The Round Mountain Gold deposit is a very large, epithermal, low-sulfidation, volcanic-hosted, hot-springs type, precious metal deposit, interpreted to be located along the margin of a buried volcanic caldera. The deposit genesis is intimately associated with the Tertiary volcanism and caldera formation. Intracaldera collapse features and sympathetic faulting in the metasedimentary rocks provided the major structural conduits for gold-bearing hydrothermal fluids. In the volcanic units, these ascending fluids deposited gold along a broad westnorthwest trend.

Gold mineralization within the Round Mountain deposit occurs as electrum in association with quartz, adularia, pyrite and iron oxides. Shear zone fractures, veins and disseminations within the more permeable units (typically open pumice sites) host the mineralization. Primary sulfide mineralization consists of electrum associated with or internal to pyrite grains. In oxidized zones, gold occurs as electrum associated with iron oxides, or as disseminations along fractures.

Alteration of the volcanic units within the Round Mountain deposit can be characterized as a continuum from fresh rock progressing through chlorite, clay, sericitic+quartz, adularia+quartz+sericite, and quartz+adularia alteration assemblages. The alteration is zoned outward from potassic at the center to propylitic on the margin. There is a reasonable correlation between increasing gold grades and increasing degrees of alteration. The central ore zone is characterized by pervasive K-feldspar found replacing the rock groundmass, replacing primary sanidine, or as crystal growths in open-space.

Ore zones within the metasediments are more subtle, largely defined by secondary quartz overgrowths, pyrite and adularia associated with narrow northwest-trending structures.

Ore-grade mineralization is also present in the Stebbins Hill unit as silicified breccias with strong argillic alteration.

The Round Mountain deposit includes the Los Gazabo Vein, Keane Vein, Mariposa Vein sheeted zone, Great Western sheeted zone, Black Hawk sheeted zone, 921 Section, 471 Vein, and Fault Fissure vein. The veins were so closely spaced as to form sheeted zones; the dips of veins steepen and change with depth. Gold grade of ore has a positive correlation with the abundance of NW-striking joints. The ore-hosting tuff consists of a 400 to 500 foot thick non-welded base, a densely welded central portion about 800 feet thick, and a less densely welded vapor-phase altered top that is 75-100 feet thick. Where narrow fractures cut the lower, non-welded portion, mineralization occurs as thin quartz veinlets and as disseminations throughout the pumiceous tuff. In the welded portion, mineralization occurs wholly as veins along high angle fractures or along hydrothermally dilated low angle joints. Dip of the ain ore body is 15SW at cap, 85SW at base.

Gold is intergrown with vein quartz associated with limonite and minor manganese oxide in small fissures. Visible gold often occurs on projecting quartz crystals in drusy cavities and is distinctly crystalline, usually in fairly well defined octahedral and more complex forms. Gold on adularia was observed in specimens from the rich veinlets on the top of Round Mountain.

The Round Mountain mine is located approximately 90 kilometres north of Tonopah in Nye County,
Nevada.

The Round Mountain mine currently operates a conventional open pit that is approximately 11,000 feet long in the north-west, south-east direction and 8,800 feet wide. The operation uses conventional openpit mining methods and recovers gold using three independent processing operations.

The Gold Hill mine is a small deposit located near the Round Mountain mine. Gold Hill is approximately 3,000 feet long in the east-west direction and up to 2,600 feet in the north-south direction. The mine is operated as an independent operation also using conventional open-pit mining methods. The ore consists of oxide material that is placed directly on a dedicated heap leach pad. Gold Hill is currently expected to end in 2023.

The mining is conducted on 35-foot to 50-foot benches by electric or hydraulic shovels and supported by the mobile equipment. Mining is conducted on both single and double bench configurations. Bench face angles and bench width vary with rock type and pit orientation. Haul roads are designed for a maximum grade between 10 and 11 percent with widths designed at 90 to 140 feet for two-lane traffic.

All explosives are stored and used in accordance with MSHA and BATF regulations.

Waste material is hauled to existing waste rock dumps, or placed in the proposed optional in-pit waste rock dump. Ore material is either hauled for further processing at the mill or placed on an authorized heap leach pad.

Mine operations are conducted on a seven-days-per-week basis for 365 days per year. Shifts are based upon a 12-hour workday, and include two shifts per day on a rotating schedule.

The operation uses conventional openpit mining methods and recovers gold using three independent processing operations. These include crushed ore heap leaching (reusable or dedicated pad), run-of- mine ore heap leaching (dedicated pad) and a mill equipped with gravity/flotation circuits. Higher grade oxidized ores are either: crushed, placed on the reusable pad, leached for 60 days, and then relocated to the dedicated pad; or, crushed, placed directly on the dedicated pad, and leached for 120 days. Lower grade oxidized ores are placed on a dedicated pad which is typically leached for 120 days. Sulfide ores are processed through the mill.

Mill represents ~15% of production:
• Capacity: 12,000 t/d;
• Primarily used to treat sulfide ore;
• Unconventional mill - only a small portion of mill feed is treated with cyanide;
* Majority of gold (~90%) recovered from carbon-in-pulp circuit
* Remainder of gold recovered with gravity separation (spirals, tables ........