Rock Identifier
Quartz Pebbles (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz Pebbles

Silicon Dioxide (SiO2)

Hardness 7 on Mohs scale; luster varies from waxy to vitreous; colors range from opaque white (milky quartz) to brownish-gray; no cleavage; conchoidal fracture.

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Physical properties

Hardness 7 on Mohs scale; luster varies from waxy to vitreous; colors range from opaque white (milky quartz) to brownish-gray; no cleavage; conchoidal fracture.

Formation & geological history

Formed from molten magma cooling at various temperatures or precipitated from hydrothermal veins. These specific specimens are river-worn or weathered pebbles found in alluvial deposits.

Uses & applications

Raw quartz is used in the glass and ceramics industry, for abrasives, and as a material for clocks and electronics (piezoelectric). Tumbled versions are used in jewelry.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz, traditionally called rock crystal, is colorless and transparent.

Field identification & locations

Identify by its hardness (will scratch glass) and lack of cleavage. Common in riverbeds, beaches, and gravel pits worldwide.