
mineral
Blue Quartz (Blue Chalcedony/Dumortierite Quartz)
Silicon Dioxide (SiO2) with inclusions (typically Dumortierite Al7(BO3)(SiO4)3O3)
AI-generated identification · may be incorrectHardness: 7 Mohs scale; Color: Pale to deep blue with golden-brown iron oxide veins; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None; Specific Gravity: 2.65
- Hardness
- 7 Mohs scale
- Color
- Pale to deep blue with golden-brown iron oxide veins
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 Mohs scale; Color: Pale to deep blue with golden-brown iron oxide veins; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None; Specific Gravity: 2.65
Formation & geological history
Formed primarily through the crystallization of silica-rich hydrothermal fluids in igneous veins or as secondary deposits in sedimentary rock cavities. The blue color is often caused by micro-inclusions of other minerals like dumortierite or tourmaline.
Uses & applications
Used extensively in lapidary for carvings, cabochons, and polished pocket stones. It is popular in the metaphysical community and for jewelry such as pendants and bracelets.
Geological facts
Unlike Blue Lace Agate, Blue Quartz often gets its color from mineral inclusions rather than structural light scattering. It is sometimes referred to as 'Blue Moon Quartz' when it displays a specific translucency.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and the presence of fibrous or moss-like blue inclusions. Found commonly in Brazil, South Africa, and the United States (Virginia).
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary