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| Valleriite
was named to
honor Johan Gottschalk Wallerius (Vallerius) (1709–1785), Swedish chemist and mineralogist.
| Discovered
in 1870; IMA
status:
Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
(Fe2+,Cu)4(Mg,Al)3S4(OH,O)6 also:
4(Fe,Cu)S
• 3(Mg,Al)(OH)2
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Iron
Copper Magnesium Aluminum Hydroxy Sulfide |
Molecular
Weight: |
475.92 gm
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Composition: |
Magnesium |
8.68 % |
Mg |
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Aluminum |
7.37 % |
Al |
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Iron |
25.82 % |
Fe |
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Copper |
24.03 % |
Cu |
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Hydrogen |
0.42 % |
H |
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Sulfur |
26.95 % |
S |
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Oxygen |
6.72 % |
O |
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100.00 % |
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Classification
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Mineral
Classification: |
Sulfides
and Sulfosalts
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Strunz 8th
Ed. ID:
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2/C.23-20
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Nickel-Strunz 10th
Ed. ID:
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2.FD.30
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2 : SULFIDES and SULFOSALTS (sulfides, selenides,
tellurides; arsenides, antimonides, bismuthides; sulfarsenites,
sulfantimonites, sulfbismuthites, etc.) F : Sulfides of arsenic, alkalies; sulfides with halide, oxide, hydroxide, H2O
D : With O, OH, H2O
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Related
to: |
Valleriite
Group.
|
Members
of Group: |
Valleriite
Group: Ekplexite,
Ferrotochilinite, Ferrovalleriite, Haapalaite, Tochilinite,
Valleriite, Yushkinite
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Varieties: |
None
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Synonyms: |
None
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Crystal
Data
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Crystallography:
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Trigonal - Hexagonal Scalenohedral
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Crystal
Habit:
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Massive,
as nodules, to 5 mm; also in tiny splinters, very thin
flakes, and thin crusts.
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Twinning:
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None
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Physical
Properties
|
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Cleavage: |
Excellent
on {0001}
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Fracture: |
n/a
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Tenacity:
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Brittle
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Moh's
Hardness: |
<
1.0
- 1.5; less
than graphite
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Density:
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3.14 (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: |
Bronze-yellow
to dark gray, resembling Pyrrhotite
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Transparency: |
Opaque
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Luster: |
Metallic
to sub-metallic |
Refractive
Index: |
R1–R2:
(400) 10.5–11.1, (420) 10.8–11.3, (440) 10.7–12.7, (460)
10.6–14.2, (480) 10.5–15.8, (500) 10.5–17.3, (520) 10.3–18.8,
(540) 10.3–20.1, (560) 10.3–21.3, (580) 10.2–22.4, (600)
10.3–23.4, (620) 10.3–24.4, (640) 10.3–25.1, (660) 10.4–25.8,
(680) 10.3–26.4, (700) 10.3–26.9
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Birefringence: |
0.000
(opaque)
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Dispersion: |
n/a |
Pleochroism: |
Strong; pale yellow to deep brown |
Anisotropism: |
Strong;
golden yellow
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Occurances
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Geological
Setting: |
An
alteration product of chalcopyrite in chromitites and
dunites (Cyprus); in copper-bearing carbonatites, replacing
magnetite (Phalaborwa, South Africa); in Cu–Ni sulfide-bearing
serpentinized and uralized ultramafic rocks. |
Common
Associations: |
Chalcopyrite,
Cubanite, Pyrrhotite, Troilite, Millerite, Pentlandite,
Pyrite, Marcasite, Mackinawite, Tochilinite, Magnetite
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Common
Impurities: |
Ni,
Ca, K, Na, Si |
Type
Locality: |
Aurora Mine, Kaveltorp Mines, Kopparberg, Ljusnarsberg, Västmanland, Sweden
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Year
Discovered: |
1870
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View
mineral photos: |
Valleriite
Mineral Photos and Locations |
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Unusual
Gem Categories
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Metallic
Gems |
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More
Information
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Mindat.org
Webmineral.com
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Valleriite
is an uncommon hydroxy-sulfide
(sulfosalt) of iron, copper, magnesium and aluminum.
It is often found associated with other similar sulfide
minerals such as Bornite,
Chalcopyrite,
Cubanite,
Marcasite,
Pentlandite, Pyrite and
Pyrrhotite.
Valleriite is an alteration product of Chalcopyrite or other copper minerals. It
is opaque, bright to dark bronze colored with metallic luster,
often resembling Pyrrhotite, but it is very soft, with
a Moh's hardness of about 1.
Valleriite
was named to
honor Johan Gottschalk Wallerius (Vallerius) (1709–1785), Swedish chemist and mineralogist.
In 1750, Wallerius was elected member of the Royal Swedish Academy of Sciences.
He is regarded as the founder of agricultural chemistry, mainly based on the significance of his work Agriculturae fundamenta chemica published in 1761.
Valleriite
distribution: an
inconspicuous mineral, now recognized from a number
of localities in addition to those listed here. In Sweden,
in Kopparberg, from the Aurora mine, Ljusnarsberg [TL],
and at Kaveltorp. In South Africa, in Transvaal, from
the Loolekop carbonatite, Phalaborwa, and at the Mooihoek
and Onverwacht pipes, in the Merensky Reef, Bushveld
complex. From near Pefkos, Cyprus. In Canada, at the
Little Chief mine, near Whitehorse, Yukon Territory;
in the Marbridge mine, Malartic, Quebec; and at Sudbury,
Ontario. In the USA, from the Elizabeth mine, South
Strafford, Strafford County, Vermont; in the Pima mine,
near Tucson, Pima County, and at the Christmas mine,
Gila County, Arizona; from the Continental mine, Fierro,
Grant County, New Mexico. In Russia, in the Talnakh
area, Noril’sk region, western Siberia; from the Kovdor
and Monchegorsk massifs, Kola Peninsula. At Alnalyk,
Uzbekistan. In the Akagane mine, Iwate Prefecture, Japan.
From Wannaway, Western Australia. On the East Pacific
Rise (21 N).
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