Rock Identifier
Basalt (Basalt (Aphanitic-to-porphyritic mafic volcanic rock)) — igneous
igneous

Basalt

Basalt (Aphanitic-to-porphyritic mafic volcanic rock)

Hardness: 6 (Mohs scale); Color: Dark grey to charcoal black; Luster: Dull to sub-metallic (when fresh); Structure: Fine-grained/Aphanitic (crystals not visible to the naked eye); Specific Gravity: 2.8–3.0

Hardness
6 (Mohs scale)
Color
Dark grey to charcoal black
Luster
Dull to sub-metallic (when fresh)
Identified More igneous

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Physical properties

Hardness: 6 (Mohs scale); Color: Dark grey to charcoal black; Luster: Dull to sub-metallic (when fresh); Structure: Fine-grained/Aphanitic (crystals not visible to the naked eye); Specific Gravity: 2.8–3.0

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava (mafic) at or very near the Earth's surface. It is the most common rock in Earth's crust, primarily making up the ocean floors.

Uses & applications

Extensively used in construction as crushed stone for road base, railroad ballast, and concrete aggregate. High-quality varieties are used for floor tiles, monuments, and stone carvings.

Geological facts

Basalt is not only the most common rock on Earth but also dominates the lunar maria (the dark patches on the moon) and much of the surface of Mars and Venus.

Field identification & locations

Identify by its heavy weight (relative to size), dark color, and fine-grained texture. It often shows 'vesicular' holes (trapped gas bubbles). Common in volcanic regions like the Pacific Northwest, Hawaii, and Iceland.