
mineral
Olivine (Peridot)
Magnesium Iron Silicate (Mg, Fe)2SiO4
Hardness: 6.5–7 (Mohs scale); Color: Olive-green, yellow-green; Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Cleavage: Poor; Specific gravity: 3.27–4.37.
- Hardness
- 6
- Color
- Olive-green, yellow-green
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Olive-green, yellow-green; Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Cleavage: Poor; Specific gravity: 3.27–4.37.
Formation & geological history
Formed in mafic and ultramafic igneous rocks (basalt, gabbro, peridotite). It is one of the first minerals to crystallize from cooling magma and can be found in the mantle. Specimens are often billions of years old.
Uses & applications
Gem-quality crystals (Peridot) are used in jewelry. Industrial-grade olivine is used in metal casting (foundry sand), as refractory sand, and in the steel industry to remove impurities.
Geological facts
Olivine has been discovered on the moon, Mars, and in pallasite meteorites from outer space. It is the primary component of the Earth's upper mantle.
Field identification & locations
Identify by its distinctive pistachio to olive green color and brittle, granular habit. Commonly found in volcanic areas like Hawaii, Arizona, or regions with exposed tectonic plates like Norway.
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