
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, vitreous to greasy luster, transparent to opaque, conchoidal fracture, lack of cleavage, specific gravity of 2.65, trigonal crystal system.
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Physical properties
Hardness of 7 on the Mohs scale, vitreous to greasy luster, transparent to opaque, conchoidal fracture, lack of cleavage, specific gravity of 2.65, trigonal crystal system.
Formation & geological history
Forms in a wide variety of geological environments including igneous, metamorphic, and sedimentary rocks. It is a primary component of granite and sandstone, and often crystallizes from hydrothermal veins.
Uses & applications
Used in electronics, oscillators, glassmaking, abrasives, gemstones, and ornamental objects.
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 identified by its hardness (scratches glass), lack of cleavage, and distinct conchoidal fracture. Found worldwide in nearly every type of geological terrain.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Soil with Mineral Detritus and Quartz Fragments
Regolith / Silicate Mineral Aggregate
sedimentary
Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
mineral
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral