The Nabob showing is located on the north fork of Glacier Creek, 9 kilometres northeast of Stewart. Several showings were explored in this area between 1910 and 1923.

A 0.3 metre wide quartz breccia vein, striking 010 degrees and dipping 75 degrees west, is hosted in argillite of the Middle Jurassic Salmon River Formation (Hazelton Group). It contains a small amount of pyrite and chalcopyrite. Another vein in the vicinity, also hosted in argillite, is up to 0.15 metre wide and is mineralized with galena and sphalerite.

In 1919, the Nabob group of claims were staked. In 1923, an opencut just above a trail at 823 metres elevation revealed a small brecciated vein. A crosscut tunnel was faced up about 15 metres below this which will have to be driven about 6 metres to intersect the vein. In 2006, Teuton Resources Corp. completed 228.1 line-kilometres of a helicopter-borne AeroTEM II electromagentic and magnetic survey on their Silver Bell property which covers the showing area.