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The South Arrow discovery is located 400 m south of the Arrow deposit and adjacent to the Patterson Corridor. Significant high-grade mineralization extends 290 m along strike and 185 m vertical depth.
Similar to the high-grade domains of the Arrow Deposit, uranium mineralization occurs as accumulations of semi-massive to massive pitchblende. The best intersections to date include:
290 m along strike and 185 m vertical depth
The South Arrow discovery is located 400 m south of the Arrow deposit and adjacent to the Patterson Corridor. Significant high-grade mineralization extends 290 m along strike and 185 m vertical depth.