Rock Identifier
Quartz (Milky Quartz / Quartzite) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (Milky Quartz / Quartzite)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Milky white with orange/brown iron staining; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Hardness
7 on Mohs scale
Color
Milky white with orange/brown iron staining
Luster
Vitreous to waxy
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Milky white with orange/brown iron staining; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Formation & geological history

Formed through hydrothermal processes or within cooling igneous magma. This specific specimen appears to be a water-worn river pebble, likely hundreds of thousands to millions of years old, shaped by erosion in a high-energy aquatic environment.

Uses & applications

Used in electronics for piezoelectric properties, as an abrasive in sandblasting, in glassmaking, as a building aggregate, and as a common stone for tumbling and decorative landscaping.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the Greek word 'krustallos' meaning ice, because ancient philosophers believed quartz was ice that had frozen so hard it would never melt.

Field identification & locations

Identify in the field by its hardness (it will scratch glass and steel knives) and lack of cleavage planes. Pebbles like this are ubiquitous in riverbeds, glacial tills, and beaches globally; they are easy for novice collectors to find and polish.