
sedimentary
Laterite
Laterite (Iron/Aluminum-rich oxide)
Hardness: 2.0-3.5 on Mohs scale (soft when wet, hardens when dry); Color: Rusty red, brown, or yellow due to iron oxides; Luster: Dull to earthy; Structure: Pitted, porous, or vesicular texture; Specific Gravity: 2.5-3.5.
- Hardness
- 2
- Color
- Rusty red, brown, or yellow due to iron oxides
- Luster
- Dull to earthy
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Physical properties
Hardness: 2.0-3.5 on Mohs scale (soft when wet, hardens when dry); Color: Rusty red, brown, or yellow due to iron oxides; Luster: Dull to earthy; Structure: Pitted, porous, or vesicular texture; Specific Gravity: 2.5-3.5.
Formation & geological history
Formed through intense and long-lasting weathering of underlying parent rock in tropical/subtropical climates. High rainfall leaches away silica, leaving behind insoluble iron and aluminum oxides. Geological age varies from Quaternary to ancient Tertiary periods.
Uses & applications
Major source of aluminum (Bauxite is a type of laterite). Historically and currently used as a building block (masonry) in tropical regions such as India and Southeast Asia. Used in road construction and as a substrate in aquariums.
Geological facts
The word 'laterite' comes from the Latin 'later', meaning brick. Many famous ancient structures, such as Angkor Wat in Cambodia and numerous South Indian temples, were built primarily using laterite blocks.
Field identification & locations
Identified in the field by its distinct reddish-orange color, porous 'sponge-like' appearance, and the fact it can often be cut with a spade when freshly dug but becomes rock-hard after exposure to air. Commonly found in India, Brazil, Australia, and Africa.
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