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NZ
Fee Minerals |
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Prepared by:
J.D. Sphar, former NZ geologist |
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NZ's
fee minerals are considered valuable because of their:
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1.
Mineral resources: especially, uranium |
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2.
Intrinsic worth: |
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As real property:
a titled right, an estate |
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Speculative element: mineral rights
could possibly represent substantial future wealth
of currently indeterminate character; the unknown
aspect creates a speculative value in and to the
mineral right. Such speculative values are amenable
to geologic comment, but seldom to ultimate economic
resolution. To the contrary, creative geologic investigative
often creates prospective mineral targets and potentials,
thus, actually increases speculative value. |
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Certain
deposits of natural resources
have been delineated over the years on NZ's mineral rights
including in order of their discovery: petrified wood,
coal, potash, industrial clay, uranium, travertine, and
oil. Beyond the possible future values from exploitation
of these discovered resources, the mineral rights per
sec also remain intrinsically valuable because of their
potential for future mineral discovery. Given the amount
of research and exploration to date, the potential for
new discovery is more constrained than wide open. Geologic
data is relatively sparse and, hence, the potentials for
discovery less constrained on the blocks of Indian Reservation
minerals. Economically, the more important issue is likely
to remain the exploitation of the known resources on NZ's
mineral rights. |
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Uranium has the potential
to be the most economically important natural resource
on NZ's fee mineral lands. In the Crownpoint-Hosta Butte
vicinity of New Mexico, uranium reserves are now calculated
at 38 million pounds. This uranium occurs in two well
defined deposits amendable to in-situ leach mining methods
at costs in the $20+ per pound range. Historically, this
uranium deposit has yielded NZ one million dollars in
leasehold payments. |
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Travertine limestone
having a calcium carbonate content of over 95% crops out
astride NZ's checkerboard fee lands on Mesa del Oro, which
is located some 40 miles west of Albuquerque. The overall
deposit, including that on intervening BLM lands, contains
over 1 billion tons and is well defined by drilling. The
potential uses include: flue gas scrubbant, the manufacture
of cement or lime, use as dimension stone, as ballast
or rip-rap, or as aggregate either for concrete or road
metal. NZ retains six sections in fee (surface and minerals)
in support of this highly tangible deposit. There is little
doubt that it will be developed for one or more of the
above uses in the future. |
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Petrified wood resources
remain only on the Milky Ranch. The Frisco Railroad, NZ's
parent company, lost most of its petrified wood when the
Petrified Forest National Park was established in 1906.
Petrified wood is a semi-precious gemstone widely used
in lapidary products. NZ's fee lands bordering the PFNP
once contained world's largest commercial supply of this
lapidary product. Petrified wood has been widely stolen
from NZ's lands and other wise marketed by NZ's lessees
since the 1930s. Something more than $300,000 was generated
from royalties paid to NZ prior to 1998. More recently,
the bulk of NZ's petrified wood resources were sold for
$500,000. The value of the remaining resource on the Milky
Ranch is put at $350,000. |
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Oil on NZ's lands was
widely rumored as early as 1912, but was not produced
until 1986, and then as a follow up to a random oil show
found in a uranium research core hole drilled for the
Department of Energy back in 1982. The resulting "Nose
Rock oil Pool" produced about 60,000 barrels of light,
sweet crude before its depletion. Geologically similar
small oil pools are possible in the same general vicinity
but exploration costs are difficult to justify for such
small oil pools. Elsewhere, all of NZ's other potential
petroleum prospects must be classified as rank new basin
wildcat. In Cibola County, New Mexico previous wildcat
wells contained prolific porosity or permeability. The
best follow-up to these trace finds would be to drill
on the Acoma Reservation where NZ has mineral rights,
but that has never been politically acceptable to the
Acomas. NZ's large mineral holdings in Northeastern Arizona
have shown little petroleum promise to date, albeit, based
upon rather sparse drilling and that done without the
benefit of even two dimensional seismic. Overall, the
prospects for new petroleum discovery on NZ's lands is
considered difficult at best. |
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Coal resources were
readily identified in the first reconnaissance geological
surveys of NZ's mineral rights in McKinley County, New
Mexico. Estimated reserves were maximally estimated in
1962 from outcrop studies at 160 million tons. The coal
occurrences were better defined by drilling in the frantic
exploration days of Jimmy Carter's "Energy Crisis".
One isolated coal deposit of only 2 million tons of strippable
coal was actually permitted but never mined. The remaining
coal is not likely to become economic under any predictable
future economic conditions. |
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Potash was the first
mineral to be discovered on NZ's mineral rights by drilling;
however, the discovery came at about the time the rich
and logistically favored Saskatchewan deposits were being
developed. No value is placed on NZ's remaining potash
resources. |
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Klannerite is the trade
name for a deposit of highly altered bedrock ("clay")
on 80 acres of NZ's mineral estate in Mohave County. It
may have some industrial value, but given the small size
of undemonstrated continuity of the material, development
is highly dubious. |
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