Iridescent Obsidian Identification Guide
How to identify iridescent (rainbow/sheen) obsidian by its glassy fracture, internal sheen from microscopic inclusions, and how it differs from labradorite and glass.
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What Iridescent Obsidian Looks Like
Iridescent obsidian is volcanic glass that displays a metallic sheen or rainbow play of color when light hits aligned microscopic inclusions (often nanoscale magnetite crystals or gas bubbles arranged in flow layers). At rest it looks like ordinary black obsidian; tilted to the light, bands of gold, green, violet, or full spectrum appear.
- Color: base is black to dark brown; sheen colors include gold, silver, green, blue, violet, or rainbow
- Luster: vitreous (glassy), high
- Transparency: translucent on thin edges, otherwise opaque
- Form: massive, no crystals — it is amorphous glass with conchoidal (shell-like) fracture
Step-by-Step Field-ID Checklist
- Confirm it's glass. Look for conchoidal fracture — smooth, curved, shell-like breaks with razor edges. This is the hallmark of obsidian.
- Tilt under a single light source. The sheen or rainbow should sweep across the surface as you rotate it, then vanish at other angles. The color lives inside the stone, not on the surface.
- Check the base color by looking at a thin edge against bright light — usually translucent grey-brown.
- Feel the weight and warmth. Obsidian is glass: it feels relatively light and warms in the hand faster than crystalline stone.
- Test hardness — about 5–5.5; it will scratch with a steel file and can scratch glass marginally.
Key Diagnostic Tests
- Mohs hardness: 5–5.5
- Streak: white
- Fracture: conchoidal — diagnostic for volcanic glass
- Cleavage: none (amorphous)
- Specific gravity: ~2.35–2.6 (low, glassy feel)
- Magnetism: generally none macroscopically, though magnetite nanoparticles cause the sheen
- No acid reaction
Common Look-Alikes and How to Tell Them Apart
- Labradorite / spectrolite: also flashes color, but labradorite is a crystalline feldspar with cleavage planes (flat reflective faces) and is harder (6–6.5). Obsidian has no cleavage and fractures conchoidally.
- Manmade slag glass / 'goldstone': goldstone shows tiny uniform copper sparkles throughout, not a directional sheen, and often has a too-perfect, evenly speckled look. Slag glass may show mold seams or bubbles in regular patterns.
- Black tourmaline or hematite: these are crystalline with no internal rainbow sheen and (for hematite) a red-brown streak.
- Rainbow moonstone: translucent white body with blue adularescence, not a black glassy base.
Where Iridescent Obsidian Is Found
Obsidian forms where felsic (rhyolitic) lava cools too fast to crystallize. Iridescent and rainbow varieties come notably from Mexico (Jalisco), the western USA (Oregon, Arizona, Glass Buttes), and Armenia. Sheen-grade material is selected and oriented by cutters to maximize the optical effect.
Frequently asked questions
How can you tell if it's real iridescent obsidian?
Look for conchoidal (shell-like) fracture and a glassy luster, then tilt it under one light source: the rainbow or metallic sheen should sweep across and disappear from inside the stone. A translucent dark edge and Mohs ~5–5.5 hardness confirm it.
What causes the rainbow sheen in iridescent obsidian?
The sheen comes from light reflecting off layers of microscopic inclusions—typically nanoscale magnetite crystals or aligned gas bubbles—frozen into the volcanic glass as it cooled. Light interference across these layers produces the color play.
Iridescent obsidian vs labradorite — what's the difference?
Labradorite is a crystalline feldspar with flat cleavage planes and Mohs 6–6.5 hardness; its flash (labradorescence) reflects off internal twin layers. Obsidian is amorphous glass with no cleavage, conchoidal fracture, and a softer 5–5.5 hardness.
Is iridescent obsidian natural or manmade?
Genuine iridescent obsidian is natural volcanic glass. Beware of manmade slag glass and goldstone sold as obsidian—these show uniform speckles or mold bubbles rather than a directional internal sheen and conchoidal fracture.
Iridescent Obsidian identified by the community
Recent Iridescent Obsidian specimens identified with Rock Identifier.