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

Green Aventurine

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

Hardness: 6.5-7 on Mohs scale. Color: Pale to dark green with a shimmering effect (aventurescence). Luster: Vitreous to waxy. Structure: Trigonal (hexagonal) crystalline aggregate. Specific Gravity: 2.64-2.69.

Hardness
6
Color
Pale to dark green with a shimmering effect (aventurescence)
Luster
Vitreous to waxy
Identified More metamorphic
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Physical properties

Hardness: 6.5-7 on Mohs scale. Color: Pale to dark green with a shimmering effect (aventurescence). Luster: Vitreous to waxy. Structure: Trigonal (hexagonal) crystalline aggregate. Specific Gravity: 2.64-2.69.

Formation & geological history

Formed through the regional metamorphism of quartz-rich sedimentary rocks (sandstone). The characteristic green color and shimmer are caused by tiny inclusions of green fuchsite mica. Formation typically occurs under high heat and pressure in tectonic belts.

Uses & applications

Primarily used in jewelry for pendants, beads, and cabochons. Also used for ornamental carvings, figurines, and as a popular 'healing stone' in metaphysical practices.

Geological facts

The name 'aventurine' comes from the Italian 'a ventura,' meaning 'by chance,' referring to the 18th-century accidental discovery of aventurine glass (Goldstone) which mimics this stone's natural glitter.

Field identification & locations

Identify by its characteristic 'aventurescence' (metallic glimmer) and mossy green color. It is softer than pure quartz but harder than nephrite jade. Most commercial specimens are sourced from India, Brazil, and Russia.