The Wollaston Lake South Project is a massive, district-scale land package positioned right within a Tier-1 neighbourhood of major producers and active junior explorers.
Located just outside the current Athabasca Basin margin, the project is a direct geological analog to the famous Eagle Point Mine setting, where high-grade uranium mineralisation extends from surface to nearly one kilometre in depth.
Eastern Basin margin, 36km south of Cameco’s Rabbit Lake Mine
Uranium (U3O8)
District-scale land package covering approximately 336km
Surface to deep basement hosted target corridors
Located just outside the current basin margin within mineralised Wollaston Group basement rocks
Basement-hosted, structurally prepared thrust-fault uranium deposits
High-density surface geochemistry and airborne target resolution
Wollaston Lake VTEM Survey Interpretation – Electromagnetic Imaging
Data from a recently flown Versatile Electromagnetic (VTEM) survey over the Maverick Minerals Limited’s Wollaston Lake claims were reviewed and interpreted to delineate potential uranium prospects based primarily on the presence and structural position of bedrock conductors defined by the VTEM data. Both areas are over 6km in length.
Extensive historic surface programs confirmed strong uranium anomalism at surface, yet no exploration drilling has ever been conducted on the property
Surrounded by the industry’s biggest players, sharing direct borders and regional trends with Denison Mines, Cameco, SkyHarbour, Purepoint, Atha Energy, and Appia
Reprocessed magnetic and gravity datasets have mapped out multiple, repeated structural targets along an immense 65km long operational window
Multiple mapped uranium occurrences indicate a distinct, subparallel mineralised corridor completely separate from the main mining trends to the west
The project is centred on highly deformed Wollaston Group basement rocks showing widespread historic uranium occurrences along strike. The asset features exceptional structural preparation for massive fluid flow, dominated by rotated thrust duplexes and extensive axial-planar fault arrays. Crucially, the property is sliced by the regionally significant, north-trending Tabbernor fault system — a major structural driver directly responsible for some of the eastern Athabasca Basin’s most valuable uranium deposits.
Government and historic regional lake-sediment surveys identified a continuous, northeast-trending uranium-pathfinder anomaly slicing through the entire property
Historic rock-chip and prospecting programs successfully validated high-grade uranium showings at surface within the exposed basement rocks
Reinterpretation of regional datasets has isolated multiple deep-seated structural traps perfect for hosting bulk uranium deposition
Located on the active eastern margin with direct proximity to established, multi-generational mining infrastructure networks
Direct connectivity to all-weather transport corridors and regional supply centres reduces seasonal exploration bottlenecks
Supported by a transparent, proactive provincial government framework committed to Western strategic critical mineral supply chains
Deploy field crews to collect rock chip (multielement, SWIR, petrographic) & biochemical samples (soil or black spruce bark)
Merge incoming high-resolution airborne geophysical data with reprocessed gravity layers
Resolve coherent target zones across the 65km corridor to establish clean, first-pass drill priorities
