Rock Identifier
Basalt (Mafic Igneous Rock (composed of plagioclase feldspar and pyroxene)) — igneous
igneous

Basalt

Mafic Igneous Rock (composed of plagioclase feldspar and pyroxene)

Hardness: 6 (Mohs scale); Color: Dark grey to black, weathering to rust-brown; Luster: Dull/earthy; Crystal Structure: Aphanitic (fine-grained); Specific Gravity: 2.8 - 3.0.

Hardness
6 (Mohs scale)
Color
Dark grey to black, weathering to rust-brown
Luster
Dull/earthy
Identified More igneous

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Physical properties

Hardness: 6 (Mohs scale); Color: Dark grey to black, weathering to rust-brown; Luster: Dull/earthy; Crystal Structure: Aphanitic (fine-grained); Specific Gravity: 2.8 - 3.0.

Formation & geological history

Formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic) at the Earth's surface or on the ocean floor. Most basaltic formations date from various Cenozoic volcanic events to the present day.

Uses & applications

Extensively used in construction as an aggregate for road bases and concrete. In industry, it is melted to create stone wool insulation. Also used as floor tiles and for landscaping.

Geological facts

Basalt is the most common rock type in the Earth's crust, covering most of the ocean floor. The dark patches on the Moon (the Lunar Maria) are also composed of basaltic lava flows.

Field identification & locations

Identify in the field by its dark color, heavy weight (relative to size), and very fine grain where individual crystals are not visible to the naked eye. Often exhibits 'desert varnish' or a pitted texture if weathered. Commonly found in volcanic regions and along oceanic ridges.