Edith River Project
Several uranium prospects were discovered in 1952 within the Lower Proterozoic Cullen Granite. 9 shallow shafts with cross drives were completed around this time. Sampled grades returned between 0.1% – 0.2% U3O8. The highly anomalous uranium grade is associated with shear/fault zones within the Cullen Granite.
Extensive radiometric anomalies remain untested throughout the area with little historical exploration work follow up. The area is highly prospective for uranium mineralisation including unconformity, sandstone, quartz-pebble conglomerate and vein deposit types.