Rock Identifier
Basalt (Aphanitic Mafic Igneous Rock) — igneous
igneous

Basalt

Aphanitic Mafic Igneous Rock

Hardness: 5-6 Mohs; Color: dark grey to black or greenish-grey; Luster: dull to sub-metallic; Crystal Structure: fine-grained (aphanitic) or porphyritic; Cleavage: none; Specific Gravity: 2.8-3.0

Hardness
5-6 Mohs
Color
dark grey to black or greenish-grey
Luster
dull to sub-metallic
Identified More igneous

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Physical properties

Hardness: 5-6 Mohs; Color: dark grey to black or greenish-grey; Luster: dull to sub-metallic; Crystal Structure: fine-grained (aphanitic) or porphyritic; Cleavage: none; Specific Gravity: 2.8-3.0

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava exposed at or very near the surface of a terrestrial planet or moon. Most terrestrial specimens are less than 200 million years old due to tectonic recycling.

Uses & applications

Extensively used in construction for aggregate, road base, railroad ballast, and high-quality concrete. Also used for high-temperature stone wool insulation and occasionally carved into monuments.

Geological facts

Basalt is the most common rock type in the Earth's crust and makes up most of the ocean floor. It is also common on the Moon, Mars, and Venus.

Field identification & locations

Identify in the field by its dark color, heavy weight (relative to size), and fine-grained texture. It often shows columnar jointing or vesicular (pitted) surfaces if formed with gas bubbles.