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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, typically white or translucent, vitreous luster, trigonal crystal structure (though massive in this pebble form), no cleavage, specific gravity of 2.65. Iron staining gives it rustic red/orange hues.

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Physical properties

Hardness of 7 on the Mohs scale, typically white or translucent, vitreous luster, trigonal crystal structure (though massive in this pebble form), no cleavage, specific gravity of 2.65. Iron staining gives it rustic red/orange hues.

Formation & geological history

Formed from igneous, metamorphic, or sedimentary processes. This specific specimen has been heavily weathered and rounded, likely tumbled by water in a stream or beach environment.

Uses & applications

Common quartz is used in glassmaking, abrasives, and construction. Smooth pebbles like this are often used in landscaping or decorative displays.

Geological facts

Quartz is the most abundant mineral found at Earth's surface. Iron oxidation within the cracks gives this piece its characteristic coloration.

Field identification & locations

Easily identified by its hardness (will scratch glass), conchoidal fracture (where not heavily smoothed), and lack of cleavage. Common in riverbeds and coastlines.