
mineral
Quartz (Milky or Druzy Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: White to translucent, Luster: Vitreous to greasy, Crystal structure: Hexagonal/Trigonal, cleavage: Indistinct/conchoidal fracture, Specific gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: White to translucent, Luster: Vitreous to greasy, Crystal structure: Hexagonal/Trigonal, cleavage: Indistinct/conchoidal fracture, Specific gravity: 2.65
Formation & geological history
Formed through hydrothermal processes, cooling of igneous magma, or precipitation from silica-rich fluids in rock cavities. Common throughout all geological ages.
Uses & applications
Used in glass manufacturing, electronics (piezoelectric properties), abrasives, and as semi-precious gemstones/jewelry.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz', which originally meant 'hard'.
Field identification & locations
Identify by its hardness (it can scratch glass), its lack of cleavage, and its characteristic waxy or glassy luster. Found globally in almost all geological environments.
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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