Rock Identifier
Green chalcedony (likely chrysoprase or dyed chalcedony) (Microcrystalline quartz, SiO₂; chrysoprase is nickel-bearing chalcedony) — gemstone
gemstone

Green chalcedony (likely chrysoprase or dyed chalcedony)

Microcrystalline quartz, SiO₂; chrysoprase is nickel-bearing chalcedony

AI-generated identification · may be incorrect

Mohs hardness 6.5–7; translucent apple-green body, waxy to vitreous luster, cryptocrystalline structure, no visible cleavage, and conchoidal fracture. The oval cabochon is polished and may contain natural or treatment-related speckling.

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Physical properties

Mohs hardness 6.5–7; translucent apple-green body, waxy to vitreous luster, cryptocrystalline structure, no visible cleavage, and conchoidal fracture. The oval cabochon is polished and may contain natural or treatment-related speckling.

Formation & geological history

Chalcedony forms when silica-rich groundwater fills cavities and fractures, commonly in volcanic rocks; chrysoprase obtains its green color from nickel. Formation ages vary widely, while vivid commercial material commonly comes from Australia, Poland, Brazil, and Tanzania.

Uses & applications

Used for cabochons, beads, carvings, and ornamental objects; attractive saturated chrysoprase can be valuable, while dyed green chalcedony is inexpensive.

Geological facts

Chrysoprase is the best-known natural green chalcedony and was prized in ancient jewelry. Color can fade with prolonged heat or strong sunlight.

Field identification & locations

Identify it by its uniform green color, translucency, hardness, and waxy polish; quartz will scratch glass, but definitive separation from dyed chalcedony requires testing or laboratory analysis. The image alone cannot confirm natural chrysoprase versus dyed material.