
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, milky white to clear color with yellowish-brown iron staining, 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, milky white to clear color with yellowish-brown iron staining, 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, most commonly as a primary mineral in igneous rocks like granite and pegmatites, in hydrothermal veins, and as detrital grains in sedimentary rocks.
Uses & applications
Used in electronics, glassware, precision instruments, abrasives, gemstones, and ornamental objects.
Geological facts
Quartz is one of the most abundant and widely distributed minerals found at Earth's surface. It exhibits piezoelectric properties, meaning it can generate an electrical charge in response to mechanical stress, making it crucial for watches and electronic oscillators.
Field identification & locations
Easily identified by its hardness (scratches glass), conchoidal fracture, and lack of cleavage. Found worldwide in nearly every type of geological setting.
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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