The Congress (Paul) occurrence is on the north side of Gun Creek, two kilometres northwest of its mouth.

The Paul zone consists of a number of west trending quartz veins following shears in greenstones of the Mississippian to Jurassic Bridge River Complex (Group). Tertiary feldspar porphyry dykes trend north across the sheared strata. Potassium/argon analysis of the dykes suggests an age date of 67.1 Ma +/- 2.2 Ma (Fieldwork 1985).

The Slide zone, just northwest of the Paul zone, follows a sheared contact between basalt and argillite of the Bridge River Complex west of a porphyry dyke. The shear is believed to splay out as it enters the incompetent sediments to the north.

The quartz veins contain disseminated to banded pyrite, arsenopyrite, tetrahedrite and stibnite, surrounded by quartz- ankerite alteration.

The Paul zone contains inferred reserves (possible underground reserves) of 83,444 tonnes grading 9.6 grams per tonne gold (George Cross News Letter #26, 1986). Drill hole intersections from the Slide zone grade up to 11.3 grams per tonne gold across 2 metres (Mineral Exploration Group Meeting (Vancouver) - B.J. Cooke, 1986).