Copper sulphate
Copper sulphate is the copper salt of sulphuric acid. It belongs to the sulphate group of substances.
In nature, copper sulphates are formed by the weathering and oxidation of sulphidic copper minerals (e.g. chalcopyrite or bornite) under the influence of oxygen, water and sulphuric acid, which is often released from sulphidic ores. Copper sulphates are mainly formed in dry areas as they are water-soluble and are easily washed out in humid environments.
The mineral chalcanthite is the naturally occurring form of copper sulphate pentahydrate, which forms bright blue crystals. It is formed in areas such as: Chile, Arizona (United States) and Namibia. Brochantite is a basic copper sulphate that often occurs in oxidised copper ores. It has a green to emerald green colour and is found in copper deposits worldwide.
Copper sulphate does not occur naturally in its pure, anhydrous form.