An unnamed silver-lead-zinc occurrence (#233) is located on the northwest side of Blunt Mountain, 24 kilometres east of Hazelton (Geological Survey of Canada Open File 2322). The showing is documented as a silver-lead-zinc vein or fracture-controlled occurrence hosted in Middle Jurassic to Lower Cretaceous Bowser Lake Group rocks. These consist of epiclastic sediments including sandstone, siltstone, shale, argillite, conglomerate and minor coal and carbonaceous units.
No other information is available.