The Bishop occurrence is located 7.5 kilometres north-northwest of Stewart, west of Skookum Creek on the east facing slope 1 kilometre north of the summit of Mountain View.

The area is underlain by the Early Jurassic Texas Creek Plutonic Suite consisting of granodiorite. At the Bishop showing, a strong quartz vein striking 315 degrees and dipping 50 degrees northeast has been traced for 182 metres by opencuts and surface exposures. It is exposed over a vertical distance of 30 metres. On average, vein widths vary between 38 to 68 centimetres but is 2.1 metres wide on the slope to Skookum Creek. Mineralization is sparse and consists of pyrrhotite and pyrite with minor chalcopyrite.