
mineral
Olivine (Peridot)
Magnesium Iron Silicate (Mg,Fe)2SiO4
Hardness: 6.5–7.0 (Mohs scale); Color: Olive-green, yellow-green, or brownish; Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Specific Gravity: 3.27–4.37; Cleavage: Poor.
- Hardness
- 6
- Color
- Olive-green, yellow-green, or brownish
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 6.5–7.0 (Mohs scale); Color: Olive-green, yellow-green, or brownish; Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Specific Gravity: 3.27–4.37; Cleavage: Poor.
Formation & geological history
Formed in the Earth's mantle and brought to the surface by volcanic activity (igneous environments). It is one of the first minerals to crystallize from magma. Found in mafic and ultramafic igneous rocks like basalt, gabbro, and peridotite.
Uses & applications
Gem-quality specimens (Peridot) are used in jewelry. Industrial-grade olivine is used in metal casting (sand casting), as a refractory material for lining furnaces, and for carbon sequestration research.
Geological facts
Olivine is a primary component of the Earth's upper mantle. It has also been discovered in meteorites (Pallasites) and identified on the surface of Mars and the Moon.
Field identification & locations
Identify in the field by its distinct olive-green color, glassy luster, and granular texture (often appearing as small sugary crystals in basalt). Commonly found in volcanic regions like Hawaii, Arizona, and Norway.
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