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

Vesicular Basalt

Extrusive Mafic Igneous Rock (Vesicular Basalt)

Hardness: 5-6 Mohs; Color: dark grey to brownish-black; Luster: dull to sub-metallic; Crystal structure: Aphanitic (fine-grained) with vesicles; Density: High specific gravity for the matrix.

Hardness
5-6 Mohs
Color
dark grey to brownish-black
Luster
dull to sub-metallic
Identified More igneous

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Physical properties

Hardness: 5-6 Mohs; Color: dark grey to brownish-black; Luster: dull to sub-metallic; Crystal structure: Aphanitic (fine-grained) with vesicles; Density: High specific gravity for the matrix.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at the earth's surface. The 'holes' (vesicles) are created by gas bubbles that were trapped in the lava as it solidified.

Uses & applications

Used in landscaping (lava rock), construction aggregate, road base, and as an abrasive in industrial applications.

Geological facts

Basalt is the most common rock type in the Earth's crust and makes up most of the ocean floor. Small vesicular specimens like this are often mistaken for meteorites by amateur collectors due to their weight and appearance.

Field identification & locations

Identify in the field by its dark color, heavy weight (relative to size, unless very porous), and the presence of small spherical or ovoid voids. Found in volcanic regions like Hawaii, Iceland, and the Pacific Northwest.