The FRM 73 (99) showing outcrops along the crest of the ridge separating Newton and Badger creeks, 3.5 kilometres south-southeast of the summit of Lodestone Mountain and 22 kilometres west-southwest of Princeton.

Four zones of chalcopyrite are hosted in hornblende clinopyroxenite in the western margin of the Early Jurassic Tulameen Ultramafic Complex, near the contact with Upper Triassic Nicola Group metavolcanics. The zones trend north to northwest over lengths of up to 30 metres. They appear to be confined to fracture zones of similar strike. The three largest zones are 4 to 6 metres wide. Assays of up to 0.5 per cent copper and 0.04 per cent nickel are reported (Assessment Report 2742, page 8). The showing was trenched and sampled by Fort Reliance Minerals Ltd. in 1970.