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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Milky white to light tan; Luster: Vitreous to waxy (when water-worn); Crystal Structure: Hexagonal (though not visible in this water-worn state); Conchoidal fracture.

Hardness
7 on Mohs scale
Color
Milky white to light tan
Luster
Vitreous to waxy (when water-worn)
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Milky white to light tan; Luster: Vitreous to waxy (when water-worn); Crystal Structure: Hexagonal (though not visible in this water-worn state); Conchoidal fracture.

Formation & geological history

Formed from cooling magma or precipitation in hydrothermal veins. This specimen shows significant rounding, suggesting it was transported by water in a river or coastal environment, contributing to its smooth, ovoid shape.

Uses & applications

Industrial use in glassmaking and electronics (when pure); used in construction as aggregate; common in landscaping and as a pocket stone for collectors.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Its high hardness and chemical resistance allow it to survive long-term erosion that destroys other minerals.

Field identification & locations

Identified by its ability to scratch glass and smooth, waxy surface. It is ubiquitously found in riverbeds, beaches, and glacial till worldwide.