rpt on the geol on the geol of a group of cls nairn twp · 2017. 1. 17. · similar to tmk south...

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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;^'*^

  • 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

  • •-

    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 .... -. .

  • -';S'

    'jfe

    .t.

    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.^

    ''- -

  • 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^^

  • k -t.

    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^

  • : . 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