
metamorphic
Quartzite
Quartzite (primarily SiO2)
Hardness: 7 on Mohs scale. Color: Tan, brown, or yellowish (due to iron oxides); Luster: Vitreous to dull; Crystal structure: Hexagonal (microcrystalline); Cleavage: None; Specific gravity: 2.6-2.7.
- Hardness
- 7 on Mohs scale
- Color
- Tan, brown, or yellowish (due to iron oxides)
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 on Mohs scale. Color: Tan, brown, or yellowish (due to iron oxides); Luster: Vitreous to dull; Crystal structure: Hexagonal (microcrystalline); Cleavage: None; Specific gravity: 2.6-2.7.
Formation & geological history
Formed through the metamorphism of quartz-rich sandstone. High heat and pressure cause the quartz grains to recrystallize and fuse together, creating a very dense and durable rock.
Uses & applications
Used in construction for road ballast, floor tiles, and countertop surfaces. Also used in glass making and as a decorative stone in landscaping.
Geological facts
Quartzite is so tough that it often survives intense weathering better than other rocks. In the field, it will reliably scratch glass and even a steel knife blade.
Field identification & locations
Identify by its grainy, sugary texture and extreme hardness. It breaks through the quartz grains rather than around them, unlike its parent sandstone. Commonly found in folded mountain belts.
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