Rock Identifier
Vesicular volcanic rock, likely weathered pumice or scoria (Pumice/scoria; predominantly volcanic glass and feldspar, with possible iron oxides) — igneous
igneous

Vesicular volcanic rock, likely weathered pumice or scoria

Pumice/scoria; predominantly volcanic glass and feldspar, with possible iron oxides

AI-generated identification · may be incorrect

Light tan, highly porous, dull to slightly earthy luster, and irregular vesicles; hardness roughly 5–6 for glassy material, though weathering makes it friable. Exact identification is limited by the photograph; pumice is usually very lightweight and may float, while scoria is darker and denser.

Identified More igneous
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Physical properties

Light tan, highly porous, dull to slightly earthy luster, and irregular vesicles; hardness roughly 5–6 for glassy material, though weathering makes it friable. Exact identification is limited by the photograph; pumice is usually very lightweight and may float, while scoria is darker and denser.

Formation & geological history

Forms when gas-rich lava erupts and rapidly cools, trapping bubbles in volcanic glass; likely Quaternary or younger, depending on locality. The cavities and tan alteration suggest substantial weathering or hydrothermal alteration.

Uses & applications

Used as lightweight aggregate, abrasive, landscaping stone, and occasionally in decorative collections; porous specimens may be sold as natural curiosities.

Geological facts

Its cellular texture records dissolved volcanic gases escaping during eruption. Pale, extremely lightweight material favors pumice; heavier, darker, iron-rich material favors scoria.

Field identification & locations

Test density, streak, and fresh surfaces: pumice may float, whereas scoria sinks; a fresh break should show glassy walls and abundant vesicles. Common around young volcanic fields, lava flows, and pyroclastic deposits.