
mineral
Clear Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, colorless or transparent, vitreous (glassy) luster, trigonal 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, colorless or transparent, vitreous (glassy) luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
Formation & geological history
Forms in a wide variety of geological environments, most notably in igneous rocks like pegmatites, as well as hydrothermal veins and sedimentary environments. Crystallizes from silica-rich fluids over millions of years.
Uses & applications
Used in electronics (oscillators), manufacturing of glass and ceramics, optical lenses, jewelry, and gemstone carving, as well as in metaphysical practices and crystal collections.
Geological facts
Clear quartz is one of the most abundant minerals in Earth's continental crust. It exhibits piezoelectric properties, meaning it can generate an electrical charge in response to mechanical stress.
Field identification & locations
Identified by its high hardness (scratches glass), transparent to translucent appearance, lack of cleavage, and characteristic conchoidal fracture. Found worldwide with major deposits in Brazil, the United States, Madagascar, and the Alps.
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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