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Bauxite is an aluminium ore. It consists largely of the Al minerals gibbsite Al(OH)₃, boehmite and diaspore AlOOH, together with the iron oxides goethite and hematite, the clay mineral kaolinite and small amounts of anatase TiO₂. It was named after the village Les Baux-de-Provence in southern France, where it was first discovered in 1821 by geologist Pierre Berthier.

Contents 1 Formation 2 World bauxite mine production, reserves, and reserve base 3 Processing 4 References 5 See also 6 External links

In geosciences lateritic bauxites (silicate bauxites) are distinguished from karst bauxites (carbonate bauxites). The early discovered carbonate bauxites occur predominantly in Europe and Jamaica above carbonate rocks (limestone and dolomite), where they were formed by lateritic weathering either of intercalated clays or of clayey dissolution residues of the limestone.

The lateritic bauxites occur in many countries of the tropical belt. They were formed by lateritization (see laterite) of various silicate rocks such as granites, gneisses, basalts, syenite, clays and shales. Compared with Fe-rich laterites the formation of bauxites demands even stronger weathering conditions with a very good drainage. This enables dissolution of kaolinite and precipitation of gibbsite. Zones with highest Al contents are frequently located below a feruginous surface layer. The aluminium hydroxide in the lateritic bauxite deposits is almost exclusively gibbsite.

(x1000 tonne, Numbers for 2001 estimated)

Country	Mine production		Reserves	Reserve base
	2000	2001
Australia	200–800	53,500	3,800,000	7,400,000
Brazil	14,000	14,000	3,900,000	4,900,000
People's Republic of China	9,000	9,200	720,000	2,000,000
Guinea	15,000	15,000	7,400,000	8,600,000
Guyana	2,400	2,000	700,000	900,000
India	7,370	8,000	770,000	1,400,000
Jamaica	11,100	13,000	2,000,000	2,500,000
Russia	4,200	4,000	200,000	250,000
Suriname	3,610	4,000	580,000	600,000
United States	NA	NA	20,000	40,000
Venezuela	4,200	4,400	320,000	350,000
Other countries	10,800	10,200	4,100,000	4,700,000
World total (rounded)	135,000	137,000	24,000,000	34,000,000

Approx. 95% of the world bauxite production is processed into aluminium. Bauxites are typically classified according to their intended commercial application: metallurgical, abrasive, cement, chemical and refractory.

Bauxites are heated in pressure vessels with sodium hydroxide solution at 150-200 °C through which aluminium is dissolved as aluminate (Bayer process). After separation of ferruginous residue (red mud) by filtering, pure gibbsite is precipitated when the liquor is cooled and seeded with fine grained aluminium hydroxide. Gibbsite is converted into aluminium oxide by heating. This is molten at approx. 1000 °C by addition of cryolite as a flux and reduced to metallic aluminium by a very energy-consumptive electrolytic process (Hall-Héroult process).

• Bardossy, G. (1882): Karst Bauxites. Bauxite deposits on carbonate rocks. Elsevier Sci. Publ. 441 p.
• Bardossy, G. and Aleva, G.J.J. (1990): Lateritic Bauxites. Developments in Economic Geology 27, Elsevier Sci. Publ. 624 p. ISBN 0-444-98811-4

• Aluminium in Africa

• USGS Minerals Information: Bauxite
• Mineral Information Institute