
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale. Color varies widely from colorless/white to smoky, pink, purple, etc. Vitreous to greasy luster. Trigonal crystal system. Conchoidal fracture with no true cleavage. Specific gravity is 2.65.
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Physical properties
Hardness of 7 on the Mohs scale. Color varies widely from colorless/white to smoky, pink, purple, etc. Vitreous to greasy luster. Trigonal crystal system. Conchoidal fracture with no true cleavage. Specific gravity is 2.65.
Formation & geological history
Forms in a wide variety of geological environments, most commonly in igneous, metamorphic, and sedimentary rocks. It is a major constituent of granite and sandstone and precipitates from hydrothermal solutions.
Uses & applications
Used in electronics (oscillators), glassmaking, abrasive materials, gemstone carving, and ornamental displays.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust, surpassed only by feldspar. It exhibits piezoelectric properties, generating an electric charge under mechanical stress.
Field identification & locations
Easily identified by its characteristic high hardness (scratches glass), conchoidal fracture, and lack of cleavage. Found worldwide in nearly every geological setting.
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Potassium Feldspar (Orthoclase)
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