igneous
Porphyritic Rhyolite
Rhyolite (Porphyritic texture)
Hardness: 6-7 (Mohs scale); Color: Reddish-brown groundmass with white/clear phenocrysts; Luster: Dull/earthy matrix with vitreous crystals; Structure: Aphanitic matrix with visible crystals (porphyritic); Cleavage: None (conchoidal fracture typical of silica-rich rocks).
- Hardness
- 6-7 (Mohs scale)
- Color
- Reddish-brown groundmass with white/clear phenocrysts
- Luster
- Dull/earthy matrix with vitreous crystals
Identified More igneous →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 6-7 (Mohs scale); Color: Reddish-brown groundmass with white/clear phenocrysts; Luster: Dull/earthy matrix with vitreous crystals; Structure: Aphanitic matrix with visible crystals (porphyritic); Cleavage: None (conchoidal fracture typical of silica-rich rocks).
Formation & geological history
Formed from the rapid cooling of silica-rich (felsic) lava at or near the Earth's surface. The large visible crystals (phenocrysts) grew slowly underground before the magma was erupted and the rest of the melt cooled quickly into a fine-grained matrix.
Uses & applications
Used primarily as decorative stone in landscaping, crushed stone for road construction, and occasionally in jewelry as 'wonderstone' or cabochons if the pattern is distinct.
Geological facts
Rhyolite is the volcanic equivalent of granite. The name comes from the Greek word 'rhyax', meaning a stream of lava. It is extremely high in silica (over 69%), making the lava very viscous.
Field identification & locations
Identify in the field by looking for a fine-grained, light-colored (pink, red, or tan) volcanic rock containing distinct, larger crystals of quartz or feldspar. Commonly found in continental volcanic arcs like the Rocky Mountains.
