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.
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.
The 12,044 ha Vulcan Property is located in the Purcell Mountains, 35 km NW of the historic Sullivan Mine at Kimberley, B.C. The Sullivan contained 160 million tons grading 12% Pb-Zn and 67 g/t Ag, with a mineable lifetime of 92 years, and a contained metal value in present dollars exceeding 35 billion dollars.
The 355 ha Wildhorse Property is located 27 km NE of Cranbrook in the Rocky Mountains of SE B.C. Situated on the east side of the Wildhorse River, where over 1 m oz. of gold was mined from gravels in the late 1800’s, the claims coincide with the furthest reported upstream placer gold occurrences.
Acquired in 2004 for its gold vein occurrences and sediment hosted copper mineralization, The project is 100% owned by Eagle Plains with a 2% NSR held by Eagle Royalties containing a 1% buy-back clause.
The 1,872ha Dianne Lake Property is located in northern Saskatchewan approximately 18 km northwest of Uranium City. The property is accessible year-round from Uranium City via ski- or float-equipped fixed wing aircraft.
The property was staked in 2020 to incorporate 3 significant silver-copper endowed mineral showings and associated east-west and north-east trending structures.
The project is 100% owned by Eagle Plains with a 2% NSR held by Eagle Royalties containing a 1% buy-back clause.
The 6165 ha George Lake Property is host to the historical, sediment-hosted, George Lake Deposit. The mineralized horizon is stratigraphically controlled, sub-vertical, and mineralization is zinc and lead dominant. Step-out drilling by Eagle Plains in 2026 has defined mineralization to a vertical depth of >400m from surface. Mineralization remains open along strike and to depth.
History
In the Pine Channel area, reconnaissance geology in the form of government reviews and mapping programs began in the late 1950’s. Several additional reports on uranium deposits and gold occurrences were carried out being carried out into modern times. In the late 80’s geological mapping at the 250k scale had been completed over the area. Additional government datasets include 3 airborne geophysical surveys and GSC lake sediment geochemistry.
The 898 ha Dragon Lake Property is located 80 km NE of Ross River, YT. It has been explored since the mid 1940’s when Cu and Au mineralization was discovered by the GSC.
Access is by helicopter service from Ross River or Faro, YT. Crews can be mobilized from the North Canol Road located 8 km to the SE. Alternate access is by boat from km 110 on the North Canol Road. An exploration camp has been established on the tenure.
The 209 ha Finex Property is located in the Pelly Mountains of the southern Yukon, 140 km east of Ross River, Yt. It is prospective for Sedimentary Exhalative (“SEDEX”) and Volcanic Massive Sulphide (“VMS”) deposits and is accessible by helicopter from the nearby Robert Campbell Hwy, 18 km south.
The property is owned 100% by Eagle Plains with no underlying royalties or encumbrances.
