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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, typically brown, tan, or clear in color, vitreous to waxy luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically brown, tan, or clear in color, vitreous to waxy luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.

Formation & geological history

Formed through the weathering and erosion of quartz-bearing rocks like granite or quartzite, followed by transportation in water streams where it becomes rounded into a pebble over long geological timescales.

Uses & applications

Used in landscaping, decorative stone, production of silicon and ferrosilicon, and as a common tumbling stone for rockhounds.

Geological facts

Quartz is one of the most abundant and durable minerals in Earth's continental crust, surviving weathering processes that destroy most other minerals.

Field identification & locations

Found worldwide in riverbeds, beaches, and alluvial deposits. Easily identifiable by its high hardness (scratches glass) and lack of cleavage.