So it falls to gathering classes to generate the items. Moving on.Įach 5 levels or so will give you access and information to better gathering points (nodes), while it can seem a bit arduous, it's not so bad if you think of the task objectively. Easy enough to do, but needs a bit more patience. You may want to level blacksmith though, just for making ingots etc, but that's optional. Higher your gathering/perception rating, better it will be. Mining is a good starting point with this.ĭifferent ore's can be gathered as you progress. Go gatherer for the more consistent gil gains. Please review our Terms of Use agreement for this data product.Původně napsal Le Grande Fromage (aka Cheez): We are continuously updating our assessment file / technical report information. Publisher Name: Ontario Division of MinesĪrticle - Geology of the High Lake area, Ewart Township, District of Kenora Mono - Gold deposits of the Kenora-Fort Frances area, districts of Kenora and Rainy River Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder BayĪuthor: Ferguson S.A., Groen H.A., Haynes R. Publisher Name: Ontario Geological Survey Publication Number: OFR5695 Page: 189-190 Mono - The geological setting of gold occurrences in the Lake of the Woods area Thesis - Mineralization of the High Lake Pluton and Adjacent Country Rocks MonoMap - Geology of High Lake-Rush Bay area, District of Kenora

Best intersection from 1958 drilling assayed 1.56 opt Au and 1.2 opt Ag over 2.1 ft., 0.74% Cu over 1.5m was also encountered. Mineralization is reported to be associated with thin quartz veins in felsite and altered quartz porphyry to consist of electrum arsenopyrite, pyrite, pyrrhotite, chalcopyrite, tourmaline and traces of galena and sphalerite and to extend slightly into the enclosing basalts (Davies 1965, p.33). (P Hinz) - Pits or trenches were sunk in basalt cut by quartz porphyry and felsite. Mineralization Mineralization and Alteration Rank The trends of some shearing and of a narrow porphyry dike suggests that a south-southeast striking cross fault may occur near the pits. On the basis of surface exposures it appears that there area several quartz porphyry dikes or lenses separated by basalt, but drilling has indicated that the geology is equally complex in the third dimension. (P Hinz) - In the vicinity of the pits, the basalt-porphyry distribution is complex. The stock has been interpreted to be two intrusivde phases (Davies 1965, Colvine 1979). (P Hinz) - The area is underlain by the High Lake porphyritic granodiorite stock, which intrudes Archean mafic metavolcanic rocks. 1958: 508 m of DD in 11 holes by Francoeur Mines Ltd. 1944: geological survey conducted by Sylvanite Gold Mines Ltd. carried out trenching, 250 tonnes removed from pits and milled for gold. 1939: Kenopo Mining and Milling Company Ltd. Optioned to Oliver-Severn Gold Mines Ltd. Exploration Historyġ936: gold discovered south of Electrum Lake. The prospect is located southeast of the elongated southern bay of Electrum Lake, approximately 500m south fo Electrum Lake. Take the High Lake Road west to the gate. Point Location Description: Pits on claim K8334, north of the High Lake Road and east of the southerly most point of Electrum LkĪccess Description: The occurrence can be accessed by travelling 2.8km south of the junction of the Shoal Lake Road and Highway 17 to the High Lake Road. Secondary Commodities: Copper, Silver Location MDI52E11NE00063 Record: MDI52E11NE00063 General Mineral Record Identification Record Name(s) Ontario Mineral Inventory Record MDI52E11NE00063: Kenopo, Electrum Pits Ontario Mineral Inventory

Electrum ore