How to identify Mahogany Obsidian
Volcanic glass (silica-rich)
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Open the appTo 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
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
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, conchoidal fracture surfaces. Amorphous, non-crystalline.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Amorphous; lacks crystal form. Occurs as massive flows, nodules, or fragments.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None. Exhibits conchoidal fracture.
- 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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