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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, white or off-white color, vitreous to dull luster depending on weathering, conchoidal fracture, specific gravity of 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, white or off-white color, vitreous to dull luster depending on weathering, conchoidal fracture, specific gravity of 2.65.

Formation & geological history

Formed through the mechanical weathering and erosion of quartz-bearing rocks like granite or quartzite, followed by transportation and rounding in aquatic environments (rivers, beaches) over geological timescales.

Uses & applications

Used in landscaping, decorative gravel, aggregate in construction, and tumbled stones for lapidary work.

Geological facts

Quartz is one of the most abundant and durable minerals on Earth's continental crust, which is why quartz pebbles are extremely common in riverbeds and beaches.

Field identification & locations

Can be identified by its high hardness (scratches glass), lack of cleavage, and resistance to chemical weathering. Found worldwide in stream beds, beaches, and conglomerate rock formations.