Geological setting is a low to intermediate epithermal gold silver and base metal veins hosted primarily in Tertiary age volcanics.
The high sierras and hills are capped by rhyolites and dacite tuffs of the "upper Volcanic Seies"
Main hosts for the veins at Coneto are andesite tuffs and andestic agglomerate of the "lower Volcanic Series" resting on a basement of cretaceous metasedimentary rocks.
Multiple steep gold- silver mineralized structures, with extensive alteration, are exposed.
Buried, unconformity controlled, flatter structures may be present.
Metal zonation shows EXPOSURES ARE THE UPPER LEVELS OF A PRESERVED EPITHERMAL SYSTEM.
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