Rock Identifier
Tumbled blue-green stone, likely chrysoprase or dyed chalcedony (Cryptocrystalline quartz (SiO₂), possibly nickel-bearing chrysoprase; exact identification requires testing) — gemstone
gemstone

Tumbled blue-green stone, likely chrysoprase or dyed chalcedony

Cryptocrystalline quartz (SiO₂), possibly nickel-bearing chrysoprase; exact identification requires testing

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs, waxy to vitreous luster, opaque to translucent, blue-green color, and no visible cleavage; the smooth elongated shape indicates tumbling or carving. The unusually vivid blue-green color may indicate dyeing or another mineral such as turquoise.

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Physical properties

Hardness about 6.5–7 Mohs, waxy to vitreous luster, opaque to translucent, blue-green color, and no visible cleavage; the smooth elongated shape indicates tumbling or carving. The unusually vivid blue-green color may indicate dyeing or another mineral such as turquoise.

Formation & geological history

Chalcedony forms when silica-rich groundwater fills cavities and fractures, commonly in volcanic rocks; chrysoprase gets its green color from nickel. Formation ages vary widely, while the specimen’s present shape is human-processed.

Uses & applications

Used for cabochons, beads, carvings, and inexpensive jewelry; attractive polished pieces are collected as lapidary material.

Geological facts

Chrysoprase is a quartz variety, not a separate mineral species. Color can fade with prolonged heat or strong sunlight, and dyed chalcedony commonly has unnaturally intense, uniform color.

Field identification & locations

Look for a smooth waxy surface, conchoidal fracture, and quartz-like hardness; it should scratch glass but not be scratched by a steel blade. Common sources include Australia, Brazil, Madagascar, and Central Asia; laboratory testing is needed to distinguish chrysoprase, turquoise, and dyed material.