Rock Identifier
Pumice (Basaltic/Scoria) (Vesicular Basalt / Scoria) — igneous
igneous

Pumice (Basaltic/Scoria)

Vesicular Basalt / Scoria

Hardness: 5-6 Mohs. Color: Dark grey to black. Luster: Dull/earthy. Crystal structure: Aphanitic/Vesicular (fine-grained with gas bubbles). Specific Gravity: 2.5-3.0 (heavier than light pumice due to iron).

Hardness
5-6 Mohs
Color
Dark grey to black
Luster
Dull/earthy
Identified More igneous
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Physical properties

Hardness: 5-6 Mohs. Color: Dark grey to black. Luster: Dull/earthy. Crystal structure: Aphanitic/Vesicular (fine-grained with gas bubbles). Specific Gravity: 2.5-3.0 (heavier than light pumice due to iron).

Formation & geological history

Formed from the rapid cooling of gas-rich mafic lava. As pressure drops during a volcanic eruption, gases dissolve out of the melt, creating bubbles (vesicles) that are frozen in place as the rock solidifies.

Uses & applications

Used in landscaping, high-temperature insulation, drainage in gardening, and as an abrasive in industrial grit and stone-washing textiles.

Geological facts

Unlike white rhyolitic pumice, dark scoria often sinks in water because its vesicle walls are thicker and denser. It is a primary component of 'lava rocks' used in gas grills.

Field identification & locations

Identify by its 'Swiss cheese' appearance and dark color. Common in volcanic regions like Hawaii, Iceland, and the Pacific Northwest. Collectors look for unique aerodynamic 'bomb' shapes.