Rock Identifier
Green Aventurine (Green Quartz) (Silicon Dioxide (SiO2) with inclusions of Fuchsite (K(Al,Cr)2(AlSi3O10)(OH)2)) — Mineral/Metamorphic rock
Mineral/Metamorphic rock

Green Aventurine (Green Quartz)

Silicon Dioxide (SiO2) with inclusions of Fuchsite (K(Al,Cr)2(AlSi3O10)(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. It is characterized by 'aventurescence'—a shimmering effect.

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

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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. It is characterized by 'aventurescence'—a shimmering effect.

Formation & geological history

Formed during regional metamorphism of quartz-rich sediments. The green color and shimmer are caused by chromium-rich mica (fuchsite) platelets being trapped inside the quartz matrix during crystallization. Specimen ages vary by deposit, often hundreds of millions of years old.

Uses & applications

Primarily used for ornamental carvings, jewelry (cabochons and beads), landscaping, and as a popular stone in the metaphysical and gemstone collecting community.

Geological facts

Aventurine is often mistaken for jade, but its shimmering aventurescence (caused by light reflecting off internal flakes of mica) is its defining geological feature. The name comes from the Italian 'a ventura,' meaning 'by chance,' originally referring to an 18th-century glass accidental discovery.

Field identification & locations

Identify in the field by its hardness (will scratch glass), green mottled color, and subtle metallic shimmer when rotated under light. Commonly found in India, Brazil, and Russia. Collectors should look for even color distribution and strong internal reflection.