The property oonoisto of three claims of approxi mately 40 acres each, situated in lot 7, Concession H,

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1 PROSPECTING GEOPHYSICS LTD. 42A12SE JAMIESON 010 REPOR GEOPHYSICAL SURVEYS ON propkhty OF NORTHERN KXPLORATIQN LTD. MS KELIY...DESMOND MINING CORPQftATION INTRODUCTION O Geophysical surveys consistinc of electromagnetic and ma photometer surveys were carried out on a three claim property held jointly by Northern Exploration Ltd. and Kelly Desmond Mining Corporation In Jamieson township, Ont. The following report and accompanying naps des cribe the resulta obtained in these surveys and give an interpretation of these resultst PROPERTY AND LOCATION The property oonoisto of three claims of approxi mately 40 acres each, situated in lot 7, Concession H, O of Jamieson township, Porcupine Mining DiviRion, Province

2 - 2 - of Ontario, They oro recorded with the Department of Mlnon an claitas P62&J9 to P inclusive and are shown on tho aooomjttnyinf; map* area generally io covered with a mantle of overburden but on the property covered in this report thoro aro two fairly large areas of outcrop, ae shown on tho accompanying raap* The underlying rooks in those are a o aro rhyolite with the exception of a diabase dyke that outcrops near tho west boundary of tho property* Map No* 23C which accompanies a report by L. O. lg Borryon, Goology of tho Robb- Jamieson Area, published by tho Ontario Daj^artcxmt of Mines shows a largo outcrop of rhyolite to tho wost of tho property which just extends Bli&htly over tho west boundary* Another outcrop of rhyolite has boon mapped in tho southeast corner which conform?- to tho area of outcrop shown on the accompanying rnopo. further to the south there io another large area of rhyolite outcrop which is cut by several quarts diabase dykoa striking slightly west of north* *Vol. Llll, Part 32, 19A4, Ontario Department of Mines*

3 - 3- Of economic interest is a band of andesite extending southeast from tho Kam-Kotia Kino toward* the Northern-Kelly property* Tho contact between tho andesite and rhyolite provides a favorable environment for oulphide mineralization* The schistosity in tho area appears to be about N65W with very atec/p dips. HI-.S1ILT.H OK THK GEOPHYSICAL SimVEYS AND and frlootromagnfttio ourvoyc wore carried out over the entire property along lino o cut at 200 foot intervals, ao ehown on the accompanying naps* A Sharpe /.-2 reagnotoroetor waa used in the ma^ietio survey and tho 01octroraa0rv.tic survey waa carried out uaing A Eonka Mark IV horizontal loop electromagnetic unit* Soil sampleo wcro uleo taken over the conductive son* and field tests made for heavy rnotale, Tho olootroroa^otic survey wan carried out * initially uoirig a 200 foot coil interval and a conductor was picked up atrongly on one line but only showed weakly on ot^er linos (ttoe Map Ho* 1)* As a result) a check uurvoy was carried out over the conductor using a 300 foot

4 coil interval for floater penetration. Thia survey was also curriod out on othor linea which had been extended from tho adjacont property and thib tfnve fairly detailed coverage of the conductor (Soo Map No* 2)* Tho results are plotted on three eeparate napa on a ocalo of 100 foot to the inch aa follows: Map No* l - Electromagnetic Survoy (200 f coil separation) Map No* 2 ~ Electromagnetic Survey (300* coil separation) Map No* 3 ~ Muftnotoraotor Survey and Geochemical results. An examination of Map Ho* 2 shows a strong conduc tive zone with a conoral north trend but at the south end it cwings to the southeast and conforms nora to the regional fichiotoaity. It has a length of 700 to SOO feet and i* atill open at the south end but it waa not possible to toko readings here because of flooded conditions* The average width of the zone is approximately 50 feet* The oonductivity is quite good with ratios up to * 3 to l* It weakens at tho north end but at tho south end nc&r the Bcnver Pond it appears to bo fairly strong* The dip appears to be nearly vertical. From the readings

5 - 5 - on lino 203 with the 200 Toot and 300 foot ooil separation, tho dopth of the conductor lo calculated to be approxi mately 35 foot* On tho othor linea it is obviously doopor. Tho raa&natio map dooo not ohow any anomaly asoociated vdth the conductive cone and this is the same condition that occurs at tho Texas Gulf deposit. A definite north trending mcnnetic anomaly was outlined to the wost of the conductor and this obviously represents a diabase dyke* Another v/ookor magnetic anomaly occurs on the northeast oido of the conductor and it is possible that this renreboht* o narrow band of andesite* Tho neochemicttl rooulto are shown on the ttofpetio map and the readings all show a sliest concentration of hohvy metals over the conductive sone* Tho best con* contrition is found on line 203 and this is to be expected as we know tho overburden is tho loast at this point* Based on the geological environment, the conductive response end the geochemical resultsi it seoma very likely that tho conductor is owuped by sulphides and one would expoct a fair concentration* Tho shape and site of the r-*-

6 - 6 - conductor suggests a replacement type body along a folded structure. Since tho geological environment is somewhat tho same aa that at Texas Gulf Sulphur, thor o would appear to be a fair chance that there may be economic mineralization present. Tho geophysical surveys were carried out along a network of linos out in a northeast direction and spaced At 20D foot interval*, The e Itctromagnotio survey was carried out using the Konjca ;4ark 22 horizontal loop equipment with 200 and 330 foot coil intervals. In tho horizontal loop type of survey, both the in-phase and out-of-phaoo components of the Dooondary field are measured, whose special character* letics make poneible a fairly accurate evaluation of tho conductivity. A conductor caused by sulphide mineralisa tion will produce a curve going fron positive readings througfr ssoro to negative and back again to positive* Both tho in-phflpo and out**of -phase readings show the same general curve. The ratio between the in-phooe and out-ofphase readings over a conductor is an indication of the

7 - 7 - conductivity of the body* A good conductor would cause a creator deviation of tha in-phane com;)onont that the out* of-phaae component* The opposite i* true of a poor conductor. Thu magnetic readings were token with a Sharpe A-2 MMtfnetofnetor moaourinc the vftri&tion* of* the vortical component of thw oarth'ft ro&nnetic field* Readings wore plotted AS fconk-nao and contoured on the aooomi**nyine maps After correction for diurmtl variation* Soil samples were taken at 25 foot intervals over * the conductive stone and tested for heavy metals uoing the dithisone method and a portable field kit* The heavy rectal content WAD oatimatod from the field tests and plotted on Map No* 3* No control analyses wore mods but copper wao detected in the field teat* CONCLUSIONS AMD K The gcophyaiciil uurvcyu outlined a gpod conductive for a length of approximately 700 feet and an Average width of 50 feet on the property* The conductor is well located on the three claim property in respect to the boundaries* T

8 Tho eoolofficnl environment is favorablo and tho r o mil t c ouf^jont that the conductor ropronents oulphidoe* On tho banlo of tho ronultn of tho nurveys nnd tho economic ninoralir-otion found on tho Toxaa Gulf property! a pronrfuri of dianvjnd drilling io moommondod to tho aone.!io0pcctfully nubnltted, CEOPIIYniCS LTD. Montreal, Cue.,. Oct. 13, UJ*

9 P4-6289I P P.I-7730! P.I P R3-6289I P CON C. 11 LOT CLAIM GROUP l"s 1/2 Mi. P l P R P LEGEND MEASUREMENT STATIONS ALONG PICKET LINES ELECTROMAGNETIC READINGS-In Phase Component (*Xo) ELECTROMAGNETIC READINGS-Out of Phase Component PROFILE-In Phase Component (Scale l"- PROFILE-Out of Phase Component (Scale r-20%) ELECTRICAL CONDUCTOR 2O0 1 COIL SEPARATION ELECTROMAGNETIC SURVEY on the property of NORTHERN EXPLORATION LTD. -and- KELLY-DESMOND MINING CORP. LTD. \/ JAMIESON TOWNSHIP. ONTARIO by PROSPECTING GEOPHYSICS LTD. OCTOBER 1964 * SCALE- l"s 100' 42Al2SE89a JAMIESON S00

10 P4-6289I P P.I P-l-77302oo P2-7730I P3-6289I P / CLAIM GROUP l" s 1/2 Mi. PI PZ (I P P LEGEND MEASUREMENT STATIONS ALONG PICKET LINES "-3 ELECTROMAGNETIC READINGS- In Phase Component (*/* -S*- ELECTROMAGNETIC READINGS-Out of Phase Component \~. PROFILE- In Phase Component (Scale!" *x f *~' Pf?OFILE-Out of Pha** Component (Scale l"-4o*/*: ELECTRICAL CONDUCTOR COIL SEPARATION ELECTROMAGNETIC SURVEY NORTHERN EXPLORATION LTD. and- KELLY-DESMOND MINING CORP. LTD. JAMIESON TOWNSHIP. ONTARIO by PROSPECTING GEOPHYSICS [TD. OCTOBER 1964 SCALE- l"* 100' 42A12SE89a JAMIESON eio

11 P4-6289I P P.! b 0 C ON C.I l LOT CLAIM GROUP l"* 1/2 Mi. R l P R LEGEND MEASUREMENT STATIONS A LO NO PICKET LINES +SOO RELATIVE VALUES OF THE VERTICAL COMPONENT t-soo FORCE OF THE EARTH'S MAGNETIC FIELD (In Gamma*) MAGNETIC CONTOURS A MAGNETIC BASE STATION 900 TO I QQ 0 GAMMAS OVER 1200 GAMMAS ELECTRICAL CONDUCTOR CONCENTRATION OF HEAVY METAL p.p.m. est. MAGNETOMETER SURVEY on the property of NORTHERN EXPLORATION LTD. -and KELLY-DESMOND MINING CORP. LTD. JAMIESON TOWNSHIP, ONTARIO A.y ^^ oy PROSPECTING GEOPHYSICS LTD. OCTOBER 1964 SCALE- l"s 100' 4SA12SE JAMIESON 320

Introducti on. Land Survey. Geomagnetic Survey. Geomagnetic Results and Interpretati ons - Conclusions and Recommendations C

Introducti on. Land Survey. Geomagnetic Survey. Geomagnetic Results and Interpretati ons - Conclusions and Recommendations C m M 42A86SW8281 63.42 PRICE 010 C O H T E H l 42A86SW828I 63.42 PRICE 010C Introducti on Land Survey Geomagnetic Survey Geomagnetic Results and Interpretati ons - Conclusions and Recommendations - - -