The El Diamante Project spans 240,000 hectares in southern Mendoza, Argentina. It represents one of the largest untested hydrogeological systems in South America, with significant potential for large-scale lithium and potassium production. The region boasts exceptional infrastructure, distinguishing it from other lithium-rich districts.
The salar system within the El Diamante basin is considered typical of a mature continental brine deposit. These systems often feature a large halite core and are characterized by brine as the primary aquifer fluid.
El Diamante has been exploited for over 100 years for the production of salt (NaCl), serving domestic consumption in Mendoza and neighboring provinces. Until 2024, exploration was minimal, offering a rare opportunity. The region exhibits an ideal geological signature, with very promising early-stage exploration results.
The salar system within the El Diamante basin is considered typical of a mature continental brine deposit. These systems often feature a large halite core and are characterized by brine as the primary aquifer fluid.
El Diamante has been exploited for over 100 years for the production of salt (NaCl), serving domestic consumption in Mendoza and neighboring provinces. Until 2024, exploration was minimal, offering a rare opportunity. The region exhibits an ideal geological signature, with very promising early-stage exploration results.
