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Travertine |
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A large world-class
quality travertine deposit is located in Mesa del Oro,
New Mexico (over 1.2 Billion Tons!) This may be the largest
of its kind in the country. |
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NZ
now has Federal claims which complement its fee lands
containing the travertine limestone. Assessment for claim
year September 1991 to September 1992 consisted of drilling
and blasting out a sample bench. There are confirming
drill holes on every major section of claimed ground. |
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Chemical analyses
have been run from cores, cutting and hand samples by
many different investigators. There is a striking uniformity
to all these analyses, and all indicate high calcium,
or chemical grade, limestone. |
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Common variety
limestones occur either in the subsurface or at the surface
on all of NZ's checkerboard tracts. Economically important
occurrences are limited to New Mexico - particularly Cibola
County. |
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The Madera
(Pennsylvanian Age) and San Andres (Permian Age) marine
limestones crop out across NZ's checkerboard minerals
in Valencia County, New Mexico. They are a target for
oil exploration but not limestone production. A massive
travertine limestone (Cenozoic Age) is found at Mesa del
Oro in Cibola County, New Mexico. This limestone was reprecipitated
from the older limestones, and it is of high chemical
purity. Analyses consistently show over 95% CaCO3 content,
with relatively low magnesium and other impurities. |
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Limestone
is the basic constituent of cement and lime. It is also
useful to acid neutralization, paper processing, and more
recently, flue gas desulphurization. In addition to such
chemical uses, limestone may be utilized as road metal.
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In general,
commercial limestone production is highly sensitive to
available transportation facilities and proximity to consumption.
The Cibola County travertine is the most likely economic
deposit from NZ's checkerboard mineral estate. |
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In the fall
of 1981, NZ granted Sunbelt, a wholly owned subsidiary
of Public Service Company of New Mexico, a one year option
to lease the entire deposit. With the claims, this came
to some 8,800 acres. Sunbelt's interest was twofold: 1)
the planned Four Corners Station, later called Dineh Power
Plant, was to use limestone scrubbing; 2) the utility
was diversifying into real estate, mining, venture capital,
and other business area. |
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The following
text is an excerpt from the Sunbelt Mining Company, Inc.
Mesa del Oro Limestone Project, Reserve Determination
report. |
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"The
Mesa del Oro limestone deposit was laid down over a Chinle
erosional peneplain of red shale and siltstone. During
deposition, localized erosional and weathering cycles
created diverse uncorrelatable depositional sequences
which are apparent in the limestone stratigraphic drill
hole sections. Subsequently dissolving by circulating
ground water has formed cavities, which is an indication
that limestone has been completely dissolved or recrystallized
locally. Also, large limestone landslide blocks have slumped
down along the mesa slopes, due to the unstable, easily
erodible nature of underlying calcium clay zones. |
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Several complicating
factors became apparent in trying to arrive at a limestone
reserve determination. The major difficulty can be attributed
to the varied and irregular configuration of the base
of the limestone deposit. The limited number of Sunbelt
drill holes and their wide spacing did not allow a valid
assessment of reserves based solely on the newly collected
data. Therefore, it was decided that computation of reserves
would utilize data previously compiled by Intrasearch
Corporation of Denver, Colorado. This data included a
structure contour map of the base of the limestone deposit,
which was then confirmed by Sunbelt's drill hole data.
The information was transferred onto Sunbelt's and modified
to include 10 foot contour intervals interpolated between
the original 40 foot contour spacings. This structure
map formed the base from which the limestone isopach map
was developed. On the isopach map, every 20 foot contour
interval for each section (tract block) was then planimetered
to obtain the number of acres of limestone within each
contour interval. Using the interval thickness and an
assumed value of 150 lbs/cu.ft. (per Fuller Company) as
an average weight for travertine, the gross tonnage was
computed for each track block. |
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It should
be noted that a limestone isopach map was not constructed
for the Northern tract. Because of limited amount of data
(one drill hole), the small area extent of the property,
and the less complicated nature of the surface geology
of the travertine deposit in this area, construction of
an isopach map is not appropriate at this time. |
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Overburden
or waste was subtracted from the gross tonnage in each
tract block. The thickness of this in-place overburden
was determined by averaging the overburden encountered
in the drill holes located in each block. The wide spacing
between each drill hole limits the overall accuracy of
this method. However, the deepest overburden zone encountered
in the drilling was only 15 feet and, therefore, it is
assumed that any inaccuracies inherent in the overburden
computations will not greatly alter the overall tonnage
figures. During the drilling of hole #157 in Section 34,
4.2 feet of basalt was encountered just below 10.1 feet
of overburden. This basalt is interpreted as a surface
flow and therefore has been included with overburden for
calculation purposes. |
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In figuring
interburden zones, widely spaced Sunbelt drill holes were
argillaceous sandstone, clay, sandy clay, pebble conglomerate
and some basalt were combined and totaled for each drill
hole. A ratio was then computed for each hole by comparing
total interburden with combines limestone and interburden
excluding overburden. Each ratio was then multiplied by
the gross tonnage to obtain a final tonnage exclusive
of overburden and interburden. This method was used only
on federal land staked by Sunbelt. On fee land owned by
NZ, a dilution ratio of 1:3 was chosen to approximate
the average of all the dilution ratios previously computed
for the Sunbelt claim group. This ratio was used to compute
all the NZ fee land reserves. |
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In Summary,
Sunbelt Mining Company, Inc., has analyzed the viability
of certain limestone leases presented in the lease option
agreement dated September 15, 1981 (Exhibit I) with NZ.
Sunbelt conducted a field exploration program in May and
July of 1982 completing 10 drill holes. Quality samples
were obtained from the limestone core in drill hole number
50. Drilling penetrated 206.4" of solid, massive
limestone. Four core samples were selected at intervals
demonstrating greatest visual and textural variability.
These four samples were sent to Fuller Company for analyses
on May 20, 1982. Fuller crushed and split each sample
and returned to the unused half to Sunbelt. The split
from Sample #2 was sent to Hazen Research, Inc. and tested
to confirm procedures and results obtained from Fuller." |
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As dimension
stone, this deposit would have a retail value of over
$2 Trillion. The calcium carbonate material is also used
for cement, lime, road-base stabilizer, and flue gas scrubber
material for coal-fired power plants (it removes the sulfur
that causes acid-rain). |
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NZ is concluding
their homework on this deposit and have resolved the following:
1. Travertine is mined Mexico and Turkey at much lower
labor costs; 2. The Italians started selling high technology
rock fabrication equipment to these countries to automate
their quarries and fabrication plants; 3. The market in
the US is mostly time sensitive custom stone fabrication. |
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NZ toured
one of the largest plants in Belen, New Mexico on October
2, 2003. The conclusion is that mining the travertine
for industrial purposes is a much larger opportunity than
a dimension stone facility. However, it seems that a dimension
stone quarry could produce an income of $250,000 per year
profit if done carefully and maintained at a smaller scale.
NZ has a lessee that pays $.50 per ton or 5% royalty whichever
is greater. If the deposit is used and depleted for a
lower value industrial application it would still payout
over $200 Million. |
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In February
2004, NZ enlisted Pincock, Allen & Holt, mineral experts
to evaluate and review the travertine mineral files. Their
conclusions are summarized in a report. |
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