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| Magnetite
is an ancient term, possibly an allusion to the locality,
Magnesia, Greece, an early locality for Lodestone.
| Discovered
in 1845;
IMA
status: Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
Fe3+2Fe2+O4 |
|
Iron
Oxide |
Molecular
Weight: |
231.54 gm |
Composition: |
Iron |
72.36 %
|
Fe
|
31.03 %
|
FeO
/ 68.97% Fe2O3
|
Oxygen |
27.64 % |
O |
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|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Oxides
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Strunz 8th
Ed. ID:
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4/B.02-20
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Nickel-Strunz 10th
Ed. ID:
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4.BB.05 |
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4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates) B : Metal: Oxygen = 3:4 and similar B : With only medium-sized cations
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Related
to: |
Spinel
Group. Iron Subgroup. Jacobsite-Magnetite Series. Magnesioferrite-Magnetite
Series.
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Varieties: |
Aluminous
Magnetite, Hydromagnetite, Ishkulite, Lodestone, Manganmagnetite,
Mg-Titanomagnetite, Mushketovite, Nickeloan Magnetite,
Silfbergite (of Niggli), Titaniferous Magnetite, Vanado-Magnetite
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Synonyms: |
Aimantine,
Diamagnetite, Ferroferrite, Heraclian, Lodestone, Magnet,
Magnetic Iron Ore, Morpholite, Octahedral Iron Ore,
Oxydulated Iron, Sideritis, Syderite
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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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Typically
octahedral, less commonly dodecahedral, striated on
{011}, to 25 cm, very rarely cubic; skeletal, granular,
massive.
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Twinning:
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On
{111} as both twin and composition plane, the spinel
law, as contact twins, flattened, lamellar.
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Physical
Properties
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|
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Cleavage: |
Parting
on {111} very good; also reported as parting planes: {001}, {011}, {138}.
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Fracture: |
Irregular/Uneven
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Tenacity:
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Brittle
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Moh's
Hardness: |
5.5
- 6.5
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Density:
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5.175 (g/cm3)
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Luminescence:
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None |
Radioactivity:
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Not
Radioactive
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Other: |
Strongly
magnetic
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Optical
Properties
|
|
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Color: |
Black,
Gray with Browninsh tint in reflected light
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Transparency: |
Opaque,
Translucent on very thin edges
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Luster: |
Metallic
to SubMetallic, may be Dull
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Refractive
Index: |
2.42 (Isotropic)
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Birefringence: |
0.00 (Isotropic)
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Dispersion: |
Strong;
r > v
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Occurances
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Geological
Setting: |
A
common accessory mineral in igneous and metamorphic
rocks, in which magmatic segregation or contact metamorphism
may produce economic deposits. Extensive deposits in
sedimentary banded iron formations; a biogenic product;
important detrital deposits. |
Common
Associations: |
Chromite,
Ilmenite, Ulvospinel, Rutile, Apatite, Silicates (igneous);
Pyrrhotite, Pyrite, Chalcopyrite, Pentlandite, Sphalerite,
Hematite, Silicates (hydrothermal, metamorphic); Hematite,
Quartz (sedimentary). |
Common
Impurities: |
Mg,
Zn, Mn, Ni, Cr, Ti, V, Al |
Type
Locality: |
Magnesia, Greece |
Year
Discovered: |
1845 |
View
mineral photos: |
Magnetite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org Webmineral.com
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Magnetite
is a naturally magnetic mineral that is a member of
the Iron Subgroup of the Spinel Group of minerals that
also includes Franklinite.
The magnetism of Magnetite is due to two different types
of Iron; Fe +2 and Fe +3. The arrangement of these two
types of Iron causes a transfer of electrons between
the two which generates the magnetic field.
There
are many localities for Magnetite, even for fine crystals.
In Sweden, at Falun, Kiruna, Vastanfors, and elsewhere.
At Arendal, Norway. From Zlatoust and Magnetigorsk,
Ural Mountains, Russia. In the Zillertal, Tirol, Austria.
From Traversella, Piedmont, Italy. In Switzerland, at
Binntal and Rimpfischwang, Valais, and elsewhere. In
the Gardiner complex, beyond the head of Kangerdlugssuaq
Fjord, Greenland. From Bancroft, Ontario, Canada. In
the USA, around Lake Sanford, Essex County, and in the
Tilly Foster mine, Brewster, Putnam County, New York;
at Magnet Cove, Hot Springs County, Arkansas; in the
Iron Springs district, Iron County, Utah. From the Cerro
del Mercado, Durango, Mexico. At Itabira, Minas Gerais,
Brazil.
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