Class : Sulphates, chromates, molybdates...
    Subclass : Hydrated sulphates
    Crystal system : Monoclinic
    Chemistry : CaSO₄ 2H₂O
    Rarity : Very common

Gypsum is the most common sulphate. It is mainly a mineral of evaporitic origin where it crystallizes by direct precipitation or by hydration of the anhydrite, it thus forms thick layers, frequently alternating with levels of marl or clays, corresponding to muddy inputs between the evaporation phases. In current evaporitic basins, the capillary rise of sulphated water in the sands allows the crystallization of large entangled lenticular crystals including grains of sand more commonly known as "desert roses". Gypsum is also common in hydrothermal sulphide deposits. It is then a secondary mineral formed by the action of sulfuric acid solutions due to the oxidation of sulphides on the host rocks ; in calcareous environment this phenomenon can take a considerable extent. Gypsum owes its name to the Latin gypsum (plaster) of which it is the main use. Gypsum crystals are common and often large, the simple form shows more or less rhombic crystals and flattened, often with a moderate elongation which can however lead to acicular crystals, with generally rounded faces, composing fibrous aggregates with live silky shine. It sometimes happens that these aggregates develop into sticks of spectacular lengths called "ram's horns" ; unlike most crystallizations, these sticks grow from their bases and not from their terminations. The large evaporitic masses, however, consist largely of very fine grains with coarser brownish horizons. Alabaster is a translucent white variety of gypsum. Colorless when pure, the gypsum is mostly white, honey yellow to brownish, yellowish-gray, sometimes slightly bluish, greenish or red (inclusions of hematite). It has a low hardness (2 on the scale of Mohs and therefore scratchable to the nail) and a perfect lamellar cleavage. Its former name of "selenite" comes from the fact that the Ancients considered that its interior whiteness varied with the Moon. Gypsum is a vital mineral in the building industry. It is indeed the raw material for the manufacture of plaster where the gypsum is heated to 75°C which partially dehydrates it and turns it into a white powder. The "hardening" of the plaster is the recrystallization caused by the hydration of a multitude of gypsum crystals. Also in the construction industry, gypsum is also a set retarder that enters 5% in the composition of cements. Plaster is also used in agriculture for the amendment of soils while alabaster is used in sculpture and stone ornamentation. The Great Pyramid of Egypt was formerly covered with alabaster plates, "recycled" in the Middle Ages in other constructions. In addition, gypsum has very occasionally been used as sulfur ore or gemstone (selenite).

France is well supplied with quality specimens. The gypsum mines of Vaucluse (Mazan especially) provide very large crystals and large transparent metric blades, slightly amber in color. But the reputation of French gypsum is mainly due to the decimetric "arrowhead" or "swallowtail" twinned crystals from Ludien of Paris Basin (gypsum quarries of Cormeilles-en-Parisis, Montmartre, Villemomble, etc...). The work of the motorway exit of the A71 at Combronde (Puy-de-Dôme), supplied in quantity of beautiful pale yellow crystals in the 2000's. The quarries of gypsum of Arignac in Ariège also produced exceptionally clear crystals as well as Carresse gypsum quarries (Pyrénées-Atlantiques), once exploited by Lafarge cement plants, which provided perfectly transparent metric blades.

Perfectly transparent gypsum blades from Brazil are commonly assembled. The matrix is reconstituted and can sometimes incorporate amethyst. We can easily identify the assembly by looking at the matrix, the reconstituted matrix is always very dark, almost black. A cleaved gypsum crystal (a blade therefore) can not be found naturally associated with other mineralization. However, it must be known that the association exists in nature, it is not very common.

Groups of gypsum crystals with exotic colors (pink, green, blue, etc ...) form naturally in brine at the exit of industrial zones. These brines are "polluted" by the industrial discharges and at the origin of these exotic colors.

Mexican white sand roses are heat treated with a torch or weed burner to make them more attractive and easier to sell. The heat dehydrates the ends of the gypsum crystals which then turn white. This is the same process as for making plaster. Desert roses become powdery and chalky on the surface and tend to crumble. Photos of Rodolphe de Mordaigle, taken at a Colorado show in 2017.