
sedimentary
Bauxite
Bauxite (Al2O3·nH2O)
Hardness: 1-3 Mohs; Color: reddish-brown, tan, or creamy white; Luster: dull to earthy; Structure: pisolitic (pea-like) or massive; Cleavage: none; Specific Gravity: 2.0-2.5
- Hardness
- 1-3 Mohs
- Color
- reddish-brown, tan, or creamy white
- Luster
- dull to earthy
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Physical properties
Hardness: 1-3 Mohs; Color: reddish-brown, tan, or creamy white; Luster: dull to earthy; Structure: pisolitic (pea-like) or massive; Cleavage: none; Specific Gravity: 2.0-2.5
Formation & geological history
Formed as a residual soil in tropical and subtropical regions through the intense chemical weathering (lateritization) of aluminum-rich silicate rocks. Most deposits are of Cenozoic or Mesozoic age.
Uses & applications
The primary ore for aluminum production. Used in the manufacture of refractory materials, abrasives, chemicals, and cement.
Geological facts
It is named after its discovery site in Les Baux, France, in 1821. It is not a single mineral but a mixture of aluminum hydroxides like gibbsite, boehmite, and diaspore.
Field identification & locations
Identify in the field by its distinctive pea-like (pisolitic) grains, reddish-brown iron staining, and relatively low density. Commonly found in Australia, Guinea, Brazil, and Jamaica.
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