Rock Identifier
Tumbled blue-green stone, likely serpentine or green jasper (Probable serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or microcrystalline quartz (SiO₂); exact identification requires testing) — mineral
mineral

Tumbled blue-green stone, likely serpentine or green jasper

Probable serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or microcrystalline quartz (SiO₂); exact identification requires testing

AI-generated identification · may be incorrect

Dark blue-green, opaque to slightly translucent, polished vitreous-to-waxy luster with mottled yellow-green areas; likely hardness 3–7 Mohs depending on composition, with no visible cleavage. Rounded shape indicates tumbling and polishing.

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Physical properties

Dark blue-green, opaque to slightly translucent, polished vitreous-to-waxy luster with mottled yellow-green areas; likely hardness 3–7 Mohs depending on composition, with no visible cleavage. Rounded shape indicates tumbling and polishing.

Formation & geological history

Serpentine forms when ultramafic rocks such as peridotite are hydrothermally altered; jasper forms from silica-rich fluids replacing or cementing sediment. These materials commonly formed during ancient tectonic and hydrothermal events.

Uses & applications

Used as a decorative tumbled stone, cabochon, ornamental object, and sometimes carving material; serpentine is also used for architectural stone, while jasper is popular in jewelry.

Geological facts

The image alone cannot reliably distinguish serpentine from jasper, nephrite, or dyed agate. A hardness test, streak, specific gravity, and magnified examination would improve identification.

Field identification & locations

Common sources include California, New Zealand, Afghanistan, Russia, Brazil, and India. Serpentine is generally softer and waxier; jasper is harder and scratches glass, while a steel nail may scratch serpentine.