Rock Identifier
Polished serpentine-rich rock (probable serpentinite) (Serpentinite; primarily serpentine-group minerals, Mg₃Si₂O₅(OH)₄, with possible calcite, magnetite, and altered host minerals) — metamorphic
metamorphic

Polished serpentine-rich rock (probable serpentinite)

Serpentinite; primarily serpentine-group minerals, Mg₃Si₂O₅(OH)₄, with possible calcite, magnetite, and altered host minerals

AI-generated identification · may be incorrect

Typically green to yellow-green, mottled, waxy to greasy luster, and opaque; Mohs hardness about 2.5–4, with poor cleavage and massive texture. The specimen appears polished or naturally smoothed, with pale mineral veins and weathered brown margins.

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Physical properties

Typically green to yellow-green, mottled, waxy to greasy luster, and opaque; Mohs hardness about 2.5–4, with poor cleavage and massive texture. The specimen appears polished or naturally smoothed, with pale mineral veins and weathered brown margins.

Formation & geological history

Forms when ultramafic mantle rocks such as peridotite undergo hydrothermal metamorphism and hydration, commonly along faults and tectonic plate boundaries. Serpentinization ranges from ancient Precambrian terrains to active modern oceanic settings.

Uses & applications

Used as an ornamental and carving stone, countertop or tile material, and lapidary rough; softer pieces are mainly collected rather than used for jewelry.

Geological facts

Serpentinite can contain magnetite and may be weakly magnetic. Some varieties are associated with chrysotile asbestos, so avoid cutting, drilling, or generating dust unless its composition is confirmed and proper precautions are used.

Field identification & locations

Identify by its mottled green color, waxy feel, low hardness, veining, and inability to scratch glass; a steel knife may scratch it. Common localities include California, Italy, New Zealand, Canada, and Oman.