
mineral
Green Aventurine
SiO2 (Silicon Dioxide with inclusions of Fuchsite mica)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Pale to translucent green, Luster: Vitreous to waxy, Crystal Structure: Trigonal/Hexagonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.64-2.69
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Pale to translucent green, Luster: Vitreous to waxy, Crystal Structure: Trigonal/Hexagonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.64-2.69
Formation & geological history
Formed in metamorphic environments where quartz-rich rocks undergo recrystallization; the green color comes from chromium-rich mica (fuchsite) trapped within the quartz matrix. Most deposits are millions of years old.
Uses & applications
Extensively used in lapidary work for carvings, figurines, cabochons for jewelry, and as a popular pocket stone for crystal collectors. Highly valued in decorative interior design.
Geological facts
Known as the 'Stone of Opportunity,' it is a variety of quartz characterized by its translucency and the presence of platy mineral inclusions that give a shimmering or glistening effect termed 'aventurescence'.
Field identification & locations
Identified by its distinctive shimmering green surface and conchoidal fracture. Commonly found in India, Brazil, and Russia. Collectors should look for the subtle 'sparkle' inside the stone that distinguishes it from green glass.
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