The Orbi showing is located on the east side of the Bulkley River, 22 kilometres southeast of Hazelton.

The property is underlain by altered Upper Cretaceous Brian Boru Formation (Kasalka Group) felsic volcanic rocks intruded by granodiorite of the Late Cretaceous Bulkley Intrusions. Argillically and siliceously altered rhyolite is cut by zones of breccia.

Drilling by Utah Mining and Construction tested an induced polarization anomaly caused by pyrite in altered rhyolite. The best intersection was 1.5 metres grading 0.78 percent zinc and 0.12 percent lead, with insignificant silver, gold and copper (Assessment Report 14525). Soil geochemical surveys by Colossal Energy Corporation obtained zinc values up to 1676 parts per million (Assessment Report 14525).