
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, white to translucent color, vitreous to greasy 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, white to translucent color, vitreous to greasy 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 including igneous, metamorphic, and sedimentary rocks. Often weathered out of parent rock and rounded into pebbles via water transport in rivers or ocean beaches.
Uses & applications
Used in landscaping, decorative gravel, glassmaking, abrasives, and gemstone carving or lapidary work.
Geological facts
Quartz is one of the most abundant and durable minerals on Earth's continental crust. Its high resistance to both mechanical and chemical weathering allows it to survive long transport distances, often outlasting almost all other minerals in a sedimentary deposit.
Field identification & locations
Easily identified in the field by its high hardness (scratches glass easily), lack of cleavage, and glassy or waxy luster. Found worldwide in stream beds, beaches, and conglomerate rock formations.
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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
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Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
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Septarian Pebble
Septarian nodule / Concretion
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral