Trans-Hudson
The Trans-Hudson Project comprises 90 claims with a total surface area of 102,708 hectares, located roughly around and in between the communities of Creighton, La Ronge, and Southend in central Saskatchewan. The properties contain 124 mapped and interpreted pegmatites that are between 0.5 and 14.5 kilometers in strike length. Pegmatites were staked based on preferred geologic environments, historical geochemistry and historical mapping. Importantly, they have seen little to no exploration for lithium. The Trans-Hudson orogeny is a series of Paleoproterozoic volcanic and metasedimentary belts that join the Superior, Hearne-Rae and Wyoming cratons of the Archean. This package hosts numerous mafic volcanics, felsic volcanics, granitoids, gneisses, metasediments, quartzites, marbles and pegmatites. Many pegmatites are described as white and containing beryl, tourmaline, garnet and/or muscovite, which indicates they are S-type and have potential to host LCT mineralization.
In the summer of 2023, BRW discovered 2 lepidolite LCT pegmatites in the La Ronge and Reindeer Lake area. The company is current assessing the next steps for this project.
Lake Athabasca
This Project comprises 96 claims with a total surface area of 10,129 hectares, located roughly 75 kilometres west of Uranium city, near the border with Alberta. The property contains 2 mapped pegmatites that are roughly 1,500 metres in strike length. Claims were staked based on preferred geologic environments and historical mapping and have seen no prior lithium exploration. The company will conduct a prospecting campaign in 2024.