The Pinchi Fault occurrence, as referred to in the National Mineral Inventory listings, is situated just north of the Lustdust occurrence (093N 009), approximately 37 kilometres east-northeast of Takla Landing. It is shown as a lead-silver occurrence on Geological Survey of Canada Map 907A, but descriptions of this mineralization have yet to be located.

The area is underlain by a north-northwest striking, steeply west-dipping sequence of interbedded sediments assigned to the Carboniferous to Jurassic Cache Creek Complex. Immediately south of the occurrence, mottled grey, massive, crystalline limestone predominates and is the most probable host to the lead-silver mineralization. These rocks have been disrupted along the Pinchi fault zone, a major regional structure that strikes northwesterly through the Omineca district and, in this area, parallels Silver Creek.

No recent information concerning this occurrence is available.