Rock Identifier
Polished green-gray stone, possibly serpentine (Likely serpentine-group rock, composed mainly of serpentine minerals; identification is uncertain from the photo) — metamorphic
metamorphic

Polished green-gray stone, possibly serpentine

Likely serpentine-group rock, composed mainly of serpentine minerals; identification is uncertain from the photo

AI-generated identification · may be incorrect

Opaque, mottled green-gray with a polished, waxy-to-greasy luster. Serpentine has Mohs hardness about 2.5–5.5 and commonly forms massive material without visible crystals; hardness and composition cannot be confirmed visually.

Identified More metamorphic →
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Physical properties

Opaque, mottled green-gray with a polished, waxy-to-greasy luster. Serpentine has Mohs hardness about 2.5–5.5 and commonly forms massive material without visible crystals; hardness and composition cannot be confirmed visually.

Formation & geological history

Serpentine forms when magnesium-rich ultramafic rocks are altered by water, commonly during metamorphism at or near tectonic plate boundaries. Such rocks range widely in age.

Uses & applications

Polished serpentine is used for carvings, beads, ornaments, and decorative stone; softer material is generally unsuitable for demanding construction uses.

Geological facts

The smooth oval shape indicates the specimen has been shaped and polished; appearance alone cannot reliably distinguish serpentine from other green stones such as jade or aventurine.

Field identification & locations

Look for mottled green color, relatively low hardness, and a waxy feel; a scratch test or mineralogical testing would help confirm identity. Serpentinite occurs in many mountain belts worldwide.