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How to identify Mahogany Obsidian

Volcanic glass (silica-rich)

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To correctly identify Mahogany Obsidian (Volcanic glass (silica-rich)), 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 reddish-brown to black, often with swirling patterns or blotches of these colors. The red-brown is due to iron oxide inclusions.

  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

    Smooth, conchoidal fracture surfaces. Amorphous, non-crystalline.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Amorphous; lacks crystal form. Occurs as massive flows, nodules, or fragments.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Exhibits conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in areas of recent or geologically young volcanic activity, typically associated with rhyolitic lava flows, domes, and ignimbrites.

Key Facts

Hardness
5 to 5.5 on the Mohs scale.
Specific Gravity
2.35 to 2.60 g/cm³.
Crystal System
Amorphous (lacks a crystal system).
Color
Dark reddish-brown to black, often with swirling patterns.
Luster
Vitreous (glassy).
Transparency
Opaque to translucent in thin pieces.
Fracture
Conchoidal (shell-like, very sharp edges).
Cleavage
None.
Composition
Primarily silicon dioxide (SiO₂) with minor amounts of iron oxides (hematite, goethite) responsible for the color, and other trace elements.

Physical characteristics

  • Crystal Habit: Massive, amorphous, typically occurring as flows, nodules, or fragments.
  • Cleavage Type: None.
  • Fracture Type: Conchoidal, producing extremely sharp edges.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy).

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