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

Green Aventurine

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

Hardness: 6.5-7 on Mohs scale; Color: Green with aventurescence (shimmer); Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: None/Conchoidal; Specific gravity: 2.64-2.69

Hardness
6
Color
Green with aventurescence (shimmer)
Luster
Vitreous to waxy
Identified More metamorphic

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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Green with aventurescence (shimmer); Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: None/Conchoidal; Specific gravity: 2.64-2.69

Formation & geological history

Formed through the metamorphism of sandstone into quartzite, where the mica inclusions (fuchsite) align to create a sugary, shimmering effect known as aventurescence. Primarily found in Precambrian shield areas.

Uses & applications

Used widely in lapidary for carvings, beads, and cabochons. Frequently used in jewelry, ornamental statues, and as a popular stone for 'healing crystal' collections.

Geological facts

The name 'Aventurine' comes from the Italian 'a ventura,' meaning 'by chance,' referencing the discovery of goldstone (a man-made glass) that looks similar accidentally in the 18th century.

Field identification & locations

Identify by its characteristic 'shimmer' caused by green fuchsite mica plates inside. Most commercial specimens come from India, Brazil, and Russia. It can be distinguished from Jade by its lower translucency and the presence of sparkling internal flakes.