
mineral
Green Aventurine (Double-Terminated Wand)
Silicon Dioxide (SiO2) containing Fuchsite (Chromium-rich Muscovite Mica)
Hardness: 7 on Mohs scale; Color: Forest green to translucent green; Luster: Vitreous to waxy with 'aventurescence' (metallic glitters); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69
- Hardness
- 7 on Mohs scale
- Color
- Forest green to translucent green
- Luster
- Vitreous to waxy with 'aventurescence' (metallic glitters)
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Physical properties
Hardness: 7 on Mohs scale; Color: Forest green to translucent green; Luster: Vitreous to waxy with 'aventurescence' (metallic glitters); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.64-2.69
Formation & geological history
Formed through the metamorphic process where magma cools within the earth's crust, or in magmatic deposits. Its green color is primarily due to inclusions of chromium-rich fuchsite mica. It is found in deposits dating back millions of years.
Uses & applications
Primary use is in lapidary work for jewelry, cabochons, and tumbled stones. Frequently used in 'crystal healing' practices and home decor due to its pleasing color. In industry, it is sometimes used for ornamental carvings.
Geological facts
The name 'Aventurine' is derived from the Italian 'a ventura,' meaning 'by chance.' This refers to the accidental discovery of aventurine glass (goldstone) in the 18th century, which the natural mineral closely resembles.
Field identification & locations
Identify in the field by its green color and the presence of shimmering mica inclusions (aventurescence). It will scratch glass. Common locations include India (the largest producer), Brazil, Russia, and Austria. Tips for collectors: Check for uniform color and the quality of the 'sparkle' inside the stone.
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