Rock Identifier
Quartzite (Metamorphosed Quartz Sandstone (SiO2)) — metamorphic
metamorphic

Quartzite

Metamorphosed Quartz Sandstone (SiO2)

Mohs hardness: 7, Color: white to light tan, Luster: vitreous to dull, Crystal structure: trigonal (microcrystalline), Cleavage: none (conchoidal fracture), Specific gravity: 2.63-2.65

Identified More metamorphic
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Physical properties

Mohs hardness: 7, Color: white to light tan, Luster: vitreous to dull, Crystal structure: trigonal (microcrystalline), Cleavage: none (conchoidal fracture), Specific gravity: 2.63-2.65

Formation & geological history

Formed from the metamorphism of quartz sandstone under intense heat and pressure, typically during mountain-building events (orogeny). The individual quartz grains recrystallize into a locked mosaic.

Uses & applications

Used extensively in road construction, as railway ballast, in the manufacture of glass and ceramics, and as a durable countertop material.

Geological facts

Quartzite is so hard and chemically resistant that it often forms the caprocks of mountain ranges. It is harder than steel and will easily scratch glass.

Field identification & locations

Identify in the field by its extreme hardness and grainy texture that looks like sandpaper but feels smooth and vitreous on fresh breaks. It is found in mountain belts and ancient shield regions globally.