The Bessie B occurrence is located on the north side of Esther Creek, a tributary of the Kennedy River.

Karmutsen Formation volcanics of the Upper Triassic Vancouver Group are intruded by the Early to Middle Jurassic Island Plutonic Suite consisting of granodiorite to quartz diorite. The Karmutsen rocks consist of andesitic to basaltic flows, tuffs and volcaniclastics. West-northwest trending fault/shear zones of Tertiary age cut the rocks.

Steep north west dipping quartz veins, with gold values, occur in a diabase dike hosted in porphyry, with a 70 degree strike.

In 1987, J. Lampman completed a program of silt sampling on the area. One sample showed anomalous gold values from the Esther Creek drainage area. In 2009 and 2010, G4G Resources Limited completed a program of prospecting and remote sensing, consisting of spectral analysis and synthetic aperture radar analyses, on the area as the G4G property.