The DXG occurrence is located between Hoodoo Creek and Confederation Glacier, about 3 kilometres north of Knight Inlet. Mineralization at DXG is characterized by silver, gold, lead, zinc and/or copper mineralization associated with a variety of felsic to intermediate intrusions of the Jurassic to Tertiary Coast Plutonic Complex.

A brown weathering, 5-centimetre-wide quartz-carbonate vein contains minor sphalerite disseminated along a quartz core. Foliated quartz diorite is altered for about 5 to 10 centimetres on either side and traceable for about 10 meters. A sample (DXG-82) taken of the vein graded 40 grams per tonne silver, 25 parts per billion gold, 0.54 per cent lead and greater than 1 per cent zinc, (Assessment Report 9710). Sample DXG-88, located about 120 metres west of sample DXG-82, was taken from a 15-centimetre-wide siliceous zone with minor chalcopyrite and chlorite on the contact of an andesite dike (presumably in foliated quartz diorite). Up to 1 per cent chalcopyrite occurs locally along quartz banding; and open spaces (from 5 to 10 per cent) occurred in the quartz. Earthy dark brown material (iron oxide?) was common in the vein. The sample graded greater than 1 per cent copper, 40 grams per tonne silver and 0.25 gram per tonne gold (Assessment Report 9710).

See Lancers Ridge (092N 076) and East 1 (092N 051) for a common work history of this area conducted mainly in 1980, 1981, 1988, 2009, and 2021.