Base Metals

Clinton: The Clinton property, located in the Northern Appalachian, some 20 kilometers southwest of the town of Mégantic, may represent a structural window within the Clinton River Anticlinorium of Ordovician Age. This window is situated between two major structures of the Northern Appalachian : The Gaspé-Connecticut Valley Synclinorium to the NorthWest and the Boudary Mountains Anticlinorium to the SouthEast. The project is underlain by volcanic rocks of the Chesham Melange, and sedimentary rocks of the Clinton Formation, and host numerous precious metal bearing VMS occurrences and small past producers, along a NE trend across the property...
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Harvey Hill: The Harvey Hill project is underlain by argillic sedimentary rocks, intermediate to mafic volcanic rocks, and talc schist of the Humber zone in the Quebec Appalachians. Three zones of Cu+Ag mineralization occur within strongly carbonate+sericitic altered argillic schists, with quartz veins and veinlets. Chalcocite, chalcopyrite, and boronite are noted in mineralized intervals...
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