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| Chemistry:
CuS | Discovered
in 1832;
IMA
status: Valid (pre-IMA; Grandfathered). Covellite,
also known as Covelline, is named after N. Covelli (1790-1829), an Italian mineralogist and discoverer of the
mineral at Mount Vesuvius. |
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Classification
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Mineral
Classification: |
Sulphides |
Strunz 8th
Ed. ID:
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2/C.22-10 |
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2 : Sulphides C : Sulphides with metal: sulphur, selenium
and tellurium = 1:1 22 : Covellite series
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Crystal
Data
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Crystallography:
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Hexagonal
- Dihexagonal Dipyramidal |
Crystal
Habit:
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Forms
hexagonal plates as large as 10 cm, flattened on [0001],
which may exhibit hexagonal striae; as rosettes of nearly
parallel plates; commonly massive and foliated.
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Twinning:
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None
reported
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Physical
Properties
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Cleavage: |
[0001]
Perfect
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Fracture: |
Irregular,
Uneven, Hackly, Flaky
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Tenacity:
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Flexible
in thin leaves
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Hardness
(Moh's): |
1.5
- 2.0 VHN100=128 - 138 kg/mm2
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Hardness
(Vickers): |
VHN100=128 - 138 kg/mm2
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Density:
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4.60 - 4.76 (g/cm3) |
Luminescence:
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None |
Radioactivity:
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Not
Radioactive
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Other: |
Nonmagnetic |
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Optical
Properties
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Color: |
Deep,
metallic, Indigo-blue, inclining towards blue-black, often iridescent with
purplish, deep red, and brassy-yellow reflections. |
Transparency: |
Opaque |
Luster: |
Metallic,
Submetallic,
inclining to resinous, somewhat pearly on cleavage;
subresinous to dull when massive. |
Refractive
Index: |
1.450 - 2.620 Uniaxial
( + ) |
Birefringence: |
1.170 |
Dispersion: |
Strong
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Pleochroism: |
Visible; deep blue to blue-white
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Anisotropism: |
Strong
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Occurances
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Geological
Setting: |
Most
commonly of secondary origin in the zone of oxidation
in sulfide copper deposits. Rarely of primary hydrothermal
origin. Widespread in most copper deposits; common as
an iridescent tarnish on other sulfides. |
Type
Locality: |
Mt. Vesuvius, Somma-Vesuvius Complex, Naples Province,
Campania, Italy |
Year
Discovered: |
1832 |
View
mineral photos: |
Covellite
Mineral Photos and Locations |
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More
Information
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Mindat.org Webmineral.com |
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Covellite
is a little known sulphide mineral in the gem world
but one look at its metallic luster, iridescent, deep
indigo blue color with purplish, deep red and brassy-yellow
reflections would make just about anyone a fan of this
rare and beautiful gem. Covellite is always opaque,
so it is only available as cabochons. But Covellite
has perfect, leafy cleavage so even cabochons are rare.
Covellite
is found in a few locations worldwide but fine crystals
are rare. The most notable occurances are Mt. Vesuvius,
Campania, and Calabona
mine, Alghero, Sardinia, Italy; Butte, Silver Bow Co.,
Montana, USA as fine crystals in the primary ore; and
at the Galactic Open Pit, Summitville, Summit District, Rio Grande Co., Colorado, USA.
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Covellite
gems for sale:
We
have not photographed our Covellite gems yet. Please
check back soon!
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