Rock Identifier
Polished greenstone (likely serpentine or altered basalt) (Serpentinite, mainly serpentine-group minerals (Mg₃Si₂O₅(OH)₄); exact identification requires testing) — metamorphic
metamorphic

Polished greenstone (likely serpentine or altered basalt)

Serpentinite, mainly serpentine-group minerals (Mg₃Si₂O₅(OH)₄); exact identification requires testing

AI-generated identification · may be incorrect

Dark green to gray-green, matte to waxy luster, fine-grained and rounded with pinkish veins or patches. Mohs hardness about 2.5–5.5; cleavage generally absent, density commonly 2.5–2.7 g/cm³.

Identified More metamorphic
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Physical properties

Dark green to gray-green, matte to waxy luster, fine-grained and rounded with pinkish veins or patches. Mohs hardness about 2.5–5.5; cleavage generally absent, density commonly 2.5–2.7 g/cm³.

Formation & geological history

Likely formed by hydrothermal alteration of magnesium-rich ultramafic rock, commonly during ancient oceanic or tectonic processes; geological age cannot be determined from the image.

Uses & applications

Used as ornamental stone, carvings, cabochons, and occasionally architectural facing; attractive green varieties are collected but usually modestly priced.

Geological facts

Serpentinite can resemble jade, but it is generally softer and less dense. Pink veins may consist of carbonate minerals or iron-rich alteration products.

Field identification & locations

Look for a greasy or waxy surface, green coloration, low hardness, and pale or pink veining; a steel nail may scratch many specimens. Common in ophiolite belts and metamorphic terrains worldwide.