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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Grayish-tan, translucent to opaque; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.

Hardness
7 on Mohs scale
Color
Grayish-tan, translucent to opaque
Luster
Vitreous to dull
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Grayish-tan, translucent to opaque; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.

Formation & geological history

Formed in various geological environments including cooling magma (igneous), precipitation from hydrothermal veins, or as grains in sedimentary deposits. This specific pebble likely achieved its rounded shape through river or coastal erosion.

Uses & applications

Small common pebbles are used as aggregate in construction, landscaping, and industrial abrasives. High-purity quartz is used in electronics and glassmaking.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to chemical and physical weathering, which is why it often remains as pebbles after other minerals have eroded away.

Field identification & locations

Identify in the field by its hardness (it can scratch glass) and lack of cleavage. Common in riverbeds, beaches, and soil worldwide.