Rock Identifier
Porphyritic Basalt or Porphyry (Porphyritic Igneous Rock) — igneous
igneous

Porphyritic Basalt or Porphyry

Porphyritic Igneous Rock

Hardness of 6 on the Mohs scale, dark grey to black groundmass with lighter plagioclase or quartz phenocrysts, dull to sub-vitreous luster, fine-grained with larger embedded crystals, specific gravity around 2.8 to 3.0.

Identified More igneous
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Physical properties

Hardness of 6 on the Mohs scale, dark grey to black groundmass with lighter plagioclase or quartz phenocrysts, dull to sub-vitreous luster, fine-grained with larger embedded crystals, specific gravity around 2.8 to 3.0.

Formation & geological history

Formed through a two-stage cooling process in volcanic or subvolcanic environments, where magma cools slowly at depth forming large crystals (phenocrysts) before erupting and cooling rapidly to form a fine-grained matrix.

Uses & applications

Used primarily as crushed stone in construction, road aggregate, and sometimes as a decorative building stone or for lapidary purposes.

Geological facts

The distinctive contrast between the large phenocrysts and the fine matrix makes porphyry historically significant, famously used by Roman emperors for imperial monuments and sarcophagi due to its rich purple-red or dark coloration.

Field identification & locations

Easily identified by distinct, lighter-colored mineral crystals embedded in a dark, fine-grained background. Commonly found in volcanic regions, ancient orogens, and glacial drift.