Rock Identifier
Pumice (Vesicular volcanic glass (silicate, frothed))
igneous

Pumice

Vesicular volcanic glass (silicate, frothed)

A frothy, lightweight volcanic glass so full of gas bubbles that it can float on water.

Mohs hardness
5.5-6 (glass; very friable)
Color
White, grey, cream, or pale brown
Type
igneous

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Overview

Pumice is a highly vesicular volcanic glass, essentially a solidified foam of magma. It forms when gas-rich, silica-rich lava is ejected so violently that dissolved gases expand and the melt quenches before the bubbles can escape, trapping countless tiny voids.

The result is a rock so porous and lightweight that many pieces float on water, a property almost unique among rocks. It is usually pale, white to grey, and feels rough and abrasive.

Pumice is technically a glass rather than a crystalline rock, since it cools too fast for minerals to form. It is closely related to scoria, which is darker, denser, and has larger, less connected bubbles.

Formation & geology

Pumice forms during explosive eruptions of viscous, silica-rich (felsic) magmas such as rhyolite and dacite. As this gas-charged magma decompresses on eruption, dissolved water and gases come out of solution and expand rapidly, frothing the melt.

The foam is then chilled almost instantly to glass as it is blasted into the air or onto the surface, freezing in the bubble structure. Large eruptions can blanket regions in pumice and pumice ash (pumicite) and produce floating rafts of pumice on the sea.

Major sources include the volcanoes of Italy (Lipari), Greece (Santorini), Turkey, Iceland, New Zealand, Japan, and the western United States. Rafts of floating pumice from undersea eruptions can drift across entire oceans.

How to identify it

Look for a very lightweight, pale (white, grey, cream) rock riddled with tiny holes and a frothy, spongy texture. The signature test is that genuine pumice often floats on water because of its trapped air.

It feels abrasive and gritty and crumbles easily. Under a lens you see a glassy, foam-like network of thin walls between bubbles.

Look-alikes include scoria (darker red-brown to black, denser, larger bubbles, usually sinks), and vesicular basalt (heavier, dark, holes but solid rock between them). Pumice's pale color, extreme lightness, and ability to float are the clearest identifiers.

Uses & significance

Pumice is widely used as an abrasive and lightweight aggregate. Ground pumice goes into cleaning products, polishes, exfoliating soaps, and the classic pumice stone for removing calluses and dead skin. Stonewashed denim is famously softened with pumice.

As a lightweight aggregate it is added to concrete, building blocks, and insulation, and it is used horticulturally to improve soil drainage and aeration. It also serves as a filtration and absorbent medium.

Geologically, pumice and pumice ash layers are valuable markers for dating and correlating volcanic eruptions and for reconstructing the explosive history of volcanoes.

Frequently asked questions

Why does pumice float?

It is full of interconnected gas bubbles trapped when frothy lava quenched to glass, making it so porous and light that air keeps it afloat until water slowly fills the pores.

Is pumice a rock or glass?

It is a volcanic rock that is also a natural glass, because it cooled too quickly for crystals to grow, leaving an amorphous, foamy silicate.

What is the difference between pumice and scoria?

Pumice is pale, very light, finely vesicular, and usually floats, while scoria is darker, denser, has larger bubbles, and generally sinks.

Is pumice safe to use on skin?

Yes, natural pumice stones are commonly used to gently remove calluses and rough skin, though they should be used lightly and kept clean to avoid irritation.

Pumice identified by the community

Real specimens identified with Rock Identifier.

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