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

Quartz Pebble

Silicon dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, typically yellow to orange-brown due to iron staining, waxy to vitreous luster, and conchoidal fracture.

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Physical properties

Hardness of 7 on the Mohs scale, typically yellow to orange-brown due to iron staining, waxy to vitreous luster, and conchoidal fracture.

Formation & geological history

Formed through the physical weathering and long-distance aqueous transport of quartz veins or parent rock, smoothing sharp edges into rounded pebbles over long periods.

Uses & applications

Used in landscaping, decorative gravel, abrasive manufacture, and as a durable aggregate in construction.

Geological facts

Quartz is one of the most abundant and stable minerals on Earth's surface, resisting chemical weathering far longer than most other minerals.

Field identification & locations

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