
mineral
Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale. Color is typically white or transparent, sometimes with impurities. Luster is vitreous (glassy). Crystal structure is trigonal. Cleavage is none (it exhibits conchoidal fracture). Specific gravity is 2.65.
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Physical properties
Hardness of 7 on the Mohs scale. Color is typically white or transparent, sometimes with impurities. Luster is vitreous (glassy). Crystal structure is trigonal. Cleavage is none (it exhibits conchoidal fracture). Specific gravity is 2.65.
Formation & geological history
Forms in a wide variety of geological environments, most notably in igneous rocks like granite and pegmatites, as well as hydrothermal veins and sedimentary rocks (sandstone).
Uses & applications
Widely used in electronics (oscillators, quartz clocks), glassmaking, abrasives, gemstones, and decorative items.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust, surpassed only by feldspar. It exhibits piezoelectric properties, meaning it can generate an electrical charge in response to applied mechanical stress.
Field identification & locations
Can be identified in the field by its high hardness (scratches glass), conchoidal fracture, and lack of cleavage. It is found worldwide on every continent.
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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