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| Alabandite
is named for its supposed discovery locality at Alabanda, Aďdin, Turkey.
| Discovered
in 1832;
IMA
status:
Valid (pre-IMA; Grandfathered) |
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Composition: |
Manganese |
63.14 % |
Mn |
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Sulfur |
36.86 % |
S |
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100.00 % |
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Classification
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Mineral
Classification: |
Sulfides
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Strunz 8th
Ed. ID:
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2/C.15-30
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Nickel-Strunz 10th
Ed. ID:
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2.CD.10
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2 : SULFIDES and SULFOSALTS (sulfides, selenides,
tellurides; arsenides, antimonides, bismuthides; sulfarsenites,
sulfantimonites, sulfbismuthites, etc.) C : Metal Sulfides, M: S = 1: 1 (and similar) D : With Sn, Pb, Hg, etc.
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Related
to: |
Galena
Group. Dimorphous
with Rambergite.
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Members
of Group: |
Galena
Group: Alabandite,
Altaite, Clausthalite, Galena, Niningerite, Oldhamite
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Varieties: |
None
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Synonyms: |
Alabandine,
Alabandite (of Beudant), Glance-blende, Manganblende
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Crystal
Data
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Crystallography:
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Isometric
- Hexoctahedral
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Crystal
Habit:
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Crystals
cubic or octahedral, to 1 cm. Commonly massive, granular.
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Twinning:
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Lamellar
|| {111}
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Physical
Properties
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Cleavage: |
Perfect
on {001}
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Fracture: |
Irregular/Uneven
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Tenacity:
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Brittle
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Moh's
Hardness: |
3.5
- 4.0; VHN
= 164–174, 167 average (100 g load)
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Density:
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3.95
- 4.04 (g/cm3)
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Luminescence:
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None
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Radioactivity:
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Not
Radioactive
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Optical
Properties
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Color: |
Iron-Black,
tarnishing Brown; in polished section, Gray-White; deep
Green to Brown and Red in thin slivers.
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Transparency: |
Opaque,
but Translucent in very thin fragments. |
Luster: |
Sub-Metallic
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Refractive
Index: |
2.70
Isotropic
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Birefringence: |
0.00
Isotropic
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Dispersion: |
None |
Pleochroism: |
None
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Other: |
Color in reflected light: white to gray
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Occurances
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Geological
Setting: |
May
be in large quantities in epithermal polymetallic sulfide
vein and especially in low-temperature manganese deposits.
An uncommon constituent of a number of meteorites. |
Common
Associations: |
Galena,
Chalcopyrite, Sphalerite, Pyrite, Acanthite, Tellurium,
Rhodochrosite, Calcite, Rhodonite, Quartz
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Common
Impurities: |
Fe,
Mg, Co |
Type
Locality: |
Sacarîmb (Săcărâmb; Szekerembe; Nagyág), Hunedoara Co., Romania
(originally incorrectly reported from Aydin,
Aydin Province, Turkey) |
Year
Discovered: |
1832
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View
mineral photos: |
Alabandite
Mineral Photos and Locations |
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More
Information
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Mindat.org
Webmineral.com
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Alabandite
is a relatively rare manganese sufide mineral that is
most often found as massive to granular aggregates but
also rarely as cubic or octahedral crystals to 1 cm.
It
was originally incorrectly reported from Aydin, Aydin
Province, Turkey but was first found at Săcărîmb, Hunedoara, Romania.
Alabandite is colored iron-black, tarnishing brown;
in polished section, gray-white; deep green to brown
and red in thin slivers.
It takes a good polish and is an attractive cabochon
gem for collectors of unusual Black
or Metallic
gems.
Selected
localities include Alabanda, 30 km south-southeast of
Aydin, Aydin Province, Turkey. At Baia-de-Aries (Offenbánya),
Săcărîmb (Nagyág), and Cavnic (Kapnikbánya), Romania.
From Adervielle, Hautes-Pyrénées, France. At Gersdorf,
Saxony, Germany. From manganese mines in Val Graveglia,
Liguria, Italy. At Nsuta, Ghana. In the Yakumo and Inakuraishi
mines, Hokkaido; the Taisei mine, Akita Prefecture;
and many other localities in Japan. From Broken Hill,
New South Wales, Australia. In Peru, at Morococha, Junin.
In the Preciosa mine, Tlalchichuca, Puebla, and at Onovas,
Sonora, Mexico. In the USA, in the Lucky Cuss mine,
Tombstone, Cochise County, Arizona; the Queen of the
West mine, Summit County, Colorado; at Schellbourne,
White Pine County, Nevada; and from Butte, Silver Bow
County, Montana.
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Alabandite
gems for sale:
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have not photographed the Alabandite gems yet. Please
check back soon.
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