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.
- 2Read the textureLook at a fresh break with a hand lens. Texture: Extremely vesicular and rough-textured. Grain size: Glassy.
- 3Pick out the mineralsComposition: Highly microvesicular volcanic glass, which may contain crystals. Identify the two or three most abundant grains.
- 4Read the lusterHold the specimen under a strong light. Luster: dull.
- 5Match the color rangeCompare against the expected color range: white, gray, cream, light brown.
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
- Luster
- Dull
- Transparency
- Opaque
- Rarity
- Common
- Uses
- Industrial, Decorative, Lapidary
- Host rock
- volcanic extrusive
- Texture
- Extremely vesicular and rough-textured
- Grain size
- Glassy
- Composition
- Highly microvesicular volcanic glass, which may contain crystals
Where rockhounds find pumice
1 mapped spotsClassic worldwide localities
- Italy
- Greece
- United States
- New Zealand
- Turkey
Field-hunting tip
Where it forms: volcanic extrusive. If you start seeing obsidian, rhyolite, trachyte in float, you are in the right ground. In the U.S., the densest reported localities are in Nevada. Start trip planning there.




