PJX Resources Inc. announced that highly anomalous gold and copper occur in soil material along with zinc, lead, and silver up slope from the discovery of Sullivan deposit style and grade semi-massive to massive sulphide boulders. The new sediment-hosted discovery of Sullivan style zinc-lead-silver mineralization in boulders occurs on the Company's Dewdney Trail Property in the Sullivan Minng District in southeastern British Columbia, Canada. Boulders of Sullivan style and grade mineralization were discovered in an area of about 50 metres (m) by 150 m at the base of a talus slope.

The boulders are strongly magnetic and appear to have not moved far down the slope of the mountain from a possible bedrock source as some are large and angular. Soil samples taken from talus material up-slope from the boulders are highly anomalous in zinc, lead, silver, gold, and copper. The soils coincide with the strong airborne magnetic anomaly immediately up-slope from the boulderers.

The highly anomalous zinc, lead, silver, gold, and copper content in soils are also coincident with a moderately strong magnetic anomaly for about 500 m along strike to the north of the 500 m long strong magnetic anomaly.