This showing is located 100 metres southwest of the peak of Mount Britton, 900 metres northwest of the Tulameen River and 12.5 kilometres west-southwest of the town of Tulameen.

The Blue Gold occurrence is hosted in a northwest trending band of metavolcanics and metasediments of the Upper Triassic Nicola Group situated between the Early Jurassic Tulameen Ultramafic Complex to the east and the Late Jurassic to Early Cretaceous Eagle Plutonic Complex to the west.

Rubble from an old pit is mineralized with coarse-grained pyrite and galena. A grab sample analysed 0.085 gram per tonne gold, 49.1 grams per tonne silver, 2.255 per cent copper, 2.9474 per cent lead, 5.742 per cent zinc and 0.1107 per cent cadmium (Assessment Report 17325, page 6).

In 2016, Rain City Resources Ltd. completed a program of prospecting and rock sampling on then area as the Northern Champion property. A rock sample (463) of quartzite metasediments hosting galena, sphalerite and pyrite assayed 12 grams per tonne silver, 0.452 per cent zinc and greater than 0.500 per cent lead (MacIntyre, D. (2018-09-17): Technical Report - Northern Champion Mineral Property).