
Mineral
Olivine (Peridot when gem-quality)
Magnesium Iron Silicate, (Mg,Fe)2SiO4
Hardness: 6.5–7 on Mohs scale; Color: typically olive-green, yellowish-green, or brownish; Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Cleavage: Poor; Specific Gravity: 3.27–4.37.
- Hardness
- 6
- Color
- typically olive-green, yellowish-green, or brownish
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: typically olive-green, yellowish-green, or brownish; Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Cleavage: Poor; Specific Gravity: 3.27–4.37.
Formation & geological history
Formed in mafic and ultramafic igneous rocks as a primary mineral. It is a major component of the Earth's upper mantle and is often found in basalt, gabbro, and peridotite. It can be found in volcanic deposits or as nodules brought to the surface by lavas.
Uses & applications
Gem-quality specimens (Peridot) are used in jewelry. Industrial uses include refractory sand for casting iron, abrasive tasks, and as a flux in steel production. It is also used to sequester CO2 in certain experimental environmental processes.
Geological facts
Olivine is one of the most common minerals on Earth by volume (comprising much of the mantle), but it weathers quickly at the surface. It is also found in meteorites (pallasites) and has been identified on the Moon and Mars.
Field identification & locations
Identify in the field by its distinctive 'olive' green color, glassy luster, and granular appearance (often described as looking like sugar or salt crystals when viewed in basalt). Commonly found in volcanic regions like Hawaii, Arizona, and Norway.
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