Trench sample of 8.5 m 2.1 g/t gold is associated with antimony- bearing structures hosted in Tertiary volcanic rocks. Target is bulk-minable stockworks zone.
Lower plate rocks, including the Roberts Mountains Formation, host gold mineralization with a high arsenic geochemical signature.
Located on the Carlin trend, the claims have potential for deep disseminated and near surface intrusive-related gold mineralization.
Located near the south end of the Carlin trend, the claims are situated along a strong ENE lineament with potential for gold hosts in stratigraphic collapse breccias and cross-cutting Tertiary intrusives.
Located in Crescent Valley, target is Carlin-type mineralization hosted in breccias derived from overlap assemblage rocks
A pediment target, in Big Smoky Valley, where Carlin type mineralization is hosted by Ordovician carbonate rocks.