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OWNER OR OPERATORIPROPRI~TAIREOU EXPLOITANT the Munro Nos

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OWNER OR OPERATORIPROPRI~TAIREOU EXPLOITANT the Munro Nos PRODUCT SILVER PROVINCE OR PROVINCE OU British Columbia N.T.S. AREA 104 B/1 REF. AG 1 PRODUIT TERRITORY TERRITOIRE R~GIONDU S. N. R. C. -- NAME OF PROPERTY MUNRO HISTORY OF EXPLORATION AND DEVELOPMENT ' NOM DE LA PROPRI~T~ 1 HISTORIOUE DE L'EXPLORATION ETDE LA MISE EN VALEUR OBJECT LOCATE,D The Munroe group is located at the 2,350 foot elevation on OBJET LOCALISE the east side of Mount Bayard, about 12 miles northwest of UNCERTAINTY Lat. 56'07 1301\ong. 130~04'3011 Stewart. FACTEUR D'INCERTITUDE La t, Long. The showings were discovered and staked by Messrs* Munro, Mining Division Skeena District Cassiar McDonald, and McBride in 1921. Development work at the main Division rn iniere District County Township or Parish showing, located on the west side of and about 100 feet above Comt6 Canton ou paroisse the Salmon Glacier, consisted of open cutting and two short Lot Concession or Range adits. The Munro Mining Company, Limited optioned the Munro Lot Concession ou rang and Boundary groups from Munro and McDonald in 1928. No Sec TP. R. Sect. Ct. R. development work was reported by the company; the option was dropped. OWNER OR OPERATORIPROPRI~TAIREOU EXPLOITANT The Munro Nos. 1-5 claims and the Big Chief Nos. 1-3 claims (Lots 5413-5415) were Crown-granted to Munro and McDonald of Hyder, Alaska in 1929. The owners continued to prospect the showings. In 1934 their property consisted of 11 surveyed and Crown-granted claims and fractions, and 9 claims and fractions, possibly the Boundary group, held by location. DESCRIPTION OF DEPOSITIDESCRIPTION DUGISEMENT The formation consists chiefly of folded, silicified argillite, with possibly some intercalated tuff beds, striking northwesterly and dipping northeasterly at varying low angles. These rocks are intruded by bosses, spurs, and dykes of granitic rocks related to the adjacent Coast Range batholith. The mineral deposit consists of a quartz vein striking north- westerly, dipping about: 15'E with the mountain slope and conformable with the formation. The vein has been traced 230 feet northwesterly from the main exposure. About 1,000 feet to the southeast a 24 inch wide quartz vein outcrops in a creek. The main exposure shows a width of from 1 inch to about 4 feet, mineralized with patches and streaks of galena, sphalerite, tetrahedrite, and chalcopyrite. In an open cut a width of from 3 to 4 feet of quartz is exposed, with irregular mineralization but carrying a streak of possibly high-grade mineralization 2 to 3 inches wide on both the hanging and the foot-wall sides of the vein. Assoc~atedminerals or products - Leadt zinc, copper, Mineral Policy Sector, Department of Energy, Mines and Resources, Ottawa Mineraux ou produits associ6s . Secteur de la politique minkrale, ministere de I'Energie, des Mines et des Ressources, Ottawa 5lns21. -- - -- . H ISTO RY OF PRODUCTIONIHISTORIQUE DE LA PRODUCTION Annual Reports, Department of Mines, British Columbia: 1922, p. 87; 1925, p. 106; 1926, p. 100; 1928, p. 118; 1934, p. B 26. Hanson, George; Portland Canal Area, British Columbia; Memoir 175, p. 160, Geol. Surv. of Canada, 1935. -- - - MAP REFE RENCES~R~F~RENCESCARTOGRAPHIQUES Map 1829, Salmon River Area, B.C., (Geol.), Sc. 11':4,000 feet - accomp. Memoir 132. Map 307 A, Portland Canal Area, B.C., (Geol.) , Sc. 1":4 miles - accomp. Memoir 175. Map 104 B, Iskut River, B.C., (Topo.), Sc. 1:250,000. REMA R KSIREMA ROUES - Cornp./Rev. By Comp. /r&. par Date . Date 108-67 BCI 104 B - 47 1 . .
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