How to identify Quartzite
Metamorphic rock, primarily composed of quartz
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Open the appTo correctly identify Quartzite (Metamorphic rock, primarily composed of quartz), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Typically white or light gray, but can be pink, red, yellow, green, or blue due to impurities. Pure quartzite is white.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) to greasy on freshly broken surfaces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Granular, sugary, interlocking crystalline texture. Original clastic grains are obliterated.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Anhedral, interlocking quartz grains, typically equigranular.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
No true cleavage. Exhibits conchoidal to splintery fracture, breaking across the quartz grains.
- 6
Geological Environment
The rock formation and setting where it occurs
Formed in regions of intense heat and pressure, such as convergent plate boundaries (orogenic belts) or areas affected by deep burial and contact metamorphism. Often found in ancient mountain ranges and cratonic shields.
Key Facts
- Hardness
- 7 on the Mohs scale
- Specific Gravity
- 2.65 g/cm³ (for pure quartz)
- Crystal System
- Trigonal (for quartz mineral)
- Color
- White, gray, pink, red, yellow, green, blue
- Luster
- Vitreous to greasy
- Transparency
- Translucent to opaque
- Fracture
- Conchoidal to splintery
- Cleavage
- None (breaks across grains)
- Composition
- Primarily quartz (SiO2), typically >90-95%.
Physical characteristics
- Crystal Habit: Massive, granular, interlocking anhedral grains.
- Cleavage Type: None. Quartz itself has no cleavage.
- Fracture Type: Conchoidal to splintery, breaking through the quartz grains.
- Tenacity: Brittle
- Luster Type: Vitreous (glassy) to greasy
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