
mineral
Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, color ranges from colorless to white, gray, purple, pink, etc.; vitreous luster; trigonal crystal system; no cleavage; specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, color ranges from colorless to white, gray, purple, pink, etc.; vitreous luster; trigonal crystal system; no cleavage; specific gravity of 2.65.
Formation & geological history
Forms in a wide variety of geological environments, including igneous, metamorphic, and sedimentary rocks. Often crystallizes from silica-rich hydrothermal veins and pegmatites.
Uses & applications
Used in electronics, watches, glassmaking, ceramics, abrasives, and as a gemstone or ornamental stone in jewelry.
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
Easily identifiable in the field by its high hardness (scratches glass), conchoidal fracture, and lack of cleavage. Found worldwide in almost every rock type.
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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