Rock Identifier
Scoria (Vesicular Basaltic Glass) — igneous
igneous

Scoria

Vesicular Basaltic Glass

Hardness: 5-6 (Mohs scale); Color: dark red, brown, or black; Luster: dull to vitreous; Structure: vesicular (porous); Specific gravity: 0.8-2.1 (some float on water briefly, but most sink).

Hardness
5-6 (Mohs scale)
Color
dark red, brown, or black
Luster
dull to vitreous
Identified More igneous

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Physical properties

Hardness: 5-6 (Mohs scale); Color: dark red, brown, or black; Luster: dull to vitreous; Structure: vesicular (porous); Specific gravity: 0.8-2.1 (some float on water briefly, but most sink).

Formation & geological history

Formed from the rapid cooling of basaltic or andesitic magma containing high levels of dissolved gases which expand to create holes (vesicles). Commonly found in cinder cones and volcanic fields.

Uses & applications

Used extensively in landscaping, drainage systems, gas grills for heat retention, lightweight concrete manufacturing, and as abrasive traction for icy roads.

Geological facts

Scoria is often confused with pumice, but it is denser and has larger vesicles; it is the primary material that makes up cinder cone volcanoes.

Field identification & locations

Identify by its rough, sponge-like texture, dark color, and lightness relative to solid basalt. Commonly found in volcanic regions like Hawaii, Italy (Mount Etna), and the American Southwest.