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| Austinite
was named to honor Professor Austin Flint Rogers (1877-1957), American mineralogist, Stanford University, Palo Alto, California, USA.
| Discovered
in 1935;
IMA
status: Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
CaZn(AsO4)(OH)
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Calcium Zinc Arsenate Hydroxide
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Molecular
Weight: |
261.39 gm
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Composition: |
Calcium |
15.33 % |
Ca |
21.45 % |
CaO |
|
Zinc |
25.02 % |
Zn |
31.14 % |
ZnO |
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Arsenic |
28.66 % |
As |
43.96 % |
As2O5 |
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Hydrogen |
0.39 % |
H |
3.45 % |
H2O |
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Oxygen |
30.60 % |
O |
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|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Phosphates
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Strunz 8th
Ed. ID:
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7/B.26-40
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Nickel-Strunz 10th
Ed. ID:
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8.BH.35
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8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
H : With medium-sized and large cations, (OH,etc.):RO4 = 1:1
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Related
to: |
Adelite-Descloizite Group. Austinite-Conichalcite Series.
The zinc analogue of Cobaltausinite and Nickelaustinite.
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Members
of Group: |
Adelite-Descloizite Group:
Adelite, Arsendescloizite, Austinite, Cechite, Cobaltaustinite,
Conichalcite, Descloizite, Duftite, Gabrielsonite, Gottlobite,
Hermannroseite, Mottramite, Nickelaustinite, Pyrobelonite,
Tangeite
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Varieties: |
Cobaltoan
Austinite,
Cuprian
Austinite
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Synonyms: |
Brickerite
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Crystal
Data
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Crystallography:
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Orthorhombic
- Disphenoidal
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Crystal
Habit:
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As
enantiomorphous bladed crystals exhibiting {011}, {111},
{111}, {010} and several other forms, sometimes forming
scepters. Also as radially fibrous crusts and nodules.
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Twinning:
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Left-
and right-handed individuals joined on (100), with (010)
and (001) coincident.
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Physical
Properties
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Cleavage: |
Good
on {011}
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Fracture: |
Irregular/Uneven,
Conchoidal
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Tenacity:
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Brittle
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Moh's
Hardness: |
4.0
- 4.5
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Density:
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4.13 (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: |
Colorless to pale Yellowish White or bright Green; Colorless in transmitted light.
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Transparency: |
Transparent
to Translucent
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Luster: |
Sub-Adamantine,
Silky in aggregates
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Refractive
Index: |
1.759
- 1.783 Biaxial ( + )
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Birefringence: |
0.0240
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Dispersion: |
Weak;
r > v
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Pleochroism: |
None
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Occurances
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Geological
Setting: |
A
rare secondary mineral in the oxidized zone of some
arsenic-rich base-metal deposits. |
Common
Associations: |
Adamite,
Limonite, Quartz, Talmessite (Gold Hill, Utah, USA)
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Common
Impurities: |
None
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Type
Locality: |
Gold Hill Mine (Western Utah Mine), Gold Hill, Gold Hill District (Clifton District), Deep Creek Mts, Tooele County, Utah, USA
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Year
Discovered: |
1935
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View
mineral photos: |
Austinite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org
Webmineral.com
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Austinite
is a fairly rare mineral and an extremely rare gem.
Mineral specimens are very collectable as they occur
as radial clusters of colorless to intense emerald
green crystals. Austinite forms in the oxidation zone
of zinc ore deposits often associated with Adamite.
Austinite
is found in just a handful of localities. In the USA,
at the Type Locality in the Western Utah mine, Gold
Hill, Tooele County, Utah; at the Mohawk mine, Clark
Mountains, San Bernardino County, California; from
the Table Mountain mine, Galiuro Mountains, Pinal County, Arizona;
at Sterling Hill, Ogdensburg, Sussex County, New
Jersey; in the Tucker’s tunnel uranium deposit, near
Durango, Hinsdale County, Colorado. From the Ojuela
mine, Mapimi, Durango, Mexico. At the Lili mine, near
Lomitos, Bolivia. From the Kamariza mine, Laurium, Greece.
At Tsumeb and Guchab, Otavi district, Namibia. In the
Puttapa zinc mine, near Beltana, South Australia.
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Austinite
gems for sale:
We
have not photographed our Austinite gems
yet. Please
check back soon.
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