Junior
The program entails several deep holes to follow up mineralization intersected in late 2000. The highest-grading intersection averaged 10.63 oz. per ton over 6 ft., starting at 145 ft. down-hole.
Mineralization is hosted by epithermal quartz-breccia veins and fault breccias that were mined in the 1930s. The structures dip steeply and vary from a few to more than 10 ft. in width.
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