Rock Identifier
Tumbled green-blue stone, likely serpentine or chlorite-rich metamorphic rock (Serpentinite (mainly antigorite/lizardite; identification is image-based)) — metamorphic
metamorphic

Tumbled green-blue stone, likely serpentine or chlorite-rich metamorphic rock

Serpentinite (mainly antigorite/lizardite; identification is image-based)

AI-generated identification · may be incorrect

Typically Mohs 2.5–4, dark green to blue-green, mottled, waxy to greasy luster, and fine-grained with no visible crystal faces; specific gravity about 2.5–2.6. The rounded surface indicates tumbling or natural abrasion.

Identified More metamorphic
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Physical properties

Typically Mohs 2.5–4, dark green to blue-green, mottled, waxy to greasy luster, and fine-grained with no visible crystal faces; specific gravity about 2.5–2.6. The rounded surface indicates tumbling or natural abrasion.

Formation & geological history

Forms when ultramafic mantle rocks such as peridotite undergo hydration and metamorphism, commonly in ancient or active tectonic zones; ages vary widely. Its blue-green appearance may also reflect chlorite, magnetite, or other accessory minerals.

Uses & applications

Used as an ornamental and carving stone, tumbled-stone material, and historically in architecture; attractive pieces may be sold as decorative specimens. Avoid dust from cutting because some serpentinite can contain asbestos-form minerals.

Geological facts

Serpentinite often shows black magnetite specks and a slippery, waxy feel. It may be weakly magnetic and can be confused with nephrite, chlorite schist, or dyed material.

Field identification & locations

Common in ophiolite belts and mountain regions, including California, the Alps, New Zealand, and the Appalachians. Field confirmation requires hardness, streak, magnetism, and ideally microscopy or spectroscopy.