The Paradise Peak Mine model was previously explored as a caldera with deposits clustered around the margins of the ring faults.  Recent work in the district suggests a more complex system with overlapping alteration and mineralization systems from nearby intrusives such as the Sullivan porphyry. 

The Old Dominion Mine is an epithermal silver-gold mineral system that is situated 23 miles north of Reno, Nevada along the south side of Nevada State Route 445. NexGen Mining currently controls 10 claims (200 acres) covering multiple veins along a structural corridor hosted in Tertiary volcanic rocks.  The Old Dominion Mine model was previously explored as a caldera with deposits clustered around the margins of the ring faults.  Recent work in the district suggests a more complex system with overlapping alteration and mineralization systems from nearby intrusives such as the Sullivan porphyry.

The company’s 100% owned Koegel Hills Property consists of 10 unpatented claims encompassing 200 acres located in Mineral County, Nevada.  The project is an extensive copper-gold bearing porphyry system manifested by intense surface alteration that extends for more than six square miles.

In the early 1990’s, Santa Fe Minerals Company (“Santa Fe”) staked the area and conducted a limited drilling program, which intersected significantly large zones of strongly anomalous copper and gold.  Values greater than 4.0% copper and 0.030 opt gold were reported in several five-foot drill samples.  Santa Fe released the property when the Company was taken over by Newmont Mining Company.

The Four Mile Basin Gold Property has two unpatented claims consisting of 20 acres and is situated in Nye County, Nevada. The claims encompass a substantial hot springs system that is characterized by prevalent surface sinter and feeder veins composed of crustiform banding and quartz replacing calcite textures.

The Gold Star Property is a high-grade precious and base metal deposit located in Mineral County, Nevada. In the project area, two types of mineralization have been encountered, free gold and copper mineralization associated with a skarn system and high-grade silver-lead-zinc mineralization hosted in a major east-west trending fault zone hosted in carbonates.

The Pyramid Mine is a high-grade, silver-gold-lead-zinc vein and stockwork system hosted in altered Tertiary dacite and rhyolite tuffs situated along the northeast bounding portion of the northwest-trending Walker Lane structural zone.  Over 10 million oz. of gold-silver mineralization has been discovered along this narrow, deep-seated, fault zone which host the Pyramid, Olinghouse, Talapoosa, Rawhide, Fairplay-Paradise Peak, San Antone-RyePatch-Midway, Hannapah-Monitor, Ellendale, Golden Arrow, Silverbow and Eden mining districts.  Intermittent small-scale mining operations have occurred in the Pyramid Mine area since 1910, which produced limited quantities of high-grade ore and concentrates.