Rock Identifier
Basalt (Basalt (Aphanitic-fine grained mafic igneous rock)) — igneous
igneous

Basalt

Basalt (Aphanitic-fine grained mafic igneous rock)

Hardness: 6 (Mohs scale); Color: Dark gray to black; Luster: Dull to sub-metallic; Crystal structure: Microcrystalline (aphanitic), typically consisting of plagioclase feldspar and pyroxene; Cleavage: None (conchoidal fracture); Specific gravity: 2.8–3.0.

Hardness
6 (Mohs scale)
Color
Dark gray to black
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 (Mohs scale); Color: Dark gray to black; Luster: Dull to sub-metallic; Crystal structure: Microcrystalline (aphanitic), typically consisting of plagioclase feldspar and pyroxene; Cleavage: None (conchoidal fracture); 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 a moon. Most basalt on Earth is formed at mid-ocean ridges. It can range from modern flows to billions of years old.

Uses & applications

Commonly used in construction for aggregate in concrete and asphalt, road base, and railroad ballast. In jewelry, it is occasionally used as 'lava stone' beads. In industry, it is melted to create basalt fiber and stone wool insulation.

Geological facts

Basalt is the most common rock type in the Earth's crust and covers most of the ocean floor. It is also the primary volcanic rock on Mars and the Moon (the lunar 'maria' or dark seas are basaltic plains).

Field identification & locations

Identify in the field by its dark color, heavy weight (relative to size due to high iron content), and very fine crystalline grain. It is found globally in volcanic regions such as Iceland, Hawaii, and the Pacific Northwest. Collectors look for vesicular basalt (containing gas bubbles) or specimens with olivine inclusions.