The property lies within the Upper Triassic Nicola Group approximately 2.5 kilometres east of the Lower Jurassic Guichon Creek batholith. Bedrock consists mainly of plagioclase-augite intermediate pyroclastic and epiclastic breccia, conglomerate, tuff, sandstone with localized shale, carbonates and augite porphyry.

The showing is exposed in a 2.74 metre adit on the northeast side of the creek at creek level. In the adit there is a 20 centimetre wide fault striking 065 degrees and dipping 45 degrees southeast. A 5 centimetre quartz-carbonate vein striking 040 degrees and dipping 50 degrees to the southeast is exposed in the footwall of the fault. The quartz carries pyrite, galena and sphalerite; the carbonate is weakly pyritic. The wallrock throughout the adit is a grey, fine-grained siliceous tuff.

A grab sample from the vein assayed 0.38 per cent copper, 0.01 per cent molybdenum, 1.0 per cent zinc, 44.56 grams per tonne silver and 1.37 grams per tonne gold (Minister of Mines Annual Report 1967).