Rock Identifier
Aventurine Quartz (Silicon Dioxide with Fuchsite inclusions (SiO2 + K(Al,Cr)2AlSi3O10(OH)2)) — mineral
mineral

Aventurine Quartz

Silicon Dioxide with Fuchsite inclusions (SiO2 + K(Al,Cr)2AlSi3O10(OH)2)

Hardness: 6.5-7 (Mohs scale); Color: Green; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Notable for its aventurescence effect.

Hardness
6
Color
Green
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Green; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Notable for its aventurescence effect.

Formation & geological history

Formed in metamorphic rocks and magmatic environments where tectonic pressure and heat allow for the growth of quartz with platy mineral inclusions like chromium-rich mica (fuchsite).

Uses & applications

Widely used in jewelry (beads, cabochons), ornamental carvings, figurines, and as a popular lucky stone for mineral collectors.

Geological facts

Aventurine is known for its shimmering effect called 'aventurescence,' caused by light reflecting off tiny inclusions of green mica. The name is derived from the Italian 'a ventura' meaning 'by chance.'

Field identification & locations

Identify by its characteristic green color and internal metallic-looking sparkles. While this specimen was found in the Las Cruces area (New Mexico), it is likely a tumbled stone that was lost or discarded, as significant green aventurine deposits are more typical of Brazil, India, and Russia.