Rock Identifier
Basalt with Vesicles (Vesicular Basalt (comprising Plagioclase Feldspar, Pyroxene, and Olivine)) — igneous
igneous

Basalt with Vesicles

Vesicular Basalt (comprising Plagioclase Feldspar, Pyroxene, and Olivine)

Hardness: 6.0 (Mohs scale); Color: Dark grey to black or brownish-red; Luster: Dull to earthy; Crystal structure: Aphanitic (fine-grained); Specific Gravity: 2.8–3.0; Contains vesicles (gas bubbles).

Hardness
6
Color
Dark grey to black or brownish-red
Luster
Dull to earthy
Identified More igneous

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Physical properties

Hardness: 6.0 (Mohs scale); Color: Dark grey to black or brownish-red; Luster: Dull to earthy; Crystal structure: Aphanitic (fine-grained); Specific Gravity: 2.8–3.0; Contains vesicles (gas bubbles).

Formation & geological history

Formed through the rapid cooling of magnesium-rich and iron-rich lava at the surface of a terrestrial planet or moon. The gas bubbles (vesicles) are trapped as the lava solidifies. Common in volcanic fields globally.

Uses & applications

Used in construction as crushed stone, for road base, concrete aggregate, and railroad ballast. Highly vesicular varieties (scoria) are used in landscaping and as thermal insulation.

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 the primary rock type on the Moon's maria and surface of Mars.

Field identification & locations

Identify in the field by its dark color, heavy weight (density), and the presence of small circular pits (holes) where gas was trapped. Frequently found in volcanic regions like Hawaii, Iceland, or the Pacific NW.