Rock Identifier
Polished green jasper cabochon (likely serpentine or nephrite imitation) (Jasper: microcrystalline quartz (SiO₂); green coloration may reflect chlorite, epidote, or iron minerals) — metamorphic
metamorphic

Polished green jasper cabochon (likely serpentine or nephrite imitation)

Jasper: microcrystalline quartz (SiO₂); green coloration may reflect chlorite, epidote, or iron minerals

AI-generated identification · may be incorrect

Opaque to slightly translucent, olive-green and brown mottling, waxy to vitreous polish, no visible crystals or cleavage; hardness approximately 6.5–7 if jasper, potentially 5–6 if serpentine. The smooth oval cabochon is human-cut and polished.

Identified More metamorphic
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Physical properties

Opaque to slightly translucent, olive-green and brown mottling, waxy to vitreous polish, no visible crystals or cleavage; hardness approximately 6.5–7 if jasper, potentially 5–6 if serpentine. The smooth oval cabochon is human-cut and polished.

Formation & geological history

Jasper forms when silica-rich fluids replace or cement volcanic or sedimentary material; green varieties commonly form through alteration involving chlorite or epidote. Exact geological age and locality cannot be determined from the photograph.

Uses & applications

Used for cabochons, beads, carvings, and ornamental objects; valued mainly for attractive pattern and polish rather than rarity.

Geological facts

The specimen may be marketed as green jasper, kambaba jasper, serpentine, or nephrite depending on its actual mineralogy; visual identification alone is unreliable.

Field identification & locations

Check streak, hardness, translucency, specific gravity, and magnification; quartz-rich jasper will resist a steel scratch, whereas serpentine generally will not. Common sources include India, South Africa, Madagascar, Australia, and the western United States.