
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, color ranges from colorless to white, vitreous to greasy luster, trigonal crystal system, conchoidal fracture, specific gravity of 2.65
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Physical properties
Hardness of 7 on the Mohs scale, color ranges from colorless to white, vitreous to greasy luster, trigonal crystal system, conchoidal fracture, specific gravity of 2.65
Formation & geological history
Forms in a wide variety of geological environments, including igneous, metamorphic, and sedimentary rocks. Commonly crystallizes from silica-rich hydrothermal veins and magma chambers.
Uses & applications
Used in electronics, oscillators, glassmaking, abrasives, and as a gemstone or ornamental mineral in jewelry.
Geological facts
Quartz is one of the most abundant and widely distributed minerals found on Earth's continental crust. It exhibits piezoelectric properties, meaning it can generate an electrical charge in response to applied mechanical stress.
Field identification & locations
Easily identified by its characteristic crystal habit, high hardness (scratches glass), and lack of cleavage. Found worldwide in nearly every geological setting.
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Arenite (SiO2 based)
sedimentary
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Regolith / Silicate Mineral Aggregate
sedimentary
Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
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Schist
Schist
Metamorphic
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral