THE PROPERTY IS UNDERLAIN BY A MODERATE TO STEEPLY DIPPING, NORTH-SOUTH STRIKING SEQUENCE OF TRIAS- SIC-JURASSIC AGE NICOLA GROUP VOLCANICS, VOLCANI- CLASTICS, SEDIMENTS AND SYNVOLCANIC DIORITE INTRUSIVES. MINOR MINERALIZATION OF CHALCOPYRITE AND BORNITE IS ASSOCIATED WITH SMALL FRACTURES. ON THE EAST SIDE OF THE CLAIM GROUP, A 2200 METRE LONG BY 100-800 METRE WIDE, HIGHLY ALTERED, BLEACHED, WHITE TO RUST-COLOURED ZONE CONTAINS 1-5% PYRITE. A STOCKWORK OF QUARTZ-SIDERITE- PYRITE-CHALCOPYRITE, GALENA, SPHALERITE AND ARGENTITE (ACANTHITE) VEINS OCCUR ON THE EASTERN EDGE OF THE ALTERATION ZONE IN CONTACT WITH FRESH NICOLA GROUP VOLCANICS.