AND TnO'MUM DCPOOITS,"ii--- A T THE OADC OF THE HURONIUM OY8TCH IN TIIC SuODURY DISTRICT,y^;, ; i. . By J, E. THOMOOH, I960.
ss^SSS^
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: . J .' " , - , .'1 ' , Hi' . ' ' ' . . - ' ,
. ; f ' ' ..2..
IQCATIO.N U ACCfSSi
THE PROPERTY CONSISTS Or 34 CLAIMS IN THE u'ORTM L'AT.Tr.WM
PORTION OF NAIRN TOWNSHIP, DEINC riMns NUMBERS 8-115177 TO S-l-'raiO
Mf cm r, l VE, WHICH ENCOMPASS l-OT 5 IN CONCESSION V,AND IN C.to'.iC'. :;^ l ON VI;
I.OT-. r., 4, 3, AND THE W.i OF THE 11.1; O F LOT ?..
THERE ARE A COUPLE OF OTHER CLAIMS OWJCD OY T*U: COMPANY IN THE
n.'i OF THE li.Is or LOT 7, CONCESSION IV, OUT THESE W-KC. n .n nn-i STICATEO.
THE CLAIM OLOCK IS READILY ACCESSIOLE f)Y C.'tAvCL ROAD rrOM
JUr.T V/C5T Or THE ORIDCE OVER THE SPANISH RIVER ON HlC'iv;AY IV, Tn:. ROAD
CXT:';:SG TO T'E NORTH EAST ALONG THE NORTH SIDE OF TIC: 'ifAfn^i /'i/i v row
A'.OUT six HILEO. GOOD SANDY HUSH ROADS EXTEND NORTH r POM THAT GRAVEL
HOAD INTO THF. SOUTHERN CART OF THE PROPERTY FROM VAIMOUO LOCATIONS, to
THAT OfULLIMO EQUIPMENT HAY READILY OC TAKEN TO Al.MO-T A'JY COMflO'i Of THE
P:IOIM:HTY.
TurnE is NO EVIOLNCE or ANY i-iiEviour. TRI n -.tnn^, M CH-P INC.
niA-:0,'!0 DRILLING OR GEOPHYSICAL SURVEYS Oil THE CLAIM I'.IO'K. li WAG,
lirw'vfR, GTAKf.O A COUPLE OP YEARS AGO AND ALSO 20 YC.ArtS tCFORE THAT,
FROM THE APPEARANCE Or HLAZCS ON THE TREES.
MOST or THC PROPERTY IS CHNTLY ROLLING OR FLAT SAND PLAIN WITH
VERY LITTLC OUTCROP. TlllO TYPE Or TERRAIN IS COVERED WITH NATURAL OlflCI!
AND POPLAR, OR, AS'lN.THC V/EGT PART OF THE GROUND, IS COVERED WITH A 35
YPArt OLD ftCD PlMn PLANTATION.
THE OUTCROPS VfHCHTHCY OCCUR TEND TO DE LARGE AREAS or H|CH ^ V *y'*''. - :" ; ' ". ; '' ; •''• : .v'- : '--'V : - \'',:.-"', '- ; .':. - ; "' - ; ' - - . , . ; v \,, f - . v-";;",nOCKO WITH VCWY OTCCP O IOED. ,^ ; - '\ . ^ 1 ^'^ ; v ^
KM^^^'fti^^ftfeE-^ ̂ ^-^^': ; Jl^ii" ^**^^^#*^^ iM^ZSSISSS
-
TAOLE or. FORHATJQM
Ci-.noj-oic. - PLEISTOCENE AMD RCCCNT, SAND, GnAvnu CLAY, SILT.
ii/ro'iroinAOLC CONTACT (FAULTING)
Pnrr.A^ijUAi^ - LATE CASIC I'lTHUSIVC ROCKD, DlAOAOC AHO CtlVMJC DlAPASC.
l;iTr;ir,i v. CONTACT (FAULTING)
fjr n i" litj^n Y^ j^goup. - ConcLOMCRATE, QUARTZITE, ARC ILL i TT., GMVWACK', AND
THE l R MCTAHOflPHIC CQU l VALF.NTC.
u-ico^foiHAOLE C ONTACT (FAULTING)
VriL':AMr /Inoj^P - VARIOU3 VOLCANIC AND MCTAVOLCAtl l C I'OCKO, NONE Or WHICH
A1C EXPOSED ON THE PROPERTY.
1 L'l '-AN!ir. fin PUP i
WHERE EXPOSED NCARUY, THESE ARE AMYGDALOID, ADD PORPHYRITIC
METAVOLCANICS, AHPHIOOLITE, GARNET AMPHIDOLITE, AMPHDOLITC SCHIST AND
HOft'iP.l.EHDE OYCIIITE.
i j" A 'i i IT H o 11 s C^o Nju^o lyjtAjc:
THIS OLIGOMICTIC QUARTZ-PEDDLE CONCLOMIiPATi; v.-'MCii OCCUUf. IN
TMPI l.r.nnCO AT OR NEAR THE OA5C OF THE SEDIMENTARY SCRIES HAS NOT YET
n^i:; FOUNO IN OUTCROP ON THE PROPERTY,
Cj^.'AL-r-Ji1A!S. (No.G ON THE HAP)
TlllO CONSISTS OF ROUNDED PEDDLES, DOULOERH AdO COUOLES OF
nANOEO ARGILLITE AND CREYWACKE IN VARIOUS ORIENTATION 1*, WITHIN A r.f!
,!p CPI.YV/ACKC MATRIX. THERE IS LITTLE OR NO SHEARING OR TENDENCY or•K?t'-"i - -: . ' -, '
'••^^ PARALLELISM AMOHCDT THE XENOLITHS.
(No.4) : ,: ; . V.. . :. ' ' .-- ; .'- ' — - -,^ ;
TlllO 10 A.-riMC ORAIWEO, GREY CVEN TCXTUREf), ORITTLH, HARD
-
QUARTZITE WHICH IS CSTIMATCO TO OC 400 TO 000 FEET THICK Ml HYMAN
TO'/rfj'IIP TO THE NORTH. THE UftANIFCttOUO PEDDLE CONCLOMfPATE 13 AT THE
|A-;r or THIS FORMATION IN HYMAN AND DRURY TOWNSHIP TO Ti|./ pojt™ AMD
NO'U'I fA3T.
A n r - A/: c o D s G IRE, YWA c ,K r (No, 3)
A GREY TO oorr COLOURED, MEDIUM TO r INI; CHAINED, GRITTY ROCK,
WHICH f'AN HE SCRATCHED WITH A KNIFE AND IS USUALLY qulTC nAJJlVC". Tn (I
nrooi:;r. IF visioLr., is 6 INCHES OR MORE IN THICKNESS.
FINE CRAINEO, EVEN TCXTUflEC) CREENICH ffOC^ VA-.K.H "A^ELY
o'', c 'j r? r,.
/V',r.. |V.'JJJL ("0 - 1 )
TlllS, THE HOr.T COMMON ROCK UNDERLYING TMl. PffOffrTV l \VLL
nr.nncn, FINE cPAiNro WITH A LIGHT AND DARK DKNDINC, -.^ cio r. f tor - ;T,:rff
AO TO REGEMDLE VARVED CLAYO. IT ALSO OCCURS AS lCn\c\T: o r 'i'r.T f!-S)
f) (l AO 5TAU!fOLITE SJHIST (l-ST), THE I.ATTEH DICPLAY 1 , A'-'J-nA'.'T STAufOLITE
rny.TALs UP TO l INCH IN LENGTH.
OJA/VA^E: (No. 5)
TllEf(E ARE TWO T YI'ES O F T HIS ftOCK. THE PATHr.fj FI NT. CHAINED
i-Y'.'iric niAOAnc (No. 5) WHICH OCCURS AS IRREGULAR I'jrf.-no^-vf.--, Gfic'TiMcs
fit:Af* COIITACTS OR ALONG FAULT PLANES. Tun OTHER TYPE, THE urn i -."i TO
coARor GRAINED OLIVENE OIAOASE OR CAnnno-oioRiTE ( r*-o) occurs A". A WIDE
PYKf rnOSSIHC THE PROPERTY AND 10 DETEf-TAOLE OY A l i:f Onitf M ACI//T | c SURVEY.
fl; - ! TtUO CONSISTS OF ANGULAR PIECES OF ARGILLITE AND AREN••r r/- *vi'-'i vi--. 1 .
f ffi S?" '•-- ' "' ; v .- ' ' X p|^^ OnKYWACKC, '.l H A MAlHIX OF CftlTTY CflCYWACKE, OCCASIONALLY WITH P IECES OF
|;^{v ; ] ' oiAnAoc. TiiEne la DISTINCT SHEAHIHC IN A CONSIOTANT OIRCCTIOH AND A
^;:-. '; ; ; PARALLELISM , TO 7HC OROKEN PICCE5 OF HOCK. :, ; 1 ",' ; ,
-
n L:oi. PC (CAI SURVEY;
l ri ORDER T O MAINTAIN C ONTROL Of THE HAPPI'.'C, T HHLC 1. 1 Mr 5
wrnr CHAINED AND PICKETED, EAST-WEST ACROSS THE PRO^PTV. i M:C ,'j,
TXT SOUTHERLY one WAS ALONG THE BOUNDARY OETWHCN TH- FIFTH AND SIXTH
CONCUSSION. LINE #0, THE ?JORTH LINK AOOUT MOO recT r.'onr-: or #1 , is
m: T we e H NAIRN AND HYMAN TOWNSHIPS. Tun MIDDLE LINT f1?, WAS A DIT WORTH
or MAt.r WAY OCTWETN THC O THEns, A LONG TMC NORTH Gl'Oir. or J|CCY lAKC.
TriAvrnsc LINCO WCIIE RUM NORTH AHO SOUTH OCTWCCN TIU pc^:i:r i. mi;.- AT AH
Avr.HACr. IIITCRVAL OF 400 FECT.
THC SEQUENCE OF DEPOSITION ACCORDING TO ^Ifj'j A'.'O CAOO IN THE
TOUNSHIPO HAS THC qiiAnTZiTE AS Tin: LOWCST II-IMATION JH^T ADOVE TMC
OA'.i'MEUT VOLCANICS AND GRANITES. THE URAN l FKROUS frntu.i: r U', ;i o ;! '.'ATT WU l CM
v/A", -IOT RCCOCNI2CO IN flAIRN TOWNSHIP HAS DEL'N FOONn AT Tnf. DA5C OK THIS
SPRITS IN HYMAN AND OnufJY TOWNSHIPS TO THE NORTH.
THC CREWACKCS AND ARCILLITCn WHICH OVf.M.IV Tur O'AKTZITC ARC
O'lVIOOCLY IMTCRMIXED AND CANNOT OE USED AS A MARKER HOR|?0?1 Of ANY SORT.
THE CONGLOMERATE (h'0.6) HAS OECN CALLED A FAULT OKCCCIA OY
ClNJJ, OUT l AM OURH IT 1C A COMCLOMCKATf AND l flCLirvc |T TO (T VERY
LOW DOWN IN THE STRATACRAfMIIC Cr.QUCNCE, PERHAPS rvrn HCAif Ttir OOTTOM
Gf P IC O.UART2ITE. IT 13 MORC RADIOACTIVE IN AT LCAST O lir. LOCATION, THAN
ANY OF THE OTHER ROCKS, WHICH MAY DC DUE TO A LITTLC ENCLOSED l/RANIFEROUS
CONGLOMERATE.
-
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* * f * *
l. As Tiicrjc is NO SU.JFACG CXPOOURF. OF THE URANIUM tuA-i.'jc
r-roni.r concLonrnATC, one CANNOT DC CERTAIN wnruc IT rxitjTc u:;;o) THC
CLAIM DLOCK, H OUC VF. ft, TUT. RAM O ACTIVITY OF Tilt CON1LOM' RAT : , WtlCH
l r. C.ONOIOCRCO TO OC WITHIN A FCW HUNDRED FF.TT OF TM' U'-A'JIUM 01.0, IT.
Hir.i'LY CUCOESTIVF. THAT IT HAY OC PRCr.'JNT.
?., T HC PRF.f.CNT DURVCY HAS IMOICATIO THAT T'"f 'Tr Ar A'.'",fH l C
LOCATION OF THE URANIUM 20IIC IT. PROCAOLY V/ITHItl l O rVJ i ' * or T'K
, on OR NTA" THE CAT.T OOUNOARY OF THE PROPERTY. A COUPLT OF
io nniLL HOLCO Anr. R^COHMP.HOEO TO MiTfritcccT IT A'*n Asrvrfin ITS t
T l'
THF. LOCATIONS AT WHICH T HI: uAscnruT ROC'" A M o m-r^ivinc
JM zone, IF purs''IT, wCiuLn or cLor,r.r,r TO f 1 " c-rv-jT ^ TAT.
A'h A", FOLLOWS:-
(A) IN CLAIM P-USIOO, NFAK THC TACT po-'MnAfv or T.*C i-foci
A VfllTICAL HOLT, CULLARK^ l 'i THC QUARTZITT O'l Tt" '.'AKTI' r'ir.' ^ i nr
OUTCflOP SHOULD CUCOUUTCn THC OACCMCNT HOCK^ UlTHCj ' -\J T O )5 0''' ri''.;T.
A VCUTICAL HOLC WOULD AVOID CUTTING TUT NEAPI1Y FAULT 70S! r.OH,: 600 FECT
TO T'lF. SOUTH.
(n) A vcftTicAL HOLE OF 1200 TO 1000 r, i'T r. L i- nr.TH in THE
Al'A'IOOHCD FARM FICLO VfOULO PROOAOLY CIICOUNTCH Till fiACCMC'lT ffCKS. A
MAJOn ANTICLINAL AXIS TXTCNDO TlinOUOH Tilt: f MILO V."MCn If; Tii'ii THE
VICINITY OF THC OLOCSTCXPOSCD ROCKS.
A. THC ANTICIPATCO COST FOH 2000 FOOT ftRILI. Pl!f).-.r(AM | fj TWO HOLE*
1C APPROXIMATELY ^11,000.
Rr.r.P r CTFutLY si
^^-.^^MM^^U.^^^-^.^.;,. . , .'t ..4 . -'" ' - -'- " * f -'~ - ."T* .•*H*Wt~.*^.^...,1
-
CERTIFICATE
M
l. W. MICHAEL H. OGDEN, or THE CITY or TORONTO, IN
THE: PROVINCE or ONTARIO, HEREBY CERTIFY AS FOLLOWS i
i.
2.
3.
4.
THAT l AN A CONSULTING MINING GEOLOGIST, AND THAT tKAINTAIN AN OFFICE IN TORONTO, ONTARIO,
THAT l AN A GRADUATE IN APPLIED SOCENOE (KININQ GEOLOOY) FRON THC UNIVERSITY OF TORONTO, A REGISTERED PROFC&SIONAL ENGINEER IN THE PROVINCE OF ONTARIO, AND THAT t HAVE OECNPRACTISING NY PROFESSION FOR SEVCNTEEN YEARS.
THAT l HAVE NO INTEREST, EITHER DIRECTOR OR INDIRECT, ANDDO NOT EXPECT TO RECEIVE ANY INTEREST IN THE PROPERTIES, OR IN THE SECURITIES OF RONOA COPPER MINES LtWTED.
THAT THIS REPORT IS BASED ON A PERSONAL KNOWLEDGE AND EXAMINATION OP THE PROPERTY, AND ON GEOLOGICAL REPORTS REFERRED TO IN "REFERENCES11 OF THIS REPORT.
MICHAEL OGDEN;
DATED AT TORONTO, ONTARIO THIS I6TH DAY OF AUGUST, 1967.
I