Rock Identifier
Olivine (Peridotite) (Magnesium Iron Silicate - (Mg, Fe)2SiO4) — igneous
igneous

Olivine (Peridotite)

Magnesium Iron Silicate - (Mg, Fe)2SiO4

Hardness: 6.5–7 on Mohs scale; Color: olive green, yellowish-green to brownish; Luster: vitreous to oily; Crystal structure: orthorhombic; Cleavage: poor; Specific gravity: 3.27–4.37.

Hardness
6
Color
olive green, yellowish-green to brownish
Luster
vitreous to oily
Identified More igneous

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 6.5–7 on Mohs scale; Color: olive green, yellowish-green to brownish; Luster: vitreous to oily; Crystal structure: orthorhombic; Cleavage: poor; Specific gravity: 3.27–4.37.

Formation & geological history

Formed in the Earth's upper mantle and brought to the surface through volcanic activity (xenoliths) or tectonic uplift (ophiolites). It is one of the first minerals to crystallize from a cooling magma melt.

Uses & applications

Used as a refractory material in steel making (due to high melting point), a slag conditioner, an abrasive (sandblasting), and high-quality specimens are cut into the gemstone 'Peridot'.

Geological facts

Olivine is a primary component of the Earth's upper mantle. It has also been discovered in meteorites (pallasites) and on the Moon and Mars.

Field identification & locations

Identify in the field by its distinct 'olive' green color and granular texture. Commonly found in basaltic rocks, ultramafic intrusions, and specific sites like the Green Sand Beach in Hawaii or various volcanic regions globally.