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Gold Mining Claim Acquisition Program
Investor Invitation


You are invited to join our team of experienced professional geologists in acquiring Federal and State mining claims for gold exploration in one of the best known gold mining districts in the world.

Our team of geologists has over 90 years of combined natural resource exploration experience in the Rocky Mountain region covering Colorado, New Mexico, Wyoming, Montana, Utah, and Nevada (Biographies).

Mr. Murer has also pioneered the geologic theory that is the basis for what we believe could be one of the BIGGEST GOLD DEPOSITS IN THE WORLD near Goldfield, Nevada.

The underlying geology of the Goldfield / Tonopah mineral zones arises from the volcanic eruptions that took place during the Miocene period (20-23 million years ago) along a ridge of mountains that contain huge mineral deposits that have been mined for many years in the region from zones of volcanic vents. (Geologic Cross Section).

To date, the Goldfield/ Tonopah area has produced approximately 5.9 million ounces of gold, 175 million ounces of silver and 7.7 million ounces of copper. (Geologic Report)

The tremendous volumes of ascending fluids that created the bonanza of gold, silver and lithium deposits of the Goldfield and Tonopah districts would have descended down the flanks of the existing strato-volcanoes to accumulate and evaporate in the adjacent “reserve pit” formed by the Cambrian rock dam know today as the Paymaster Ridge. These fluids erupted for over one million years (USGS Bulletin Number 1646).

Geologic evidence suggests this natural basin existed at the time of the epithermal mineralization and it is not difficult to imagine the massive paleo-evaporate tabular ore concentration that may now underlie the placer accumulation. (Geologic Cross Section)

During the initial violent stages of the eruption, the potential of molten metals to be ejected from the volcanic vents would have also been likely. To date no drilling has been done to test the bottom of the ‘reserve pit’ for accumulation of metals that could contain a world class gold deposit. (See Geologic Cross Section Map).

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