Rock Identifier
Vesicular Basalt (Scoria) (Aphanitic Mafic Igneous Rock (Vesicular Basalt)) — igneous
igneous

Vesicular Basalt (Scoria)

Aphanitic Mafic Igneous Rock (Vesicular Basalt)

Hardness: 6.0; Color: Dark grey to reddish-black; Luster: Dull/Earthy; Structure: Vesicular (gas bubbles); Cleavage: None (conchoidal fracture); Specific Gravity: 2.8–3.0

Hardness
6
Color
Dark grey to reddish-black
Luster
Dull/Earthy
Identified More igneous

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Physical properties

Hardness: 6.0; Color: Dark grey to reddish-black; Luster: Dull/Earthy; Structure: Vesicular (gas bubbles); Cleavage: None (conchoidal fracture); Specific Gravity: 2.8–3.0

Formation & geological history

Formed during explosive volcanic eruptions or on the surface of lava flows when volcanic gases expand and get trapped in cooling magma during the Cenozoic era.

Uses & applications

Used in landscaping, lightweight concrete, gas grill lava rocks, drainage systems, and as an abrasive in stone-washing textiles.

Geological facts

The holes, called vesicles, are formed by gases coming out of solution as the magma depressurizes. If a specimen has enough holes, it can occasionally float on water briefly, though less so than pumice.

Field identification & locations

Identified by its swiss-cheese appearance and high density compared to pumice. Commonly found in volcanic regions like Hawaii, Iceland, and the Pacific Northwest.