Rock Identifier
Tumbled pale-green stone, likely serpentine or green aventurine (Probably serpentine-group minerals, chiefly lizardite/antigorite; exact identification requires testing) — mineral
mineral

Tumbled pale-green stone, likely serpentine or green aventurine

Probably serpentine-group minerals, chiefly lizardite/antigorite; exact identification requires testing

AI-generated identification · may be incorrect

Opaque to faintly translucent, pale green, smooth and matte-to-waxy with weak banding; serpentine hardness is about 2.5–4 Mohs, while quartz-rich aventurine is about 7. No visible crystals or cleavage; specific gravity roughly 2.5–2.7.

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Physical properties

Opaque to faintly translucent, pale green, smooth and matte-to-waxy with weak banding; serpentine hardness is about 2.5–4 Mohs, while quartz-rich aventurine is about 7. No visible crystals or cleavage; specific gravity roughly 2.5–2.7.

Formation & geological history

Serpentine forms when ultramafic mantle rocks hydrothermally alter, commonly during tectonic processes; deposits range from Precambrian to modern geologic settings. Its rounded shape indicates human tumbling or natural abrasion.

Uses & applications

Used as an ornamental stone, carving material, lapidary cabochons, and inexpensive decorative specimens; some varieties are marketed as “new jade.”

Geological facts

The image alone cannot reliably distinguish serpentine from pale green aventurine, jade, chalcedony, or dyed stone. True jade is considerably tougher and typically denser.

Field identification & locations

Common in serpentinite belts worldwide, including California, Italy, New Zealand, China, and Canada. Check hardness, density, streak, and magnification; avoid acid or heat tests without care.