THn AUERTcAN M rxERALocrsr
marcasite in close association. It is noteworthl,' that the oniy' other iron sulfide observed in the drill cores was a small amount of pyrite occurring as disseminated crystals in the interval 843 874 feet from hole 3. Greigite was not directly associated with the pvrite, and was not observed in hole 3 above 1622 feet.