Name:
Gypsum
Origin of name:
from the Greek, gypsos, meaning chalk
Chemical composition:
CaSO4.2H2O
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
Hardness:
2
Cleavage:
perfect
Colour:
commonly colourless, white, grey or brownish
Specific gravity:
2.32

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