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Seven holes totaling 485 m were drilled on the U Zone, a massive quartz vein structure hosted in sheared and altered granodiorite in 2008.
Visible gold was encountered in hole EL-08-01 at 18.5 m in the heart of the U zone quartz veining. The zone is described as a strong to intense white, milky, weakly brecciated quartz vein structure with granodiorite xenoliths. It contains trace to 1% fine grained disseminated pyrite and galena and locally up to 3-5% over 10 to 20 cm sections. Moreover, in hole EL-08-04, the U Zone was intersected over a 15 m down hole width.
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