Rock Identifier
Green Aventurine (Silicon Dioxide (SiO2) with inclusions of Fuchsite) — metamorphic
metamorphic

Green Aventurine

Silicon Dioxide (SiO2) with inclusions of Fuchsite

Hardness: 7 Mohs; Color: Pale to dark green with a shimmering effect (aventurescence); Luster: Vitreous; Crystal Structure: Trigonal (hexagonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69

Hardness
7 Mohs
Color
Pale to dark green with a shimmering effect (aventurescence)
Luster
Vitreous
Identified More metamorphic

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Physical properties

Hardness: 7 Mohs; Color: Pale to dark green with a shimmering effect (aventurescence); Luster: Vitreous; Crystal Structure: Trigonal (hexagonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69

Formation & geological history

Formed in metamorphic environments where quartz sandstone is subjected to intense heat and pressure, with the green color provided by the mica mineral fuchsite. It is primarily found in Pre-Cambrian to Paleozoic geological formations.

Uses & applications

Used extensively in jewelry (beads, cabochons), ornamental carvings, crystal healing, and as a decorative stone in architecture and interior design.

Geological facts

The name 'Aventurine' comes from the Italian 'a ventura', meaning 'by chance', referring to the accidental discovery of aventurine glass in the 18th century. Most green aventurine is sourced from India and Brazil.

Field identification & locations

Identify by its 'aventurescence'—the metallic glitter caused by platy inclusions within the quartz. It is much harder than fluorite but lacks the unique feel of genuine jade. Commonly found in India, Russia, and Brazil.