Rock Identifier
Green Aventurine (Silicon Dioxide with Fuchsite (SiO2 + K(Al,Cr)2AlSi3O10(OH)2)) — metamorphic
metamorphic

Green Aventurine

Silicon Dioxide with Fuchsite (SiO2 + K(Al,Cr)2AlSi3O10(OH)2)

Hardness: 6.5-7 (Mohs scale); Color: Pale to deep green; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.64-2.69

Hardness
6
Color
Pale to deep green
Luster
Vitreous to waxy
Identified More metamorphic
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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Pale to deep green; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.64-2.69

Formation & geological history

Formed as a metamorphic rock (quartzite) where quartz is recrystallized under heat and pressure. The green color and 'aventurescence' sparkle are caused by platy inclusions of green chromium-rich mica known as Fuchsite.

Uses & applications

Used widely in lapidary work for cabochons, beads, figurines, and tumbled stones. Also popular in ornamental carvings, architectural accents, and the metaphysical gemstone market.

Geological facts

The name comes from the Italian 'a ventura' (by chance), originally referring to accidental discovery of aventurine glass. Natural aventurine is often called the 'Stone of Opportunity' in folklore. Its distinct shimmer is an optical effect called aventurescence.

Field identification & locations

Identified by its grainy quartz texture combined with a shimmering green sheen. To distinguish from green jade, check for the granular/sugary texture of quartz. It is commonly found in India, Brazil, Russia, and Austria.