
mineral
Green Quartz (Aventurine)
Silicon Dioxide with Fuchsite inclusions (SiO2 + K(Al,Cr)2(AlSi3O10)(OH)2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Pale to medium green with 'aventurescence'; Luster: Vitreous to waxy; Crystal Structure: Trigonal (hexagonal system); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.64-2.69
- Hardness
- 6
- Color
- Pale to medium green with 'aventurescence'
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Pale to medium green with 'aventurescence'; Luster: Vitreous to waxy; Crystal Structure: Trigonal (hexagonal system); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.64-2.69
Formation & geological history
Formed in magmatic and metamorphic environments, specifically within pegmatites or metamorphic rocks where mica is present. The green color is primarily due to inclusions of chrome-rich fuchsite mica.
Uses & applications
Predominantly used for lapidary work including tumbled stones, beads, figurines, and cabochons. It is also a popular specimen for metaphysical collectors and landscape architecture.
Geological facts
The name 'aventurine' comes from the Italian word 'a ventura,' meaning 'by chance.' This refers to the lucky discovery of aventurine glass (goldstone) in the 18th century, which looks similar to this natural mineral.
Field identification & locations
Look for a shimmering or glinting effect (aventurescence) when rotated under light, caused by platy mineral inclusions. It is commonly found in India, Brazil, and Russia. Unlike jade, it is often more translucent and has visible graininess.
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