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

Green Aventurine

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

Hardness: 6.5-7 (Mohs scale); Color: Pale to dark green with a shimmering effect; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69

Hardness
6
Color
Pale to dark green with a shimmering effect
Luster
Vitreous to waxy
Identified More mineral

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Pale to dark green with a shimmering effect; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69

Formation & geological history

Formed in metamorphic rocks (schist) and through hydrothermal processes. The green color is primarily caused by platy inclusions of mica (fuchsite) trapped within the quartz as it crystallizes. It is found in various geological layers spanning the Proterozoic to recent eras.

Uses & applications

Used widely in lapidary work for cabochons, beads, and tumbled stones. Also used for ornamental carvings, household decor items, and as a popular stone for metaphysical collecting.

Geological facts

Green Aventurine is best known for its 'aventurescence,' a optical phenomenon where the mica inclusions reflect light like tiny sparkles. It is often called the 'Stone of Opportunity' in folklore.

Field identification & locations

Identify by its characteristic green shimmer (aventurescence) and quartz-like hardness. Frequently found in India, Brazil, Russia, and Tanzania. Unlike jade, it has a granular texture under magnification due to the quartz grains.