
mineral
Quartz pebble
Silicon dioxide (SiO2)
Hardness of 7 on the Mohs scale, typically white, clear, or grey, vitreous luster, hexagonal crystal system when well-formed, conchoidal fracture, specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, typically white, clear, or grey, vitreous luster, hexagonal crystal system when well-formed, conchoidal fracture, specific gravity of 2.65.
Formation & geological history
Formed via the crystallization of silica-rich solutions in hydrothermal veins or as residual grains weathering out of igneous and metamorphic rocks over millions of years.
Uses & applications
Used in landscaping, abrasive materials, glassmaking, electronics, and as collector specimens.
Geological facts
Quartz is one of the most abundant and durable minerals in the Earth's continental crust, highly resistant to both chemical and mechanical weathering.
Field identification & locations
Can be identified by its high hardness (scratches glass) and conchoidal fracture; found universally in riverbeds, beaches, and soils worldwide.
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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