igneous
Rhyolite
Rhyolite (Extrusive Felsic Igneous Rock)
Hardness: 6-7 (Mohs scale); Color: Gray, reddish-brown, pink, or tan; Luster: Dull (aphanitic/fine-grained) to vitric (if glass-rich); Crystal structure: Microcrystalline to porphyritic; Specific gravity: 2.4-2.6.
- Hardness
- 6-7 (Mohs scale)
- Color
- Gray, reddish-brown, pink, or tan
- Luster
- Dull (aphanitic/fine-grained) to vitric (if glass-rich)
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Physical properties
Hardness: 6-7 (Mohs scale); Color: Gray, reddish-brown, pink, or tan; Luster: Dull (aphanitic/fine-grained) to vitric (if glass-rich); Crystal structure: Microcrystalline to porphyritic; Specific gravity: 2.4-2.6.
Formation & geological history
Formed from the rapid cooling of high-silica (felsic) lava at or near the Earth's surface. These lavas are usually very viscous, preventing large crystals from growing. Often associated with continental volcanic activity throughout various geological ages.
Uses & applications
Used primarily in crushed stone and construction aggregate. Occasionally used as decorative stones or for stone tools in prehistoric times. High-quality varieties like 'Rainforest Jasper' (a type of rhyolite) are used in jewelry.
Geological facts
Rhyolite has the same chemical composition as granite but cooled much faster. If rhyolite lava cools almost instantly, it becomes obsidian; if it is gas-charged and cools quickly, it becomes pumice.
Field identification & locations
Identify in the field by its light color (felsic composition), rough texture, and potential presence of small phenocrysts (embedded crystals) or flow banding. Common in volcanic regions with explosive history.
