Collom is underlain by Payson Ophiolite that includes volcanics, sheeted dike swarms, diorite, gabbro and tonalite. This lies on a basement complex of granitic rocks that include felsic volcanics and volcaniclastic rocks. The district is highly fractured and faulted with fissures with auriferous quartz veins. High grade, free milling gold was initially mined above the water table.
The veins are polymetallic with primarily copper, lead, gold and silver. The Company has completed a geophysical survey as well as several extensive sampling programs on this property. The presence of multiple samples of high-grade silver and copper warrant further follow-up and possibly drilling.