Rock Identifier
Scoria (Lava Rock) (Vesicular Basalt / Scoria) — igneous
igneous

Scoria (Lava Rock)

Vesicular Basalt / Scoria

Hardness: 5-6 (Mohs scale); Color: Black to dark grey; Luster: Dull/Earthy; Structure: Highly vesicular (pitted with air bubbles); Specific Gravity: 0.8 to 2.1 (often floats temporarily)

Hardness
5-6 (Mohs scale)
Color
Black to dark grey
Luster
Dull/Earthy
Identified More igneous

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Physical properties

Hardness: 5-6 (Mohs scale); Color: Black to dark grey; Luster: Dull/Earthy; Structure: Highly vesicular (pitted with air bubbles); Specific Gravity: 0.8 to 2.1 (often floats temporarily)

Formation & geological history

Formed from gas-rich mafic magma cooling rapidly during a volcanic eruption. The 'holes' are created by trapped gas bubbles (vesicles) as the lava solidifies. It is usually from the Cenozoic era or younger in active volcanic regions.

Uses & applications

Commonly used for landscaping (lava rocks), gas grill heating stones, high-temperature insulation, and lightweight concrete aggregate.

Geological facts

Unlike pumice, which is also vesicular, scoria is denser and will usually sink in water eventually. It is a major component of volcanic cinder cones.

Field identification & locations

Identify in the field by its very light weight relative to appearance, rough/sharp texture, and dark color. Common in volcanic fields like those in Hawaii, Iceland, and the Western United States.