Rock Identifier
Olivine (Peridotite) (Olivine Group; (Mg, Fe)2SiO4) — igneous
igneous

Olivine (Peridotite)

Olivine Group; (Mg, Fe)2SiO4

Hardness: 6.5-7 (Mohs scale); Color: Olive-green, lime-green, or brownish-green; Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Specific Gravity: 3.2-4.4

Hardness
6
Color
Olive-green, lime-green, or brownish-green
Luster
Vitreous (glassy)
Identified More igneous

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Olive-green, lime-green, or brownish-green; Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Specific Gravity: 3.2-4.4

Formation & geological history

Formed in the Earth's upper mantle and brought to the surface by volcanic eruptions of basaltic lavas or within ultramafic igneous rocks like peridotite or dunite.

Uses & applications

Used as a refractory material in steel making (sand casting), as a gemstone (Peridot) for jewelry, and occasionally as an abrasive or decorative landscaping stone.

Geological facts

Olivine is one of the most common minerals in the Earth's upper mantle. It is also found in meteorites (Pallasites), which can contain beautiful, translucent olivine crystals trapped in a nickel-iron matrix.

Field identification & locations

Identify by its distinctive pistachio to olive-green color and sugary, granular texture in coarse-grained rocks. Common in volcanic regions (Hawaii) or tectonic suture zones. It lacks a clear cleavage, often showing conchoidal fracture.