
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, color ranges from colorless/white to various shades of grey, vitreous luster, hexagonal 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/white to various shades of grey, vitreous luster, hexagonal 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. Often crystallizes from silica-rich hydrothermal veins or magma.
Uses & applications
Used in electronics (oscillators), glassmaking, abrasives, gemstones, and construction materials.
Geological facts
Quartz is one of the most abundant minerals in the Earth's continental crust and exhibits piezoelectric properties, meaning it can generate an electrical charge under mechanical stress.
Field identification & locations
Easily identifiable by its high hardness (scratches glass), conchoidal fracture, and lack of cleavage. Found worldwide in virtually every type of geological environment.
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Arenite (SiO2 based)
sedimentary
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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