The InfiniTEM® 2010 ground survey, added with the compilation of previous works, has also

confirmed the presence of two additional structures parallel to the Rocky-Brook-Millstream Fault that

will be explored in the current program. The Rocky-Brook-Millstream Fault is the primary control for

the mineralization found in the Haché, Shaft, Henry, PineTree, and Great Northern lenses. All three

structures together host 16 promising silver deposits and showings over a strike length of 10

kilometers, which will be examined in greater detail. The location and the best silver results from

these deposits and showings are showed on the web site at www.explorationpuma.com.

Their sources indicate weak to good conductors steeply dipping and extending in some case for

more than 500 m at depth. The main feature detected in the geophysical survey is the anomaly EM-

05 which corresponds to the Haché and Shaft lenses. This anomaly has been trace for more than 3.1

km to the east, from the known Shaft lens toward the Henry lens. Two deep holes (FH11-01 and

FH11-03) were drilled in the Henry area. These holes were designed to verify this anomaly but also

to conduct a borehole InfiniTEM survey to better locate the source of the anomaly which extends

from the surface to a depth of 500 meters. From the 12 anomalies detected over the entire survey

length of 3.5 km, only five have been verified by the current drilling program and correspond to

sulphide mineralization

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