What is Pumice?
Pumice is a light-colored, extremely porous igneous rock that forms during explosive volcanic eruptions. It is used as aggregate in
lightweight concrete, as landscaping aggregate, and as an abrasive in a variety of industrial and consumer products.
Many specimens have a high enough porosity that they can float on water until they slowly become waterlogged.
How Does Pumice Form?
The pore spaces (known as vesicles) in pumice are a clue to how it forms. The vesicles are actually gas bubbles that were trapped in the rock
during the rapid cooling of a gas-rich frothy magma.
Some magmas contain several percent dissolved gas by weight while they are under pressure. Stop for a moment and think about that.
Gas weighs very little at Earth's surface, but these magmas under pressure can contain several percent gas by weight held in solution.
This is similar to the large amount of dissolved carbon dioxide in a sealed bottle of carbonated beverage such as beer or soda. If
you shake the container, then immediately open the bottle, the sudden release of pressure allows the gas to come
out of solution, and the beverage erupts from the container in a frothy mess.
A rising body of magma, supercharged with dissolved gas under pressure, behaves in a similar way. As the magma breaks through Earth's surface, the sudden pressure drop causes the gas to come out of solution. This is what produces the enormous rush of high-pressure gas from the vent.
This rush of gas from the vent shreds the magma and blows it out as a molten froth. The froth rapidly solidifies as it flies through the air and falls back
to Earth as pieces of pumice. The largest volcanic eruptions can eject many cubic kilometers of material. This material can range in size from tiny
dust particles to large blocks of pumice the size of a house.
Large eruptions can blanket the landscape around the volcano with over 100 meters of pumice and launch dust and ash high into the atmosphere.
The sections below give quotations from United States Geological Survey reports describing the production of pumice at two major eruptions.
Gas and Pumice at the Pinatubo Eruption
The second most powerful volcanic eruption of the 20th century was at Mount Pinatubo in 1991. The description below explains how enormous volumes of dissolved
gas powered the eruption and how a cubic mile of ash and pumice lapilli was blasted from the volcano.
"From June 7 to 12, the first magma reached the surface of Mount Pinatubo. Because it had lost most of the gas contained in it on the way to the surface, the magma oozed out to form a lava dome but did not cause an explosive eruption. However, on June 12, millions of cubic yards of gas-charged magma reached the surface and exploded in the reawakening volcano's first spectacular eruption.
When even more highly gas charged magma reached Pinatubo's surface on June 15, the volcano exploded in a cataclysmic eruption that ejected more than 1 cubic mile of material. [...] A blanket of volcanic ash and pumice lapilli blanketed the countryside.
Huge avalanches of searing hot ash, gas, and pumice roared down the flanks of Mount Pinatubo, filling once-deep valleys with fresh volcanic deposits as much as 660 feet thick. The eruption removed so much magma and rock from below the volcano that the summit collapsed to form a large volcanic depression 1.6 miles across." 
Mount Mazama Eruption (Crater Lake)
"The cataclysmic eruption of Mount Mazama 7,700 years ago started from a single vent on the northeast side of the volcano as a towering column of pumice and ash that reached some 30 miles high. Winds carried the ash across much of the Pacific Northwest and parts of southern Canada. So much magma erupted that the volcano began to collapse in on itself. As the summit collapsed, circular cracks opened up around the peak. More magma erupted through these cracks to race down the slopes as pyroclastic flows. Deposits from these flows partially filled the valleys around Mount Mazama with up to 300 feet of pumice and ash. As more magma was erupted, the collapse progressed until the dust settled to reveal a volcanic depression, called a caldera, 5 miles in diameter and one mile deep." 
Composition of Pumice
Most pumice erupts from magmas that are highly charged with gas and have a rhyolitic composition.
Rarely, pumice can erupt from gas-charged magmas of basaltic or andesitic composition.
Pumice Has a Very Low Specific Gravity
The abundant vesicles in pumice and the thin walls between them give the rock a very low specific gravity.
It typically has a specific gravity of less than one, giving the rock an ability to float on water.
Large amounts of pumice produced by some island and subsea eruptions will float on the surface and be pushed about by the
winds. The pumice can float for long periods of time - sometimes years - before it finally becomes waterlogged
and sinks. Large masses of floating pumice are known as "pumice rafts." They are large enough to be tracked by
satellites and are a hazard to ships that sail through them (see images at right).
Uses of Pumice
The largest use of pumice in the United States is the production of lightweight concrete blocks and other lightweight concrete products. When this concrete is mixed, the vesicles
remain partially filled with air. That reduces the weight of the block. Lighter blocks can reduce the
structural steel requirements of a building or reduce the foundation requirements. The trapped air also gives the blocks
a greater insulating value.
The second most common use of pumice is in landscaping and horticulture. The pumice is used as a decorative ground
cover in landscaping and planters. It is used as drainage rock and soil conditioner in plantings. Pumice and scoria are also popular rocks for use as substrates in hydroponic gardening.
Pumice has many other uses. Together these account for less than a few percent of consumption in the United States,
but these are the products that most people think of when they hear the word "pumice."
Lots of people have found small pumice pebbles in the pockets of brand new "stone washed jeans," and almost
everyone has seen the famous "Lava Soap" that uses pumice as an abrasive.
Below we list these and some of the other minor uses of pumice (in no particular order).
- an abrasive in conditioning "stone washed" denim
- an abrasive in bar and liquid soaps such as "Lava Soap"
- an abrasive in pencil erasers
- an abrasive in skin exfoliating products
- a fine abrasive used for polishing
- a traction material on snow-covered roads
- a traction enhancer in tire rubber
- an absorbent in cat litter
- a fine-grained filter media
- a lightweight filler for pottery clay
Pumice and Pumicite Production
Pumice is produced in two forms: rock pumice and pumicite. "Pumicite" is a name given to very fine grained pumice
(less than 4 millimeters in diameter down to submillimeter sizes). The word can be used synonymously with "volcanic ash."
It is mined from volcanic ash deposits or it can be produced by crushing rock pumice.
About 500,000 metric tons of pumice and pumicite were mined in the United States in 2011. The total value of this pumice was about
$11,200,000 or an average of about $23 per ton at the mine. The producing states were, in order of decreasing production:
- New Mexico
Imported Pumice and Substitutes
All of the pumice production in the United States occurs west of the Mississippi River. In 2011, most of the pumice for consumption in the eastern United
States was imported from Greece.
In the eastern United States, expanded aggregate, produced by heating specific types
of shale under controlled conditions, is used as a substitute for pumice in lightweight aggregate, horticultural and
Contributor: Hobart King
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|A pyroclastic flow will sometimes contain large pieces of pumice. This photograph shows a USGS scientist examining blocks of pumice at the toe of a pyroclastic flow at Mount St. Helens. Image by Terry Leighley, Sandia Labs.|
|The explosive eruption of Mount Pinatubo in the Philippines on June 12, 1991 ejected more than five cubic kilometers of material and was rated as a VEI 5 eruption on the volcanic explosivity index. Much of that material was pumice lapilli (see image below) that blanketed the landscape around the volcano. USGS image.
|Dacitic pumice fragments erupted by Mount Pinatubo, Philippines, during an enormous eruption on 15 June 1991. Photo by W.E. Scott, USGS image.|
| A variety of health and beauty products that contain pumice. They include the famous "Lava Soap" that cleans dirty hands with tiny pieces of pumice abrasive, a foot scrub cream that works as an exfoliant to smooth "sandal feet," two pumice stones, and a sponge with embedded pumice abrasive.
| Some of the concrete used to construct the Pantheon by the Romans in 126 AD was lightweight material made with pumice aggregate. Photography by Roberta Dragan, used under a Creative Commons license.
|A "raft" of lightweight pumice floating on the surface of the South Pacific after an eruption in the Tonga Islands. NASA image.|
|View of a pumice raft from a boat. Waves can be seen moving under the pumice. The rafts can float for years until all of the pumice becomes waterlogged and sinks or it is dissipated by waves and wind. USGS image.
|Reticulite is a basaltic pumice in which all of the bubbles have burst, leaving a honeycomb structure. Photograph by J.D. Griggs, USGS image.|
| Photograph of stratified pumice deposit produced by pyroclastic flows at Mount St. Helens, Washington. USGS image by L. Topinka.
 The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines:
Chris Newhall, James W. Hendley II, and Peter H. Stauffer; United States Geological Survey Fact Sheet 113-97, published 1997.
 Mount Mazama and Crater Lake: Growth and Destruction of a Cascade Volcano:
Ed Klimasauskas, Charles Bacon, and Jim Alexander; United States Geological Survey Fact Sheet 092-02, published 2002.
 New Island and Pumice Raft in the Tongas: Earth Observatory image from NASA, November 16, 2006.
 Maritime Impacts of Volcanic Eruptions: A Guide for the Prudent Mariner, National Weather Service, Ocean Prediction Center, NOAA, website accessed March 2013.
 Pumice and Pumicite: Robert D. Crangle, Jr., 2011 Minerals Yearbook, United States Geological Survey, August 2012.