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How to identify Snowflake Obsidian

Volcanic glass with spherulites of cristobalite

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To correctly identify Snowflake Obsidian (Volcanic glass with spherulites of cristobalite), 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

    Dark (black, dark gray, sometimes dark brown) with white to grayish-white 'snowflake' patterns.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to sub-vitreous.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Aphanitic (glassy) matrix with visible spherulitic inclusions. Smooth to the touch, but can feel slightly granular where spherulites are prominent.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Amorphous (glassy) matrix; spherulites are microcrystalline radial aggregates of cristobalite.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None (amorphous glass).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Associated with silicic volcanic eruptions, typically found in lava flows, domes, and volcanic necks where rapid cooling of high-silica magma occurred.

Key Facts

Hardness
5-5.5 on Mohs scale (for the glass matrix); cristobalite is slightly harder at 6-7.
Specific Gravity
2.35-2.60 g/cm³
Crystal System
Amorphous (glass) for the matrix; spherulites are microcrystalline aggregates of cristobalite (tetragonal or orthorhombic at room temperature, but formed as high-temperature cubic polymorph).
Color
Black, dark gray, or dark brown with white to grayish-white spherulites.
Luster
Vitreous (glassy).
Transparency
Opaque to translucent on thin edges.
Fracture
Conchoidal (for the glass matrix).
Cleavage
None.
Composition
Primarily SiO2 (70-75%), with minor amounts of Al2O3, Fe2O3, MgO, CaO, Na2O, K2O, and H2O. The spherulites are composed of cristobalite (SiO2).

Physical characteristics

  • Crystal Habit: Amorphous (glassy) matrix; spherulites are radial aggregates of microcrystalline cristobalite.
  • Cleavage Type: None.
  • Fracture Type: Conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy).

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