Rock Identifier
Tumbled green stone, possibly serpentine or prehnite (Provisional identification: serpentine-group mineral, commonly antigorite; alternatively prehnite or green calcite) — mineral
mineral

Tumbled green stone, possibly serpentine or prehnite

Provisional identification: serpentine-group mineral, commonly antigorite; alternatively prehnite or green calcite

AI-generated identification · may be incorrect

Pale green, opaque to translucent, rounded and polished with a dull-to-waxy luster; likely Mohs 2.5–6 depending on species. The blurred image does not resolve cleavage, crystal structure, or specific gravity.

Identified More mineral
Explore Tumbled green stone, possibly serpentine or prehnite in the encyclopedia →

Identify your own rocks.

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

Physical properties

Pale green, opaque to translucent, rounded and polished with a dull-to-waxy luster; likely Mohs 2.5–6 depending on species. The blurred image does not resolve cleavage, crystal structure, or specific gravity.

Formation & geological history

Serpentine forms when ultramafic rocks undergo hydration and alteration, commonly in convergent-plate settings; prehnite forms in low-temperature hydrothermal veins and cavities. Geological ages vary widely.

Uses & applications

Tumbled pieces are sold as decorative specimens, craft stones, and metaphysical items; serpentine may also be carved or used decoratively, while prehnite is occasionally used in jewelry.

Geological facts

Identification is uncertain because the specimen is small, rounded, and out of focus; color alone cannot reliably distinguish green minerals.

Field identification & locations

Check streak, hardness, translucency, specific gravity, and reaction to dilute acid; serpentine is typically waxy and softer, whereas prehnite is harder and often translucent with a pearly sheen. Common sources include California, Italy, New Zealand, South Africa, and Australia.