The Cork Project is located 15km south-west of Cork in southern Ireland.
The Project consists of carboniferous mudstones and limestone, and hosts the Rag Bridge zinc-lead anomaly where previous exploration has returned 1.63m grading 3.79% Zn+Pb from 17m and 1.6m grading 3.84% Zn+Pb from 120.75m.
Mineralisation at the Cork Project is associated with faults, with one target area to the east shown to coincide with interpreted fault zones. A second key target area exists to the west of the Rag Bridge anomaly in relatively under-explored terrain.
These anomalies along with several small zones of untested geochemical anomalies provide immediate re-sampling targets.