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

Basalt

Basalt (Aphanitic Mafic Igneous Rock)

Hardness: 6.0 (Mohs); Color: Dark gray to black (often weathers to brown); Luster: Dull to sub-metallic; Crystal structure: Aphanitic (fine-grained); Cleavage: None; Specific gravity: 2.8–3.0.

Hardness
6
Color
Dark gray to black (often weathers to brown)
Luster
Dull to sub-metallic
Identified More igneous

Identify your own rocks.

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

Physical properties

Hardness: 6.0 (Mohs); Color: Dark gray to black (often weathers to brown); Luster: Dull to sub-metallic; Crystal structure: Aphanitic (fine-grained); Cleavage: None; Specific gravity: 2.8–3.0.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at or very near the Earth's surface. Most specimens found on the surface date from the Cenozoic era, though basaltic crust exists from various geological ages.

Uses & applications

Extensively used as aggregate in construction (road base, railroad ballast, concrete), as a raw material for stone wool insulation, and occasionally in ground-form as a soil supplement/fertilizer.

Geological facts

Basalt is the most common rock type in the Earth's crust and makes up the majority of the ocean floor. It is also found in abundance on the Moon (the dark 'Maria' plains) and Mars.

Field identification & locations

Identify in the field by its dark color, heavy weight (high density), and lack of visible crystals to the naked eye. Commonly found in volcanic fields or as river cobbles in areas with volcanic history.