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How to identify Snowflake Obsidian

Volcanic Glass (Obsidian) with Cristobalite inclusions

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To correctly identify Snowflake Obsidian (Volcanic Glass (Obsidian) with Cristobalite inclusions), 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

    Black to dark gray groundmass with white to grayish-white 'snowflake' patterns.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) on fresh surfaces, duller on weathered surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth, conchoidal fracture. The 'snowflakes' are slightly rougher to the touch than the glassy matrix.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Amorphous (glassy) matrix with spherulitic (radial, spherical aggregates) cristobalite inclusions.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None (due to its amorphous nature).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in areas of recent felsic volcanic activity, typically associated with rhyolitic lava flows or domes.

Key Facts

Hardness
5-5.5 on the Mohs scale (for the glass matrix); cristobalite is slightly harder at 6-7.
Specific Gravity
2.35-2.50
Crystal System
Amorphous (glassy) for the obsidian matrix; Cristobalite is tetragonal (high-temperature form) or orthorhombic (low-temperature form).
Color
Black to dark gray with white to grayish-white inclusions.
Luster
Vitreous (glassy).
Transparency
Opaque to translucent in thin sections.
Fracture
Conchoidal (shell-like).
Cleavage
None.
Composition
Primarily SiO2 (silica) with minor amounts of Al2O3, Fe2O3, MgO, CaO, Na2O, K2O, and H2O. The 'snowflakes' are almost pure SiO2 (cristobalite).

Physical characteristics

  • Crystal Habit: Amorphous (glassy) matrix; cristobalite forms spherulitic aggregates.
  • Cleavage Type: Absent.
  • Fracture Type: Conchoidal, producing very sharp edges.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy).

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