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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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