
metamorphic
Quartzite
Quartzite (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: yellowish-tan to white with iron staining; Luster: vitreous to dull; Crystal structure: hexagonal (microcrystalline); Cleavage: none (conchoidal fracture); Specific gravity: 2.63-2.65
- Hardness
- 7 on Mohs scale
- Color
- yellowish-tan to white with iron staining
- Luster
- vitreous to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: yellowish-tan to white with iron staining; Luster: vitreous to dull; Crystal structure: hexagonal (microcrystalline); Cleavage: none (conchoidal fracture); Specific gravity: 2.63-2.65
Formation & geological history
Formed from the metamorphism of quartz-rich sandstone under intense heat and pressure, typically during mountain-building events. This specimen shows significant rounding consistent with alluvial or river transport.
Uses & applications
Used primarily as crushed stone for road construction, railroad ballast, and as a raw material for glass and ceramics. Polished varieties are used for countertops and decor.
Geological facts
Quartzite is so tough that it often outlasts the surrounding stones during erosion, creating prominent ridges. It is harder and more durable than its parent rock, sandstone.
Field identification & locations
Identify in the field by its hardness (it will scratch glass) and its sugary, granular texture. Commonly found in riverbeds, glacial tills, and mountain ranges globally.
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