Rock Identifier
Vesicular Basalt (Extrusive Mafic Volcanic Rock) — igneous
igneous

Vesicular Basalt

Extrusive Mafic Volcanic Rock

Hardness: 5-6 Mohs. Color: dark gray to black, often weathering to reddish-brown. Luster: dull to sub-metallic. Texture: vesicular (pitted with gas bubbles). Composition: primarily plagioclase feldspar, pyroxene, and olivine.

Hardness
5-6 Mohs
Color
dark gray to black, often weathering to reddish-brown
Luster
dull to sub-metallic
Identified More igneous

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Physical properties

Hardness: 5-6 Mohs. Color: dark gray to black, often weathering to reddish-brown. Luster: dull to sub-metallic. Texture: vesicular (pitted with gas bubbles). Composition: primarily plagioclase feldspar, pyroxene, and olivine.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at or very near the Earth's surface. The pits (vesicles) are created by trapped gas bubbles that escaped as the lava solidified.

Uses & applications

Commonly used in construction as aggregate, road base, and railroad ballast. In landscaping, it is used for decorative stones and 'lava rocks' for grills. Some specimens are used for stone massage therapy.

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

Identify by its dark color, heavy weight (relative to size), and characteristic holes or 'vesicles'. It reacts poorly to acid and will not scratch glass easily. Commonly found in volcanic fields such as those in Iceland, Hawaii, and the Pacific Northwest.