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The Kulyk Lake property covers approximately 96 square km and was staked to cover known historical uranium mineral occurrences and uranium lake sediment anomalies within prospective folded and faulted basement lithologies of the Wollaston group. Much of the known uranium mineralization occurs along Wollaston group contacts and fault intersections, particularly in the presence of pegmatite. Historical trenching at one such occurrence revealed 0.369 per cent U3O8 over 3.4 meters (SMDI 0993). Grab sampling from another occurrence returned up to 1.68 per cent U3O8 (SMDI 0978). Please visit the company website for a property map.
The 50 square km Jenny Lake area also covers prospective basement lithologies of the Wollaston domain at its eastern limit along a major tectonic boundary. Known uranium mineral occurrences are associated with several large-scale structures that suggest excellent regional prospecting potential. Historical grab samples of yellow-stained fractures in gneiss and pegmatite returned values up to 0.47 per cent U3O8 (SMDI 0981). To the east, a single historical drill hole near the Needle Falls shear zone intersected a sulphide and graphite-bearing zone in pelitic host rock.
Maps
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