Rock Identifier
Porphyritic Rhyolite (Red Porphyry) (Porphyritic Rhyolite (Felsic volcanic rock)) — igneous
igneous

Porphyritic Rhyolite (Red Porphyry)

Porphyritic Rhyolite (Felsic volcanic rock)

Hardness: 6-7 on Mohs scale; Color: Reddish-brown to maroon matrix with white or cream-colored phenocrysts; Luster: Dull to sub-vitreous; Structure: Porphyritic (fine-grained groundmass with larger visible crystals); Cleavage: None (conchoidal fracture); Specific Gravity: 2.4-2.6

Hardness
6-7 on Mohs scale
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Reddish-brown to maroon matrix with white or cream-colored phenocrysts; Luster: Dull to sub-vitreous; Structure: Porphyritic (fine-grained groundmass with larger visible crystals); Cleavage: None (conchoidal fracture); Specific Gravity: 2.4-2.6

Formation & geological history

Formed from the rapid cooling of silica-rich lava at or near the Earth's surface, where larger crystals (phenocrysts) began forming at depth before a secondary eruption caused a fine-grained matrix to solidify. Often dates from the Proterozoic to more recent volcanic eras.

Uses & applications

Used primarily as decorative stone, construction aggregate, and for lapidary work such as cabochons or polished river rocks. Historically used by Romans as 'Imperial Porphyry' for statues and pillars.

Geological facts

The term 'Porphyry' comes from the Ancient Greek word for purple. This rock's unique 'chocolate chip' appearance is caused by a two-stage cooling process of the magma.

Field identification & locations

Identify by looking for distinct, rectangular or blocky white feldspar crystals embedded in a hard, fine-grained reddish matrix. Commonly found in glaciated regions (as eratics), volcanic fields, and riverbeds in areas like the American Southwest, Egypt, or Northern Europe.