
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, typically white or translucent with a vitreous to greasy luster, hexagonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, typically white or translucent with a vitreous to greasy luster, hexagonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
Formation & geological history
Forms in a wide variety of geological environments, including igneous, metamorphic, and sedimentary rocks. It is a major constituent of granites and sandstones and precipitates out of hydrothermal veins.
Uses & applications
Used in electronics (oscillators), glassmaking, abrasive materials, gemstone carving, and optical instruments.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust, surpassed only by feldspar. Due to its piezoelectric properties, quartz crystals are used in watches and electronics to generate a precise frequency.
Field identification & locations
Easily identified in the field by its high hardness (scratches glass), lack of cleavage, and conchoidal fracture. Found worldwide in nearly all types of geological formations.
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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
Schist
Schist
Metamorphic
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral