Rock Identifier
Basalt (Basalt (primarily composed of Plagioclase feldspar and Pyroxene)) — igneous
igneous

Basalt

Basalt (primarily composed of Plagioclase feldspar and Pyroxene)

Hardness: 6 on Mohs scale. Color: dark grey to black. Luster: dull to earthy. Crystal structure: fine-grained (aphanitic), often containing microscopic crystals. Specific gravity: 2.8–3.0.

Hardness
6 on Mohs scale
Color
dark grey to black
Luster
dull to earthy
Identified More igneous

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Physical properties

Hardness: 6 on Mohs scale. Color: dark grey to black. Luster: dull to earthy. Crystal structure: fine-grained (aphanitic), often containing microscopic crystals. 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. It can be found in oceanic crust and volcanic regions worldwide.

Uses & applications

Extensively used in construction for aggregate in road base, concrete, and railroad ballast. Also used as dimension stone for statues and architecture, and occasionally in jewelry as 'lava rock' beads.

Geological facts

Basalt is the most common rock type in the Earth's crust and makes up most of the ocean floors. It is also common on the Moon and Mars—the dark 'seas' on the Moon (Maria) are actually giant basaltic plains.

Field identification & locations

Identify in the field by its dark color, heavy weight (high density), and fine-grained texture with no visible large crystals. It often breaks with a conchoidal fracture. Commonly found in volcanic fields or near coastal areas with ancient lava flows.