Pumice is a highly vesicular, low-density volcanic glass formed during explosive eruptions of silica-rich magma. It is unique for its ability to float on water due to its porous structure and is commonly found in association with rhyolitic lava flows.
Is this pumice?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch pumice with a known reference. Pumice sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pumice leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pumice typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, gray, cream, light brown.
- 5Look at form & habitTypical habit: vesicular.
Often confused with
Pumice vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pumice
Minerals reported to co-occur with pumice. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 5.5-6
- Density
- 0.25-0.9 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Vesicular
- Cleavage
- None
- Rarity
- Common
- Uses
- Industrial, Decorative, Lapidary
- Host rock
- Volcanic Extrusive
- Typical price
- $1-20 per specimen
Where rockhounds find pumice
1 mapped spotsClassic worldwide localities
- Italy
- Greece
- United States
- New Zealand
- Turkey
Field-hunting tip
Look in volcanic extrusive country, the host setting where pumice typically forms. If you start seeing obsidian, rhyolite, trachyte in float, you are in the right ground. Field specimens usually show a vesicular habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Nevada. Start trip planning there.




