Rock Identifier
Basalt (Mafic Volcanic Basalt (Major minerals: Plagioclase feldspar, Pyroxene; Minor: Olivine, Magnetite)) — igneous
igneous

Basalt

Mafic Volcanic Basalt (Major minerals: Plagioclase feldspar, Pyroxene; Minor: Olivine, Magnetite)

Hardness: 6 (Mohs scale); Color: Dark gray to black; Luster: Dull/earthy; Crystal Structure: Aphanitic (fine-grained, crystals not visible to eye); Cleavage: None (conchoidal/irregular fracture); Specific Gravity: 2.8–3.0

Hardness
6 (Mohs scale)
Color
Dark gray to black
Luster
Dull/earthy
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/earthy; Crystal Structure: Aphanitic (fine-grained, crystals not visible to eye); Cleavage: None (conchoidal/irregular 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 moon. Most basalt on Earth is less than 150 million years old due to tectonic recycling.

Uses & applications

Used extensively in construction as crushed stone for road bases, concrete aggregate, and railroad ballast. Denser varieties are used for high-end countertops or in 'stone therapy' massages due to heat retention.

Geological facts

Basalt is the most common rock type in the Earth's crust, making up almost most of the ocean floor. It is also common on the Moon, Mars, and Venus, where it forms the dark 'seas' known as lunar maria.

Field identification & locations

Identify in the field by its distinctive dark color, heavy weight (density), and fine-grained texture. It often weathers to a reddish or brownish crust. Commonly found in volcanic fields, oceanic islands (like Hawaii), and mid-ocean ridges.