
mineral
Green Aventurine
Silicon Dioxide with Fuchsite inclusions (SiO2 + K(Al,Cr)2AlSi3O10(OH)2)
Hardness: 7 on Mohs scale; Color: Pale to dark green; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.64-2.69. It displays a characteristic shimmering effect called aventurescence.
- Hardness
- 7 on Mohs scale
- Color
- Pale to dark green
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale to dark green; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.64-2.69. It displays a characteristic shimmering effect called aventurescence.
Formation & geological history
Formed in magmatic and metamorphic environments where quartz-rich deposits undergo high pressure or heat, allowing mica inclusions (usually Fuchsite) to form within the quartz structure. Most deposits are millions of years old.
Uses & applications
Primarily used in jewelry (beads, cabochons), ornamental carvings, and as a popular stone for collectors and metaphysical practitioners. Occasionally used in interior decor like mosaics.
Geological facts
The name 'Aventurine' comes from the Italian 'a ventura', meaning 'by chance', originally referring to accidental aventurine glass production in the 18th century. It is known as the 'Stone of Opportunity' in folklore.
Field identification & locations
Identify by its 'shimmer' or 'glitter' (aventurescence) caused by mica flakes. It is a common find in river beds or quarries in regions like India, Brazil, and Russia. Collectors should look for a uniform green color and strong sparkling effect.
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