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| Berzelianite
was named for Jöns Jacob Berzelius (1779–1848), Swedish
chemist, who discovered selenium.
| Discovered
in 1832;
IMA
status: Valid (pre-IMA; Grandfathered) |
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Composition: |
Copper |
61.68 % |
Cu |
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Selenium |
38.32 % |
O |
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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/B.03-10
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Nickel-Strunz 10th
Ed. ID:
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2.BA.20
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2 : SULFIDES and SULFOSALTS (sulfides, selenides,
tellurides; arsenides, antimonides, bismuthides; sulfarsenites,
sulfantimonites, sulfbismuthites, etc.) B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
A : With Cu, Ag, Au
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Related
to: |
Berzelianite-Umangite Group.
Dimorphous with Bellidoite.
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Members
of Group: |
Berzelianite-Umangite Group:
Berzelianite, Umangite
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Varieties: |
None
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Synonyms: |
Berzeline (of Beudant),
Selencuprite, Selenite (of Rau), Selenocuprite
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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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As
thin dendritic crusts; fine grained and disseminated
as powdery inclusions.
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Twinning:
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None
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Physical
Properties
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Cleavage: |
None
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Fracture: |
Irregular/Uneven
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Tenacity:
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Malleable
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Moh's
Hardness: |
2.7;
VHN
= 21–24 (100 g load)
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Density:
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6.71 (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: |
Silver-White, shiny lead-grey; easily tarnishes iridescent blue-grey
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Transparency: |
Opaque
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Luster: |
Metallic
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Refractive
Index: |
R:
(400) 25.8, (420) 28.9, (440) 30.0, (460) 30.7, (480)
31.1, (500) 31.0, (520) 30.2, (540) 28.7, (560) 27.0,
(580) 25.5, (600) 24.1, (620) 22.9, (640) 21.8, (660)
20.7, (680) 19.7, (700) 18.7
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Birefringence: |
0.000
(Isotropic)
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Dispersion: |
n/a |
Pleochroism: |
None
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Anisotrophism: |
Isotropic;
may
be slightly anisotropic
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Occurances
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Geological
Setting: |
With
other selenides in hydrothermal veinlets in dolostone
(Clausthal, Germany); in iron ores (Lerbach, Germany);
with other selenides in calcite veins in serpentine
(Skrikerum, Sweden); in a gold-quartz-orthoclase deposit
(Redjang-Lebong, Sumatra). |
Common
Associations: |
Eucairite,
Clausthalite, Tiemannite, Umangite, Klockmannite, Aguilarite,
Crookesite, Athabascaite, Stromeyerite, Polybasite,
Pearceite, Gold, Uraninite, Pyrite, Marcasite, Calcite.
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Common
Impurities: |
Ag,
Ti |
Type
Locality: |
Skrikerum Mine, Valdemarsvik, Östergötland, Sweden
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Year
Discovered: |
1832
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View
mineral photos: |
Berzelianite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org
Webmineral.com
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Berzelianite
is a copper selenide mineral that is relatively soft,
with a Moh's hardness of only 2.7, and is somewhat malleable.
It has a metallic luster and silver-white to shiny lead-grey
color when freshly broken and easily tarnishes to iridescent blue-grey.
Berzelianite was named for Jöns Jacob Berzelius (1779–1848),
Swedish chemist, who discovered selenium, one of the
main components of Berzelianite. A recent study showed the existence of a complete solid-solution series between high Digenite [cubic, high-temperature Digenite] and Berzelianite (Pirard & Hatert, 2008).
Distribution:
At Skrikerum, near Tryserum, Kalmar, Sweden (Type Locality). From
Lerbach, Tilkerode, Zorge, Clausthal, and St. Andreasberg,
Harz Mountains; at Niederschlema, Saxony; and the Mullenbach
uranium deposit, Black Forest, Germany. In the Czech
Republic, in the Habrí and Bukov mines, near Tisnova;
at the Petrovice uranium deposit, near Ždar; and the
Predborice uranium deposit, near Krásna Hora. From the
Kyzylalmasay gold deposit, Uzbekistan. In the Sierra
de Umango, and at Tuminico, Sierra de Cacho, La Rioja
Province, Argentina. From the Elefante prospect, near
the Serra Pelada Au–Pd–Pt deposit, Pará, Brazil. At
Redjang-Lebong, Sumatra. From Kalgoorlie and in the
Copper Hills prospect, East Pilbara region, Western
Australia, and at El Sharana, Northern Territory, Australia.
In the Pinky Fault uranium deposit, Lake Athabasca,
Saskatchewan, Canada. From the Durant vein, Aurora district,
Mineral County, Nevada, USA.
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