The MOH 3 (Saul) occurrence is located on a southwest facing ridge, approximately 1.5 kilometres east of Upper Campbell Lake.

The area is underlain by basaltic volcanic rocks consisting of basaltic lava, pillow lava, breccia and tuff of the Upper Triassic Karmutsen Formation. These have been intruded by granodiorite, quartz diorite, granite and quartz monzonite of the Jurassic Island Plutonic Suite to the east.

Locally, a north-south fault zone in Karmutsen volcanics hosts pyrite and chalcopyrite. In 1982, rock sampling yielded values up to 0.25 per cent copper, 2.4 grams per tonne silver and 0.52 gram per tonne gold (Sample 4 Saul; Assessment Report 11105).

In 1982 and 1983, Rich Lode Gold completed programs of prospecting and geochemical sampling on the area after a piece of float quartz vein containing native gold was discovered from the rock fill on the western approach to a bridge crossing between Upper Campbell and Upper Quinsam lakes. The float sample assayed 3301.4 grams per tonne gold (Assessment Report 11105). During 1997 through 2003, MinLand Resources explored the area as part of the Bacon Lake (MINFILE 092F 256) property.