
mineral
Green Aventurine
Aventurine Quartz (SiO2 with inclusions of Fuchsite)
Hardness: 7 (Mohs scale); Color: Pale to deep green; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.64-2.69. Known for 'aventurescence' (a shimmering effect caused by platy inclusions).
- Hardness
- 7 (Mohs scale)
- Color
- Pale to deep green
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: Pale to deep green; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.64-2.69. Known for 'aventurescence' (a shimmering effect caused by platy inclusions).
Formation & geological history
Formed as a sedimentary or metamorphic rock, aventurine is a form of quartzite. The green color and shimmering quality are the result of chromium-rich mica (fuchsite) inclusions becoming trapped in the quartz as it undergoes pressure and heat.
Uses & applications
Predominantly used for ornamental carvings, semi-precious jewelry (beads, cabochons), tumbled stones for collecting, and lapidary art.
Geological facts
The name 'Aventurine' comes from the Italian 'a ventura', meaning 'by chance'. This refers to the accidental discovery of 'goldstone' (aventurine glass) in the 18th century, which the natural mineral was later named after because of its similar appearance.
Field identification & locations
Identify by its characteristic green 'shimmer' when rotated under light (aventurescence) and its ability to scratch glass. It is commonly found in India, Brazil, and Russia. Beginners should distinguish it from jade, which is tougher and lacks the plate-like mica reflections.
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