The Mo showings are located 8 kilometres northwest of Hazelton on the west slope of Hazelton Mountain. The area is underlain by a small intrusive granodiorite body, of the Late Cretaceous Bulkley Intrusions, which cuts sandstone, siltstone and shale of the Lower Cretaceous Kitsuns Creek Formation (Skeena Group).

Several small quartz veins carrying disseminated chalcopyrite, sphalerite and arsenopyrite have been found on the Mo claim. The mineralized veins occur at the sheared contact zone of the granodiorite with sedimentary rocks. The host rocks also carry disseminated mineralization.

A sample from a 2.5 centimetre wide quartz vein carrying arsenopyrite and sphalerite assayed 9.9 grams per tonne gold, 126.7 grams per tonne silver, 1.4 per cent zinc, 1.2 per cent lead and 2.4 per cent arsenic (Assessment Report 13184).