The Morning Star Copper showing is located near the headwaters of the north fork of Glacier Creek, 9.5 kilometres northeast of Stewart. A vein was periodically investigated in this area for copper between 1919 and 1923.

The showing consists of a 1.8 metre wide quartz-calcite vein, striking 040 degrees and dipping 40 degrees southeast, hosted in argillite (slate) of the Middle Jurassic Salmon River Formation (Hazelton Group). The vein has been traced along surface for approximately 210 metres and a parallel diorite dike forms the hangingwall. The vein contains abundant pyrite and chalcopyrite on the hangingwall side for a width of 0.6 metre and the remaining 1.2 metres on the footwall side is only sparsely pyritized.

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.