Annual report . oyoi-. Tlio map on ]inu.v 22 sliows tlio old claimlinos, no actual survey liavinji as yet boon niado of tlio now (dainis. 24 Department of Mines No. 4 The claims on which the Xipissiiig was doing most work were: H.S. 238,U.S. 239, H.S. 240, H.S. 241. During the time that the geological examinationwas being made the Nipissing Mining Company had a gang of eight or ten menat work in trencliing and sampling and doing some blasting. A log cabin andthree tents were on the property and the work was in charge of George Tucker. The veins on which most of the work was being done occur on
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Annual report . oyoi-. Tlio map on ]inu.v 22 sliows tlio old claimlinos, no actual survey liavinji as yet boon niado of tlio now (dainis. 24 Department of Mines No. 4 The claims on which the Xipissiiig was doing most work were: H.S. 238, U.S. 239, H.S. 240, H.S. 241. During the time that the geological examinationwas being made the Nipissing Mining Company had a gang of eight or ten menat work in trencliing and sampling and doing some blasting. A log cabin andthree tents were on the property and the work was in charge of George Tucker. The veins on which most of the work was being done occur on a liill whichrises some 35 feet above a shallow, weedy pond about an eighth of a mile indiamctei. Tlie rocks on tlie southwest face oE this hill are impregnated withankerite, or other iron-bearing carbonate, whicli has caused them to become rusty. Tliere are four main veins on this liili, striking about north 25° west magnetic, and (lipping al)ont vertically. These veins vai-y in width from a few inches to 4 or. Camp 0)1 Tucker claims, Katrine township. 5 feet or more. Ojie of tlieni lias been traced at least 400 feet, and is probablylongei. The veiuuS consist mainly of quartz, and contain also iron pyrites, copper|)yi-ites, S])ccularito, galena, and at times consideiable ankerite or other similarcarbonate. Fiagnicnts of piidv syenitic-looking rock commoidy occur in the vein. The Bureau of Mines party did not sample these veins, but the results of the.-ampling oj)erations by the ISTipissing Mining Company Avere kindly made known, ft was stated that tlie highest values in gold were obtained from a small vein onthe face of the hill, known as No. 1 vein. Some shots had been put in this veinat a certain point, exposing IG inches of vein material. This IG inches consistedof 4 inches of quartz in the centre, the remainder consisting of red, fine-grainedS}-enitic material, impregnating greenish-grey rock matter. The west side of tlievein material shoAvcd stringers of quartz, one-half