Rock Identifier
Pumice (Vesicular Rhyolite / Pumice) — igneous
igneous

Pumice

Vesicular Rhyolite / Pumice

Hardness: 5-6 Mohs (though fragile), Color: light gray to tan/cream, Luster: dull to pearly (silky), Structure: highly vesicular (pitted/porous), Cleavage: none, Specific Gravity: 0.25 to 0.70 (often floats in water).

Identified More igneous

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Physical properties

Hardness: 5-6 Mohs (though fragile), Color: light gray to tan/cream, Luster: dull to pearly (silky), Structure: highly vesicular (pitted/porous), Cleavage: none, Specific Gravity: 0.25 to 0.70 (often floats in water).

Formation & geological history

Formed during explosive volcanic eruptions when highly pressurized, gas-rich magma is ejected. The rapid cooling and depressurization cause gases to expand rapidly, creating a frothy glass foam that hardens. Geological age varies by volcanic region.

Uses & applications

Used as an abrasive in soaps, foot care (pumice stones), and industrial polishing. Also used as a lightweight aggregate in concrete, as a soil conditioner in horticulture, and for stone-washing denim textiles.

Geological facts

Pumice is the only rock that consistently floats on water. Massive 'pumice rafts' created by underwater volcanoes have been known to drift across oceans for thousands of miles, sometimes impacting shipping lanes.

Field identification & locations

Identify in the field by its unusually light weight (low density) and the presence of numerous small holes (vesicles). It is commonly found in areas of past or present explosive volcanic activity, such as Italy, Greece, and the Western United States.