THE PROPERTY IS UNDERLAIN BY EARLY JURASSIC HAZELTON VOLCANICS, WHICH ARE INTRUDED BY SMALL IRREGULAR BODIES OF SYENO-MONZONITE. QUARTZ AND QUARTZ CARBONATE VEINS, SHOWING NO PREFERRED ORIENTATION, CUT THE VOLCANIC ROCKS AND LOCALLY CONTAIN MINOR AMOUNTS OF CHALCOPYRITE, GALENA AND SPHALERITE. PYRITE IN AMOUNTS UP TO 5% OCCURS AS FINE DISSEMINATIONS WITH GOSSANS. NO SIGNIF- ICANT ZONES OF ALTERATION AND SILICIFICATION HAVE BEEN FOUND TO DATE. PROSPECTING AND GEOCHEMICAL SURVEYS HAVE NOT LOCATED ANY SIGNIFICANT GOLD AND SILVER ZONES. SCATTERED ANOMALOUS LEAD AND ZINC VALUES PROBABLY INDICATE THE PRESENCE OF GALENA/ SPHALERITE IN QUARTZ VEINS.