
Claim Geology
The northeast portion of Boundary County is dominated by the presence of Belt Series of sediments, specifically the Aldridge-Prichard formation, which is the oldest formation of the Belt Series. The formation is made up of dominantly quartzites and argillites. A series of mafic sills and moyie sills intrude the sediments, usually along contacts of quartzite and argillites. The sills do not cut across bedding planes. The sills are gabbroic in nature, with variations to basalt and diorite. The sills are also of Precambrian Age. The main mineralized potential in the area is the mineralization in the diorite sills. Magnetite, pyrrhotite, and chalcopyrite have been introduced, possibility at the same time as the quartz veins. The mineralization also includes minerals of nickel, silver, gold and possibly platinum.