Classification
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Mineral
Classification: |
Oxides
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Strunz 8th
Ed. ID:
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4/D.25-10
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Nickel-Strunz 10th
Ed. ID:
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4.DE.30
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4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites,
bismuthites, sulfites, selenites, tellurites, iodates) D : Metal: Oxygen =
1:2 and similar E : With medium-sized cations; with various polyhedra
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Related
to: |
Cervantite - Chiluite Series.
Dimorph of Clinocervantite.
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Varieties: |
None
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Synonyms: |
Antimonial Ochre,
Antimonous Acid
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Crystal
Data
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Crystallography:
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Orthorhombic
- Pyramidal
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Crystal
Habit:
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Minute acicular crystals, massive.
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Twinning:
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None
observed.
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Physical
Properties
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Cleavage: |
Perfect
on {001}, Distinct on {100}
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Fracture: |
Conchoidal
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Tenacity:
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Brittle
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Moh's
Hardness: |
4.0
- 5.0
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Density:
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6.50
- 6.64 (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: |
Yellow, off-White, Reddish-White; Colorless in transmitted light
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Transparency: |
Semi-Translucent
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Luster: |
Greasy,
Pearly; Earthy when powdery
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Refractive
Index: |
2.000
- 2.100 Biaxial ( ? )
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Birefringence: |
0.100
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Dispersion: |
Relatively
Weak
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Pleochroism: |
None
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Occurances
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Geological
Setting: |
A
secondary mineral formed from the oxidation of stibnite.
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Common
Associations: |
Stibnite
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Common
Impurities: |
None
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Type
Locality: |
Cervantes, Sierra de Ancares, Lugo, Galicia, Spain
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Year
Discovered: |
1850
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View
mineral photos: |
Cervantite
Mineral Photos and Locations |
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More
Information
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Mindat.org
Webmineral.com
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Cervantite
is a rare oxide mineral that is formed from the oxidation
of Stibnite. It is usually found as minute acicular crystal
clusters or massive material but rarely as fine
needle inclusions in Quartz.
These inclusions in Quartz make for beautiful gems
showing bright yellow needles.
Cervantite
is found in several locations worldwide but the main
occurance of fine needle inclusions in Quartz is Minas
Gerais, Brazil.
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