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." The TSX Venture Exchange has not reviewed and does not
accept responsibility for the adequacy or accuracy of this release.
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