
mineral
Blue Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, pale to deep blue color, vitreous to greasy luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, pale to deep blue color, vitreous to greasy luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
Formation & geological history
Forms in igneous, metamorphic, and sedimentary environments. The blue color is typically caused by microscopic inclusions of fibrous minerals like crocidolite or dumortierite, or due to Rayleigh scattering from lattice defects.
Uses & applications
Used primarily in lapidary arts, making tumbled stones, carvings, jewelry, and decorative items, as well as mineral specimen collecting.
Geological facts
Natural blue quartz is relatively rare compared to other varieties like amethyst or citrine. Many commercial blue quartz specimens on the market are actually dyed or heat-treated quartz.
Field identification & locations
Can be identified by its conchoidal fracture, lack of cleavage, hardness of 7, and characteristic blue coloration. Found worldwide, with notable deposits in Brazil, India, and the United States.
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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