vlem sur rpt moberly & thorburn twps · oaa rock outcrop i* kaawa to k* pr ***at a* tk*...

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63 42A13SE0897 63.1512 MOBERLY 010 Report 9* tk* VattUal LAO* JU9*tro*Bafaati* Coadmct*d am tka Pffaaavty *f Mobwly aad Tkorbura Tawaakipa - Porcvpiaa iftatof JMtiaiaa af OataH*. nft**a vertical loop *J9cti'o*naf**tlc Mia*a*jl*i **t* omtliaad am tk* property. s*y*a of taaaa aaMMt ajialitiaa wait* a*a ia*avav*t9a t* coaAtativ* aaat9rtai U Ut* ^aaVaak af tk* prop*rtjr. TaU aaHttiv* aaa*mriaA y b* *ith*r *aip*i*:* niaayaUaatioa or frapaltU CONCLUSIONS} Tk* aaaoaalia* aya all t*w*a by glaaiai 4*aa)*Ma aad a** *iiaata4 ia a goolofical o*.viraain*at lavoraal* fay Ika praaaaa* af ka** aM*al *kia*ral d*po*itioa. It i* v*c0aiva*a**d tkat *aoni*lio* VI , Vi. V)* Vi. V7, Vf aad VI* b* iav**tifat*d by at l*a*t aa* drIU kala. Tkia waald *at*ll XMO faat af diaaaea* drilliag at aa **tiaiat*d co.! of |2ft Tk* iacatioa of tka *r*a r*eo*Bm*ad*d drtti kalaa aad ard*r af drilUag i* a* follow*:* Hoi* No. Papamr* Latttad* *ariag(A*t) gta- i.*agtk It. 64-1 Ua* 20^00 JEaat 40+50 N. of B. L. M 44** *l* 904 44-2 Lin. 4400 Wot 7+WN. o/B, L. N 44' I fi* tOO 44*3 Uiu 24+00 W.tt 4+SON. ofB. L. K 44** W 140 44*4 Lin* 40+00 W**t 24243. of B. L. N 44* M 14* it* 44-f Llao 14440 W**t 21+SO N. of B. I*. 1144 s* S SI* W4 44-4 Uaa 4+00 JU.t 14+15 W. of B. L. M 49* A li* 444 s 44-7 Ua* 24+04 *aat 14+15 M. of B. L, If 44* X 55* Any succtta la aay af til* abov* kol*4 voald *atail drill footaf * *v*r aad abov* tkat r*coanaa*ad*d.

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Page 1: VLEM SUR RPT MOBERLY & THORBURN TWPS · Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to

63

42A13SE0897 63.1512 MOBERLY 010

Report 9* tk* VattUal LAO* JU9*tro*Bafaati* Coadmct*d am tka Pffaaavty *f

Mobwly aad Tkorbura Tawaakipa - Porcvpiaa iftatof JMtiaiaaaf OataH*.

nft**a vertical loop *J9cti'o*naf**tlc Mia*a*jl*i **t* omtliaad am tk* property. s*y*a of taaaa aaMMt ajialitiaa wait* a*a ia*avav*t9a t* coaAtativ* aaat9rtai U Ut* ^aaVaak af tk* prop*rtjr. TaU aaHttiv* aaa*mriaA

y b* *ith*r *aip*i*:* niaayaUaatioa or frapaltU

CONCLUSIONS}

Tk* aaaoaalia* aya all t*w*a by glaaiai 4*aa)*Ma aad a** *iiaata4 ia a goolofical o*.viraain*at lavoraal* fay Ika praaaaa* af ka** aM*al *kia*ral d*po*itioa.

It i* v*c0aiva*a**d tkat *aoni*lio* VI , Vi. V)* Vi. V7, Vf aad VI* b* iav**tifat*d by at l*a*t aa* drIU kala. Tkia waald *at*ll XMO faat af diaaaea* drilliag at aa **tiaiat*d co.! of |2ft

Tk* iacatioa of tka *r*a r*eo*Bm*ad*d drtti kalaa aad ard*r af drilUag i* a* follow*:*

Hoi* No. Papamr* Latttad* *ariag(A*t) gta- i.*agtk It.

64-1 Ua* 20^00 JEaat 40+50 N. of B. L. M 44** *l* 904

44-2 Lin. 4400 Wot 7+WN. o/B, L. N 44' I fi* tOO

44*3 Uiu 24+00 W.tt 4+SON. ofB. L. K 44** W 140

44*4 Lin* 40+00 W**t 24243. of B. L. N 44* M 14* it*

44-f Llao 14440 W**t 21+SO N. of B. I*. 1144s* S SI* W4

44-4 Uaa 4+00 JU.t 14+15 W. of B. L. M 49* A li* 444s

44-7 Ua* 24+04 *aat 14+15 M. of B. L, If 44* X 55*

Any succtta la aay af til* abov* kol*4 voald *atail drill footaf * *v*r aad abov* tkat r*coanaa*ad*d.

Page 2: VLEM SUR RPT MOBERLY & THORBURN TWPS · Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to

-i*

PHOPSKTT, LOCATION. ACCOt.

Tk* prep*** of Mor A Haakte Mtettal Jdiaa* UvOtod **a*i*t* f *tety-f**r (44) taatigaoa*. vara* *a? ad aad *apat*at*d Mteiag aUfcft*. Tkay ar* ommbered P-fOltO to P-MWf te*kj*f**, P-m*4 to P*ft**ftiaclatire aad P-41 t*l to P-4149f tecteaiv*. Tk* araa ** tk* *Ute* gf *ap U 2346 acr**, mor* or i****

Tk* cUlaa group U located *lBM*t **tir*tf ia ta* cora*r of M***?iy Taw**aip t alta*vga pa*t *f td* elalv gr*ap th* a^oiaiag Tm*aip *f Tk*r*urm, aU tacatoA te A* P*r**p4m* MRaUg Divivioa. U ta* Proirta** af

Ac***a to ta* pr*p*rtf i* tait* lffl*alt. Ta*v* ar* a* r*aa* witaU **v*rai aaU** of th* py*p*rtf M a*r ar* ta*r* aay **aj** of watwr vaiea eaa 6* v**d a* a laavlag fl*W fat aki o* fl*a*-**.aipp*4 airaraff. Ik* most practical a*aa* *f a***** i* ay k*li**ptor f raw la* towa -*f . TUnnsiai , Qatar to. Ta* ai*taac* front HauMiaa to ta* pr*p*tt| U akaajt M air nil**.

Ta* *arfa** of tk* pr*p*rty U Hat aa* w**a**U atially of vpruc*, jaakpla* aa4 miaor poplar. tk*r* ar* a* larg* or river* oa tk* property.

MSTORTt-"-Si-,

Tk* property waa *tak*4 to eor*r a aro*4* aigk iatoatity * aortkw**t trikiag a*roaaaga*tl* aaomaty. fallovtag ta* aaa**a*at*i*at af Tk* Twtaa Oalf Sttlpkar ba** m*tal **po*tt ia XU4 T^racaip.

Tkar* i* ao r**or4 or *vid*ac* *f aval**atoty vatk kavteg Ma* p*rforai*4 aa tk* claim gr*vp, prior to it'* acfaiaittaa ky Nartk ilaakia Jttak*! Miaa* Limited.

la Ifftft, Nortk Aaakia Nick*! Uia*t Umitad p*rf*r**4 a maga*ticaad k*riaoatal loop *l**tromagaatia *arv*y *v*r tk* aialvi gramp at a pick*tUa* iatorval of 400 f**t.

For detail* of aad tk* r**vlt* *ataia*d te tk*aa moNraya * erne i* r*f*rrad to tk* report oa tk* akova te tk* coatpaay1 * fil** aad dated April Il*t, HaS.

PRQPJJtTY OS.OLOGY; i

Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to e*T*r*d ky

glacial d*po*it*, **tiaiatad to ka te *ma*a of 190 f**t te d*ptk. vartteally.

Page 3: VLEM SUR RPT MOBERLY & THORBURN TWPS · Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to

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Baeed oa tt* pattera of i**a*ag**tU lia** aad **g**tic ' gradleat* ol tke greaad ataf**tic **rr*y , it it iatorpretod tkat tt* Mrtk**M two-third* ol til* property i* *ad*rlaia by a c*wple* at K**watia lav** awl miaor **dioa*ate. Tk* eevtk oae-tkird of tke property l* aadarUia ay **tfc*r graalt* mad/or sediment* . Td* maia oeatact **tw*** Hi* tw* t**ttifirtyMt ait* i* Irregular Md lo**i*d a*eot 1000 feet to*ta *f tb* kM* Ua* Md ur l*c* paralUl* it.

VJCHTICAL LOOP SL&CTaOMAOHETlC

A dval fr*^tt**cy v*rti**l aUetVMMf aatic awrrvy vsiaf tk* 1000/5000 cycU *fttipvMt wa* elaiao gr**p. A miaiama

Tai* *l*ctrowafa*ttc t**a*i*ja* ia*a*m*** ta* ia*HaatJM *r dip at iaga*tie li*ld la d*fr***. '

F, M f, h *l*ct*v)mafa*tic aaMaaJi** w*r* ovtliaad awl tk*** depicted ia tae aceootpaayiaf plaa* a* Vi t* T14

Aaomeiy V l;, occvr* aa claim* P-IUO awl F-ttttt. ft i* 1600 f**t la length ead *triko N M* W. It l* a law aeafaitade t**yawM, mitexaibit* moderate to food eoadvettvity.

Ta*r* i* ao appreciable magaatic r***em** or** til* **wte*f*r * OeoiogicmUy it Ues to ta* *a*t el a a*vta****tR ttrikiag dlaka** dyke.

Attorney VI;- Uee oa claiv F-fttfl. ft i* a low MvpUlad* r*af oa** *awl eakibiu poor to lair coadvetivity^ It i* ab*tit UOf l*et to leaftk awl *am*alire ody i* steeply dippiag. Tkere U good dir**t mafaetlt carrelatioa vitk ta* MM t*l over 4000 gajmnae . It womld appear taat tai* *oadM*t*v U da* to eitiier mlaaide miaeraliaatioa or graphite ia aa vltrakajte aody. '; 4

Aaoroely V 3;* tale aaeeaaly U*e eoatacaet W T I, aa elalaM P-*144f, 41*14 aad 61 Ml. It i* akwtt 000 feat la l*a|tk aad *wdkit* p**r to Moderate eoadttctivity. Tke vertical loop retpeae* i* ceiaeidaat witk a majaeti* Meieaiy ol *ver SOOt gamma* aad it alao c*la*id*4 vitk a aoviaoatal l^op E. M* Mewaly.

It i* laterpreted taat ta* Mowaly, Uk* V X. i* d*c to aitaer emlpkid* nlaeraUaatioa or grapaito U aamlttaaa*i* awty.

"' -! f i. ' - " " * ,'' -

Aaoeaaiy V 4i* lie* ea ciaUa F-IUT1. h U awMt 40* fe*t ia l*aftk aad vertical ia dip. Coadactiyity le g*od. Tk)*r*i* a* ajaga*H* r**a*aa* *m ta* aa**, - ' ; . ' , ' . * ' ' -. ^ ^~-/ . -V' \ " '

' '\:'5". ' ' '""

Aaomaly V Si- located aa date P-Hlt3. It *trik*. M if* W aad U 4ft feet ia l*agtk. It appear* to a* *t*ep la di** Tke aaewaly edkfbit* caadactivity awl it l* located b*tw*ea two preaimac*d aiafa*1lc *

Page 4: VLEM SUR RPT MOBERLY & THORBURN TWPS · Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to

-d*

Tbara to a broad 100 gamma ralial dtroctty avar tfca coadvator.

It ia totarpratad taat tb.a aaomaly to probably aa*aad ay a maar aeaa.

Aawaly Y 4:* Uaa aa atolma P-414W aad ?*4l4tf . tt to UOO laat to laagta , strike* N Id* W MA Atoa taeply ta tke a***. Ceadvettvity variaa Iron poor to good aloag atrika*

It i* located to a aUgfct mag aatU dopvaaeioa* , Oaaked by twa aaattlva Mooaaliee of about 709 gaauaae abave baakfroMd*

Tml* anomaly ia dna to vitkar mtoayaltoatloa or grafaitto adtoMata.

Aaomaly Y Tt* Uaa aortawa*t al Y i aaA vara ar toaa an atrika, H ia aaa*t 000 faat ia Ungtii Md r.rtiaal to Ato. It aMlMta food coadmattTity aaajractarUtic*. Uka V 9 , it to toibravatad ta aa aauaad ay Mlphida mtoaraUaatiaaor graphitic dim out*. -

AaaiBaly VOi* occmr* oa elaim ^-fWf I MA MO laat aartk al Y 2 MAparaUal to it. It i* a low magaitado raaaawaa aaA axAactivtty af taa aaaa to gaad to axeallaat. It i* aitaatad aa th* Haak al a aigh iataaaity Magaatit aaamaly. Taa aaaca of tait ro*f nasa could waU aa Aaa la Mtoaraltoatto* to kadrock al tfea praparty. ,

Anomaly Y 9t- tait anomaly lias oa t)**** P-414tt , M299 MA 414*4. It i* about 1400 faat to loagtfc aad ttaaply dipptog. .CaaAaftMty al tka aaaa atoag atrika variaa Iraaa good ta axaaliaat. llkajra to aa appf aatobla magaatto raapaaaa oro tka aoaa aaA aaar tka totttkoaM aaA ( a aarta-a*Mfc dtotaaa diha abaat 100 laat to width cut* acroia tha aeoau

A waak aartooatal loaf aaaoaaty (O) to cotoaidaat witk tlM vartiaal laaa aaaoMly*

Tai* Manaly ia Aaa to aitkar avtaMAa miaaraUaatioa ar grapaitte aAtooaita.

Y 10;- Uaa a* elatoa P-SIM9 . MA MMt 000 laat to laag*. It ia a law ajaplitad* aaojnaly MA aadmathritf to aaar ta fair. It trawto at 90 dagraai to a low iataaaity magaatic aaawaJy .

Tbia aaanalama aoao apaaart to Ha camaad by a caadaatfra haar aoaa ar ovarbuvdaa.

Ajanatyjrii t- it to * aaa Itoa Maaaaly lytog abo*t 100 laat aorta al aortkwaat avtramity al Y f* Coadoctivity to poor to madarata* typtoal ala

roopoaca obtatoad oror shaar aoaaa.

Page 5: VLEM SUR RPT MOBERLY & THORBURN TWPS · Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to

. i *

Aa**a*ly Y lil* tala aa**aaly l* ft ***-Ua* r**poa** **at*r *d ea *iaiaa P-St2H* H i* a low tatoa*itjr r***oa** aad to* tfc* *araav)t* *l a eoadactiv* ov*rbvrd*a or a *a*av **a*.

Aa*aaaly V Hi* occur* o* elate P-ftit*t aa4 200 l**t aorta*a*t of ta* *a*t *ad of aaoasaly V f. Ta* w**t *Btr*ttity *l la* aaMaaly l* M*i*tly a aifli if*qtt*acy r*apoa** aa* proe**4iaf *a*t*rly ( cawlMttvltg top r*r**cua*id*ra*ly. Th* aaoaaaly a0a**jr* to trik*-off in* tJM aaj+ialaj Hit* V f, ta*r* t* a* aypr*ciaM* aoapxti* r****a**

Aaoaaaly V 14;- U lo*at*4 *m *l*4m* F-UU4 aa* P-Ulf i. HI* 1000 i**t la Uagth a*4 *t*ik** N SO* V. Ta* e*tt*ativ* bo4y coal* ** mp

to 100 I**t ia widU. C*MMcttvttf r*ri** ITMI fair to f*od. Ta*r* t* a aao4**t mAfovtic r**poa** *oia*id**J vita ta* w**fc p**t of ta*ja*BHlf, amt ta* maga*tU aa*OMly it**ll tread* **Ufa*ly to ta* atrlk* of ta* fi. M,

It i* iat*rpv*t*A taat ta* *n*m*ly t* da* to mOaaM* amia*rali*atioa graphitic *4ian*at*. ,

Aaomaly V l i; - l**at*4 *lmo*t *aUr*iy oa eUima P-41**4 aad P-*U*7. It ctrik** WWW. a*tv*ao*ote aad Mor* *tr MM* I*tl*vf a a*rta- oata M*fMtic tr*a4* Utorpr*t*4 to r*pr***at a aiaaa** dim*. Ta* irtigaifi*f ta* r** pea*** i* aot fr*at* aar di* tine t f *oa**fa**4ty * ta* aa**matjr aaayw*U a* dw* to cuodaettr* *v*r*mvd*a.

Frotn maga*tU d*ta, d*pth gl *T**bttx4L*a ia aroaad ta* *l**tri*al aaoaaaiott* araa* af ta* prop*rty fga*at* to k* a***t 100 to 110 f**t.

M. JB. M. CONSULTAKTS LUfl TO).

MZ/vp

Page 6: VLEM SUR RPT MOBERLY & THORBURN TWPS · Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to

42AI3SE0897 63.1512 MOBERLY 020Report on the Magnetic and Electromagnetic Surveyson the Property of

NORTH RANKIN NICKEL MINES LIMITED Moberly and Thorburn Townships - Porcupine Mining DivisionProvince of Ontario

SUMMARY

The property of North Rankin Nickel Mines Limited consists of aixty-four (64) contiguous unsurveyedj and unpatented mining claims and are situated in the northeast and northwest corners of tile townships of Moberly and Thorburn respectively, all in the Porcupine Mining Divisionof the Province of Ontario. * :

There are no rock outcrops on the property and the surface is covered by a varying thickness of glacial debris, mostly clay.

The property was acquired by staking to cover an airborne xnagnetie anomaly, following the announcement of a majfcr base metal discovery by the Texas Gulf Sulphur Company in Kidd township.

CONCLUSIONS

Based entirely on the pattern of isomagnetic lines and magnetic gradients of the recently completed ground magnetic survey, it is interpreted that the northeast two-thirds of the property i* underlain by a complex of Keewatin lavas and minor sediments. The southwest one-third of the property is underlain by either granite or sediments. The main contact between the two stratigraphic units is irregular and more or less, parallels the base line of the property.

Sills of peridotite or gabbro intrude the lava-sediment complex. Northerly striking diabase dikes intrude all the above rock*.The general strike of the rocks on the property is K 45"W, astronomic and dips are steep.

Ten electromagnetic anomalies wart outlined. These are weak in magnitude, narrow in width and exhibit poor conductivity characteristics. It is interpreted that these anomalies are probably caused by conductive overburden, although there is a remote possibility that several may be dueto poorly conductive material in the bedrock.

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Further exploratory work, prior to any contemplated program of diamond drilling, should consist of additional check geoffeysic&l surveying utilizing another electromagnetic technique. ,;*

Sufficient assessment c redits are available from the w*rk preformed,to keep the claims in good standing until April 27th.

RECOMMENDATIONS

It is recommended that all the horizontal -loop electromagnetic anomalies outlined on the property be surveyed i* detail by the vertical loop electromagnetic technique in order to provide additional information towards interpretation of these anomalies. IB addition, it le recommended - . ' that the survey be extended to cover the areas interpreted to be underlain by basic sill -like bodies on the property;

The cost of this additional geophysical work i* estimated at |3,00t.f0,maximum. . -- '' .-: " . :^./ ,. . "- ,. ' - .

-. - ' '" ' : ~ v J' *

Upon completion of this survey work, a more intelligent decision aa to whether or not further investigation of the property by diamond drilliag i*warranted. ' r ,.

. . ' ' ' -r : : :, "

PROPSRT Y . LOCATION , ACCgSS, ETC.

The property of North Rankin Nickel Mi ne a Limited cozulate of four (64) contiguous, unsurveyed and unpatented mining claim^i They numbered P-58300 to P-53309 inclusive, F -58264 to i F-5S299 ISiclaWr P-61482 to P-61699 inclusive. The area of the claim group i* Z 56 O acres,more or less.

The claim group is located almost entirely in the n^rtheaat Moberly Township, although part of the claim g rot^ ekttakd* into t2M Township of Thorburn, all located in the Porcupine Mining Division, in the Province of Ontario.

Access to the property is quite difficult. There are no roads several miles of the property, aar are there any todies of water wMcfe can be used as a landing field for ski or float -equipped aircraft. The most practical means of access is by helicopter from the town of Tixgminc, Ontario. The distance from Timmins to tfee property is about 28 air mile*.

The surface of the property i* flat and woeded. f he forest 40xt*ista ^essentially of spruce, jackpine and minor poplar . There a*e no Iarg4i'or rivers on the property. -? - ^

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HISTORY

There i a no evidence, nor are there any recoil* *f exploratorywork having been performed on this property.

The property was staked to coyer a broad. Ugh intensity, northwest striking aeromagnetic anomaly. ThU staking followed th* discovery of Texas Gulf Sulphur base metal deposit in Kidd Township.

PROPERTY GEOLOGY

-l - * ' G ',

There arc no rockfoutcrgps cm the property an4fiB r that matter there appears to be no rock outcrops in the entire township of Mobfurly , Thebedrock surface im covered by a varying thicknet* of glacial depQfit*.

GEOPHYSICAL SURVEYS1 . - " * IT. ' " ' . j*- - , . ^ '

The Magnetic Survey was performed usjng a MF- 1 FlujKgate It measures the vertical component of the earth's magttetKllold, shown on the accompanying plan to the scale of one ii^ equal* -0* feet.

The main trend of i somagnetic tines i a N . 4S* Vt af^rejaMTbjc . The magnetic background of the northeast two -thirds of the property is almost twice that of the southwest one-third, This magnetic xaBtlf**t vtxggvtta Us*; presence of a geological contact between two distiiu^ fO)(^**q\**nc**. tt is interpreted that the northeast two -thirds of the property by lava flows with minor sedimentary rocks. The ' third of th* property are either granite or sodiments. the two distinct rock types is irregular and itoOre or i^*4 r pATAils^ll the base line and strikes North 45" West, a st ronftnaic. Aloaf Ul*s contact and wUMn the lava complex, there are a series of ft&oz&glous aojwtitioxuir of rather bifk : magnetic susceptibility. These ate interpreted to b* cattlted by several tabular bodies of basic rock, either periodotite or gabbro in coiapo^ition,

A secondary pattern of magnetic an*ra4io*ji"COJ&dUitfM. W*t0 These are fairly narrow in width, of fair ass^itilde and stslXje ia a direction. These are interpreted to be caused by dlahtte* dUte*. Twin dik*foccur in the \frest part of the property, ^wo others occur ,'it.^w. *Sj*t fcfif C * the property. * '~

* ' i " . J " ' ' w

Several fault zones are interpreted to be present. On* luit occurs the northwest part of the property, it strikes North 45' Eiilti'JFke main of basic, sill-like, intrusives appear to b* off set by this structure. In movement along this fault appears to be pr e-diabase. Aaother f4uit ccur* i*; the northeast corner of the property. Thor* appearf^to be som* dis|tlacemsttK; of the diabase dikes in this area. Strike of this assumed fault' ay^eajrs to B* about North 6 0" West. '

Page 9: VLEM SUR RPT MOBERLY & THORBURN TWPS · Oaa rock outcrop i* kaawa to k* pr ***at a* tk* pr*p*rty. tt i* loaatad ia ta* aartkv**t part of claim P-St 3 00. Tk* rot of tk* pr*p*rty to

- 4 -

From magnetic data, depth of overburden in the anomalous area*of the property to be 100 feet, minimum.

T lv: --i 'i r /i-:-;/ v/as conducted using a Ronka Mark 4. Horizontal Loop elect L o nr.igr.c'ii .. .mi- u.u lining a coil separation of 300 feet and a frequency o i 8/6 f - , '.'. -: . Phis notriod measures che in -phase and out-of-phase cou: pone i; i j ..u ;;ic- tici.ui.diir/ magnetic field in terms oi percent of normal or uniform f i do, ;v^iio?; of the in -phase to out-of-phase readings are considered tc civ'-.1 lil ci lv, a i, i o rv c .-i , ondd.cuivity oi causative bodies. A coil separation of 300 :^-.-t w;..--. ,!t,c-d ^i/inp; a :!epL.ti penetration in the o rder of 1 25 to 150 feet.

uieTin c - -: - .'. :. /oy revealed ten anomalous zones. These are indicated on o.^;p:'Jiyine ::ir;i. ;,i." the c-L:: :tromagnetic sui'vey as A to J inclusive.

l i. t'"-e -- .iccfic-. iles outlined are weak in magnitude^ narrow in width ;.ii'Hi exhil-it pooi condutaivity ...naracieristios. Although several show magnetic coinciderx c Li is nc/orthci.ijas interpreted tha; the anomalies outlined arc pvimaiilv fau;:i;:.i by conductive clay overburden, i here is a possibility that i; e v eva', .c tile anornuues uiay o e caused by pooily conductive material in the Oydro-ci:. and covtraci uy glacial deposits in excess of 100 feet in depth. Ur.de t Uv?.-.'e - onditiom-. t li c- horizontal loop equipment, with a 300 foot coil SfVJai.-ttLor; , '.s o'K-ratinf' ac the limits of maximum depth penetration.

Re spectrally submitted,

M. i,. M. CONSULTANTS LTD,

Michael ZarowaKi, B. Se. . p. lin gj r i. , ,

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