Rock Identifier
Basalt with Iron Oxide staining (Mafic Igneous Rock (primarily Plagioclase and Pyroxene)) — igneous
igneous

Basalt with Iron Oxide staining

Mafic Igneous Rock (primarily Plagioclase and Pyroxene)

Hardness: 6.0; Color: Dark grey to black with reddish-brown oxidation; Luster: Dull to earthy; Structure: Fine-grained (aphanitic); Cleavage: None; Specific Gravity: 2.8-3.0.

Hardness
6
Color
Dark grey to black with reddish-brown oxidation
Luster
Dull to earthy
Identified More igneous

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Physical properties

Hardness: 6.0; Color: Dark grey to black with reddish-brown oxidation; Luster: Dull to earthy; Structure: Fine-grained (aphanitic); Cleavage: None; Specific Gravity: 2.8-3.0.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at or very near the Earth's surface. The orange-brown spots are due to the oxidation of iron minerals (weathering).

Uses & applications

Commonly used as aggregate in construction (roads/concrete), industrial stone, and occasionally for basalt fiber or landscaping.

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 common on the Moon and Mars.

Field identification & locations

Identify by its heavy weight relative to size, dark color, and lack of visible crystals. Commonly found in volcanic regions or as river stones.