It may indicate to us that the formation comes from the south and represents a new find. As we close in on the boundary we could hit big money.

DDH 404 is approximately 400 metres south of DDH 421

DDH CF404 tested an IP anomaly located 1,456m south of DDH CF403 and intersected a zone of significant but low-grade copper-silver mineralization hosted in andesite before entering a series of post mineralization mafic dikes.

The upper 82m of DDH CF404 intersected andesite and thereafter was completed to a depth of 255m in a series of late, post mineralization porphyritic, dioritic to gabbroic intrusive dikes.