Bauxite

Rock made of gibbsite, boehmite, diaspore

Common · Al(OH)₃ and AlO(OH), with iron oxides and kaolinite

A sedimentary rock of deep weathering, dull reddish brown, white or tan, made of the aluminium minerals gibbsite, boehmite and diaspore with iron oxides and kaolinite. Named after Les Baux in Provence, where Pierre Berthier found it in 1821; it forms as laterite over granite, basalt and shale in the tropics, or as karst bauxite over limestone. The world's main source of aluminium, a metal of the industrial age: it is refined to alumina by the Bayer process, then reduced by electrolysis in molten cryolite. Strip mined near the surface; Guinea, Australia and China lead today.

Rock

Kind of rock
Chemical sedimentary rock
Also contains
Goethite, Hematite, Kaolinite
Deposits
Lateritic deposit
Metals
Aluminum
How it forms
Deep tropical weathering (laterite) over granite, basalt and shale, or karst bauxite over limestone.
Uses
The main ore of aluminium, refined by the Bayer process.

Identity

Formula
Al(OH)₃ and AlO(OH), with iron oxides and kaolinite
Chemical class
Oxide
Also known as
Aluminium ore
Ore of
Aluminum

Crystallography

Crystal system
Amorphous
Habits
Earthy, Nodular, Massive
Fracture
Uneven

Physical properties

Mohs hardness
2
Density
2.5 g/cm³
Luster
Dull, Earthy
Colors
reddish brown, white, brown, pale yellow
Transparency
Opaque

Geology

Origins
Sedimentary
Host rocks
Volcanic rock, Limestone and chalk
Associated minerals
Gibbsite, Boehmite, Diaspore, Goethite, Hematite, Ilmenite
Geography
Guinea, Australia, China, France (Les Baux, Provence), Jamaica, Suriname, Guyana

Classification

Rarity
Common
Gem quality
No

Sources

Browse the Crystal Encyclopedia — MGS Toolbox