May 1 , 2003
The anomaly is generally overlain by visible oxide copper development with residual chalcopyrite (primary copper sulphide) occurring occasionally as coarse clots. A central portion of the anomaly measuring about 800 by 300 meters was previously drilled (1963-64) and reported a weighted average of 1.03% leachable copper in 48 holes mineralized from surface to about 30 metres . One hole, only, was drilled to 75 meters and also reported 1.03% leachable copper with grades up to two percent near bottom where associated with chalcocite (secondary copper sulphide). No holes were drilled deep enough to test the induced polarization anomaly.
A structural feature cutting through the drilled area
was formerly high graded for gold and silver and there is evidence of
elevated gold distributed in the oxide
"Gary Medford, PhD., P.Geo."
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