| Name: Gypsum |
Origin of name: from the Greek, gypsos, meaning chalk |
Chemical composition: CaSO4.2H2O |
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Gypsum, calcium sulphate, is the most common sulphate mineral. Most gypsum deposits have been formed by the evaporation of seas and salt lakes.
Crystals of gypsum are tabular and diamond-shaped, but massive, granular and fibrous habits are also common. Many forms have specific names: transparent tabular crystals are referred to as "selenite", radiating aggregates (such as those illustrated) are known as "daisy gypsum", fibrous gypsum is called "satin spar", whilst fine-grained aggregates are known as alabaster. When heated and crushed, gypsum is used to make "Plaster of Paris". Alabaster is used as an decorative stone; its softness allows it to be carved easily. |
Crystal system: monoclinic |
| Class: Sulphates |
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| Hardness: 2 |
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| Cleavage: perfect |
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| Colour: commonly colourless, white, grey or brownish |
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| Specific gravity: 2.32 |