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

Quartz pebble

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: White/Tan; Luster: Vitreous to greasy; Crystal structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Hardness
7 (Mohs scale)
Color
White/Tan
Luster
Vitreous to greasy
Identified More mineral

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Physical properties

Hardness: 7 (Mohs scale); Color: White/Tan; Luster: Vitreous to greasy; Crystal structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Formation & geological history

Formed from the crystallization of silica-rich magma or from hydrothermal solutions. This specimen appears to be a water-worn river or beach pebble formed via erosion of primary quartz veins.

Uses & applications

Industrial uses include glassmaking, abrasives, and electronics. Small pebbles of this quality are used for landscaping or decorative gravel.

Geological facts

Quartz is one of the most abundant minerals in the Earth's crust. It is chemically stable at the Earth's surface, which is why it often remains as small pebbles after other minerals have weathered away.

Field identification & locations

Identify in the field by its hardness (will scratch glass) and lack of cleavage. Often found in stream beds, gravel pits, and beaches worldwide.