The high temperature geochemical vector molybdenum increasing towards the Kawich target in the covered valley west of the range provides evidence for the center and proximal source area of the overall polymetallic system at Reveille. This magmatic-hydrothermal element, indicative of an intrusive heat source is found in increasing amounts and across broader zones in the target area. View of the 3D model is to the Southeast, with field of view of roughly 1km.
The high temperature geochemical vector molybdenum increasing towards the Kawich target in the covered valley west of the range provides evidence for the center and proximal source area of the overall polymetallic system at Reveille. This magmatic-hydrothermal element, indicative of an intrusive heat source is found in increasing amounts and across broader zones in the target area. View of the 3D model is to the Southeast, with field of view of roughly 1km.