
mineral
Green Chalcedony
Silicon Dioxide (SiO2) with trace minerals
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale; Color: Pale to deep green; Luster: Waxy to vitreous; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Pale to deep green
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on the Mohs scale; Color: Pale to deep green; Luster: Waxy to vitreous; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64.
Formation & geological history
Formed from the precipitation of silica-rich water in volcanic cavities (vugs) or sedimentary environments at relatively low temperatures over millions of years.
Uses & applications
Primarily used in jewelry (beads, cabochons), ornamental carvings, seals, and as a collector's specimen. Historically used for amulets and tools.
Geological facts
Green chalcedony is often called 'Chrysoprase' when colored by nickel or 'Prase' when colored by chlorite. It has been used since ancient Greek and Roman times as a decorative gemstone.
Field identification & locations
Identify by its waxy luster, lack of visible grain, and green translucency. Common locations include Brazil, India, Madagascar, and the USA (California/Oregon). Collectors should look for even color distribution and translucency.
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