
mineral
Green Aventurine
Silicon Dioxide (SiO2) with inclusions of Fuchsite (K(Al,Cr)2(AlSi3O10)(OH)2)
Hardness: 6.5-7 (Mohs scale); Color: Pale to dark green with a shimmering effect; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69
- Hardness
- 6
- Color
- Pale to dark green with a shimmering effect
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Pale to dark green with a shimmering effect; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69
Formation & geological history
Formed in metamorphic rocks (schist) and through hydrothermal processes. The green color is primarily caused by platy inclusions of mica (fuchsite) trapped within the quartz as it crystallizes. It is found in various geological layers spanning the Proterozoic to recent eras.
Uses & applications
Used widely in lapidary work for cabochons, beads, and tumbled stones. Also used for ornamental carvings, household decor items, and as a popular stone for metaphysical collecting.
Geological facts
Green Aventurine is best known for its 'aventurescence,' a optical phenomenon where the mica inclusions reflect light like tiny sparkles. It is often called the 'Stone of Opportunity' in folklore.
Field identification & locations
Identify by its characteristic green shimmer (aventurescence) and quartz-like hardness. Frequently found in India, Brazil, Russia, and Tanzania. Unlike jade, it has a granular texture under magnification due to the quartz grains.
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