Rock Identifier
Likely serpentine-rich greenstone (Serpentinite/serpentinized ultramafic rock; chiefly serpentine-group minerals (Mg₃Si₂O₅(OH)₄), possibly with chlorite, talc, magnetite, or epidote) — metamorphic
metamorphic

Likely serpentine-rich greenstone

Serpentinite/serpentinized ultramafic rock; chiefly serpentine-group minerals (Mg₃Si₂O₅(OH)₄), possibly with chlorite, talc, magnetite, or epidote

AI-generated identification · may be incorrect

Dark to vivid green, fine-grained and waxy to greasy luster, with mottled veining; typically Mohs 2.5–4, non-cleaving to weakly foliated, and relatively dense (about 2.5–2.7). The image is strongly backlit, so exact texture and mineral identification are limited.

Identified More metamorphic
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Physical properties

Dark to vivid green, fine-grained and waxy to greasy luster, with mottled veining; typically Mohs 2.5–4, non-cleaving to weakly foliated, and relatively dense (about 2.5–2.7). The image is strongly backlit, so exact texture and mineral identification are limited.

Formation & geological history

Forms when olivine- and pyroxene-rich mantle rocks hydrate during metamorphism, commonly along faults and ophiolite belts. The specimen’s age cannot be determined from the photograph.

Uses & applications

Used decoratively as ‘serpentine marble,’ for carvings, tiles, and ornamental stone; attractive pieces are collected. Avoid cutting or grinding unknown material because some serpentinite can contain asbestos-form minerals.

Geological facts

The intense green color commonly reflects serpentine minerals, while black specks may be magnetite. Serpentinite is not itself an igneous rock, although its protolith was usually peridotite or pyroxenite.

Field identification & locations

Green, soft, waxy-looking rock that may scratch with a steel knife and often leaves a pale streak; commonly occurs in ophiolites and tectonic mélanges. Around central Afghanistan, serpentinite and other metamorphic rocks are geologically plausible, but this identification remains image-limited.