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

Green Quartzite (Aventurine variety)

Silicon Dioxide (SiO2) with inclusions of Fuchsite

Hardness: 7 (Mohs scale), Color: Pale to medium green, Luster: Vitreous to waxy, Structure: Trigonal/Hexagonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.64-2.69

Identified More metamorphic

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Physical properties

Hardness: 7 (Mohs scale), Color: Pale to medium green, Luster: Vitreous to waxy, Structure: Trigonal/Hexagonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.64-2.69

Formation & geological history

Formed through the regional metamorphism of quartz-rich sandstone. High heat and pressure cause quartz grains to recrystallize and fuse. The green color is typically derived from the presence of tiny chromium-rich mica minerals (fuchsite) trapped within the quartz matrix during formation.

Uses & applications

Commonly used for ornamental carvings, landscape stones, decorative aggregate, and in 'healing' crystal collections. Fine specimens are used in jewelry as cabochons or beads.

Geological facts

Green aventurine is often called the 'Stone of Opportunity' in metaphysical circles. This specific specimen’s rounded edges suggest it has been water-worn or mechanically tumbled.

Field identification & locations

Identify in the field by its inability to be scratched by a steel knife and its lack of carbonate reaction (fizzing) with acid. It is commonly found in India, Brazil, and parts of Russia. This specimen shows 'platy' inclusions that are characteristic of green mica varieties.