How to identify Snowflake Obsidian
Volcanic glass with spherulites of cristobalite
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Open the appTo 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
Color
Overall color and any zoning or banding
Dark (black, dark gray, sometimes dark brown) with white to grayish-white 'snowflake' patterns.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) to sub-vitreous.
- 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
Crystal Form
Shape of visible crystals or crystal faces
Amorphous (glassy) matrix; spherulites are microcrystalline radial aggregates of cristobalite.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None (amorphous glass).
- 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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