
mineral
Olivine (Peridot)
Magnesium Iron Silicate (Mg,Fe)2SiO4
Hardness: 6.5–7.0 on the Mohs scale; Color: Olive-green, yellow-green, or brownish-green; Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Cleavage: Poor; Specific gravity: 3.27–4.37.
- Hardness
- 6
- Color
- Olive-green, yellow-green, or brownish-green
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 6.5–7.0 on the Mohs scale; Color: Olive-green, yellow-green, or brownish-green; Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Cleavage: Poor; Specific gravity: 3.27–4.37.
Formation & geological history
Formed in the Earth's mantle and brought to the surface by tectonic or volcanic activity. It is a primary mineral in mafic and ultramafic igneous rocks like basalt and peridotite. Can also be found in pallasite meteorites.
Uses & applications
Used as a gemstone (Peridot) in jewelry. Industrially used as a flux for steel production, a refractory material for casting molds, and for sandblasting. It is also being studied for its ability to sequester carbon dioxide.
Geological facts
Olivine is one of the most common minerals in the Earth's upper mantle and has been found on the Moon and Mars. It is also known as the 'Evening Emerald' because its green glow remains visible under artificial light.
Field identification & locations
Identify in the field by its distinct olive-green color, glassy luster, and granular texture (often appearing as small 'sugary' aggregates in basalt rocks). Commonly found in volcanic regions such as Hawaii, Arizona, and Norway.
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