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How to identify Strawberry Quartz

Quartz (SiO2) with inclusions of hematite or goethite

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To correctly identify Strawberry Quartz (Quartz (SiO2) with inclusions of hematite or goethite), 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

    Pink, red, or orange, often with visible specks or needles of red/brown inclusions. The color is due to internal inclusions, not the quartz itself.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to greasy on fractured surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth when polished; rough to granular on unpolished surfaces, depending on crystal habit.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically occurs as prismatic hexagonal crystals, often terminated, or in massive, anhedral forms. Inclusions are visible within the quartz matrix.

  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

    Hydrothermal veins, pegmatites, and vugs within igneous and metamorphic rocks. It is found in environments where silica-rich fluids interact with iron-bearing minerals, leading to the co-precipitation or inclusion of iron oxides during quartz growth.

Key Facts

Hardness
7 (Mohs scale)
Specific Gravity
2.65 g/cm³
Crystal System
Trigonal
Color
Colorless to white quartz with pink, red, or orange inclusions.
Luster
Vitreous
Transparency
Transparent to translucent
Fracture
Conchoidal
Cleavage
None
Composition
Silicon dioxide (SiO2) with inclusions of hematite (Fe2O3) or goethite (FeO(OH)).

Physical characteristics

  • Crystal Habit: Prismatic hexagonal crystals, often terminated; also massive, granular, or cryptocrystalline aggregates.
  • Cleavage Type: None (lacks cleavage planes).
  • Fracture Type: Conchoidal (shell-like, curved fractures).
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy) on crystal faces and fresh fractures; sometimes greasy on massive varieties.

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