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The Ledge Project, located in the northeast Athabasca Basin, consists of 7 mineral dispositions totalling 38,784ha (38km2). The Athabasca Basin unconformity-contact crosscuts the northern mineral dispositions of the property, and the sandstone extends southwards to a maximum thickness of 200 metres. The basement rocks underlying the Ledge Project consist of mainly Archean felsic gneisses with lesser Archean and Paleoproterozoic supracrustal rocks.


  • Targeting basement-hosted and unconformity-associated Uranium mineralization.
  • Property Structural Fabric: Curvilinear NE-trending belt dominated by dome-and-basin-style interference-folding  typical of the Mudjatik Domain.
  • Major Structures include Tabbernor faults, Mackenzie diabase dykes, and potential extension of the Cable Bay Shear Zone.
  • Numerous drill holes and boulder sampling has been completed on the property with anomalous Uranium and scintillometer values which have been linked to the granitoids.
  • Proximity to Known Mineralization: Moosonees Lake Bedrock Uranium Showing on Property ( Surficial Boulder Sample at 0.19% U3O8).  
  • Recent Work: XciteTM helicopter-borne time-domain electromagnetic (HTDEM) system flown over entire property in 2023, which defined 50 linear-kilometres of conductive lineaments.

Recommended Work

  1. Complete drillhole and surficial geochemistry compilation work initiated by ATHA Energy Corp.
  2. Property-wide airborne gravity survey.
  3. Property-wide geologic mapping, prospecting.
  4. Property-wide ground geochemistry/boulder survey.