Rock Identifier
Scoria (Vesicular Basalt / Scoria (Mafic volcanic rock)) — igneous
igneous

Scoria

Vesicular Basalt / Scoria (Mafic volcanic rock)

Hardness: 5-6 (Mohs scale); Color: Dark reddish-brown to black; Luster: Dull/Earthy; Structure: Vesicular (highly porous/holey); Cleavage: None; Specific Gravity: 2.5-3.0 (though it feels light due to air pockets).

Hardness
5-6 (Mohs scale)
Color
Dark reddish-brown to black
Luster
Dull/Earthy
Identified More igneous

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Physical properties

Hardness: 5-6 (Mohs scale); Color: Dark reddish-brown to black; Luster: Dull/Earthy; Structure: Vesicular (highly porous/holey); Cleavage: None; Specific Gravity: 2.5-3.0 (though it feels light due to air pockets).

Formation & geological history

Formed through the rapid cooling of gas-rich mafic magma (lava) ejected from a volcano. The holes, or vesicles, are created by expanding gas bubbles trapped as the lava solidifies. It is usually associated with Cenozoic volcanic activity.

Uses & applications

Commonly used in landscaping (lava rock), gas grill briquettes, high-temperature insulation, drainage stones, and lightweight concrete aggregate. It is rarely used in jewelry due to its abrasive texture.

Geological facts

Scoria is different from pumice because it is mafic (rich in iron and magnesium) and denser; unlike pumice, scoria will usually sink in water. It is a primary component of 'cinder cones' found in volcanic fields.

Field identification & locations

Identify in the field by its distinct 'sponge-like' appearance, rough/sharp edges, and reddish-dark color. It is commonly found in volcanic regions such as the American Southwest, Iceland, and Hawaii.