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| Crocidolite
is named from the Greek kpokus, meaning nap
of cloth, in allusion to its finely fibrous habit.
Riebeckite is named for Emil Riebeck (1853-1885), German explorer.
| Discovered
in 1815;
IMA
status: Riebeckite is Valid (pre-IMA; Grandfathered) |
|
Information
below is for Riebeckite |
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Chemistry
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Chemical
Formula: |
Na2Fe2+3Fe3+2(Si8O22)(OH)2
|
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Iron
Sodium Silicate Hydroxide |
Molecular
Weight: |
935.90 gm |
Composition: |
Sodium |
4.91 % |
Na |
6.62 % |
Na2O |
|
Iron |
29.84 % |
Fe |
23.03 % |
FeO
/ 17.06% Fe2O3 |
|
Silicon |
24.01 % |
Si |
51.36 % |
SiO2 |
|
Hydrogen |
0.22 % |
H |
1.92 % |
H2O |
|
Oxygen |
41.03 % |
O |
|
|
|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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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/F.08-50
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Nickel-Strunz 10th
Ed. ID:
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9.DE.25
|
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9 : SILICATES (Germanates) D : Inosilicates E : Inosilicates with 2-periodic double chains, Si4O11; Clinoamphiboles
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Related
to: |
Amphibole
Group. Sodic Clino-Amphibole Subgroup. Magnesioriebeckite-Riebeckite
Series.
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Varieties: |
Crocidolite
is a variety of Riebeckite
|
Synonyms: |
Abriachanite,
Blue Asbestos, Blue Ironstone, Cape Asbestos, Cape Blue,
Krokydolith, South
African cat's eye
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Crystal
Data
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Crystallography:
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Monoclinic
- Prismatic
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Crystal
Habit:
|
As
prismatic crystals, to 20 cm. Commonly fibrous, asbestiform;
earthy, massive.
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Twinning:
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Simple
or multiple twinning || {100}.
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Physical
Properties
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|
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Cleavage: |
Perfect
on {110} intersecting
at 56° and 124°; partings on {100}, {010}
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Fracture: |
Conchoidal
to Uneven, Splintery
|
Tenacity:
|
Brittle
|
Moh's
Hardness: |
5.0
- 6.0
|
Density:
|
3.28
- 3.44 (g/cm3)
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Luminescence:
|
None |
Radioactivity:
|
Not
Radioactive
|
Other: |
An asbestos mineral. Fibres, if breathed in, can cause serious and irreversable lung damage. Avoid exposure to dust.
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Optical
Properties
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|
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Color: |
Gray-Blue to leek-Green
|
Transparency: |
Semi-transparent
to Opaque
|
Luster: |
Vitreous
to Silky
|
Refractive
Index: |
1.656
- 1.740 Biaxial ( + ) or ( - )
|
Birefringence: |
0.005
- 0.008
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Dispersion: |
Strong
|
Pleochroism: |
X
= blue, indigo; Y
= yellowish green, yellowbrown; Z
= dark blue
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Other: |
Exhibits
chatoyance and cat's eye effect
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Occurances
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Geological
Setting: |
In
alkalic granites and syenites; rarer in felsic volcanics
and granite pegmatites; in some schists. In iron formations
as asbestiform "Crocidolite." |
Common
Associations: |
Aegirine,
Nepheline, Albite, Arfvedsonite (igneous); Tremolite,
Ferro-actinolite (metamorphic); Grunerite, Magnetite,
Hematite, Stilpnomelane, Ankerite, Siderite, Calcite,
Chalcedony, Quartz (iron formations) |
Common
Impurities: |
Fe,
Ti, Mg, Al, Mn |
Type
Locality: |
Socotra Island, Adan Governorate, Yemen
|
Year
Discovered: |
1815
(Crocidolite); 1888 (Riebeckite) |
View
mineral photos: |
Crocidolite
Mineral Photos and Locations |
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More
Information
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Mindat.org
(Crocidolite) Mindat.org
(Riebeckite) Webmineral.com
(Riebeckite)
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|
Crocidolite
is a fibrous, or asbestiform, variety of Riebeckite
and belongs to the Amphibole Group of minerals that
also includes Actinolite ,
Arfvedsonite,
Riebeckite and Tremolite.
Riebeckite forms in alkalic granites and syenites while
Crocidolite forms in iron formations. Crocidolite was
first described in 1815 by M. H. Klaproth under the
name Blaueisenstein
meaning blue
ironstone,
and in 1831 by J. F. Hausmann, who gave it its present
name Crocidolite which is from the Greek word kpokus
meaning nap of cloth in allusion to its fibrous
habit. Crocidolite fibers are finely textured and hair-like, occurring in naturally formed bundles
or mats. Its resemblance to asbestos has earned it the name
Cape Asbestos, the chief occurrence being in Cape Colony, South Africa. Crocidolite
is formed by geologic alteration by the removal of alkali
and peroxidation of the ferrous iron and furher by deposition
of silica between the fibers or by their replacement
by silica. A hard siliceous mineral is formed which
can be polished and exhibits a beautiful chatoyance
with silky luster and a smooth "cat's eye"
effect. Upon further alteration and deposition of silica
this mineral becomes the popular golden brown mineral
known as "tiger-eye" or "hawk's-eye"
when colored blue. Another alteration product of Crocidolite, consisting of silica and ferric hydrate, is called Griqualandite
for its occurance in the Asbestos Mountains, Griqualand West, Cape Colony,
South Africa.
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Crocidolite
gems for sale:
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have not photographed our Crocidolite gems. Please
check back soon.
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