A lead-zinc showing (#236) is located north of the Babine River, 50 kilometres north of Hazelton (Geological Survey of Canada Open File 2322).
The showing is documented as a vein or fracture-related occurrence hosted in Middle Jurassic to Lower Cretaceous Bowser Lake Group sedimentary rocks. These consist of epiclastic sediments including sandstone, shale, siltstone, argillite, conglomerate and minor coal and carbonaceous units.
No other information is available.