
mineral
Quartz pebble
Silicon dioxide (SiO2)
Hardness of 7 on the Mohs scale, clear to milky white or greyish color, vitreous luster, trigonal crystal system, conchoidal fracture, specific gravity of 2.65
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Physical properties
Hardness of 7 on the Mohs scale, clear to milky white or greyish color, vitreous luster, trigonal crystal system, conchoidal fracture, specific gravity of 2.65
Formation & geological history
Formed through crystallization from silicate melts or hydrothermal solutions, often weathering out of igneous and metamorphic parent rocks and transported by water to form smooth pebbles in sedimentary environments
Uses & applications
Used in landscaping, decorative stone, abrasives, glassmaking, and electronic components
Geological facts
Quartz is one of the most abundant and durable minerals in Earth's continental crust, highly resistant to both chemical and mechanical weathering
Field identification & locations
Easily identified by its high hardness (scratches glass), lack of cleavage, and conchoidal fracture; commonly found in riverbeds, beaches, and gravel deposits worldwide
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Soil with Mineral Detritus and Quartz Fragments
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Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
mineral
Schist
Schist
Metamorphic
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral