View northwest at drill hole GR-18-001 at Granite Mountain in the eastern part of the Junction property, showing the concentration of granite dykes within a broad zone of potassic alteration, where copper occurs in both the dykes and intervening host rock. The broad arrow on surface are the vectors for further exploration, based on the correlation of copper mineralization to the highly resistive potassic alteration (also shown in drill hole graphic log in Figure 3).
View northwest at drill hole GR-18-001 at Granite Mountain in the eastern part of the Junction property, showing the concentration of granite dykes within a broad zone of potassic alteration, where copper occurs in both the dykes and intervening host rock. The broad arrow on surface are the vectors for further exploration, based on the correlation of copper mineralization to the highly resistive potassic alteration (also shown in drill hole graphic log in Figure 3).