Annual report . Ideal Sections, A-G-B, C-D and E-F, showing relationship of the diabase sill to the older scale same as plan; vertical distances not to scale, hence only general relalioiiship is indicated. LEGEND ? Ev] E n m Kee-watm Granite Conglomerate Diabase Diabase dike Shaft Road Geolo^cal Boimdaries (aefinsdr (assumea) Scale: 3000 Feet to I Inch 0 3000 6000 9000 Geological plan of part of the Gowganda Silver Area, scale 3,000 feet to the inch, showing Sections in the vicinity of Miller Lake. 1920 Qowgranda Silver Area 79 The Huroniau rocks iinclerlying the particular si
Annual report . Ideal Sections, A-G-B, C-D and E-F, showing relationship of the diabase sill to the older scale same as plan; vertical distances not to scale, hence only general relalioiiship is indicated. LEGEND ? Ev] E n m Kee-watm Granite Conglomerate Diabase Diabase dike Shaft Road Geolo^cal Boimdaries (aefinsdr (assumea) Scale: 3000 Feet to I Inch 0 3000 6000 9000 Geological plan of part of the Gowganda Silver Area, scale 3,000 feet to the inch, showing Sections in the vicinity of Miller Lake. 1920 Qowgranda Silver Area 79 The Huroniau rocks iinclerlying the particular sill on which the OBrien and Millerettare located are very clearly exposed less than a mile west of these properties, and prospectinj;there has so far had no good results. It would seem, nevertheless, that the claims thuslocated would merit particularly thorough development if Professor Millers theory asdeduced at Cobalt is in any measure applicable to the Gowganda district. Professor Millerstates that at Cobalt
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectminesandmineralresou
