Not to be confused with anhydride.

Anhydrite, Chihuahua, Mexico
Category Sulfate mineral
(repeating unit)
Anhydrous calcium sulfate:CaSO4
Strunz classification 7.AD.30
Dana classification
Crystal system Orthorhombic
Crystal class Dipyramidal (mmm)
H–M symbol: (2/m 2/m 2/m)
Space group Amma
Unit cell a = 6.245(1) Å, b = 6.995(2) Å
c = 6.993(2) Å; Z = 4
Color Colorless to pale blue or violet if transparent; white, mauve, rose, pale brown or gray from included impurities
Crystal habit Rare tabular and prismatic crystals. Usually occurs as fibrous, parallel veins that break off into cleavage fragments. Also occurs as grainy, massive, or nodular masses
Twinning Simple or repeatedly on {011} common; contact twins rare on {120}
Cleavage [010] perfect
[100] perfect
[001] good, resulting in pseudocubic fragments
Fracture Conchoidal
Tenacity Brittle
Mohs scale hardness 3.5
Luster Pearly on {010}
vitreous to greasy on {001}
vitreous on {100}
Streak White
Diaphaneity Transparent to translucent
Specific gravity 2.97
Optical properties Biaxial (+)
Refractive index nα = 1.567–1.574
nβ = 1.574–1.579
nγ = 1.609–1.618
Birefringence δ = 0.042–0.044
Pleochroism For violet varieties
X = colorless to pale yellow or rose
Y = pale violet or rose
Z = violet.
2V angle 56–84°
Fusibility 2
Other characteristics Some specimens fluoresce; many more fluoresce after heating
References [1][2][3][4]

Anhydrite is a mineral—anhydrous calcium sulfate, CaSO4. It is in the orthorhombic crystal system, with three directions of perfect cleavage parallel to the three planes of symmetry. It is not isomorphous with the orthorhombic barium (baryte) and strontium (celestine) sulfates, as might be expected from the chemical formulas. Distinctly developed crystals are somewhat rare, the mineral usually presenting the form of cleavage masses. The Mohs hardness is 3.5 and the specific gravity is 2.9. The color is white, sometimes greyish, bluish, or purple. On the best developed of the three cleavages, the lustre is pearly; on other surfaces it is glassy. When exposed to water, anhydrite readily transforms to the more commonly occurring gypsum, (CaSO4·2H2O) by the absorption of water. This transformation is reversible, with gypsum or calcium sulfate hemihydrate forming anhydrite by heating to around 200 °C (400 °F) under normal atmospheric conditions.[5] Anhydrite is commonly associated with calcite, halite, and sulfides such as galena, chalcopyrite, molybdenite, and pyrite in vein deposits.


Crystal structure of anhydrite

Anhydrite is most frequently found in evaporite deposits with gypsum; it was, for instance, first discovered, in 1794, in a salt mine near Hall in Tirol. In this occurrence, depth is critical since nearer the surface anhydrite has been altered to gypsum by absorption of circulating ground water.

From an aqueous solution calcium sulfate is deposited as crystals of gypsum, but when the solution contains an excess of sodium or potassium chloride, anhydrite is deposited if the temperature is above 40 °C (104 °F). This is one of the several methods by which the mineral has been prepared artificially, and is identical with its mode of origin in nature. The mineral is common in salt basins.

Tidal flat nodules

Anhydrite occurs in a tidal flat environment in the Persian Gulf sabkhas as massive diagenetic replacement nodules. Cross sections of these nodular masses have a netted appearance and have been referred to as chicken-wire anhydrite. Nodular anhydrite occurs as replacement of gypsum in a variety of sedimentary depositional environments.[6]

Salt dome cap rocks

Massive amounts of anhydrite occur when salt domes form a caprock. Anhydrite is 1–3% of the salt in salt domes and is generally left as a cap at the top of the salt when the halite is removed by pore waters. The typical cap rock is a salt, topped by a layer of anhydrite, topped by patches of gypsum, topped by a layer of calcite.[7] Interaction with oil can reduce SO4 creating calcite, water, and hydrogen sulfide (H2S).[8]

Igneous rocks

Anhydrite has been found in some igneous rocks, for example in the intrusive dioritic pluton of El Teniente, Chile and in trachyandesite pumice erupted by El Chichón volcano, Mexico.[9]

Naming history

The name anhydrite was given by A. G. Werner in 1804, because of the absence of water of crystallization, as contrasted with the presence of water in gypsum. Some obsolete names for the species are muriacite and karstenite; the former, an earlier name, being given under the impression that the substance was a chloride (muriate). A peculiar variety occurring as contorted concretionary masses is known as tripe-stone, and a scaly granular variety, from Volpino, near Bergamo, in Lombardy, as vulpinite; the latter is cut and polished for ornamental purposes.

Other uses

Relief carving of an anhydrite kiln, made from a piece of anhydrite, by Ophelia Gordon Bell

The Catalyst Science Discovery Centre, Widnes, has a relief carving of an anhydrite kiln, made from a piece of anhydrite, for the United Sulphuric Acid Corporation.


  1. Klein, Cornelis; Hurlbut, Cornelius S. (1985). Manual of Mineralogy (20th ed.). New York: John Wiley and Sons. ISBN 0-471-80580-7.
  2. "Anhydrite". Webmineral.
  3. "Anhydrite".
  4. "Anhydrite" (PDF). Handbook of Mineralogy.
  5. Deer; Howie; Zussman (1992). An Introduction to the Rock=Forming Minerals (2nd ed.). England: Pearson Education. p. 614. ISBN 0-582-30094-0.
  6. Michael A., Church (2003). Encyclopedia of Sediments & Sedimentary Rocks. Springer. p. 17–18. ISBN 978-1-4020-0872-6.
  7. Walker, C. W. (Dec 1976). "Origin of Gulf Coast salt-dome cap rock". AAPG Bulletin. 60 (12): 2162–2166. doi:10.1306/c1ea3aa0-16c9-11d7-8645000102c1865d.
  8. Saunders, James A.; Thomas, Robert C. (September 1996). "Origin of 'exotic' minerals in Mississippi salt dome cap rocks: results of reaction-path modeling". Applied Geochemistry. 11 (5): 667–676. doi:10.1016/S0883-2927(96)00032-7.
  9. Luhr, James F. (2008). "Primary igneous anhydrite: Progress since its recognition in the 1982 El Chichón trachyandesite". Journal of Volcanology and Geothermal Research. 175: 394–407. doi:10.1016/j.jvolgeores.2008.02.016.

Further reading

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