APR RECEIVE STURDY MINES LIMITED ELECTROMAGNETIC AND MAGNETOM2TRIC SURVEY KISZHKOW RIVER PROPERTY PATRICIA MINING DIVISION

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1 52P**NE94e ACHAPI LAKE 010 a RECEIVE APR PROJECTS r SECTION STURDY MINES LIMITED ELECTROMAGNETIC AND MAGNETOM2TRIC SURVEY KISZHKOW RIVER PROPERTY AREA OF ACHAPI LAKE PATRICIA MINING DIVISION ONTARIO April 21, 1972

2 52P04NE99 Z. 843 ACHAPI LAKE 010C TABLE OF CONTENTS Page No. TITLE PAGE TABLE OF CONTENTS CERTIFICATE OF QUALIFICATIONS PROPERTY CLAIMS LIST LOCATION AND ACCESSIBILITY GEOLOGY SUMMARY OF THE ELECTROMAGNETIC SURVEY SUMMARY OF THE MAGNETGMETRIC SURVEY APPENDICES: A. O.D.M. Technical Data Statement E. Electromagnetic Survey Plan: Scale l" = 0 feet. C. Magnetometric Survey Plan: Scale l" s 0 feet. Sfifctii,

3 CERTIFICATE OF QUALIFICATIONS I, Carmen F. Desson, of the town of Winona, in the County of Wentworth in the Province of Ontario, do hereby certify that: 1. That I air. a Registered Professional Engineer and a member of the Association of Pro fessional Engineers of the Province of Ontario, That I a:., an Honours Graduate of the Provin cial Institute of Mining, Haileybury, Ontario and have been practising my profession in ^lining for over years. That I have a good knowledge of the area covered by this report having prospected the claims arid personally supervised isost of the work declared herein. Dated at Toronto, Ontario this 21st day of April, 1972 Carmen F. Desson, P.Eng.

4 PROPERTY CLAIMS LIST The property consists of 45 contiguous Crown Land ndning claims al.01 the Ach/ml T-aVg Ar^. f Patricia. Mining Divison of Ontario, and are numbered as follows: PA38579 to PA38596 (inc.) j PA4414S to PA44153 (inc.). PA43469 to PA43489 (inc.) J The Electromagnetic Survey was carried out over all of the above claims except for claims PA38J)85; PA ; PA43469 and PA43A86. The Maaaetometr.xc Survey was carried out over all of the claim group except for claims PA44153; PA43469 and PA LOCATION AND ACCESSIBILITY The property straddles the i-iisehkow River and is loc ated ir. the Area of Achapi Lake, Patricia Mining Division of Ontario. The geographical centre of the claiir. group lies 3; miles SE of the village of Pickle Crow and 63 miles NW of ^he village of Armstrong which is on the transcontinental line of the C.K. R. Best means of access is by charter bush aircraft from Pickle Lake airbase near Pickle Crow, operated presently by Hooker Air Services. Pickle Crew is reached via gravel road 170 miles north east of the village of Ignace, Ontario which is on the C.N."P. G50LOGY The area is underlain by typical Archtvji Age sediments, volcanics, and intrusives of the Precambrian Era. Prospecting and drilling shows these rocks more specifically to be andesite, tuff, graphitic tuff, banded iron formation, greywacke, quartzite and possibly rhyolite as well as granitic porphyry, gabbro and diorite. The main geological feature is the main band of iron formation which crosses the middle of the claim group striking N 650 E and dipping steeply north and south.

5 - 3 - SUMMARY OF THE ELECTROMAGNETIC SURVEY The property was gridded with cut, chained and nick- T striking N 53O E up the middle of the Misehkow River. The survey was conducted with the. Crone J. E. M. 460/ 1800 c. p. s. E. M. Unit, using the "shoot-back" method. Rea ve're taken at 100 foot station intervals and at 50 foot er vals over conductive areas. SfiYprL nnrr! '"^'t"^ Yfi zones were detected and are described as follows: Conductive Zone l A sit3.ll one-line conductor which plots over a magnetic iigh and is probably caused by minor pyrite and pyrrhotite in jabbro or diorite. Conductive Zone 2 This is a long, strong conductor caused by the main band of magnetite heavy iron formation, which includes tuff and graphitic schist. Conductive Zone 3 This is a weak discontinuous conductor probably attrib uted to surficial features. Conductive Zone 4 This is a medium to strong conductor with coincident magnetics and is probably caused by magnetic iron formation with some pyrite and pyrrhotite. Conductive Zone 5 This is a weak to medium strength conductor. One drill hole which sectioned the conductor with a small coincident magnetic high showed the cause to be banded tuff with minor magnetite plus disseminated pyrite and pyrrhotite plus a narrow massive inter section of the latter sulphides. Conductive Zone 6 This is a weak conductor lying just south of and parallel to Zone 5 and is probably caused by sheared or bedded tuff with minor pyrite.

6 - 4 - Conductive Zone 7 This is a weak short conductor possibly caused by sheared tuff projected from Conductive Zone 5. mcsietometsic SURVEY The survey was conducted over the same line grid as the Electromagnetic Survey using the XcPhar Fluxgate Magnetometer. Model No. M70G.. Readins we ra t at. ion foot with 50 foot readings take.i in some anomalous areas. Eight magnetically high anomalies were detected, designated A to K and are described as follows: Magnetic Zone "A" A weak xo moderately high anomaly lying in an area of kr.pvrr; gabbro outcrops. Cause of the anomaly is a sill-like gabbro mass. Magnetic Zone "S" Similiar and parallel to Zone "A" and probably caused by a sill-like mass of gabbro or diorite. Magnetic Zone "C" Weakly magnetic anomaly parallel to above. Reason unknown but could be gabbro or diorite under deep overburden. Xa^netic Zone "D" Caused by a thick bed of banded magnetite in tuff. (Iron formation). Magnetic Zone "E" A moderately high anomaly probably caused by minor magnetite and pyrrhotite in tuff. Magnetic Zone "F" A discontinuous zone with probable folding. probably tuff with minor magnetite and pyrrhotite. Cause is

7 Magnetic Zone "G" A local magnetic high which was tested by one drill hole which intersected tuff with minor magnetite and dissemin ated pyrrhotite plus a narrow zone of massive pyrrhotite and pyrite. Magnetic Zone "H" A conformable weak magnetic high attributed to tuff with niinor magnetite and disseminated pyrrhotite. Respectfully submitted, C.F. DESSON, P.Eng,

8 APPENDIX "A" File. GICAL - GEOCHEMICAL TA STATEMENT ACHAP, LAKE 900 m* ne.n.c.nz.r.u NOT BE REPEATED IN REPORT TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC. Type of Survey Township or Area. Claim holder(s) GEOPHYSICAL ACHAPI LAKE STURDY MINES LIMITED MINING CLAIMS TRAVERSED Liit numerically Author oi Report C.F. DESSON.-ss 1A Hwy if 8, Winona, Ontario Covering Dales of K..rv.T Mar. 1-31, 1968; June 3-Ji (linccuttinx to office) Total Miles of Line cut A1.2 (prefix) (number) SPKri A I. PROVISIONS CRKDITS RKQL'LSTKl) Geophysical DAYS KMT.R days (includes line cut tint;) tor lirst survey. - Radiometric SEE KM: K 'JO days for each aildilmii.tl survey iimiii; same i;rid. Other.-. tieocheinical. A l R IK) R.\ K (JRKD1IS (Special provision i.rrd''i du not apply lo airborne jiirvryt) Magnetometer..Klectromaiinctic.. Radiometric (t:nt**r clays prr tlui SIGNATURE. Author of Report J PROJKCI'SSKCTION Res. Geol..... Previous Surveys ^±. Qualificalions Ltkkl- Checked hv..date. GKOIXKilCAl. BRANCH. Approved by..date. GEOLOGICAL BRANCH. Approved by..date. TOTAL ri.a IMS 42

9 GEOPHYSICAL TECHNICAL DATA GROUND SURVEYS Mag Number of Si Mt...n. Mag ; E.M Number of Reading* E.M Station mt-,v,i Mag * and 50'; E.M * ^ Line spacing 0* with a few at Qt Profile scale or Contour intervals Mag gammas up to 10,000 and 30,000 gammas thereafter (specify for each type of survey) MAGNETIC Instrument McPhar M700 Fluxgate.^^ Accuracy - Scale mnu:mi - 5 gammas on most sensitive scale Diurnal correction mt-thoti AH readings levelled to maan base control st.a-r.-i nn - 'l Base station location Base Control Station L 52 W - 700* south ^ ELECTROMAGNETIC Instrument Crone J.E.M. - - Coil configuration in-line ^ Coil separation 0* Accuracy - 1 degree of dip angle Method: O Fixed transmitter LjJ Shoot back O In line D Parallel line Frequency 480/1800 c.p.s.- -.^ ^. ^ ^ (ipccify V.L.K. station) Parameters measured Dip angle in degrees of induced secondary field,, ^ GRAVITY Instrument. Scale constant. Corrections made. Base station value and location. Elevation accuracy- - ^ --. INDUCED POLARIZATION - RESISTIVITY Instrument Time domain Frequency domain. Frequency Range Power ^ -.^ Electrode array Electrode spacing. Type of electrode.

10 STURDY MINES LIMITED :HAPI LAKE AREA, ONTARIO ELECTROMAGNETIC SURVEY CLAIM NO DAYS CLAIM NO DAYS PA3S579 PA365SO PA38581 PA3S3S2 PA3S583 PA385b^. PA3S5S6 PA3S3S7 PA3655S PA333^9 j-\ ^ t o f*1 r\ Pn.oto90 V A PA33392 PA3S593 PA33594 PA36395 PA38596 PA43^70 PA43471 PA43472 PA43473 PA43474 PA43475 PA43476 PA43477 PA43478 PA43479 PA434&0 PA43481 PA43482 PA43483 PA43484 PA43485 PA43487 PA434SS PA434S9 PA4414S PA44U9 PA44150

11 STURDY MINES LIMITED CHAPI LAKE AREA, ONTARIO MAGNETOMl TER SURVEY CLAIM XO. DAYS CLAIM NO, DAYS PA3S579 PA3S5SO P A PA PA3S583 P A P A P A P A P A P A P A P A P A PA PA 3359^ PA P A P A PA43471 P A PA PA PA P A P A P A P A P A PA43431 P A P A P A P A P A P A P A P A P A P A PA44151 P A Ci *" ""0 ^v HIM srjj, w

12 ga TAR1C Room W 1617 Parliament Buildings Queen's Park, Toronto 182 iinistry "rtural rees 416: June 16, 1972 Mr. W. A. Buchan Mining Recorder Court Houpe Sioux Lookout, Ontario Dear Sir: Re: Mining Claims Pa et al, Achapi Lake File The Geophysical (Electromagnetic and Magnetometer) assessment work credits as listed with my Notice of Intent dated May 26, 1972 have been approved as of the date above. Please inform the recorded holder and so indicate on your records. Yours very truly, OJ/mw Fred W. Matthews Supervisor Projects Section cc: cc: Sturdy Mines Limited Attn; Mr. W.B. Murphy Resident Geologist j**- Kenora, Ontario

13 ^~ ; f-'''- ' ' ' '^/ ;^'A^H^?^t-":?'fi^\ : ' -i :" v-\ j \ AREA OF ACHAPI LAKE DISTRICT OF KENORA-THUNDER BAY (PATRICIA PORTION) PATRICIA MINING DIVISION SCALE: 1-INCH 4O CHAINS LEGEND PATENTED LAND *OWN LAND SALE "S c.s. (D

14 73 g H o r 2.P 04- m H s 0 f0 o l ^

15 k 'rf

16 44/ / -i-4-y 5 2. a 5' P^ \, f-3 4 r/ \. rv ^73 K M/A/ES A&EA or AC H 'A AT/A//A/G D/I//S/OA/ SCALE:-//// = 2.00^-7: SURVEY 3S 58 S 3&S79 38S3& 3QS83 3 S S3 O :\-N.^ 52PB4NE ACHAPI LAKE

17

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