The Pablo 24-2 occurrence is located on a ridge, west of Klaskish Basin.

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 and pyrite are disseminated throughout a silicified breccia at the volcanic-intrusive contact. A sample (30504) over 5.0 metres assayed 0.42 per cent copper and 5.6 grams per tonne silver (Assessment Report 4598).

Similar mineralization occurs on the Pablo 24-3 claim located about 300 metres to the southwest. Minor disseminated chalcopyrite and bornite are hosted within a breccia zone along the intrusive contact.

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.