Halite

For the market widely known as "Halite", see Central Sofia Market Hall.

Halite
Halite from the Wieliczka salt mine, Małopolskie, Poland
General
Category	Halide mineral
Formula (repeating unit)	NaCl
Strunz classification	03.AA.20
Crystal symmetry	Isometric hexoctahedral 4/m 3 2/m
Unit cell	a = 5.6404(1) Å; Z = 4
Identification
Formula mass	58.433 g/mol
Color	Colorless or white; also blue, purple, red, pink, yellow, orange, or gray
Crystal habit	Predominantly cubes and in massive sedimentary beds, but also granular, fibrous and compact
Crystal system	Cubic
Cleavage	Perfect {001}, three directions cubic
Fracture	Conchoidal
Tenacity	Brittle
Mohs scale hardness	2.0 - 2.5
Luster	Vitreous
Streak	White
Diaphaneity	Transparent
Specific gravity	2.17
Optical properties	Isotropic
Refractive index	n = 1.544
Solubility	Water-soluble
Other characteristics	Salty flavor, Fluorescent
References

Halite /ˈhælaɪt/, commonly known as rock salt, is a type of salt, the mineral form of sodium chloride (NaCl). Halite forms isometric crystals. The mineral is typically colorless or white, but may also be light blue, dark blue, purple, pink, red, orange, yellow or gray depending on the amount and type of impurities. It commonly occurs with other evaporite deposit minerals such as several of the sulfates, halides, and borates.

Occurrence

Halite cubes from the Stassfurt Potash deposit, Saxony-Anhalt, Germany (size: 6.7 × 1.9 × 1.7 cm)

Halite occurs in vast beds of sedimentary evaporite minerals that result from the drying up of enclosed lakes, playas, and seas. Salt beds may be hundreds of meters thick and underlie broad areas. In the United States and Canada extensive underground beds extend from the Appalachian basin of western New York through parts of Ontario and under much of the Michigan Basin. Other deposits are in Ohio, Kansas, New Mexico, Nova Scotia and Saskatchewan. The Khewra salt mine is a massive deposit of halite near Islamabad, Pakistan. In the United Kingdom there are three mines; the largest of these is at Winsford in Cheshire producing on average a million tonnes per year.

Salt domes are vertical diapirs or pipe-like masses of salt that have been essentially "squeezed up" from underlying salt beds by mobilization due to the weight of overlying rock. Salt domes contain anhydrite, gypsum, and native sulfur, in addition to halite and sylvite. They are common along the Gulf coasts of Texas and Louisiana and are often associated with petroleum deposits. Germany, Spain, the Netherlands, Romania and Iran also have salt domes. Salt glaciers exist in arid Iran where the salt has broken through the surface at high elevation and flows downhill. In all of these cases, halite is said to be behaving in the manner of a rheid.

Unusual, purple, fibrous vein filling halite is found in France and a few other localities. Halite crystals termed hopper crystals appear to be "skeletons" of the typical cubes, with the edges present and stairstep depressions on, or rather in, each crystal face. In a rapidly crystallizing environment, the edges of the cubes simply grow faster than the centers. Halite crystals form very quickly in some rapidly evaporating lakes resulting in modern artifacts with a coating or encrustation of halite crystals. Halite flowers are rare stalactites of curling fibers of halite that are found in certain arid caves of Australia's Nullarbor Plain. Halite stalactites and encrustations are also reported in the Quincy native copper mine of Hancock, Michigan.

Uses

Halite is often used both residentially and municipally for managing ice. Because brine (a solution of water and salt) has a lower freezing point than pure water, putting salt or saltwater on ice that is near 0 °C (32 °F) will cause it to melt. (This effect is called freezing-point depression.) It is common for homeowners in cold climates to spread salt on their sidewalks and driveways after a snow storm to melt the ice. It is not necessary to use so much salt that the ice is completely melted; rather, a small amount of salt will weaken the ice so that it can be easily removed by other means. Also, many cities will spread a mixture of sand and salt on roads during and after a snowstorm to improve traction. In addition to de-icing, rock salt is occasionally used in agriculture. An example of this would be inducing salt stress to suppress the growth of annual meadow grass in turf production.

Salt is also used extensively in cooking as a flavor enhancer and to cure a wide variety of foods such as bacon and fish. Larger pieces can be ground in a salt mill or dusted over food from a shaker as finishing salt.

Some cultures, especially in Africa, prefer a wide variety of different rock salts for different dishes. Pure salt is avoided for particular colors of salt indicating the presence of different impurities. Many recipes call for a particular kinds of rock salt, and imported pure salt often has impurities added to adapt to local tastes.

Gallery

• SaltCrystalCasts.JPG

  Hopper crystal cast of halite in a Jurassic rock, Carmel Formation, Utah

• 

  Unusual halite crystals from Faiyum, Egypt

• 

  Large natural crystal of halite, showing cubic cleavage breaks

• 

  Halite from Potash Corporation of Saskatchewan Mine in Rocanville, Saskatchewan, Canada

• 

  Devil's Golf Course in Death Valley, California. Halite formed by the evaporation of ancient Lake Manly.

• 

  Halite from a potash mine in New Mexico. The orange and blue coloration is caused by radiation from potassium-40 in nearby potash minerals.

• 

  Large crystals of halite that have been rounded into pebbles on the Dead Sea coast.

See also

• Salt
• Salt tectonics

References

• Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., John Wiley and Sons, New York ISBN 0-471-80580-7
• Anthony, John W; Bideaux, R.A.; Bladh, K.W.; Nicois, M.C., 1997, Handbook of Mineralogy: Halides, Hydroxides, Oxides, Mineral Data Publishing, Tucson ISBN 0-9622097-2-4
• Minerals.net
• Material Safety Data Sheet
• Desert USA
• Halite stalactites