Locations of the nine drill holes completed to-date at Reveille, plotted on a 3D iso-shell image of the large and high amplitude (32 mV/V) DCIP anomaly named Kawich. Grid lines show the overall coverage of the IP survey that was completed in two stages in February and May, respectively. Also shown are the crustal-scale ring fault complexes bounding the Kawich and Goblin Knobs volcanic calderas, respectively, because they are the deeply seated structural framework that accommodates the polymetallic hydrothermal fluid system at Reveille.
Locations of the nine drill holes completed to-date at Reveille, plotted on a 3D iso-shell image of the large and high amplitude (32 mV/V) DCIP anomaly named Kawich. Grid lines show the overall coverage of the IP survey that was completed in two stages in February and May, respectively. Also shown are the crustal-scale ring fault complexes bounding the Kawich and Goblin Knobs volcanic calderas, respectively, because they are the deeply seated structural framework that accommodates the polymetallic hydrothermal fluid system at Reveille.