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Geology
The Company's main targets of interest at Reese River are veins and shear zones that are formed at or near the contact between intrusive rocks and overlying sediments. Many of these shears have shallow to moderate dips and appear to follow bedding planes in the sediments and form "stacked" tabular zones of mineralization. Other veins and shears on the property cross cut bedding with generally steeper dips and can be projected into the underlying intrusive rocks. These are the likely feeder structures to the mineral system. This contact area is a structurally disrupted zone that facilitated the introduction and dispursment of mineralizing solutions and this favourable environment has seen very limited exploration in modern times.
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