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How to identify Amethyst

SiO2 (Quartz variety)

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To correctly identify Amethyst (SiO2 (Quartz variety)), 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

    Ranges from pale lilac to deep violet-purple. Color zoning (uneven distribution of color) is common.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy).

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly rough on crystal faces, conchoidal fracture surfaces.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically forms as hexagonal prisms terminating in rhombohedral faces (pyramidal). Can also be massive or granular.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None (lacks cleavage).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in hydrothermal veins, pegmatites, and especially in geodes and vugs within volcanic rocks (e.g., basalt) and granitic intrusions.

Key Facts

Hardness
7 (Mohs scale)
Specific Gravity
2.65 g/cm³
Crystal System
Trigonal
Color
Violet, purple, often with color zoning
Luster
Vitreous
Transparency
Transparent to translucent
Fracture
Conchoidal
Cleavage
None
Composition
Silicon dioxide (SiO2)

Physical characteristics

  • Crystal Habit: Prismatic, often terminated by rhombohedral faces; also massive, granular, drusy.
  • Cleavage Type: None (lacks cleavage).
  • Fracture Type: Conchoidal (shell-like, curved breaks).
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy).

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