
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, vitreous to greasy luster, transparent to opaque, conchoidal fracture, no true cleavage, specific gravity of 2.65, trigonal crystal system.
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Physical properties
Hardness of 7 on the Mohs scale, vitreous to greasy luster, transparent to opaque, conchoidal fracture, no true cleavage, specific gravity of 2.65, trigonal crystal system.
Formation & geological history
Forms in a wide variety of geological environments including igneous, metamorphic, and sedimentary rocks. Often crystallizes from silica-rich hydrothermal solutions or cooling magma.
Uses & applications
Used in electronics, oscillators, glassmaking, abrasive materials, gemstone carving, and mineral specimen collecting.
Geological facts
Quartz is one of the most abundant and widely distributed minerals on Earth's continental crust. It exhibits piezoelectric properties, meaning it can generate an electrical charge when mechanical stress is applied.
Field identification & locations
Can be identified by its characteristic conchoidal fracture, high hardness (scratches glass easily), and hexagonal crystal prism habits when well-formed. Found globally.
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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