A regional-scale Carlin-type gold system 38 km southwest of Dobbin, with shallow historic mineralization and underexplored carbonates at depth.
120 km SW of Eureka, NV
11 in 425 m × 250 m
< 46 m depth
Paleozoic carbonates
Carlin-replacement-style mineralization within Paleozoic carbonate host rocks — the Denay, Rabbit Hill, Roberts Mountain and Pogonip limestone formations — with a combined thickness exceeding 1,000 ft.
Previous explorers drilled shallow holes (90–122 m) focused on Tertiary volcanics. The deeper Paleozoic carbonates remain underexplored, and the property displays high levels of arsenic, antimony, mercury and locally gold.
