Ownership: 100% owned and staked by Element One Hydrogen and Critical Minerals.
Location
The HY Project consists of 9 contiguous mineral claims covering 2,757.59 ha located in the Omineca Mining Division of northwest British Columbia.
The project is located within 15-20 km of Fort St. James in north-central British Columbia as well as near the communities of Prince George, Burns Lake, Houston and Smithers
The property lies within the traditional territories of the Nak’azdli Whut’en and Binche Whut’en First Nations
Geology
Ultramafic–Mafic Core: The property is anchored by large, fault-bounded Trembleur ultramafic intrusions forming major ridges and hosting pyroxenite, dunite, gabbro, and serpentinized rocks – key units often linked to nickel-copper mineralization.
Linked Igneous & Structural Features: The Ruby Igneous Complex and localized blueschist zones occur along major structural contacts, highlighting a dynamic, subduction-related geological setting with potential magmatic connections.
Prospective Surrounding Sequences: Adjacent Takla volcanic rocks and Tezzeron basin sediments (argillite, greywacke, limestone) wrap the intrusion in fault-controlled basins, adding multiple prospective stratigraphic and structural targets.
