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

Green Aventurine

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

Hardness: 6.5–7; Color: Pale to deep green; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.63–2.69

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

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Physical properties

Hardness: 6.5–7; Color: Pale to deep green; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.63–2.69

Formation & geological history

Formed as a metamorphic quartzite which crystallized over millions of years under high pressure and temperature. The green color is primarily caused by platy inclusions of chromium-rich mica (fuchsite) during its formation.

Uses & applications

Predominantly used for lapidary work, jewelry, ornamental carvings, and as a popular 'healing stone' in metaphysical collections. Occasionally used as an architectural stone.

Geological facts

It is famous for the 'aventurescence' effect, which is the shimmering or glistening caused by tiny inclusions reflecting light. The name is derived from the Italian word 'a ventura', meaning 'by chance'.

Field identification & locations

Identify by its distinct glistening schiller effect (aventurescence) when turned under light. Found commonly in Brazil, India, Russia, and Tanzania. Unlike jade, it often has a more grainy, sugary appearance on raw surfaces.