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How to identify Quartz

Quartz

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To correctly identify Quartz (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. 1

    Color

    Overall color and any zoning or banding

    Highly variable; colorless, white, gray, purple (amethyst), yellow (citrine), pink (rose quartz), brown (smoky quartz), green, black. Often transparent to translucent.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to greasy.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Typically smooth to slightly rough on crystal faces; conchoidal fracture surfaces are smooth and curved.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Hexagonal prisms terminated by hexagonal pyramids. Often found as anhedral (irregular) grains in rocks or as massive aggregates. Well-formed crystals are common in vugs and veins.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Quartz exhibits conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Igneous rocks (granite, rhyolite, pegmatite), metamorphic rocks (gneiss, schist, quartzite), sedimentary rocks (sandstone, chert), hydrothermal veins, geodes, and as detrital grains in sediments.

Key Facts

Hardness
7 on the Mohs scale
Specific Gravity
2.65 g/cm³
Crystal System
Trigonal (low quartz) or Hexagonal (high quartz)
Color
Colorless, white, gray, purple, yellow, pink, brown, green, black
Luster
Vitreous to greasy
Transparency
Transparent to opaque
Fracture
Conchoidal
Cleavage
None
Composition
Silicon dioxide (SiO2)

Physical characteristics

  • Crystal Habit: Prismatic, massive, granular, cryptocrystalline (e.g., chalcedony). Well-formed crystals are typically hexagonal prisms terminated by rhombohedra (often appearing as hexagonal pyramids).
  • Cleavage Type: Absent. Quartz lacks cleavage.
  • Fracture Type: Conchoidal (shell-like), producing smooth, curved surfaces with sharp edges.
  • Tenacity: Brittle
  • Luster Type: Vitreous (glassy) on crystal faces; greasy on massive or fractured surfaces.

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