Rock Identifier
Quartz Pebble (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

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, specific gravity of 2.65

Identified More sedimentary
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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, specific gravity of 2.65

Formation & geological history

Formed through weathering and water erosion of primary quartz-bearing rocks, commonly rounded by water transport in streams, rivers, or beach environments.

Uses & applications

Used in landscaping, decorative stone, abrasive manufacturing, and lapidary work.

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

Easily identified by its high hardness (scratches glass), lack of cleavage, and smooth, water-worn shape found globally in riverbeds and beaches.