Rock Identifier
Quartzite (Quartzite (primarily SiO2)) — metamorphic
metamorphic

Quartzite

Quartzite (primarily SiO2)

Hardness: 7 (Mohs scale); Color: White, tan, or grey with dark mineral streaks; Luster: Vitreous to dull; Structure: Granoblastic, non-foliated; Cleavage: None (conchoidal fracture); SG: 2.6-2.7

Hardness
7 (Mohs scale)
Color
White, tan, or grey with dark mineral streaks
Luster
Vitreous to dull
Identified More metamorphic
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Physical properties

Hardness: 7 (Mohs scale); Color: White, tan, or grey with dark mineral streaks; Luster: Vitreous to dull; Structure: Granoblastic, non-foliated; Cleavage: None (conchoidal fracture); SG: 2.6-2.7

Formation & geological history

Formed from the metamorphism of quartz-rich sandstone under high heat and pressure. This specimen shows water-worn rounding, likely originating from a riverbed or coastal environment.

Uses & applications

Used in construction as road ballast, railway ballast, and decorative stone. Highly pure quartzite is used to produce silica for glassmaking and silicon industrial products.

Geological facts

Quartzite is so tough that it often outlasts the surrounding rock in mountain ranges, forming prominent ridges and peaks. It is distinguished from sandstone because it breaks through the grains rather than around them.

Field identification & locations

Identify in the field by its extreme hardness (cannot be scratched by a steel knife) and its grainy but fused texture. It is extremely common in ancient mountain belts and glacial till.