Projects

Focus Properties

Stevens Basic

Rhyolite porphyry with low-sulfidation gold mineralization is hosted by Tertiary volcanic rocks near the margin of Fairview Peak caldera.

Three target zones with potential for bulk-minable gold and silver mineralization occur in Triassic sedimentary rocks. Sheeted veins host silver mineralization at historic workings where dump samples carry up to 35.4 opt silver and 3.18 g/t gold.

Black Point Project

Disseminated gold mineralization is associated with widespread silicification and silver veins that occur in imbricated thrust fault slivers that include the Pilot Shale.

Owyhee

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.

Petes Summit

Lower plate rocks, including the Roberts Mountains Formation, host gold mineralization with a high arsenic geochemical signature.

BLS Claim

Located on the Carlin trend, the claims have potential for deep disseminated and near surface intrusive-related gold mineralization.

NS Claim

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.

Golden Reef

Located in Crescent Valley, target is Carlin-type mineralization hosted in breccias derived from overlap assemblage rocks

Ziggy

A pediment target, in Big Smoky Valley, where Carlin type mineralization is hosted by Ordovician carbonate rocks.

Prince

Historical silver on adjacent claims associated with widespread silicification is interpreted to be surface expression of deeper target for precious metals mineralization hosted in Cambrian siltstones.

Tip Top

Potential for high-grade, precious metals vein mineralization is present along with potential for disseminated gold hosted in Tertiary volcanics with a high-level epithermal geochemical signature.

Mud Springs

Target concept is bulk-minable, volcanic-hosted gold and silver mineralization developed near resurgent domes within Tertiary caldera