
mineral
Green Aventurine
Silicon Dioxide (Quartz variety) with Fuchsite inclusions (SiO2 + K(Al,Cr)2(AlSi3O10)(OH)2)
Hardness: 6.5-7 on Mohs scale; Color: Green (from Fuchsite mica); Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None; Specific Gravity: 2.64-2.69; Presence of 'aventurescence' (shimmer).
- Hardness
- 6
- Color
- Green (from Fuchsite mica)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Green (from Fuchsite mica); Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None; Specific Gravity: 2.64-2.69; Presence of 'aventurescence' (shimmer).
Formation & geological history
Formed in metamorphic rocks (phyllites and schists) and occasionally in igneous rocks. The shimmering effect is caused by platy inclusions of mica (Fuchsite) aligning during geological pressure and cooling.
Uses & applications
Commonly used for lapidary work, jewelry (beads, cabochons), ornamental carvings, tumbled stones for collectors, and landscaping stone.
Geological facts
Aventurine is known for its metallic shimmer, a phenomenon called 'aventurescence'. While green is the most common color, it can also be found in blue, orange, and red depending on the inclusions.
Field identification & locations
Identify by its characteristic green color and internal shimmering flakes (mica). It is commonly found in India (the primary source), Brazil, and Russia. Collectors value deep, uniform color and high aventurescence.
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