Obsidian specimen

Crystal & mineral guide

Obsidian

Volcanic glass (felsic)

IgneousVolcanicRock

Natural volcanic glass — historically prized for razor-sharp tools.

Identify Obsidian with RockScan

About Obsidian

Obsidian lacks a crystal lattice, so it breaks in curved conchoidal shells sharper than surgical steel. Snowflake obsidian contains cristobalite spherulites. Rainbow and sheen varieties show thin-film interference.

Obsidian belongs in a crystal identifier workflow because photo cues — color zoning, crystal habit, and surface luster — combine with measurable traits like Mohs 5–5.5 and specific gravity 2.3–2.6. Use RockScan’s camera to get a first-pass ID, then confirm with the checklist below.

Obsidian properties

Mohs hardness5–5.5
Crystal systemAmorphous
LusterVitreous
ColorBlack; also mahogany, snowflake, rainbow
CompositionSilica-rich volcanic glass
FormationRapid cooling of high-silica lava
OccurrenceUSA (Oregon, California), Mexico, Iceland, Japan
Specific gravity2.3–2.6
CleavageNone (conchoidal fracture)

How to identify Obsidian

  1. Glassy luster and curved fracture
  2. Softer than quartz (scratched by steel sometimes)
  3. Often jet black and opaque in hand specimen

Collector notes

  • Used by ancient cultures for blades and mirrors
  • Not a true mineral because it is non-crystalline

Value context: Specialty sheens and large clean carvings drive collector interest.

Obsidian FAQ

How do you identify Obsidian?

Obsidian (Volcanic glass (felsic)) is typically recognized by black; also mahogany, snowflake, rainbow color, vitreous luster, Mohs hardness 5–5.5, and amorphous crystal system. RockScan can suggest Obsidian from a photo and surface these checks on the result card.

What is Obsidian made of?

Obsidian composition: Silica-rich volcanic glass. It forms via rapid cooling of high-silica lava and is found in USA (Oregon, California), Mexico, Iceland, Japan.

Is Obsidian valuable?

Specialty sheens and large clean carvings drive collector interest.