The sampling targeted ore-bearing zones exposed in the cliff faces of Antimony Canyon, where mineralization occurs as veinlets, lenses, and irregular blebs of stibnite (Sb₂S₃) within fractured sandstone and shale formations. The canyon walls rise up to 240 meters above the creek bed, providing accessible exposures for sampling. The mineralized zones typically range from 5 to 20 feet thick. However, the specific depths from which each sample was taken are not detailed in the available reports. The sampling focused on surface exposures and accessible underground workings, aiming to assess the extent and grade of antimony mineralization in the district.
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