Stone Gold Inc. provides an exploration update regarding its contiguous 21,000-hectare Batchewana Bay District (?BBD?) unpatented claims package situated 80 km. north of Sault Ste Marie Ontario. The Batchewana Bay District claims are located on the eastern edge of the Late Proterozoic (1050-1115 Ma) Midcontinent Rift, most of which trends beneath Lake Superior. Numerous past-producing and present Cu, Ni and precious metal deposits are distributed around Lake Superior adjacent and/or associated with the rift, including the prolific native copper deposits of the Keweenawan Peninsula, Michigan. The district is situated within the Mamainse Point Formation of the Keweenawan Group in the Proterozoic Southern Province, on the eastern edge of the Mid Continental Rift. The western and central part of the claims package straddles the NNW trending unconformity between the Mamainse Point Formation to the west and rocks of the Batchewana Greenstone Belt of the Archean Superior Province to the east. The Keweenawan Group stratigraphy is characterized by shallow westerly dipping sub-aerial flood basalts and intercalated conglomerates intruded by felsic sub-volcanic intrusives and breccias. Significant sections of the district were closed to staking from 1972-2006, accordingly the area has seen only sporadic mineral exploration since the 1970s.