Extensive chalcedonic gossanous stock work and feeder veins form the higher grade portions of this estimated 300 foot thick siliceous envelope. High pathfinder element values occur in eruption debris at the top of each fumarole. Silica flooded auriferous flow brecciated volcanics are integrated within this complex hot spring system and can be traced into an extensive pediment. A total of 127 third party rock chip samples for the claims average 1.04 ppm Au. Measuring the area within the 1.0 ppm gold contour developed over the unconformity produces an area of 394 acres resulting in a POTENTIAL GEOLOGIC RESOURCE OF 10.1 MILLION ounces!
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