The 3,759 ha Lost Horse property is located in South-Central British Columbia, 99 km north of Kamloops and 27 km west-southwest of Clearwater. The project, owned 100% by Eagle Plains Resources, is comprised of the main Lost Horse claim with 4 non contiguous mineral claims and were acquired through staking and third-party purchase agreements.
The claims are highly prospective for porphyry intrusion and epithermal type precious- and base-metal mineralization. The property is road accessible via a well-maintained network of forest service roads.
Drilling Commences at Eagle Plains’ 100%-Owned Vulcan Critical Metals Project, Southeastern BC
Eagle Plains/NevGold Subsidiary Execute Option Agreement for Multiple British Columbia Critical Metal Projects
Eagle Plains/Amaroq Execute Option Agreement for Findlay Critical Metals Project
Eagle Plains Secures Contractors for Fully Funded Drill Program at the Vulcan Project
The 2084 ha Snowstorm Property, located 45 km east of Nakusp, BC, hosts high-grade Au-Ag-Pb-Zn. Mineralization typically forms as sulphide ore shoots hosted in structurally controlled quartz-carbonate veins that can be up to 2.0 m wide and as disseminations and cleavage infill proximal to mineralized veins.
The 356ha Sphinx Property is located 60 km west of Kimberley, in SE BC. Reacquired by staking in 2023, the claims are highly prospective for intrusion related Molybdenum/Tungsten mineralization and host a historical resource of molybdenum.
The property is road accessible via a network of logging and mineral exploration roads. A hydro-power right of way exists directly to the north while other services are available nearby in Cranbrook, the regional center.
Eagle Plains Stakes Multiple Lithium Prospects in Western Canada
Geology
Geology in the Theory region is primarily comprised of lower Jurassic Hazelton Group volcanics, which unconformably overlie late Triassic Takla Group volcanics. The entire package of rocks is intruded by late Triassic and early Jurassic stocks. The majority of the Theory property encompasses the highly prospective Jurassic-Triassic unconformity (~200 Ma), termed by the BC Geological Survey as the ‘Red-Line,’ which has a high spatial correlation to many of the known deposits throughout the Golden Triangle and Toodoggone.
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