An unnamed silver-lead-zinc occurrence (#244) is shown on Geological Survey of Canada Open File 2322 as being located four kilometres southwest of New Hazelton near Chicago Creek.

The showing is documented as being a vein or fracture-related occurrence hosted in a small stock of the Late Cretaceous Bulkley Intrusions and in Upper Jurassic to Lower Cretaceous Bowser Lake Group sedimentary rocks. The Bulkley Intrusions are mainly granodiorite in composition, and the Bowser Lake Group sedimentary rocks are mainly sandstone, siltstone, shale, conglomerate and argillite and minor coal and carbonaceous units.

No other information is available on the occurrence.