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Location: 60 km SE from Moab, Utah, United States
P.O. Box 400MoabUtah, United States84532
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Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
Shaft depth, mining scale, backfill type and mill throughput data.Full profiles of select mines and projects.
Equipment type, model, size and quantity.Full profiles of select mines and projects.
Camp size, mine location and contacts.Full profiles of select mines and projects.
Lisbon Valley can be considered a “sandstone-hosted copper deposit”.Mineralization at the three Lisbon Valley deposits consists of low-temperature copper minerals disseminated throughout certain porous and permeable sandstone beds in the Dakota and Burro Canyon formations. Copper minerals are either sulfides (chalcocite, djurleite, covellite, bornite, chalcopyrite), carbonates (malachite, azurite), or oxides (tenorite, cuprite, neotocite/copper wad). The vast majority of contained copper is in malachite, chalcocite, azurite, and tenorite, in that order. Sulfides occur at depth, while the oxides and carbonates predominate within 150 feet or so of the surface.
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