The Kipper showing was located on the east slopes of Mt. Seaton, just east of the Brooks Peninsula. Access is by helicopter or float plane to several beach locations. The mountainsides are thickly covered by coastal rain forest. The property was staked to investigate regional geochemical metals anomalies.

The region is underlain by a complex, fault-bounded package dominated by the Jurassic Vancouver Group and the Triassic Bonanza Group. These groups trend north westerly and are strongly deformed. Intruded into the package are stocks and plutons of the Island Intrusive Suite.

Locally, thin to medium bedded black shaly limestone of the Parsons Bay Formation and massive to thinly bedded dacite and rhyodacite of the Bonanza Group are present. The Bonanza volcanics are intruded by the Jurassic Mount Seaton pluton and associated quartz-feldspar porphyry dikes. The dikes appear spatially related to several quartz veins. Both trend northerly and mineralization in the veins comprises pyrite, chalcopyrite and malachite. Analyses of the veins yielded a best value of 725 parts per billion gold (Assessment Report 20253).

In 1990, Teck Explorations completed a program of geological mapping and geochemical sampling on the area.