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

Green Aventurine

Quartzite with Fuchsite inclusions (SiO2 + K(Al,Cr)2AlSi3O10(OH)2)

Hardness: 7 on Mohs scale; Color: Pale to deep green; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69

Hardness
7 on Mohs scale
Color
Pale to deep green
Luster
Vitreous to waxy
Identified More metamorphic

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 7 on Mohs scale; Color: Pale to deep green; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69

Formation & geological history

Formed through the regional metamorphism of quartz-rich sedimentary rocks (sandstone) where mica inclusions like green fuchsite are present. It is typically found in Precambrian metamorphic terrains.

Uses & applications

Primarily used as a gemstone for jewelry (beads, cabochons), ornamental carvings, stone inlays, and widely sold in the metaphysical or 'healing crystals' market.

Geological facts

Aventurine is known for 'aventurescence,' a shimmering effect caused by platy mineral inclusions reflecting light. The name comes from the Italian 'a ventura' (by chance), originally referring to the accidental discovery of goldstone glass in the 18th century which looks similar.

Field identification & locations

Identify in the field by its grainy, quartzite-like texture and its distinctive internal shimmer when rotated under light. Most commonly sourced from India, Brazil, and Russia. Collectors look for even saturation of color and high mica content.