Resistivity inversion section across the Denio Summit trend in the western part of the Junction property. The large, high contrast and near surface resistivity anomaly located to the east of drill hole DS-18-001 will be the focus of follow-up exploration in 2019 because copper mineralization in drill hole GR-18-001 at Granite Mountain is hosted in highly resistive potassic alteration (Figures 2 and 3). Further, this new and obvious target at Denio Summit is covered and previously unexplored.
Resistivity inversion section across the Denio Summit trend in the western part of the Junction property. The large, high contrast and near surface resistivity anomaly located to the east of drill hole DS-18-001 will be the focus of follow-up exploration in 2019 because copper mineralization in drill hole GR-18-001 at Granite Mountain is hosted in highly resistive potassic alteration (Figures 2 and 3). Further, this new and obvious target at Denio Summit is covered and previously unexplored.