Interpretive cross section of holes 21OMI-001 and 21OMI-002. Two levels/episodes of mineralization are evident. The lower system was buried by volcaniclastic material which was, in turn. buried by a rhyolite lava flow. The hydrotherm system re-established itself following these events. Irving believes the lower mineralized system is fertile for discovery and that areas around the Honpi structure could host important precious metal veins.