Japan Gold's new Togi Project is located on the northern flank of a regional graben, hosted in early Miocene andesite volcanics and under-lain by a northeast trending gravity anomaly. A similarly oriented graben-gravity feature and Miocene host rocks are noted 160 kilometres along strike to the northeast on Sado Island, which hosted Japan's second largest gold mine, the Sado Mine which produced 2.5 million ounces of gold and 74 million ounces of silver² until its closure in 1974. The Company believes the area is underexplored and highly prospective for epithermal vein discoveries, akin to the Sado Mine.