The Hom occurrence consists of gold-silver mineralization. Its location is known only very approximately, being approximately 6 kilometres east-northeast of Homathko Peak and 9 kilometres southwest of the southern end of Tatlayoko Lake.

Very little information is available (Minister of Mines Annual Report 1965). Geologically, the occurrence is situated in a Late Triassic to Cretaceous Eastern Waddington thrust belt imbricate zone consisting of structurally interleaved slices of metamorphic rocks unit lKCD, lKO, uTrMo, uTrlm, uTrsv, uTrMM. The imbricate zone is in fault contact with mafic volcanic rocks of the Upper Triassic Mount Moore Formation about 1 kilometre north of the MINFILE plot.

The thrusting has resulted in the interleaving of Upper Triassic volcanic units comprising mainly andesitic pyroclastics and flows and sedimentary units comprising mainly shale, sandstone and conglomerate. The thrusts strike east and dip south; the strata within them apparently strike northeast and dip moderately southeast.

The presence of gold and silver is related to arsenopyrite, pyrite and chalcopyrite mineralization in fissure veins. Field investigations in 2011 identified the presence of arsenopyrite hosted by quartz carbonate in tonalite, but it is unclear whether or not the sampled material is the same referred to in Minfile 092N 023.

In 2010, Transition Metals Corp. staked the property and completed prospecting and mapping in 2010 and 2011.