Rock Identifier
Tumbled pale-green stone, likely serpentine or aventurine (Most likely serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or green aventurine quartz (SiO₂); identification is uncertain from the photograph alone.) — mineral
mineral

Tumbled pale-green stone, likely serpentine or aventurine

Most likely serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or green aventurine quartz (SiO₂); identification is uncertain from the photograph alone.

AI-generated identification · may be incorrect

Smoothly tumbled, pale sage-green, translucent to opaque, with a waxy-to-dull luster and a small rusty inclusion. Serpentine is Mohs 2.5–4; aventurine quartz is Mohs 7; neither cleavage nor crystal form is visible.

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Physical properties

Smoothly tumbled, pale sage-green, translucent to opaque, with a waxy-to-dull luster and a small rusty inclusion. Serpentine is Mohs 2.5–4; aventurine quartz is Mohs 7; neither cleavage nor crystal form is visible.

Formation & geological history

Serpentine forms when ultramafic rocks hydrothermally alter, commonly during oceanic-plate or mountain-building processes; aventurine forms in silica-rich veins. Geological ages vary widely.

Uses & applications

Used as a decorative tumbled stone, carving material, and ornamental aggregate; aventurine is also used in low-cost jewelry.

Geological facts

The color may come from iron-bearing serpentine minerals or fuchsite mica in aventurine. A hardness test and specific-gravity measurement are needed for confident identification.

Field identification & locations

Common sources include California, New Zealand, Italy, Russia, India, and Brazil. Test inconspicuous areas: quartz scratches glass, whereas serpentine usually does not; avoid relying on color alone.