This 500 meter long mineralization zone is interpreted to be the surface expression of the EM-1 geophysical anomaly detected during the 2011 winter survey (see press release 19/05/2011). The EM-1 geophysical anomaly was the most conductive feature detected during the survey, and shows a long trend extending on more than 1.2 km and open-ended to the west. The estimated "depth-to-top" of the conductor or the strongest electromagnetic signal is interpreted to be between 150 and 250 meters deep. No hole has tested this mineralization zone at depth
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The 2011 drilling program also defined the position of the Rocky Brook-Millstream Fault. This fault has been followed by drilling, over a distance of 5.5 km and contains gold mineralization over the entire length. Holes FH11-02, FH11-03 and F11-04 confirmed the gold enrichment of the fault with respectively 4.84 g/t over 0.25m, 1.51 g/t Au over 0.25m and 1.72 g/t Au over 1.4m. The Rocky Brook-Millstream Fault played a major role in the precious metals enrichment of the sulphide lenses discovered at Nicholas-Denys so far and it is usually located within 75 meters of the main sulphide lenses. The InfiniTEM® 2010 ground survey and the compilation of previous and actual works has also confirmed the presence of two structures parallels to the Rocky-Brook-Millstream Fault that will be explored in the current program.

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