How to identify Quartz
SiO 2
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Open the appTo correctly identify Quartz (SiO 2), 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
Colorless, white, milky, purple (amethyst), yellow (citrine), pink (rose quartz), brown (smoky quartz), green, black. Often transparent to translucent.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) to greasy.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to slightly rough, depending on crystal habit and fracture.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Typically forms hexagonal prisms terminating with hexagonal pyramids. Can also be massive, granular, cryptocrystalline (e.g., chalcedony), or botryoidal.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None. Exhibits conchoidal fracture.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in igneous rocks (granite, rhyolite, pegmatite), metamorphic rocks (gneiss, schist, quartzite), and sedimentary rocks (sandstone, chert). Common in hydrothermal veins and as detrital grains in sediments.
Key Facts
- Hardness
- 7 (Mohs scale)
- Specific Gravity
- 2.65 g/cm³
- Crystal System
- Trigonal (often appears hexagonal)
- Color
- Colorless, white, milky, purple, yellow, pink, brown, black, green
- Luster
- Vitreous to greasy
- Transparency
- Transparent to opaque
- Fracture
- Conchoidal
- Cleavage
- None
- Composition
- Silicon dioxide (SiO2)
Physical characteristics
- Crystal Habit: Prismatic (hexagonal), massive, granular, cryptocrystalline, drusy, botryoidal
- Cleavage Type: None
- Fracture Type: Conchoidal
- Tenacity: Brittle
- Luster Type: Vitreous (glassy) to greasy
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