The Pablo 22 occurrence is located on the northern side of Klaskish Inlet, approximately 300 metres from shore.

The area is underlain by andesite and basalt of the Upper Triassic Vancouver Group, Karmutsen Formation. The volcanics have been intruded by a granodiorite to diorite stock related to the Jurassic Island Plutonic Suite. The volcanics are epidote altered and host disseminated pyrite and pyritic fracture fillings.

Locally, chalcopyrite, pyrrhotite, magnetite and sphalerite mineralization is disseminated within the andesite near the intrusive contact. A sample (30501) taken over 7 metres assayed 0.37 per cent copper, 1.92 per cent zinc and 9.95 grams per tonne silver. Another, nearby, sample (30502) assayed 0.2 per cent copper, 1.79 per cent zinc, 7.2 grams per tonne silver and 13.6 per cent iron over 2.1 metres (Assessment Report 4598, Map 8).

In 1973, Pechiney Development and Dowa Mining completed a program of geological mapping, geochemical sampling, trenching and a ground magnetometer survey on the area as the Pablo claims.