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

Vesicular Basalt

Mafic Igneous Rock (primarily Plagioclase and Pyroxene)

Hardness: 5-6 Mohs. Color: Dark gray to black, often weathered to rusty brown. Luster: Dull/earthy until wet. Structure: Vesicular (contains air bubbles or gas pits). Density: High.

Hardness
5-6 Mohs
Color
Dark gray to black, often weathered to rusty brown
Luster
Dull/earthy until wet
Identified More igneous
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Physical properties

Hardness: 5-6 Mohs. Color: Dark gray to black, often weathered to rusty brown. Luster: Dull/earthy until wet. Structure: Vesicular (contains air bubbles or gas pits). Density: High.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava exposed at or very near the Earth's surface. The holes (vesicles) were formed by gas bubbles trapped in the cooling lava. Most basalt is relatively young geologically (Cenozoic era).

Uses & applications

Commonly used as crushed stone for road base, concrete aggregate, and railroad ballast. Decorative uses include landscaping rocks and aquarium decor.

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 on the Moon and Mars.

Field identification & locations

Look for a heavy, dark rock with numerous small pits or holes. Often found in volcanic regions or areas with ancient lava flows. It will not react with acid, unlike limestone.