How to identify Obsidian in Rhyolite
Volcanic glass (Obsidian) within a fine-grained felsic volcanic rock (Rhyolite)
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Open the appTo correctly identify Obsidian in Rhyolite (Volcanic glass (Obsidian) within a fine-grained felsic volcanic rock (Rhyolite)), 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
Obsidian: Typically black, dark brown, dark green, or rarely red/gray. Rhyolite: Light-colored, often pink, gray, white, or light brown.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Obsidian: Vitreous (glassy). Rhyolite: Dull to earthy, sometimes waxy if cryptocrystalline.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Obsidian: Amorphous, conchoidal fracture, smooth. Rhyolite: Aphanitic (fine-grained), sometimes porphyritic (with larger crystals in a fine matrix), often exhibits flow banding.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Obsidian: None (amorphous). Rhyolite: Microscopic crystals, sometimes phenocrysts of quartz, feldspar, or biotite.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Obsidian: None. Rhyolite: None (due to fine-grained nature).
- 6
Geological Environment
The rock formation and setting where it occurs
Volcanic domes, lava flows, caldera rims, and explosive eruption deposits in areas of felsic volcanism.
Key Facts
- Hardness
- Obsidian: 5-5.5 (Mohs); Rhyolite: 6-7 (due to quartz and feldspar content)
- Specific Gravity
- Obsidian: 2.35-2.50; Rhyolite: 2.3-2.6
- Crystal System
- Obsidian: Amorphous; Rhyolite: Cryptocrystalline to microcrystalline (no macroscopic crystal system)
- Color
- Obsidian: Black, dark brown, dark green; Rhyolite: Pink, gray, white, light brown
- Luster
- Obsidian: Vitreous; Rhyolite: Dull to earthy
- Transparency
- Obsidian: Opaque to translucent in thin pieces; Rhyolite: Opaque
- Fracture
- Obsidian: Conchoidal; Rhyolite: Irregular to subconchoidal
- Cleavage
- Obsidian: None; Rhyolite: None
- Composition
- Both are felsic, primarily SiO2 (typically >69 wt%), with minor Al2O3, K2O, Na2O, FeO, MgO, CaO. Obsidian is essentially supercooled liquid of rhyolitic composition.
Physical characteristics
- Crystal Habit: Obsidian: Amorphous, massive; Rhyolite: Aphanitic to porphyritic, massive, often flow-banded
- Cleavage Type: None for both
- Fracture Type: Obsidian: Conchoidal; Rhyolite: Irregular to subconchoidal
- Tenacity: Obsidian: Brittle; Rhyolite: Brittle
- Luster Type: Obsidian: Vitreous; Rhyolite: Dull to earthy
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