Rock Identifier
Basalt (Mafic Igneous Rock (primarily Plagioclase Feldspar and Pyroxene)) — igneous
igneous

Basalt

Mafic Igneous Rock (primarily Plagioclase Feldspar and Pyroxene)

Hardness: 6 (Mohs scale); Color: Black to dark grey; Luster: Dull to sub-metallic; Crystal Structure: Aphanitic (fine-grained) to porphyritic; Cleavage: None (conchoidal fracture); Specific Gravity: 2.8–3.0

Hardness
6 (Mohs scale)
Color
Black to dark grey
Luster
Dull to sub-metallic
Identified More igneous

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Physical properties

Hardness: 6 (Mohs scale); Color: Black to dark grey; Luster: Dull to sub-metallic; Crystal Structure: Aphanitic (fine-grained) to porphyritic; Cleavage: None (conchoidal fracture); Specific Gravity: 2.8–3.0

Formation & geological history

Formed from the rapid cooling of low-viscosity magnesium-rich and iron-rich lava (mafic lava) at or very near the Earth's surface. Most commonly formed at mid-ocean ridges and hotspots.

Uses & applications

Extensively used in construction as crushed stone for road base, railroad ballast, and concrete aggregate. High-quality specimens are used for 'hot stone' massage therapy and as decorative landscaping stones.

Geological facts

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

Field identification & locations

Identify by its dark color, heavy weight (relative to size), and fine-grained texture. Commonly found in volcanic regions, riverbeds near volcanic flows, and along coastlines. It often shows 'vesicles' (gas bubbles) or a smooth, water-worn appearance like this specimen.