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| Poldervaartite
was named to honor Arie Poldervaart (1918 - 1964), who
was a Professor of Petrology at Columbia University,
New York City, New York, USA.
| Discovered
in 1992;
IMA
status: Valid (Approved 1993) |
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Chemistry
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Chemical
Formula: |
(CaMn2+)2(SiO3OH)(OH)
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Calcium
Manganese Silicate Hydroxide |
Molecular
Weight: |
197.68 gm
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Composition: |
Calcium |
30.41 % |
Ca |
42.55 % |
CaO |
|
Manganese |
13.90 % |
Mn |
17.94 % |
MnO |
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Silicon |
14.21 % |
Si |
30.39 % |
SiO2 |
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Hydrogen |
1.02 % |
H |
9.11 % |
H2O |
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Oxygen |
40.47 % |
O |
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Classification
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Mineral
Classification: |
Silicates (Germanates)
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Strunz 8th
Ed. ID:
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8/B.22-22
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Nickel-Strunz 10th
Ed. ID:
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9.AF.90
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9 : SILICATES (Germanates)
A : Nesosilicates F :
Nesosilicates with additional anions; cations in [4], [5] and/or only [6]
coordination
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Related
to: |
Olmiite
- Poldervaartite Series. The Ca-dominant analogue of Olmiite.
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Varieties: |
None
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Synonyms: |
IMA1992-012
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Crystal
Data
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Crystallography:
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Orthorhombic - Dipyramidal
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Crystal
Habit:
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Crystals
are prismatic, with {110}, {100}, {010}, and {001},
to 7 mm; aggregates in sheaves.
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Twinning:
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None
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Physical
Properties
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Cleavage: |
None
observed
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Fracture: |
Irregular/Uneven
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Tenacity:
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Very
Brittle
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Moh's
Hardness: |
5.0
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Density:
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2.91 (g/cm3)
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Luminescence:
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Fluoresces
deep red under SW UV. |
Radioactivity:
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Not
Radioactive
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Optical
Properties
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Color: |
Colorless, milky white, pink-white
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Transparency: |
Transparent,
Translucent |
Luster: |
Vitreous
on fractures to Sub-Vitreous on crystal faces |
Refractive
Index: |
1.634 - 1.656 Biaxial ( +
) |
Birefringence: |
0.0220
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Dispersion: |
Weak; r < v |
Pleochroism: |
Weak;
X
= colorless; Y
= light gray; Z
= bluish gray |
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Occurances
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Geological
Setting: |
In
a pocket in massive manganese ores in a bedded manganese
ore deposit. |
Common
Associations: |
Braunite,
Hausmannite, Henritermierite, Bultfonteinite, Hematite,
Calcite
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Common
Impurities: |
Fe,
Mg, H2O
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Type
Locality: |
Wessels Mine (Wessel's Mine), Hotazel, Kalahari manganese fields, Northern Cape Province, South Africa
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Year
Discovered: |
1992;
(IMA
approved 1993)
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View
mineral photos: |
Poldervaartite
Mineral Photos and Locations |
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More
Information
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Mindat.org
Webmineral.com
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Poldervaartite is an
extremely rare mineral
that was discovered in 1992 at the Wessels Mine, Hotazel,
Kalahari manganese fields, Northern Cape Province, South
Africa. Wessels Mine and N'Chwaning Mine, both
at the Kalahari manganese fields, are still
the only known sources of Poldervaartite. It is a very rare gem because most crystals
or not suitable for faceting. It ranges in color
from colorless to light orangish-pink. (photograph above courtesy
of Jay Medici, gem in picture also faceted by Jay Medici).
It
has recently been determined that most Poldervaartite
mineral specimens and gems are actually the mineral
Olmiite. The two are very closely related, being differentiated
only by the percentage of Calcium (Ca) versus Manganese
(Mn) contained. Specimens with Mn dominance are Olmiite
and those with Ca dominance are Poldervaartite. This
would mean that most, if not all, Poldervaartite specimens
and gems currently on the market are, in fact, Olmiite
and that there may not even be any Poldervaartite
gems in existance!
It is impossible to determine the difference between
the two visually and must be tested by electron microprobe analysis.
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Poldervaartite
gems for sale (please see our Olmiite gems
for sale)
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