The margin of a Miocene caldera is located just to the east of altered outcrops and constitutes a highly prospective feeder structure that is untested by drilling. The caldera is associated with slab window magmatism, a tectonic driver linked to recent Walker Lane discoveries including Silicon and Allegiant Gold’s Eastside Project (1.4 Moz gold resource). Cuprite has been historically regarded as a gold-poor system because it displays barren alteration at the surface–an assumption that was proven untrue at Silicon. The property is virtually untested, has exceptional blue sky potential, and represents a rare opportunity in a mature, politically stable jurisdiction like Nevada.