
mineral
Blue Quartz (Dumortierite Quartz)
Silicon Dioxide (SiO2) with inclusions of Dumortierite (Al7BO3(SiO4)3O3)
Hardness: 7.0 on Mohs scale; Color: Denim blue, violet-blue, or indigo; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.62-2.67
- Hardness
- 7
- Color
- Denim blue, violet-blue, or indigo
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7.0 on Mohs scale; Color: Denim blue, violet-blue, or indigo; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.62-2.67
Formation & geological history
Formed in silica-rich pegmatites or metamorphic environments where alumina-rich sediments were subjected to high-grade metamorphism. The blue color is derived from fibrous inclusions of the mineral dumortierite.
Uses & applications
Used primarily for ornamental purposes, jewelry (beads, cabochons), metaphysical collecting, and as a pocket stone/tumbled stone.
Geological facts
Unlike Sapphire or Blue Lace Agate, the blue in this quartz is caused by inclusions of another mineral rather than trace chemical elements. It was named after the French paleontologist Eug ne Dumortier.
Field identification & locations
Identify by its denim-blue hue and typical quartz hardness (cannot be scratched by steel). It is commonly found in Brazil, Namibia, Madagascar, and the USA. Collectors should look for the characteristic fibrous patterns within the stone.
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