Rock Identifier
Quartzite (or Milky Quartz pebble) (Quartzite (Metamorphosed Sandstone) / Silicon Dioxide (SiO2)) — metamorphic
metamorphic

Quartzite (or Milky Quartz pebble)

Quartzite (Metamorphosed Sandstone) / Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: White, light gray, or tan; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal (microcrystalline); Cleavage: None; Specific gravity: 2.65.

Hardness
7 (Mohs scale)
Color
White, light gray, or tan
Luster
Vitreous to dull
Identified More metamorphic

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Physical properties

Hardness: 7 (Mohs scale); Color: White, light gray, or tan; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal (microcrystalline); Cleavage: None; Specific gravity: 2.65.

Formation & geological history

Formed from the metamorphism of quartz-rich sandstone under intense heat and pressure, typically during mountain-building events. Geological age can range from Precambrian to Cenozoic depending on location.

Uses & applications

Used widely in construction as crushed stone for road bases, railway ballast, and as a raw material for glass manufacturing. Highly durable for landscaping.

Geological facts

Quartzite is so hard and chemically resistant that it often forms the tops of ridges and mountains because it resists weathering better than surrounding rocks. It can be distinguished from marble because it will not react with acid.

Field identification & locations

Identify in the field by its ability to scratch glass and its grainy, sandpaper-like texture that has been 'welded' into a smooth, hard mass. Commonly found in metamorphic belts and as river-worn pebbles.