The hole encountered the favourable gabbro at 650m and continued in the same rock to the depth capacity of the drill at 1317m. Within the gabbro a 70 metre section contained numerous fragments, xenoliths and rafts of mafic volcanics, cherty sulphide rich exhalite and sulphide facies iron formation. The gabbro within this interval is variably mineralized with disseminated pyrrhotite and chalcopyrite (<1% - 15%, visually estimated). This indicates that the magma had access to a sulphur source, a condition that is considered important for the formation of accumulations of massive Cu-Ni-PGE sulphide mineralization within the magma chamber. The mineralized core has been sampled and sent for assay at AGAT labs in Sudbury, Ontario.