Magnetite

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Magnetite
Magnetite Russia.jpg
Magnetite from the Kola Peninsula, Russia
General
CategoryMineral
Chemical formulairon(II,III) oxide, Fe3O4
Identification
ColorBlack, greyish
Crystal habitOctahedral, fine granular to massive
Crystal systemIsometric
CleavageIndistinct
FractureUneven
Mohs Scale hardness5.5 - 6.5
LusterMetallic
Refractive indexOpaque
StreakBlack
Specific gravity5.17 - 5.18
Major varieties
LodestoneMagnetic with definite north and south poles

Magnetite is a ferrimagnetic mineral and one of several types of iron oxide. Its common chemical name is ferrous-ferric oxide, its official (IUPAC) name is iron(II,III) oxide, and its chemical formula is Fe3O4. It is a member of the spinel group of minerals and its crystals are black and opaque. It is the most magnetic of all naturally occurring minerals on Earth. Lodestone, used as an early form of magnetic compass, was a naturally magnetized form of magnetite.

This mineral is a valuable iron ore. In addition, as it carries the dominant magnetic signature in rocks, it has played a critical role in understanding plate tectonics. Changes in the oxygen content of the Earth's atmosphere can be inferred by studying sedimentary rocks containing magnetite. Moreover, interactions between magnetite and other oxide minerals have been studied to determine the oxidizing conditions and evolution of magmas over geological history.

Occurrence

Magnetite occurs in many sedimentary rocks, and huge deposits have been found in banded iron formations. In addition, this mineral (especially in the form of small grains) occurs in almost all igneous and metamorphic rocks. Many igneous rocks contain magnetite-rich and ilmenite-rich grains that precipitated together from magma. Magnetite is also produced from peridotites and dunites by serpentinization.

Magnetite is sometimes found in large quantities in beach sand. It is carried to the beach by the erosive action of rivers and is concentrated by waves and currents. Such mineral sands (also called iron sands or black sands) are found in various places, including beaches in California and the west coast of New Zealand. In June 2005, an exploration company (Candero Resources) discovered a vast deposit of magnetite-bearing sand dunes in Peru, where the highest dune is more than 2,000 meters (m) above the desert floor. The dune field covers 250 square kilometers (km²), and ten percent of the sand is magnetite.[1]

Large deposits of magnetite have been found in Kiruna, Sweden, and the Pilbara region of Western Australia. Additional deposits occur in Norway, Germany, Italy, Switzerland, South Africa, India, and Mexico. In the United States, it is found in the states of New York (Adirondack region), New Jersey, Pennsylvania, North Carolina, Virginia, New Mexico, Colorado, Utah, and Oregon.

Biological occurrences

Crystals of magnetite have been found in some bacteria (such as Magnetospirillum magnetotacticum) and in the brains of bees, termites, some birds (including pigeons), and humans. These crystals are thought to be involved in magnetoreception—the ability to sense the polarity or inclination of the Earth's magnetic field—and to aid in navigation. Also, chitons have teeth made of magnetite on their radula, making them unique among animals. This means they have an exceptionally abrasive tongue with which to scrape food from rocks. The study of biomagnetism began with the discoveries of Caltech paleoecologist Heinz Lowenstam in the 1960s.

Laboratory preparation

Magnetite can be prepared in the laboratory as a ferrofluid using the Massart method. It involves mixing iron(II) chloride and iron(III) chloride in the presence of sodium hydroxide.

Characteristics

This mineral is the most magnetic of all known naturally occurring minerals. Its Curie temperature is about 580 °C. Chemically, it dissolves slowly in hydrochloric acid.

The interactions between magnetite and other iron-rich oxide minerals—such as ilmenite, hematite, and ulvospinel—have been studied extensively, as the complicated reactions between these minerals and oxygen influence how magnetite preserves records of the Earth's magnetic field.

Uses

  • Magnetite is an important ore of iron.
  • Lodestone, a naturally magnetized form of magnetite, played an important role in the study of magnetism and was used as an early form of magnetic compass.
  • Magnetite typically carries the dominant magnetic signature in rocks, and so it has been a critical tool in paleomagnetism, a science important in discovering and understanding plate tectonics.
  • Igneous rocks commonly contain grains of two solid solutions: one between magnetite and ulvospinel, the other between ilmenite and hematite. A range of oxidizing conditions are found in magmas, and compositions of the mineral pairs are used to calculate how oxidizing the magma was and the possible evolution of the magma by fractional crystallization.

See also

Notes

  1. Ferrous Nonsnotus Retrieved September 12, 2007.

References
ISBN links support NWE through referral fees

  • Chang', Shih-Bin Robin, and Joseph Lynn Kirschvink. Magnetofossils, the Magnetization of Sediments, and the Evolution of Magnetite Biomineralization Ann. Rev. Earth Planet. Sci. 17:169-95, 1989. Retrieved September 12, 2007.
  • Farndon, John. The Practical Encyclopedia of Rocks & Minerals: How to Find, Identify, Collect and Maintain the World's best Specimens, with over 1000 Photographs and Artworks. London: Lorenz Books, 2006. ISBN 0754815412
  • Klein, Cornelis, and Barbara Dutrow. Manual of Mineral Science. 23rd ed. New York: John Wiley, 2007. ISBN 978-0471721574
  • Lowenstam, Heinz A., and Stephen Weiner. On Biomineralization. New York: Oxford University Press, 2003. ISBN 0195049772
  • Pellant, Chris. Rocks and Minerals. Smithsonian Handbooks. New York: Dorling Kindersley, 2002. ISBN 0789491060
  • Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman. Rocks, Gems and Minerals. Rev. ed. New York: St. Martin's Press, 2001. ISBN 1582381321
  • Mindat.org. Magnetite Mindat.org, 2007. Retrieved September 12, 2007.
  • Mineral Gallery. The Mineral Magnetite Amethyst Galleries, 2006. Retrieved September 12, 2007.

External links

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