REPORT FOR BFAUOOROH TSLLOWCTIPg MIWB8 LIMITED on th*

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Baldric Thornton
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1 LACKNER 01(2) REPORT FOR BFAUOOROH TSLLOWCTIPg MIWB8 LIMITED on th* of MINERAL CLAIMS to I BOLUS IV B IAOCTHR TOW1CHIP - SUDBURY MCTIEQ DIVI8IOII OlfURIO BIMARD uta CTIOKT inning Coniultnati Toronto, Onbwlo SAULT STE. KAR3E RECEIVED SEP 3 O MINING DSVESSON

2 REPORT FOR BEAUCOEUR TBUXWCTIFK KIHBS LIMITBD on the MKWHTOMfcTKR SURVEY Of MINERAL CLAIMS 0*80014 to 6*80049 IHOLUSIVB UCKHKR "OWBSHIP * SUDBURY MTSIHO DIVI6IOI QfTARIO PaOPBRfY t The property investigated includes a compact group of thirty-fix unsurveyed and uapatented mineral claims numbered 8*80014 to 8*60049 inclusive* These claims fora a compact group, equare in shape and approximately one and one-half Biles to the side. The south boundary of the property adjoins the north boundary of claim group 8*80995 to 6*81001 inclusive and to inclusive also held by this company. OEHBRAL IBFORMATIOI A siailar survey was oonduoted on this latter olaia group ttt Deoejfeer 1954 and January 1956 and the results of this work are fully covered in our report to the oonpany dated January SI, 1956* AOCB88 Aooess to the property is by the sane wjssm as fer the adjaoent claims held by the company, namely, by tractor road fron the property of lailti* Minerals Limited or by aircraft from Chapleau to MoAuley Lakep thenoe by foot trail. Tiie distance fron UoAuley Lake to the west boundary of the elaifts it less than one-half mile. TOPOffliPHT fc Overburden oonditions are extreme throughout the area aad rook exposures are not numerous being confined to the hills* One small lake is present in the northeastern part of the property* A stream flows from this

3 - 8 - lake along the eastern side of the property into Wright Creek to the louth. A second stream flows in a southwesterly direction across the nost northerly olaitts into IfoAuley Lake. The property is heavily wooded with spruoe, cedar, biroh and pine. PPRPOSK OF THB Mineralisation in the area has bean found frequently associated with deposits of disssednated to Massive concentrations of Magnetite* Such loon! areas nay be determined by an increase in Magnetic intensity* In* survey described in this report was oonduoted to determine if disseminations or concentrations of magnetite are present on the property* MSTHOD A base line was out aeross the oentrai part of the property in a north-couth direction. Picket lines, spaoed at intervals of 400 feet were out to the east and west of the base line to the property boundaries* These lines and the property boundaries were ohained and narked piokets were plaoed at intervals of 100 feet. A Sharpe D-l-M type Magnetometer was used to Measure Magnetic intensities on the property. Station readings were Made at 100 foot intervals on all of thft picket lines, i&gnotio values so obtained were corrected for diurnal and daily variation, converted to gaana equivalents and plotted on a plan whose scale it l inch equals 800 feet. This plan ha* been contoured at intervals of 200 gammas for those intensities in exoess of 8000 gamnas, and all areas of an intensity of less than 5000 gantas are shown as Magnetic lows.

4 . s. The geology of the property is presumed to be eivilar to that of adjacent olaitn (groups to the north-west, west and south where detailed geological reoonnaissanoe was wade late in 1064* Fro* the results of these reconnaissances, it is presumed that this property is underlain by Pre-Cambrien paragneiss intruded by dykes and sills of nepheline syenite and the basie types of intrusive rooks* RS3UITS OF THE MAOKKTIO BUHVSY No large anomalies of high Magnetic intensity were found present on the property. Seven areas deliaited in site to less than 600 feet in diameter, ooour whore increases in tcagnotio intensity of plus 800 gatsmm above the nonsal are present* These are numbered l to 7 inclusive, on the aooobpanying plan of the property. A few other areas are shown where only one high reading was obtained. cosclusioas tt Tho anonalous areas are presumed to be oaused by the presence of in a disseminated form. These areas deserve further investigation. The determination of their origin and their relationship, if any, to ooluabiusi mineralisation would be determined best by a program of geological napping* This oould be accomplished in conjunction with a siailar program on the ooapany's acreage adjoining to the south. Plans for additional expenditures such at diamond drilling should await the results of this surface program. Respectfully subsdtted, SI! Toronto, Ontario September 18, 1966.

5 S-8O043 S-80O2? s-booir S-8O028 S-SOO27 S-8OO29 S- 8003O S S-SO03T 5 i :^ " * ^ \ ? L&GE-NO Pl us 42OO 40OO-420O ow anomclu G A ME Y ~^L M t -s, \^ BORDEN CROCKET CMAUgHT \_ACKNE HA LCROW LACKNER. LAKE S-&OO19 s-sooie M OUNT8ATTEN HALSEY KEY MAP TOOM S S-8OOZI SYMBOLS Picket Lines Contour Lines ^ S-8OQ42 Lines Lake Contour

6 S-S0027 S-8OOZ9 S-8003O S-8O032 S SO 03 S-8O03T S-S O03 LE-GE-NO Plus 42OO M UcSt7^tl'c aooma SAULT STE. KA RECESVE SEP 3 O 1955 MINING DIVISION BEAUCOEUR YELLOWKNIFE MINES LIMITED LACKNER TOWNSHIP - ONTARIO SUDBURY MINING DIVISION MAGNETOMETER SURVEY SCALE 1 INCH * 3OO FEET BORDEN CROCKET fv/1 CNAUCHT LACKNER HA LC ROW BEAUCOEUR. YtLlQWKMtfE LTO. LACKNER LAKE S-8O019 5-sooie S-8OOI7 S-8O028 M OUNTBATTEN HALSEY KEY MAP TOOM S S-80^0 S-SOOEl SYMBOLS Picket Lines Contour Lines 5-8O04-I S Claim Lake Contour 004/e S S S-8O046 S-SO038 LACKNER

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 - - -