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Annual report . nerals: albite, talc, sericite, calcite, pyrite and gold, the pyritebeing more abundant in the rusty schist than in the quartz. A 50-foot verticalshaft has been sunk on the deposit. Many samples with visible gold can be foundon the dump. It is reported that there is a rich ore shoot here which is 75 feet 1920 West Shiningtree Qold Area 41 long and two feet wide on the surface. The rocks are largely altered green basicvolcanics, with which is associated a narrow slaty band. These rocks and the veinhave been intruded by a narrow diabase dike. Since leaving the area it is reported
Annual report . nerals: albite, talc, sericite, calcite, pyrite and gold, the pyritebeing more abundant in the rusty schist than in the quartz. A 50-foot verticalshaft has been sunk on the deposit. Many samples with visible gold can be foundon the dump. It is reported that there is a rich ore shoot here which is 75 feet 1920 West Shiningtree Qold Area 41 long and two feet wide on the surface. The rocks are largely altered green basicvolcanics, with which is associated a narrow slaty band. These rocks and the veinhave been intruded by a narrow diabase dike. Since leaving the area it is reported that gold has been found on tlie Kingstonclaim, Xo. 3715, which lie? immediately south of the Bennett. Churchill (3773, 3774, 3741, 4044).—The Churchill Mining Company ownsfour claims to the southwest of Michiwakcnda lake, Churchill township. The prin-cipal showings, which were discovered by J. A. Knox, are on claim 3774. Twoveins from two to three feet wide occur in t]io rusty pillow lava* schist. They
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectminesandmineralresou