Rock Identifier
Peridotite (Ultramafic intrusive igneous rock) — igneous
igneous

Peridotite

Ultramafic intrusive igneous rock

AI-generated identification · may be incorrect

Hardness of 6-7 on the Mohs scale, typically dark green to greenish-brown in color, with a vitreous to dull luster. It has a dense, coarse-grainedphaneritic texture primarily composed of olivine and pyroxene.

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Physical properties

Hardness of 6-7 on the Mohs scale, typically dark green to greenish-brown in color, with a vitreous to dull luster. It has a dense, coarse-grainedphaneritic texture primarily composed of olivine and pyroxene.

Formation & geological history

Forms from the slow cooling and crystallization of ultramafic magma deep within the Earth's mantle, dating from various geological eras.

Uses & applications

Used primarily as a source rock for diamonds, and occasionally as a decorative architectural stone or for extracting magnesium.

Geological facts

Peridotite is the dominant rock type of the Earth's upper mantle. When altered by hydrothermal fluids, it transforms into serpentine.

Field identification & locations

Identify in the field by its heavy density, dark greenish color, and high proportion of green olivine crystals. Commonly found in ophiolite complexes and fault zones.