The Fair showing is located on the Fair crown grant (L. 2839) on the Big Missouri pack trail south of the Big Missouri deposit (104B 046). The property was examined by Granduc Mines Ltd. in 1967.

Located in the Intermontane Belt, the area, bounded on the west by the Coast Crystalline Complex and on the east by the Bowser Basin, is part of the volcanic arc assemblage of the Stikinia Terrane.

Mineralization is hosted by the Upper Triassic to Lower Jurassic Hazelton Group, Unuk River Formation metavolcanics. The Hazelton Group is a northwest trending steeply east dipping belt of folded andesitic lapilli tuffs, flows and breccia containing a thick sequence of argillite and siltstone infolded along a synclinal axis. The sequence is intruded by the Early Jurassic Texas Creek plutonic suite of dacitic porphyry dykes.

Host rocks in the area have been silicified, pyritized and sheared. The showing consists of a quartz vein mineralized with minor tetrahedrite. At the south end of the crown grant there is a well mineralized (minerals undefined) porphyry zone about 6.1 metres wide which has not been broken into. No other information is available.

The Fair area is part of the Silver Coin property worked on by Mountain Boy Minerals and Jayden Resource since the early 2000s.

See Silver Butte (104B 150) for related geological details and a common Silver Coin property work history. See also Silver Coin (104B 095).