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| The Gap Zone is located between the Southwest Zone and Windjammer South along the iron formation. Mineralization is the similar to that of adjacent Windjammer South and is currently confirmed over 450 metres of strike along the (south) iron formation contact in the hanging wall sediments. Additional mineralization with an associated vein system is along a north-westerly trending and steep southwesterly dipping cross structure.
Previous highlights included 1.04g/t over 117.1m with 5.15g/t over 14.3m, 1.04g/t over 55.0m with 5.52g/t over 4.0m, and 1.14g/t over 39.0m including 1.98g/t over 6.0m.
The mineralized system is currently known to extend for 450 metres along strike, 150m width and to a depth of 500 metres. Significant untested potential remains at depth between the current Gap Zone mineralization and the Southwest Zone.
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