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 — that is 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.




