Rock Identifier
Porphyritic basalt (Basalt, likely plagioclase- and pyroxene-bearing) — igneous
igneous

Porphyritic basalt

Basalt, likely plagioclase- and pyroxene-bearing

AI-generated identification · may be incorrect

Dark gray-green, fine-grained volcanic rock with pale mineral grains or patches; typically Mohs 5–6, dull to faintly vitreous, with no obvious cleavage. Exact composition and texture are uncertain from the image alone.

Identified More igneous →
Explore Porphyritic basalt in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Dark gray-green, fine-grained volcanic rock with pale mineral grains or patches; typically Mohs 5–6, dull to faintly vitreous, with no obvious cleavage. Exact composition and texture are uncertain from the image alone.

Formation & geological history

Formed when iron- and magnesium-rich lava cooled at or near Earth’s surface; basalt occurs from many geological periods and settings, including oceanic crust and volcanic flows.

Uses & applications

Basalt is used as crushed aggregate, road stone, building stone, and occasionally for decorative objects; this small specimen is mainly suitable for collecting.

Geological facts

The light spots may be larger crystals embedded in a finer volcanic groundmass, a texture called porphyritic.

Field identification & locations

Look for a dense, dark, fine-grained rock with scattered pale crystals; basalt is common in volcanic regions worldwide. A hand lens and streak or hardness tests would help confirm identification.