How to identify Obsidian
Obsidian
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Open the appTo correctly identify Obsidian (Obsidian), 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
Typically jet black, but can also be dark brown, dark green, or rarely red, blue, or iridescent (rainbow obsidian). The color is due to trace elements and inclusions.
- 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
Smooth, homogeneous, and glassy. May contain small phenocrysts (microlites) or gas bubbles, but generally lacks a crystalline texture.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Amorphous (non-crystalline).
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None. Exhibits characteristic conchoidal fracture.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in areas of recent volcanic activity where felsic lavas (rhyolite, dacite, andesite) have cooled rapidly. Common in lava flows, domes, and margins of dikes and sills.
Key Facts
- Hardness
- 5-6 on the Mohs scale
- Specific Gravity
- 2.35-2.60
- Crystal System
- Amorphous (lacks a crystal structure)
- Color
- Black, dark brown, dark green; rarely red, blue, or iridescent
- Luster
- Vitreous (glassy)
- Transparency
- Translucent to opaque, thin edges may be transparent
- Fracture
- Conchoidal (shell-like), producing extremely sharp edges
- Cleavage
- None
- Composition
- Primarily silicon dioxide (SiO2), typically 70-75% SiO2, with minor amounts of aluminum, sodium, potassium, iron, and magnesium oxides. It is essentially a supercooled liquid, not a true mineral.
Physical characteristics
- Crystal Habit: Amorphous masses, flow bands often visible
- Cleavage Type: None
- Fracture Type: Conchoidal, very sharp
- Tenacity: Brittle
- Luster Type: Vitreous (glassy)
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