
mineral
White Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, milky white 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, milky white color, vitreous to greasy luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
Formation & geological history
Forms in a wide variety of geological environments, most commonly crystallizing from silica-rich hydrothermal veins and magma chambers, as well as in pegmatites and metamorphic rocks.
Uses & applications
Used in the manufacture of glass, electronics, optical lenses, abrasive materials, and as a popular decorative or lapidary stone for tumbling and carving.
Geological facts
Quartz is one of the most abundant and ubiquitous minerals found in the Earth's continental crust. Its piezoelectric properties make it essential in modern electronics for precise frequency control in watches and computers.
Field identification & locations
Identified by its high hardness (scratches glass easily), white color, and lack of cleavage with a conchoidal fracture. Found worldwide in nearly every geological setting.
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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