The Freedom Project encompasses the most lithium-prospective portion of the Copper Mountain Mining District, located in the eastern region of the Owl Creek Mountains (also known as the Bridger Range). The District is a mineral rich region with historic lithium, tantalum, tungsten, beryl, copper, gold, and silver mining occurring between 1906 and 1940².

Lithium-bearing pegmatites have been historically mapped in the area that the project was staked, with these reportedly hosting spodumene, lepidolite or petalite^2,3. The pegmatites are interpreted to be associated with an Archean-aged granitic intrusion hosted in Archean metasedimentary schists, gneisses, and amphibolite. There are two generations of pegmatites: an older set that is concordant to host rock foliation and mineralogically simple, and a younger, discordant, more mineralogically complex set. The pegmatites typically outcrop as long, narrow ridges generally oriented SW to NE. Grain-sizes are typically coarse (1-5 centimetres) and during staking many of these were recorded to host spodumene, lepidolite, hornblende, tourmaline, red garnet, muscovite, perthite and quartz. Historical mapping recorded apparent thicknesses of bodies as much as in excess of 30 metres (“m”), with an average of 6 m.