The Babine showing is located 42 kilometres east-northeast of Hazelton, on the south side of Thoen Mountain.
The showing consists of a small vein, 15 to 20 centimetres wide, carrying arsenopyrite and quartz (Minister of Mines Annual Report 1920). The vein strikes 065 degrees, dipping 65 degrees northwest. The host rocks are Middle Jurassic to Lower Cretaceous Bowser Lake Group quartzites.
Average samples reportedly contained from 8.36 to 20.05 grams per tonne gold ($5 to $12 per ton) and 34.28 to 102.84 grams per tonne silver (Minister of Mines Annual Report 1921, page 100).
Work History
The Babine vein was first described in 1921.
In 2008, co-owner of the Hot property John Ostler (2009) observed from a high-level helicopter flight that the area reported to host the Babine vein was south of the Main Hot gossan and within the confines of the Hot property mineral tenures (Assessment Report 30829).
In 2014, Xander Resources Inc. completed an airborne magnetic and radiometric survey over the Hot property totalling 937 line-kilometres.