Rock Identifier
Polished green serpentine sphere (Serpentinite; chiefly serpentine-group minerals (antigorite, lizardite, chrysotile), commonly with magnetite) — metamorphic
metamorphic

Polished green serpentine sphere

Serpentinite; chiefly serpentine-group minerals (antigorite, lizardite, chrysotile), commonly with magnetite

AI-generated identification · may be incorrect

Typically Mohs 2.5–4, dark green to mottled pale green, waxy to greasy luster, opaque to translucent; massive and fine-grained with no visible crystal cleavage. The pictured polished sphere shows characteristic cloudy green veining.

Identified More metamorphic
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Physical properties

Typically Mohs 2.5–4, dark green to mottled pale green, waxy to greasy luster, opaque to translucent; massive and fine-grained with no visible crystal cleavage. The pictured polished sphere shows characteristic cloudy green veining.

Formation & geological history

Forms when ultramafic mantle rocks such as peridotite undergo hydrothermal alteration and hydration, commonly along tectonic plate boundaries; ages vary from Precambrian to modern. This specimen has been cut and polished.

Uses & applications

Used as ornamental stone, carvings, spheres, countertops, and decorative objects; historically used in some cultures for carving and architecture. Chrysotile-rich material should not be cut or abraded because of asbestos risk.

Geological facts

Serpentinite is named for its snake-skin-like appearance and commonly contains magnetite, giving some pieces weak magnetic response. It is softer and less durable than jade, despite occasional misleading trade names.

Field identification & locations

Identify by its mottled green color, waxy polish, low hardness, and commonly soapy feel; it can be scratched by a steel knife. Common sources include California, New Zealand, Italy, Canada, Russia, and Afghanistan.